Piedmont Glaciers
Image Description from historic lecture booklet: "Glaciers of the piedmont type are formed where alpine glaciers leave the rugged defiles through which they flow and expand and unite on an adjacent plain. They may be considered as analogous to lakes, for the reason that they are fed by tributary ice streams."
Original Collection: Visual Instruction Department Lantern Slides
Item Number: P217:set 012 005
You can find this image by searching for the item number by clicking here.
Want more? You can find more digital resources online.
We're happy for you to share this digital image within the spirit of The Commons; however, certain restrictions on high quality reproductions of the original physical version may apply. To read more about what “no known restrictions” means, please visit the Special Collections & Archives website, or contact staff at the OSU Special Collections & Archives Research Center for details.
Piedmont Glaciers
Image Description from historic lecture booklet: "Glaciers of the piedmont type are formed where alpine glaciers leave the rugged defiles through which they flow and expand and unite on an adjacent plain. They may be considered as analogous to lakes, for the reason that they are fed by tributary ice streams."
Original Collection: Visual Instruction Department Lantern Slides
Item Number: P217:set 012 005
You can find this image by searching for the item number by clicking here.
Want more? You can find more digital resources online.
We're happy for you to share this digital image within the spirit of The Commons; however, certain restrictions on high quality reproductions of the original physical version may apply. To read more about what “no known restrictions” means, please visit the Special Collections & Archives website, or contact staff at the OSU Special Collections & Archives Research Center for details.