English: Shear or herring-bone crevasses on the Emmons Glacier; such crevasses often form near the edge of a glacier where interactions with underlying or marginal rock impede flow. In this case, the impediment appears to be some distance from the near margin of the glacier.
ꯃꯥꯟꯅꯕꯥ ꯁꯥꯔꯨꯛ – ꯀꯔꯤꯒꯨꯝꯅ ꯅꯪꯅ ꯌꯥꯟꯁꯤꯟꯅꯔꯕ, ꯍꯣꯡꯗꯣꯛꯍꯟꯂꯕ, ꯅꯠꯇ꯭ꯔꯒ ꯄꯣꯠꯆꯪꯁꯤꯡ ꯁꯥꯒꯠꯂꯕꯗꯤ, ꯅꯪꯒꯤ ꯍꯣꯠꯅꯖꯃꯟ ꯑꯗꯨ ꯃꯁꯤꯒꯤ same or compatible licenseꯒꯤ
ꯃꯈꯥꯗ ꯎꯠꯀꯗꯕꯅꯤ ꯑꯁꯦꯡꯕ ꯑꯅꯧꯕ ꯱ ꯑꯣꯏꯅ ꯂꯧꯗꯨꯅ ꯫
This licensing tag was added to this file as part of the GFDL licensing update.http://creativecommons.org/licenses/by-sa/3.0/CC BY-SA 3.0Creative Commons Attribution-Share Alike 3.0truetrue