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Yosemite National Park

Yosemite National Park is a national park of the United States in California. It is bordered on the southeast by the Sierra National Forest and on the northwest by Stanislaus National Forest. The park is managed by the National Park Service and covers 1,187 mi2 (3,070 km2) in four counties – centered in Tuolumne and Mariposa, extending north and east to Mono and south to Madera. Designated a World Heritage Site in 1984, Yosemite is internationally recognized for its granite cliffs, waterfalls, clear streams, groves of giant sequoia, lakes, mountains, meadows, glaciers, and biological diversity. Almost 95 percent of the park is designated wilderness. Yosemite is one of the largest and least fragmented habitat blocks in the Sierra Nevada mountain range.

Toponym
The word Yosemite (derived from ''yohhe'meti, "they are killers" in Miwok) historically referred to the name that the Miwok gave to the Ahwahneechee, the resident indigenous tribe. Previously, the region had been called "Ahwahnee" ("big mouth") by the Ahwahneechee. The term Yosemite'' in Miwok is easily confused with a similar term for "grizzly bear", and is still a common misconception. ==History==
History
Ahwahneechee and the Mariposa Wars The first humans of Yosemite called themselves the Ahwahneechee, meaning "dwellers" in Ahwahnee. The Ahwahneechee People were the only tribe that lived within the park boundaries, but other tribes lived in surrounding areas. Together they formed a larger Indigenous population in California, called the Southern Sierra Miwok. They are related to the Northern Paiute and Mono tribes. Other tribes like the Central Sierra Miwoks and the Yokuts, who both lived in the San Joaquin Valley and central California, visited Yosemite to trade and intermarry. This resulted in a blending of culture that helped preserve their presence in Yosemite after early American settlements and urban development threatened their survival. About 70 years before the Gold Rush, the indigenous population was estimated to be 300,000, quickly dropping to 150,000, and just ten years later, only about 50,000 remained. It started in December 1850 when California funded a state militia to drive Native people from contested territory to suppress Native American resistance to the European American influx. Yosemite tribes often stole from settlers and miners, sometimes killing them, in retribution for the extermination/domestication of their people, and loss of their lands and resources. Accounts from this battalion were the first well-documented reports of European Americans entering Yosemite Valley. Attached to Savage's unit was Doctor Lafayette Bunnell, who later wrote about his awestruck impressions of the valley in The Discovery of the Yosemite. Bunnell is credited with naming Yosemite Valley, based on his interviews with Chief Tenaya. Bunnell wrote that Chief Tenaya was the founder of the Ahwahnee colony. Bunnell falsely believed that the word "Yosemite" meant "full-grown grizzly bear". Indigenous peoples' continuing presence (1885–1955), a Mono Lake Paiute and Southern Sierra Miwok Native American artist from the Yosemite region|163x163px After the Mariposa War, Native Americans continued to live in the Yosemite area in reduced numbers. The remaining Yosemite Ahwahneechee tribe members there were forced to relocate to a village constructed in 1851 by the state government. The last full-blooded Ahwahneechee died in 1931. Her name was Totuya, or Maria Lebrado. She was the granddaughter of Chief Tenaya and one of many forced out of her ancestral homelands. In 1953, the National Park Service banned all non-employee Natives from residing in the Park and evicted the non-employees who had residence. In 1969, with only a few families left in the Park, the National Park Service evicted the remaining Native people living within the Park (all Park employees and their families) to a government housing area for park employees and destroyed the village as part of a fire-fighting exercise. The National Park Service has created policies to protect sacred sites and allow Native People to return to their homelands and use National Park resources. Early tourists In 1855, entrepreneur James Mason Hutchings, artist Thomas Ayres, and two others were the first tourists to visit. Hutchings and Ayres were responsible for much of Yosemite's earliest publicity, writing articles and special issues about the valley. Ayres' style was detailed with exaggerated angularity. His works and written accounts were distributed nationally, and an exhibition of his drawings was held in New York City. Hutchings' publicity efforts between 1855 and 1860 increased tourism to Yosemite. Natives supported the growing tourism industry by working as laborers or maids. Later, they performed dances for tourists, acted as guides, and sold handcrafted goods, notably woven baskets. Galen Clark discovered the Mariposa Grove of giant sequoia in Wawona in 1857. He had simple lodgings and roads built. In 1879, the Wawona Hotel was built to serve