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Stansbury's 1852 map of the Great Salt Lake and adjacent country in the Utah Territory. There are several maps dating back to 1575 that show the Great Salt Lake at the correct latitude and longitude, within an accuracy of a few degrees. [citation needed] One example is a map by Nicolas Sanson dated 1650. [8]
On July 3, the lake's average daily surface water elevation was measured as 4,190.1 feet at the U.S. Geological Survey gauge at Saltair Boat Harbor on the southern end of the lake. Last year, on
The Dugway Range is a 13-mile (21 km) long [1] mountain range located in central-south Tooele County, Utah, on the Juab County north border.. The Dugway Range extends northwesterly into the south of the Great Salt Lake Desert, the region at the west and southwest of the Great Salt Lake, about three times its area, a region of a flat white, salt flat, flat alluvial plains, and some alluvial ...
Google Maps' satellite view is a "top-down" or bird's-eye view; most of the high-resolution imagery of cities is aerial photography taken from aircraft flying at 800 to 1,500 feet (240 to 460 m), while most other imagery is from satellites. [5]
Some areas of the Wasatch Range in the path of the lake-effect receive up to 500 inches (12,700 mm) per year. This micro climate of enhanced snowfall from the Great Salt Lake spans the entire proximity of the lake. The cottonwood canyons adjacent to Salt Lake City are located in the right position to receive more precipitation from the lake. [8]
The Promontory Mountains are a block fault range typical of the Basin and Range Province.The west side of the range is bounded by the East Great Salt Lake normal fault which passes under the lake along the west side of Antelope Island and on to the south shore of the lake to the west side of the Oquirrh Mountains where it continues on strike as the Oquirrh Fault.
Deseret Peak is the highest peak in the Stansbury Mountains with an elevation of 11,035 ft. It is located in the Deseret Peak Wilderness area west of Grantsville, Utah and east of Skull Valley Indian Reservation. It is the fourth most topographically prominent peak in the state of Utah. [4]
As a result, the elevation of the Bonneville shoreline is 243 ft (74 m) higher in the Lakeside Mountains, elevation 5,335 ft (1,626 m), west of the Great Salt Lake near the center of the Lake Bonneville water load, than at Red Rock Pass, 5,092 ft (1,552 m), where the lake was very shallow. [31]