Unit 3 Flashcards
straition
grooves gouged in bedrock formed by rocks frozen in the ice and run in the same direction as movement of glaciers
spillways
deep, wide valleys formed by glacier melt water
misfit streams
small streams in the middle of spillways that occur when melt water disappears
till plains
till is material like gravel, clay and sand in ice.
- gently rolled plains formed by deposits of sand, clay and gravel from glaciers and if not acted upon by water, are pointy and angular
lake plains
fertile and flat plains formed by deposits of silt and glacial meltwater (good for agriculture
moraines
an ice sheet that has deposited till at it’s edge, hilly swapy, and thin soil (good for forestation)
drumlins
an egg-shaped hill with a steep side (wide end) and a gentle slope formed when glaciers move deposited material over (soil is well drained)
erratics
are picked up by ice sheets and carried hundreds of km over to make up different bedrock. ex- rocks from the canadian shield were carried hundreds on km away/to the lowlands
eskers
when rivers flow within melted ice, they carry sand and gravel and lay them in a river bed (are left as steep-sided ridges)
alpine glacier
formed in the mountains and move down valleys by gravity “sharpening” the features of the mountain to look rugged
continental glaciers
move outward under their own ice and snow weight. the surface becomes smoother since they erode at high points of terrain and deposit eroded material is at the bottom
folding
happens over a long period of time when the rock layers bend together instead of break due to high temperatures and pressure. the pressure currents are exerted to the midddle, causing folding ridges
faulting
is fractures in bedrock along where movement has taken place and appear in the Earth’s crust by stress of convention currents that occur in the mantle. If the rock is brittle or bends quick, it breaks and forms a fault
plate tectonics
the internal forces that deform the Earth’s crust
- there are 20 located in water bodies and land
- the plates move due to uneven distribution of heat, and move over a weak layer of hot rock hundreds of km below the surface
glacier advance
glaciers advance when the rate of snow is lower than the rate of accumulation