Icefields

Title
Icefields
LC Subject
Mountaineers Glaciers Ice Mountaineering
Description
Image Description from historic lecture booklet: "Every large snow-field is also an ice-field, for where snow accumulates to great depth and lies long upon the surface, it is changed to ice. the beginning of this change may be seen in the snow a few days after it falls, for it soon loses its light, flaky character and becomes granular, so that it feels harsh to the hand. The change is very distinct in the last banks of snow in the spring. They are made up of coarse grains (granules) of ice, sometimes as larges as peas. The change from flakes of snow to granules of ice is due, in part, to the melting of the snow and the freezing of the water. If there is much snow, it is compressed by its own weight, and after being compacted in this way, the freezing of the sinking water binds the granules together. By this and perhaps other process, the large part of every thick snow-field becomes an ice-field merely coated over with snow."
Work Type
lantern slides
Date
1915
Identifier
P217:07:39
Rights
No Copyright - United States
Rights Holder
OSU Special Collections & Archives Research Center
Local Collection Name
Visual Instruction Department Lantern Slides, 1900-1940 (P 217)
Type
Image
Format
image/tiff
Set
OSU Special Collections & Archives Research Center
Primary Set
OSU Special Collections & Archives Research Center
Is Part Of
Set 12 - Glaciers
Institution
Oregon State University
Modified
2011-07-18
Submission Date
2010-11-11
Note
Hand-tinted