JOINTING: Cracks where there is no movement of rock, often caused by cooling, tension, unloading weight from above
DIPPING: Rock and bedding planes (seperates layers of sedimentary rock) are at an angle from the horizontal
FAULTING: Cracks where there is movement of rock, often larger than joints, often caused by tectonic movements
FOLDING: Bending of rocks due to compressional forces. Upfold= anticline, Downfold= syncline
This all has important influences on coastal morphology, erosion rates, the formation of cliff profiles and occurrence of micro features
e.g. caves, blowholes, geos. A weak point will be weathered/eroded, that joint is then enlarged, may become large enough to form a cave
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