Depositional landforms timed essay study Flashcards
formation of beaches
beaches form from the accumulation of sediment such as sand, shingle and pebbles, deposited by wave action
the profile and shape of a beach are largely dictated by the characteristics of the incoming waves
constructive waves
these waves have a strong swash and weak backwash
they gently deposit materials, building up the beach
this leads to a wide, flat beach with a gradual slope
destructive waves
characterised by a strong backwash and weak swash, these erode beach materials
they typically create narrow, steep beaches
swash aligned beaches
develop when waves approach the coast head on
the swash and backwash distribute sediment evenly along the beach maintaining a relatively straight shoreline
drift aligned beaches
form as a result of longshore drift where waves hit the coast at an angle, moving sediment laterally along the shoreline
these beaches often develop features like spits
spits
these are narrow, elongated landforms extending from the coast into the sea or a river mouth
formed by the longshore drift, spits often curve at their ends due to wave refraction and changing wind directions
tombolos
a unique landform connecting an island to the mainland, created when sediment accumulates in the sheltered area between them
the formation of a tombolo can significantly alter a local coastal dynamic including tidal patterns and sediment distribution
stabilising factors
vegetation: plants are vital in stabilising these. their roots bind the sediment reducing erosion
human interventions: coastal management practices like the construction of groynes or breakwater can help maintain the shape and position of spits and tombolos
barrier beaches
these are extensive, narrow strips of single lying parallel to the coastline
their formation involves the accumulation of sediment above the high tide mark, often stabilised by vegetation over time
dunes
sand dunes are formed by wind action where sand is deposited in areas with reduced wind velocity, usually behind an obstruction
the succession of vegetation on dunes starts with hardy pioneer species which are gradually replaced by more complex plant communities
coastal protection
natural defences: barrier beaches and dunes serve as natural buffers against coastal erosion and storm surge flooding
ecosystem services: they support diverse ecosystems and are crucial in maintaining coastal biodiversity
estuaries
these are transitional zones between river environments and maritime environments
they play a pivotal role in trapping sediments carried by rivers and tidal actions, creating unique habitats like mudflats
mudflats
these are flat, muddy areas exposed at low tide
their formation is due to the deposition of fine sediments in areas with calm waters such as estuaries or behind barrier islands
mudflat ecology
rich in nutrients and support a wide array of organisms including benthic animals, birds and fish
they serve as feeding and breeding grounds for many species and are vital in nutrient cycling and energy transfer in the coastal ecosystem
saltmarshes
found in temperate regions, these are grassy marshlands that have adapted to saline conditions
they are dominated by salt tolerant plants such as cordgrass