Joints
Natural fractures in rocks that occur without significant lateral displacement
Common in igneous and sedimentary rocks
Occur due to tensile/tectonic stress
Bedding planes
Horizontal layers that separate successive layers of sedimentary rock
Common in sedimentary rocks
Form during sedimentation when layers of sediment are deposited over time
Fissures
Narrow openings or cracks in rock surfaces, often forming networks of fractures.
Very common in limestone
Occur due to Tectonic stress, expansion and contraction and
chemical weathering processes.
What is their overall effect on cliffs?
Increase water penetration
Accelerate weathering and erosion
Promote mass movement processes such as rockfalls, slides and slumping
Leads to unstable cliffs that retreat inland over time.