Great Sugar Loaf
|This article does not cite any references or sources. (July 2015)|
|Great Sugar Loaf|
The Great Sugar Loaf, from the west
|Elevation||501 m (1,644 ft)|
|Prominence||216 m (709 ft)|
|Topo map||OSi Discovery 56|
Though only 501 metres (1,644 ft) high, the Great Sugar Loaf's isolation from other hills, steep slopes and volcanic appearance makes it appear much taller than it is. Due to its height relative to the surrounding landscape, the hill qualifies as a Marilyn.
The Great Sugar Loaf is composed of Cambrian quartzite, in contrast to the rounded mountains to the west, which are made of Devonian granite. Popularly mistaken for a volcano, it is in fact an erosion-resistant metamorphosed sedimentary deposit from the deep sea.
The Little Sugar Loaf from the summit of the Great Sugar Loaf.
Sunrise over the Great Sugar Loaf, as seen from Glencullen, County Dublin.
The Great Sugar Loaf as seen from Powerscourt Estate.
|Wikimedia Commons has media related to Great Sugar Loaf.|
|This article related to the geography of County Wicklow, Ireland is a stub. You can help Wikipedia by expanding it.|