Fish Lake Valley
| Fish Lake Valley | |
| Valley | |
| Country | United States |
|---|---|
| States | Nevada, California |
| Region | Fish Lake-Soda Spring Watershed |
| Districts | Esmeralda County NV, Inyo County, CA |
| Borders on | White Mountains-W, SW & S Silver Peak Range-E & SE Monte Cristo Range-NE Nev Rte 773 & Excelsior Mountains-NW |
| Cities | Dyer, NV, Coaldale, NV |
| Coordinates | 37°41′40.88″N 118°04′41.91″W / 37.6946889°N 118.0783083°WCoordinates: 37°41′40.88″N 118°04′41.91″W / 37.6946889°N 118.0783083°W |
| Lowest point | Fish Lake Marsh |
| - location | Fish Lake Valley |
| - elevation | 4,400 ft (1,341 m) |
| Length | 25 mi (40 km), SSW-NNE |
| Width | 8 mi (13 km), (variable width) |
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The Fish Lake Valley is a 25 mi (40 km) longendorheic valley in southwest Nevada, one of many contiguous inward-draining basins collectively called the Great Basin. The alluvial valley lies just northwest of Death Valley and borders the southeast, and central-northeast flank of the massif of the White Mountains of California. The valley's southern end lies in eastern Inyo County, California. The valley is sparsely populated with ranchers and indigenous Paiute. Business services are located in the valley's only town Dyer.
Fish Lake Valley is a slightly southwest-northeast trending valley, in its northern and central section. It borders the White Mountains on the southwest and receives water from Cottonwood Creek and other small, permanent mountain streams. The extension of the mountains southeasterly provides a feeder valley with some small dry lakes and salt pans. The major section of the valley contains a borax mixed salt pan for 10 mi of the valley. A small dry lake is in the center, approximately 1.5 mi long. It is fed from the White Mountains, and the small subvalley southeastwards. Alluvial fans are west of the dry lake, with Nevada State Route 264 in the hills to the northwest that also feed southeast and eastwards. To the east and southeast, the Silver Peak Range borders the valley with no alluvial fans, and is the smaller massif probably block faulted from the White Mountains, and thru block faulting creating the smaller feeder valley on the White Mountains' southeast, (the Furnace Creek Fault Zone).
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