File:Mono_Lake_aerial.jpg · Wikimedia Commons · See Wikimedia Commons
Key facts
- Location
- Mono County, California
- Type
- Endorheic , Monomictic
- Primary inflows
- Rush Creek , Lee Vining Creek , Mill Creek
- Primary outflows
- Evaporation
- Catchment area
- 780 sq mi (2,030 km )
- Basin countries
- United States
- Max length
- 13 mi (21 km)
- Max width
- 9.3 mi (15 km)
- Surface area
- 70 mi (180 km )
- Average depth
- 57 ft (17 m)
- Max depth
- 159 ft (48 m)
- Water volume
- 2,970,000 acre⋅ft (3.66 km )
- Surface elevation
- 6,383 ft (1,946 m) above sea level
- Islands
- Two major: Negit Island and Paoha Island ; numerous minor outcroppings (including tufa rock formations). The lake's water level is notably variable.
- References
- U.S. Geological Survey Geographic Names Information System: Mono Lake
via Wikipedia infobox
~21 min read
Encyclopedic overview
Mono Lake (/ˈmoʊnoʊ/ MOH-noh) is a saline soda lake in Mono County, California, formed at least 760,000 years ago as a terminal lake in an endorheic basin. The lack of an outlet causes high levels of salts to accumulate in the lake which make its water alkaline.
The desert lake has an unusually productive ecosystem based on brine shrimp, which thrive in its waters, and provides critical habitat for two million annual migratory birds that feed on the shrimp and alkali flies (Ephydra hians). Historically, the native Kutzadika'a people ate the alkali flies' pupae, which live in the shallow waters around the edge of the lake.
Excerpted from Wikipedia’s “Mono Lake” article, available under the CC BY-SA 4.0 licence.