Glacial striations on bedrock. Rocks embedded in the bottom of the glacier served as "tools" that scratched the bedrock over which the glacier moved. These features are useful indicators both of the former presence of glaciers and of the direction in which the glacier moved.
Calcite slickenlines on a fault surface. Slickensides are a polished and striated surface that forms along a rock surface as a result of friction along a fault plane.