Useful Links | Tools | Glossary | Search


Share:   | feedback

Alluvial fan

From petrofaq
Jump to: navigation, search

Alluvial fan:

  1. A mass of sediment deposited at a point along a river where there is a decrease in gradient, e.g. from a mountain to a plain. The mass is thickest at its point of origin, and thins rapidly in a downstream direction. In time, adjacent fans may coalesce and extend for many kilometres away from the mountain front.
  2. A pattern of sedimentary deposit frequently laid down by streams or rivers where they spread out into plains. Alluvial fans from past geological eras are potential reservoir structures.
Personal tools
Namespaces
Variants
Actions
Navigation
Contact us (or request an account)
Google AdSense