Frequently Asked Questions about Lake Tahoe and the Basin
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Tahoe is 22 miles long, North to South, and 12 miles wide, with 72 miles of shoreline.
The best estimate is that Lake Tahoe itself formed about two million years ago, and has been roughly the size we see today
for the last million years. The forest landscape surrounding the lake developed over the last 10,000 years.
Lake levels and depth vary only slightly today. The deepest recorded depth of Lake Tahoe is 1,645 feet. To visualize this
depth, imagine the bottom of Tahoe reaching down 100 feet lower than Carson City, Nevada, sitting in the basin far below Tahoe
to the east.
What we see as "normal" Lake Tahoe depth is only our perspective. Over its history, the lake level has been much
lower or much higher than today. We can see clear evidence of lower lake levels in the past lasting hundreds of years. Many
locations around the lake have submerged mature tree stumps twenty feet below current lake levels. By examining and dating
the tree rings of these underwater stumps, we can see that shoreline forests have repeatedly been drowned by ups and downs in
the historic lake levels of Tahoe.
No, but Tahoe is among the deepest. The maximum-recorded depth of Tahoe is 1,645 ft. or 501 meters. In North America, two
other lakes are deeper than Tahoe; one is Crater Lake in Oregon at 1,945 feet or 593 meters in depth. In Canada, Great Slave
Lake is 2,015 ft. or 614 meters in depth.
The deepest, largest and oldest of all lakes is Lake Baikal in Siberia, at 5,400
ft. or 1,637 meters in depth. Lake Baikal at 25 million years old is the largest fresh water lake, containing over 20% of
all surface fresh water on Earth.
Although Tahoe is not the largest, deepest or oldest, it is one of the clearest and most
beautiful lakes in the world, and is regarded as the Jewel of the Sierra.
Lake Tahoe contains an average of 37 trillion gallons of water. That's hard to imagine, but
it is enough water to cover a flat
surface, the size of California with 14 inches of water. If you did ever manage to drain Tahoe, it would take around 700
years to fill back up again.
The basin formed at least two million years before the lake. Many people think Tahoe was formed by giant glaciers; however
glaciers came along too late to form the massive Tahoe Basin. Others have heard it was once a huge volcano.
Volcanoes did not form the basin, but like glaciers, volcanic activity played a part in the formation of the Tahoe Basin.
Around five million years ago a very active period of mountain building took place. Large blocks or plates were pushed up forming
the crest of the Sierra Nevada. Where the basin is today, two parallel blocks pushed up, one on the west, another to the
east. Between these, another smaller block slipped down. This created a very deep and steep sided valley basin, open to
The open north end allowed snowmelt to flow out of the basin, and then through valleys towards the east and down
to the Great Basin. The "valley basin" changed into a "lake basin" some two million years ago when several large volcanic
eruptions occurred. One of these, called Mount Pluto, poured lava and volcanic mudflows into the northern outlet of the
basin, blocking it up. Over time, snowmelt and rain filled the basin, creating one of America's most famous and beautiful
Glaciers would later help shape some areas of the western slopes on the California side, with the most notable
traces being Emerald Bay and Fallen Leaf Lake. We can also see traces of the volcanic period in the form of volcanic
"plugs." These are the hard solidified cores now exposed by erosion. Cave Rock and Shakespeare Point along the
shore are examples, easily seen today along Highway 50.
Not as old as many think. Although the lake is well over a million years old, and the basin around it five million years
old, the forests are much younger. Ten thousand years ago the climate was colder and drier, and much of the plant life in
the basin was a type of sagebrush. Conifers or "evergreens" such as types of junipers and single-leaf pines quickly colonized
the basin as the climate became warmer and wetter. The large stands of conifers we know today became well established around
seven thousand years ago.
Archeologists believe that the first people came to the lake at least 9,000 years ago, seasonally at first. Later,
semi-permanent communities developed. The Washoe Tribe of Nevada and California will tell you that it cannot be said when
the first people came to the lake, as the Washoe have always been at Tahoe.
The origin of the name "Tahoe" has some controversy, however it is probably on the Washoe Tribe's term
"Da ow ga" or
simply "the lake." Early Euro-Americans heard the Washoe pronunciation, and the variation
"Tahoe" was soon applied.
Sixty-three streams flow into Lake Tahoe, but only one, the Truckee River, flows out past Reno and into Pyramid Lake.
