bigfootjim.com

As much as I would like some understanding, I will not risk the friendship between 2 young ladies whom I adore, and love like they were my own, for my benefit.  Because when I say I love someone, I mean it.  With every bit of my heart.  I do not see them as objects to be used, or puppets for people’s games.  I will live with the regret and unanswered questions, before allowing someone to break that bond, or teach another little one that people and relationships are only useful for personal gain, and so easily disposable.

Threatening 11 y/o girls and using them as pawns.  That is all the understanding I need right now, to know that someone is not worthy of my effort.  I am sorry I wasted 9 months of my time, trying to remind someone of what it was like before their hatchet wielding mind started chopping it to pieces.  I’m sorry I believed in someone so much, that I compromised across the board to demonstrate true loyalty, to someone that knows so little of it.

This site will not receive any major updates prior to 20310418.
In Tempore Veritas…

🧠

20250625

20250619

20250614

20250611

Zion National Park is a national park of the United States located in southwestern Utah near the town of Springdale. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park’s four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. The lowest point in the park is 3,666 ft (1,117 m) at Coalpits Wash and the highest peak is 8,726 ft (2,660 m) at Horse Ranch Mountain. A prominent feature of the 229-square-mile (590 km²) park is Zion Canyon, which is 15 miles (24 km) long and up to 2,640 ft (800 m) deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River. The park attracted 5 million visitors in 2023.

Human habitation of the area started about 8,000 years ago with small family groups of Native Americans, one of which was the semi-nomadic Basketmaker Ancestral Puebloans (who used to be called Anasazi by early non-indigenous archeologists) (c. 300 CE). Subsequently, what has been called the Virgin Anasazi culture (c. 500) and the Parowan Fremont group developed as the Basketmakers settled in permanent communities. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s.

In 1909, President William Howard Taft named the area Mukuntuweap National Monument in order to protect the canyon. In 1918, the acting director of the newly created National Park Service, Horace Albright, drafted a proposal to enlarge the existing monument and change the park’s name to Zion National Monument, Zion being a term used by the Mormons. According to historian Hal Rothman: “The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience.” On November 19, 1919, Congress redesignated the monument as Zion National Park, and the act was signed by President Woodrow Wilson. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the national park in 1956. Congress designated 85% of the park a wilderness area in 2009.

The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateau lifted the region 10,000 feet (3,000 m) starting 13 million years ago.

As stated in the foundation document:

The purpose of Zion National Park is to preserve the dramatic geology including Zion Canyon and a labyrinth of deep and brilliantly colored Navajo sandstone canyons formed by extraordinary processes of erosion at the margin of the Colorado Plateau; to safeguard the park’s wilderness character and its wild and scenic river values; to protect evidence of human history; and to provide for scientific research and the enjoyment and enlightenment of the public.

The park is located in southwestern Utah mostly in unincorporated areas in Washington, Iron, and Kane counties. The territory of Springdale extends into the park.

Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: the Colorado Plateau, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15, exit 40.

The 8,726-foot (2,660 m) summit of Horse Ranch Mountain is the highest point in the park; the lowest point is the 3,666-foot (1,117 m) elevation of Coal Pits Wash, creating a relief of about 5,100 feet (1,600 m).

Streams in the area take rectangular paths because they follow jointing planes in the rocks. The stream gradient of the Virgin River, whose North Fork flows through Zion Canyon in the park, ranges from 50 to 80 feet per mile (9.5 to 15.2 m/km) (0.9–1.5%)—one of the steepest stream gradients in North America.

The road into Zion Canyon is 6 miles (9.7 km) long, ending at the Temple of Sinawava, which is named for the coyote god of the Paiute Indians. The canyon becomes more narrow near the Temple and a hiking trail continues to the mouth of The Narrows, a gorge only 20 feet (6 m) wide and up to 2,000 feet (610 m) tall. The Zion Canyon road is served by a free shuttle bus from early April to late October and by private vehicles the other months of the year. Other roads in Zion are open to private vehicles year-round.

The east side of the park is served by Zion – Mount Carmel Highway (SR-9), which passes through the Zion – Mount Carmel Tunnel and ends at US 89 at Mount Carmel Junction. Park features on the east side of the park include Checkerboard Mesa and The East Temple.

The Kolob Terrace area, northwest of Zion Canyon, features a slot canyon called The Subway, and a panoramic view of the entire area from Lava Point. The Kolob Canyons section, further to the northwest near Cedar City, features Tucupit Point and one of the world’s longest natural arches, Kolob Arch.

Other notable geographic features of Zion Canyon include Angels Landing, The Great White Throne, the Court of the Patriarchs, The Sentinel, The West Temple, Towers of the Virgin, the Altar of Sacrifice, The Watchman, Weeping Rock, and the Emerald Pools.

Spring weather is unpredictable, with stormy, wet days being common, mixed with occasional warm, sunny weather. Precipitation is normally heaviest in March. Spring wildflowers bloom from April through June, peaking in May. Fall days are usually clear and mild; nights are often cool. Summer days are hot (95 to 110 °F; 35 to 43 °C), but overnight lows are usually comfortable (65 to 70 °F; 18 to 21 °C). Afternoon thunderstorms are common from mid-July through mid-September. Storms may produce waterfalls as well as flash floods. Autumn tree-color displays begin in September in the high country; in Zion Canyon, autumn colors usually peak in late October. Winter in Zion Canyon is fairly mild. Winter storms bring rain or light snow to Zion Canyon and heavier snow to the higher elevations. Clear days may become quite warm, reaching 60 °F (16 °C); nights are often 20 to 40 °F (−7 to 4 °C). Winter storms can last several days and make roads icy. Zion roads are plowed, except the Kolob Terrace Road which is closed when covered with snow. Winter driving conditions last from November through March.

Climate

Zion National Park has a BSk (Köppen climate classification) cold semi-arid climate consisting of very hot summers and mild winters with a limited amount of precipitation throughout the year.

History

Archaeologists have divided the long span of Zion’s human history into three cultural periods: the Archaic, Protohistoric and Historic periods. Each period is characterized by distinctive technological and social adaptations.

The first human presence in the region dates to 8,000 years ago when family groups camped where they could hunt or collect plants and seeds. About 2,000 years ago, some groups began growing corn and other crops, leading to an increasingly sedentary lifestyle. Later groups in this period built permanent villages called pueblos. Archaeologists call this the Archaic period and it lasted until c. 500. Baskets, cordage nets, and yucca fiber sandals have been found and dated to this period. The Archaic toolkits included flaked stone knives, drills, and stemmed dart points. The dart points were attached to wooden shafts and propelled by throwing devices called atlatls.

By c. 300, some of the archaic groups developed into an early branch of seminomadic Anasazi, the Basketmakers. Basketmaker sites have grass- or stone-lined storage cists and shallow, partially underground dwellings called pithouses. They were hunters and gatherers who supplemented their diet with limited agriculture. Locally collected pine nuts were important for food and trade.

20250607

Just a break from random articles for a little update.  Saw another solid month according to the stats; thank you.  And while I can’t be bothered to go through them all, because I honestly don’t care, I’m almost certain the babysitters are among them.  So while it has been explained elsewhere, I will remind those of you here again that there will be nothing more shared on this site.  You all need to understand that if I am content being silenced here, that it really is for the best of reasons.  And while the threat made against the children is a very big part of that, it isn’t the only reason.  I gave my word about sharing things on this site, and I believe that it will be important for my friend’s children to see what actual integrity, and genuine loyalty, to my friend, and them, looks like.

I also agreed not to share anything here so as not to diminish the work of the professional, because I have complete faith in her efforts and goals.  While I am frustrated at the time she is taking, I understand and appreciate how thorough she has been.  Honestly, she’s like a bloodhound, chasing down everything she can.  Where I saw and focused on a handful of obvious things, she’s dissected things down to the DNA level.  If you’ve never witnessed how women can take apart someone’s bullshit with laser like precision, I don’t know what to tell you.  Her work so far has been enlightening, to say the least, and I probably wouldn’t have agreed to work with her had I not been silenced here.  So again, it’s for the best.

Other things in the works still.  If anybody is a graphics artist, I’m looking for someone to do some pro bono, or at least reasonably priced, graphics work for the new adventures project while I get it up and running.  Hit the contact page if you can help.  I’ve got some trips planned over the next month that will kick things off.

That’s it for now.  Thank you all.

20250601

Death Valley National Park is a national park of the United States that straddles the California–Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley, the northern section of Panamint Valley, the southern section of Eureka Valley and most of Saline Valley.

The park occupies an interface zone between the arid Great Basin and Mojave deserts, protecting the northwest corner of the Mojave Desert and its diverse environment of salt-flats, sand dunes, badlands, valleys, canyons and mountains.

Death Valley is the largest national park in the contiguous United States, as well as the hottest, driest and lowest of all the national parks in the United States. It contains Badwater Basin, the second-lowest point in the Western Hemisphere and lowest in North America at 282 feet (86 m) below sea level. More than 93% of the park is a designated wilderness area.

The park is home to many species of plants and animals which have adapted to the harsh desert environment including creosote bush, Joshua tree, bighorn sheep, coyote, and the endangered Death Valley pupfish, a survivor from much wetter times. UNESCO included Death Valley as the principal feature of its Mojave and Colorado Deserts Biosphere Reserve in 1984.

A series of Native American groups inhabited the area from as early as 7000 BC, most recently the Timbisha around 1000 AD who migrated between winter camps in the valleys and summer grounds in the mountains. A group of European-Americans, lost in the valley in 1849 while looking for a shortcut to the gold fields of California, gave this valley its grim name, even though only one of their group died there.

Several short-lived boom towns sprang up during the late 19th and early 20th centuries to mine gold and silver. The only long-term profitable ore to be mined was borax, which was transported out of the valley with twenty-mule teams. The valley later became the subject of books, radio programs, television series, and movies. Tourism expanded in the 1920s when resorts were built around Stovepipe Wells and Furnace Creek. Death Valley National Monument was declared in 1933 and the park was substantially expanded and became a national park in 1994.

The natural environment of the area has been shaped largely by its geology. The valley is actually a graben with the oldest rocks being extensively metamorphosed and at least 1.7 billion years old. Ancient, warm, shallow seas deposited marine sediments until rifting opened the Pacific Ocean. Additional sedimentation occurred until a subduction zone formed off the coast. The subduction uplifted the region out of the sea and created a line of volcanoes. Later the crust started to pull apart, creating the current Basin and Range landform. Valleys filled with sediment and, during the wet times of glacial periods, with lakes, such as Lake Manly.

Death Valley is the fifth-largest American national park and the largest in the contiguous United States. It is also larger than the states of Rhode Island and Delaware combined, and nearly as large as Puerto Rico. In 2013, Death Valley National Park was designated as a dark sky park by the International Dark-Sky Association.

There are two major valleys in the park, Death Valley and Panamint Valley. Both of these valleys were formed within the last few million years and both are bounded by north–south-trending mountain ranges. These and adjacent valleys follow the general trend of Basin and Range topography with one modification: there are parallel strike-slip faults that perpendicularly bound the central extent of Death Valley. The result of this shearing action is additional extension in the central part of Death Valley which causes a slight widening and more subsidence there.

Uplift of surrounding mountain ranges and subsidence of the valley floor are both occurring. The uplift on the Black Mountains is so fast that the alluvial fans (fan-shaped deposits at the mouth of canyons) there are small and steep compared to the huge alluvial fans coming off the Panamint Range. Fast uplift of a mountain range in an arid environment often does not allow its canyons enough time to cut a classic V-shape all the way down to the stream bed. Instead, a V-shape ends at a slot canyon halfway down, forming a ‘wine glass canyon.’ Sediment is deposited on a small and steep alluvial fan.

At 282 feet (86 m) below sea level at its lowest point, Badwater Basin on Death Valley’s floor is the second-lowest depression in the Western Hemisphere (behind Laguna del Carbón in Argentina), while Mount Whitney, only 85 miles (137 km) to the west, rises to 14,505 feet (4,421 m) and is the tallest mountain in the contiguous United States. This topographic relief is the greatest elevation gradient in the contiguous United States and is the terminus point of the Great Basin’s southwestern drainage. Although the extreme lack of water in the Great Basin makes this distinction of little current practical use, it does mean that in wetter times the lake that once filled Death Valley (Lake Manly) was the last stop for water flowing in the region, meaning the water there was saturated in dissolved materials. Thus, the salt pans in Death Valley are among the largest in the world and are rich in minerals, such as borax and various salts and hydrates. The largest salt pan in the park extends 40 miles (64 km) from the Ashford Mill Site to the Salt Creek Hills, covering some 200 square miles (520 km²) of the valley floor. The best known playa in the park is the Racetrack, known for its moving rocks.

According to the Köppen climate classification system, Death Valley National Park has a hot desert climate (BWh). The plant hardiness zone at Badwater Basin is 9b with an average annual extreme minimum temperature of 28.0 °F (−2.2 °C).

Death Valley is the hottest and driest place in North America due to its lack of surface water and low relief. It is so frequently the hottest spot in the United States that many tabulations of the highest daily temperatures in the country omit Death Valley as a matter of course.

On the afternoon of July 10, 1913, the United States Weather Bureau recorded a high temperature of 134 °F (57 °C) at Greenland Ranch (now Furnace Creek) in Death Valley. This temperature stands as the highest ambient air temperature ever recorded at the surface of the Earth. (A report of a temperature of 58 °C (136 °F) recorded in Libya in 1922 was later determined to be inaccurate.) Daily summer temperatures of 120 °F (49 °C) or greater are common, as well as below freezing nightly temperatures in the winter. July is the hottest month, with an average high of 117 °F (47 °C) and an average low of 91 °F (33 °C). December is the coldest month, with an average high of 66 °F (19 °C) and an average low of 41 °F (5 °C). The record low is 15 °F (−9.4 °C). There are an average of 197.3 days annually with highs of 90 °F (32.2 °C) or higher and 146.9 days annually with highs of 100 °F (37.8 °C) or higher. Freezing temperatures of 32 °F (0 °C) or lower occur on an average of 8.6 days annually.

Several of the larger Death Valley springs derive their water from a regional aquifer, which extends as far east as southern Nevada and Utah. Much of the water in this aquifer has been there for many thousands of years, since the Pleistocene ice ages, when the climate was cooler and wetter. Today’s drier climate does not provide enough precipitation to recharge the aquifer at the rate at which water is being withdrawn.

The highest range within the park is the Panamint Range, with Telescope Peak being its highest point at 11,049 feet (3,368 m). The Death Valley region is a transitional zone in the northernmost part of the Mojave Desert and consists of five mountain ranges removed from the Pacific Ocean. Three of these are significant barriers: the Sierra Nevada, the Argus Range, and the Panamint Range. Air masses tend to lose moisture as they are forced up over mountain ranges, in what climatologists call a rainshadow effect.

The exaggerated rain shadow effect for the Death Valley area makes it North America’s driest spot, receiving about 1.5 inches (38 mm) of rainfall annually at Badwater, and some years fail to register any measurable rainfall. Annual average precipitation varies from 1.92 inches (49 mm) overall below sea level to over 15 inches (380 mm) in the higher mountains that surround the valley. When rain does arrive it often does so in intense storms that cause flash floods which remodel the landscape and sometimes create very shallow ephemeral lakes.

The hot, dry climate makes it difficult for soil to form. Mass wasting, the down-slope movement of loose rock, is therefore the dominant erosive force in mountainous areas, resulting in “skeletonized” ranges (mountains with very little soil on them). Sand dunes in the park, while famous, are not nearly as widespread as their fame or the dryness of the area may suggest. The Mesquite Flat dune field is the most easily accessible from the paved road just east of Stovepipe Wells in the north-central part of the valley and is primarily made of quartz sand. Another dune field is just 10 miles (16 km) to the north but is instead mostly composed of travertine sand. The highest dunes in the park, and some of the highest in North America, are located in the Eureka Valley about 50 miles (80 km) to the north of Stovepipe Wells, while the Panamint Valley dunes and the Saline Valley dunes are located west and northwest of the town, respectively. The Ibex dune field is near the seldom-visited Ibex Hill in the southernmost part of the park, just south of the Saratoga Springs marshland. All the latter four dune fields are accessible only via unpaved roads. Prevailing winds in the winter come from the north, and prevailing winds in the summer come from the south. Thus, the overall position of the dune fields remains more or less fixed.

