Collaborative Research: Integrating Geomorphological and Paleoecological Studies to Reconstruct Neogene Environments of the Transantarctic Mountains / Slide15_Moss layer at surface 1
Allan Ashworth, Adam Lewis and David Marchant
Lake sediments exposed at the ground surface. Sandy beds (left) deposited from small streams rest above diatom and moss layers (dark grey, center) deposited in a small alpine lake 14 million years ago. Sediments have been swept clean; scale is in 10's of centimeters.