Coasts Flashcards
Littoral zone
The wider coastal zone including adjacent land areas and shallow parts of the sea just offshore
Cliff profile
The height and angle of a cliff face as well as its features, such as wave-cut notches or changes in slope angle
Coastal accretion
The deposition of sediment at the coast and the seaward growth of the coastline, creating new land. If often involves sediment deposition being stabilised by vegetation
Dynamic equilibrium
The balanced state of a system when inputs and outputs balance over time. If one element of the system changes because of an outside influence, the internal equilibrium of the system is upset and other components of the system change. By a process of feedback, the system adjusts to the change and the equilibrium is regained
Holocene
The geological epoch that began about 12,000 years ago at the end of the last Pleistocene ice age. It’s early stages were marked by large sea level rises of about 35m and a warming interglacial climate
Faults
Major fractures in rocks produced by tectonic forces and involving the displacement of rocks on either side of the fault line
Unconsolidated sediment
Material such as sand, gravel, clay and silt that has not been compacted and cemented to become sedimentary rock (it has not undergone the process of lithification) and so is loose and easily eroded
Pore water pressure
The pressure water experiences at a particular point below the water table due to the weight of water above it
Fetch
The uninterrupted distance across water over which a wind blows, and therefore the distance waves have to grow in size
Swash
The flow of water up a beach as a wave breaks
Backwash
When water runs back down the beach to meet the next incoming wave
Beach morphology
The shape of a beach, including its width and slope (the beach profile) and features such as berms, ridges and runnels. It also includes the type of sediment (shingle, sand, mud) found at different locations on the beach
Blow hole
Forms when a coastal cave turns upwards and breaks through the flat cliff top. Usually this is because of erosion of especially weak strata or the presence of a fault line
Currents
Flows of seawater in a particular direction driven by winds or differences in water density salinity or temperature. Some are almost continuous such as those that form the global thermohaline circulation and others are more sporadic such as long shore currents which some last only a few hours such as rip currents
Mass movement
The downslope movement of rock and soil; it is an umbrella term for a wide range of specific movements including landslides rockfall and rotational slides