Mantle-controlled planation of pediments

Clicks: 1
ID: 295058
1966
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 #5,211 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
On the basis of observations at the heads of granitic and schist pediments in central Australia, it is concluded that grading has largely acted through the mantles, as a result of which the smoothness of depositional profiles has been transmitted to suballuvial and part-subaerial pediments.
Reference Key
openalex_W1989407181 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors J. A. Mabbutt
Journal american journal of science
Year 1966
DOI
10.2475/ajs.264.1.78
URL
https://ajs.scholasticahq.com/article/59115.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.