High And Low Energy Environments Flashcards

(28 cards)

1
Q

What is an example of a HIGH ENERGY coastline?

A

Saltburn to Flamborough Head- Yorkshire
(Rocky, upland are, 60km coastline)

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2
Q

Geology of Saltburn to Flamborough

A
  • Flamborough Head- Southern stretch of coastline:
    Large chalk headland; spectacular cliffs topped with till (deposit left behind by glaciers during Devensian glacial period); Bays+ headlands and high cliffs (varied scenery) due to differences in rock resistance.
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3
Q

what is the dominant wave direction and fetch length of s to f?
what about rates of erosion?
wave height?

A

*Dominant waves from north + northwest
*fetch over 1500km
*most exposed coast is northfacing e.g. nearest Saltburn (relieves highest inputs of wave energy)
*rates of erosion: due to differences in wave energy and geology; weak shale + clay areas rate is 0.8m p.a. and more resistant sandstones+ limestones is 0.1m p.a.
*wave height- often exceeded 4m even in summer (usually less stormy)
*high energy inputs responsible for longshore drift (North to south)- in some places sediment movement interrupted by headlands; sand and shingle accumulates forming beaches and bays (e.g Filey Bay)

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4
Q

Example of a bay along s to f coastline

A

Filey bay
Bridlington bay

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5
Q

What are sediment sources for s to f coastline

A
  • cliff erosion
  • only large river (the esk) enters north sea at Whitby - limited fluvial supply of sediment due to construction of weirs and reinforced banks along its course.
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6
Q

what are the cliffs like at Flamborough Head?

A

made of chalk- physically very strong; vertical cliffs typically 20-30m high, with overlying till lowered by mass movement processes to angle about 40 degrees.

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7
Q

what are the cliffs like between Robin Hoods Bay and Saltburn?

A

further north than Flamborough: higher cliffs, often with stepped profile (more varied geology)

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8
Q

when are steeper sloped cliffs formed?

A

more resistant sandstones and limestones; gentler slopes corresponding to weaker clays.

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9
Q

what LANDFORMS can be found at Robin Hoods bay?

A

high energy waves + active erosion means cliffs are retreating, leaving behind WAVE- CUT PLATFORMS.
HEADLANDS AND BAYS: discordant coastline, weaker rock retreated and more resistant rock forming headlands (limestone and chalk).

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10
Q

what does the prominent headland at Flamborough consist of?

A

CHALK
deep bays made of CLAY

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11
Q

what landforms have formed on these headlands from s to f?

A

Robin hoods bay- WAVE- CUT NOTCH
FLAMBROUGH HEAD is a large CHALK HEADLAND between FILEY and BRIDLINGTON bays
WAVE REFRACTION- wave energy concentrated of headlands that project out to north sea; weaknesses e.g. CRACKS AND JOINTS are exploited + enlarged to form caves + arches. (e.g. SELWICK’S BAY at Flamborough Head).
GREEN STACKS PINNACLE: a stack at end of headland.
over 50 GEOS along coastline (aligned to NE/ NEE dom. wind direction)

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12
Q

What is an example of a LOW ENERGY COASTAL ENVIRONMENT?

A

the Nile Delta

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13
Q

What is a delta?

A

Large areas of sediment found at mouths of rivers- deposited by rivers+ tidal currents

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14
Q

How do deltas form?

A

Sediment is deposited at a faster rate than wave/ tides can remove it.
Typically form where:
* rivers entering sea carry large loads
* low tidal range
* low energy environments on coastline (e.g. bay)

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15
Q

What is an ARCUATE delta?

A

Sufficient sediment supply available for delta to grow seawards, but wave action is strong enough to smooth leading edge - has lagoons.
* Fan/ triangle shape with rounded leading edge

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16
Q

How long is the RIVER NILE?

17
Q

What is the Niles CATCHMENT AREA?

A

Over 3 million km³
Large proportion of Nile flow originates in Ethiopia + comes from summer monsoon rains- some from central Africa

19
Q

The nile carries a huge sediment load despite relatively low discharge, what sediment can be found in the suspended load?

A

30% clay
40% silt
30% fine sand

20
Q

Where does the coastal plain of the nile delta occupy?

A

Northern part of nile delta

21
Q

What landforms/ features are found on the foreshore plain of the delta?

A

Lagoons, salt marshes and alluvial deposits in the depressions between dunes and bars e,g, lake manzala

22
Q

What features/ landforms can be found at the sandy zone at the delta?

23
Q

Where does the delta split into two distributaries?
What has formed here?

A
  • Cairo
  • wave action in the Mediterranean redistributes sediment at front of delta - reworked sediment forms series of CURVED BARRIER BARS; closes off segments of Mediterranean sea to form LAGOONS.
24
Q

where is the HOLDERNESS COAST?

A

coastline extending from Flamborough Head to Spurn point (a spit)

25
Q

GEOLOGY at HOLDERNESS

A

SOFT BOULDER CLAY- rapidly eroded by marine processes- STRUCTURALLY WEAK so very LITTLE RESISTANCE
(sloping cliffs 5-20m high)
CHALK surrounds the boulder clay; STRONGER but has eroded along FAULT LINES+ BEDDING PLANES- resulting in erosional features such as cliffs, caves, arches, stacks

26
what is the Holderness's RATE OF RETREAT? how much has it retreated?
2M/ YEAR- one of Europe's FASTEST ERODING COASTLINES has retreated 4KM SINCE ROMAN TIMES (at least 29 villages submerged)
27
Holderness- dominant wave direction
NE wind+ wave direction
28
Holderness- fetch
500-800KM- not particularly large, but other factors increase wave energy: * CURRENTS: move to UK from ATLANTIC that has 5000KM FETCH (high energy destructive waves) * the north sea has INTENSE STORMS (high energy) * BATHYMETRY: the north sea has deep sea floor- waves not slowed down by sea bed
29
main problem at Holderness
BEACHES- consist of BOULDER CLAY- easily eroded+ produces FINE CLAY PARTICLES which are easily transported by LONGSHORE DRIFT so don't accumulate in front of cliffs to form natural rock armour NARROW BEACHES- don't absorb much wave energy so waves hit base of cliff, esp. during high tide