The Old Head of Kinsale, is a headland near Kinsale, County Cork, Ireland. It is notable for being the nearest land point to the site of the sinking of the RMS Lusitania in 1915.
The old head of Kinsale was formed by differential erosion. An outcrop of hard sandstone is lodged between two layers of shale. The shale is eroded by marine action at a faster rate than the sandstone. The sandstone anticlines were much more resistant to erosion than the slate filled synclines. Thus over time the headland was formed.
http://en.wikipedia.org/wiki/Old_Head... (CC-BY)
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