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 ______________ |