explain under construction USGS home NPS home USGS/NPS banner
Valley glacier cross-section.
A slice through a valley glacier.

Glacier growth

spacer image As the glacier flows downhill, it descends to warmer zones where the snow melts from year to year. The boundary where loss from melting and evaporation equals accumulation from snowfall is called the annual snowline or firn limit-"firn" being the term for partially compacted snow carried over from previous seasons.
spacer image The firn limit fluctuates from year to year in response to changes in precipitation and temperature. The firn limit can be as much as 1,000 ft lower in elevation on the shaded north sides of mountain peaks tan on their sunny south sides. For this reason, many present-day glaciers are found on the north-facing mountain slopes.
spacer image The section of the glacier through which the maximum amount of ice flows coincides with the firn limit, because as the glacier flows toward the firn limit, it is continually augmented by new net snowfall; and downvalley from the firn limit, more ice is lost by melting and evaporation-together called ablation-each year than is added by snowfall. As the glacier flows downvalley from the firn limit, more and more of the ice ablates, and the glacier grows thinner or narrower, or both. Ultimately a point is reached where the ice front can advance no farther because the ice melts there as rapidly as it is provided by inflow from up glacier. If the yearly rates of accumulation and ablation were constant, this point would be fixed. However, they vary, and for that reason alone the terminus of the glacier is not likely to be fixed in position. As the climate turns warmer or drier, a glacier will gradually waste away, rather than melting catastrophically.
| RETURN |

horizontal bar
| USGS Geology in the Parks home | NPS Park Geology Tour home |

Privacy statement / General Disclaimer

This site is a cooperative project of the
US Geological Survey Western Earth Surface Processes Team
and the National Park Service.

Please share your comments and suggestions with us!
parkgeology@den.nps.gov

http://www.nature.nps.gov/grd/usgsnps/glacier/glform2.html
This page was last updated on 5/10/99