There are rare exceptions to the dry nature of the area. In 2005, an unusually wet winter created a ‘lake’ in the Badwater Basin and led to the greatest wildflower season in the park’s history. In October 2015, a “1000 year flood event” with over three inches of rain caused major damage in Death Valley National Park. A similar widespread storm in August 2022 damaged pavement and deposited debris on nearly every road, trapping 1,000 residents and visitors overnight.

Human history

Four Native American cultures are known to have lived in the area during the last 10,000 years. The first known group, the Nevares Spring People, were hunters and gatherers who arrived in the area perhaps 9,000 years ago (7000 BC) when there were still small lakes in Death Valley and neighboring Panamint Valley. A much milder climate persisted at that time, and large game animals were still plentiful. By 5,000 years ago (3000 BC) the Mesquite Flat People displaced the Nevares Spring People. Around 2,000 years ago the Saratoga Spring People moved into the area, which by then was probably already a hot, dry desert. This culture was more advanced at hunting and gathering and was skillful at handcrafts. They also left mysterious stone patterns in the valley.

One thousand years ago, the nomadic Timbisha (formerly called Shoshone and also known as Panamint or Koso) moved into the area and hunted game and gathered mesquite beans along with pinyon pine nuts. Because of the wide altitude differential between the valley bottom and the mountain ridges, especially on the west, the Timbisha practiced a vertical migration pattern. Their winter camps were located near water sources in the valley bottoms. As the spring and summer progressed and the weather warmed, grasses and other plant food sources ripened at progressively higher altitudes. November found them at the very top of the mountain ridges where they harvested pine nuts before moving back to the valley bottom for winter.

The California Gold Rush brought the first people of European descent known to visit the immediate area. In December 1849 two groups of California Gold Country-bound travelers with perhaps 100 wagons total stumbled into Death Valley after getting lost on what they thought was a shortcut off the Old Spanish Trail. Called the Bennett-Arcane Party, they were unable to find a pass out of the valley for weeks; they were able to find fresh water at various springs in the area, but were forced to eat several of their oxen to survive. They used the wood of their wagons to cook the meat and make jerky. The place where they did this is today referred to as “Burnt Wagons Camp” and is located near Stovepipe Wells.

After abandoning their wagons, they eventually were able to hike out of the valley. Just after leaving the valley, one of the women in the group turned and said, “Goodbye Death Valley,” giving the valley its name. Included in the party was William Lewis Manly whose autobiographical book Death Valley in ’49 detailed this trek and popularized the area (geologists later named the prehistoric lake that once filled the valley after him).

The ores that are most famously associated with the area were also the easiest to collect and the most profitable: evaporite deposits such as salts, borate, and talc. Borax was found by Rosie and Aaron Winters near The Ranch at Death Valley (then called Greenland) in 1881. Later that same year, the Eagle Borax Works became Death Valley’s first commercial borax operation. William Tell Coleman built the Harmony Borax Works plant and began to process ore in late 1883 or early 1884, continuing until 1888. This mining and smelting company produced borax to make soap and for industrial uses. The end product was shipped out of the valley 165 miles (266 km) to the Mojave railhead in 10-ton-capacity wagons pulled by “twenty-mule teams” that were actually teams of 18 mules and two horses each.

The teams averaged two miles (3.2 km) an hour and required about 30 days to complete a round trip. The trade name 20-Mule Team Borax was established by Francis Marion Smith’s Pacific Coast Borax Company after Smith acquired Coleman’s borax holdings in 1890. A memorable advertising campaign used the wagon’s image to promote the Boraxo brand of granular hand soap and the Death Valley Days radio and television programs. In 1914, the Death Valley Railroad was built to serve mining operations on the east side of the valley. Mining continued after the collapse of Coleman’s empire, and by the late 1920s the area was the world’s number one source of borax. Some four to six million years old, the Furnace Creek Formation is the primary source of borate minerals gathered from Death Valley’s playas.

Other visitors stayed to prospect for and mine deposits of copper, gold, lead, and silver. These sporadic mining ventures were hampered by their remote location and the harsh desert environment. In December 1903, two men from Ballarat were prospecting for silver. One was an out-of-work Irish miner named Jack Keane and the other was a one-eyed Basque butcher named Domingo Etcharren. Quite by accident, Keane discovered an immense ledge of free-milling gold by the duo’s work site and named the claim the Keane Wonder Mine. This started a minor and short-lived gold rush into the area. The Keane Wonder Mine, along with mines at Rhyolite, Skidoo and Harrisburg, were the only ones to extract enough metal ore to make them worthwhile. Outright shams such as Leadfield also occurred, but most ventures quickly ended after a short series of prospecting mines failed to yield evidence of significant ore (these mines now dot the entire area and are a significant hazard to anyone who enters them). The boom towns which sprang up around these mines flourished during the first decade of the 1900s, but soon declined after the Panic of 1907.

The first documented tourist facilities in Death Valley were a set of tent houses built in the 1920s where Stovepipe Wells is now located. People flocked to resorts built around natural springs thought to have curative and restorative properties. In 1927, Pacific Coast Borax turned the crew quarters of its Furnace Creek Ranch into a resort, creating the Furnace Creek Inn and resort. The spring at Furnace Creek was harnessed to develop the resort, and as the water was diverted, the surrounding marshes and wetlands started to shrink.

Soon the valley was a popular winter destination. Other facilities started off as private getaways but were later opened to the public. Most notable among these was Death Valley Ranch, better known as Scotty’s Castle. This large ranch home built in the Spanish Revival style became a hotel in the late 1930s and, largely because of the fame of Death Valley Scotty, a tourist attraction. Death Valley Scotty, whose real name was Walter Scott, was a gold miner who pretended to be the owner of “his castle”, which he claimed to have built with profits from his gold mine. Neither claim was true, but the real owner, Chicago millionaire Albert Mussey Johnson, encouraged the myth. When asked by reporters what his connection was to Walter Scott’s castle, Johnson replied that he was Mr. Scott’s banker.

President Herbert Hoover proclaimed a national monument in and around Death Valley on February 11, 1933, setting aside almost two million acres (8,100 km²) of southeastern California and small parts of Nevada.

The Civilian Conservation Corps (CCC) developed infrastructure in Death Valley National Monument during the Great Depression and on into the early 1940s. The CCC built barracks, graded 500 miles (800 km) of roads, installed water and telephone lines, and a total of 76 buildings. Trails in the Panamint Range were built to points of scenic interest, and an adobe village, laundry and trading post were constructed for the Timbisha Shoshone Tribe. Five campgrounds, restrooms, an airplane landing field and picnic facilities were also built.

The creation of the monument resulted in a temporary closing of the lands to prospecting and mining. However, Death Valley was quickly reopened to mining by Congressional action in June 1933. As improvements in mining technology allowed lower grades of ore to be processed, and new heavy equipment allowed greater amounts of rock to be moved, mining in Death Valley changed. Gone were the days of the “single-blanket, jackass prospector” long associated with the romantic west. Open pit and strip mines scarred the landscape as international mining corporations bought claims in highly visible areas of the national monument. The public outcry that ensued led to greater protection for all national park and monument areas in the United States. In 1976, Congress passed the Mining in the Parks Act, which closed Death Valley National Monument to the filing of new mining claims, banned open-pit mining and required the National Park Service to examine the validity of tens of thousands of pre-1976 mining claims. Mining was allowed to resume on a limited basis in 1980 with stricter environmental standards. The last mine in the park, Billie Mine, closed in 2005.

In 1952 President Harry Truman added the Devils Hole to Death Valley National Monument; it is the only habitat of the Devils Hole pupfish.

Death Valley National Monument was designated a biosphere reserve in 1984. On October 31, 1994, the monument was expanded by 1.3 million acres (5,300 km²) and re-designated as a national park, via congressional passage of the California Desert Protection Act (Public Law 103–433). Consequently, the elevated status for Death Valley made it the largest national park in the contiguous United States. On March 12, 2019, the John D. Dingell, Jr. Conservation, Management, and Recreation Act added 35,292 acres (55 sq mi; 143 km²) to the park.

Many of the larger cities and towns within the boundary of the regional groundwater flow system that the park and its plants and animals rely upon are experiencing some of the fastest growth rates of any place in the United States. Notable examples within a 100-mile (160 km) radius of Death Valley National Park include Las Vegas and Pahrump, Nevada. In the case of Las Vegas, the local Chamber of Commerce estimates that 6,000 people are moving to the city every month. Between 1985 and 1995, the population of the Las Vegas Valley increased from 550,700 to 1,138,800.

In 1977, parts of Death Valley were used by director George Lucas as a filming location for Star Wars, providing the setting for the fictional planet Tatooine.

The park has a diverse and complex geologic history. Since its formation, the area that comprises the park has experienced at least four major periods of extensive volcanism, three or four periods of major sedimentation, and several intervals of major tectonic deformation where the crust has been reshaped. Two periods of glaciation (a series of ice ages) have also had effects on the area, although no glaciers ever existed in the ranges now in the park.

Little is known about the history of the oldest exposed rocks in the area due to extensive metamorphism (alteration of rock by heat and pressure). Radiometric dating gives an age of 1,700 million years for the metamorphism during the Proterozoic. About 1,400 million years ago a mass of granite now in the Panamint Range intruded this complex. Uplift later exposed these rocks to nearly 500 million years of erosion.

The Proterozoic sedimentary formations of the Pahrump Group were deposited on these basement rocks. This occurred following uplift and erosion of any earlier sediments from the Proterozoic basement rocks. The Pahrump is composed of arkose conglomerate (quartz clasts in a concrete-like matrix) and mudstone in its lower part, followed by dolomite from carbonate banks topped by algal mats as stromatolites, and finished with basin-filling sediment derived from the above, including possible glacial till from the hypothesized Snowball Earth glaciation. The very youngest rocks in the Pahrump Group are basaltic lava flows.

A rift opened and subsequently flooded the region as part of the breakup of the supercontinent Rodinia in the Neoproterozoic (by about 755 million years ago) and the creation of the Pacific Ocean. A shoreline similar to the present Atlantic Ocean margin of the United States lay to the east. An algal mat-covered carbonate bank was deposited, forming the Noonday Dolomite. Subsidence of the region occurred as the continental crust thinned and the newly formed Pacific widened, forming the Ibex Formation. An angular unconformity (an uneven gap in the geologic record) followed.

A true ocean basin developed to the west, breaking all the earlier formations along a steep front. A wedge of clastic sediment then began to accumulate at the base of the two underwater precipices, starting the formation of opposing continental shelves. Three formations developed from sediment that accumulated on the wedge. The region’s first known fossils of complex life are found in the resulting formations. Notable among these are the Ediacara fauna and trilobites, the evolution of the latter being part of the Cambrian Explosion of life.

The sandy mudflats gave way about 550 million years ago to a carbonate platform (similar to the one around the present-day Bahamas), which lasted for the next 300 million years of Paleozoic time (refer to the middle of the timescale image). Death Valley’s position was then within ten or twenty degrees of the Paleozoic equator. Thick beds of carbonate-rich sediments were periodically interrupted by periods of emergence. Although details of geography varied during this immense interval of time, a north-northeastern coastline trend generally ran from Arizona up through Utah. The resulting eight formations and one group are 20,000 feet (6 km) thick and underlay much of the Cottonwood, Funeral, Grapevine, and Panamint ranges.

In the early-to-mid- Mesozoic the western edge of the North American continent was pushed against the oceanic plate under the Pacific Ocean, creating a subduction zone. A subduction zone is a type of contact between different crustal plates where heavier crust slides below lighter crust. Erupting volcanoes and uplifting mountains were created as a result, and the coastline was pushed to the west. The Sierran Arc started to form to the northwest from heat and pressure generated from subduction, and compressive forces caused thrust faults to develop.

A long period of uplift and erosion was concurrent with and followed the above events, creating a major unconformity, which is a large gap in the geologic record. Sediments worn off the Death Valley region were carried both east and west by wind and water. No Jurassic- to Eocene-aged sedimentary formations exist in the area, except for some possibly Jurassic-age volcanic rocks (see the top of the timescale image).

Basin and Range-associated stretching of large parts of crust below southwestern United States and northwestern Mexico started around 16 million years ago and the region is still spreading. This stretching began to affect the Death and Panamint valleys area by 3 million years ago. Before this, rocks now in the Panamint Range were on top of rocks that would become the Black Mountains and the Cottonwood Mountains. Lateral and vertical transport of these blocks was accomplished by movement on normal faults. Right-lateral movement along strike-slip faults that run parallel to and at the base of the ranges also helped to develop the area. Torsional forces, probably associated with northwesterly movement of the Pacific plate along the San Andreas Fault (west of the region), is responsible for the lateral movement.

Igneous activity associated with this stretching occurred from 12 million to 4 million years ago. Sedimentation is concentrated in valleys (basins) from material eroded from adjacent ranges. The amount of sediment deposited has roughly kept up with this subsidence, resulting in the retention of more or less the same valley floor elevation over time.

Pleistocene ice ages started 2 million years ago, and melt from alpine glaciers on the nearby Sierra Nevada Mountains fed a series of lakes that filled Death and Panamint valleys and surrounding basins (see the top of the timescale image). The lake that filled Death Valley was the last of a chain of lakes fed by the Amargosa and Mojave Rivers, and possibly also the Owens River. The large lake that covered much of Death Valley’s floor, which geologists call Lake Manly, started to dry up 10,500 years ago. Salt pans and playas were created as ice age glaciers retreated, thus drastically reducing the lakes’ water source. Only faint shorelines are left.

Habitat varies from salt pan at 282 feet (86 m) below sea level to the sub-alpine conditions found on the summit of Telescope Peak, which rises to 11,049 feet (3,368 m). Vegetation zones include creosote bush, desert holly, and mesquite at the lower elevations and sage up through shadscale, blackbrush, Joshua tree, pinyon-juniper, to limber pine and bristlecone pine woodlands. The salt pan is devoid of vegetation, and the rest of the valley floor and lower slopes have sparse cover, although where water is available, an abundance of vegetation is usually present. These zones and the adjacent desert support a variety of wildlife species, including 51 species of native mammals, 307 species of birds, 36 species of reptiles, 3 species of amphibians, and 2 species of native fish.

Small mammals are more numerous than large mammals, such as bighorn sheep, coyotes, bobcats, kit foxes, cougars, and mule deer. Mule deer are present in the pinyon/juniper associations of the Grapevine, Cottonwood, and Panamint ranges. Bighorn sheep are a rare species of mountain-dwelling sheep that exist in isolated bands in the Sierra and in Death Valley. These are highly adaptable animals and can eat almost any plant. They have no known predators, but humans and burros compete for habitat.

The ancestors of the Death Valley pupfish swam to the area from the Colorado River via a long-since dried-up system of rivers and lakes (see Lake Manly). They now live in two separate populations: one in Salt Creek and another in Cottonball Marsh. Death Valley is one of the hottest and driest places in North America, yet it is home to over 1,000 species of plants; 23 of which, including the very rare rock lady (Holmgrenanthe), are not found anywhere else.

Adaptation to the dry environment is key. For example, creosote bush and mesquite have tap-root systems that can extend 50 feet (15 m) down in order to take advantage of a year-round supply of ground water. The diversity of Death Valley’s plant communities results partly from the region’s location in a transition zone between the Mojave Desert, the Great Basin Desert and the Sonoran Desert. This location, combined with the great relief found within the park, supports vegetation typical of three biotic life zones: the lower Sonoran, the Canadian, and the arctic/alpine in portions of the Panamint Range. Based on the Munz and Keck (1968) classifications, seven plant communities can be categorized within these life zones, each characterized by dominant vegetation and representative of three vegetation types: scrub, desert woodland, and coniferous forest. Microhabitats further subdivide some communities into zones, especially on the valley floor.

Unlike more typical locations across the Mojave Desert, many of the water-dependent Death Valley habitats possess a diversity of plant and animal species that are not found anywhere else in the world. The existence of these species is due largely to a unique geologic history and the process of evolution that has progressed in habitats that have been isolated from one another since the Pleistocene epoch.

