Edge Rewrite
everything Source code View original
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a223c821181fd685

Jump to content

Interference ripples

Add links
From Wikipedia, the free encyclopedia

Interference ripples are a type of sedimentary structure[1] made up of two sets of ripples formed at right-angles to each other as a result of there being two dominant paleocurrents. These ripples may be formed in the beds of intermittent streams.[2]

References

[edit]
  1. ↑ "Physical Geology Slides-Sedimentary Rocks". Uwgb.edu. Retrieved 2016-03-19.
  2. ↑ M. Dane Picard and Lee R. High (1970-06-01). "Interference ripple marks formed by ephemeral streams". Journal of Sedimentary Research. 40 (2). Jsedres.geoscienceworld.org: 708–711. Bibcode:1970JSedR..40..708P. doi:10.1306/74D7201D-2B21-11D7-8648000102C1865D. Retrieved 2016-03-19.

Further reading

[edit]
  • Prothero, D. R. and Schwab, F., 1996, Sedimentary Geology, pg. 43-64, ISBN 0-7167-2726-9


Retrieved from "https://en.wikipedia.org/w/index.php?title=Interference_ripples&oldid=1292608523"