Coastal Landscapes and Change - enquiry q1 Flashcards

1
Q

Littoral Zone

A

a coastal area/zone - can be divided into subzones

  • offshore, nearshore, foreshore, backshore, coast
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2
Q

Coastal plains

A

the land gradually slopes towards the sea across an area of deposited sediment - aka alluvial coasts

  • e.g. sand dunes and mud flats

North Northumberland

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3
Q

Primary coasts

A

are dominated by land based processes

  • e.g. deposition at the coast from rivers or new coastal land from lava flows

Nile River Delta

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4
Q

Secondary coasts

A

are dominated by marine erosion or deposition processes

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5
Q

Emergent coasts

A

where the coats are rising relative to sea level

  • e.g. due to tectonic uplift

Hudson Bay, Canada

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6
Q

Submergent coasts

A

are being flooded by the sea, either due to rising sea levels and/ or subsiding land

Western Norway

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7
Q

Estuarine coastline

A
  • gradually transition from land to sea
  • extensive mud flats
  • at mouths of rivers, sometimes form slat marshes

The Thames mouth

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8
Q

Sandy coastline

A
  • lots of sand dunes
  • high tide covers beaches
  • vegetation prevents erosion

Whitby beach, Yorkshire

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9
Q

Cliffed coastline

A
  • low tide exposes rocky platforms
  • vertical steep rocks or shallow angled rocks
  • transitions from land to sea is abrupt

Whit cliffs of Dover, Kent

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10
Q

Sub-aerial processes

A

land based processes that occur above the waterline. They include weathering and mass movement, which happen on the cliff rocks.

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11
Q

Marine erosion

A

a type of erosion facilitated by wave and tidal action

  • the repetitive nature of wave action produces a mechanism able to erode loose soils/sands and wear down rock cliff surfaces as well
  • e.g. hydraulic action, abrasion, attrition
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12
Q

Cliff profile

A

the height and angle of a cliff face and its features

  • e.g. wave cut platform
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13
Q

Erosion resistance

A

rocks forming cliffs vary in terms of their resistance to erosion and weathering

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14
Q

Geology

A

the study and understanding of rocks

  • their type and arrangement
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15
Q

Geological structure

A

the arrangement of rocks in 3 dimension

~ strata - layers of rock within an area

~ deformation - the degree to which rock units have been deformed (tilted or folded) by tectonic activity

~ faulting - the presence of major fractures that have moved rocks from their original positions

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16
Q

Strata

A

layers of rock within an area

17
Q

Deformation

A

the degree to which rock units have been deformed (titled or folded) by tectonic activity

18
Q

Faulting

A

the presence of major fractures that have moved rocks from their original positions

19
Q

Concordant

A

(Pacific coasts) concordant coasts are generated when rock strata run parallel to the coastline

20
Q

Discordant

A

(Atlantic coasts) form when different rock strata intersect the coast at an angle, so geology varies along the coastline

21
Q

Dip

A

the angle of the rock strata in relation to the horizontal caused by tectonic activity

  • horizontal dip, seaward dip
22
Q

Lithology

A

the rock type and its main characteristics

  • igneous, metamorphic, sedimentary0
23
Q

Joint

A

fractures in rocks created without displacement of rock

  • displacement of the rock is not observable
24
Q

Fault

A

the fracture in the rock strata due to strain in which the displacement of the rock is observable

25
Fissures
small cracks in rocks, often only a few cm or mm long
26
Intrusion
when molten igneous rocks is injected and emplaced into existing rocks (the country rock) and on cooling becomes an igneous intrusion
27
Bedding Plane
the planar surface which separates one layer of sedimentary rock form another
28
Sill
an igneous intrusion which is in concordance with (in parallel with) the surrounding rock layers and is normally injected as a near horizontal sheet between the bedding planes of country rock
29
Fold/ folding
a bending or flexure of the Earth's crust due to compressional tectonic forces
30
Unconsolidated sediment
material such as sand, gravel, clay and silt that has not been compacted and cemented to become sedimentary rock
31
Sedimentary rocks
rocks formed from the accumulation of material derived from pre existing rocks and organic sources less resistant to erosion than igneous rocks erosion rate = moderate - fast e.g. sandstone, limestone, shale
32
Igneous rocks
rocks that have formed from the crystallisation and solidification of magma more resistant to erosion erosion rate = very slow e.g. granite, basalt, dolerite intrusive - formed inside volcano extrusive - formed outside volcano
33
Metamorphic rocks
form when rocks are subjected to high heat, high pressure, hot mineral rich fluids or commonly a combination of these factors more resistant to erosion erosion rate = slow e.g. slate, schist, marble
34
Pore water pressure
the pressure water experiences at a particular point below the water table due to the weight of water above it
35
Coastal accretion
the deposition of sediment at the coast and the seaward growth of the coastline, creating new land it often involves sediment deposition being stabilised by vegetation forward movement of a coastline due to deposition
36
Coastal recession
the movement of the coastline backwards due to erosion
37
Psammasere
a sand dune ecosystem