Glacial Depositional Landforms Flashcards
1
Q
Lateral moraine:
A
- Debris from freeze thaw weathering of the valley sides falls onto a glacier
- It is then transported and deposited at the edge of the glacier where it melts
2
Q
Medial moraine:
A
- At the confluence of two tributary glaciers, the lateral moraine joins to form a medial moraines
- This is then deposited during ice melt and retreat
3
Q
Terminal moraine:
A
-Debris is deposited at the maximum extent of a glacier, especially if the glacier is in equilibrium and the snout is stationary and debris will be continuously supplied to the same place
4
Q
Drumlins:
A
- Formed when the ice becomes overloaded with sediment
- When the competence of the glacier is reduced, material is deposited
- The glacier may have experienced a reduction in its competence for several reasons, including melting of the ice and changes in velocity.
- E.g. when glacier ice becomes overloaded with debris when exiting an upland area
- The deposits are then streamlined and shaped by the moving ice
- Forms steep stoss side and elongated lee side
5
Q
Erratics:
A
- Large pieces of till, usually boulders which are carried by a glacier to a different geographic location to when they originated from
- E.g. huge erratic boulders weighing up to 16,000tonnes were carried 300km from Canadian Rockies to plains of Alberta by Cordilleran Ice Sheet
6
Q
Till Plains:
A
- Formed when a large section of ice detaches from the main body of the glacier and melts
- The suspended debris will be suddenly deposited and form a large plain of unsorted till
7
Q
Lodgement till:
A
- Occurs beneath the ice mass when subglacial debris that was being transported becomes lodged or stuck on the glacier bed
- Friction between the subglacial debris and the bed becomes greater than the drag of the ice moving over it
8
Q
Ablation till:
A
- Material that has been dumped as the glacier melts and thaws
- Can include material that has travelled within the glacier at any point i.e. subglacially, englacially, supraglacially
9
Q
Recessional moraine:
A
- Moraine deposited during temporary readvancement of a glacier when it begins to retreat again
- Indicates which direction the glacier is retreating
- Lies parallel to terminal moraine