8.1. Marine Erosion, Sub-aerial Processes, and Marine Transportation and Deposition Flashcards
Marine erosion processes
caused by the action of waves
1) abrasion (corrasion)
2) wave Quarrying
3) cavitation (in Wave Quarrying)
4) solution (corrosion)
5) attrition
Abrasion (corrasion)
where rock fragments are hurled at cliffs by breaking waves, gradually scraping away at the cliff face
Wave Quarrying
- as waves break against the cliff face, the pressure
of the breaking wave can compresses air in cracks. - this compressed air gradually forces open the crack in the rock - as this process continues, the rock becomes increasingly weakened.
Cavitation (in Wave Quarrying)
(the implosion or collapsing of air bubbles)
- is also part of this process; as the air bubbles collapse, they release jets of water which further weakens the rock.
Solution (corrosion)
- this occurs where the salt water is able to dissolve some of the chemicals in rocks
- for example, limestone cliffs are gradually weakened as the salt water dissolves the
calcium carbonate in the limestone.
Attrition
this is where rock fragments carried by the waves hit
against each other and gradually wear down to form sand and silt
Hydraulic Action (Wave Pounding)
- the sheer force (power) of waves hitting against the cliff face, remove or pull away (‘pluck’) loose rocks from the cliff face.
- these dislodged blocks of rock later abrade the
cliff base.
Sub-aerial processes
1) weathering
2) mass movement
Types of sub-aerial weathering
1) Solution weathering
2) Salt crystallisation
3) Biological weathering
4) Freeze-thaw weathering
5) Slaking
Solution weathering
- the change in the chemicals in rocks by acidic rainwater.
- in particular, limestone is weathered by rainwater
containing dissolved CO2.
Salt crystalisation
the growth of chloride crystals (from seawater) loosens rock fragments for erosional processes to work on.
Biological weathering
molluscs in their search for food wear down rock surfaces.
Freeze-thaw weathering
water enters the cracks in a rock and freezes; it expands and pushes the cracks further apart.
Slaking
- Alternate wetting and drying of rocks; the accumulation of successive layers of water molecules in between mineral grains of a rock.
- The increasing thickness of the water pulls the rock grains apart with great tensional stress.
Sub-aerial mass movements
soil creep, landslides, slumping and rock falls