Irelands physical geography is very unique and shows clearly how the island as we know it today was formed. Often compared to a saucer or frying pan because of the low lying center raised edges, costal mountains surround the lower middle plain of the island making for beautiful scenery and interesting geographic inquiry. Ireland is the product of several natural processes that help explain the landscape.
The coast is lined with small mountains that encircle the lower lying central plain
Plate tectonics are responsible for the bulk of the physical features that define the island. Ireland, as it is today, is on the Eurasian Plate, but the distinguishable north western part of Ireland was once part of the tectonic plate that now makes up the North American Plate. These two plates collided 400 million years ago when a divergent plate boundary stopped spreading and the two plates were forced together. The resulting convergence, combined with the duration of that convergence, caused compression that led to major mountain building and syncline folding that can still be observed today.
Copyright of the Geological Survey of Ireland 2006.
An example of some syncline folding left behind by the convergent boundary that helped
create the mountainous coast of Ireland
Ireland's landscapes not only makes for nice pictures, but in understand how they were formed a broader picture can be drawn about the island, as well as the world have been shaped by a slow but tumultuous past.
Sources:
http://www.doeni.gov.uk/niea/index.htm
http://www.ringofgullion.org/
http://www.ireland-information.com/
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