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Sinkholes Tellus Border Earthquake - Geological Survey of Ireland

Sinkholes Tellus Border Earthquake - Geological Survey of Ireland

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Geology Matters: Summer 2013<br />

Bedrock collapse dolines are<br />

caused by collapse <strong>of</strong> bedrock<br />

into an underlying void. They are<br />

commonly due to the collapse<br />

<strong>of</strong> the ro<strong>of</strong> <strong>of</strong> a cave and can<br />

be catastrophic. Although<br />

solution is a significant process<br />

driving the creation <strong>of</strong> these<br />

dolines, they are principally<br />

due to mechanical processes,<br />

although the collapse must be<br />

preceded by sufficient solution<br />

<strong>of</strong> the bedrock to form a void<br />

into which the material can fall<br />

(Williams, 2004a).<br />

They can also be caused by<br />

lowering <strong>of</strong> the water table<br />

removing buoyant support.<br />

They are usually characterised<br />

by a high depth to width ratio and<br />

vertical bedrock sides, although<br />

in time they may degrade and<br />

infill. These are less common<br />

in <strong>Ireland</strong>.<br />

Bedrock collapse Doline Formation (Jennings 1985)<br />

Pollelva doline in Co. Clare.<br />

Photo: Colin Bunce, Clare Caving Club<br />

page 21

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