tourists visiting Mariposa Grove. As tourism increased, so did the number of trails and hotels to build on it. The Wawona Tree, also known as the Tunnel Tree, was a giant sequoia that grew in the Mariposa Grove. It was tall, and was in circumference. When a carriage-wide tunnel was cut through the tree in 1881, it became even more popular as a tourist photo attraction. Carriages and automobiles traversed the road that passed through the tree. The tree was permanently weakened by the tunnel, and it fell in 1969 under a heavy load of snow. It was estimated to have been 2,100 years old. Yosemite's first concession was established in 1884 when John Degnan and his wife established a bakery and store. In 1916, the National Park Service granted a 20-year concession to the Desmond Park Service Company. It bought out or built hotels, stores, camps, a dairy, a garage, and other park facilities. The Hotel Del Portal was completed in 1908 by a subsidiary of the Yosemite Valley Railroad. It was located at El Portal, California just outside of Yosemite. The Curry Company started in 1899, led by David and Jennie Curry, to provide concessions. They founded Camp Curry, now Curry Village. Park service administrators felt that limiting the number of concessionaires in the park would be more financially sound. The Curry Company and its rival, the Yosemite National Park Company, were forced to merge in 1925 to form the Yosemite Park & Curry Company (YP&CC). The company built the Ahwahnee Hotel in 1926–27. Yosemite Grant Concerned by the impact of commercial interests, citizens, including Galen Clark and Senator John Conness, advocated protection for the area. The 38th United States Congress passed legislation that was signed by President Abraham Lincoln on June 30, 1864, creating the Yosemite Grant. This is the first time land was set aside specifically for preservation and public use by the U.S. government, and set a precedent for the 1872 creation of Yellowstone national park, the nation's first. According to Rolf Diamant and Ethan Carr, "the Yosemite Grant was a direct consequence of the war ... an embodiment of the ongoing process of remaking government ... an intentional assertion of a steadfast belief in the eventual Union victory." Yosemite Valley and the Mariposa Grove were ceded to California as a state park, and a board of commissioners was established two years later. Galen Clark was appointed by the commission as Grant's first guardian, but neither Clark nor the commissioners had the authority to evict homesteaders (which included Hutchings). Clark and the commissioners were ousted in a dispute that reached the Supreme Court in 1880. The two Supreme Court decisions affecting management of the Yosemite Grant are considered precedents in land management law. Hutchings became the new park guardian. John Muir was a Scottish-born American naturalist and explorer. Muir's leadership ensured that many National Parks were left untouched, including Yosemite. Muir wrote articles popularizing the area and increasing scientific interest in it. Muir was one of the first to theorize that the major landforms in Yosemite Valley were created by alpine glaciers, bucking established scientists such as Josiah Whitney. Muir wrote scientific papers on the area's biology. Landscape architect Frederick Law Olmsted emphasized the importance of conservation of Yosemite Valley. Increased protection efforts Overgrazing of meadows (especially by sheep), logging of giant sequoia, and other damage led Muir to become an advocate for further protection. Muir convinced prominent guests of the importance of putting the area under federal protection. One such guest was Robert Underwood Johnson, editor of Century Magazine. Muir and Johnson lobbied Congress for the Act that created Yosemite National Park on October 1, 1890. The State of California, however, retained control of Yosemite Valley and Mariposa Grove. Muir's writings raised awareness about the damage caused by sheep grazing, and he actively campaigned to virtually eliminate grazing from Yosemite's high country. The newly created national park came under the jurisdiction of the United States Army's Troop I of the 4th Cavalry on May 19, 1891, which set up camp in Wawona with Captain Abram Epperson Wood as acting superintendent. National Park Service The National Park Service (NPS) was formed in 1916, and Yosemite was transferred to that agency's jurisdiction. Tuolumne Meadows Lodge, Tioga Pass Road, and campgrounds at Tenaya and Merced lakes were also completed in 1916. Automobiles started to enter the park in ever-increasing numbers following the opening of all-weather highways to the park. The Yosemite Museum was founded in 1926 through the efforts of Ansel Franklin Hall. In the 1920s, the museum featured Native Americans practicing traditional crafts, and many Southern Sierra Miwok continued to live in Yosemite Valley until they were evicted from the park in the 1960s. Although the NPS helped create a museum that included Native American culture, its early actions and organizational values were dismissive of Yosemite