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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
IThe 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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