Quaternary deposits and features Flashcards

(30 cards)

1
Q

Where do most corries form? Why?

A

NE face of mountains

North face because it is colder, so there is more snow and less melting. The South face gets the most sun (it rises in East and sets in West so the whole face gets it too) so snow cannot be supported, there will be less of it and there will be more melting.
East side because the prevailing wind is from the South West, so the wind will blow the snow away from the West side of the mountain.

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

What are the characteristics of an unconsolidated deposit?

A

Sediments that are not stuck together
Also known as drift

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

What are the characteristics of a glacial deposit?

A
  • angular
  • poorly sorted
  • structureless (no stratification)
  • no alignment
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What are the characteristics of a fluvioglacial deposit?

A
  • sub rounded
  • stratified
  • right angles to the direction of flow
  • more sorted
  • imbrication
  • indicates a paleocurrent
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

What are the characteristics of a periglacial deposit?

A
  • dominated by freeze-thaw
  • permafrost
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

What are the characteristics of an interglacial deposit?

A
  • plants (peat)
  • beach
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

In what order are the deposits from the ablation of a glacier arranged?

A

Till
Outwash
Head
Peat

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

What are the glacial depositional landforms?

A

DRUMLINS
MORAINES:
- lateral
- medial
- end
- terminal

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

What is the

a) shape
b) orientation
c) texture
d) location

of a lateral moraine?

A

a) long and thin
b) parallel to the glacier
c) poorly sorted
d) side

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

What is the

a) shape
b) orientation
c) texture
d) location

of a medial moraine?

A

a) long and thin
b) parallel to the glacier
c) poorly sorted, angular, no orientation, no stratification
d) middle

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

What is the

a) shape
b) orientation
c) texture
d) location

of end moraines?

A

a) long and thin
b) perpendicular to the glacier
c) poorly sorted, angular, no orientation, no stratification
d) end middle

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

What is the

a) shape
b) orientation
c) texture
d) location

of a drumlin?

A

a) egg shaped with a tapering end/tail
b) parallel to the glacier
c) angular, alignment, no stratification
d) middle

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

What is the difference between end moraine and terminal moraine?

A

End moraines are the series of moraines deposited as the glacier retreats and advances, whereas the terminal moraine is the last one

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

What are lacustrine deposits?

A

sedimentary deposits formed in lakes (glacial lakes)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

How do lacustrine deposits form?

A
  • glacial lakes are a temp. feature of the natural landscape, forming at the end of a glacial when ice sheets melt away then remain during the following climatic episode
  • in time, they may become infilled with sediment from inflowing streams and rivers, and organic material (e.g. plants) grow along their margin
  • deposits are often thinly flat-laminated, each lamination varying in grain size relating to the strength of water currents entering the lake
  • strong currents = coarser sediment, weaker currents = finer sediment`
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

What are varves?

A
  • glacial lake deposits
  • thin layers of clay and silt of contrasting colour and texture which represent the deposit of a single year (summer and winter) in a lake
  • the layers can be measured to determine the chronology of glacial sediments

SUMMER = meltwater, higher energy flowing into the lake
WINTER = glaciation. no meltwater. The clay in suspension settles out

17
Q

What are fluvioglacial deposits?
Give the fluvioglacial deposits

A

Deposits relating to meltwater produced by a glacier

  • eskers
  • kames
  • outwash plains
18
Q

Where can meltwater from a glacier (then used in fluvioglacial deposits) come form?

A
  • ablation (summer)
  • subglacial pressure melting
  • precipitation
  • retreating glacier/deglaciation
19
Q

How does an esker form?

What do they show?

A
  1. meltwater that flows at the base of an ice sheet carves itself a winding channel or ice cave in which to flow
  2. during summer lots of material is carried which is deposited as the flow slows
  3. sands and gravels are deposited on the floor of the cave so that after the ice has gone a ridge of sand and gravel winding over the outwash plain remains

They can show the general trend of meltwater and ice movement by their orientation
- you can also see stratification in them because they are built up seasonally

20
Q

What are the other names for outwash plains?
What are outwash plains?

A

Sandur/proglacial plains
- area in front of the glacier made up of a mixture of sediments that have been washed out of the glacier

21
Q

What are the types of deposits?

A

Glacial
Fluvioglacial
Lacustrine

22
Q

What is a periglacial landscpe?

A

a very cold but not glaciated area around the edges of a glacial landscape characterised by intense cycles of freezing and thawing

23
Q

What are the features of a periglacial landscape?

A

Permafrost
Ice wedge
Ice wedge cast
Solifluction
Head

24
Q

What is permafrost?

A
  • permanently frozen ground
  • in the summer the temperatures may increase enough to allow melting of the top portion of the soil to take place
  • the soil below remains permanently frozen - this frozen portion is the permafrost layer; it is impermeable
  • the top layer of the soil, when it thaws in summer, becomes saturated and mobile - the active layer
25
What is an ice wedge?
- common periglacial landform formed in areas with permafrost where freezing and thawing cause the ground to crack - water enters these cracks and freezes, expanding and widening them over time
26
What is an ice wedge cast?
- RELICT FEATURES - fossil ice wedges created as the ice wedges melt and the cracks remaining are filled with silts and sands left by the meltwater and when surrounding sediments collapse into the void left by the ice - contains sediments which are clearly different from the surrounding material as they are often well-bedded sands which are wind blown deposits
27
What is solifluction?
the slow, viscous, downslope flow of waterlogged soil and other unsorted and saturated superficial deposits - non-frozen version of gelifluction (= over impermeable permafrost layer) - produces solifluction lobes
28
What is a head deposit?
weathered material moved by solifluction, containing material produced by frost shattering of the bedrock, so tends to be of one rock type - angular like till, but also tends to show alignment
29
What is a) an interglacial b) the deposit
a) where the climate warms and the tundra recedes polewards following the ice sheets. Forests return to areas that once supported tundra vegetation b) Peat
30
What is peat?
an accumulation of plant material, partially decomposed under anoxic conditions in stagnant water or waterlogged ground - formed in interglacials in lowland poorly draining sites or at altitude where precipitation is high - deposits may become eroded resulting in large 'rafts' being carried some way downstream before being redeposited - the peat may have been part of a warm stage deposit or represent a warm interval in an otherwise cold sequence