White crusts of natural salts along a tributary to Muddy Creek, WY
Detailed Description
White crusts of natural salts along a tributary to Muddy Creek, Wyoming. Natural salts are present in soils from drier climates, and rain and snowmelt can percolate into the soil and carry the salts to streams.
Sources/Usage
Public Domain.
Related
Soil Disturbance Can Increase Stream Salinity in Semiarid Watersheds
Soil disturbance from construction of roads, pipelines, and well pads on naturally salt-rich soils was determined to be a potential factor resulting in increased salinity in a southern Wyoming stream. Construction can expose salt-rich soils in the subsurface to increased contact with rain and snow, thus mobilizing salts through runoff or water percolating into soils.
Related
Soil Disturbance Can Increase Stream Salinity in Semiarid Watersheds
Soil disturbance from construction of roads, pipelines, and well pads on naturally salt-rich soils was determined to be a potential factor resulting in increased salinity in a southern Wyoming stream. Construction can expose salt-rich soils in the subsurface to increased contact with rain and snow, thus mobilizing salts through runoff or water percolating into soils.