6.2: Glacial Deposition, landforms and landscapes Flashcards

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1
Q

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

A

Drumlins

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2
Q

Name the 2 places where moraines form

A
  1. sub glacially
  2. along the margins of a glacier (ice-marginal)
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3
Q

Name the Moraine by its description

A ridge of moraine along the edge of the valley floor

A

Lateral Moraine

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4
Q

Name the Moraine by its description

A ridge of moraine down the middle of the valley floor

A

Medial Moraine

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5
Q

Name the Moraine by its description

A ridge of moraine extending across the valley at the furthest point the glacier reached

A

Terminal Moraine

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6
Q

Name the Moraine by its description

A series of ridges running across the valley behind the terminal moraine

A

Recessional Moraine

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7
Q

Name the Moraine by its description

A ridge of moraine with stones tilted upwards

A

Push Moraine

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8
Q

Name the Moraine by its description

Chaotic jumble of till mounds

A

Hummocky or disintegration moraine (non-linear)

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9
Q

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.

A

Lateral Moraine

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10
Q

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.

A

Medial Moraine

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11
Q

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.

A

Terminal or end moraine

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12
Q

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.

A

Recessional Moraine

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13
Q

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.

A

Push Moraine

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14
Q

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.

A

Hummocky or disintegration moraine (non-linear)

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15
Q

Describe the typical pattern of formation that Drumlins have

A

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

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16
Q

Name this glacial depositional feature by its description

an extensive flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place, depositing the sediments it carried

A

Till Plain

17
Q

Name this glacial depositional feature by its description

it forms as a sheet of well-compacted sediment beneath a glacier, and ranges from several centimetres to many meters in thickness.

A

Lodgement Till

18
Q

Name this glacial depositional feature by its description

till was carried on or near the surface of the glacier and was let down as the glacier melted.

A

Ablation till

19
Q

What can be deduced from the shape and orientation of a drumline

A

The direction of ice flow