Sightseeing is available by personal automobile, four-wheel drive, motorcycle, bicycle, mountain bike (on established roadways only), and hiking. State Route 190, the Badwater Road, the Scotty’s Castle Road, and paved roads to Dante’s View and Wildrose provide access to the major scenic viewpoints and historic points of interest. More than 350 miles (560 km) of unpaved and four-wheel-drive roads provide access to wilderness hiking, camping, and historical sites. Unlike many other national parks in the U.S. there are no formal entrance stations, and instead entry fees can be paid at the visitor centers, ranger stations, or various fee machines around the park. There are hiking trails of varying lengths and difficulties, but most backcountry areas are accessible only by cross-country hiking. The peak season for visiting the park is from October to May, avoiding summer extreme temperatures. Costumed living history tours of the historic Scotty’s Castle were suspended in October 2015 due to extensive flood damage to the buildings and grounds. It remains closed to the public.

There are nine designated campgrounds within the park, and overnight backcountry camping permits are available at the visitor center. Xanterra Parks & Resorts owns and operates a private resort, the Oasis at Death Valley, which comprises two separate and distinct hotels: the Inn at Death Valley is a four-star historic hotel, and the Ranch at Death Valley is a three-star ranch-style property reminiscent of the mining and prospecting days. Panamint Springs Resort is in the western part of the park. Death Valley Lodging Company operates the Stovepipe Wells Resort under a concession permit. There are a few motels near entrances to the park, in Shoshone, Death Valley Junction, Beatty, and Pahrump.

Furnace Creek Visitor Center is located on CA-190 and includes exhibits and a film about the park’s geology, climate, wildlife and natural history, as well as human history and pioneer experience. During the winter season—November through April—rangers offer interpretive tours and a variety of walks, talks, and presentations about Death Valley cultural and natural history. The Death Valley Natural History Association maintains a bookstore.

The northeast corner of Saline Valley has several developed hot spring pools accessible by several hours’ drive on unpaved roads or by flying a personal aircraft to the Chicken Strip—an uncharted airstrip a short walk from the springs.

Death Valley National Park is a popular location for stargazing as it has one of the darkest night skies in the United States. Despite its remote location, air quality and night visibility are threatened by civilization. In particular, light pollution is introduced by nearby Las Vegas. The darkest skies are located in the northwest of the park; Ubehebe Crater is a Bortle class 1 or “excellent dark sky” site. The Andromeda Galaxy and the Triangulum Galaxy are visible to the unaided eye under these conditions, and the Milky Way casts shadows; optical phenomena such as zodiacal light or “false dawn” and gegenschein are also visible to the unaided eye under these conditions. Most southern regions of the park are Bortle class 2 or “average dark sky” sites.

This article uses material from the Wikipedia article Death Valley National Park, which is released under the Creative Commons Attribution-Share-Alike License 4.0

20250530

The neurodiversity paradigm is a framework for understanding human brain function that considers the diversity within sensory processing, motor abilities, social comfort, cognition, and focus as neurobiological differences. This diversity falls on a spectrum of neurocognitive differences. The neurodiversity paradigm argues that diversity in neurocognition is part of humanity and that some neurodivergences generally classified as disorders, such as autism, are differences with strengths and weaknesses as well as disabilities that are not necessarily pathological.

The neurodiversity movement started in the late 1980s and early 1990s with the start of Autism Network International. Much of the correspondence that led to the formation of the movement happened over autism conferences, namely the autistic-led Autreat, penpal lists, and Usenet. The framework grew out of the disability rights movement and builds on the social model of disability, arguing that disability partly arises from societal barriers and person-environment mismatch, rather than attributing disability purely to inherent deficits. It instead situates human cognitive variation in the context of biodiversity and the politics of minority groups. Some neurodiversity advocates and researchers including Judy Singer and Patrick Dwyer argue that the neurodiversity paradigm is the middle ground between a strong medical model and a strong social model.

Neurodivergent individuals face unique challenges in education and the workplace. The efficacy of accessibility and support programs in career development and higher education differs from individual to individual. Social media has introduced a platform where neurodiversity awareness and support has emerged, further promoting the neurodiversity movement.

The neurodiversity paradigm has been controversial among disability advocates, especially proponents of the medical model of autism, with opponents arguing it risks downplaying the challenges associated with some disabilities (e.g., in those requiring little support becoming representative of the challenges caused by the disability, thereby making it more difficult to seek desired treatment), and that it calls for the acceptance of things some wish to be treated for. In recent years, to address these concerns, some neurodiversity advocates and researchers have attempted to reconcile what they consider different seemingly contradictory but arguably partially compatible perspectives. Some researchers have advocated for mixed or integrative approaches that involve both neurodiversity approaches and biomedical interventions or advancements, for example teaching functional communication (whether verbal or nonverbal) and treating self-injurious behaviors or co-occurring conditions like anxiety and depression with biomedical approaches.

The word neurodiversity first appeared in publication in 1998, in an article by American journalist Harvey Blume, as a portmanteau of the words neurological diversity, which had been used as early as 1996 in online spaces such as InLv to describe the growing concept of a natural diversity in humanity’s neurological expression. The same year, it was published in Judy Singer’s sociology honors thesis, drawing on discussions on the independent living mailing list that included Blume. Singer has described herself as “likely somewhere on the autistic spectrum”.

Blume was an early advocate who predicted the role the Internet would play in fostering the international neurodiversity movement. In a New York Times piece on June 30, 1997, Blume described the foundation of neurodiversity using the term neurological pluralism. Some authors also credit the earlier work of autistic advocate Jim Sinclair in laying the foundation for the movement. Sinclair’s 1993 speech “Don’t Mourn For Us” emphasized autism as a way of being, claiming “it is not possible to separate the person from the autism.”

The Neurodiversity Movement grew largely from online interaction. The internet’s design lent well to the needs of many autistic people. People socialized over listservs and IRCs. Some of the websites used for organizing in the Neurodiversity Movement’s early days include sites like Autistics.Org and Autistic People Against Neuroleptic Abuse. Core principles were developed from there. Principles such as advocating for the rights and autonomy of all people with brain disabilities with a focus on autism. The main conflicts from the beginning were about who the real experts on autism are, what causes autism, what interventions are appropriate, and who gets to call themselves autistic. During the 2000s, people started blogs such as Mel Baggs’ Ballastexistenz and Kevin Leitch’s Left Brain Right Brain. Eventually, Autistic Self Advocacy Network (ASAN) was started by Ari Ne’eman and Scott Robertson to further align the Neurodiversity Movement with the greater disability rights movement. ASAN led the Ransom Notes Campaign to successfully remove stigmatizing disability ads posted by the NYU Child Study Center. This was a massive turning point for the Neurodiversity Movement.

From there, the Neurodiversity Movement continued to grow with the formation of more organizations in the early 2010s such as Autistic Women & Nonbinary Network and The Thinking Person’s Guide to Autism. More autistic people were appointed to federal advisory boards like Interagency Autism Coordinating Committee and National Council on Disability. There were various campaigns like the ongoing #StopTheShock related to the use of aversive treatment at Judge Rotenberg Center and various protests against Autism Speaks. Various flashblogs popped up during the 2010s to support campaigns. Annual traditions were formed such as Disability Day of Mourning and Autistics Speaking Day.

Damian Milton notes that, in 2014, Nick Walker attempted to define neurodiversity, the neurodiversity movement, and the neurodiversity paradigm. Walker tied neurodiversity to the idea that “all brains are to a degree unique”. She also defined the movement as a rights movement, and the paradigm as a broader discussion of diversity, cultural constructions and social dynamics.

An important question is which neurodivergences traditionally viewed as disorders should be depathologized and exempt from attempts to remove them. Autistic advocate Nick Walker suggested preserving “forms of innate or largely innate neurodivergence, like autism” while conditions like epilepsy or traumatic brain injury could be removed from the person without fundamentally changing the person because these are not pervasively linked to the individual’s personality or perception of the world.

In recent years, the concept of neurodiversity and many related findings that challenged traditional knowledge and practices in the autism field have gained traction among many members of the scientific and professional communities, who have argued that autism researchers have sometimes been too ready to interpret differences as deficits. It has also been suggested that there are both ethical issues and practical risks in attempting to reduce or suppress some autistic traits (e.g. some stimming behaviors that do not cause harm to self or others, focused interests) that can sometimes be adaptive or instilling neurotypical social behaviors (e.g. eye contact, body language) through interventions. Researchers and advocates are concerned about such issues and risks as most recent studies and multiple systematic reviews have indicated that higher levels of masking, passing as neurotypical, or camouflaging are generally associated with poorer mental health outcomes including depression, clinical anxiety, and suicidality among autistic people (including children, adolescents, and adults) and across various regions or cultures. In addition, two reviews published in 2024 indicated some forms of repetitive behaviors can be adaptive for sensory regulation and emotional regulation of some autistic people, and masking or suppressing some autistic repetitive behaviors that can be adaptive may risk worsening mental health and well-being. One multiple-year longitudinal study found that autistic children who showed decrease in repetitive behaviors experienced more severe and worsening in mental health symptoms, whereas autistic children who showed increase in repetitive behaviors experienced less severe mental health challenges. Relatedly, qualitative studies have shown some forms of behavioral interventions increase camouflaging or masking of autistic traits (e.g. stimming) for some autistic people, with negative effects on mental health. In addition, quantitative evidence regarding adverse effects (e.g. in terms of trauma and reinforcement of masking) of some behavioral interventions is limited but emerging.Moreover, researchers have found that psychoeducation based on the medical model is associated with higher stigma. Another study found that endorsements of normalization and curative goals (goals of some medical models) are associated with heightened stigma. Similarly, some researchers and advocates also argue that a medicalizing approach can contribute to stigma and ableism, and that the persistent focus on biological research in autism based on deficit-based medical model is at odds with the priorities of those in the autism community.

The neurodiversity paradigm is controversial in autism advocacy. A prevalent criticism is that autistic people with higher support needs would continue to have challenges even if society was fully accommodating and accepting of them. Some critics of the neurodiversity paradigm, such as family members that are responsible for the care of such an autistic individual, think it might lead to overlooking or downplaying these challenges. In response, it has been stated that neurodiversity does not deny disability and support needs and that not having certain abilities or needing support is not intrinsically a bad thing, because notions of normal functioning are culturally and economically relative and historically contingent and there are cultures in which questions like “Will my child ever be able to live independently?” or “Who will care for my child after I die?” do not arise because support is provided by other members of the community as a matter of course.Autistic self-advocate and researcher Ari Ne’eman has suggested a trait-based approach, where elements of the medical (or pathology) model can be applied in treating certain traits, behaviors, or conditions that are intrinsically harmful (e.g. self-injury behaviors, epilepsy, or other co-occurring health conditions), while neurodiversity approaches can be applied to non-harmful or sometimes adaptive autistic traits (e.g. some stimming behaviors that do not result in self-injury, intense interests) of the same individual. Relatedly, some neurodiversity researchers, as well as autistic people, advocates and researchers, have advocated for application and sometimes integration or combination of both neurodiversity approaches and biomedical research plus practice.

In recent years, researchers, providers of various support services, and neurodivergent people have advocated for more neurodiversity-affirming interventions, with both new intervention strategies being developed and advancements or reforms of existing intervention strategies (e.g. social skills training, ABA interventions, occupational therapy) informed by experiences, strengths, interests, preferences, and feedback of autistic people as well as neurodiversity approaches and findings, with some evidence for beneficial effects. In addition, some researchers and advocates have called for more neurodiversity-affirming psychoeducation and stigma reduction methods.

As the neurodiversity paradigm has gained traction in mainstream discourse, a diluted form has emerged—commonly referred to as “neurodiversity-lite”. This version retains the vocabulary of neurodiversity but strips it of its original political and disability rights roots. Instead of emphasizing systemic ableism, access barriers, or the need for structural change, neurodiversity-lite frames cognitive difference as a benign form of diversity—something novel, even fashionable.

At first glance, neurodiversity-lite appears to offer an important cultural shift. It reframes conditions like autism and ADHD in a more positive light, emphasizing strengths such as creativity, attention to detail, hyperfocus, or out-of-the-box thinking. In doing so, it counters the historically deficit-based narratives that have dominated psychology and medicine. This framing can help reduce stigma, encourage self-acceptance, and support hiring initiatives that recognize neurodivergent talent. For many, this more affirming view has opened doors—both personally and professionally.

However, this surface-level positivity comes at a cost. Critics argue that neurodiversity-lite risks overemphasizing exceptional abilities while erasing the real-world challenges many neurodivergent individuals face—especially those with high support needs, intellectual disabilities, or non-speaking communication. It is most visible in corporate or media narratives that promote the idea of neurodivergence as a “superpower”, particularly when it serves productivity and innovation—often framing autistic individuals as ideal workers in tech and STEM fields. These narratives selectively uplift individuals who can “perform” in neurotypical environments with little to no accommodation, leaving behind those who do not fit this mold. In doing so, they reproduce existing inequities under the guise of inclusion.

Moreover, by focusing only on traits that align with institutional value—like tech aptitude or problem-solving—neurodiversity-lite enables a form of inclusion without accountability. It avoids confronting structural ableism, fails to advocate for accessibility, and silences those whose support needs challenge the productivity-first mindset of modern institutions. In short, it reduces neurodiversity from a justice-oriented framework into a branding strategy.

According to Kassiane Asasumasu, who coined the terms in the year 2000, neurodivergent/neurodivergence refers to those “whose neurocognitive functioning diverges from dominant societal norms in multiple ways”. She emphasized that it should not be used to exclude people but rather to include them and therefore intended for these terms to apply to a broad variety of people, not just people with neurodevelopmental differences, such as autism, attention-deficit hyperactivity disorder, and dyslexia. It is also used as an umbrella term to describe people with atypical mental and behavioral traits, such as mood, personality, and eating disorders. However, people with non-cognitive neurological conditions, such as cerebral palsy, Parkinson’s disease, and multiple sclerosis, are normally excluded.

Under the neurodiversity framework, these differences are often referred to as “neurodivergences”, in an effort to move away from the medical model of disability (sometimes referred to in the neurodiversity community as the “pathology paradigm”). This term provided activists a way to advocate for increased rights and accessibility for non-autistic people who do not have a neurocognitive functioning that is considered typical.

Neurotypical (an abbreviation of neurologically typical, sometimes NT) is a neologism widely used in the neurodiversity movement as a label for anyone who has a neurotype that fits into the norm of thinking patterns. Thus, the term “neurotypical” includes anyone who is not autistic, and does not have ADHD, dyslexia, anxiety, or any other difference that would be considered neurodivergent. The term has been adopted by both the neurodiversity movement and some members of the scientific community.

Neuroscience writer Mo Costandi views terms like “neurotypical” as not being of use in neuroscience, while others, including Uta Frith and Francesca Happé, use the term freely. Ginny Russell mentions that there is no clear bimodal distribution separating autistic and non-autistic people because many non-autistic people have some autistic traits. Another criticism, that “neurotypical” was a dubious construct because there is nobody who could be considered truly neurotypical, has been said by Nick Walker to reflect a misunderstanding of the term because it is meant to describe those who can adapt to society’s norms without much effort, not to imply that all neurotypical people’s brains are the same.

Early definitions described neurotypicals as individuals who are not autistic. Early uses of NT were often satirical, as in the Institute for the Study of the Neurologically Typical, but it has been adopted by the neurodiversity movement too, and is now used in a serious manner.

In contrast to some of the shortcomings of terms like “neurotypical” (such as its underlying assumption that neurodivergent experiences are an anomaly, i.e. not typical), a growing group of advocates in the neurodivergent movement prefer other terms such as “neuroconforming”. The term “allistic” is also used, meaning “not autistic”.

The theory of the double empathy problem argues that autistic people do not inherently lack empathy as often supposed by people who see autism as pathological, but most autistic people may struggle in understanding and empathizing for non-autistic people whereas most non-autistic people also lack understanding and empathy for autistic people. It was originally conceived in 2012 by autistic scholar Damian Milton. The theory argues that characteristics and experiences of autistic and non-autistic people are so different that it is hard for one to understand how the other thinks and empathize with each other; for example, non-autistic people may not understand when an autistic person is overwhelmed.

An increasing number of studies in the 2010s and 2020s found support for double empathy theory and related concepts such as bidirectional social interaction. One study comparing the conversations and socialization of autistic groups, non-autistic groups, and mixed groups found that autistic people were more able to build rapport with other autistic people than with non-autistic people, and at a level similar to the purely non-autistic group. A systematic review published in 2024 found that most autistic people have good interpersonal relations and social-communication experiences with most autistic people, and interactions between autistic people are associated with better quality of life across multiple domains, including mental health and emotional well-being.

