Corrasion by wind-blown snow in polar regions

Clicks: 1
ID: 296266
1939
Free PDF
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal

Ranked #3,696 of 8,486 articles by views in american journal of science

Most read Least read

Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 8,486 in total.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Sign in to mint
Abstract
The hardness of ice increases with decreasing temperature until at-50 degrees it has a hardness of about 6. No doubt then at low temperatures snow possesses the physical properties required for corrasion effects even on hard rocks. Certain polished surfaces and mushroom-shaped rocks in glacial regions may well be due to wind-blown snow.
Reference Key
openalex_W2313381524 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Curt Teichert
Journal american journal of science
Year 1939
DOI
10.2475/ajs.237.2.146
URL
https://ajs.scholasticahq.com/article/57827.pdf
Keywords Keywords not found

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

Comments

No comments yet. Be the first to comment on this article.