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Whitewater River (California)
The Whitewater River is a small permanent stream in western Riverside County, California, with some upstream tributaries in southwestern San Bernardino County. The river's headwaters are in the San Bernardino Mountains, and it terminates at the Salton Sea in the Mojave Desert. The area drained by the Whitewater River is part of the larger endorheic Salton Sea drainage basin. Initially called Agua Blanco by early Spanish explorers, and later translated into English as ''white water'', the river received its name for its milky appearance created by the silicate and lime sediments it carries. The community of Whitewater was named after the river, and became a key stop on the Bradshaw Trail stagecoach runs. Geography San Bernardino Mountains The Whitewater River has three significant tributaries: the North, Middle, and South Forks, all within the Sand to Snow National Monument. The North Fork begins in the subalpine zone at about on San Gorgonio Mountain and descends steepl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salton Sea
The Salton Sea is a shallow, landlocked, highly saline body of water in Riverside and Imperial counties at the southern end of the U.S. state of California. It lies on the San Andreas Fault within the Salton Trough that stretches to the Gulf of California in Mexico. Over millions of years, the Colorado River has flowed into the Imperial Valley and deposited alluvium (soil), creating fertile farmland, building up the terrain, and constantly moving its main course and river delta. For thousands of years, the river has alternately flowed into the valley, or diverted around it, creating either a saline lake called Lake Cahuilla, or a dry desert basin, respectively. When the Colorado River flows into the valley, the lake level depends on river flows and the balance between inflow and evaporative loss. When the river diverts around the valley, the lake dries completely, as it did around 1580. Hundreds of archaeological sites have been found in this region, indicating possibly long-ter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mission Creek (Whitewater River)
Mission Creek (from Spanish: ''misión'') is a river in San Francisco, California. Once navigable from the Mission Bay inland to the vicinity of Mission Dolores, where several smaller creeks converged to form it, Mission Creek has long since been largely culverted. Its only remaining portion above-ground is the Mission Creek Channel which drains into China Basin.Museum of California Watershed map, access date December 31, 2008 The two Indian villages of Chutchui and Sitlintac were located on Mission Creek. Background The Spanish named the waterway, ''Arroyo de Nuestra Señora de los Dolores'', in English, "Our Lady of Sorrows ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whitewater, California
Whitewater (formerly, White Water) is a census-designated place in Riverside County, California. It is directly off Interstate 10 halfway between North Palm Springs and Cabazon on the way from Palm Springs to Los Angeles. It is known as the site of the San Gorgonio Pass Wind Farm. The ZIP Code is 92282, and the community is inside area code 760. The population was 859 at the 2010 census. The elevation is . Whitewater is famous for its recently renovated trout farm in the canyon of the Whitewater River. History Whitewater, still a populated place on the west bank of the Whitewater River, is located 10 miles (16 km) northwest of Palm Springs. It began as rest and watering place for travelers on the Bradshaw Trail between San Bernardino and La Paz Arizona Territory in 1862. With the start of the Colorado River Gold Rush the trail was created to ship goods and allow people to cross the desert to the new boom towns on the Colorado River and the interior of Arizona Territory. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endorheic
An endorheic basin (; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but drainage converges instead into lakes or swamps, permanent or seasonal, that equilibrate through evaporation. They are also called closed or terminal basins, internal drainage systems, or simply basins. Endorheic regions contrast with open and closed lakes, exorheic regions. Endorheic water bodies include some of the largest lakes in the world, such as the Caspian Sea, the world's largest inland body of water. Basins with subsurface outflows which eventually lead to the ocean are generally not considered endorheic; they are cryptorheic. Endorheic basins constitute local base levels, defining a limit of erosion and deposition processes of nearby areas. Etymology The term was borrowed from French ''endor(rh)éisme'', coined from the combining form ''endo-'' (from grc, ἔνΠ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mojave Desert
The Mojave Desert ( ; mov, Hayikwiir Mat'aar; es, Desierto de Mojave) is a desert in the rain shadow of the Sierra Nevada mountains in the Southwestern United States. It is named for the indigenous Mojave people. It is located primarily in southeastern California and southwestern Nevada, with small portions extending into Arizona and Utah. The Mojave Desert, together with the Sonoran, Chihuahuan, and Great Basin deserts, forms a larger North American Desert. Of these, the Mojave is the smallest and driest. The Mojave Desert displays typical basin and range topography, generally having a pattern of a series of parallel mountain ranges and valleys. It is also the site of Death Valley, which is the lowest elevation in North America. The Mojave Desert is often colloquially called the "high desert", as most of it lies between . It supports a diversity of flora and fauna. The desert supports a number of human activities, including recreation, ranching, and military training. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Source
