The shape of atolls; an inheritance from subaerial erosion forms
Clicks: 1
ID: 293672
1954
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.
Reader Engagement
0.0
/100
1 views
0 readers
AI Quality Assessment
Not analyzed
Readership in this journal
Ranked #6,059 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 mintedCreate 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
Abstract
Reviews various theories of atoll formation and summarizes observations in the northern Marshall islands which lead to the conclusion that the annular reef and lagoon structure of some oceanic atolls reflects marginal rims and central depressions developed by subaerial weathering processes on emerged limestone platforms, modified by subsequent organic growth following resubmergence of the platform. Alternation of organic growth and erosion was related to eustatic changes of sea level during the Pleistocene.
| Reference Key |
openalex_W2157600007
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | F. Stearns MacNeil |
| Journal | american journal of science |
| Year | 1954 |
| DOI |
10.2475/ajs.252.7.402
|
| URL | |
| 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.