Dry valley
id:
dry-valley-241-11341991
title:
Dry valley
text:
A dry valley may develop on many kinds of permeable rock, such as limestone, chalk, sand stone and sandy terrains that do not regularly sustain surface water flow. Such valleys do not hold surface water because it sinks into the permeable bedrock. There are many examples of chalk dry valleys along the North and South Downs in Southern England. Notably the National Trust-owned Devil's Dyke near Brighton covers some 200 acres (0.81 km2) of downland scarp, and includes the deepest dry valley in the
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Dry_valley
date created:
date modified:
2024-02-09T13:38:48Z
main entity:
{"identifier":"Q1672567","url":"https://www.wikidata.org/entity/Q1672567"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/7/7b/Dry_Valley_Near_Rackham_Hill_-_geograph.org.uk_-_548019.jpg","width":640,"height":480}
fields total:
13
integrity:
14