coasts Flashcards
what are the characteristics of rocky coasts
resistant geology
(withstands erosive forces of sea, rain and wind), often in a high-energy environment
erosion > deposition
what are the characteristics of costal plain landscapes
deposition > erosion
found near areas of low relief and result from supply of sediment from different terrestrial and offshore sources, often in a low-energy environment.
deposition and transportation
what is responsible for concordant and discordant coastlines
Geological structure is responsible for the formation of
concordant and discordant coasts.
what is geological structure
Geological structure (jointing, dip, faulting, folding) is an important influence on coastal morphology and erosion rates, and also on the formation of cliff profiles
Geological structure influences coastal morphology: Dalmatian and Haff type concordant coasts and headlands and bays on discordant coasts.
dipping comes under geological structure, what are the 4 types of dipping
-horizontal dipping= more easily eroded
-seaward dipping (low angle)= may produce overhanging rock that is vulnerable to rock falls
-seaward dipping (high angle)= vulnerable to rock slides
-landward dip= stable cliff, reduced rock falls
what does rates of costal recession depend greatly on
-bedrock lithology (igneous, sedimentary, metamorphic) and unconsolidated material (boulder clay) geology are important in understanding rates of coastal recession
- alternating strata in cliffs (permeable/impermeable, resistant/less resistant) produces complex cliff profiles and influences recession rates. (differential erosion)
-Vegetation is important in stabilising sandy coastlines through dune successional development and salt marsh successional development in estuarine areas.
-geological structure
what marine erosion processes contribute to distinctive costal landscapes
- wave type (constructive and destructive)
-erosional processes (HA, Corrosion, abrasion, attrition)
apart from marine erosion, what other processes affect distinctive costal landforms
-transportation and deposition
-subaerial processes
-bedrock lithology and geology
-plant succession can stabilise coastlines
what distinctive costal landforms does marine erosion create
wave cut notches, wave cut platforms, cliffs, the cave-arch-stackstump sequence
what is sediment transportation influences by
s influenced by the angle of wave attack, the process of longshore drift, tides and currents.
what distinctive costal landforms does deposition and transportation create
(beaches, recurved and double spits,
offshore bars, barrier beaches and bars, tombolos and cuspate forelands), which can be stabilised by plant succession.
what do sediment cells explain
equilibrium and positive and negative feedback
what is contempory sea level change caused by
-global warming
-tectonics
sea level change has produced emergent coastlines, what are they
-raised beaches (a old beach now above tide level)
-fossil cliff (a steep slope found behind a raised beach exhibiting past evidence of marine erosion)
sea level change has produced submergent coastlines, what are they
-dalmation coastline
-ria
-fjard
-fjord
define eustatic
(ice formation/melting,
thermal changes)