The double empathy problem theory implies there is no simple fix that can help each group better empathize with each other, but it is worthwhile to bridge the double empathy gap through more equal contact and enhancing public understanding and empathy about autistic people based on neurodiversity-affirming approaches. The advantage of the theory is reducing pathologization of autistic people by identifying that most people struggle to empathize with people with different neurotypes. It can also help neurotypical individuals to better understand how neurodivergent people think and empathize and to recognize their own limitations in empathizing with autistic people. Jaswal and Akhtar (2019) highlight the difference between being socially uninterested and appearing socially uninterested, and challenge preconceived notions of a lack of social motivation. For example, testimonies from autistic individuals report that avoiding eye contact serves an important function of helping them to concentrate during conversation, and should not be interpreted as expressing social disinterest.

Proponents of neurodiversity strive to reconceptualize autism and related conditions in society by acknowledging that neurodivergence is not something that needs to be cured and that the idea of curing it makes no conceptual sense because differences like autism are so pervasive that removing the autistic parts of the person is tantamount to replacing the autistic person by a different person. An important aim is also changing the language from the current “condition, disease, disorder, or illness”-based nomenclature, “broadening the understanding of healthy or independent living”, acknowledging new types of autonomy, and giving neurodivergent individuals more control over their interventions, including the type, timing, and whether there should be interventions at all.

Activists such as Jennifer White-Johnson have helped bring attention to the neurodiversity movement, by creating symbols of protest and recognition, including a combination of the black power fist and infinity symbol.

A 2009 study separated 27 students with conditions including autism, dyslexia, developmental coordination disorder, ADHD, and having suffered a stroke into two categories of self-view: “A ‘difference’ view—where neurodiversity was seen as a difference incorporating a set of strengths and weaknesses, or a ‘medical/deficit’ view—where neurodiversity was seen as a disadvantageous medical condition”. They found that, although all of the students reported uniformly difficult schooling careers involving exclusion, abuse, and bullying, those who viewed themselves from the “difference” view (41% of the study cohort) “indicated higher academic self-esteem and confidence in their abilities and many (73%) expressed considerable career ambitions with positive and clear goals”. Many of these students reported gaining this view of themselves through contact with neurodiversity advocates in online support groups.

A 2013 online survey which aimed to assess conceptions of autism and neurodiversity suggested that conception of autism as a difference, and not a deficit, is developmentally beneficial and “transcend[s] a false dichotomy between celebrating differences and ameliorating deficit”.

Neurodiversity advocate John Elder Robison argues that the disabilities and strengths conferred by neurological differences may be mutually inseparable. “When 99 neurologically identical people fail to solve a problem, it’s often the 1% fellow who’s different who holds the key. Yet that person may be disabled or disadvantaged most or all of the time. To neurodiversity proponents, people are disabled because they are at the edges of the bell curve, not because they are sick or broken.”

There are several models that are used to understand disability. There is the medical model of disability that views people as needing to be treated or cured. Another model is the social model of disability, which puts emphasis on the way that society treats people with disabilities. Through the social model of disability, the experiences of neurodivergent students in higher education are partially influenced by the reactions and attitudes of other students and the institution itself.

The emotional experiences of neurodivergent students in higher education depend on a combination of factors, including the type of disability, the level of support needs, and the student’s access to resources and accommodations. A common difficulty for neurodivergent students is maintaining social relationships, which can give rise to loneliness, anxiety, and depression. There is also the added stress and difficulty of transitioning into higher education, as well as the responsibilities and task management required in college. Many neurodivergent students may find that they need added support. As for academics, neurodivergent students may experience difficulties in learning, executive function, managing peer relationships in the classroom or in group work, and other difficulties that can affect academic performance and success in higher education. However, neurodivergent students may find that their differences are a strength and an integral part of their new social roles as adults.

The typical curriculum and format of higher education may pose as a challenge for neurodivergent students, and a lack of support and flexibility from staff may further complicate the university experience. Thus, reasonable adjustments are available to students who disclose their disabilities. However, these adjustments or accommodations may put an emphasis on academics, and less on the various challenges of higher education on neurodivergent students. For instance, neurodivergent students in higher education also report a need for non-academic supports, such as social mentorships and resources for strength-based interventions in order to further assist neurodivergent students in the social aspects of college life. Similarly, career preparation that is specifically targeted for neurodivergent students is lacking. There are several programs, such as supported employment, that exist to help assist neurodivergent individuals in finding and obtaining a job. However, many of these programs do not exist in schools. This can make it difficult for neurodivergent students to find a career path that they feel is attainable for them. Another consideration is the implementation of a universal design approach (UDL) when building learning spaces or communal areas that considers the needs of neurodivergent students. A UDL design incorporates a design that accommodates the needs of all students, including the neurodivergent population.

According to an article published in 2023, universities and post-secondary establishments would show more tolerance towards neurodivergent people. A tolerant environment can increase autonomy, leading to kindness and understanding among students. Higher education institutions offer counseling and support services to students. However, neurodivergent students face particular challenges that impair their ability to receive consistent support and care. Additionally, counseling and support services face a lack of funding, personnel, and specialists that can adequately support neurodivergent students. Overall, these services work for some students and not for others.

Nachman and colleagues reviewed several articles published by two-year community colleges and found some discrepancies in the way that they perceived and categorized “disabled” students and “non-disabled” students. They found that all of the articles were attempting to normalize disability. Many of them put a distinct separation between typical and atypical learners as well as their potential academic achievement. Nachman also found that many of the articles showed a lack of autonomy for neurodivergent students. They had little power in regard to academic choices and classroom management.

Neurodivergent individuals are subjected to bias when applying and interviewing for job positions. Specifically, neurodivergent individuals can have their social engagement style compared to neurotypical individuals, which can affect their ability to obtain a job position. Stigmas against neurodivergence (especially against autistic individuals) and cognition challenges in social situations can hinder an individual’s ability to perform well in a traditional job interview. Organizations such as Specialisterne aim to use neurodivergent employees’ particular skills – such as pattern recognition, detection of deviations, attention to detail, analytical thinking, and extended focus – in the workforce, as well as educate companies on supporting neurodivergent employees.

In a systematic review that considered developmental dyslexia as “an expression of neurodiversity”, it was suggested that neurodiversity is not yet an established concept in the workplace, and therefore, support from social relationships and work accommodations is minimal. Furthermore, another systematic review that focused on pharmacological and combined pharmacological/psychosocial interventions for adults with attention deficit hyperactivity disorder found that there were few workplace-based intervention studies, and suggested that additional research needs to be conducted to figure out how to best support neurodivergent employees in the workplace.

A study conducted during the COVID-19 pandemic suggested that neurodivergent individuals would benefit from remote work as it allowed them to engage in their interests, but that social engagement is still necessary for productivity and performance. Another study supported these findings and stressed the need for redesigned work and social conditions to be more inclusive for autistic individuals.

The increase in representation of the neurodiversity movement in the media came about with changes in the technology of the media platforms themselves. The recent addition of text-based options on various social media sites allows disabled users to communicate, enjoy, and share at a more accessible rate. Social media has a two-fold benefit to the neurodivergent community: it can help spread awareness and pioneer the neurodiversity movement, and it can also allow members of the communities themselves to connect.

Media platforms allow the connection of individuals of similar backgrounds to find a community of support with one another. Online networking and connections enable users to determine their comfort level in interactions, giving them control over their relationships with others. For the neurodivergent community, social media has proven to be a valuable tool for forming relationships, especially for those who find social situations challenging. By connecting neurodivergent users, media platforms provide “safe spaces” that are helpful in forming relationships. Some media developers have created platforms like Blossom that are designed specifically to connect neurodivergent users and families.

Social media also allows users to spread awareness about the neurodiversity movement. Increasing awareness about mental conditions has been shown to increase the amount of factual information spread. The spread of information through social media exposure can assist the neurodiversity movement in educating the public about understanding disabilities such as autism and sifting out misinformation. By sharing neurodivergent experiences from a first-hand perspective, social media can educate the public and destigmatize certain conditions. Still, negative portrayals of neurodivergence can have an obstructive impact on members of the community.

Higher awareness and acceptance through social media can lead people to self-identify as neurodivergent. Generally, self-diagnosis is discouraged in psychiatry because it is thought to be wrong more often than a professional assessment and because it is said that it trivializes challenges by turning them into fashion labels. Robert Chapman, in contrast, questions the reliability of professional autism assessments as they often overlook the experiences of individuals who are not white cisgender male children and states that self-identification is not done for fashion purposes but because it helps understanding one’s strengths and challenges. Sue Fletcher-Watson argues that because autism should not be classified as a disorder and no treatment should follow a diagnosis, autistic individuals should have the autonomy to self-identify as autistic, liberating them from the power of medical professionals in defining autism and determining who belongs to the autistic community. A group of researchers created a preliminary self-report questionnaire for autistic people.

Although representation of the neurodivergent community has grown with the help of social media platforms, those users are often criticized and misunderstood. Social media has not entirely removed the social barriers that restrict inclusion of neurodivergent people. Some have reported needing to conform to the mainstream view of their disability to be seen as “authentic” users. Doing so has indirectly made it more difficult for neurodivergent users to grow platforms. Non-disabled users assessing the authenticity of neurodivergent individuals based on stereotypes indicates that the neurodiversity movement has not achieved its goal of inclusion.

Medicine and healthcare

Medical and healthcare professionals have begun to acknowledge neurodivergence among employees. Specifically, more groups are being created that are centered around advocacy and peer support among medical and healthcare professionals who associate themselves with neurodiversity, such as the Autistic Doctors International created by Dr. Mary Doherty. Another approach is the implementation of a 5-minute video summary (5MVS) for medical learners and physicians who have attention deficit hyperactivity disorder (ADHD). It consists of a 5-minute recorded video summary in which an engaging speaker presents the relevant information from a scientific article about ADHD using a brief PowerPoint presentation shared using videoconferencing technology. The researchers state that providing this educational tool for helping medical learners and physicians with ADHD acquire relevant information from scientific articles could help in addressing their inattention, impulsivity or hyperactivity, and improve their development of critical appraisal skills when working in healthcare.

Similarly, healthcare systems may benefit from hiring neurodivergent individuals to gain a unique perspective when caring for patients. Some healthcare staff agree that inviting neurodivergent individuals to join patient advisory groups or hiring them as staff are essential steps to acceptance and integration in the workforce. Neurodivergent people’s unique strengths can be vital to health system innovation and improvement efforts. One example of the push toward this is the Stanford Neurodiversity Project, in which one of their goals is to discover the strengths of neurodivergent individuals and make use of their talents to increase innovation and productivity of their society, such as working in the field of healthcare and medicine.

Neurodiversity has also recently been investigated as a new way of working within neurodevelopmental clinics in the UK. A team of researchers in Portsmouth, England, have created an approach in aiding neurodivergent individuals known as PANDA, or the Portsmouth Alliance Neurodiversity Approach. This approach may help medical and healthcare professionals facilitate understanding, communication and early support for children who may identify as being neurodivergent.

Neurodiversity and the role it plays in therapeutic settings has been a central focal point in recent years. Many therapists and mental health professionals have pushed for more inclusive psychotherapeutic frameworks appropriate for neurodivergent individuals. One example is neurodivergence-informed therapy, which reframes dysfunction as interconnectedness among society rather than strictly individual, advocating for acceptance and pride in the neurodiversity community, and the push for therapists to pursue humility regarding the knowledge and education associated with individuals who identify as neurodivergent. Similarly, neurodiversity affirming therapy supports neurodivergent differences, rather than viewing them as something that should be eliminated, and to offer ways to support the individual with difficult areas, while still appreciating their needs and strengths.

Therapeutic programs and interventions are also being investigated for the neurodivergent community. Self-determination programs to help neurodivergent individuals achieve goals in their life have been found to be successful, with neurodivergent participants finding it to be “appropriate, acceptable, and feasible”. Various approaches (e.g., eye-tracking, longitudinal data, computational modeling) in understanding perceptual decision-making in neurodivergent individuals are also being studied and the implications it may have in the therapeutic environment in working with the neurodivergent population.

Another form of therapeutic intervention in that has been investigated in neurodivergent individuals is the use of Naturalistic Developmental Behavioral Interventions (NDBIs). NDBIs have been shown to have positive effects on language and social-communication while, at the same time, respecting individuals’ needs and autonomy. One of the key goals in this type of intervention is putting the focus of therapy on the neurodivergent individual themselves in the creation of intervention goals, procedures, and outcomes. In doing so, they are likely to be seen as more acceptable, useful, and effective to that individual.

In addition to support from neurodiversity advocates for affirming therapies, concerns have been raised about the role of certain approaches such as applied behavior analysis. Neurodivergent individuals and activists tend to emphasize that these interventions aim to enforce conformity with expectations of society rather than addressing the needs of the person receiving the intervention. While a large body of research on the role of ABA seems to support its efficacy in cognitive and behavioral outcomes, a meta-analysis by Sandbank et al. challenges the evidence. Additionally, there are concerns regarding long-term mental health impacts and with the measures used in determining social validity by those who have raised these concerns. In addition to advocates from within the neurodivergent community, some behavioral analysts have begun to reconsider the role of these therapies with the context of a neurodiversity framework.

This article uses material from the Wikipedia article Neurodiversity, which is released under the Creative Commons Attribution-Share-Alike License 4.0

20250526

Utah is a landlocked state in the Mountain West subregion of the Western United States. It is one of the Four Corners states, sharing a border with Arizona, Colorado, and New Mexico. It also borders Wyoming to the northeast, Idaho to the north, and Nevada to the west. In comparison to all the U.S. states and territories, Utah, with a population of just over three million, is the 13th largest by area, the 30th most populous, and the 11th least densely populated. Urban development is mostly concentrated in two regions: the Wasatch Front in the north-central part of the state, which includes the state capital, Salt Lake City, and is home to roughly two-thirds of the population; and Washington County in the southwest, which has approximately 180,000 residents. Most of the western half of Utah lies in the Great Basin.

Utah has been inhabited for thousands of years by various indigenous groups, such as the ancient Puebloans, the Navajo, and the Ute. The first Europeans to arrive – in the mid-16th century – were the Spanish. Because of the region’s challenging geography and harsh climate, it only became a peripheral part of New Spain (and later of Mexico). Even while it was Mexican territory, many of the Utah region’s earliest European settlers were from the United States; notable among these were Mormons who were fleeing marginalization and persecution in the United States and arrived via the so-called Mormon Trail. In 1848, after the Mexican–American War, the region was annexed by the U.S., becoming part of the Utah Territory, which included what later became Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah’s admission as a state: in 1896, after it agreed to outlaw polygamy, it was admitted as the 45th state.

People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. The LDS Church greatly influences Utah’s culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.

Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah’s water security and impacting the state’s economy.

The name Utah derives from the name of the Ute tribe, meaning ‘people of the mountains’. However, no such word exists in the Utes’ language, and the Utes refer to themselves as Noochee. The meaning of Utes as ‘the mountain people’ has been attributed to the neighboring Pueblo Indians, as well as to the Apache word Yuttahih, which means ‘one that is higher up’ or ‘those that are higher up’. In Spanish, it was pronounced Yuta; subsequently, English-speaking people may have adapted the word as Utah.

Thousands of years before the arrival of Europeans, the Ancestral Puebloans and the Fremont people lived in what is now known as Utah, some of which spoke languages of the Uto-Aztecan group. Ancestral Pueblo peoples built their homes through excavations in mountains, and the Fremont people built houses of straw before disappearing from the region around the 15th century.

Another group of Native Americans, the Navajo, settled in the region around the 18th century. In the mid-18th century, other Uto-Aztecan tribes, including the Goshute, the Paiute, the Shoshone, and the Ute people, also settled in the region. These five groups were present when the first European explorers arrived.

The southern Utah region was explored by the Spanish in 1540, led by Francisco Vázquez de Coronado while looking for the legendary Cíbola. A group led by two Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the coast of California. The expedition traveled as far north as Utah Lake and encountered the native residents. The Spanish made further explorations in the region but were not interested in colonizing the area because of its desert nature. In 1821, the year Mexico achieved its independence from Spain, the region became known as part of its territory of Alta California.

European trappers and fur traders explored some areas of Utah in the early 19th century from Canada and the United States. The city of Provo, Utah, was named for one Étienne Provost, who visited the area in 1825. The city of Ogden, Utah, was named after Peter Skene Ogden, a Canadian explorer who traded furs in the Weber Valley.

