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1966_Glacier margins derived from USGS 1966 topographic maps for the named glaciers of Glacier National Park, MT and environs

Dates

Publication Date
Start Date
1966
End Date
1968

Citation

Fagre, D.B., McKeon, L.A., Dick, K.A., and Fountain, A.G., 2017, Glacier margin time series (1966, 1998, 2005, 2015) of the named glaciers of Glacier National Park, MT, USA: U.S. Geological Survey data release, https://doi.org/10.5066/F7P26WB1.

Summary

The 1966 polygons included in this data release represent the main body portion of the 37 named glaciers of Glacier National Park (GNP) and 2 named glaciers on the U.S. Forest Service’s Flathead National Forest land. This is a subset of the original mapping effort derived from 1:24000 scale mapping of named glaciers and permanent snowfields within Glacier National Park, Montana which were digitized by Richard Menicke (Glacier National Park) and Carl Key (U.S. Geological Survey) in 1993. These data are based on USGS 7.5 minute quadrangle mapping published from 1966 through 1968 which were the result of the earliest park-wide aerial surveys of snow and ice features in GNP. Examination of the aerial photographs shows that seasonal snow [...]

Contacts

Point of Contact :
Daniel B Fagre
Originator :
Daniel B Fagre, Lisa A McKeon
Metadata Contact :
Lisa A McKeon
Publisher :
U.S. Geological Survey
Distributor :
U.S. Geological Survey - ScienceBase

Attached Files

Click on title to download individual files attached to this item.

Shapefile: GNPglaciers_1966.zip
GNPglaciers_1966.cpg 5 Bytes
GNPglaciers_1966.dbf 21.62 KB
GNPglaciers_1966.prj 425 Bytes
GNPglaciers_1966.sbn 492 Bytes
GNPglaciers_1966.sbx 132 Bytes
GNPglaciers_1966.shp 236.3 KB
GNPglaciers_1966.shx 412 Bytes

Purpose

The purpose of this dataset is to develop a time series and history of glacier recession in Glacier National Park, Montana, USA. This dataset consists of polygons that delineate the 1966 perimeters of the named glaciers of Glacier National Park and two additional glaciers on U.S. Forest Service’s Flathead National Forest land (the Bob Marshall Wilderness Complex) which borders GNP to the south. Establishing the rates of glacier retreat, using the decreasing area of glacier ice, is key to understanding the Glacier National Park ecosystem and future state of resources. For instance, glacial meltwater provides critical habitat for endangered stream insects. More broadly, retreating glaciers are indicative of long term climate change and have hydrologic and ecologic importance to many park resources. Glaciers and their retreat are of great interest to park visitors and the American public and are part of Glacier National Park's appeal. This is important because Glacier National Park is a major driver of the regional economy. Appropriate use of these data include comparing Glacier National Park's glacier area from different periods, such as subsequent years included in the data release, and from different parts of the world. The change in glacier area can be used to test models of glacier-climate interactions, and to estimate glacier contributions to streamflow. A caveat to use of this dataset is the recognition that mapping technologies of 1966 were different from current technologies in accuracy and resolution. Thus, the glacier outlines in this dataset are more generalized than those from subsequent years included in this data release.

Additional Information

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