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Coastal Dunes

chidat Geography A level Englisch 8 Folien

Coastal Dunes

Folien in diesem Satz (8)

  1. Coastal Sand Dunes

  2. Formation

    • For a sand
    • dune to form there
    • must be a reliable
    • supply of sand, a
    • means of transporting it (wind), and somewhere
    • for it to be deposited more quickly than it is eroded.
    • •The dry grains of
    • sand can then be transported by the wind through a process of saltation. If the wind
    • blows towards the land, sand will be transported up the beach and beyond the
    • high tide mark. When the dry
    • particles of sand reach the top of the beach they might be trapped by driftwood
    • and rocks.
    • If the sands
    • is not eroded again, plants might start growing on it increasing the size and
    • hence trapping more sand.
  3. Conditions of formation

    • Strong onshore
    • winds
    • Large
    • expanses/area of dry sand ( spits, cuspate forelands, bays)
    • Reliable
    • supply of sand
    • Large tidal
    • range
    • Vegetation to
    • act as obstacles to limit/trap sand movement and deposition can occur –
    • vegetation cause wind velocity to drop.
  4. Sand Dune Characteristics

    • Sand Dune Characteristics
    • Bildunterschrift: http://www.s-cool.co.uk/a-level/geography/coastal-processes/revise-it/coastal-deposition
  5. Characteristics of a sand dune

    • Embryo – this is the
    • first part of the dune to develop and are formed in sheltered areas. Once the
    • pioneer plant species such as Lyme grass, sand couch grass and sea rocket
    • stabilise, the sand is trapped and accumulated over time - the dune grows.
    • Conditions in this dune are dry thus plants adapt by growing long roots and/or
    • thorny leaves to reduce evapotranspiration. The early colonising plants will
    • eventually die off and decompose. They
    • add nutrients to the soil which makes the dunes more hospitable for new and
    • larger plants to grow therefore giving them the capability trap more sand –
    • larger dunes develop.
    • Vegetation
    • makes the dunes stable.
  6. Folie 6

    • Fore dune – They tend to
    • be very yellow as they have limited vegetation so no real humus layers develop.
    • Marram grass is the main coloniser and stabiliser.
    • Yellow dune – The colour
    • darkens as organic material add nutrients and humus to the soil. Sea couch and marram grass stabilise the
    • dune.
    • Grey dunes – Developing
    • humus layers changes the colour of the dune form yellow to grey. Water retention is also increased
    • (soil becomes damper and richer) due to more humus therefore more species of plants
    • thrive e.g. Creeping willow, red fescue and dewberry. In time, the dune stops growing because the
    • sheltered means that there is a lack of wind to blow the sand.
  7. Folie 7

    • Mature dunes –
    • The dunes can
    • sustain more plants such as thistle, evening primrose, bracken, bramble and
    • heather because the humus layers grow more. Less than 10% of sand is exposed on
    • these dunes.
    • Dune slacks - are low lying
    • depressions between the dunes. Plants in
    • the dune slacks include wild strawberries, buttercup and violets with some flag iris and willow in the
    • slacks at the rear of the main dune system. In the slacks, vegetation covers almost
    • everything.
  8. Folie 8

    • It
    • is key to remember that during the development of mature dunes, the embryo
    • dunes are continually being formed at the base of the dune system consequently,
    • the dune system is advancing seaward.

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Beschreibung
Coastal Land forms: Dunes
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