In late 1824, Jim Bridger became the first known English-speaking person to sight the Great Salt Lake. Due to the high salinity of its waters, he thought he had found the Pacific Ocean; he subsequently learned this body of water was a giant salt lake. After the discovery of the lake, hundreds of American and Canadian traders and trappers established trading posts in the region. In the 1830s, thousands of migrants traveling from the Eastern United States to the American West began to make stops in the region of the Great Salt Lake, then known as Lake Youta.

Following the death of Joseph Smith in 1844, Brigham Young, as president of the Quorum of the Twelve, became the leader of the LDS Church in Nauvoo, Illinois. To address the growing conflicts between his people and their neighbors, Young agreed with Illinois Governor Thomas Ford in October 1845 that the Mormons would leave by the following year.

Young and the first group of Mormon pioneers reached the Salt Lake Valley on July 24, 1847. Over the next 22 years, more than 70,000 pioneers crossed the plains and settled in Utah. For the first few years, Brigham Young and the thousands of early settlers of Salt Lake City struggled to survive. The arid desert land was deemed desirable by the Mormons as a place where they could practice their religion without harassment.

Settlers buried thirty-six Native Americans in one grave after an outbreak of measles occurred during the winter of 1847.

The first group of settlers brought three African slaves with them, making Utah the only place in the western United States to have African slavery. The three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with the first group of settlers in 1847.

Utah was a Mexican territory when the first pioneers arrived in 1847. Early in the Mexican–American War in late 1846, the United States had taken control of New Mexico and California. The entire Southwest became U.S. territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 11. Learning that California and New Mexico were applying for statehood, the settlers of the Utah area (originally having planned to petition for territorial status) applied for statehood with an ambitious plan for a State of Deseret.

The Mormon settlements provided pioneers for other settlements in the West. Salt Lake City became the hub of a “far-flung commonwealth” of Mormon settlements. With new church converts coming from the East and around the world, Church leaders often assigned groups of church members as missionaries to establish other settlements throughout the West. They developed irrigation to support fairly large pioneer populations along Utah’s Wasatch front (Salt Lake City, Bountiful and Weber Valley, and Provo and Utah Valley). Throughout the remainder of the 19th century, Mormon pioneers established hundreds of other settlements in Utah, Idaho, Nevada, Arizona, Wyoming, California, Canada, and Mexico—including in Las Vegas, Nevada; Franklin, Idaho (the first European settlement in Idaho); San Bernardino, California; Mesa, Arizona; Star Valley, Wyoming; and Carson Valley, Nevada.

Prominent settlements in Utah included St. George, Logan, and Manti (where settlers completed the LDS Church’s first three temples in Utah, each started after but finished many years before the larger and better-known temple built in Salt Lake City was completed in 1893), as well as Parowan, Cedar City, Bluff, Moab, Vernal, Fillmore (which served as the territorial capital between 1850 and 1856), Nephi, Levan, Spanish Fork, Springville, Provo Bench (now Orem), Pleasant Grove, American Fork, Lehi, Sandy, Murray, Jordan, Centerville, Farmington, Huntsville, Kaysville, Grantsville, Tooele, Roy, Brigham City, and many other smaller towns and settlements. Young had an expansionist view of the territory that he and the Mormon pioneers were settling, calling it Deseret—which according to the Book of Mormon was an ancient word for “honeybee”. This is symbolized by the beehive on the Utah flag, and the state’s motto, “Industry”.

The Utah Territory was much smaller than the proposed state of Deseret, but it still contained all of the present states of Nevada and Utah as well as pieces of modern Wyoming and Colorado. It was created with the Compromise of 1850, and Fillmore, named after President Millard Fillmore, was designated the capital. The territory was given the name Utah after the Ute tribe of Native Americans. Salt Lake City replaced Fillmore as the territorial capital in 1856.

By 1850, there were around 100 black people in the territory, the majority of whom were slaves. In Salt Lake County, 26 slaves were counted. In 1852, the territorial legislature passed the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners formally legalizing slavery in the territory. Slavery was abolished in the territory during the Civil War.

In 1850, Salt Lake City sent out a force known as the Nauvoo Legion and engaged the Timpanogos in the Battle at Fort Utah.

Disputes between the Mormon inhabitants and the U.S. government intensified due to the practice of plural marriage, or polygamy, among members of the LDS Church. The Mormons were still pushing for the establishment of a State of Deseret with the new borders of the Utah Territory. Most, if not all, of the members of the U.S. government opposed the polygamous practices of the Mormons.

Members of the LDS Church were viewed as un-American and rebellious when news of their polygamous practices spread. In 1857, particularly heinous accusations of abdication of government and general immorality were leveled by former associate justice William W. Drummond, among others. The detailed reports of life in Utah caused the administration of James Buchanan to send a secret military “expedition” to Utah. When the supposed rebellion should be quelled, Alfred Cumming would take the place of Brigham Young as territorial governor. The resulting conflict is known as the Utah War, nicknamed “Buchanan’s Blunder” by the Mormon leaders.

In September 1857, about 120 American settlers of the Baker–Fancher wagon train, en route to California from Arkansas, were murdered by Utah Territorial Militia and some Paiute Native Americans in the Mountain Meadows massacre.

Before troops led by Albert Sidney Johnston entered the territory, Brigham Young ordered all residents of Salt Lake City to evacuate southward to Utah Valley and sent out the Nauvoo Legion to delay the government’s advance. Although wagons and supplies were burned, eventually the troops arrived in 1858, and Young surrendered official control to Cumming, although most subsequent commentators claim that Young retained true power in the territory. A steady stream of governors appointed by the president quit the position, often citing the traditions of their supposed territorial government. By agreement with Young, Johnston established Camp Floyd, 40 miles (60 km) away from Salt Lake City to the southwest.

Salt Lake City was the last link of the First Transcontinental Telegraph, completed in October 1861. Brigham Young was among the first to send a message, along with Abraham Lincoln and other officials.

Because of the American Civil War, federal troops were pulled out of Utah Territory in 1861. This was a boon to the local economy as the army sold everything in camp for pennies on the dollar before marching back east to join the war. The territory was then left in LDS hands until Patrick E. Connor arrived with a regiment of California volunteers in 1862. Connor established Fort Douglas just 3 miles (4.8 km) east of Salt Lake City and encouraged his people to discover mineral deposits to bring more non-Mormons into the territory. Minerals were discovered in Tooele County and miners began to flock to the territory.

Beginning in 1865, Utah’s Black Hawk War developed into the deadliest conflict in the territory’s history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and LDS authorities.

On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the territory and several influential businesspeople made fortunes there.

During the 1870s and 1880s laws were passed to punish polygamists due, in part, to stories from Utah. Notably, Ann Eliza Young—tenth wife to divorce Brigham Young, women’s advocate, national lecturer, and author of Wife No. 19 or My Life of Bondage—and Fanny Stenhouse, author of Tell It All: My Life in Mormonism, testified to the happiness of the very early Church members before polygamy. They independently published their books in 1875. These books and the lectures of Ann Eliza Young have been credited with the United States Congress’s passage of anti-polygamy laws by newspapers throughout the United States, as recorded in “The Ann Eliza Young Vindicator”, a pamphlet which detailed Ms. Young’s travels and warm reception throughout her lecture tour.

T. B. H. Stenhouse, former Utah Mormon polygamist, a Mormon missionary for thirteen years, and a Salt Lake City newspaper owner, finally left Utah and wrote The Rocky Mountain Saints. His book gives a witnessed account of life in Utah, both the good and the bad. He finally left Utah and Mormonism after financial ruin occurred when Brigham Young sent Stenhouse to relocate to Ogden, Utah, according to Stenhouse, to take over his thriving pro-Mormon Salt Lake Telegraph newspaper. In addition to these testimonies, The Confessions of John D. Lee, written by John D. Lee—alleged “Scapegoat” for the Mountain Meadow Massacre—also came out in 1877. The corroborative testimonies coming out of Utah from Mormons and former Mormons influenced Congress and the people of the United States.

In the 1890 Manifesto, the LDS Church banned polygamy. When Utah applied for statehood again, it was accepted. One of the conditions for granting Utah statehood was that a ban on polygamy be written into the state constitution. This was a condition required of other western states that were admitted into the Union later. Statehood was officially granted on January 4, 1896.

Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah became known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes featured in the popular mid-century western film genre. From such films, most US residents recognize such natural landmarks as Delicate Arch and “the Mittens” of Monument Valley. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.

Since the establishment of Alta Ski Area in 1939 and the subsequent development of several ski resorts in the state’s mountains, Utah’s skiing has become world-renowned. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world (the state license plate once claimed “the Greatest Snow on Earth”). Salt Lake City won the bid for the 2002 Winter Olympic Games, and this served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues built along the Wasatch Front continue to be used for sporting events. Preparation for the Olympics spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the reconstruction of the freeway system around the city.

In 1957, Utah created the Utah State Parks Commission with four parks. Today, Utah State Parks manages 43 parks and several undeveloped areas totaling over 95,000 acres (380 km²) of land and more than 1,000,000 acres (4,000 km²) of water. Utah’s state parks are scattered throughout Utah, from Bear Lake State Park at the Utah/Idaho border to Edge of the Cedars State Park Museum deep in the Four Corners region and everywhere in between. Utah State Parks is also home to the state’s off highway vehicle office, state boating office, and the trails program.

During the late 20th century, the state grew quickly. In the 1970s growth was phenomenal in the suburbs of the Wasatch Front. Sandy was one of the fastest-growing cities in the country at that time. Today, many areas of Utah continue to see boom-time growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Management of transportation and urbanization are major issues in politics, as development consumes agricultural land and wilderness areas and transportation is a major reason for poor air quality in Utah.

On March 18, 2020, Utah suffered a 5.7 magnitude earthquake originating 3.7 mi (6.0 km) northeast of Magna, near Salt Lake City.

Utah is known for its natural diversity and is home to features ranging from arid deserts with dunes to thriving pine forests in mountain valleys. It is a rugged and geographically diverse state at the convergence of three distinct geological regions: the Rocky Mountains, the Great Basin, and the Colorado Plateau.

Utah covers an area of 84,899 sq mi (219,890 km²). It is one of the Four Corners states and is bordered by Idaho in the north, Wyoming in the north and east, Colorado in the east, at a single point by New Mexico to the southeast, by Arizona in the south, and by Nevada in the west. Only three U.S. states (Utah, Colorado, and Wyoming) have exclusively latitude and longitude lines as boundaries.

One of Utah’s defining characteristics is the variety of its terrain. Running down the middle of the state’s northern third is the Wasatch Range, which rises to heights of almost 12,000 ft (3,700 m) above sea level. Utah is home to world-renowned ski resorts made popular by light, fluffy snow and winter storms that regularly dump up to three feet of it overnight. In the state’s northeastern section, running east to west, are the Uinta Mountains, which rise to heights of over 13,000 feet (4,000 m). The highest point in the state, Kings Peak, at 13,528 feet (4,123 m), lies within the Uinta Mountains.

At the western base of the Wasatch Range is the Wasatch Front, a series of valleys and basins that are home to the most populous parts of the state. It stretches approximately from Brigham City at the north end to Nephi at the south end. Approximately 75 percent of the state’s population lives in this corridor, and population growth is rapid.

Western Utah is a mostly arid desert with a basin and range topography. Small mountain ranges and rugged terrain punctuate the landscape. The Bonneville Salt Flats are an exception, being comparatively flat as a result of once forming the bed of ancient Lake Bonneville. Great Salt Lake, Utah Lake, Sevier Lake, and Rush Lake are all remnants of this ancient freshwater lake, which once covered most of the eastern Great Basin. West of the Great Salt Lake, stretching to the Nevada border, lies the arid Great Salt Lake Desert. One exception to this aridity is Snake Valley, which is (relatively) lush due to large springs and wetlands fed from groundwater derived from snow melt in the Snake Range, Deep Creek Range, and other tall mountains to the west of Snake Valley. Great Basin National Park is just over the Nevada state line in the southern Snake Range. One of western Utah’s most impressive, but least visited attractions is Notch Peak, the tallest limestone cliff in North America, located west of Delta.

Much of the scenic southern and southeastern landscape (specifically the Colorado Plateau region) is sandstone, specifically Kayenta sandstone and Navajo sandstone. The Colorado River and its tributaries wind their way through the sandstone, creating some of the world’s most striking and wild terrain (the area around the confluence of the Colorado and Green Rivers was the last to be mapped in the lower 48 United States). Wind and rain have also sculpted the soft sandstone over millions of years. Canyons, gullies, arches, pinnacles, buttes, bluffs, and mesas are common sights throughout south-central and southeast Utah.

This terrain is the central feature of protected state and federal parks such as Arches, Bryce Canyon, Canyonlands, Capitol Reef, and Zion national parks, Cedar Breaks, Grand Staircase–Escalante, Hovenweep, and Natural Bridges national monuments, Glen Canyon National Recreation Area (site of the popular tourist destination, Lake Powell), Dead Horse Point and Goblin Valley state parks, and Monument Valley. The Navajo Nation also extends into southeastern Utah, and the tribe is part of the coalition that manages Bears Ears National Monument. Southeastern Utah is also punctuated by the remote, but lofty La Sal, Abajo, and Henry mountain ranges.

Eastern (northern quarter) Utah is a high-elevation area covered mostly by plateaus and basins, particularly the Tavaputs Plateau and San Rafael Swell, which remain mostly inaccessible, and the Uinta Basin, where the majority of eastern Utah’s population lives. Economies are dominated by mining, oil shale, oil, and natural gas-drilling, ranching, and recreation. Much of eastern Utah is part of the Uintah and Ouray Indian Reservation. The most popular destination within northeastern Utah is Dinosaur National Monument near Vernal.

Southwestern Utah is the lowest and hottest spot in Utah. It is known as Utah’s Dixie because early settlers were able to grow some cotton there. Beaverdam Wash in far southwestern Utah is the lowest point in the state, at 2,000 feet (610 m). The northernmost portion of the Mojave Desert is also located in this area. Dixie is quickly becoming a popular recreational and retirement destination, and the population is growing rapidly. Although the Wasatch Mountains end at Mount Nebo near Nephi, a complex series of mountain ranges extends south from the southern end of the range down the spine of Utah. Just north of Dixie and east of Cedar City is the state’s highest ski resort, Brian Head.

Like most of the western and southwestern states, the federal government owns much of the land in Utah. Over 70 percent of the land is either BLM land, Utah State Trustland, or U.S. National Forest, U.S. National Park, U.S. National Monument, National Recreation Area or U.S. Wilderness Area. Utah is the only state where every county contains some national forest.

– Idaho (north)
– Wyoming (east and north)
– Colorado (east)
– Nevada (west)
– Arizona (south)

Utah features a dry, semi-arid to desert climate, although its many mountains feature a large variety of climates, with the highest points in the Uinta Mountains being above the timberline. The dry weather is a result of the state’s location in the rain shadow of the Sierra Nevada in California. The eastern half of the state lies in the rain shadow of the Wasatch Mountains. The primary source of precipitation for the state is the Pacific Ocean, with the state usually lying in the path of large Pacific storms from October to May. In summer, the state, especially southern and eastern Utah, lies in the path of monsoon moisture from the Gulf of California.

Most of the lowland areas receive less than 12 inches (305 mm) of precipitation annually, although the I-15 corridor, including the densely populated Wasatch Front, receives approximately 15 inches (381 mm). The Great Salt Lake Desert is the driest area of the state, with less than 5 inches (127 mm). Snowfall is common in all but the far southern valleys. Although St. George receives only about 3 inches (76 mm) per year, Salt Lake City sees about 60 inches (1,524 mm), enhanced by the lake-effect snow from the Great Salt Lake, which increases snowfall totals to the south, southeast, and east of the lake.

Some areas of the Wasatch Range in the path of the lake effect receive up to 500 inches (1,270 cm) per year. This micro climate of enhanced snowfall from the Great Salt Lake spans the entire proximity of the lake. The cottonwood canyons adjacent to Salt Lake City are located in the right position to receive more precipitation from the lake. The consistently deep powder snow led Utah’s ski industry to adopt the slogan “the Greatest Snow on Earth” in the 1980s. In the winter, temperature inversions are a common phenomenon across Utah’s low basins and valleys, leading to thick haze and fog that can last for weeks at a time, especially in the Uintah Basin. Although at other times of year, its air quality is good, winter inversions give Salt Lake City some of the worst wintertime pollution in the country.

