A parallel-bedded accumulation of sediments forms a low ridge on the upcurrent side of a partially moated knoll. These sediments were deposited beneath a southwestward-flowing current where it is locally decelerated by the obstructing knoll.
Download full-text PDF |
Source |
|---|---|
| http://dx.doi.org/10.1126/science.157.3796.1552 | DOI Listing |
Publication Analysis
Top Keywords
knoll sediment
4
sediment drift
4
drift hudson
4
hudson canyon
4
canyon parallel-bedded
4
parallel-bedded accumulation
4
accumulation sediments
4
sediments forms
4
forms low
4
low ridge
4
Similar Publications
Want AI Summaries of new PubMed Abstracts delivered to your In-box?
Enter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!