t-glaciers

a large mass of ice and snow moving on land under its own weight

slow movement of a glacier in which ice crystals slip over each other

process that adds various sizes of sediment to the glacier's bottom as it freezes and melts

a mixture of different-sized sediments that is dropped from the base of a reterating glacier

large boulders transported and deposited by a glacier

grooves carved into rock, caused by glacial till

the smoothing and leveling of rock by fine debris

a large ridge of rocks and soil deposited by a glacier when it stops moving forward

material deposited by meltwater from a glacier

a winding ridge of sand and gravel that is left behind when a glacier melts

a long, low, tear-shaped mound of till

Continental Glaciers are found in and around the Arctic, Antarctic circles, Greenland and island in the polar regions

Valley Glaciers are found in mountain regions all over the world. They begin in the mountain where it is snows all year and the temperatures are always below freezing

a rock or bedrock hill that has been smoothed on the side the glaciers came from and plucked and jagged on the side the glaciers leave

is a shallow, sediment-flled body of water formed by retreating glaciers or draining floodwaters

the shape of the valley which a glacier carves

the rising and falling of the Earth's temperature over time (ex. during hot periods, ice will melt and sea levels wil rise and during cold periods, ice will build and glaciers will form