Glaciation ❄️ Flashcards
(40 cards)
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.
Explain/ summarise the third and final process of the glacier system: Plucking!
The water at the bottom of the glacier freezes onto the rock on the valley base. As the glacier moves, the Rick is pulled away from the valley base. Plucking mainly occurs when the rock is well-jointed.
Explain/ summarise a CORRIE:
-Snow collects in a natural hollow on the side of a mountain.
-Overtime more snow gals into the hollow, this
extra weight compressing the snow underneath
and turning it to ice.
-The hollow is deepened by abrasion and plucking.
-This leads to an ‘armchair’ shape and causes a
‘rock lip’ to be formed.
Describe an ARÊTE:
An ARÊTE is a very narrow ridge on a mountain and is sometimes described like a ‘knife edge.’
Describe and then give an example of a Pyramidal peak:
A PYRAMIDAL PEAK is an angular sharply pointed mountain peak which results from CORRIE erosion due to multiple glaciers diverging from a central point.
An example of a PYRAMIDAL PEAK is: The Matterhorn in the Alps
Describe a GLACIAL TROUGH/U-SHAPED VALLEY:
This is when glaciers cut distinctive U-SHAPED VALLEYS with a flat floor and steep sides
Describe a TRUNCATED SPUR:
As the valley glacier moves, abrasion and plucking erode the protruding tips of the spurs leaving them truncated
Describe a HANGING VALLEY:
This is a side valley that enters a main valley at a height high above the main valley floor
Describe a MISFIT STREAM:
This is a stream that is too small to have eroded the U-SHAPED VALLEY in which it flows