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・ Sodiq Safoyev
・ Sodiq Suraj
・ Sodium
・ Soda Creek Formation
・ Soda Creek/Deep Creek Band
・ Soda Dam
・ Soda Drinker Pro
・ Soda fountain
・ Soda Fountain Shuffle
・ Soda Gulch
・ Soda gun
・ Soda jerk
・ Soda Lake
・ Soda lake
・ Soda Lake (San Bernardino County)
Soda Lake (San Luis Obispo County)
・ Soda Lake (Washington State)
・ Soda Lakes
・ Soda lime
・ Soda locomotive
・ Soda Mountain Wilderness
・ Soda Mountains
・ SODA Off-Road Racing
・ Soda PDF
・ Soda Pictures
・ Soda pop (disambiguation)
・ Soda Pop-Rip Off
・ Soda Popinski
・ Soda Poppa
・ Soda pulping


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Soda Lake (San Luis Obispo County) : ウィキペディア英語版
Soda Lake (San Luis Obispo County)

Soda Lake is a shallow, ephemeral, alkali endorheic lake in the Carrizo Plain in southeastern San Luis Obispo County, California. The lake is located on the southwest side of the northern Carrizo Plain, east of San Luis Obispo. It can be reached by Soda Lake Road, which runs northwest–southeast between State Route 166 and State Route 58. The lake is at an elevation of and covers an area of about .
==Endorheic drainage basin==

Internal drainage of the Carrizo Plain and the formation of Soda Lake began during Pliocene-Pleistocene time when tectonic deformation associated with the San Andreas Fault defeated a stream that once drained the valley. An originally fresh to brackish water lake probably persisted through much of the Pleistocene during which coastal California was wetter and cooler than now. Diminished Holocene precipitation and a higher evaporation rate led to shrinkage of the ancestral lake and associated increased salinity which set the stage for clay dune formation.
About 30% of the closed or endorheic drainage basin is to the north of the lake and 70% is south of it. The Soda Lake complex consists of two larger basins, and at least 130 smaller pans. The large L-shaped northern basin is about 10.5 km² in area. The remaining basins, including both those that feed the northern basin and those that have no surface outlets, comprise an area of about 4.8 km². Water levels in the basins rise and fall seasonally. Rainfall on the Carrizo Plain is only about 20 cm in an average year but is higher on the surrounding mountains. Following exceptionally wet winters, typically El Niño years, the large northern and southern basins do not evaporate completely, although the water retreats toward the center of the basin leaving a salt crust up to 20 cm thick. Most of the large and small pans are fringed by clay dunes. It is one of the largest alkali wetlands remaining in natural condition in California. It supports fairy and brine shrimp, as well as migratory and nesting birds. A boardwalk was built along the shore to prevent damage to the saltbush habitat that borders the lake.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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