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Summer and Winter Playground |
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Lake Tahoe
is a beautiful, crystal-clear blue lake nestled among mountain
peaks of California and Nevada. Here you'll find unparalleled
panoramic beauty with an abundant choice of recreation for every
season.
In the summer, enjoy hiking, biking, rafting,
fishing, sailing, golf, horseback riding, tennis, hot air ballooning,
parasailing, boating, and much more. It's for these reasons,
Lake Tahoe is often called America's All Year Playground.
Located at 6,225 feet above sea level, magnificent Lake Tahoe
is a paradise for outdoor lovers. In the winter, Lake Tahoe
is home to the highest concentration of world class ski resorts!
There is enough variety that every winter sport enthusiast
will find their home at one of the many ski resorts in Lake
Tahoe.
You won't find a more exciting and versatile vacation destination
area anywhere. But don't just take our word for it, come see
for yourself -- any time of the year. |
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Did You Know? |
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Lake
Tahoe is the highest lake of its size in the United States
and the largest alpine lake in North America. |
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Lake Tahoe is
as long as the English Channel is wide with the width of
Tahoe being half again as wide as San Francisco Bay. |
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With one dispersion
of Lake Tahoe's water, the State of California would be
completely covered to a depth of 14.5 inches. |
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The Panama Canal (700 feet in width
and 50 feet in depth) could be filled by Lake Tahoe's water
and extend completely around the earth at the equator, with
enough remaining in the lake to fill another channel of the
same width and depth running from San Francisco to New York. |
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An average 1,400,000 tons of water evaporates
from the surface of Lake Tahoe every 24 hours, yet this drops
the lake level only one-tenth of an inch. |
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If the water
that evaporates from the lake every 24 hours could be recovered,
it would supply the daily requirements of a population
of 3,500,000 people. |
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Lake Tahoe's
water is 99.9% pure. The water is so clear that a 10 inch
white dinner plate would be visible at 75 feet below the
surface. |
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There are 63
tributaries draining into Lake Tahoe with only one outlet
at the Truckee River. |
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Lake Tahoe never
freezes due to the constant mass movement of water from
the bottom to the surface. In February 1989, Emerald Bay
froze over for the first time since 1952. |
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Lake Facts and Statistics |
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Maximum Elevation: 6,229
feet |
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Length: 22
miles |
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Width: 12
miles |
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Maximum
Depth: 1,645
feet |
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Average
Depth: 989 feet |
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Shoreline: 72
miles |
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Surface
Area: 193 sq.
mi. or 122,200 acres |
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Volume: 39
trillion gallons or 122 million acre feet of water |
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Surface
Water Temperatures: Maximum
- 68 degrees F, Minimum - 41 degrees |
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Temperatures
at 200 feet: Maximum
- 47 degrees, F Minimum - 41 degrees F |
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Population: South
Lake Tahoe, including the Stateline area, has a permanent,
year-round population of 34,000. |
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Sunshine: The
sun shines at Lake Tahoe during 75% of the year, or 274
days. |
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Snowfall: At
lake level, annual snowfall averages 125 inches. At alpine
skiing elevations, the snowfall averages 300 to 500 inches
each year. |
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Gaming: There
are six 24-hour casinos in the South Lake Tahoe area. Together,
they have a total of 7,051 slot machines and 411 game tables. |
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Skiing: Skiers
can hit the slopes on one of the 182 ski trails in the
midst of more than 8,800 total ski resort acres. The longest
ski run in the area is 5.5 miles long. Lake Tahoe's greatest
vertical drop is 3,600 feet. Both runs are at Heavenly. |
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Fishing: The
biggest fish ever caught in Lake Tahoe, a Mackinaw lake
trout, weighed 37 pounds and 6 ounces. |
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Famous
Residents: Famous
neighbors include and have included Charles Bronson,
Cher, Natalie Cole, Sammy Davis Jr., Liza Minelli, Wayne
Newton and the Captain and Tennile. |
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Movies
Filmed at Lake Tahoe
The first
movie filmed at the lake was a 1920's musical
short (sort of an early version of a music
video) starring Jeanette MacDonald singing "Indian
Love Call." In 1974, Francis Ford Coppola
shot sections of his Oscar-winning "The
Godfather, Part II" (1974) here. Director
Renny Harlin and star Bruce Willis came here
in 1989 to film the snowmobile- borne, machine-gun
battle in "Die Hard II: Die Harder." Nearby
Fallen Leaf Lake served as a major setting
for the hit "The Bodyguard" (1992),
which starred Kevin Costner and Whitney Houston.
