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Jc geography
Glaciation
Cirque
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Created by
Agata Szwejda
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One feature of
glacial erosion
is a
cirque.
A cirque is a
basin- shaped hollow
in a
mountain.
A cirque was the
birthplace
of a
glacier
A
cirque
is formed when
snow
accumulates
in a
hollow
high
up
in a mountain. The snow is
compressed
to form
ice
The ice
plucks
rocks from the
sides
of the
mountain
as it begins to
move.
these rocks make the
hollow deeper
through the process of
abrasion
Diagram
of
cirque
The
ice
eventually
overflows
from the hollow and
gravity
causes the ice to move
downhill
The
ice
that is left behind
melts
and forms a lake that is known as a
tarn
E.g the Devils Punchbowl near
Killarney
,
Co. Kerry