AQA gcse geography physical landscapes: Lake District glacial landforms

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The document summarizes key landforms of erosion and deposition found in the Lake District, which was affected by past glaciation. It identifies corries, aretes, and troughs as major erosional landforms, such as Red Tarn, Striding Edge, and Grisedale. Depositional landforms discussed include erratics, drumlins formed parallel to glacier flow, and different types of moraines (terminal, lateral, and medial moraines). Ground moraines are also mentioned as piles of varying rock types and sizes.

Lake District - landforms of
glacial erosion & deposition
AQA spec:
an upland area in the UK affected by glaciation to
identify its major landforms of erosion and
deposition.

Lake District - landforms of glacial erosion
Red Tarn - corrie
Striding Edge - arete
Grisedale - trough
n.b. Grisedale ribbon
lake

Lake District - landforms of glacial deposition
ERRATIC - boulders carried by
the glacier and then deposited in
an area of differing rock type. E.g
blocks of dark grit which stand
on the limestone platform at
Norber near Settle
Drumlins - These are smooth mounds of deposited material that are formed parallel to
the direction of the movement of the glacier. Between 30 and 40 m high and up to 500
m long.
A "swarm of drumlins" = usually a number in one single area. Formed by moraine being
deposited due to an obstruction causing an increase in friction or a slowing of the glacier.
Most of the material is deposited at one end of the drumlin,

Different types of moraine
● Terminal moraines are found at the terminus or the
furthest (end) point reached by a glacier.
● Lateral moraines are found deposited along the sides
of the glacier.
● Medial moraines are found at the junction between
two glaciers.
● Ground moraines are disorganised piles of rocks of
various shapes, sizes and of differing rock types.
Lake District - landforms of glacial deposition

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AQA gcse geography physical landscapes: Lake District glacial landforms

1. Lake District - landforms of glacial erosion & deposition AQA spec: an upland area in the UK affected by glaciation to identify its major landforms of erosion and deposition.

2. Lake District - landforms of glacial erosion Red Tarn - corrie Striding Edge - arete Grisedale - trough n.b. Grisedale ribbon lake

3. Lake District - landforms of glacial deposition ERRATIC - boulders carried by the glacier and then deposited in an area of differing rock type. E.g blocks of dark grit which stand on the limestone platform at Norber near Settle Drumlins - These are smooth mounds of deposited material that are formed parallel to the direction of the movement of the glacier. Between 30 and 40 m high and up to 500 m long. A "swarm of drumlins" = usually a number in one single area. Formed by moraine being deposited due to an obstruction causing an increase in friction or a slowing of the glacier. Most of the material is deposited at one end of the drumlin,

4. Different types of moraine ● Terminal moraines are found at the terminus or the furthest (end) point reached by a glacier. ● Lateral moraines are found deposited along the sides of the glacier. ● Medial moraines are found at the junction between two glaciers. ● Ground moraines are disorganised piles of rocks of various shapes, sizes and of differing rock types. Lake District - landforms of glacial deposition

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AQA gcse geography physical landscapes: Lake District glacial landforms

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AQA gcse geography physical landscapes: Lake District glacial landforms