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Whitewater River Below Palm Springs Airport
Whitewater forms in a rapid context, in particular, when a river's gradient changes enough to generate so much turbulence that air is trapped within the water. This forms an unstable current that froths, making the water appear opaque and white. The term "whitewater" also has a broader meaning, applying to any river or creek that has a significant number of rapids. The term is also used as an adjective describing boating on such rivers, such as whitewater canoeing or whitewater kayaking. Fast rivers Four factors, separately or in combination, can create rapids: gradient, constriction, obstruction, and flow rate. Gradient, constriction, and obstruction are streambed topography factors and are relatively consistent. Flow rate is dependent upon both seasonal variation in precipitation and snowmelt and upon release rates of upstream dams. Streambed topography Streambed topography is the primary factor in creating rapids, and is generally consistent over time. Increased fl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cathedral Canyon
A cathedral is a church that contains the ''cathedra'' () of a bishop, thus serving as the central church of a diocese, conference, or episcopate. Churches with the function of "cathedral" are usually specific to those Christian denominations with an episcopal hierarchy, such as the Catholic, Eastern Orthodox, Anglican, and some Lutheran churches.New Standard Encyclopedia, 1998 by Standard Educational Corporation, Chicago, Illinois; page B-262c Church buildings embodying the functions of a cathedral first appeared in Italy, Gaul, Spain, and North Africa in the 4th century, but cathedrals did not become universal within the Western Catholic Church until the 12th century, by which time they had developed architectural forms, institutional structures, and legal identities distinct from parish churches, monastic churches, and episcopal residences. The cathedral is more important in the hierarchy than the church because it is from the cathedral that the bishop governs the area under ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palm Canyon Wash (Whitewater River)
Palm Canyon Wash is an arroyo and tributary ephemeral stream or wash of the Whitewater River, in Riverside County, California. Palm Canyon Wash runs southward from Bull Canyon then north down Palm Canyon then east to its confluence with the Whitewater River at an elevation of . Its source is at , at an elevation of 6,165 feet, at the head of Bull Canyon on the southern western slope of a ridge in the San Jacinto Mountains The San Jacinto Mountains (''Avii Hanupach''Munro, P., et al. ''A Mojave Dictionary''. Los Angeles: UCLA. 1992. in Mojave) are a mountain range in Riverside County, located east of Los Angeles in southern California in the United States. The mou .... The waters of Palm Canyon Wash are augmented by Bull Canyon Spring at , at an elevation of . There the mouth of an unnamed creek flows north down from Vandeventer Flat into the head of Palm Canyon at its confluence with the creek of Palm Canyon Wash where it is flowing out of Bull Canyon at at an elevation of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chino Canyon (California)
Chino Canyon is a desert canyon in Riverside County, California, United States. It is one of the steepest canyons in North America, dropping from over at the south rim to less than on the valley floor in less than a mile. The Palm Springs Aerial Tramway was built in the canyon in 1963 to quickly transport people from the valley floor to the top of the mountain. After it was redesigned in 2000, it became the largest rotating aerial tramway in the world. The canyon is located in the northern end of the San Jacinto Mountains at the northwestern end of the Coachella Valley. Its associated stream is a tributary of the Whitewater River. The upper reaches of the canyon are bordered by Mount San Jacinto State Park, while the lower end terminates near California State Highway 111, and is being encroached by the outskirts of Palm Springs, California. In 1942, Chino Canyon was the site of a mid-air collision between American Airlines Flight 28 and a U.S. Army Air Force bomber. Chin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
San Gorgonio River
The San Gorgonio River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed March 16, 2011 river primarily flowing in western Riverside County, with a small upstream section in southwestern San Bernardino County, in southern California. Geography The river's headwaters arise in the San Bernardino Mountains, southwest of San Gorgonio Mountain at the southern base of Galena Peak within Sand to Snow National Monument. The source is at and an elevation of approximately 5600 feet at the confluence of Burnt and Sawmill canyons.''San Gorgiano Mountain'', 7.5 Minute Topographic Quadrangle, USGS, 1996 The river flows southwest through Banning Canyon then cuts back southeast through the town of Banning, California. It then heads east to its confluence with the Whitewater River in the western Coachella Valley at and an elevation of 1096 feet. It drains the land east of the San Gorgonio Pass, while the South Fork of the Santa Ana R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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