Jackson Glacier
In 1850, there were an estimated 150 glaciers in the park. Glaciologists have stated that by the year 2030, many if not all of the glaciers in the park may disappear completely. Jackson and Blackfoot glaciers have been selected for monitoring by the U.S. Geological Survey's Glacier Monitoring Research program, which is researching changes to the mass balance of glaciers in and surrounding Glacier National Park. The glacier is being monitored using remote sensing equipment and repeat photography, where images of the glacier are taken from identical locations periodically. Jackson Glacier is one of the easiest of the park's glaciers to observe, and is located south of the Going-to-the-Sun Road on the east side of the Continental Divide, upper St. Mary Valley.
See also
References
- ^ "Jackson Glacier". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved August 12, 2012.
- ^ "Retreat of Glaciers in Glacier National Park" (PDF). United States Geological Survey. 2010. Archived from the original (PDF) on May 11, 2012. Retrieved November 4, 2011.
- ^ Mount Jackson, MT (Map). Topoquest (USGS Quads). Retrieved November 4, 2011.
- ^ Myrna, H.; P. Hall; Daniel B. Fagre (February 2003). "Modeled Climate-Induced Glacier Change in Glacier National Park, 1850–2100" (PDF). BioScience. 52 (2): 131–140. doi:10.1641/0006-3568(2003)053[0131:mcigci]2.0.co;2. Archived from the original (PDF) on February 21, 2013. Retrieved November 4, 2011.
- ^ "Monitoring and Assessing Glacier Changes and Their Associated Hydrologic and Ecologic Effects in Glacier National Park". U.S. Geological Survey. Archived from the original on December 17, 2007. Retrieved November 4, 2011.