2B.2b Flashcards
What does lithology involve
strata, bedding planes, joints or cracks, folds, faults, dips
What does geological structure have an impact on
coastal morphology, erosion rates, the formation of cliff profiles and the occurrence of micro-features, e.g. caves
Define cliff profiles
Define coastal morphology
shape and form of coastal landscapes and their features
Define jointing
Joints are fractures in rocks created without displacement.
Define faulting
also state their scale, effects on rate of erosion and how faulting occurs
- major fractures in rock created by tectonic forces, with displacement of rocks either side of the fault line.
- often large scale, extending many kilometres.
- significantly increases rate of erosion, since zones of faulted rock are much more easily eroded.
- Huge forces are involved in faulting and displacing them. Because of this, either side of the fault line, rocks are often heavily fractured and broken, which is easily exploited by marine erosion
Joints vs Faults
If rocks on one side of the break shift relative to rocks on the other side, then the fracture is a fault. If there is no movement of one side relative to the other, and if there are many other fractures with the same orientation, then the fractures are called joints.
What are folds
Folds are bends in rocks. They are produced by sedimentary rock layers being squeezed by tectonic forces. The two main types are anticlines and synclines.
Define dipping
Dip is the angle of inclination of the rock strata from the horizontal. It’s a tectonic feature. Sedimentary rocks are deposited horizontally, but can be tilted by folding and faulting by tectonic forces
Define cliff profile
the height and angle of a cliff face, plus its features such as wave-cut notches or changes in slope angle
Define cliff profile
the height and angle of a cliff face, plus its features such as wave-cut notches or changes in slope angle
What is horizontal dipping like
produces a vertical, or near-vertical profile, with notches reflecting weathering and small scale mass movement of strata that are jointed or more easily eroded
Describe High angle of seaward dip
(>45) produces a sloping, low-angled profile with one rock layer facing the sea; vulnerable to rock slides down the dip slope when uppermost strata are attacked by sub-aerial processes. The profile slopes corresponding to that of strata dip. Bedding planes between strata are weakly bonded and readily loosened by weathering
Describe Low angle of seaward dip
(<45) produces a steep profile, that may even exceed 90 degrees, creating areas of overhanging rock; very vulnerable to rock falls. Frequent small-scale mass movement of material weathered from cliff face. Major cliff collapse when undercutting by marine erosion makes overhang unsustainable
describe Landward dipping strata
produces steep profiles on 70-80’ as downslope gravitational force pulls loosened blocks into place. Very stable profile with few rock falls