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  2. Skellig Michael - Wikipedia

    en.wikipedia.org/wiki/Skellig_Michael

    Skellig Michael consists of approximately 22 hectares (54 acres) of rock, with its highest point, known as the Spit, 218 m (714 ft) above sea level. The island is defined by its twin peaks and intervening valley (known as Christ's Saddle), which make its landscape steep and inhospitable.

  3. Saint Michael's line - Wikipedia

    en.wikipedia.org/wiki/Saint_Michael's_line

    Like many places dedicated to St. Michael, the aligned sites are almost all located on prominent hilltops or other hard to reach places, and include Skellig Michael, St Michael's Mount, Mont Saint-Michel, the Sacra di San Michele, San Michele Arcangelo, the Sanctuary of Monte Sant'Angelo, the Panormitis Monastery of the Archangel Michael, and Stella Maris Monastery.

  4. Skellig Islands - Wikipedia

    en.wikipedia.org/wiki/Skellig_Islands

    Also known as Great Skellig (Sceilig Mhichíl in Irish [3]), this is the larger of the two islands, with two peaks rising to over 230 m (750 ft) above sea level.With a sixth-century Christian monastery perched at 160 m (520 ft) above sea level on a ledge close to the top of the lower peak, Great Skellig is designated as a UNESCO World Heritage Site.

  5. Skellig Michael Weather - Hourly Forecasts and Local ... - AOL

    www.aol.com/.../ireland/skellig-michael-56557145

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  6. County Kerry - Wikipedia

    en.wikipedia.org/wiki/County_Kerry

    Skellig Michael is a World Heritage Site, famous for the medieval monastery clinging to the island's cliffs. The county contains the extreme west point of Ireland, Dunmore Head on the Dingle Peninsula, or including islands, Tearaght Island , part of the Blaskets.

  7. Little Skellig - Wikipedia

    en.wikipedia.org/wiki/Little_Skellig

    Little Skellig is the smaller of the two Skellig Islands, the other being Skellig Michael, 1 km to the south-west. [1] The islands rose c. 374–360 million years ago during a period of mountain formation, along with the MacGillycuddy's Reeks mountain range. Later, they were separated from the mainland by rising water levels. [3] [4]

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