glaciers
ice shelves
permanent floating sheets of ice connected to a landmass
ice sheet
glacial ice more than 50,000 square kilometres
formation
movement
crevices
ice gets streched/squashed = cracks
glacials/ice ages
interglacials
warm periods
glacial budget
ablation
glacial budget
accumulation
glacial budget
calving
glacial budget
inputs
fresh snow + avalanches
outputs
glacial budget
plucking
melt water freezes onto rocks, as th glacier moves it rips out those fragment = rough, jagged surface
weathering
freeze-thaw weathering
subglacial moraine
material carried underneath glacier
englacial moraine
material within the glacier
supraglacial moraine
moraine on top
terminal moraine
final point the glacier and moraine it was pushing infront
snout
front of glacier
bulldozing
pushing material infront of it