Death Valley

1:DEATH VALLEY

This article is nearby the valley. For the park, see Death Valley National Park. For other usages, see Passing Valley.

1:Death Valley is a located in Eastern California, in the north Mojave Desert adjacent the Countless Bowl Desert. It is one of the burning places in the world lengthways with deserts in the Middle East.

Located near the border of California and Nevada, in the Excessive Basin, east of the Sierra Nevada mountains, Death Valley organizes much of Death Valley National Park and is the principal feature of the Mojave and Colorado Deserts Biosphere Backup. It is located mostly in Inyo Region, California. It runs from northern to south between the Armargosa Range on the east and the Panamint Range on the west; the Gossip Mountains and the Owls head Mountains form its northerly and southern limits, respectively. It has an area of about 3,000 sq. mi 7,800 km². The uppermost point in Death Valley itself is Agreement Peak in the Panamint Collection, which has an promotion of 11,043 feet (3,366 m).

Geology

Main article: Geology of the Death Valley area

showing the system of once-interconnected in Calefornia.

Death Valley is an example of a graven, or a down released block of land between two mountain ranges. It lies at the southern end of a environmental trough known as Walker Lane, which runs north to Oregon. The valley is intersected by a right side strike slip fault system, represented by the Death Valley Liability and the Furnace Creek Fault. The eastern end of the left lateral Garlicky Fault intersects the Death Valley Fault. Furnace Stream and the Armargosa Waterway flow through the valley but eventually disappear into the sands of the valley floor.

Death Valley, July 3, 2017, Sentinel-2 true color cable

Death Valley also contains salt pans. According to current physical consensus, at various times through the middle of the Pleistocene era, which over unevenly 10,000–12,000 years ago, an internal lake meant to as Lake Manly formed in Death Valley. Lake Manly was nearly 100 miles (160 km) extended and 600 feet (180 m) deep, the end-basin in a chain of lakes that inaugurated with Mono Lake in the north and continued from side to side multiple basins down the Owens River Valley through Searle’s and China Ponds and the Panamint Valley to the immediate west.

As the area twisted to desert, the water evaporated, leaving the abundance of evaporate salts such as public sodium salts and borax, which were later broken during the modern history of the region, mainly 1883 to 1907.

Climate

Death Valley has a subtropical, hot desert weather with long, extremely hot summers and short, mild winters, as well as little rainfall.
Death Valley is exceptionally dry because it sits in the rain shadow of four bigger mountain ranges (including the Sierra Nevada and Panamint Range). Moisture moving inland from the Pacific Ocean must pass eastward over compound mountains to reach Death Valley; as air masses are forced uphill by each range, the air cools and dampness condenses to fall as rain or snow on the western slopes. When the air the many ultimately reach Death Valley, most of the wetness has already been "squeezed out" and there is little left to fall as rain fall.
The dangerous heat of Death Valley is attributable to a confluence of geographical and topographic factors. Experts have identified a number of key backers  to Death Valley's famously hot conditions:·         Solar heating: The valley's outward (consisting of soil, rocks, sand, etc.) undertakes powerful solar heating due to clear, dry air and dark, sparingly vegetated land. This is especially manifest in summer when the sun is straight overhead.
·         Air sinking and warming: Any air mass that bowls into lower elevations (e.g. 282 feet below sea level at bad water) gets compressed and warmed—due to the developed atmospheric pressure originate at lower elevations. This is an example of adiabatic warming.
·         Trapping of warm air: Warm air naturally increases and cools.
·         But in Death Valley this air is subject to continual rewarming as it is stuck by high, steep valley ramparts and recycled back to the gorge floor. Another factor that tricks warm air is the valley's north-south location, which runs perpendicular to prevailing west-to-east winds.
·         Migration of warm air from other areas (advection): Sincere desert regions surrounding Death Valley, especially to the south and east, often heat air before it come to in Death Valley.
·         Warm mountain winds: As winds are enforced up and over mountains (e.g. the numerous arrays west of Death Valley), the breezes can become progressively heater due to several factors. The resulting dry, deep winds are known as fen winds. Their warmth can in part be produced by the release of latent heat, which occurs when water gas condenses into clouds.

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