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Published byAshlynn Shields Modified over 8 years ago
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Aspen Glaciation Objective: –Be able to identify and distinguish local glacier features
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Aspen Glaciation 4 KNOWN glacial periods –There could have been more Last 2mya- Glacial/interglacial period –Freeze/melt cycles Last glacier melted ~10,000 mya Montezuma Basin- last glacial remnants
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Glacial Development Picture 1- Glacier 1 –Original Glacier filled in river valley with erosional sediments Called outwash Picture 2- Glacier 2 –Deeper valley made by Roaring Fork eroding the outwash –Each glacier created its own outwash plain Picture 3- Glacier 3 –Aspen Terrace is the largest outwash plain –3 rd glacier- never reached town Picture 4- Glacier 4 –All of these flats are outwash plains created by the river eroding the sediment
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Outwash Plains Outwash is glacial till carried by Water.
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Calculating Glacier Thickness 1. Find average elevation of lateral moraines –Contour lines 2. Find elevation of river valley 3. SUBTRACT lateral moraine (big) elevation from river valley (small) elevation
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Rock Glaciers Rock on the outside - ice on the inside Can be found: –Pearl Pass –Pyramid Peak –Mnt Sopris
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Rock Glaciers
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