How Was The Lake Formed?

Several geological incidents millions of year ago resulted in the famous blue and green waters of Lake Tahoe.

The Lake Tahoe Basin was formed by faulting (fractures in the earth’s crust allowing blocks of land to rise and sink) occurring over several million years. A fault on the eastern margin created the Carson Range, while the Sierra Nevada rose out of a shallow sea on the western side.

From the “up-thrown” fault blocks rose to the highest peaks in the Tahoe Basin. A lake formed near the southern and lowest part of the basin, fed by snow, rain and rivers. The lake rose until it found an outlet near the present town of Truckee.

Several active volcanoes poured lava into the basin, eventually damming the outlet, and then the waters rose again, several hundred feet higher than the present level. A new outlet was cut, east of Mount Pluto (the present location of Northstar). Rivers of ice followed the V-shaped stream canyons, carving them, as they moved downward, to smooth U-shaped valleys.

Why is the water so clear?

The Tahoe Basin is mostly granite, with little topsoil, and therefore few nutrients have washed into the lake to promote the growth of algae and other organisms that make water murky.

As well, 40 percent of the precipitation falling into the Lake Tahoe Basin, lands directly on the lake. The remaining precipitation drains through the decomposed granitic soils found in marshes and meadows, creating a good filtering system for water.

The colors of Lake Tahoe vary according to the water’s depth. The bluer the water, the deeper it is. The more shallow the water, the greener the color becomes.

Where does the water go?

The Truckee River is Tahoe’s only outlet and flows from the dam in Tahoe City east through Reno and eventually drains into Pyramid Lake in the Nevada desert. From there, it evaporates back into the atmosphere.

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