Previous studies have indicated a widespread decline in snowpack over Utah accompanied by a decline in the snow–snow-precipitation ratio while anecdotal evidence claims have been put forward that measured changes in Utah’s snowpack are spurious and do not reflect actual change. A 2012 study found that the proportion of winter (January–March) precipitation falling as snow has decreased by nine percent during the last half century, a combined result of a significant increase in rainfall and a minor decrease in snowfall. Meanwhile, observed snow depth across Utah has decreased and is accompanied by consistent decreases in snow cover and surface albedo. Weather systems with the potential to produce precipitation in Utah have decreased in number with those producing snowfall decreasing at a considerably greater rate.

Utah’s temperatures are extreme, with cold temperatures in winter due to its elevation, and very hot summers statewide (except mountain areas and high mountain valleys). Utah is usually protected from major blasts of cold air by mountains lying north and east of the state, although major Arctic blasts can occasionally reach the state. Average January high temperatures range from around 30 °F (−1 °C) in some northern valleys to almost 55 °F (13 °C) in St. George.

Temperatures dropping below 0 °F (−18 °C) should be expected on occasion in most areas of the state most years, although some areas see it often (for example, the town of Randolph averages about fifty days per year with temperatures that low). In July, average highs range from about 85 to 100 °F (29 to 38 °C). However, the low humidity and high elevation typically lead to large temperature variations, leading to cool nights on most summer days. The record high temperature in Utah was 118 °F (48 °C), recorded south of St. George on July 4, 2007, and the record low was −69 °F (−56 °C), recorded at Peter Sinks in the Bear River Mountains of northern Utah on February 1, 1985. However, the record low for an inhabited location is −49 °F (−45 °C) at Woodruff on December 12, 1932.

Utah, like most of the western United States, has few days of thunderstorms. On average, there are fewer than 40 days of thunderstorm activity during the year, although these storms can be briefly intense when they do occur. They are most likely to occur during monsoon season from about mid-July through mid-September, especially in southern and eastern Utah. Dry lightning strikes and the generally dry weather often spark wildfires in summer, while intense thunderstorms can lead to flash flooding, especially in the rugged terrain of southern Utah. Although spring is the wettest season in northern Utah, late summer is the wettest period for much of the south and east of the state. Tornadoes are uncommon in Utah, with an average of two striking the state yearly, rarely higher than EF1 intensity.

One exception of note, however, was the unprecedented Salt Lake City Tornado that moved directly across downtown Salt Lake City on August 11, 1999. The F2 tornado killed one person, injured 60 others, and caused approximately $170 million in damage; it was the second strongest tornado in the state behind an F3 on August 11, 1993, in the Uinta Mountains. The only other reported tornado fatality in Utah’s history was a 7-year-old girl who was killed while camping in Summit County on July 6, 1884.

Utah is home to more than 600 vertebrate animal species as well as numerous invertebrates and insects.

Mammals are found in every area of Utah. Non-predatory larger mammals include the plains bison, elk, moose, mountain goat, mule deer, pronghorn, and multiple types of bighorn sheep. Non-predatory small mammals include muskrat, and nutria. Large and small predatory mammals include the black bear, cougar, Canada lynx, bobcat, fox (gray, red, and kit), coyote, badger, black-footed ferret, mink, stoat, long-tailed weasel, raccoon, and otter.

The brown bear was formerly found within Utah, but has since been extirpated. There are no confirmed mating pairs of gray wolves in Utah, although there have been sightings in northeastern Utah along the Wyoming border.

As of January 2020, there were 466 species included in the official list managed by the Utah Bird Records Committee (UBRC). Of these, 119 are classed as accidental, 29 are classed as occasional, 57 are classed as rare, and 10 have been introduced to Utah or North America. Eleven of the accidental species are also classed as provisional.

Due to the “Miracle of the Gulls” incident in 1848, the most well-known bird in Utah is the California gull, which is also the Utah state bird. A monument in Salt Lake City commemorates the Miracle of the Gulls. Other gulls common to Utah include Bonaparte’s gull, the ring-billed gull, and Franklin’s gull.

Other birds commonly found include the American robin, the common starling, finches (black rosy, Cassin’s, and goldfinch), the black-billed magpie, mourning doves, sparrows (house, tree, black-chinned, black-throated, Brewer’s, and chipping), Clark’s grebe, the ferruginous hawk, geese (snow, cackling, and Canada), eagles (golden and bald), California quail, mountain bluebird, and hummingbirds (calliope, black-chinned, and broad-tailed).

Utah is host to a wide variety of arachnids, insects, mollusks, and other invertebrates. Arachnids include the Arizona bark scorpion, Western black widow spiders, crab spiders, hobo spiders (Tegenaria agrestis), cellar spiders, American grass spiders, woodlouse spiders. Several spiders found in Utah are often mistaken for the brown recluse spider, including the desert recluse spider (found only in Washington County), the cellar spider, and crevice weaving spiders. The brown recluse spider has not been officially confirmed in Utah as of summer 2020.

One of the rarest insects in Utah is the Coral Pink Sand Dunes tiger beetle, found only in Coral Pink Sand Dunes State Park, near Kanab. It was proposed in 2012 to be listed as a threatened species, but the proposal was not accepted. Other insects include grasshoppers, green stink bugs, the Army cutworm, the monarch butterfly, and Mormon fritillary butterfly. The white-lined sphinx moth is common to most of the United States, but there have been reported outbreaks of large groups of their larvae damaging tomato, grape and garden crops in Utah. Four or five species of firefly are also found across the state.

In February 2009, Africanized honeybees were found in southern Utah. The bees had spread into eight counties in Utah, as far north as Grand and Emery counties by May 2017.

Several thousand plants are native to Utah, including a variety of trees, shrubs, cacti, herbaceous plants, and grasses. As of 2018, there are 3,930 species of plants in Utah, with 3,128 of those being indigenous and 792 being introduced through various means.

Common trees include pines/piñons (white fir, Colorado, single-leaf, Great Basin bristlecone, ponderosa, Engelmann spruce, Rocky Mountain white), and Acer grandidentatum, quaking aspen, bigtooth maple, Utah juniper, speckled alder, red birch, Gambel oak, desert willow, blue spruce, and Joshua trees. Utah has a number of named trees, including the Jardine Juniper, Pando, and the Thousand Mile Tree. Shrubs include a number of different ephedras (pitamoreal, Navajo, Arizona, Nevada, Torrey’s jointfir, and green Mormon tea), sagebrushes (little, Bigelow, silver, Michaux’s wormwood, black, pygmy, bud, and Great Basin), blue elderberry, Utah serviceberry, chokecherry, and skunkbush sumac. Western poison oak, poison sumac, and western poison ivy are all found in Utah.

There are many varieties of cacti in Utah’s varied deserts, especially in the southern and western parts of the state. Some of these include desert prickly pear, California barrel cactus, fishhook cactus, cholla, beavertail prickly pear, and Uinta Basin hookless cactus. Despite the desert climate, many different grasses are found in Utah, including Mormon needlegrass, bluebunch wheatgrass, western alkali grass, squirreltail, desert saltgrass, and cheatgrass.

Several invasive species of plants are considered noxious weeds by the state, including Bermuda grass, field bindweed, henbane, jointed goatgrass, Canada thistle, Balkan and common toadflax, giant cane, couch grass, St. John’s wort, hemlock, sword grass, Russian olive, myrtle spurge, Japanese knotweed, salt cedar, and goat’s head.

At the 2020 U.S. census, Utah had a population of 3,271,616. The U.S. Census Bureau estimated that the population of Utah was 3,205,958 on July 1, 2019, a 16.00% increase since the 2010 U.S. census. The center of population of Utah is located in Utah County in the city of Lehi. Much of the population lives in cities and towns along the Wasatch Front, a metropolitan region that runs north–south with the Wasatch Mountains rising on the eastern side. Growth outside the Wasatch Front is also increasing. The St. George metropolitan area is currently the second fastest-growing in the country after the Las Vegas metropolitan area, while the Heber micropolitan area is also the second fastest-growing in the country (behind Palm Coast, Florida).

Utah contains five metropolitan areas (Logan, Ogden-Clearfield, Salt Lake City, Provo-Orem, and St. George), and six micropolitan areas (Brigham City, Heber, Vernal, Price, Richfield, and Cedar City).

According to HUD’s 2022 Annual Homeless Assessment Report, there were an estimated 3,557 homeless people in Utah.

The majority of Utah’s immigrants come from Mexico.

Utah ranks among the highest in total fertility rate, 47th in teenage pregnancy, lowest in percentage of births out of wedlock, lowest in number of abortions per capita, and lowest in percentage of teen pregnancies terminated in abortion. However, statistics relating to pregnancies and abortions may also be artificially low from teenagers going out of state for abortions because of parental notification requirements. Utah has the lowest child poverty rate in the country, despite its young demographics. According to the Gallup-Healthways Global Well-Being Index as of 2012, Utahns ranked fourth in overall well-being in the United States. A 2002 national prescription drug study determined that antidepressant drugs were “prescribed in Utah more often than in any other state, at a rate nearly twice the national average”. The data shows that depression rates in Utah are no higher than the national average. In 2022, Utah had the lowest percent of births to unmarried women of any US state, at 20.3 percent.

This article uses material from the Wikipedia article Utah, which is released under the Creative Commons Attribution-Share-Alike License 4.0

20250522

Orion is a prominent set of stars visible during winter in the northern celestial hemisphere. It is one of the 88 modern constellations; it was among the 48 constellations listed by the 2nd-century astronomer Ptolemy. It is named after a hunter in Greek mythology.

Orion is most prominent during winter evenings in the Northern Hemisphere, as are five other constellations that have stars in the Winter Hexagon asterism. Orion’s two brightest stars, Rigel (β) and Betelgeuse (α), are both among the brightest stars in the night sky; both are supergiants and slightly variable. There are a further six stars brighter than magnitude 3.0, including three making the short straight line of the Orion’s Belt asterism. Orion also hosts the radiant of the annual Orionids, the strongest meteor shower associated with Halley’s Comet, and the Orion Nebula, one of the brightest nebulae in the sky.

Orion is bordered by Taurus to the northwest, Eridanus to the southwest, Lepus to the south, Monoceros to the east, and Gemini to the northeast. Covering 594 square degrees, Orion ranks twenty-sixth of the 88 constellations in size. The constellation boundaries, as set by Belgian astronomer Eugène Delporte in 1930, are defined by a polygon of 26 sides. In the equatorial coordinate system, the right ascension coordinates of these borders lie between 04^h 43.3^m and 06^h 25.5^m , while the declination coordinates are between 22.87° and −10.97°. The constellation’s three-letter abbreviation, as adopted by the International Astronomical Union in 1922, is “Ori”.

Orion is most visible in the evening sky from January to April, winter in the Northern Hemisphere, and summer in the Southern Hemisphere. In the tropics (less than about 8° from the equator), the constellation transits at the zenith.

In the period May–July (summer in the Northern Hemisphere, winter in the Southern Hemisphere), Orion is in the daytime sky and thus invisible at most latitudes. However, for much of Antarctica in the Southern Hemisphere’s winter months, the Sun is below the horizon even at midday. Stars (and thus Orion, but only the brightest stars) are then visible at twilight for a few hours around local noon, just in the brightest section of the sky low in the North where the Sun is just below the horizon. At the same time of day at the South Pole itself (Amundsen–Scott South Pole Station), Rigel is only 8° above the horizon, and the Belt sweeps just along it. In the Southern Hemisphere’s summer months, when Orion is normally visible in the night sky, the constellation is actually not visible in Antarctica because the sun does not set at that time of year south of the Antarctic Circle.

In countries close to the equator (e.g., Kenya, Indonesia, Colombia, Ecuador), Orion appears overhead in December around midnight and in the February evening sky.

Orion is very useful as an aid to locating other stars. By extending the line of the Belt southeastward, Sirius (α CMa) can be found; northwestward, Aldebaran (α Tau). A line eastward across the two shoulders indicates the direction of Procyon (α CMi). A line from Rigel through Betelgeuse points to Castor and Pollux (α Gem and β Gem). Additionally, Rigel is part of the Winter Circle asterism. Sirius and Procyon, which may be located from Orion by following imaginary lines (see map), also are points in both the Winter Triangle and the Circle.

Orion’s seven brightest stars form a distinctive hourglass-shaped asterism, or pattern, in the night sky. Four stars—Rigel, Betelgeuse, Bellatrix, and Saiph—form a large roughly rectangular shape, at the center of which lie the three stars of Orion’s Belt—Alnitak, Alnilam, and Mintaka. His head is marked by an additional 8th star called Meissa, which is fairly bright to the observer. Descending from the “belt” is a smaller line of three stars, Orion’s Sword (the middle of which is in fact not a star but the Orion Nebula), also known as the hunter’s sword.

Many of the stars are luminous hot blue supergiants, with the stars of the belt and sword forming the Orion OB1 association. Standing out by its red hue, Betelgeuse may nevertheless be a runaway member of the same group.

– Betelgeuse, also designated Alpha Orionis, is a massive M-type red supergiant star nearing the end of its life. It is the second brightest star in Orion, and is a semiregular variable star. It serves as the “right shoulder” of the hunter (assuming that he is facing the observer). It is generally the eleventh brightest star in the night sky, but this has varied between being the tenth brightest to the 23rd brightest by the end of 2019. The end of its life is expected to result in a supernova explosion that will be highly visible from Earth, possibly outshining the Moon and being visible during the day. This is most likely to occur within the next 100,000 years.

– Rigel, also known as Beta Orionis, is a B-type blue supergiant that is the seventh brightest star in the night sky. Similar to Betelgeuse, Rigel is fusing heavy elements in its core and will pass its supergiant stage soon (on an astronomical timescale), either collapsing in the case of a supernova or shedding its outer layers and turning into a white dwarf. It serves as the left foot of the hunter.

– Bellatrix is designated Gamma Orionis by Johann Bayer. It is the twenty-seventh brightest star in the night sky. Bellatrix is considered a B-type blue giant, though it is too small to explode in a supernova. Bellatrix’s luminosity is derived from its high temperature rather than a large radius. Bellatrix marks Orion’s left shoulder and it means the “female warrior”, and is sometimes known colloquially as the “Amazon Star”. It is the closest major star in Orion at only 244.6 light years from the Solar System.

– Mintaka is designated Delta Orionis, despite being the faintest of the three stars in Orion’s Belt. Its name means “the belt”. It is a multiple star system, composed of a large B-type blue giant and a more massive O-type main-sequence star. The Mintaka system constitutes an eclipsing binary variable star, where the eclipse of one star over the other creates a dip in brightness. Mintaka is the westernmost of the three stars of Orion’s Belt, as well as the northernmost.

– Alnilam is designated Epsilon Orionis and is named for the Arabic phrase meaning “string of pearls”. It is the middle and brightest of the three stars of Orion’s Belt. Alnilam is a B-type blue supergiant; despite being nearly twice as far from the Sun as the other two belt stars, its luminosity makes it nearly equal in magnitude. Alnilam is losing mass quickly, a consequence of its size. It is the farthest major star in Orion at 1,344 light years.

– Alnitak, meaning “the girdle”, is designated Zeta Orionis, and is the easternmost star in Orion’s Belt. It is a triple star system, with the primary star being a hot blue supergiant and the brightest class O star in the night sky.

– Saiph is designated Kappa Orionis by Bayer, and serves as Orion’s right foot. It is of a similar distance and size to Rigel, but appears much fainter. It means the “sword of the giant”

– Meissa is designated Lambda Orionis, forms Orion’s head, and is a multiple star with a combined apparent magnitude of 3.33. Its name means the “shining one”.

Belt

Orion’s Belt or The Belt of Orion is an asterism within the constellation. It consists of the three bright stars Zeta (Alnitak), Epsilon (Alnilam), and Delta (Mintaka). Alnitak is around 800 light years away from Earth and is 100,000 times more luminous than the Sun and shines with magnitude 1.8; much of its radiation is in the ultraviolet range, which the human eye cannot see. Alnilam is approximately 2,000 light years away from Earth, shines with magnitude 1.70, and with ultraviolet light is 375,000 times more luminous than the Sun. Mintaka is 915 light years away and shines with magnitude 2.21. It is 90,000 times more luminous than the Sun and is a double star: the two orbit each other every 5.73 days. In the Northern Hemisphere, Orion’s Belt is best visible in the night sky during the month of January around 9:00 pm, when it is approximately around the local meridian.

