Glaciation ❄️ Flashcards
When was the last Ice Age?
About 18,000 years ago
Ice Ages have intermittent ..?.. ..?.. These are called ‘..?..’
Ice Ages have intermittent WARM PERIODS. These are called ‘INTERGLACIALS’
What is the definition for: GLACIER?
GLACIERS are slow moving ‘rivers of ice’
Give an example of a glacier in Europe!
An example of a glacier in Europe is: Mer de Glace, France
What is the definition for: ICE SHEETS?
These are the large areas of thick ice found in Antarctica and Greenland
What is the definition for: ICE CAPS?
These are smaller areas of thick ice
What is the definition for: CREVASSES?
These are cracks in the ice
What’s does the GLACIER SYSTEM consist of?
Inputs, transfers (flows), stores and outputs
What are INPUTS?
INPUTS come from avalanches along the sides of the glacier but mainly from precipitation as snow.
Explain STORAGE!
Over time snow accumulates and is compressed into ice. The water held in STORAGE is the glacier
Under the force of gravity, the glacier ..?.. downhill
Under the force of gravity, the glacier FLOWS downhill
Explain OUTPUTS!
Meltwater is the main OUTPUT from the glacier, along with some evaporation
Explain the balance between INPUTS and OUTPUTS!
In winter: - inputs usually exceed outputs
near the head of a glacier.
(accumulation)
- Here the glacier advances.
In Summer: - Outputs will exceed inputs
(ablation)
- Here the glacier retreats.
What are most of the world’s GLACIERS doing today?
They are retreating
Summarise the first process in the glacier system: Frost Shattering!
-Water fills small cracks in the rock.
-At night (0-) the water in the cracks
freezes.
-When it warms up again (daytime) the frozen
water thaws.
-This process is repeated many many time
causing more cracks to start appearing in
the rock.
-This process is called FROST SHATTERING or FREEZE THAW WEATHERING.
Explain/ summarise the second process in the glacier system: Abrasion!
The material frozen into the glacier scours the valley sides and base. This is sand-papering effect, similar to corrasion by a river but on a much larger scale.