Sinkholes Tellus Border Earthquake - Geological Survey of Ireland
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 />
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