Glaciation Flashcards
What are glaciers?
Masses of ice that fill valleys and slowly move downhill.
They can carve up the landscape through erosion.
What is the history of glaciers in the UK?
Lots of glacial periods during the last 2.6m years.
During some periods, parts of the UK were covered in a massive ice sheet; All Scotland, Wales, Northern Ireland and Northern England.
The erosion, transport and deposition of material by ice has been important in shaping the landscapes in the UK.
How do glaciers erode the landscape as they move?
The weight of the ice moving downhill (known as advancing) erodes in 2 ways:
1) Plucking occurs when meltwater at the base, back and sides freezes onto the rock. As the glacier moves forward it pulls pieces out of the rock.
2) Abrasion is where bits of rock stuck in the glacier grid against the rock below the glacier, wearing it away.
How does the top end of a glacier move?
The ice moves in a circular motion, known as rotational slip. This erodes hollows and deepens them into bowl shapes.
What is freeze thaw weathering?
This is where water gets into cracks, freezes and expands. If this process is repeatedly the rock eventually breaks away.
What are the different landforms produced by glaciation?
1) Arete
2) Corries
3) Ribbon lakes
4) Pyramidal peak
5) Truncated spurs
6) Hanging valleys
7) Glacial troughs
What is an arete?
A narrow steep sided ridge formed when two glaciersflow in parallel valleys. The glaciers erode the sides of the valley and this produces the ridge between the glaciers.
An example is Striding Edge in the Lake District. The steep back wall of Red Tarn corrie lake forms part of the arete.
What is a corrie?
These begin life as hollows containing a small glacier. As the ice moves the rotational slip erodes the hollw into a steep sided armchair shape. when it melts it can leave a small circular lake called a tarn.
An example is Red Tarn in the Lake District. The erosion has left a deep wide hollow that has been filled with water in the post glacial period
What is a ribbon lake?
This is a long thin lake that forms when a glacier retreats. They form in hollows where softer rock erodes more than the surrounding rock.
An example is Lake Windermere in the Lake District and the Scottish Lochs.
What is a pyramidal peak?
It’s a pointed mountain peak with a least three sides. It is formed when three or more back to back glaciers erode a mountain.
An example is Mount Snowdon in Wales.
What is a truncated spur?
These are cliff like edges on the valley side formed when ridges of land (spurs) that stick out of the main valley are cut off as the glacier moves past.
What is a hanging valley?
These are valleys formed by small glaciers that flow into the main glacier. The main glacier is more deeply eroded so when the glaciers melt, the smaller glaciers are left at a higher level.
What are glacial troughs?
Steep sided valleys with flat bottoms. They start as V shaped formed by rivers but then become U shaped when the sides and bottom are eroded.
An example is Keswick in the lake District.
How glaciers transport and deposit Till?
The material is frozen in the glacier, carried on its surface or pushed (bulldozing) in front of it.
It is deposited when the ice melts, by dropping it on the valley floor. It can make moraines and drumlins.
Deposits are all mixed up together, all sizes and shapes. This is different than a river that sorts.
Sometimes the sand and gravel get washed in front by meltwater streams. The streams sort by size and deposit it in layers (called outwash) in front of the glacier.
What are the different types of morraine?
1) Lateral - a long mound of till deposited where the side of the glacier was. Formed when valley walls are eroded and carried along the sides of the glacier.
2) Medial - a long ridge of till deposited along the centre of a valley floor. When two valleys meet the lateral morraines meet and form a line of material.
3) Terminal - builds up at the snout of the glacier. Material that’s abraded and plucked from the valley floor is transported at the front and then deposited as semicircular mounds as the ice retreats.
4) Ground morraine - eroded is dragged along the base of the glacier and is deposited over a wide area on the valley floor as the ice melts.