3.1.4.4 Fluvioglacial Landforms Flashcards
What is produced when glaciers melt to transport a lot of debris
Huge quantities of meltwater
What are meltwater streams like
Often flow under pressure so have high velocity + turbulent flow.
Can pick up + transport a larger amount of material than normal rivers can
What causes meltwater to deposit material
What’s this material like when it’s deposited
It’s discharge decreasing causing energy loss
Heavier particles are dropped first so material is sorted. Can also be found in layers due to seasonal variations in meltwater flow
Describe a fluvioglacial landscape
- Meltwater
- wide multi-channelled (braided) river flowing over a vast area of 2 types of sediment
- very dynamic landscapes with river channels migrating + changing course
2 types of sediment in a fluvioglacial landscape
Poorly sorted angular glacial till
Well sorted more rounded out wash (sandy/gravelly)
2 fluvioglacial landforms due to erosion
Meltwater channels
Proglacial lakes + overflow channels
Describe meltwater channels
When glacial ice melts, it’s water forms streams of meltwater
It flows through tunnels underneath the glacier before running out of the snout
Why do meltwater streams cause more erosion than rivers
4 types of erosion
Due to the ice’s pressure causing meltwater to flow very quickly
Abrasion
Attrition
Solution
Hydraulic action
How do meltwater channels form
Meltwater streams form deep troughs in the landscape called meltwater channels.
As meltwater streams have a lot of erosive power, the meltwater channels produced are very wide + deep
Describe proglacial lakes + overflow channels
During deglaciation, lakes develop on edges of ice, some occupying large areas
Overflows that cross lowest points for the watersheds will create new valleys
When the ice dimming these meltwater lakes melts, many new valleys are left dry
What was the huge proglacial lake formed as ice blocked the River Severn valley
Lake lapworth
How did the river Severn and lower Severn form one
What did it form in the process
Lake lapworth eventually overflowed the water shed to the south to join the lower Severn and when it retreated back north, the route was blocked by glacial deposits
Formed a gorge in the process
4 fluvioglacial landforms due to deposition
Eskers
Kames
Kettle holes
Outwash plains (sandur)
What are eskers
Long sinuous (winding) ridges of material running in direction of ice advance 5-20m high
What do eskers consist of
Sorted coarse material (coarse sands and gravel)