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Additional
Inliers and outliers (geology)
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Inliers and outliers (geology)
An
inlier
is an area of older
rocks
surrounded by younger rocks. Inliers are typically formed by the
erosion
of overlying younger rocks to reveal a limited
exposure
of the older underlying rocks.
Faulting
or
folding
may also contribute to the observed
outcrop
pattern. A classic example from
Great Britain
is that of the inlier of folded
Ordovician
and
Silurian
rocks at
Horton in Ribblesdale
in
North Yorkshire
which are surrounded by the younger flat-lying
Carboniferous Limestone
. The location has long been visited by
geology
students. Another example from
South Wales
is the
Usk Inlier
in
Monmouthshire
where Silurian age rocks are upfolded amidst
Old Red Sandstone
rocks of
Devonian
age.
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