Glaciation Flashcards
What is a glacier?
A glacier is a large body of ice which moves down a valley (which is usually sheltered from the sun) which it has mostly carved out itself.
How do glaciers form?
- Glaciers form when snow and ice do not completely melt before next years snowfall.
- This usually occurs in shaded areas between tall peaks at high altitudes where it is cooler.
- As the depth and weight increases, the bottom layers compress and crystallise.
What is moraine?
Lines can appear when two glaciers come together, causing transported material called moraine on the sides of the glaciers to merge between the two.
What are accumulation / ablation?
Accumulation:
- A zone where a glacier gains ice.
Ablation:
- A zone where a glacier loses ice.
How does a glacier move?
- At the top of a mountain, temperatures are cold and so snow accumulates, getting deeper and deeper.
- This adds weight to the glacier causing it to eventually slide downhill.
- As it gets lower, the temperature increases, and so ablation occurs through:
- Sublimation = when a solid turns to gas.
- Icebergs = if a glacier runs into a lake, icebergs break off into the lake.
- Melting = can occur if temperatures are very high.
What causes a glacier to move faster?
- Once a glacier is thick enough, the heat from the core of the Earth as well as the increased pressure from the extra weight causes the base of the ice to melt.
- This forms a layer of liquid water, causing the glacier to move very quickly.
What type of flow does a glacier have?
Plastic Flow:
- Shear stresses within the glacier cause the ice crystals to change shape, producing gentle flow through the shear deformation of ice.
What are the differences between warm and cold based glaciers?
Warm (water) based:
- The whole glacier will slide in a basal slip because the shear strength is low at the base.
Cold (frozen) based:
- The glacier cracks and folds as the base is frozen to the ground meaning the particles at the bottom do not move.
How can you tell if a glacier is advancing/retreating?
Advancing glacier:
- The ground ‘in front’ of the glacier will have vegetation on it.
- The ‘front’ of the glacier will be very steep and jagged.
Retreating glacier:
- The ground ‘in front’ of the glacier will be made up of exposed moraine material.
- The ‘front’ of the glacier is a gentle slope.
- Overall the glacier is moving downwards but is being dominated by melting.
What is an ice cap?
- An ice cap is a glacier where so much snow and ice accumulate that the weight of it pushes downwards on the continental crust.
- Eventually, when the snow and ice melt, this continental crust fills with water.
- After this, an isostatic rebound will occur where the continental crust rises again to become exposed ground surface.
What are the types of moraine?
End moraine:
- Found at the ice front.
Terminal moraine:
- Found at the ice front marking the farthest advance of ice.
Lateral moraine:
- Found along the edge of a glacier where it scrapes the side walls of the valley.
Medial moraine:
- Found when two glaciers merge, joining their lateral moraine.
Ground moraine:
- Found beneath the ice as a layer of glacial debris.
What are striations?
Lines produced when accumulated rocks (that are being driven along by the ice that they are frozen into) gouge a groove into the rocks that a glacier moves over.
What types of valley do glaciers produce?
Glaciers erode around their whole perimeter meaning very large u-shaped valleys are produced.
How are crevices formed?
When a glacier moves around corners or over bumps, they change direction, forming deep cracks called crevices.
What happens when a glacier moves over a drop?
Lots of moraine is deposited at the bottom of the drop, leading to an accumulation of different sediments.
How is end moraine deposited?
It is deposited at the end of a glacier where the stream doesn’t have enough energy to transport materials.
What is a drift?
The material left at the front of a glacier.
What is outwash?
Material which is transported by the melted ice.
What are the features of a post-glacial landscape?
- V-shaped valleys are generated by rivers, typically producing rounded mountain profiles.
- The glaciers then fill the whole of these valleys, scouring out the entire valley side, producing a U-shaped valley.
- Tributary glaciers join the main glacier meaning erosion comes to a halt, producing a hanging valley with a waterfall somewhere up the side of the main valley.
- This waterfall then gradually cuts a V-shaped valley into the tributary U-shape valley.
- This forms sharp aretes between two adjacent glaciers.
What are fjords?
A fjord is an in-field depression where a glacier has previously been eroding away.
- Ice bergs which have been carved off of the glacier float away and continue to erode the valley deeper and deeper.
- However, once they reach the sea, erosion stops and so the fjords are much deeper than the sea itself.
- If the sea level falls, land locked lakes are formed.
How can a series of lakes be produced?
A series of lakes may be produced in the bottom of a U-valley where bands of end-moraine result in damming of the valley.
Quick Clay, The Rissa Landslide, Norway (Case study)
- Deposits of marine clay were built upon on a farm in Norway.
- The earth removed to build a basement was placed on the edge of the fjord.
- The load produced by this earth fill caused the shoreline to slide into the lake and disappear.
- Each new slide resulted in a complete liquefaction of the quick clay.
What are the effects of an ice sheet?
If an entire area is covered by an ice sheet, everything gets smoothed over by the ice of the glacier and so the hills are small and rounded.
How are braided meltwater streams produced?
Streams below the glaciers carry lots of sediment which is deposited to form a pattern of water flow.