The features that may be common along active faults, like the San Andreas is given below"
"Some features that may be common along active faults, like the San Andreas, are:
Offset landforms: These are features that are displaced or separated by the movement of the fault. For example, streams, roads, fences, or walls that cross the fault may appear to be shifted or broken by the fault. The amount of offset can indicate how much the fault has slipped over time.
Linear valleys or ridges: These are features that are formed by the erosion or uplift of the fault zone. For example, a fault may create a low area where water and sediment accumulate, forming a valley. Or a fault may push up rocks along its edge, forming a ridge.
Fault scarps: These are steep slopes or cliffs that are created by the vertical displacement of the fault. For example, a fault may cause one side of the land to rise or drop relative to the other side, creating a sudden change in elevation.
Sag ponds: These are small lakes or ponds that are formed by the accumulation of water in depressions along the fault. For example, a fault may bend or warp the land surface, creating a basin where water can collect.
Springs or seeps: These are places where water flows out of the ground along the fault. For example, a fault may fracture the rocks and create pathways for water to reach the surface.
Lastly, Fault gouge or breccia: These are types of rocks that are formed by the grinding or crushing of the fault. For example, a fault may pulverize the rocks along its surface, creating a fine-grained material called fault gouge. Or a fault may break the rocks into angular fragments, creating a coarse-grained material called fault breccia."
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