Currently, the volume of land ice on Earth is decreasing, driving consequential changes to global sea level and local stream habitat. Glacier retreat in Glacier National Park, Montana, U.S.A., is one example of land ice loss and glacier change. The U.S. Geological Survey Benchmark Glacier Project conducts glaciological research and collects field measurements across select North American glaciers, including Sperry Glacier located in Glacier National Park. These records provide direct evidence of glacier change. The amount and timing of Earth’s land ice that will be lost in the future depends on the future trajectory of greenhouse gas emissions. Ongoing glaciological research will enhance physical understanding and forecasting capabilities; however, the continued retreat and ice mass loss of small glaciers in Glacier National Park is certain.
Florentine, C., 2019, Glacier retreat in Glacier National Park, Montana (ver. 1.1, December 2019): U.S. Geological Survey Fact Sheet 2019–3068, 2 p., https://doi.org/10.3133/fs20193068.
ISSN: 2327-6932 (online)
ISSN: 2327-6916 (print)
Table of Contents
- How Is the U.S. Geological Survey Assessing Glacier Ice Mass?
|Publication Subtype||USGS Numbered Series|
|Title||Glacier retreat in Glacier National Park, Montana|
|Series title||Fact Sheet|
|Edition||Version 1.1; December 6, 2019|
|Publisher||U.S. Geological Survey|
|Publisher location||Reston, VA|
|Contributing office(s)||Northern Rocky Mountain Science Center|
|Other Geospatial||Glacier National Park|
|Online Only (Y/N)||N|
|Google Analytic Metrics||Metrics page|