Unlike most bodies of water in North America, Lake Tahoe's water never flows into the ocean. Lake Tahoe also loses much of
its water to evaporation; if the water that evaporates from the lake every 24 hours could be recovered, it would supply the
daily requirements of a city the size of Los Angeles.
No. Partly this is due to its size, but also to the action of energy. The great volume of water is constantly in a slow
rolling motion, generated largely by the energy of sunlight. The waters of Tahoe are like a giant battery, absorbing and
holding heat from solar energy during the day, and radiating it off at night. This causes water to circulate in flowing
currents known as convections, preventing the lake from freezing.
The upper surface of the lake can store an amazing amount of solar energy. Deep in winter, it is not unusual for the
morning air temperature at lake level to be noticeably warmer than the air in Carson City over 1,500 feet lower. The solar
energy stored up by the lake is radiated off at night.
Tahoe is one of the world's clearest lakes. You can credit geology with much of the answer. The lake formed in a basin
high in the Sierra, around 6,225 feet at lake level. On average the elevation and average temperatures help inhibit the
growth of algae, which gives most other lakes a greenish look. The steep geology and soil types forming the basin around
the lake have developed into a natural filtering watershed system. Decomposed granite soil absorbs water, and helps
filter out materials and sediments that would otherwise cloud the water. Over 10,000 years, plants and soils locked up
much of the phosphorus and nitrogen, and stream banks stabilized into a delicate but highly effective watershed, creating
famously clear lake waters.
In the 1860s, lake waters were so clear, that objects 100 feet below the surface could clearly be seen. Over recent
decades, there has been a 25% reduction in clarity in Lake Tahoe. Until recently, the pace of unregulated or unplanned
development actions blocked or damaged the watershed and increased or concentrated erosion. This disturbance altered the
natural filtering ability of the basin, allowing phosphorus and nitrogen to wash out of soils and feed algae. Silts and
air pollution have also been factors. Maintaining and restoring the delicate watershed is a major effort of Forest Service
activities in the Lake Tahoe Basin Management Unit (LTBMU). Other federal, state and local actions are reducing erosion and runoff, designed to halt and
reverse the trend.
Primarily the US Forest Service, Lake Tahoe Basin Management Unit (LTBMU) is responsible for the conservation,
preservation and restoration of the Lake Tahoe watershed ecosystem within National Forest Lands. Projects and programs
also include habitat, fire management, and urban lot management. Additionally the LTBMU provides and maintains high quality
recreational opportunities for millions of visitors and residents annually.
Compared to other National Forest Lands the LTBMU is small, yet it is the Tahoe Basin's largest land manager, responsible
for 78% of basin lands. As such the Forest Service has the largest single role in ecosystem and watershed management and
protection. The LTBMU is a part of National Forest System Lands, yet is managed somewhat differently than other National
Forests. Many common forest activities such as mining, grazing or timber harvesting are either not a part of LTBMU management
or play a very small role. Since the lake is so dependent on all that happens around it, LTBMU programs manage the whole of
the basin as a complete inter-dependent system.
The LTBMU is a unique inter-mix of forest and urban communities, presenting challenges and complexities few other National
Forests experience. Since its establishment in 1973, the LTBMU has become a pioneer and leader in the science of forest and
ecosystem management. The work of the Forest Service supports and is supported by many partners. Other federal, state
and local agencies are working together in the effort to face challenges, conserve and restore natural and cultural
resources, and enhance the recreational values of the Lake Tahoe Basin.
The story started in 1899 when President McKinley created the Lake Tahoe Forest Reserve becoming the core of later National
Forest Lands in the Tahoe Basin. Three separate forests were developed out of the reserve, the Tahoe, Eldorado and Toiyabe
National Forests. Each of these forests extended into the basin and managed separate sections.
In 1973, the LTBMU was created from basin portions of the three existing National Forests, forming a single
unit." This unification provided the focus needed for the basin, and more effective management of
its watershed and ecological
and recreational resources. The name "Lake Tahoe Basin Management Unit" was originally a temporary
one, but after three decades, the name remains.
Established in 1905, the Forest Service is an agency of the U.S. Department of Agriculture. The Forest Service manages
public lands in national forests and grasslands. Gifford Pinchot, the first Chief of the Forest Service, summed up the
mission of the Forest Service - "to provide the greatest amount of good for the greatest amount of people in the long run."
National forests and grasslands encompass 191 million acres (77.3 million hectares) of land, which is an area equivalent to
the size of Texas.