A slope of the land surface that conforms approximately with the dip of the underlying rocks; specifically, the long, gently inclined face of a cuesta.

a geological formation often created by tilted strata

a slope where the dip direction of rock bedding is sub-parallel to the look direction of a slope

A natural slope of the land surface that relates primarily to the tilt (dip) of the underlying bedrock or tilt of the bedding planes with in a tectonically uplifted block of sedimentary rock

A hill slope underlain by bedding parallel to the slope.