Grand Canyon of the Tuolumne

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Grand Canyon of the Tuolumne
Grand Canyon of the Tuolumne River (6120571907).jpg
The Grand Canyon of the Tuolumne, looking west. Muir Gorge cuts diagonally across the middleground.
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Grand Canyon of the Tuolumne
Location in California
Floor elevation3,957 ft (1,206 m)
Geography
Location Sierra Nevada, California, United States
Coordinates 37°56′45″N119°31′04″W / 37.9457547°N 119.5176662°W / 37.9457547; -119.5176662 [1]

The Grand Canyon of the Tuolumne is the notable canyon section of the river valley of the Tuolumne River, located within Yosemite National Park, in Tuolumne County and the Sierra Nevada, California.

Contents

As defined by the United States Geological Survey, the canyon begins at Glen Aulin and ends directly above Hetch Hetchy Valley. [1]

Geography

The Grand Canyon of the Tuolumne starts at Glen Aulin, immediately below the confluence of Cold Canyon, Conness Creek, and the Tuolumne River. Here, the valley walls pull away from each other and become steeper. The water meanders and forms deep pools. After the waterfall that marks the end of Glen Aulin, the canyon becomes deeper again, and roughly "V"-shaped in cross-section. The walls are not as steep and bare as those of Yosemite Valley. The flora of the valley bottom is a haphazard melange of chaparral, manzanita scrub and oak woodland [2] characteristic of the foothills and lowlands with a coniferous forest reminiscent of (but different from) that found above the canyon rim. This vegetation clings and clambers up every ledge of the valley walls to the top, giving it a lusher appearance than Yosemite Valley, though this area in fact experiences a drier climate.[ citation needed ]

Many dramatic waterfalls are found in the Grand Canyon of the Tuolumne. [3] Whereas Yosemite Valley's celebrated falls occur on tributary streams along the sides, these lie on the main river itself. Many watercourses do join the Tuolumne River, but their canyons form deep clefts in the sides of the Grand Canyon and descend to its bottom. The Tuolumne's own bed, beginning even above Glen Aulin, is fashioned as a great staircase punctuated by waterfalls.

Waterwheel Falls Waterwheel Falls in Yosemite.jpg
Waterwheel Falls

Perhaps the greatest of these is 800-foot (240 m) Waterwheel Falls, named for a dramatic circular plume of water that appears when the river and the winds run high. A few kilometres below Glen Aulin, the walls of the lower canyon pinch together to form a narrow chasm of less than 1 kilometre (0.62 mi) in length, the Muir Gorge. A short way below the Muir Gorge, the Grand Canyon widens again, much as it does at Glen Aulin, though here it is deeper. This broad plain bears the name of "Pate Valley." Some 6 kilometres (3.7 mi) below here, Hetch Hetchy Reservoir (created by O’Shaughnessy Dam) claims the Tuolumne River.

Recreation

A trail runs along the Tuolumne River from its headwaters to below Pate Valley (though it leaves the valley floor for some time to avoid the impassable Muir Gorge). It is diligently built, but due to the nature of the terrain it is often rocky, steep and generally difficult. The walking distance from the Tioga Road to the Glen Aulin High Sierra Camp is roughly 10 kilometres (6.2 mi) . White Wolf campground, southeast of Hetch Hetchy Reservoir, is within day-hiking distance of the canyon rim, but the return trip from the very bottom is long and steep. Between the eastern tip of the reservoir and the point where the trail begins the climb to White Wolf, the valley is a trackless wilderness.

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<span class="mw-page-title-main">Yosemite National Park</span> National park in California, United States

Yosemite National Park is a national park in California. It is bordered on the southeast by Sierra National Forest and on the northwest by Stanislaus National Forest. The park is managed by the National Park Service and covers 759,620 acres 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, giant sequoia groves, 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.