Natives and the Ahwahneechee. In 1913, the O'Shaughnessy Dam was approved via passage of the Raker Act. In 1918, Clare Marie Hodges was hired as the first female Park Ranger in Yosemite. Following Hodges in 1921, Enid Michael was hired as a seasonal Park Ranger By 1968, traffic congestion and parking in Yosemite Valley during the summer months had become a concern. NPS reduced artificial inducements to visit the park, such as the Firefall, in which red-hot embers were pushed off a cliff near Glacier Point at night. In 1984, preservationists persuaded Congress to designate , or about 89 percent of the park, as the Yosemite Wilderness. As a wilderness area, it would be preserved in its natural state with humans being only temporary visitors. In 2025, laid-off National Park Service workers displayed a giant upside down American flag as a "distress signal" at El Capitan to protest layoffs recently made by the Trump administration. ==Geography==
Geography
Yosemite National Park is located in the central Sierra Nevada. Three wilderness areas are adjacent to Yosemite: the Ansel Adams Wilderness to the southeast, the Hoover Wilderness to the northeast, and the Emigrant Wilderness to the north. The park contains thousands of lakes and ponds, of streams, of hiking trails, and of roads. Two federally designated Wild and Scenic Rivers, the Merced and the Tuolumne, begin within Yosemite's borders and flow westward through the Sierra foothills into the Central Valley of California. Rocks and erosion , a granite monolith on Yosemite Valley's northern escarpment Almost all of the landforms are cut from the granitic rock of the Sierra Nevada Batholith (a batholith is a large mass of intrusive igneous rock that formed deep below the surface). About five percent of the park's landforms (mostly in its eastern margin near Mount Dana) are metamorphosed volcanic and sedimentary rocks. These roof pendants once formed the roof over the underlying granitic magma. Erosion acting upon different types of uplift-generated joint and fracture systems is responsible for producing the valleys, canyons, domes, and other features. These joints and fracture systems do not move, and are therefore not faults. Spacing between joints is controlled by the amount of silica in the granite and granodiorite rocks; more silica tends to form a more resistant rock, resulting in larger spaces between joints and fractures. Pillars and columns, such as Washington Column and Lost Arrow, are generated by cross joints. Erosion acting on master joints is responsible for shaping valleys and later canyons. Taft Point provides notable views of the valley floor, below. The high country of Yosemite contains other important features such as Tuolumne Meadows, Dana Meadows, the Clark Range, the Cathedral Range, and the Kuna Crest. The Sierra Crest and the Pacific Crest Trail run through Yosemite. Mount Dana and Mount Gibbs are peaks of red metamorphic rock. Granite peaks include Mount Conness, Cathedral Peak, and Matterhorn Peak. Mount Lyell is the highest point in the park, standing at . The Lyell Glacier is the largest glacier in the park and one of the few remaining in the Sierra. The park has three groves of ancient giant sequoia (Sequoiadendron giganteum) trees; the Mariposa Grove (200 trees), the Tuolumne Grove (25 trees), and the Merced Grove (20 trees). Water and ice flowing through Yosemite Valley, a U-shaped valley The Tuolumne and Merced River systems originate along the crest of the Sierra in the park and have carved river canyons deep. The Tuolumne River drains the entire northern portion of the park, an area of approximately . The Merced River begins in the park's southern peaks, primarily the Cathedral and Clark Ranges, and drains an area of approximately . Hydrologic processes, including glaciation, flooding, and fluvial geomorphic response, have been fundamental in creating park landforms. Wetlands flourish in valley bottoms throughout the park, and are often hydrologically linked to nearby lakes and rivers through seasonal flooding and groundwater. Meadow habitats, distributed at elevations from in the park, are generally wetlands, as are the riparian habitats found on the banks of Yosemite's watercourses. flows from a U-shaped hanging valley that was created by a tributary glacier. Yosemite is famous for its high concentration of waterfalls in a small area. Numerous sheer drops, glacial steps, and hanging valleys in the park feature spectacular cascades, especially during April, May, and June (as the snow melts). Located in Yosemite Valley, Yosemite Falls is the fourth tallest waterfall in North America at according to the World Waterfall Database. Also in the valley is the much lower volume Ribbon Falls, which has the highest single vertical drop, . Park glaciers are relatively small and occupy areas that are in almost permanent shade, such as north- and northeast-facing cirques. Lyell Glacier is the largest glacier in Yosemite (the Palisades Glaciers are the largest in the Sierra Nevada) and covers . None of the Yosemite glaciers are a remnant of the Ice Age alpine