Just southwest of Alnitak lies Sigma Orionis, a multiple star system composed of five stars that have a combined apparent magnitude of 3.7 and lying 1150 light years distant. Southwest of Mintaka lies the quadruple star Eta Orionis.

Orion’s Sword contains the Orion Nebula, the Messier 43 nebula, the Running Man Nebula, and the stars Theta Orionis, Iota Orionis, and 42 Orionis.

Three stars comprise a small triangle that marks the head. The apex is marked by Meissa (Lambda Orionis), a hot blue giant of spectral type O8 III and apparent magnitude 3.54, which lies some 1100 light years distant. Phi-1 and Phi-2 Orionis make up the base. Also nearby is the very young star FU Orionis.

Stretching north from Betelgeuse are the stars that make up Orion’s club. Mu Orionis marks the elbow, Nu and Xi mark the handle of the club, and Chi¹ and Chi² mark the end of the club. Just east of Chi¹ is the Mira-type variable red giant U Orionis.

West from Bellatrix lie six stars all designated Pi Orionis (π¹ Ori, π² Ori, π³ Ori, π⁴ Ori, π⁵ Ori and π⁶ Ori) which make up Orion’s shield.

Around 20 October each year the Orionid meteor shower (Orionids) reaches its peak. Coming from the border with the constellation Gemini as many as 20 meteors per hour can be seen. The shower’s parent body is Halley’s Comet.

Hanging from Orion’s belt is his sword, consisting of the multiple stars θ1 and θ2 Orionis, called the Trapezium and the Orion Nebula (M42). This is a spectacular object that can be clearly identified with the naked eye as something other than a star. Using binoculars, its clouds of nascent stars, luminous gas, and dust can be observed. The Trapezium cluster has many newborn stars, including several brown dwarfs, all of which are at an approximate distance of 1,500 light-years. Named for the four bright stars that form a trapezoid, it is largely illuminated by the brightest stars, which are only a few hundred thousand years old. Observations by the Chandra X-ray Observatory show both the extreme temperatures of the main stars—up to 60,000 kelvins—and the star forming regions still extant in the surrounding nebula.

M78 (NGC 2068) is a nebula in Orion. With an overall magnitude of 8.0, it is significantly dimmer than the Great Orion Nebula that lies to its south; however, it is at approximately the same distance, at 1600 light-years from Earth. It can easily be mistaken for a comet in the eyepiece of a telescope. M78 is associated with the variable star V351 Orionis, whose magnitude changes are visible in very short periods of time. Another fairly bright nebula in Orion is NGC 1999, also close to the Great Orion Nebula. It has an integrated magnitude of 10.5 and is 1500 light-years from Earth. The variable star V380 Orionis is embedded in NGC 1999.

Another famous nebula is IC 434, the Horsehead Nebula, near ζ Orionis. It contains a dark dust cloud whose shape gives the nebula its name.

NGC 2174 is an emission nebula located 6400 light-years from Earth.

Besides these nebulae, surveying Orion with a small telescope will reveal a wealth of interesting deep-sky objects, including M43, M78, as well as multiple stars including Iota Orionis and Sigma Orionis. A larger telescope may reveal objects such as the Flame Nebula (NGC 2024), as well as fainter and tighter multiple stars and nebulae. Barnard’s Loop can be seen on very dark nights or using long-exposure photography.

All of these nebulae are part of the larger Orion molecular cloud complex, which is located approximately 1,500 light-years away and is hundreds of light-years across. It is one of the most intense regions of stellar formation visible within the Milky Way Galaxy.

The distinctive pattern of Orion is recognized in numerous cultures around the world, and many myths are associated with it. Orion is used as a symbol in the modern world.

The Babylonian star catalogues of the Late Bronze Age name Orion ^MULSIPA.ZI.AN.NA, “The Heavenly Shepherd” or “True Shepherd of Anu” – Anu being the chief god of the heavenly realms. The Babylonian constellation is sacred to Papshukal and Ninshubur, both minor gods fulfilling the role of ‘messenger to the gods’. Papshukal is closely associated with the figure of a walking bird on Babylonian boundary stones, and on the star map the figure of the Rooster is located below and behind the figure of the True Shepherd—both constellations represent the herald of the gods, in his bird and human forms respectively.

In ancient Egypt, the stars of Orion were regarded as a god, called Sah. Because Orion rises before Sirius, the star whose heliacal rising was the basis for the Solar Egyptian calendar, Sah was closely linked with Sopdet, the goddess who personified Sirius. The god Sopdu is said to be the son of Sah and Sopdet. Sah is syncretized with Osiris, while Sopdet is syncretized with Osiris’ mythological wife, Isis. In the Pyramid Texts, from the 24th and 23rd centuries BC, Sah is one of many gods whose form the dead pharaoh is said to take in the afterlife.

The Armenians identified their legendary patriarch and founder Hayk with Orion. Hayk is also the name of the Orion constellation in the Armenian translation of the Bible.

The Bible mentions Orion three times, naming it “Kesil” (כסיל, literally – fool). Though, this name perhaps is etymologically connected with “Kislev”, the name for the ninth month of the Hebrew calendar (i.e. November–December), which, in turn, may derive from the Hebrew root K-S-L as in the words “kesel, kisla” (כֵּסֶל, כִּסְלָה, hope, positiveness), i.e. hope for winter rains.: Job 9:9 (“He is the maker of the Bear and Orion”), Job 38:31 (“Can you loosen Orion’s belt?”), and Amos 5:8 (“He who made the Pleiades and Orion”).

In ancient Aram, the constellation was known as N^ephîlā′, the Nephilim are said to be Orion’s descendants.

In Greek mythology, Orion was a gigantic, supernaturally strong hunter, born to Euryale, a Gorgon, and Poseidon (Neptune), god of the sea. One myth recounts Gaia’s rage at Orion, who dared to say that he would kill every animal on Earth. The angry goddess tried to dispatch Orion with a scorpion. This is given as the reason that the constellations of Scorpius and Orion are never in the sky at the same time. However, Ophiuchus, the Serpent Bearer, revived Orion with an antidote. This is said to be the reason that the constellation of Ophiuchus stands midway between the Scorpion and the Hunter in the sky.

The constellation is mentioned in Horace’s Odes (Ode 3.27.18), Homer’s Odyssey (Book 5, line 283) and Iliad, and Virgil’s Aeneid (Book 1, line 535).

In medieval Muslim astronomy, Orion was known as al-jabbar, “the giant”. Orion’s sixth brightest star, Saiph, is named from the Arabic, saif al-jabbar, meaning “sword of the giant”.

In China, Orion was one of the 28 lunar mansions Sieu (Xiù) (宿). It is known as Shen (參), literally meaning “three”, for the stars of Orion’s Belt. (See Chinese constellations)

The Chinese character 參 (pinyin shēn) originally meant the constellation Orion (Chinese: 參宿; pinyin: shēnxiù); its Shang dynasty version, over three millennia old, contains at the top a representation of the three stars of Orion’s belt atop a man’s head (the bottom portion representing the sound of the word was added later).

The Rigveda refers to the Orion Constellation as Mriga (The Deer).

Nataraja, ‘the cosmic dancer’, is often interpreted as the representation of Orion. Rudra, the Rigvedic form of Shiva, is the presiding deity of Ardra nakshatra (Betelgeuse) of Hindu astrology.

The Jain Symbol carved in Udayagiri and Khandagiri Caves, India in 1st century BCE has striking resemblance with Orion.

Bugis sailors identified the three stars in Orion’s Belt as tanra tellué, meaning “sign of three”.

In old Hungarian tradition, Orion is known as “Archer” (Íjász), or “Reaper” (Kaszás). In recently rediscovered myths, he is called Nimrod (Hungarian: Nimród), the greatest hunter, father of the twins Hunor and Magor. The π and o stars (on upper right) form together the reflex bow or the lifted scythe. In other Hungarian traditions, Orion’s belt is known as “Judge’s stick” (Bírópálca).

In Scandinavian tradition, Orion’s belt was known as “Frigg’s Distaff” (friggerock) or “Freyja’s distaff”.

The Finns call Orion’s belt and the stars below it “Väinämöinen’s scythe” (Väinämöisen viikate). Another name for the asterism of Alnilam, Alnitak and Mintaka is “Väinämöinen’s Belt” (Väinämöisen vyö) and the stars “hanging” from the belt as “Kaleva’s sword” (Kalevanmiekka).

In Siberia, the Chukchi people see Orion as a hunter; an arrow he has shot is represented by Aldebaran (Alpha Tauri), with the same figure as other Western depictions.

There are claims in popular media that the Adorant from the Geißenklösterle cave, an ivory carving estimated to be 35,000 to 40,000 years old, is the first known depiction of the constellation. Scholars dismiss such interpretations, saying that perceived details such as a belt and sword derive from preexisting features in the grain structure of the ivory.

The Seri people of northwestern Mexico call the three stars in the belt of Orion Hapj (a name denoting a hunter) which consists of three stars: Hap (mule deer), Haamoja (pronghorn), and Mojet (bighorn sheep). Hap is in the middle and has been shot by the hunter; its blood has dripped onto Tiburón Island.

The same three stars are known in Spain and most of Latin America as “Las tres Marías” (Spanish for “The Three Marys”). In Puerto Rico, the three stars are known as the “Los Tres Reyes Magos” (Spanish for The three Wise Men).

The Ojibwa/Chippewa Native Americans call this constellation Mesabi for Big Man.

To the Lakota Native Americans, Tayamnicankhu (Orion’s Belt) is the spine of a bison. The great rectangle of Orion is the bison’s ribs; the Pleiades star cluster in nearby Taurus is the bison’s head; and Sirius in Canis Major, known as Tayamnisinte, is its tail. Another Lakota myth mentions that the bottom half of Orion, the Constellation of the Hand, represented the arm of a chief that was ripped off by the Thunder People as a punishment from the gods for his selfishness. His daughter offered to marry the person who can retrieve his arm from the sky, so the young warrior Fallen Star (whose father was a star and whose mother was human) returned his arm and married his daughter, symbolizing harmony between the gods and humanity with the help of the younger generation. The index finger is represented by Rigel; the Orion Nebula is the thumb; the Belt of Orion is the wrist; and the star Beta Eridani is the pinky finger.

The seven primary stars of Orion make up the Polynesian constellation Heiheionakeiki which represents a child’s string figure similar to a cat’s cradle. Several precolonial Filipinos referred to the belt region in particular as “balatik” (ballista) as it resembles a trap of the same name which fires arrows by itself and is usually used for catching pigs from the bush. Spanish colonization later led to some ethnic groups referring to Orion’s belt as “Tres Marias” or “Tatlong Maria.”

In Māori tradition, the star Rigel (known as Puanga or Puaka) is closely connected with the celebration of Matariki. The rising of Matariki (the Pleiades) and Rigel before sunrise in midwinter marks the start of the Māori year.

In Javanese culture, the constellation is often called Lintang Waluku or Bintang Bajak, referring to the shape of a paddy field plow.

The imagery of the belt and sword has found its way into popular western culture, for example in the form of the shoulder insignia of the 27th Infantry Division of the United States Army during both World Wars, probably owing to a pun on the name of the division’s first commander, Major General John F. O’Ryan.

The film distribution company Orion Pictures used the constellation as its logo.

In artistic renderings, the surrounding constellations are sometimes related to Orion: he is depicted standing next to the river Eridanus with his two hunting dogs Canis Major and Canis Minor, fighting Taurus. He is sometimes depicted hunting Lepus the hare. He sometimes is depicted to have a lion’s hide in his hand.

There are alternative ways to visualise Orion. From the Southern Hemisphere, Orion is oriented south-upward, and the belt and sword are sometimes called the saucepan or pot in Australia and New Zealand. Orion’s Belt is called Drie Konings (Three Kings) or the Drie Susters (Three Sisters) by Afrikaans speakers in South Africa and are referred to as les Trois Rois (the Three Kings) in Daudet’s Lettres de Mon Moulin (1866). The appellation Driekoningen (the Three Kings) is also often found in 17th- and 18th-century Dutch star charts and seaman’s guides. The same three stars are known in Spain, Latin America, and the Philippines as “Las Tres Marías” (The Three Marys), and as “Los Tres Reyes Magos” (The three Wise Men) in Puerto Rico.

Even traditional depictions of Orion have varied greatly. Cicero drew Orion in a similar fashion to the modern depiction. The Hunter held an unidentified animal skin aloft in his right hand; his hand was represented by Omicron² Orionis and the skin was represented by the 5 stars designated Pi Orionis. Kappa and Beta Orionis represented his left and right knees, while Eta and Lambda Leporis were his left and right feet, respectively. As in the modern depiction, Delta, Epsilon, and Zeta represented his belt. His left shoulder was represented by Alpha Orionis, and Mu Orionis made up his left arm. Lambda Orionis was his head and Gamma, his right shoulder. The depiction of Hyginus was similar to that of Cicero, though the two differed in a few important areas. Cicero’s animal skin became Hyginus’s shield (Omicron and Pi Orionis), and instead of an arm marked out by Mu Orionis, he holds a club (Chi Orionis). His right leg is represented by Theta Orionis and his left leg is represented by Lambda, Mu, and Epsilon Leporis. Further Western European and Arabic depictions have followed these two models.

Orion is located on the celestial equator, but it will not always be so located due to the effects of precession of the Earth’s axis. Orion lies well south of the ecliptic, and it only happens to lie on the celestial equator because the point on the ecliptic that corresponds to the June solstice is close to the border of Gemini and Taurus, to the north of Orion. Precession will eventually carry Orion further south, and by AD 14000, Orion will be far enough south that it will no longer be visible from the latitude of Great Britain.

Further in the future, Orion’s stars will gradually move away from the constellation due to proper motion. However, Orion’s brightest stars all lie at a large distance from the Earth on an astronomical scale—much farther away than Sirius, for example. Orion will still be recognizable long after most of the other constellations—composed of relatively nearby stars—have distorted into new configurations, with the exception of a few of its stars eventually exploding as supernovae, for example Betelgeuse, which is predicted to explode sometime in the next million years.

This article uses material from the Wikipedia article Orion (constellation), which is released under the Creative Commons Attribution-Share-Alike License 4.0

20250519

Rammstein ([ˈʁamʃtaɪn], lit. “ramming stone”) is a German Neue Deutsche Härte band formed in Berlin in 1994. The band’s lineup—consisting of lead vocalist Till Lindemann, lead guitarist Richard Kruspe, rhythm guitarist Paul Landers, bassist Oliver Riedel, drummer Christoph Schneider, and keyboardist Christian “Flake” Lorenz—has remained unchanged throughout their history, along with their approach to songwriting, which consists of Lindemann writing and singing the lyrics over instrumental pieces the rest of the band has completed beforehand. Prior to their formation, some members were associated with the punk rock acts Feeling B and First Arsch.

After winning a local contest, Rammstein was able to record demos and send them to different record labels, eventually signing with Motor Music. Working with producer Jacob Hellner, they released their debut album Herzeleid in 1995. Though the album initially sold poorly, the band gained popularity through their live performances and the album eventually reached No. 6 in Germany. Their second album, Sehnsucht, was released in 1997 and debuted at No. 1 in Germany, resulting in a worldwide tour lasting nearly four years and spawning the successful singles “Engel” and “Du hast” and the live album Live aus Berlin (1999). Following the tour, Rammstein signed with major label Universal Music and released Mutter in 2001. Six singles were released from the album, all charting in countries throughout Europe. The lead single, “Sonne”, reached No. 2 in Germany. Rammstein released Reise, Reise in 2004 and had two more singles reach No. 2 in Germany: “Mein Teil” and “Amerika”; the former song reached No. 1 in Spain, becoming their first No. 1 single.

