| terminalmoraines | | streams which flow over hanging valleys |
| glacialerratics | | u-shaped valleys which have been eroded to below sea level and flooded |
| ushapedvalleys | | moraines left as glacier retreats |
| hornpeak | | small lake in the bottom of a cirque |
| outwashplains | | formed when ice blocks glacial meltwaters |
| cirques | | mixture of clay, gravel and sand |
| eskers | | bowl-like depression in rock formed by erosion |
| glacialtill | | ridges of sands and gravel left by glacial streams |
| icedamnedlake | | formed at the furthest point the glacier reaches |
| kames | | formed along the sides of a glacier |
| tarn | | rocks which are carried far distances then deposited |
| hangingvalleys | | formed along the centre of the glacier |
| lateralmoraines | | tear-shaped hills formed by a re-advancing glacier |
| fiords | | deltas left behind in shape of a small hill |
| recessionalmoraines | | ridges formed between cirques |
| drumlins | | eroded by a glacier to be wider with gentler curves |
| arĂȘtes | | a rectangular peak created when many cirques erode into a mountain |
| bridalveilfalls | | meltwaters flow from glaciers and deposit silt and sand form _____________ |
| medialmoraines | | valleys of smaller glaciers which sit above larger glaciers for ______________ |