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Lake Tahoe at a Glance

  • Lake Tahoe is one of the clearest and most beautiful large sub-alpine lakes in the world.
  • It has a relatively small watershed (800 square kilometers, including the lake) for the size of the lake surface (500 square kilometers).
  • Lake Tahoe formed about 2 million years ago due to plate tectonics and a volcanic dam at its north end. It lies at an elevation of 6,225 feet.
  • At 1,657 feet, Lake Tahoe is the 11th deepest lake in the world. The average depth is 1,027 feet. It is 23 miles long at it´s longest and 12 miles wide at it´s widest.
  • 63 streams feed into Lake Tahoe; only one flows out of it – the Truckee River.
  • The lake was naturally clear before European-American settlement, because its watershed filtered contaminants such as sediments and nutrients before they entered the lake.
  • The lake was known only to the Washoe Indians until General John Charles Fremont discovered it in 1844.
  • Between 1870 and 1900, the forests of the basin were heavily logged for use in mine shafts at the Comstock Silver Lode. Today the forest is only 5 percent old-growth.
  • Urbanization of the basin has eliminated 75 percent of its marshes, 50 percent of its meadows, and 35 percent of its stream zone habitats.
  • In 2000, government census numbers showed that the residential or year-round population at Lake Tahoe was 62,891 people.
  • Millions of visitors come to Lake Tahoe, with 23 million visitor-days per year.
  • The primary cause for the loss in water clarity is fine particles from both natural and human caused erosion.
  • The growth of algae has increased about four-fold since measurements were first taken in the lake 1950´s. The lake is losing an average of over one foot of clarity each year.
  • The three main sources of new nutrients entering Lake Tahoe are streams, groundwater, and direct atmospheric deposition onto the lake surface.