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EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES •What does isostatic mean? •What does eustatic mean? •Which is changing in these photos – land level or sea level?
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EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Mar 22, 2016

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EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES. What does isostatic mean? What does eustatic mean? Which is changing in these photos – land level or sea level?. Aerial view of the raised beach on the west coast of Arran. - PowerPoint PPT Presentation
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Page 1: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

•What does isostatic mean?•What does eustatic mean?•Which is changing in these photos – land level or sea level?

Page 2: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Aerial view of the raised beach on the west coast of Arran.

Old stacks

Raised beach covered with coarse shingle.

Old cliff line

Diagram from Arrran and the Clyde Islands, Scottish Natural Heritage

Page 3: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Raised beaches

http://www.bbc.co.uk/scotland/education/geog/coastline/standard/physical/features/sea_level/

Sea level 13,000 years ago

Sea level 6,000 years ago

Sea

Cross section though raised beaches

RockCave

Rock platform

Beach

Raised beaches

Stack

Page 4: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Raised beach, Newton Point, Arran

wave-cut platform old cliff line

Page 5: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

King’s Cave, from the Drumadoon sill

wave-cut platform

old cliff line

Page 6: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

King’s CaveAll the caves are full of very rounded pebbles , which have the same texture as beach pebbles.

The caves also contain many marine shells, which are encrusted with lichens. They are not part of the present marine deposits.

Page 7: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Raised sea stack, Bute.

Raised beach

Diagram from Arrran and the Clyde Islands, Scottish Natural Heritage

Page 8: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Raised natural arch

Page 9: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Raised beach deposits are

usually made of coarse, rounded pebbles. This

deposit is cemented with iron. Godrevy Point, Cornwall

Page 10: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Close-up of the

Godrevy Point

deposit

Page 11: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Marine platformsIsland above old sea level

Page 12: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Penberth, Cornwall

Marine platform

Page 13: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

River terracesThe Graded Steam

Idealised cross section

Upper reaches

Middle reaches

Lower reaches

Oblique view upstream

Terraces

Knick point

A

B

C

A

C

B

Idealised long profile

Knick points

Sea level 2

Sea level 3

Sea level 1

River

Page 14: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

River terraces, NW Scotland

Page 15: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

River terraces, Catacol

Page 16: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Drowned coast-lines

Drowned glacial trough

West coast of Norway

Fjord

Page 17: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Norwegian fjord

Page 18: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Drowned coast-linesSouth coast of Devon

ria

Drowned river valley

Page 19: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Ria in Cornwall

Page 20: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

Raised coastlines Skogarfoss

Iceland

Atlantic

Old cliff line

Page 21: EVIDENCE FOR ISOSTATIC AND EUSTATIC SEA LEVEL CHANGES

The End

River Skoga, falling over the post-glacial cliff

THE END