June Lake | |
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Census designated place | |
Town of June Lake
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Location in California | |
Coordinates: 37°46′47″N 119°04′32″W / 37.77972°N 119.07556°WCoordinates: 37°46′47″N 119°04′32″W / 37.77972°N 119.07556°W | |
Country | United States |
State | California |
County | Mono |
Area | |
• Total | 8.779 sq mi (22.737 km2) |
• Land | 7.988 sq mi (20.689 km2) |
• Water | 0.791 sq mi (2.048 km2) 9.01% |
Elevation | 7,654 ft (2,333 m) |
Population (April 1, 2010) | |
• Total | 629 |
• Density | 72/sq mi (28/km2) |
Time zone | Pacific (UTC-8) |
• Summer (DST) | PDT (UTC-7) |
ZIP code | 93529 |
Area codes | 442/760 |
GNIS feature IDs | 1658875, 2583044 |
U.S. Geological Survey Geographic Names Information System: June Lake, California; U.S. Geological Survey Geographic Names Information System: June Lake, California |
June Lake is a census-designated place in Mono County, California. It is located against the southern rim of the Mono Basin, 12.5 miles (20 km) south of Lee Vining, at an elevation of 7654 feet (2333 m).
The majority of the developed community is spread narrowly along a five-mile stretch of California State Route 158., which is also known as the June Lake Loop Road, or in the populated areas, Boulder Drive. The Mono County Community Development Department defines June Lake's planning area to encompass the entire June Lake Loop, including the section of U.S. Route 395 between the north and south junctions of the Loop Road.
The population was 629 at the 2010 census. In the Summer that can grow by 2500 visitors: fisherman, campers, tourists, backpackers and outdoors enthusiasts. The ZIP Code is 93529.
The June Lake Loop is situated against the west rim of the Great Basin and Range Province, abutting the steep eastern escarpment of the Sierra Nevada. Rush Creek originates from an alpine watershed just north of the headwaters of the San Joaquin River, and south of the Tuolumne River, then flows northeast, becoming the major tributary to the great inland sea, Mono Lake.
June Lake's looped valley, often described as a horseshoe-shaped canyon, was formed by glacial action. The Rush Creek glacier split in two when it encountered the resistant rock of what is now known as Reversed Peak. The main glacier flowed toward the north creating the Rush Creek Canyon. Another glacial branch turned south and east but its flow was impeded and eventually stopped as the granitic bedrock on this southern branch created an uphill path toward the volcanic area of the Mono Craters. When the glacier receded it left behind terminal moraine material in the area now known as Oh! Ridge.