Glaciation Flashcards
What is the cryosphere
Frozen landscapes
What are the deposited glacial landforms?
Till Erratics Crag-and-tails Moraines Drumlins
What are the 4 types of moraines and where do they form?
Medial - Forms in the middle of two glaciers
Lateral - Forms along the sides of glaciers
Terminal - Forms in front of a glacier when it stops advancing
Recessional - Marks an interruption to the glacier’s retreat
What are the 3 types of glacial erosion?
Plucking
Freeze-thaw
Abrasion
Describe the location and formation of drumlins:
Found in large swarms on valley floors in lowland areas.
Moraine material formed into low egg-shaped hills.
Blunt and steep at the stoss end
Gentle and wide at the lee end (Down-glacier end).
Formed by the streamlined movement of glacial ice sheets across rock debris, or till.
What is till?
Glacially transported material, usually made up of sand, mud and gravel-sized material deposited directly from glacial ice.
What are moraines made of?
The build-up of till.
What are the 5 types of glacial movement
Internal deformation Basal Slippage Rotational Flow Extensional Flow Compressional Flow
How does internal deformation work
individual particles of ice melt around their edges allowing air to escape
one by one the particles slip forward on the thin film of water and immediately refreeze, causing momentary movement
internal deformation characteristics
Commonly at the base of the glacier
Very slow movement.
Ice is polycrystalline.
Individual crystals move.
Base of crystal stays still and top moves downhill under gravity.
Creates crevasses on glacier surface
what is basal slippage
The sliding of a glacier over bedrock, a process usually facilitated by the lubricating effect of meltwater.
Occurs when glacier slides over surrounding sediment and rocks.
what is rotational flow
This is a downhill flow of ice which, like a landslide, pivots around a point producing a rotational movement.
describe the process of extensional flow
Extensional flow = gradient increases – velocity increases – lower valley ice moves faster than upper valley (ice runs away with itself) – ice thins and spreads out = cracks/crevasses
describe the process of compressional flow
Compressional flow – gradient reduced – velocity reduced – upper floor ice is pushing on lower valley ice.
what does the rate of movement depend on?
Gravity – steeper the gradient, the greater the pull
Friction – Less friction, more movement
Meltwater – Lubrication of the ground allowing slip
Ice temperature
Ice mass – The heavier it is, the more energy it has to move