Geology of the catchement areas of the Glencullen, Lug Duff, Avoca and Campus rivers.

Jun 30th, 2015
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The Clencullen river - The Clencullen river rises in the wicklow mountains at Tibradden. It flows in a south easterly direction through Glencullen to Enniskerry where it becomes the Cookstown river. It meets the Dargle river just north of Kilcroney which continues northeastwards meeting the Irish sea at Bray harbour. (Grid refs to be added).

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Geology of the catchement areas of the Glencullen, Lug Duff, Avoca and Campus rivers.The Clencullen river The Clencullen river rises in the wicklow mountains at Tibradden. It flows in a south easterly direction through Glencullen to Enniskerry where it becomes the Cookstown river. It meets the Dargle river just north of Kilcroney which continues northeastwards meeting the Irish sea at Bray harbour. (Grid refs to be added).The bedrock over which the Glen Cullen river flows is predominantly Granite, part of the Leinster Granite Batholith. This is the largest batholith in Ireland and Britain and forms the core of the Wicklow mountains. It comprises 5 plutons which intruded simultaneously during the Acadian orogeny. The Glen Cullen river flows across the Northern Pluton (which extends over an area of approximately 440 km2 extending from Dun Laoghaire southwestwards to the Wicklow Gap

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