glacio fluvial landforms Flashcards
what are glacio fluvial landforms
landforms produced by the meltwater from glaciers
what is the deposit produced by glacio-fluvial streams known as
outwash
what are three key characteristics of outwash
- smooth and rounded due to attrition
- sorted horizontally with the largest furthest up the stream
- stratified vertically with distinctive seasonal layers of annual sediment accumulation
how do seasons impact the discharge of glacio fluvial rivers
- in winter months there is minimal discharge so the river will only have energy to carry small material
- in the summer melting season there will be extremely high discharge enabling glacio fluvial rivers to carry large sediment and even boulders
give a specific example of a glacier with discharge significantly influenced by season
-the glacier d’Angentiere, lying perpendicular to Chamonix in france has a winter discharge of 0.1-0.5 cumecs but summer discharge of 10-11 cumecs.
what is a kame
a hill or hummock composed of stratified gravel and sand laid down by glacial meltwater
what are the two types of kames
- delta kames
- kame terraces
describe the two ways in which delta kames can be formed
- some formed by en-glacial streams when the stream exists the glacier at its snout, losing energy and depositing the material
- some are formed by supra glacial streams entering a lake, losing their energy as they enter the static body of water
what are kame terraces
ridges of material running along the valley floor
how are kame terraces formed
supra glacial rivers running along the side of the glacier collect material which is deposited when the glacier retreats
how are kame terraces different from lateral moraines
although they appear simiar, kame terraces are composed of outwash which is smaller, rounder and smoother than material deposited directly from a glacier
give a specific example of kame terraces
kames are widespread in lothian, scotland
what is an esker
-a long sinuous ridge composed of stratified sand and gravel laid down by glacial meltwater
how do eskers form
material is deposited in sub glacial tunnels as meltwater is decreased
what is a secondary theory to the formation of eskers
scientist argue that deposition occurs as material emerges from the glacial snout. as the glacier retreats the snout moves further back resulting in the long ridge.