Key terminology Flashcards
Bedding planes
Natural breaks in the strata.
Cliff profile
The height and the angle of the cliff, as well as its features, such as wave cut notches or changes in the cliff angle.
Coastal Accretion
The deposition of sediment and the coast, and the seaward growth of the coastline, creating new land.
Coastal plains (Alluvial coastline)
The land gradually slopes towards the sea across and area of deposited sediment. E.g., sand dunes or mud flats. Usually found in low energy coastlines.
Concordant coastline
Rock strata runs parallel to the coastline
dip
the angle rock strata lies.
discordant coastline
Where different resistant rock strata layers intersect the coastline
dynamic equilibrium
A balanced system where inputs and outputs balance over time.
emergent coast
Where coasts are rising relative to sea levels.
faults
major fractures in rock caused by tectonic forces, and causing the displacement of rocks on either side of the Faultline.
geological structure
the arrangement of rocks in three dimensions: Deformation, faulting, and strata.
halophyte
plants that can tolerate salty environments.
high energy coastline
Exposed coasts facing prevailing winds with long wave fetches resulting in powerful waves.
Lithification
Where materials such as sand, gravel ,and clay is compacted over time and becomes rock.
Lithology
The characteristics of rock (Permeability, resistance, type of rock, presence of fissures, porosity, joints and bedding planes)
Littoral zone
The wider coastal zone including adjacent land areas and shallow areas of sea offshore.
low energy coastlines
sheltered coasts with limited fetch and slow winds resulting in small waves.
Plant succession
the changing structure of a plant community over time as once bare sediment is consolidated by plants.
pore water pressure
the pressure water experiences below a certain point under the water table due to the water above it.
Primary coasts
dominated by land-processes such as deposition from rovers or lava flows.
rocky coastlines
resistant rocks, with cliffs varying in height from a few metres to hundreds of metres, usually found in high energy environments.
secondary coasts
Dominated by marine processes such as erosion and marine deposition.
submergent coasts
Where coasts are being flooded by the sea, either by rising sea levels or subsiding land.
unconsolidated sediment
materials such as sand, gravel, clay and silt that has not been compacted or cemented to become sedimentary rock.
wave refraction
the bending of waves around a headland.
xerophyte
plants that can tolerate very dry environments
abrasion
where sediment picked up by breaking waves is thrown against the cliff face, causing it to chip away.