Difference between revisions of "Great Sugar Loaf"

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The '''Great Sugar Loaf''' is a mountain in east [[County Wicklow]] in [[Ireland]].
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The '''Great Sugar Loaf''' is a mountain in the east of [[County Wicklow]].
  
 
This hill is also known as the '''Big Sugar Loaf''' and often as simply the '''Sugar Loaf''',and in Gaelic is named ''Ó Cualann'' or ''Beannach Mhór'' or, anciently, ''Sliabh na Gealta''.<ref>'A Week at Killarney' by Samuel Carter Hall, p. 56</ref>)
 
This hill is also known as the '''Big Sugar Loaf''' and often as simply the '''Sugar Loaf''',and in Gaelic is named ''Ó Cualann'' or ''Beannach Mhór'' or, anciently, ''Sliabh na Gealta''.<ref>'A Week at Killarney' by Samuel Carter Hall, p. 56</ref>)

Latest revision as of 08:55, 24 January 2019

Great Sugar Loaf
County Wicklow
IMG GreatSugarLoaf1038c.jpg
The Great Sugar Loaf, from the west
Range: Wicklow Mountains
Summit: 1,644 feet O237130
53°9’18"N, 6°9’0"W

The Great Sugar Loaf is a mountain in the east of County Wicklow.

This hill is also known as the Big Sugar Loaf and often as simply the Sugar Loaf,and in Gaelic is named Ó Cualann or Beannach Mhór or, anciently, Sliabh na Gealta.[1])

Geography

The mountain is located between Delgany and Kilmacanogue, and just to the north of the Glen of the Downs Nature Reserve. The smaller Little Sugar Loaf lies to the east (on the other side of the N11 road.

Though only 1,644 feet high, the Great Sugar Loaf's isolation from other hills, steep slopes and volcanic appearance makes it stand out in the landscape. Due to its height relative to the surrounding landscape, the hill qualifies as a 'Marilyn'.

Geology

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.

Gallery

Outside links

Commons-logo.svg
("Wikimedia Commons" has material
about Great Sugar Loaf)

References

  1. 'A Week at Killarney' by Samuel Carter Hall, p. 56