Lesson 5 Flashcards

(56 cards)

1
Q

What are the 3 circumstances under which glaciers generally deposit their load?

A
  • When the velocity is reduced
  • When they become overloaded with debris
  • When ablation increases
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2
Q

Why do glaciers deposit their load when velocity is reduced?

A

As the glacier slows down, it has less power to move material

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3
Q

Why do glaciers deposit their load when they become overloaded with debris?

A

The glacier tends to drop things

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4
Q

Why do glaciers deposit their load when ablation increases?

A

The glacier starts melting, leading to material in it being dropped

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5
Q

What is glacial till?

A

Debris underneath the ice

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6
Q

What is the transport of glacial till like?

A

It can be transported hundreds of miles to areas with different geology

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7
Q

What is supraglacial debris?

A

Glacial debris carried on top of the glacier

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8
Q

Where does most supraglacial debris come from?

A

Freeze-thaw action

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9
Q
A
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10
Q

What is englacial debris?

A

Glacial debris located within the glacier

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11
Q

What is subglacial debris?

A

Glacial debris located at the bottom of a glacier

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12
Q

What are erratics?

A

Debris carried by glacier which is made up of a different type of rock to the bedrock it now rests upon

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13
Q

How are erratics carried?

A

Supraglacially

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14
Q

Explain the formation of erratics:

A
  • Rock debris falls onto the glacier due to freeze-thaw or plucking of valley sides
  • It is then transported on/in the glacier
  • It is deposited when ablation increases, so it can no longer carry the weight
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15
Q

How can you tell where erratics have come from?

A

Geology
e.g. erratics found in boulder clay in Northumberland have travelled from Scandinavia

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16
Q

Processes of glacial deposition
What is lodgement till?

A

Subglacial material that becomes lodged in the glacier bed

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17
Q

Give an example of a landform formed by lodgement till:

A

Drumlins

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18
Q

Processes of glacial deposition
What is ablation till?

A

Material dumped by a melting glacier that is no longer able to carry debris

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19
Q

Give an example of a landform formed by ablation till?

A

Terminal moraine

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20
Q

Processes of glacial deposition
What is deformation till?

A

Where weak bedrock is moved by the glacier as it turns to sediment

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21
Q

Give an example of deformation till:

A

Rock flour

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22
Q

Processes of glacial deposition
What is flow till?

A

When high meltwater content causes glacial debris to flow during deposition
Also produces rock flour

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23
Q

Lodgement Till
When does it form?

A

When subglacial debris gets stuck or ‘lodged’ in the bed

24
Q

Lodgement Till
Where can it occur within the ice?

A

Anywhere, generally occurs where subglacial load is high and therefore the erosive ability of the ice is reduced

25
Lodgement Till What are some characteristics?
Compared to ablation till: - More rounded - Less angular - Elongated and orientated to the flow of ice (geology of rocks face the same way)
26
What can both lodgement and ablation till form?
Large flat till plains like the ones found in East Anglia and Minnesota
27
Ablation Till What causes it?
The melting of ice around the debris
28
Ablation Till What sort of sediments does it usually come from?
Supraglacial sediments, derived from freeze-thaw eroded material
29
Ablation Till Where is debris carried?
Into the ablation zone and deposited towards the snout of the glacier
30
Ablation Till What are some characteristics?
Compared to lodgement till: - More angular (less altered by abrasion) - Less spherical - Less compact - Reduced amount of glacial flour
31
Flow Till Due to the high meltwater content, how is material deposited?
Material flows during deposition With so much small material, it can act like a fluid
32
Flow Till How is material carried?
Usually supraglacially
33
Flow Till What are some characteristics?
- Finer - More angular, less spherical - Has evidence of sorting
34
Name the different types of moraines: 6
- Drumlins - Lateral moraines - Medial moraines - Terminal moraines - Recessional moraines - Hummocky moraines
35
What type of features are moraines?
Ice contact features
36
Drumlins What type of till are they primarily made of? What size are they? How do they show ice direction?
1. Primarily made of lodgement till 2. 10-50m high and 200-2000m long 3. They are stoss and lee features - the steeper, blunt end is the stoss end
37
Drumlins How are they formed?
Drumlins form through the deposition of glacial till beneath the glacier. As ice moves over the till, it shapes it into a streamlined mound
38
Drumlins Where are they found?
- They are often found in swarms, forming a basket of eggs topography - They are typically found in lowland areas, often regularly spaced
39
Drumlins What is the elongation ratio about?
The elongation ratio is used to measure the shape: length of drumlin -------------------------- = elongation ratio maximum width Greater elongation suggests a more powerful ice flow
40
Lateral moraines Where do they form?
A lateral moraine forms along the sides of a glacier
41
Lateral moraines How do they form?
As the glacier scrapes along, it tears off rock and soil from both sides of its path This is left at the side of the glacier, forming a lateral moraine
42
Medial moraines Where do they form?
Where 2 tributary glaciers come together
43
Medial moraines Why are they generally not preserved after ice retreats?
They are generally features found on the surface of the ice, consisting of rock that has fallen from a rock wall where the glaciers converged. Due to them being thin and surficial, they are rarely preserved after ice retreats.
44
Terminal moraines What do they mark?
The maximum limit a glacier advanced
45
Terminal moraines How are they formed?
As the glacier accumulates, debris accumulates at the snout. As the glacier ablates, ablation till is added to this snout. When the glacier retreats, the terminal moraine is left behind as a prominent feature.
46
Terminal moraines How is their shape significant?
They mirror the shape of the ice margin at the time of deposition
47
Recessional moraines Where do they form?
They form behind the terminal moraine
48
Recessional moraines How do they form?
Debris accumulates during short-lived phases of glacier advance or a standstill disrupting the general pattern of glacier retreat They may form on a yearly basis in some locations
49
Hummocky moraines How do they form?
Used to be thought it was due to ice stagnation (ice wouldn't move and would drop all its debris without moving when it melted) however its now believed they are polygenetic landforms, forming over multiple ice ages
50
Hummocky moraines What do they look like?
A chaotic pattern of small, irregular mounds, that are typically mounded in shape.
51
Name the ice-marginal moraines
- Lateral - Medial - Terminal - Recessional - Hummocky All linear in topography except for hummocky which are non-linear
52
Give an example of a location with drumlins
Drumlin Belt, Ireland
53
Give an example of a location with lateral moraines
Langdale
54
Give an example of a terminal moraine
Valparaiso moraine
55
Give an example of a recessional moraine
Some in Langdale valley
56
Give an example of hummocky moraines
Coire a'Cheud-chnoic