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Glaciers
Surface Processes Part 4
| Term | Definition |
|---|---|
| Glacier | Naturally formed mass of ice and snow that move downhill under the force of gravity (develop when snowfall is greater than melting) |
| Glacier Movement | As snow accumulate the glacier moves forward under its own mass and the pull of gravity, Sometimes called "river of ice" glaciers act like fluids and flow in a plastic-like motion, tend to move into stream cut valleys |
| Continental glacier | Huge sheets of ice that cover entire land masses |
| Valley Glacier | Glacier that form in high elevation in mountain valleys |
| U-Shaped Valleys | Shape of the valley walls from glacial erosion |
| Erratics | Large deposited fragments that can be transported hundreds of miles inside or on top of the glacier |
| Drumlins | Streamlined oval shaped mounds of unsorted sediments |
| Eskers | A long winding ridge of sand and gravels |
| Terminal Moraines | A mound of till deposited along the leading edge of the glacier |
| Till | Unsorted sediments deposited by a glacier |
| Glacial Grooves | Long parallel scratches formed by sediment embedded in a glacier that has passed over the surface (the grooves indicate the glacier has traveled Location: central Park, NY) |
| Kettle Lake | Depression left in the ground that is filled with glacial melt water |
| Outwash Plain | Broad glacial feature of smaller sediment carried from the melting water of a retreating glacier |