MacGillycuddy's Reeks
MacGillycuddy's Reeks
Main page
2246305

MacGillycuddy's Reeks

logo
Community Hub0 subscribers
2246305

MacGillycuddy's Reeks

logo
Community Hub0 subscribers
What are your thoughts?
Be the first to start a discussion here.
Be the first to start a discussion here.
MacGillycuddy's Reeks

MacGillycuddy's Reeks (Irish: Na Cruacha Dubha, meaning 'the black stacks') is a sandstone and siltstone mountain range in the Iveragh Peninsula in County Kerry, Ireland. Stretching 19 kilometres (12 miles), from the Gap of Dunloe in the east, to Glencar in the west, the Reeks is Ireland's highest mountain range, and includes most of the highest peaks and sharpest ridges in Ireland, and the only peaks on the island over 1,000 metres (3,300 feet) in height.

Near the centre of the range is Carrauntoohil, Ireland's highest mountain at 1,038.6 metres (3,407 ft). The range was heavily glaciated which carved out deep corries (e.g. the Eagle's Nest), U-shaped valleys (e.g. Lough Coomloughra), and sharp arêtes and ridges (e.g. the Beenkeragh Ridge).

The range, part of the Reeks District, is a destination for mountain walkers and climbers and includes some of Ireland's most regarded walking routes such as the 15–kilometre (10 mile) Coomloughra Horseshoe, and the 26-kilometre (16 mile) MacGillycuddy's Reeks Ridge Walk that traverses the full range; it is estimated that over 140,000 people visit the range each year. The entire range is in private ownership; however, reasonable access is given for recreational use.

MacGillycuddy's Reeks are composed of sandstone particles of various sizes, which are collectively known as the Old Red Sandstone. The rocks date from the Upper Devonian period (310–450 million years ago) when Ireland was in a hot equatorial setting. During this 60 million year period, Ireland was the site of a major basin, known as the Munster basin, and the counties of Cork and Kerry were effectively a large alluvial floodplain. Chemical oxidation stained the material with a purple–reddish colour (and green in places from chlorination), still visible today. There are virtually no fossils in Old Red Sandstone. The composition of Old Red Sandstone is variable and contains quartz stones, mudstones, siltstones, and sandstone particles (boulders of conglomerate rock containing quartz pebbles are visible throughout the range). The Reeks were also subject to significant glaciation which led to fracturing of the rock, and resulted in deep corries (e.g. the Eagle's Nest), U-shaped valleys (e.g. Lough Coomloughra), and sharp arêtes and ridges (e.g. the Beenkeragh Ridge).

MacGillycuddy's Reeks are variously described as consisting of two main sections, containing all ten of the Reeks that are above 3,000 ft:

The Eastern Reeks meet the Coomloughea Reeks at the col of the Devil's Ladder, a popular ascent route for Carrauntoohil.

MacGillycuddy's Reeks contains the three peaks in Ireland which are over 1,000 metres (3,300 feet) in height, namely: Carrauntoohil, Ireland's highest mountain at 1,038.6 m (3,407 ft), followed by Beenkeragh at 1,008 m (3,307 ft) and Caher at 1,000 m (3,300 ft).

The range contains eleven of the fourteen peaks in Ireland that are over 3,000 ft (910 m) in height, and meet the Vandeleur-Lynam classification of a mountain—peaks with a prominence over 15 m (49 ft). All but one of these eleven 3,000 ft peaks, namely Cnoc an Chuillinn East Top, are amongst the list of thirteen Irish Furths—peaks which meet the Scottish Mountaineering Club's criteria for a Munro, and they are therefore also known as Irish Munros.

See all
User Avatar
No comments yet.