glaciers responsible for sculpting the Yosemite landscape. Instead, they were formed during one of the neoglacial episodes that have occurred since the thawing of the Ice Age (such as the Little Ice Age). Many Yosemite glaciers have disappeared, such as the Black Mountain Glacier that was marked in 1871 and had gone by the mid-1980s. Yosemite's final two glaciers – the Lyell and Maclure glaciers – have receded over the last 100 years and are expected to disappear as a result of climate change. Climate Yosemite has a Mediterranean climate (Köppen climate classification Csa), meaning most precipitation falls during the mild winter, and the other seasons are nearly dry (less than three percent of precipitation falls during the long, hot summers). Because of orographic lift, precipitation increases with elevation up to where it slowly decreases to the crest. Precipitation amounts vary from at elevation to at . Snow does not typically accumulate until November in the high country. It deepens into March or early April. Mean daily temperatures range from to at Tuolumne Meadows at . At the Wawona Entrance (elevation ), mean daily temperature ranges from . At the lower elevations below , temperatures are hotter; the mean daily high temperature at Yosemite Valley (elevation ) varies from . At elevations above , the hot, dry summer temperatures are moderated by frequent summer thunderstorms, along with snow that can persist into July. The combination of dry vegetation, low relative humidity, and thunderstorms results in frequent lightning-caused fires as well. ==Geology==
Geology
image) Tectonic and volcanic activity The location of the park was a passive continental margin during the Precambrian and early Paleozoic. Heat generated from the Farallon Plate subducting below the North American Plate led to the creation of an island arc of volcanoes on the west coast of proto-North America between the late Devonian and Permian periods. Material accreted onto the western edge of North America, and mountains were raised to the east in Nevada. The first phase of regional plutonism started 210 million years ago in the late Triassic and continued throughout the Jurassic to about 150 million years before present (BP), which led to the creation of the Sierra Nevada Batholith. Around the same time, the Nevadan orogeny built the Nevadan mountain range (also called the Ancestral Sierra Nevada) to a height of . The second major pluton emplacement phase lasted from about 120 million to 80 million years ago during the Cretaceous. Starting 20 million years ago (in the Cenozoic) and lasting until 5 million years ago, a now-extinct extension of Cascade Range volcanoes erupted, bringing large amounts of igneous material to the area. These igneous deposits blanketed the region north of the Yosemite region. Volcanic activity persisted past 5 million years BP east of the current park borders in the Mono Lake and Long Valley areas. Uplift and erosion s cause erosion in granitic rocks, creating many domes including Half Dome. Starting 10 million years ago, vertical movement along the Sierra fault started to uplift the Sierra Nevada. Subsequent tilting of the Sierra block and the resulting accelerated uplift of the Sierra Nevada increased the gradient of western-flowing streams. The streams consequently ran faster and thus cut their valleys more quickly. Additional uplift occurred when major faults developed to the east, forming Owens Valley from Basin and Range-associated extensional forces. Sierra uplift accelerated again about two million years ago during the Pleistocene. The uplifting and increased erosion exposed granitic rocks to surface pressures, resulting in exfoliation (responsible for the rounded shape of the many domes in the park) and mass wasting following the numerous fracture joint planes (cracks, especially vertical ones) in the now solidified plutons. Pleistocene glaciers further accelerated this process, while glacial meltwater transported the resulting talus and till from valley floors. Numerous vertical joint planes controlled where and how fast erosion took place. Most of these long, linear, and very deep cracks trend northeast or northwest and form parallel, often regularly spaced sets. Glacial systems reached depths of up to and left their marks. The longest glacier ran down the Grand Canyon of the Tuolumne River for , passing well beyond Hetch Hetchy Valley. Merced Glacier flowed out of Yosemite Valley and into the Merced River Gorge. Lee Vining Glacier carved Lee Vining Canyon and emptied into Lake Russel (the much-enlarged ice age version of Mono Lake). Only the highest peaks, such as Mount Dana and Mount Conness, were not covered by glaciers. Retreating glaciers often left recessional moraines that impounded lakes such as the long Lake Yosemite (a shallow lake that periodically covered much of the floor of Yosemite Valley). ==Ecology and environment==
Ecology and environment
