Glaciers Flashcards
Characteristics of glacial environments
Snow and ice covering most of the landscape.
Consistently low temperatures.
Development of significant amounts of snow and ice led to formations of glaciers.
Glaciers radiated from the north and west and carved deep glacial valleys and troughs.
What is an ice age ?
A period of long-term cooling of the Earth’s atmosphere, resulting in an expansion of ice sheets and glaciers.
Glacial abrasion
The sandpaper effect caused by the weight of the ice scouring the valley floor. It leaves a smooth, polishes surface. Scratches called striations caused by large rocks beneath the ice can often be seen.
Plucking
When the meltwater beneath the glacier freezes and bonds the base of the glacier to the rocky surface below, like glue. As the glacier moves, loose fragments of rock will be ‘plucked’ away. This leaves behind a jagged, rocky surface.
Basal slip
Where meltwater acts as a lubricant to the glacier, enabling it to move downhill. This can be sudden and occurs more in summer months.
Glacial rotational slip
Where ice moves along a curved surface to enlarge + develop hollows.
Internal deformation
In winter, the glacier becomes frozen to the rocky surface. The weight of the ice and the influence of gravity causes individual ice crystals to change shape in a plastic-like way. This causes the glacier to move downhill.
Bulldozing
Renewed further movement of the glacier pushes depositional material downhill. The buildup of sediment can form a hummock, which is a small mound of sediment.
Where is deposition of material carried in the glacier found ?
The snout
What causes glacial deposition ?
Constant transport of new, debris-laden ice into lowland areas results in deposition of all the eroded and weathered material from the uplands. This is called till.
What is till ?
Poorly sorted debris carried by the ice and dumped when the ice melts. It comprises of a range of particle sizes and tends to be angular, having had little water transport.
What is outwash ?
Carried by meltwater streams - is rounded and well-sorted, with gradually finer materials being deposited with distance away from the ice front.
What is an arete ?
Also known as a free-thaw ridge.
A knife-edged ridge formed when 2 corries develop side by side or back to back. As the 2 corries erode towards each other, a ridge is formed between them.
Eg. Striding edge, Lake District
What is a hanging valley ?
A tributary valley that is higher than the main valley.
Formed when a tributary glacier flows from the valley sides towards the main glacial valley.
As the glaciers flowed through the rock on the valley sides, they eroded smaller tributaries into the valley sides, leaving valleys ‘hanging’ over the valley below.
Eg. Nant Lilau, Snowdonia
What is a pyramidal peak ?
A peak formed when 3 or more corries develop on all sides of a mountain.
Eg. Stob Dearg, Scotland
What is a truncated spur ?
A blunt ended, sloping ridge which descends from the flank of a valley.
Formed by the force of a glacier bulldozing through a valley, removing large portions of the valley sides.
Eg. The Devil’s Point, Scotland
What is a glacial trough ?
Before glaciation, a river valley would’ve been v-shaped.
During glaciation, the rock in the valley sides is removed through plucking and abrasion.
This results in a U-shaped valley or glacial trough. It has steep sides and a flat, wide valley floor.
Eg. Glencoe, Scotland
What is a corrie ?
A deep, armchair shaped hollow found on the side of a mountain where a glacier was once found.
When the glacier melts, it leaves a lake called a tarn.
Eg. Red Tarn, Lake District
How is a corrie formed ?
Snow accumulates in a sheltered hollow on a hillside.
Nivation enlarges the hollow enabling more snow to collect.
Gradually, the snow turns to ice and a small corrie glacier is formed.
Through rotational slip, the glacier abrades an over-deepened hollow.
Reduced erosion at the front of the corrie, due to the ice being thinner and less erosive, forms a raised lip.
Sometimes moraine may be deposited here.
A tarn may form in the bottom of the corrie.
What are ribbon lakes ?
Long narrow lakes in glacial troughs.
Formed in the base of the glacial trough once the ice has melted, they may be created in an area of soft rock, where the glacier has eroded this area deeper.
The meltwater sits in the depression and leaves a ribbon lake.
What is a drumlin ?
A small egg-shaped hill, often found on the floor of a glacial trough.
Elongated features that can reach 1km in length, 500m in width, and over 50m in height.
Steep Stoss end, shallow Lee end
How are drumlins formed ?
Formed when the glacier deposits material. As the glacier is carrying so much, it is overloaded and struggles to carry it as it is nearer the end and is melting.
Small obstacles lead to moraine being deposited around them as the ice cannot overcome them and carry material.
The moraine moulds around the obstacle, the blunt end being the deposited material upstream of the ice, and the long tapered end where the ice has flowed over and trailed the moraine with it.
When the ice sheet moves over the material, it shapes it, depending on the direction of ice flow.
What are erratics ?
Rocks that have been transported by ice and deposited elsewhere. This lithology that the erratic is made from is different to the lithology of the bedrock where the erratic is deposited.
What is moraine ?
Deposited material from a glacier