An ice shelf is a thick platform of ice that forms at the grounding line of a glacier, where the glacier meets the coastline. Most freshwater on earth is bound in the huge ice shield covering almost entire Antarctica and extending in shelf-ice to the sea. Increasing melt of Antarctic ice would lead to significant sea level rise.
Using this item and referring to it is encouraged, and please use
it in presentations, web pages, newspapers, blogs and reports.
For any form of publication, please include the link to this
page and give the creator credit
(in this case Peter Prokosch)
If the high-resolution file is not available, please contact
email@example.com for request and
permission for usage.