Save
Geography paper 1 living world
Glaciation
Save
Share
Learn
Content
Leaderboard
Learn
Created by
Rachael
Visit profile
Cards (17)
Glacial
processes
1. Freezes in
winter
and thaws in
summer
2.
Repeatedly
freezes and thaws
3.
Pieces
of
rock
4.
Freeze
5.
Thaw
weathering
6.
Water
weakens rock
7.
Crack
8.
Scree
slopes
9.
Solid
flows
Glacier movement
Slow movement through internal
deformation
(when downhill due to gravity)
Basal slip
(sliding on a layer of meltwater)
Movement depends on whether
glacier
is frozen to rock or has a layer of
meltwater
Moraine
Material transported by
glacier
Deposition
1.
Glaciers
deposit material when they
melt
2. Most material deposited at
glacier's snout
3. Piles of material left behind are known as
till
or
boulder clay
Outwash
Smaller and finer material carried further away from the
snout
of the glacier by
meltwater
Freeze-thaw weathering
1.
Water
continuously gets into
cracks
and freezes, expanding the cracks
2. Eventually leads to
rock breaking
apart
Glacial erosion
1.
Abrasion
as glacier moves
downhill
, rocks and pebbles embedded in base and sides scrape along land
2. Plucking as
glacial meltwater freezes
and sticks to rocks, pulling them
away
from land
Corrie
Snow collects in small
hollow
on mountainside, compacted over time into
ice
Rotational slip, plucking,
abrasion
and
freeze-thaw
weathering enlarge the hollow
Arête
Sharp
knife-like ridge formed by corries eroding back by processes of
erosion
and freeze-thaw weathering
Pyramidal
peak
Pointed mountain peak formed when three or more corries form, eroding back to meet at a central point
Truncated spur
Steep-sided
valley created when a
glacier
erodes through the interlocking spurs of an old river
valley
Glacial
trough
U-shaped
valley widened and
deepened
through glacial processes
Ribbon lake
Long
thin
lake found in glaciated valleys, formed in places where the glacier had more
erosive
power
Hanging
valley
Valley created by a tributary connected to the main
glacier
, often smaller as less
erosion
occurred
shaped
valley
Wide valley carved out by
glaciers
, with steep sides and a
flat
floor
Misfit
streams meander through the flat wide U-shaped
valley
floor, not having
eroded
much after the larger glacier had formed the
valley
Glacial transportation
1. Rocks plucked from bottom and sides are moved
downhill
2. Bulldozing as rocks and debris are pushed
downhill
by
sheer force
of moving ice