Snake coils (geology)

Snake coils is a descriptive term used by physical geologist and glaciologists to describe the "snake coil"-like shape that occurs along certain ablation lines. Essentially miniature tunnel valleys, the peculiar natural shapes were first described by French Geologist Jean-Jerome Peytavi in 1973 during an expedition to northern Greenland, and later confirmed by a team of Danish geologists. It is believed that snake coils are formed through the same mechanism as tunnel valleys.

References

This article is issued from Wikipedia - version of the Sunday, June 22, 2014. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.