6.2: Glacial Deposition, landforms and landscapes Flashcards
Name this glacial depositional feature by its description
oval-shaped hills, largely composed of glacial drift, formed beneath a glacier or ice sheet and aligned in the direction of ice flow
Drumlins
Name the 2 places where moraines form
- sub glacially
- along the margins of a glacier (ice-marginal)
Name the Moraine by its description
A ridge of moraine along the edge of the valley floor
Lateral Moraine
Name the Moraine by its description
A ridge of moraine down the middle of the valley floor
Medial Moraine
Name the Moraine by its description
A ridge of moraine extending across the valley at the furthest point the glacier reached
Terminal Moraine
Name the Moraine by its description
A series of ridges running across the valley behind the terminal moraine
Recessional Moraine
Name the Moraine by its description
A ridge of moraine with stones tilted upwards
Push Moraine
Name the Moraine by its description
Chaotic jumble of till mounds
Hummocky or disintegration moraine (non-linear)
Name the Moraine by its formation
Exposed rock on the valley side is weathered and fragments fall down on to the edge of the glacier. This is then carried along the valley and deposited when the ice melts. Parallel to ice flow.
Lateral Moraine
Name the Moraine by its formation
When two valley glaciers converge, two lateral moraines combine to form a medial moraine. Material is carried and deposited when melting occurs. Parallel to ice flow.
Medial Moraine
Name the Moraine by its formation
Advancing ice carries moraine forward and deposits it at the point of maximum advance when it retreats. The up-valley (ice contact) side is generally steeper than the other side as the advancing ice rose over the debris. Transverse to ice flow.
Terminal or end moraine
Name the Moraine by its formation
Each recessional moraine, and there may be many, represents a still-stand during ice retreat. They are good indicators of the cycle of advance and retreat that many glaciers experience. Transverse to ice flow.
Recessional Moraine
Name the Moraine by its formation
Any morainic material at the glacier snout will be pushed forward during advance. The faster the velocity of advance, the steeper the angle of tilt or stones. Transverse to ice flow.
Push Moraine
Name the Moraine by its formation
Originally considered a product of ice stagnation and dropped from a debris-rich glacier, now associated with active glacial retreat. Limited orientation.
Hummocky or disintegration moraine (non-linear)
Describe the typical pattern of formation that Drumlins have
They usually range from 10 - 50 meters high and 20 to 2000 meters long
they usually occur in ‘swarms’
they are typically found in lowland areas