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The rock is highly compressed and contains a number of fracture lines and jointing.
As a result of erosion along a major north–south-trending fault line containing bedrock much more brittle that that on surrounding areas, a large part of the rock broke away, resulting in the depression between the peaks, which is today known as Christ's Saddle.
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The island is defined by its twin peaks and intervening valley (known as Christ's Saddle), which make its landscape steep and inhospitable.
When the Atlantic ocean level rose, it created deep marine inlets such as Bantry Bay and left the Skelligs detached from the mainland.
Later, they were set adrift and surrounded by rising water levels.
Skellig Michael consists of approximately 54 acres of rock, with its highest point, known as the Spit, 714 feet (218 m) above sea level.
The monastery is situated at an elevation of 550 to 600 feet (170 to 180 m), Christ's Saddle at 422 feet (129 m), and the flagstaff area at 120 feet (37 m) above sea level.
The monastery can be approached by a number of narrow and steep flights of stone steps which ascend from three landing points.