3.1.4.4 Fluvioglacial Landforms Flashcards

1
Q

What is produced when glaciers melt to transport a lot of debris

A

Huge quantities of meltwater

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What are meltwater streams like

A

Often flow under pressure so have high velocity + turbulent flow.
Can pick up + transport a larger amount of material than normal rivers can

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

What causes meltwater to deposit material

What’s this material like when it’s deposited

A

It’s discharge decreasing causing energy loss

Heavier particles are dropped first so material is sorted. Can also be found in layers due to seasonal variations in meltwater flow

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Describe a fluvioglacial landscape

A
  • Meltwater
  • wide multi-channelled (braided) river flowing over a vast area of 2 types of sediment
  • very dynamic landscapes with river channels migrating + changing course
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

2 types of sediment in a fluvioglacial landscape

A

Poorly sorted angular glacial till

Well sorted more rounded out wash (sandy/gravelly)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

2 fluvioglacial landforms due to erosion

A

Meltwater channels

Proglacial lakes + overflow channels

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Describe meltwater channels

A

When glacial ice melts, it’s water forms streams of meltwater
It flows through tunnels underneath the glacier before running out of the snout

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Why do meltwater streams cause more erosion than rivers

4 types of erosion

A

Due to the ice’s pressure causing meltwater to flow very quickly

Abrasion
Attrition
Solution
Hydraulic action

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

How do meltwater channels form

A

Meltwater streams form deep troughs in the landscape called meltwater channels.

As meltwater streams have a lot of erosive power, the meltwater channels produced are very wide + deep

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Describe proglacial lakes + overflow channels

A

During deglaciation, lakes develop on edges of ice, some occupying large areas
Overflows that cross lowest points for the watersheds will create new valleys
When the ice dimming these meltwater lakes melts, many new valleys are left dry

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

What was the huge proglacial lake formed as ice blocked the River Severn valley

A

Lake lapworth

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

How did the river Severn and lower Severn form one

What did it form in the process

A

Lake lapworth eventually overflowed the water shed to the south to join the lower Severn and when it retreated back north, the route was blocked by glacial deposits
Formed a gorge in the process

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

4 fluvioglacial landforms due to deposition

A

Eskers
Kames
Kettle holes
Outwash plains (sandur)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

What are eskers

A
Long sinuous (winding) ridges of material running in direction of ice advance
5-20m high
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

What do eskers consist of

A

Sorted coarse material (coarse sands and gravel)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

How do eskers form

A

Stream’s channel is restricted by ice walls causing hydrostatic pressure allowing a large load to be carried

Load builds up the bed of the channel above surrounding land/close to the snout the hydrostatic pressure may drop leading to deposition

17
Q

When is a ridge left during esker formation

A

When the glacier retreats during deglaciation

18
Q

What are kames

A

Mounds of fluvioglacial material
Deltaic deposits left when meltwater flows into a lake dammed up in front of the glacial snout by recessional moraine deposits

19
Q

What are the 3 types of kame

A

Kame terrace
Kame delta
Crevasse kame

20
Q

What’s a kame terrace

A

Most extensive kame
Results from infilling of a marginal glacial lake
When ice melts the kame terrace is abandoned as a ridge of valley side

21
Q

What’s a kame delta

A

Smaller feature that forms when a stream deposits material on entering a marginal lake

They form small,mound-like hills on the valley floor + can be identified by deltaic sedimentation characteristics

22
Q

What’s a crevasse kame

A

Kame resulting from fluvial deposition of sediments in surface crevasses
When ice melts they’re deposited on valley floor to form small hummocks

23
Q

What’s a kettle hole

A

Depression in a glaciated lowland area that usually contains a small lake

24
Q

How do kettle holes form

A

Results from blocks of ice that get detached from the icefront as the glacier retreats
These blocks get covered in glacial + fluvioglacial debris and slowly melt
As they disappear a hollow is produced on the site which later fills with water

25
Q

What’s an outwash plain (sandur)

A

An extensive, gently sloping area of sands + gravel formed in front of a glacier

26
Q

How are outwash plains (sandur) formed

A

Result from outwash of material carried by meltwater streams + rivers. At the end of a glacial period, huge quantities of meltwater will be spread out over the outwash plain.

27
Q

What season are more outwash plains formed

A

Summer (more melting)

28
Q

What distance are the coarsest material and finest material (clay) found at in outwash plains

A

Coarsest - travels shortest distance so is found near to glacier
Finest - carrier further across the plain before being deposited