Glacial Landforms
There is a huge variety of glacial landforms recognised in the geological record. However, they are difficult to see in Antarctica, because they are usually buried beneath ice.
On a few small islands around the Antarctic Peninsula, however, you can see evidence of past glaciations through glacier sediments and landforms.
The contrast between landforms being made by different processes is clear around the Antarctic Peninsula. Small islands and ice-free areas, such as James Ross Island, are characterised by small moraines made by polythermal glaciers. However, on the continental shelf, there are large landforms generated by ice streams at the Last Glacial Maximum (LGM). The next section contrasts these different environments and their landforms.
James Ross Island
Some of our examples of glacial landforms come from James Ross Island, which is located on the northeast tip of the Antarctic Peninsula, at about 64°S (see map below)[1].
The area was glaciated during the Last Glacial Maximum, with cosmogenic nuclide exposure ages indicating recession of the main glacier ice around 11,000 to 9500 years ago[2] (see ice sheet evolution).
The landscape is now characterised by permafrost (see Periglaciation)[3, 4], with small cold and polythermal glaciers, and periglacial landforms, such as rock glaciers[5], protalus ramparts, patterned ground, snow patches and small ephemeral streams.
The most obvious glacier landforms on James Ross Island are ice-cored moraines around small glaciers on Ulu Peninsula. These glaciers are surrounded by sharp-crested moraines with a core of glacier ice. The glacier ice is stratified with blue and white, bubble-rich ice and debris-rich bands, suggesting that it is basal glacier ice.
The crests of the moraines range from sharp-crested to chaotic, with the ice wasting and melting in situ. The buried glacier ice means that water cannot drain away, and many small frozen and unfrozen lakes and ponds are impounded on the moraines.
You can see many more examples of glacial landforms on the Glaciers Online photoglossary.
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We hope to see more information about Antartica.thank you?
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this is very help full, i cant wait to see more of this
The absence of a stretch of bare cock without any significant vegetation between the end moraine and the galcier is in sharp contast with such galciers that I have seen in my lifetime. Could it be that ice retreat in Antarctica has been less pronounced than it has been with temperate zone mountain galciers, because gobal warming is bringing more moisture from warmer oceans, and therefore more snowfall to Antarctica?
In my country we have chance .we can not found glacial landforms. we have temperate zone,no global warming or greenhouse
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