Glacial Landscapes Flashcards
How was ice a powerful force in shaping landscape of UK?
by glacial processes:
freeze thaw weathering
erosion - abrasion and plucking
movement and transportation - rotational slip and bulldozing
deposition - glaciers depositing sediment
What is Freeze thaw weathering?
provides sediment for glacier to use in erosion
precipitation seeps into rock in side of valley
water freezes and expands by 10%
puts pressure on surrounding rock
repeated freezing and thawing creates expansion and contraction: rock is broken down and becomes angular
Where does Freeze thaw weathering occur?
side of mountains, below snout of glacier
scree becomes stuck in glacier
What is abrasion?
material stuck in bottom glacier grinds away bedrock
scraping action creates a smooth bedrock
long sharp edge rocks cause grooves
What are striations?
long grooves made by sharp rocks in bottom of glacier
What is plucking?
thin layer of melt water at bottom of glacier
when this freezes, glacier sticks to rocks surface
as glacier moves, particles are pulled away
rock becomes angular
for this process to be effective, rock must be weakened in some way, perhaps by freeze thaw weathering
What is rotational slip?
glacier moves into hollow, begins to rotate in semi-circular motion, carving the hole bigger
once glacier melts it forms a lake in the corrie called a tarn
What is a corrie?
hollow formed by rotational slip of a glacier
What is a tarn?
the lake that forms in the corrie?
What is bulldozing?
rocks and debris are moved forward at the front of the glacier by sheer force of the ice
What is glacial deposition?
debris in the glacial environment may be deposited directly by the ice, or by melt water streams. the resulting deposits are called glacial drift
What is an arete?
when two corries are formed next to each other
What is a pyramidal peak?
when three or four corries are formed back to back
What is an erratic?
large boulder moved by glacier and deposited in a different environment
What is a drumlin?
elongated hill formed by streamlined formation of glacial ice sheets across rock debris
-aligned with the flow of ice