1. Cuesta: A cuesta is a long, low ridge with a gentle slope on one side (the dip slope) and a steep slope on the other (the escarpment). The tough rock forms the dip slope, while the softer rock forms the escarpment.
2. Hogback: Similar to a cuesta, but the dip slope is much steeper, making it appear like a sharp ridge. This occurs when the layers of rock are tilted at a much steeper angle.
3. Mesa: A mesa is a flat-topped hill with steep sides, formed when the soft rock is eroded away, leaving a plateau of the resistant rock on top.
4. Butte: Similar to a mesa, but smaller in size. It can be formed by the erosion of a mesa or directly from a large, isolated block of resistant rock.
5. Cliffs: When the difference in erosion resistance is significant, the resistant rock can form sheer cliffs along the edge of the soft rock layer.
6. Plateaus: Large, flat areas of resistant rock elevated above the surrounding landscape.
7. Inselbergs: Isolated hills or mountains of resistant rock rising abruptly from a plain.
8. Escarpments: Steep cliffs formed at the boundary between resistant and easily eroded rocks.
The specific landform that develops depends on the thickness of the layers, the angle of the layers, the type of rock, and the erosive forces acting on the landscape.