Chapter 18 Flashcards
Glacier
thick mass of ice that forms over hundreds and thousands of years by accumulation, compaction, and recrystallization of snow
Two basic cycles of Glaciers
Hydrologic cycle
Rock cycle
Valley Glaciers
Glaciers that exist in valleys of mountainous areas
ice sheets
exist on a larger scale than valley glaciers
sea ice
frozen sea water
up to 4m thick
Covers Arctic Ocean rather than glacial ice
Glaciers form on land
- Greenland in northern hem
- Antarctica in southern hem
ice shelves
glacial ice flows out to sea
- In shallow water ice touches bottom
- deep water ice shelf floats
- Thickest on landward side and thin seaward
- Breakup of ice shelves attributed to regional global warming
ice caps
cover some uplands and plateaus
outlet glaciers
ice caps and ice sheets feed them, tongues of ice extending outward from the large masses
Piedmont glaciers
form when one or more alpine glacier emerges from the valley and spreads out in a broad lobe
snowline
snow above this line does not melt in the summer
How glaciers form
- air is forced out
- snow is recrystallized into a much denser mass of small grains (firn)
- Once thickness of ice and snow exceeds 50 meters, firm fuses into a solid mass of interlocking ice crystals-glacial ice
Glacial ice moves as
flow
Plastic flow of glaciers
involves movement within the ice; under pressure ice behaves as plastic material
Basal slip
entire ice mass slides along the ground, meltwater acts as lubricant