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Historical events in Owens Valley inspired aspects of the film Chinatown.
| 300px Owens River from Bishop Tuff tableland. |
The Owens Valley stretches from Haiwee Reservoir in the south to the Sherwin Summit in the north (just north of the town of Bishop). Other towns in the Owens Valley include Lone Pine, Independence and Big PineBig Pine is a census-designated place located in Inyo County, California. As of the 2000 census, the CDP had a total population of 1,350. Geography Big Pine is located at 37°9'55" North, 118°17'47" West (37. 165377, -118. According to the United States Ce.
Beginning about 3 million years ago, the Sierra Nevada and White Mountains fault systems became active with repeated episodes of slip ( earthquakeAn earthquake is a trembling or shaking movement of the Earth's surface. Earthquakes typically result from the movement of faults, quasi-planar zones of deformation within its uppermost layers. The word earthquake is also widely used to indicate the sourcs) gradually producing the impressive relief of the eastern Sierra Nevada and White Mountain escarpmentIn geology, an escarpment is a transition zone between different physiogeographic provinces that involves an elevation differential, often involving high cliffs. Most commonly, an escarpment, also called a scarp, is a transition from one series of sedimens that bound the northern Owens Valley- Mono Basin region.
Owens Valley is a grabenIn geology, a graben is a depressed fault block bordered by normal faults. See also rift (geology). There are municipalities and communities names that have the name Graben ; In Germany Graben bei Augsburg Graben bei Treuchtlingen ; In Switzerland Graben,: a downdropped block of land between two vertical faults. Owens Valley is the westernmost graben in the Basin and Range Province.
The western flank of much of the valley has large moraineMoraine is the general term for debris of all sorts originally transported by glaciers or ice sheets that have since melted away. The following are commonly recognized types of moraine: Lateral moraine The talus and other material from the sides of a glacs coming off the Sierra Nevada. These unsorted piles of rock, boulders and dust were bulldozed to where they are by glacierA glacier is a large, long-lasting river of ice that is formed on land and moves in response to gravity. Equivalently, it is a multi-year ice accretion in mountainous terrain. The glacier fringe is the area where the glacier has recently melted. There ares during the last ice ageFor the animated movie, see Ice Age (movie . For the band, see Ice Age (band . An ice age is a period of long-term downturn in the temperature of Earth's climate, resulting in an expansion of the polar ice caps and mountain glaciers (" glaciation"). Glaci. An excellent example of a moraine is on California Highway 168 as it climbs into Buttermilk Country .
This graben was formed by a long series of earthquakes, such as the 1872 Lone Pine earthquake, that have moved the graben down and helped move the Sierra Nevada up. The graben is in fact much larger than the depth of the valley infers; gravity studies suggest that 10,000 feet (3 km) of sedimentary rock mostly fills the graben and that a very steep escarpment is buried under the western length of the valley. The topmost part of this escarpment is exposed at Alabama Hills.
See also: Inyo and Mono Craters. Small versions of the Devils Postpile, can be found, for example, by Little Lake .