Lake Tahoe Nevada
Nevada Division of State Parks - Lake Tahoe-Nevada State Park
L ake Tahoe-Nevada State Park offers a number ofdifferent areas for visitors to enjoy. Sand Harbor is the most popular, with sandy beaches, a boat launch, picnicking and group use facilities. Sand Harbor is located three miles south of Incline Village on State Route 28. Memorial Point and Hidden Beach , Situated between Incline Village and Sand Harbor, are areas which offer outstanding views of the lake and more secluded access to its shores. Spooner Lake, at the intersection of StateRoute 28 and U.S. 50, is popular for picnicking, hiking, mountain biking , catch-and-release fishing and cross-country skiing . A group use area is available as well as rentalcabins . Spooner Lake is also a trail head with access to the back country. The back country between Lake Tahoe and Carson City provides miles of hiking, equestrian and Mountain biking trails plus ... [Read More]
Nevada Division of State Lands - Nevada Tahoe Resource Team
Special vehicle license plates to benefit Lake Tahoe are available through the Department of MotorVehicles . Buyers of these plates pay special fees of $25 the first year and $20 each continuing year. These fees go into a dedicated Lake Tahoe fund, which is administered by DSL for projects and programs that will preserve or restore the natural environment of Lake Tahoe. These funds are available as grants. The submittal deadline for the 2005Lake Tahoe License Plate Grant Applications for 2005 closed on Monday, Feb. 28, 2005. Grant Application andProcedures ... [Read More]
Facts about Lake Tahoe.
Snow, rain, and streams filled the southern and lowest part of the basin, forming the ancestral Lake Tahoe. 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 and into Pyramid Lake in Nevada. ... that the depth of Lake Tahoe changes every day as the lake level changes. The deepest measurement from the 1998 bathymetric survey was 1,637 ft (499 m) deep. The depth of Lake Tahoe depends on the height it is measured from; some measurements use sea level as a base reference, others use different points of reference. The appropriate reference, or datum, for Lake Tahoe's depth is still being debated. Therefore the measured depth of a lake is only preliminary data and may change. ... [Read More]
Nevada Division of State Parks -
Parks: Dayton, Mormon State, Lake Tahoe, Washoe Lake ... *Lifeguard positions are only available at Lake Tahoe-Nevada StatePark in Carson Region. All others are available in all regions. ... Parks: Cathedral Gorge, Regional Visitor Center, Cave Lake, Echo Canyon, Kershaw Ryan, Beaver Dam, Spring Valley ... [Read More]
Lake Tahoe Change Detection
Burn area Extensive changes resulting from forest fires can be observed insatellite images. Changes in greenness, displayed here as a dark bluecolor, show an area of vegetation which has become blackened from burning. Conifer mortality Scientists at Boston University have made ground measurements toquantify the decrease in the forest canopy as a result of drought. Thesustained drought conditions weakened the trees and made them moresusceptible to insect attacks. Satellite images can be used to estimatethe geographic extent of the damaged area. Forest clear-cutting Droughts increase the geographic extent of exposed lakebeds, where newvegetation can be seen using satellite images. Changes in land use ortimber harvesting activities can also be seen in this forested area. Dry lake These images were taken at the beginning and culmination of droughtconditions in the western U.S. A broad shallow lake that was full ofwater in 1986 was empty, and the entire lake bed exposed, in 1992. ... [Read More]
Geology and Natural History of Lake Tahoe
The Tahoe Basin, like the Carson Valley, has dropped between two uplifted blocks, The Sierra crest on the west and the Carson Range on the east. This is a relatively recent development, occurring within the last several million years. Magma generated by the pressures and temperatures that also caused the faulting and uplifting welled up through gaps in the faults. A prominent area of this volcanic area occurred just north of the lake. Andesite flows from these vents bisected and dammed the valley. Eventually, as the lake rose the Truckee River was able to cut through these flows and find its present course around the volcanics to the lowlands of Nevada. Subsequent glacial (2 million to 20,000 years ago) action just downstream of the lake (from the Alpine Meadows and Squaw Valley canyons) dammed the river and so the level of the lake has fluctuated drastically over time. The maximum lake level during glaciation approached 800 feet higher than its present level. Large sedimentary terrace ... [Read More]
Nevada Division of State Parks - Lake Tahoe-Nevada State Park - Marlette-Hobart Backcountry
The trail to Marlette Lake via North Canyon Road is the easiest access into the back-country. A steeper access is available at Tunnel Creek Road. The one time millpond, Spooner Lake, now offers fishing and is surrounded by a peaceful, attractive natural area that provides opportunities for walking and nature study in the spring, summer and fall. The most sought-after trails in the backcountry are the historic Marlette Flume Trail and the Tahoe Rim Trail . ... [Read More]
Background on the Lake Tahoe Initiative.
