Stream channels and point bars are more “active” depositional sites. Stream channel deposits may have pebbles and cobbles whereas sediments on the adjacent point bars are normally composed of sand. Typical sedimentary structures include small dunes and ripples. Explain the consistent difference in grain size between channel and point-bar sediments.
Subscribe to:
Post Comments (Atom)
-
Create a 2 pages page paper that discusses sex change.  .The controversy that will surround the red...
-
As part of the application process, you will be asked to write a 500 word or less essay on the topic: What do...
-
Imagine you are the judge hearing the case brought against John Brown. Given what you know about the histor...
No comments:
Post a Comment