And Oscar winner Tommy Lee Jones starred in
the Ty Cobb biopic, "Cobb" (1994),
which used the Tahoe area for some locations. "City
of Angels" (1997) with Meg Ryan and Nicholas
Cage was flimed with the High Sierras of Lake
Tahoe as the backdrop. And most recently, the
film "Smokin' Aces" was filmed in
October 2005 at the Horizon and MontBleu Casinos,
starring Ben Affleck, Ray Liotta, Jeremy Piven,
Taraji Henson and Alicia Keys. |
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Water Sports |
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During the summer,
the lake is popular for water sports and beach activities. The
two cities most identified with the Lake Tahoe tourist area are
South Lake Tahoe, California and the smaller Stateline, Nevada;
smaller centers on the northern shoreline include Tahoe City
and Kings Beach.
Boating, the primary activity in Tahoe
in the summer, is known worldwide. There are lakefront restaurants
all over the Lake, most equipped with docks and buoys. There
are all sorts of boating events, such as sailboat racing, firework
shows over the lake, guided cruises, and more. Lake Tahoe also
has its own Coast Guard. |
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Hiking and Mountain Biking |
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There are hundreds of hiking/mountain biking
trails all around the lake. They range in size, length, difficulty,
and popularity. One of the most famous of Tahoe's trails is the
Tahoe Rim Trail, a 165 mile trail that circumnavigates the lake. |
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Gambling |
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Gambling is legal on the Nevada side of the
lake, the resort area of Lake Tahoe attracts all kinds of fun seekers,
year round. In the town of Stateline, near Heavenly Mountain Resort,
there are myriads of enormous casinos filled all year long. |
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Geography |
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Lake Tahoe is a freshwater
lake in the Sierra Nevada, on the border between the U.S. states
of California and Nevada, near Carson City. Approximately two-thirds
of the shoreline is in California. The area is home to a number
of ski resorts
Lake Tahoe is one of the deepest (1645
feet/501 m), largest (192 sq. mi./497 km²) ¹,
and highest (6229 feet/1898 m) lakes in the United States.
Only Oregon's Crater Lake is deeper at 1930 feet (588 m).
Although for much of Tahoe's perimeter, highways
run within sight of the lake shore, some important parts of the
California shoreline now lie within state parks or are protected
by the United States Forest Service. Lake Tahoe is about 22 mi
(35 km) long and 12 mi (19 km) wide and has 72 mi (116 km)
of shoreline and a surface area of 191 square miles or 495 square
kilometers.
The Lake Tahoe Basin was formed by geologic
block (normal) faulting about 2 to 3 million years ago. A geologic
block fault is a fracture in the Earth's crust causing blocks
of land to move up or down. Uplifted blocks created the Carson
Range on the east and the Sierra Nevada on the west. Down-dropped
blocks created the Lake Tahoe Basin in between. Some of the highest
peaks of the Lake Tahoe Basin that formed during this process
were Freel Peak at 10,891 ft (3320 m), Monument Peak at
10,067 ft (3068 m) (the present Heavenly Valley Ski Area),
Pyramid Peak at 9,983 ft (3043 m) (in the Desolation Wilderness),
and Mount Tallac at 9,735 ft (2967 m).
Snowmelt filled the southern and lowest part
of the basin, forming the ancestral Lake Tahoe, with rain and
runoff adding additional water. Modern Lake Tahoe was shaped
and landscaped by the scouring glaciers during the Ice Age (the
Great Ice Age began a million or more years ago). Many streams
flow into Lake Tahoe, but the lake is drained only by the Truckee
River, which flows northeast through Reno, Nevada and into Pyramid
Lake in Nevada.
Mean annual precipitation ranges from over
55 inches/year or 140 cm in watersheds on the west side
of the basin to about 26 inches/year or 67 cm near the lake
on the east side of the basin. Most of the precipitation falls
as snow between November and April, although rainstorms combined
with rapid snowmelt account for the largest floods. There is
a pronounced annual runoff of snowmelt in late spring and early
summer, the timing of which varies from year to year. In some
years, summertime monsoonal storms from the Great Basin bring
intense rainfall, especially to high elevations on the east side
of the basin. As the climate in the northern Sierra warms, hydrologists
anticipate that an increasing fraction of the precipitation in
basin will fall as rain rather than snow.
