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Cliffs of Moher, Ireland, September 1999

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Sandstone is more resistant to erosion than siltstone, and stick out from the cliff-face compared with the intervening layers of siltstone. One of these sandstone forms the platform below the path at the viewing point.   The sediments that now form the rock of the cliffs were originally deposited on an ancient sea-bed some 320 million years ago. The shore of the sea is quite a distance away to the north.  Rivers flowing off the land deposit their sediment into the sea in a series of deltas.

Clonmacnoise - The Burren - The Dohlmans - Cliffs of Moher
Dublin
- Glendalough - Fanore - More Highlights

updated: 12/28//07

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