Resurrected Oligocene hills, eastern Oregon
Clicks: 1
ID: 304998
1964
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 #7,373 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
Several hills near Turtle Cove, John Day State Park, represent part of an erosion surface on Cretaceous and pre-Cretaceous rocks, capped by volcanic claystones and siltstones of the John Day formation of late Oligocene-early Miocene age. Formation of the surface took place in Oligocene time. The red color of the unconformably overlying John Day rocks is due to iron oxide-stained montmorillonite formed by weathering of John Day volcanic ash during deposition.
| Reference Key |
openalex_W2328787720
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | Richard V. Fisher |
| Journal | american journal of science |
| Year | 1964 |
| DOI |
10.2475/ajs.262.6.713
|
| 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.