Buffalo Valley Hot Springs
Buffalo Valley Hot Springs flows at 174°F on Bureau of Land Management public lands in Lander County at 4,626 feet elevation, requiring a 554-meter walk from the nearest road. Recent USGS analysis documented water with pH 6.8, sodium content of 300 mg/L, and sulfate levels of 83 mg/L, reflecting deep geothermal circulation through Nevada's basin-range aquifers.
The spring emerges in valley-floor terrain where sagebrush flats receive 9.9 inches of precipitation and 24.8 inches of snow annually. At mid-elevation in the Buffalo Valley drainage, alluvial sediments and volcanic bedrock underlie vegetation communities dominated by big sagebrush and greasewood. The Mount Lewis Field Office manages surrounding public lands for multiple uses.
Buffalo Valley Hot Springs takes its name from the valley itself, historically grazed by cattle operations through the 19th and 20th centuries. Specific documentation of early use remains limited. The thermal feature continues to flow on unrestricted BLM lands accessible to the public.
Visit spring through fall when valley roads remain passable; winter snow and mud can close access routes. The half-kilometer walk crosses sagebrush terrain; wear sturdy boots. Water at 174°F requires substantial cooling before bathing is possible—bring containers and plan accordingly. No facilities exist; pack out all waste. High-clearance vehicles recommended for the final approach to trailhead parking.
Is Buffalo Valley Hot Springs worth visiting?
Best for
- Observing powerful hot springs
Not ideal for
- Casual soaking
The water at Buffalo Valley Hot Springs is neutral (pH 6.8). It is notably rich in sodium (supports circulation and skin hydration).