Mount Brandon - Geography

Geography

Brandon is in the middle of a high ridge, sometimes called the Brandon Group, which runs north-south for 10 kilometres (6.2 mi) across the peninsula. This ridge also includes the peaks of Barr an Ghéaráin at 840 metres (2,760 ft), Binn Fhaiche 822 metres (2,697 ft), Más an Tiompán at 763 metres (2,503 ft), and Piaras Mór at 748 metres (2,454 ft).

Mount Brandon owes its craggy shape to the work of local glaciers during the ice age, which gouged out a series of corries on the eastern flank of the mountain. The summit of Mount Brandon is rounded and smooth because it was a nunatuk, and presents a stark contrast to the conical top of Barr an Ghéaráin, which is almost alpine in appearance. The western slope of Mount Brandon presents a huge contrast from its eastern side, as it largely escaped the gouging effect of the glaciers, with the result that it presents an almost unbroken grassy slope.

The glen on the mountain's east side is a series of rock steps, each of which includes a small Paternoster lake. There at least ten of these lakes, which grow in size as one descends the mountain. From highest to lowest (and smallest to biggest) they are the Locha Chom an Chnoic (Coumaknock Loughs), Loch na Lice (Lough Nalacken) and Loch Cruite (Lough Cruttia).