Actions to Protect Lake Tahoe ... Prior to their visit, the Clinton Administration convened Lake Tahoe workshops on water quality, forest restoration, recreation and tourism, and transportation. From those workshops the President directed his administration to begin acting on specified recommendations. ... Background on the Lake Tahoe Initiative ... [Read More]
USGS: Pacific Sea-Floor Mapping: Lake Tahoe
The major objective of this survey was to map the bathymetry of Lake Tahoe, California-Nevada to fulfill a commitment made during the Lake Tahoe Presidential Forum in 1997. The only existing bathymetry of Lake Tahoe, collected in 1923, was recently compiled by Rowe and Stone (1997), but the data density is inadequate for the level of scientific studies ongoing and anticipated in the near future for Lake Tahoe. Recent advances in marine multibeam-sonar capabilities now permit a cost-effective way, to precisely map the bathymetry of large areas of the ocean floor with 100% coverage. This survey applied this state-of-the-art ocean technology to Lake Tahoe. The newest of these high-resolution multibeam mapping systems also simultaneously collects backscatter (similar to sidescan sonar) imagery that results in a complimentary and co-registered data set that is related to the distribution of lake-floor materials and textures. The two types of maps that resulted from this cruise provide the m ... [Read More]
US Dept of State
SR 20 [NORTHWEST CALIFORNIA] THE WESTBOUND CONNECTOR TO SOUTHBOUND US 101 /IN CALPELLA/ (MENDOCINO CO) IS CLOSED 24 HRS A DAY MONDAY THRU FRIDAY THRU 7/22/05 - DUE TO CONSTRUCTION - A DETOUR IS AVAILABLE 1-WAY CONTROLLED TRAFFIC AT VARIOUS LOCATIONS FROM 5.1 MI WEST OF THEMENDOCINO/LAKE CO LINE TO THE MENDOCINO/LAKE CO LINE FROM 0700 HRS TO 1900 HRS MONDAY THRU FRIDAY THRU 7/22/05 - DUE TO CONSTRUCTION - MOTORISTSARE SUBJECT TO 15 MINUTE DELAYS [NORTH CENTRAL CALIFORNIA & SIERRA NEVADA] 1-WAY CONTROLLED TRAFFIC AT VARIOUS LOCATIONS FROM BUTTE VISTA WY TOMOON BEND RD /IN COLUSA/ (COLUSA CO) FROM 0600 HRS TO 1500 HRS MONDAY THRUFRIDAY THRU 7/22/05 - DUE TO CONSTRUCTION - MOTORISTS ARE SUBJECT TO 20 MINUTE DELAYSSR 28 [NORTH CENTRAL CALIFORNIA & LAKE TAHOE BASIN] NO TRAFFIC RESTRICTIONS ARE REPORTED FOR THIS ROUTE.US 50 [IN THE SACRAMENTO VALLEY & THE LAKE TAHOE BASIN] THE WESTBOUND CONNECTOR TO EASTBOUND & WESTBOUND I 80 /IN WEST SACRAMENTO/ (YOLO CO) IS CLOSED FROM 2000 HRS EACH NIGHT T ... [Read More]
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