noun a geological feature characterized by a steep, downslope face
In civil engineering, slip faces can refer to the slope failure on embankments or cut slopes, where the soil or rock mass moves downslope due to gravity.
In geology, a slip face refers to the steeply inclined surface of a sand dune or other aeolian landform, formed by the movement of grains of sand.
In meteorology, slip faces can be associated with dust storms or sandstorms, where the wind erodes the surface of a dune or landform to create a steep slip face.
In geomorphology, slip faces are important features of dunes and other sedimentary structures, indicating the direction of sediment transport.
In the field of geology, a writer may use the term 'slip face' when describing the steep, leeward-facing slope of a sand dune or other aeolian landform.
A geologist would use the term 'slip face' to refer to the steep, leeward side of a sand dune or other sedimentary deposit where material is actively moving down due to gravity.
A geomorphologist may use 'slip face' when studying landforms and sediment transport, particularly in relation to dunes and other aeolian features.
In civil engineering, 'slip face' may be used to describe the potentially unstable side of a slope or embankment where sliding or slumping can occur.