8 - variations of coastal processes over timescales Flashcards

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1
Q

what is a storm surge

A

result of extreme meteorological conditions and the configuration of coastline

water levels rise higher than predicted at high tide

can result in property damage and death

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2
Q

what is the most recent disastrous storm surge in england

A

in 2013 , december 5-7, North Sea Storm Surge

intense rain, stormy seas, spring tide, low pressure system and low lying coastline and shallow sea lead to high storm surge

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3
Q

what strong relationship can be seen regarding waves and the beach

A

WAVES (particularly steepness) and ANGLE of the beach

steepness = ratio from height to length. higher the value, greater energy brought to beach

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4
Q

differences between winter and summer beaches

A

WINTER - waves have more energy due to stronger depressions. erode and transport material off beach and out to sea in powerful backwash. lower beach profile and less mass

SUMMER - waves have less energy - increased anticyclonic activity. deposit material in swash so built up profile. some beaches sandy in summer rocky in winter

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5
Q

how can tides influence beach profiles

A

(LUNAR monthly cycle - spring high tide, neap high tide, neap low tide and spring low tide)

4 marks are made during the cycle

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6
Q

how can seasonal variations influence beach profile

A

areas of monsoon activity or seasonal rainfall patterns

wet or dry seasons impact beach profile

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7
Q

how does beach steepness influence other factors

A

steepness changes seasonally - type of beach may change

STEEP beaches have plunging waves - REFLECTIVE beach

SHALLOW beaches have breaking/spilling waves - DISSIPATIVE beach

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8
Q

what are two main causes of long term change

A

EUSTATIC

ISOSTATIC

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9
Q

what is eustatic changes

A

EUSTATIC = changes in absolute global sea levels, all seas/oceans interconnected

2 main causes:

  • thermal expansion (warmer water expands with global warming)
  • glacio-eustatic changes (melting ice caps/sheets release water locked up for long)
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10
Q

what are isostatic changes

A

ISOSTATIC - regional changes of sea level

earths crust (lithosphere) floating on asthenosphere below

isostatic balance changed by increase/decrease in relative weight or changing meeting point of land and sea

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11
Q

what is ISOSTATIC readjustment/rebound

A

in ice age, weight of glacier depressing land and sea levels raised

ice melts = land ‘rebounds’ slowly to original position increasing height relative to sea

still occurs in NW britain today, land rebounding since pleistocene epoch

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12
Q

what is isostasy

A

GLACIO-ISOSTASY = occurs when weight of glaciers depresses land relative to sea

HYDRO-ISOSTASY = increased weight of water depresses ocean basins relative to land

fall in sea level = negative changes and EMERGENCE occurs

positive changes = SUBMERGENCE

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13
Q

what can cause sea level to rise relatively

A
  1. sea level falls + land rises, remains the same or falls at slower pace
  2. sea level remains fixed while land level rises
  3. sea level rises, land rises at faster pace
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14
Q

what can also affect landforms as well as sea level change

A
  1. discordant/concordant coastline
  2. relief of land
  3. special local factors (eg was coast glaciated before sea level change)
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15
Q

what are the landforms of submergence?

A
  • ria
  • fjord
  • dalmation coast
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16
Q

what are landforms of emergence

A
  • raised beach
17
Q

what is a RIA and how is it formed (example?)

A
  • former river valley floods and opens into sea
  • caused by eustatic reasons of sea level rise, isostatic reason of land sinking below sea level
  • Pourtsmouth Harbour in Hampshire, submergent coastline
18
Q

what is a FJORD and named example

A
  • a fjord is a drowned glacial valley
  • formed when glacier retreats
  • has steep rising walls, straighter long profile and is deeper than a ria due to glaciers over deepening valley
  • west coast of Norway
19
Q

what is a DALMATION coast and how is it formed (example)

A
  • concordant coastline produced by geological structure of folds parallel to coast
  • series of longitudinal river valleys next to the coast that have been flooded (synclines) leaving parallel ranges of watershed ridges as islands
  • tectonic forces produced by african/eurasian collision compressed limestone causing anticlines and synclines
20
Q

what is a RAISED beach

A
  • beach above shoreline not reachable by waters at high tide
  • sometimes called marine terrace
  • formed by wave action when close to waterline
  • Ballyhillin Beach in mainland Ireland
21
Q

what is a RELICT CLIFF

A

a cliff that has been abandoned by sea level fall displaying CASS

emergent landform

22
Q

what is an ELEVATED MARINE PLATFORM

A

wave cut platform which now exists as extensive flat area in front of relict cliff above wave action

23
Q

what is the main positive impact of the coast on humans

A

attracts human activities - fishing, tourism, port development, settlement

24
Q

what physical resources make people travel to the coast

A
  • scenery (eg cliffs)
  • ecosystems (eg coral reefs)
  • sandy beaches
  • sunny climates
  • high quality seawater free from strong currents and rip tides
25
Q

what human resources make people travel to the coast

A
  • cultural attractions
  • heritage resources
  • quality provision of services
  • leisure facilities
  • watersports