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. Old stacks Raised beach covered with coarse shingle. Old cliff line Diagram from Arrran and the Clyde Islands, Scottish Natural Heritage
Raised beaches ard/physical/features/sea_level /
Raised beach, Newton Point, Arran wave-cut platform old cliff line
King’s Cave, from the Drumadoon sill wave-cut platform old cliff line
King’s Cave All 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.
Raised sea stack, Bute. Raised beach Diagram from Arrran and the Clyde Islands, Scottish Natural Heritage
Raised natural arch
Raised beach deposits are usually made of coarse, rounded pebbles. This deposit is cemented with iron. Godrevy Point, Cornwall
Close-up of the Godrevy Point deposit
Marine platforms Island above old sea level
Penberth, Cornwall Marine platform
River terraces
River terraces, NW Scotland
River terraces, Catacol
Drowned coast-lines Drowned glacial trough West coast of Norway Fjord
Norwegian fjord
Drowned coast-lines South coast of Devon ria Drowned river valley
Ria in Cornwall
Raised coastlines Skogarfoss Iceland Atlantic Old cliff line
The End River Skoga, falling over the post-glacial cliff THE END