Habitats in Yosemite Valley The park has an elevation range from and contains five major vegetation zones: chaparral and oak woodland, lower montane forest, upper montane forest, subalpine zone, and alpine. Of California's 7,000 plant species, approximately 50% occur in the Sierra Nevada, and more than 20% within the park. The park contains suitable habitat for more than 160 rare plants, with rare local geologic formations and unique soils characterizing the restricted ranges many of these plants occupy. In contrast to surrounding lands, which have been significantly altered by logging, the park contains some of old-growth forest. Taken together, the park's varied habitats support over 250 species of vertebrates, which include fish, amphibians, reptiles, birds, and mammals. Yosemite's western boundary has habitats dominated by mixed coniferous forests of ponderosa pine, sugar pine, incense cedar, white fir, Douglas fir, and a few stands of giant sequoia, interspersed by areas of black oak and canyon live oak. These habitats support relatively high wildlife diversity. Wildlife include black bear, coyote, raccoon, mountain kingsnake, Gilbert's skink, white-headed woodpecker, bobcat, river otter, gray fox, red fox, brown creeper, two species of skunk, cougar, spotted owl, and bats. Despite the richness of high-quality habitats in Yosemite, the brown bear, California condor, and least Bell's vireo have become extinct in the park within historical time, and another 37 species currently have special status under either California or federal endangered species legislation. The most serious current threats include loss of a natural fire regime, exotic species, air pollution, habitat fragmentation, and climate change. On a more local basis, factors such as road kill and the availability of human food have affected some wildlife species. competes with Yosemite's native plants. Bull thistle (Cirsium vulgare), common mullein (Verbascum thapsus), and Klamath weed (Hypericum perforatum) have been identified as noxious pests in Yosemite since the 1940s. More recently recognized species are yellow star thistle (Centaurea solstitialis), sweet clover (Melilot spp.), Himalayan blackberry (Rubus armeniacus), cut-leaved blackberry (Rubus laciniatus) and large periwinkle (Vinca major). Restoration Projects In 2016, The Trust for Public Land (TPL) purchased Ackerson Meadow, a 400-acre tract (160 ha) on the western edge of the park for $2.3 million. Ackerson Meadow was originally included in the proposed 1890 park boundary but never acquired by the federal government. The purchase and donation of the meadow was made possible through a cooperative effort by TPL, NPS, and Yosemite Conservancy. On September 7, 2016, NPS accepted the donation of the land, making the meadow the largest addition to Yosemite since 1949. The meadow was purchased and donated because it faced several issues, including extensive gully erosion from years of cattle ranching, timber harvest, and domestic water diversion which have over the decades lowered the water table drying out vegetation. Additionally, the use of roads over the years had compacted soils, and invasive species have taken hold across the wetland. To address these issues, the National Park Service, in conjunction with the Forest Service, restored the meadow at a cost of $17.7 million with funding coming from a variety of nonprofit organizations. Today the wetland has been restored as a critical wildlife corridor and serves important functions like flood attenuation, carbon sequestration, and improving water quality. Wildfires burns in Little Yosemite Valley, 2014 Indigenous residents intentionally set small fires in the early 1860s and before to clear the ground of brush as part of their farming practices. Some early uncontrolled forest fires were set accidentally by the militia group led by Major John Savage when the group burned down the Ahwahneechee camp in an attempt to expel them. The house fires eventually spread to a large section of the forest, and the militia group ended up having to abandon their raid to save their own camp from the conflagration. Small fires damage the income generated by tourism. During late July and early August 2018, the Valley and other sections of the park, temporarily closed due to the Ferguson Fire at its western boundary. The closing was the largest in almost thirty years. Climate change Yosemite National Park has been showing signs of climate change over the past few decades. Temperatures have gone up and caused the Sierra Nevada snowpack to shrink compared to what it used to be. Snow melts earlier now, more winter precipitation is falling as rain, and the timing of river flow throughout the park has shifted. These changes affect the plants and animals that live in the park. For example, climate change can decrease both atmospheric and soil moisture in the Sierra Nevada, which will harm drought-sensitive plant species. Climate change is making it more difficult for coniferous forests to return after wildfire in the Western United States. Smoke from wildfires in the Sierra Nevada can drift for many miles, causing human illness and excess death far away from the park. ==Activities==
Activities
