Lake Fryxell

Lake Fryxell is located near the mouth of Taylor Valley, between Canada Glacier and Commonwealth Glaciers. It is long and at most wide, with a max depth of . Several streams, chiefly among them Canada Stream, flow into the lake on a seasonal basis, but the lake has no natural outflow. between and . The streams flow for about 4–12 weeks out of the year. Nearly half of the water flowing into the lake comes from Canada, Lost Seal, and Von Guerard streams. ==Climate==

Lake Fryxell is located within the McMurdo Dry Valleys, which experience an exceptionally dry climate partially due to katabatic winds descending from the nearby mountains. These winds can exceed under certain conditions and can raise the temperature, melting snow and evaporating water. Average precipitation in the area surrounding the valley is equivalent to about of rain a year and a mean annual temperature of with summer temperatures getting above freezing. }} ==Lake Fryxell Camp==

Mapped by the British Antarctic Expedition under Robert Falcon Scott, the lake was visited by Professor T.L. Péwé during Operation Deep Freeze, 1957–58, who named it for Dr. Fritiof M. Fryxell, glacial geologist of Augustana College, Illinois. Lake Fryxell is a focus of scientific research and contains a semi-permanent camp containing four labs and two other buildings. Electricity is generated at the camp using solar panels and a wind turbine. The four labs are used for experimenting with radioactive materials, electronics, chemicals and other materials. When staying at the camp, researchers sleep in tents, some of which are the same style as those used in some Antarctic expeditions in the early 20th century. There is internet and phone access at the camp. Research activities largely deal with the lake itself and can include scientists diving into the water. ==Ecology==

There are multiple forms of algae within the lake, including a sizable population of sulfate-reducing bacteria. Some samples of these bacteria live in very specific areas, such as specific water depths or locations causing them to experience differing physiochemical conditions. There are also a few archaea living in the anoxic zone, that contribute to the methane pockets under 12 m below the surface. There is a lack of oxygen within Lake Fryxell, which is unique when compared to other lakes in the region because the euphotic zone only extends to below the lake surface. This creates an environment similar to the planet about 2.4 billion years ago. Within anoxic areas, scientists have found microbial mats that create small pockets saturated with oxygen. ==See also==