Sierra Shores Rentals Lake Tahoe
LAKE TAHOE
TOLL FREE 800-988-8260
  SUMMER AND WINTER PLAYGROUND  
 

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.

 
     
  DID YOU KNOW?  
 
Lake Tahoe is the highest lake of its size in the United States and the largest alpine lake in North America.
 
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.
 
With one dispersion of Lake Tahoe's water, the State of California would be completely covered to a depth of 14.5 inches.
 
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.
 
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.
 
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.
 
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.
 
There are 63 tributaries draining into Lake Tahoe with only one outlet at the Truckee River.
 
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.
 
 
     
  LAKE FACTS AND STATISTICS  
 
 
Maximum Elevation: 6,229 feet
 
Length: 22 miles
 
Width: 12 miles
 
Maximum Depth: 1,645 feet
 
Average Depth: 989 feet
 
Shoreline: 72 miles
 
Surface Area: 193 sq. mi. or 122,200 acres
 
Volume: 39 trillion gallons or  122 million acre feet of water
 
Surface Water Temperatures: Maximum - 68 degrees F, Minimum - 41 degrees
 

Temperatures at 200 feet: Maximum - 47 degrees, F Minimum - 41 degrees F
 
Population: South Lake Tahoe, including the Stateline area, has a permanent, year-round population of 34,000.
 
Sunshine: The sun shines at Lake Tahoe during 75% of the year, or 274 days.
 
Snowfall: At lake level, annual snowfall averages 125 inches. At alpine skiing elevations, the snowfall averages 300 to 500 inches each year.
 
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.
 
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.
 
Fishing: The biggest fish ever caught in Lake Tahoe, a Mackinaw lake trout, weighed 37 pounds and 6 ounces.
 
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.
 
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.
   
 
     
  WATER SPORTS  
 

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.

 
     
  HIKING AND MOUNTAIN BIKING  
  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.  
     
  GAMBLING  
  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.  
     
GEOGRAPHY  
 

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.

 
     
  HISTORY  
 

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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Sierra Shores 3371 Lake Tahoe Blvd, South Lake Tahoe, CA - (530) 541-9360
 
 
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