Public access Yosemite National Park is open year-round, though certain roads close during snowy months, usually from November through May or June. Certain trails also close during winter, including The 4-Mile Trail and part of The Mist Trail. Traffic congestion in the valley is heavy during the peak summer season (June to August), and a free shuttle bus system operates in the valley. Parking in the valley during the summer is often full. Amtrak and the Yosemite Area Regional Transportation System (YARTS) provide public transit into Yosemite from four gateway communities: Merced, Fresno, Sonora, and Mammoth Lakes/Lee Vining. The Merced route provides service year-round. The natural and cultural history of Yosemite Valley is presented at the Yosemite Valley Visitor Center, the adjoining Yosemite Museum, and the Nature Center at Happy Isles. The parks' two National Historic Landmarks are the Sierra Club's LeConte Memorial Lodge (Yosemite's first public visitor center), and the Ahwahnee Hotel. Camp 4 is on the National Register of Historic Places. Hiking cables on a busy summer day in 2008 Over of trails are available to hikers A maximum of 300 hikers, selected by lottery, are permitted to advance beyond the base of the subdome each day, including 225 day hikers and 75 backpackers. The park can be divided into five sections—Yosemite Valley, Wawona/Mariposa Grove/Glacier Point, Tuolumne Meadows, Hetch Hetchy, and Crane Flat/White Wolf. Numerous books describe park trails, while the National Park Service provides free information. Between late spring and early fall, much of the park can be accessed for backpacking trips. All overnight trips into the back country require a wilderness permit Driving While some locations in Yosemite are accessible only on foot, other locations can be reached via road. The most famous road is Tioga Road. Bicycles are allowed on the roads, but only of paved off-road trails are available in Yosemite Valley itself; mountain biking is not allowed. Climbing Rock climbing is an important part of Yosemite. In particular the valley is surrounded by summits such as Half Dome and El Capitan. Camp 4 is a walk-in campground in the Valley that was instrumental in the development of rock climbing as a sport, and is listed on the National Register of Historic Places. Climbers can generally be spotted in the snow-free months on anything from ten-foot-high (3 m) boulders to the face of El Capitan. Classes on rock climbing are offered there. Tuolumne Meadows is well known for rock and mountain climbing. Winter activities walk in the park Away from the Valley, the park is snowed in during the winter months, with many roads closed. Downhill skiing is available at the Badger Pass Ski Area—the oldest downhill skiing area in California, operating from mid-December through early April. Much of the park is open to cross-country skiing and snowshoeing, and backcountry ski huts are available. Wilderness permits are required for backcountry overnight ski trips. The Bracebridge dinner is an annual holiday event, held since 1927 at the Ahwahnee Hotel, inspired by Washington Irving's descriptions of Squire Bracebridge and English Christmas traditions of the 18th century in his Sketch Book. Between 1929 and 1973, the show was organized by Ansel Adams. Other Yosemite has 13 official campgrounds. Bicycle rentals are available from spring through fall. Over of paved bike paths are available in Yosemite Valley. In addition, bicyclists can ride on roads. Helmets are required for children under 18 years of age. Off-trail riding and mountain biking are not permitted in the park. Water activities are plentiful during warmer months. Rafting can be done through the valley on the Merced River from late May to July. Swimming pools are available at Yosemite Lodge and Curry Village. ==In popular culture==
In popular culture
sign advising young visitors not to feed the bears at Yosemite National Park. The opening scenes of Star Trek V: The Final Frontier (1989) were filmed in Yosemite National Park. Films such as The Last of the Mohicans (1920) and Maverick (1994) have also been shot there. The 2014 documentary Valley Uprising is centered around Yosemite Valley and its history with an emphasis on climbing culture. The Academy Award-winning 2018 documentary Free Solo was filmed in Yosemite. The 2018 Travis Scott album Astroworld's twelfth song is titled "Yosemite". The Dawn Wall, a 2017 documentary, was filmed there. The park is a playable map in the park management simulation game, Jurassic World Evolution 2. Untamed, a 2025 drama murder mystery series, though set almost entirely in Yosemite, was filmed in the Canadian province of British Columbia. ==See also==
General references
• • Diamant, Rolf, and Carr, Ethan (2022). Olmsted and Yosemite: Civil War, Abolition, and The National Park Idea. Amherst, Massachusetts: Library of American Landscape History Online review of this book. • • • • Muir, John. "Features of the Proposed Yosemite National Park " The Century; a popular quarterly (Sept. 1890) 40#5 • • • • • • • • • ==External links==
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