In structural geology, an asymmetrical fold in which both limbs dip in the same direction, though usually at different angles, is known as a:

💡 Solution & Explanation

A monocline is defined as a step-like fold in rock strata consisting of a zone of steeper dip within an otherwise horizontal or gently inclined sequence of layers. Isoclinal and recumbent folds feature limbs parallel or nearly horizontal under intense compressional tectonic forces, differing structurally from step-like flexures. Geomorphology and structural geology terms are frequently tested in geography papers.