Their fifth album, Rosenrot, was released in 2005, and the lead single, “Benzin”, reached No. 6 in Germany. Their second live album, Völkerball, was released in 2006. The band released their sixth album, Liebe ist für alle da, in 2009, with its lead single, “Pussy”, becoming their first No. 1 hit in Germany despite having a controversial music video that featured hardcore pornography. The band then entered a recording hiatus and toured for several years, releasing the Made in Germany greatest hits album as well as the Rammstein in Amerika and Paris live albums. After a decade without new music, Rammstein returned in 2019 with the song “Deutschland”, which became their second No. 1 hit in Germany. Their untitled seventh studio album was released in May 2019 and reached No. 1 in 14 countries. While sheltering during COVID-19 lockdowns, the band spontaneously wrote and recorded their eighth studio album, Zeit, which was released in April 2022.

Rammstein was one of the first bands to emerge within the Neue Deutsche Härte genre, with their debut album leading the music press to coin the term, and their style of music has generally had a positive reception from music critics. Commercially, the band has been very successful, earning many No. 1 albums as well as gold and platinum certifications in countries around the world. Their grand live performances, which often feature pyrotechnics, have contributed to the growth in their popularity. Despite success, the band has been subject to some controversies, with their overall image having been criticized; for instance, the song “Ich tu dir weh” forced its parent album Liebe ist für alle da to be placed on the “index” maintained by the German Federal Review Board for Media Harmful to Minors and re-released in Germany with the song removed due to its sexually explicit lyrics.

History

Founding and Herzeleid (1989–1996)

20250515

Grand Canyon National Park is a national park of the United States located in northwestern Arizona, the 15th site to have been named as a national park. The park’s central feature is the Grand Canyon, a gorge of the Colorado River, which is often considered one of the Wonders of the World. The park, which covers 1,217,262 acres (1,901.972 sq mi; 4,926.08 km2) of unincorporated area in Coconino and Mohave counties, received more than 4.7 million recreational visitors in 2023. The Grand Canyon was designated a World Heritage Site by UNESCO in 1979. The park celebrated its 100th anniversary on February 26, 2019.

History

The Grand Canyon became well known to Americans in the 1880s after railroads were built and pioneers developed infrastructure and early tourism. In 1903, President Theodore Roosevelt visited the site and said, The Grand Canyon fills me with awe. It is beyond comparison—beyond description; absolutely unparalleled throughout the wide world …. Let this great wonder of nature remain as it now is. Do nothing to mar its grandeur, sublimity and loveliness. You cannot improve on it. But you can keep it for your children, your children’s children, and all who come after you, as the one great sight which every American should see.

Despite Roosevelt’s enthusiasm and strong interest in preserving land for public use, the Grand Canyon was not immediately designated as a national park. The first bill to establish Grand Canyon National Park was introduced in 1882 by then-Senator Benjamin Harrison, which would have established Grand Canyon as the third national park in the United States, after Yellowstone and Mackinac. Harrison unsuccessfully reintroduced his bill in 1883 and 1886; after his election to the presidency, he established the Grand Canyon Forest Reserve in 1893. Theodore Roosevelt created the Grand Canyon Game Preserve by proclamation on November 28, 1906, and the Grand Canyon National Monument on January 11, 1908. Further Senate bills to establish the site as a national park were introduced and defeated in 1910 and 1911, before the Grand Canyon National Park Act (Pub. L. 65–277) was finally signed by President Woodrow Wilson on February 26, 1919. The National Park Service, established in 1916, assumed administration of the park.

The creation of the park was an early success of the conservation movement. Its national park status may have helped thwart proposals to dam the Colorado River within its boundaries. (Later, the Glen Canyon Dam would be built upriver.) A second Grand Canyon National Monument to the west was proclaimed in 1932. In 1975, that monument and Marble Canyon National Monument, which was established in 1969 and followed the Colorado River northeast from the Grand Canyon to Lees Ferry, were made part of Grand Canyon National Park. In 1979, UNESCO declared the park a World Heritage Site. The 1987 the National Parks Overflights Act found that “Noise associated with aircraft overflights at the Grand Canyon National Park is causing a significant adverse effect on the natural quiet and experience of the park and current aircraft operations at the Grand Canyon National Park have raised serious concerns regarding public safety, including concerns regarding the safety of park users.”

In 2010, Grand Canyon National Park was honored with its own coin under the America the Beautiful Quarters program. On February 26, 2019, the Grand Canyon National Park commemorated 100 years since its designation as a national park.

The Grand Canyon had been part of the National Park Service’s Intermountain Region until 2018. Today, the Grand Canyon is a part of Region 8, also known as the Lower Colorado Basin.

Legal history timeline

 – 1882 First unsuccessful attempt to establish a Grand Canyon National Park
 – 1893 Designated a “forest reserve” by President Benjamin Harrison (Presidential Proclamation #45)
 – 1908 Established as Grand Canyon National Monument by President Theodore Roosevelt (Presidential Proclamation #794)
 – 1919 Designation of Grand Canyon National Park by an act of Congress on February 26 (40 Stat 1175)
 – 1975 Grand Canyon National Park Enlargement Act an act of Congress on January 3 (88 Stat 2089) (Pub. L. 93–620)
 – 1979 Designation as a World Heritage Site on October 26

Administrators

 – William Harrison Peters (acting): August 1919 – September 1920
– Dewitt L. Raeburn: October 1920 – December 1921
– John Roberts White (acting): December 1921 – February 1922
– Walter Wilson Crosby: February 1922 – January 1924
– George C. Bolton (acting): January 1923 – June 1923
– John Ross Eakin: January 1924 – April 1927
– Miner Raymond Tillotson: April 1927 – December 1938
– James V. Lloyd (acting): December 1938 – February 1939
– Harold Child Bryant (acting): February 1939 – January 1940
– James V. Lloyd (acting): January 1940 – August 1940
– Frank Alvah Kittredge: August 1940 – July 1941
– Harold Child Bryant: August 1941 – March 1954
– Preston P. Patraw: May 1954 – July 1955
– John Sherman McLaughlin: August 1955 – March 1964
– Howard B. Stricklin: March 1964 – February 1969
– Robert R. Lovegren: April 1969 – July 1972
– Merle E. Stitt: August 1972 – January 1980
– Bruce W. Shaw (acting): January 1980 – May 1980
– Richard W. Marks: May 1980 – December 1988
– John C. Reed (acting): December 1988 – January 1989
– John H. Davis: January 1989 – August 1991
– Robert Chandler: October 1991 – October 1993
– Boyd Evison (acting): January 1994 – July 1994
– Robert L. Arnberger: July 1994 – October 2000
 – Dave Uberauga: 2011 – May 2016
 – Christine Lehnertz: August 2016 – March 2019
 – Ed Keable: April 2020 – present

Geography

The Grand Canyon, including its extensive system of tributary canyons, is valued for its combination of size, depth, and exposed layers of colorful rocks dating back to Precambrian times. The canyon itself was created by the incision of the Colorado River and its tributaries after the Colorado Plateau was uplifted, causing the Colorado River system to develop along its present path.

The primary public areas of the park are the South and North Rims, and adjacent areas of the canyon itself. The rest of the park is extremely rugged and remote, although many places are accessible by pack trail and backcountry roads. The South Rim is more accessible than the North Rim and accounts for 90% of park visitation.

The park headquarters are at Grand Canyon Village, not far from the South Entrance to the park, near one of the most popular viewpoints.

South Rim

Most visitors to the park come to the South Rim, arriving on Arizona State Route 64. The highway enters the park through the South Entrance, near Tusayan, Arizona, and heads eastward, leaving the park through the East Entrance. Interstate 40 provides access to the area from the south. From the north, U.S. Route 89 connects Utah, Colorado, and the North Rim to the South Rim. Overall, some 30 miles of the South Rim are accessible by road.

Grand Canyon Village is the primary visitor services area in the park. It is a full-service community, including lodging, fuel, food, souvenirs, a hospital, churches, and access to trails and guided walks and talks.

Several lodging facilities are available along the South Rim. Hotels and other lodging include El Tovar, Bright Angel Lodge, Kachina Lodge, Thunderbird Lodge, and Maswik Lodge, all of which are located in Grand Canyon Village, and Phantom Ranch, located on the canyon floor. There is also an RV Park named Trailer Village. All of these facilities are managed by Xanterra Parks & Resorts, while the Yavapai Lodge (also in the village area) is managed by Delaware North.

North Rim

The North Rim area of the park is located on the Kaibab Plateau and Walhalla Plateau, directly across the Grand Canyon from the principal visitor areas on the South Rim. The North Rim’s principal visitor areas are centered around Bright Angel Point. The North Rim is higher in elevation than the South Rim, at over 8,000 feet (2,400 m) of elevation. Because it is so much higher than the South Rim, it is closed from December 1 through May 15 each year, due to the enhanced snowfall at elevation. Visitor services are closed or limited in scope after October 15. Driving time from the South Rim to the North Rim is about 4.5 hours, over 220 miles (350 km).

On the North Rim is the historic Grand Canyon Lodge, managed by Forever Resorts, and a campground near the lodge managed by the national park staff.

Climate

According to the Köppen climate classification system, Grand Canyon National Park has five climate zones; Cold Semi-Arid (BSk), Humid Continental Dry Cool Summer (Dsb), Humid Continental Dry Warm Summer (Dsa), Warm Summer Mediterranean (Csb), and Hot Summer Mediterranean (Csa). The plant hardiness zone at Grand Canyon Visitor Center is 7a with an average annual extreme minimum temperature of 3.3 °F (−15.9 °C).

Activities

North Rim

There are few roads on the North Rim, but there are some notable vehicle-accessible lookout points, including Point Imperial, Roosevelt Point, and Cape Royal. Mule rides are also available to a variety of places, including several thousand feet down into the canyon.

Many visitors to the North Rim choose to make use of the variety of hiking trails including the Widforss Trail, Uncle Jim’s Trail, the Transept Trail, and the North Kaibab Trail. The North Kaibab Trail can be followed all the way down to the Colorado River, connecting across the river to the South Kaibab Trail and the Bright Angel Trail, which continue up to the South Rim of the Grand Canyon.

The Toroweap Overlook is located in the western part of the park on the North Rim. Access is via unpaved roads off Route 389 west of Fredonia, Arizona. The roads lead through Grand Canyon–Parashant National Monument and to the overlook.

South Rim

A variety of activities at the South Rim cater to park visitors. A driving tour (35 miles (56 km)) along the South Rim is split into two segments. The western drive to Hermit’s Point is eight miles (13 km) with several overlooks along the way, including Mohave Point, Hopi Point, and the Powell Memorial. From March to December, access to Hermit’s Rest is restricted to the free shuttle provided by the Park Service. The eastern portion to Desert View is 25 miles (40 km), and is open to private vehicles year round.

Walking tours include the Rim Trail, which runs west from the Pipe Creek viewpoint for about eight miles (13 km) of paved road, followed by seven miles (11 km) unpaved to Hermit’s Rest. Hikes can begin almost anywhere along this trail, and a shuttle can return hikers to their point of origin. Mather Point, the first view most people reach when entering from the south entrance, is a popular place to begin.

Private canyon flyovers are provided by helicopters and small airplanes out of Las Vegas, Phoenix, and Grand Canyon National Park Airport. Due to a crash in the 1990s, scenic flights are no longer allowed to fly within 1,500 feet (460 m) of the rim within the Grand Canyon National Park.

Grand Canyon Conservancy

The Grand Canyon Association (GCA) is the National Park Service’s official nonprofit partner. It raises private funds to benefit Grand Canyon National Park by operating retail shops and visitor centers within the park, and providing educational opportunities about the natural and cultural history of the region. Its goals include:

 – Creating Inter-tribal cultural sites
– Dark Sky Preservation
– Discovery and exploration of the Park
– Trail creation and preservation

Historic Buildings

Village Historic District

 – Hopi House (1905), Architect: Mary Jane Colter
– Verkamp’s Visitor Center
– Train Depot
– El Tovar Hotel
– Bright Angel Lodge (1935), Architect: Mary Jane Colter
– Buckey O’Neill Cabin (1890), Architect: William “Buckey” O’Neill
– Lookout Studio (1914), Architect Mary Jane Colter
– Kolb Studio (1904), Architects: Ellsworth Kolb and Emery Kolb

 – Hermit’s Rest (1914), Architect: Mary Jane Colter
– Phantom Ranch (1922), Architect: Mary Jane Colter
– Desert View Watchtower (1932), Architect: Mary Jane Colter

This article uses material from the Wikipedia article Grand Canyon National Park, which is released under the Creative Commons Attribution-Share-Alike License 4.0

20250511

Before we get started, I want to wish wish all the genuinely great moms a Happy Mother’s Day.  I’ve heard a few disturbing stories from friends and clients about truly horrible mothers over the last week or so and found it baffling and heartbreaking.  So to all the loving, selfless moms out there, the moms working 2-3 jobs to provide, the moms driving hours for their children to see their loved ones, the moms helping their children to accomplish their goals, instead of using their children to accomplish their own, I hope you have the best day possible today.

So I have not bothered checking stats here since early September.  A flurry of posts at the other place, after I celebrated a special day with a simple cake emoji here, prompted me to take a peek last week.  Damn, you people are hungry!  Last month saw a huge spike in traffic and resulted in a record setting month.  Since you all are still here wanting and waiting, I figured I’d give some updates.

First, I know I said that I might share her 2 definitive questions here, but after some discussion, she has asked me to refrain from doing so for the time being.  The first question demonstrates the depth of her work, while the second would reveal the nature of her profession.  Both of which she feels best left unmentioned until she gets further along in her process. Those of you from the other place already understand this, but for those of you here, I want to assure you that it’s certainly worth the wait.  Hell, this has been a year of talking about some very heavy topics, going back over 20+ years, and if I can be patient while she does her thing, so can you.  And to put an end to any and all speculation, she is not a LEO or lawyer, and is not involved in the legal field in any way, shape, or form. Although we do have laws protecting her work.  Believe me, the understanding, the catharsis, and the healing I have received from working with her has been far greater than all the doctors, the psychologist, and therapists, combined.  And at absolutely no cost to me, other than time.

Now, since everyone is still here, and checking in, I feel obligated to give you all something to read on a regular basis.  Sadly, I suspect that some of the traffic includes the babysitters, and those that want to control what I say here.  I will remind you that my word actually means something, and carries weight.  My loyalty lies solely with my friend now, and his wishes.  All of them.  So I still will not share anything here that could be used to further disrespect his wishes, or marginalize the friendship of those girls more than it already has been, against his wishes.  Instead, I will be sharing articles that I find interesting and/or relevant.  Of course, I may drop hints, subtle clues buried deep in the text of those articles, or hidden within the site, that may lead somewhere else.  If I do, it will not be easy.  I suspect only the most dedicated readers, those that are technically apt, and intelligent puzzle solvers, will be able to put the pieces together.

Finally, I have been working on a new adventures platform.  It’s something entirely different and heading in a new direction.  I’ve got a couple more pieces to put together  before it goes live, but I am really looking forward to getting it up and running.

Again, thank you for the interest and concern.  And be patient.

20240905

Still quite a bit of traffic coming in. Seriously, I appreciate the interest and concern, but there will be no major updates to this site for the foreseeable future. I will do what I can to demonstrate my love and concern for them, as well as to honor the dying wish of my friend, and insure the friendship between these 2 young ladies remains intact. But do not believe for a moment that I have or will forget. Every time I wake, whether it’s a good night’s sleep, or a rough night, I am instantly flooded with heartbreaking guilt and regret for leaving a defenseless little girl I cherish behind. So I will post public birthday wishes, and maybe an occasional thought in this space here, but nothing more. Besides, it was decided at the end of May that understanding would be best left to the professional. And she is doing an exceedingly thorough job. Honestly, receiving a colonoscopy in the middle of Times Square, live streamed on those jumbo screens and the Internet, would feel less invasive. But, that’s the price we pay for understanding, and she’s proven to be invaluable, presenting two definitive questions, that she and her work answer. Maybe I’ll be able to share those questions down the road, but for now, she’s in research mode.

Anyway, a couple days ago it was 03 September, and that marked a year since I turned a corner and forced myself to focus on the positive. To work to change my perspective, and hopefully others. That decision was based on my thinking about today, 05 September, which sadly, is no longer looked upon warmly as a day of positive change. While that experiment was only half-successful, it did provide an enormous amount of data to reinforce the facts. However, despite the reality of those facts, I am still focused on being positive, because every time I look at the “Cujo” puppet hanging on my wall, I know somebody I love will need that down the road. So, on that note, I hope everybody has a happy Egregious Lie Day!

https://youtu.be/g4xNBrEPlps?si=wfTj1c0IBlZmyljs

😉