Sloping or inclined in the same direction, especially referring to geological formations or rock strata that dip uniformly in one direction.
From Greek 'kata-' (down) + 'klinein' (to lean or incline). The term emerged in 19th-century geology to describe systematic directional slopes in layered rock formations.
Geologists use this word to describe how mountains and rock layers tell a story—when strata all slope the same way, it reveals ancient forces that pushed the earth in one direction, like a giant hand tilting the planet's pages.
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