<span class="mw-page-title-main">Sierra Nevada</span> Mountain range in the Western United States

The Sierra Nevada is a mountain range in the Western United States, between the Central Valley of California and the Great Basin. The vast majority of the range lies in the state of California, although the Carson Range spur lies primarily in Nevada. The Sierra Nevada is part of the American Cordillera, an almost continuous chain of mountain ranges that forms the western "backbone" of the Americas.

<span class="mw-page-title-main">Tuolumne Meadows</span> Meadow in Yosemite National Park, US

Tuolumne Meadows is a gentle, dome-studded, sub-alpine meadow area along the Tuolumne River in the eastern section of Yosemite National Park in the United States. Its approximate location is 37°52.5′N119°21′W. Its approximate elevation is 8,619 feet (2,627 m). The term Tuolumne Meadows is also often used to describe a large portion of the Yosemite high country around the meadows, especially in context of rock climbing.

<span class="mw-page-title-main">Hetch Hetchy</span> Valley, reservoir, and aqueduct in California, USA

Hetch Hetchy is a valley, a reservoir, and a water system in California in the United States. The glacial Hetch Hetchy Valley lies in the northwestern part of Yosemite National Park and is drained by the Tuolumne River. For thousands of years before the arrival of settlers from the United States in the 1850s, the valley was inhabited by Native Americans who practiced subsistence hunting-gathering. During the late 19th century, the valley was renowned for its natural beauty – often compared to that of Yosemite Valley – but also targeted for the development of water supply for irrigation and municipal interests. The controversy over damming Hetch Hetchy became mired in the political issues of the day. The law authorizing the dam passed Congress on December 7, 1913. In 1923, the O'Shaughnessy Dam was completed on the Tuolumne River, flooding the entire valley under the Hetch Hetchy Reservoir. The dam and reservoir are the centerpiece of the Hetch Hetchy Project, which in 1934 began to deliver water 167 miles (269 km) west to San Francisco and its client municipalities in the greater San Francisco Bay Area.

<span class="mw-page-title-main">Geology of the Yosemite area</span>

The exposed geology of the Yosemite area includes primarily granitic rocks with some older metamorphic rock. The first rocks were laid down in Precambrian times, when the area around Yosemite National Park was on the edge of a very young North American continent. The sediment that formed the area first settled in the waters of a shallow sea, and compressive forces from a subduction zone in the mid-Paleozoic fused the seabed rocks and sediments, appending them to the continent. Heat generated from the subduction created island arcs of volcanoes that were also thrust into the area of the park. In time, the igneous and sedimentary rocks of the area were later heavily metamorphosed.

<span class="mw-page-title-main">Tuolumne River</span> River from Yosemite to the San Joaquin Valley, California

The Tuolumne River flows for 149 miles (240 km) through Central California, from the high Sierra Nevada to join the San Joaquin River in the Central Valley. Originating at over 8,000 feet (2,400 m) above sea level in Yosemite National Park, the Tuolumne drains a rugged watershed of 1,958 square miles (5,070 km2), carving a series of canyons through the western slope of the Sierra. While the upper Tuolumne is a fast-flowing mountain stream, the lower river crosses a broad, fertile and extensively cultivated alluvial plain. Like most other central California rivers, the Tuolumne is dammed multiple times for irrigation and the generation of hydroelectricity.

<span class="mw-page-title-main">Raker Act</span>

The Raker Act was an act of the United States Congress that permitted building of the O'Shaughnessy Dam and flooding of Hetch Hetchy Valley in Yosemite National Park, California. It is named for John E. Raker, its chief sponsor. The Act, passed by Congress in 1913 by the Wilson administration, specified that because the source of the water and power was on public land, no private profit could be derived from the development. The plan for damming the valley was fought for years by John Muir. Construction of the dam was finished in 1923.

<span class="mw-page-title-main">Wapama Falls</span> Waterfall in California, United States

Wapama Falls is the larger of two waterfalls located on the northern wall of Hetch Hetchy Valley below Hetch Hetchy Dome, in Yosemite National Park. It flows almost year-round and during peak flow has been known to inundate the trail bridge crossing its base, making the falls impossible to pass. The falls consist of two primary drops angled roughly 60 degrees to each other, and a broad cascade at its base.

