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Mono Lake | Tufa columns

WI_ca145.jpg

The saline Mono Lake occupies the bottom of an endorheic basin of tectonic origin, located directly east of the Sierra Nevada. The lake is characterized by a high biological diversity, and by limestone formations known as tufa columns.

Location
View on OpenStreetMap
Created
on Saturday 20 September 2003 by Martin Mergili
Visits and license
2665 visits, CC BY-NC-SA 4.0 DEED license