Glacial and periglacial sequence and floristics in Jaw Cirque, central Teton Range, western Wyoming

Clicks: 3
ID: 299924
1984
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
Emerging

Ranked #5,770 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
Relative ages are determined by topographic position, weathering features, lichenometry, vegetation characteristics, and soils. A four-fold sequence is identified and correlated with the Gannett Peak, Audubon, and Indian Basin advances of Neoglaciation and the late-Pinedale Glaciation in the Wind River Range (Wyo.), Front Range (Colo.), Wallowa Mountains (Oreg.), and Mount Adams (Cascade Range, Wash.). On a floristic basis, only differences in species composition are present between substrates of Neoglacial age. Most species collected on Neoglacial deposits in Jaw Cirque are identified in other parts of the Teton Range on deposits of similar age, and no vascular plant species is useful in discriminating between the stratigraphic units.--Modified journal abstract.
Reference Key
openalex_W2062332178 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors William C. Mahaney, John R. Spence
Journal american journal of science
Year 1984
DOI
10.2475/ajs.284.9.1056
URL
https://doi.org/10.2475/ajs.284.9.1056
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.