<span class="mw-page-title-main">Cherry Creek (Tuolumne River tributary)</span> River in California, United States

Cherry Creek is a large, swift-flowing stream in the Sierra Nevada mountain range, and is the largest tributary of the Tuolumne River. The creek is 40 miles (64 km) long measured to its farthest headwaters; the main stem itself is 26 miles (42 km) long, draining a watershed of 234 square miles (610 km2) in the Stanislaus National Forest. Part of the drainage also extends into the northwest corner of Yosemite National Park.

<span class="mw-page-title-main">William Edward Colby</span>

William Edward Colby was an American lawyer, conservationist, and first Secretary of the Sierra Club.

The Hetch Hetchy Railroad (HHRR) was a 68-mile (109 km) standard gauge Class III railroad constructed by the City of San Francisco to support the construction and expansion of the O'Shaughnessy Dam across Hetch Hetchy Valley.

<span class="mw-page-title-main">Geography of the Yosemite area</span>

Yosemite National Park is located in the central Sierra Nevada of California. 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.

<span class="mw-page-title-main">Kolana Rock</span>

Kolana Rock is a prominent granite dome located along the southern edge of Hetch Hetchy Valley in Yosemite National Park. John Muir stated that Kolana was the Indian name for the rock. It towers 2,000 feet (610 m) above the Hetch Hetchy Reservoir, and is across from Hetch Hetchy Dome.

<span class="mw-page-title-main">Falls Creek (California)</span> River in California, United States

Falls Creek, also known as the Falls River, is a tributary of the Tuolumne River in Yosemite National Park, California, United States. The creek begins at the northern boundary of the national park and flows 24 miles (39 km) to empty into the Tuolumne at Hetch Hetchy Reservoir, dropping over two well-known waterfalls. The Pacific Crest Trail and other national park trails follow the creek for much of its course.

<span class="mw-page-title-main">Restore Hetch Hetchy</span>

Restore Hetch Hetchy is a US non-profit organization seeking to restore the Hetch Hetchy Valley in Yosemite National Park to its original condition.

<span class="mw-page-title-main">O'Shaughnessy Dam (California)</span> Dam in Tuolumne County, California, United States

O'Shaughnessy Dam is a 430-foot (131 m) high concrete arch-gravity dam in Tuolumne County, California, United States. It impounds the Tuolumne River, forming the Hetch Hetchy Reservoir at the lower end of Hetch Hetchy Valley in Yosemite National Park, about 160 miles (260 km) east of San Francisco. The dam and reservoir are the source for the Hetch Hetchy Aqueduct, which provides water for over two million people in San Francisco and other municipalities of the west Bay Area. The dam is named for engineer Michael O'Shaughnessy, who oversaw its construction.

Piute Creek is a 19-mile (31 km) long stream in northern Yosemite National Park, in Tuolumne County, California. It is a major tributary of the Tuolumne River, draining a rugged and remote area of the Sierra Nevada.

<span class="mw-page-title-main">Rancheria Creek (Tuolumne County, California)</span> Stream in California

Rancheria Creek is a 22-mile (35 km) long stream in northern Yosemite National Park mostly in Tuolumne County, California and is a tributary of the Tuolumne River. Draining a large area of the Sierra Nevada, it is the largest tributary of the Tuolumne within Yosemite National Park. The stream is labeled as Kerrick Creek on some early maps.

References

  1. 1 2 "Grand Canyon of the Tuolumne". Geographic Names Information System . United States Geological Survey, United States Department of the Interior.
  2. "Tuolumne Wild & Scenic River". California Wilderness Coalition. Retrieved 2018-07-27.
  3. "Yosemite High Country Waterfalls". World of Waterfalls. Retrieved 2018-07-27.