Russell Glacier (Mount Rainier) Explained

Russell Glacier
Type:Mountain glacier
Location:Mount Rainier, Pierce County, Washington, USA
Coords:46.8978°N -121.7889°W
Area:1.3sqmi, 1983[1]

The Russell Glacier is a medium-sized glacier on the north flank of Mount Rainier, Washington. Named for the geologist Israel Russell,[2] it covers 1.3sqmi and contains 3.1 billion ft3 (88 million m3) of ice.[1] Starting from its highest point at 9400feet, the Russell Glacier flows northeast towards the Carbon Glacier and contributes ice to the larger glacier before becoming distinct below 7000feet.[3] With most of the ice located from 8000feet to 9000feet, the glacier only descends to 6800feet, unlike the much lower extent of the Carbon Glacier.[3] Echo Rock and 83640NaN0 Observation Rock, two minor sub-peaks of Rainier, lie northwest of this glacier. Meltwater from the glacier eventually reaches the Carbon River.[1]

See also

Notes and References

  1. Web site: DESCRIPTION: Mount Rainier Glaciers and Glaciations - Mount Rainier Glacier Hazards and Glacial Outburst Floods. 2007-11-19. USGS.
  2. Book: Majors, Harry M. . Exploring Washington . Van Winkle Publishing Co . 1975 . 125 . 978-0-918664-00-6.
  3. Web site: USGS Mowich Lake (WA) Topo Map. USGS Quad maps. TopoQuest.com. 2008-05-17.