Vegetation in the basin is dominated by a
mixed conifer forest of Jeffrey pine (P. Jeffreyi),
lodgepole pine (P. murrayana), white fir (Abies
concolor), and red fir (A. magnifica). The basin
also contains significant areas of wet meadows and riparian areas,
dry meadows, brush fields (with Arctostaphylos and Ceanothus)
and rock outcrop areas, especially at higher elevations. Ceanothus is
capable of fixing nitrogen, but mountain alder (Alnus tenuifolia),
which grows along many of the basin’s streams, springs
and seeps, fixes far greater quantities, and contributes measurably
to nitrate-N concentrations in some small streams.
Soils of the basin are derived primarily
from andesitic volcanic rocks and granodiorite, with minor areas
of metamorphic rock. Some of the valley bottoms and lower hillslopes
are mantled with glacial moraines, or glacial outwash material
derived from the parent rock. Cryopsamments, Cryumbrepts, rockland,
rock outcrops and rubble and stoney colluvium account for over
70% of the land area in the basin (see USA soil taxonomy). The
basin soils (in the < 2 mm fraction) are generally 65-85%
sand (0.05–2.0 mm).
The south shore is dominated by the lake's
largest city, South Lake Tahoe, California, which neighbors Stateline,
Nevada. Tahoe City, California is located on the lake's northwest
shore. |
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History |
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Tahoe’s history
began 2–3 million years ago when the faults that created
the Carson Range simultaneously molded the Tahoe Basin. Eruptions
from the extinct volcano Mt. Pluto formed a dam on the north
side. The Pleistocene (Ice Age) molded the basin to its current
form followed by drainage from ice and snow which filled the
lake.
The area around Lake Tahoe was originally
inhabited by the Washoe tribe of Native Americans. Lake Tahoe
was the center and heart of Washoe Indian territory, including
the upper valleys of the Walker, Carson, and Truckee Rivers.
They called this area "Da ow a ga", which means "edge
of lake". When early pioneers came they mispronounced
this word, saying "Da ow", it later evolved into
what we call it today, Lake "Tahoe".. Lt. John
C. Frémont and Kit Carson were the first non-indigenous
people to see Lake Tahoe. It was Fremont's 2nd exploratory
expedition. On February 14, 1844, while searching for the Bonaventura
river he first sighted the lake from Red Lake Peak in what
is now the Carson Pass. After arriving at Sutter's Fort he
designated it Lake Bonpland, in honor of the French explorer
and botanist Aimé Jacques Alexandre Bonpland. John Calhoun
Johnson, Sierra explorer and founder of "Johnson's Cutoff" (now
Hwy 50), was the first white-man to see Meeks Bay and from
a peak above the lake he named "Fallen Leaf Lake, California" after
his Indian guide. His first employment in the west was in the
government service, carrying the mail on snowshoes from Placerville
to Nevada City, during which time he gave the name of Lake
Bigler to that beautiful body of water now known as Lake Tahoe
in honor of California’s governor John Bigler. In 1853
William Eddy, the surveyor general of California, identified
Tahoe as Lake Bigler. In 1862 the U.S. department of interior
first introduced the name Tahoe which continued a debate about
naming the lake, in which both names were used until well into
the next decade. It wasn’t until 1945 that it was finally
and officially named Lake Tahoe. The compromise to partition
Tahoe with 2/3 to California and 1/3 to Nevada was reached
when California became a state. Putting the state line right
through the middle of the lake and then at 39 degrees north
latitude, the stateline obliques southeasterly towards the
Colorado River. Upon discovery of gold in the South Fork of
the American River in 1848, thousands of west-bound gold seekers
passed near the basin on their way to the gold fields. European
civilization first made its mark in the Lake Tahoe basin with
the 1858 discovery of the Comstock Lode, a silver deposit just
15 miles (24 km) to the east in Virginia City, Nevada. From
1858 until about 1890, logging in the basin supplied large
timbers to shore up the underground workings of the Comstock
mines. The logging was so extensive that almost all of the
native forest was cut. In 1864, Tahoe City was founded as a
resort community for Virginia City, the first recognition of
the basin’s potential as a destination resort area.
Public appreciation of the Tahoe basin grew, and during the
1912, 1913, and 1918 Congressional sessions, unsuccessful efforts
were made to designate the basin as a national park. During
the first half of this century, development around the lake
consisted of a few vacation homes. The post-World War II population
and building boom, followed by construction of gambling casinos
in the Nevada part of the basin during the mid-1950’s,
and completion of the interstate highway links for the 1960
Squaw Valley Olympics, resulted in a dramatic increase in development
within the basin. From 1960 to 1980, the permanent resident
population increased from about 10,000 to greater than 50,000,
and the summer population grew from about 10,000 to about 90,000.
Since the 1980s, development has slowed somewhat due to land
use controls. |
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