One of the major characteristics of the area are that its hills are formed of marl-covered soft chalk, as opposed to the Judean Hills which are made of hard chalk and dolomite. The valleys and lower areas contain soil with a high sand content, as well as large tracts of fertile areas. Seasonal swamps can develop during the rainy season. The southern part is made up of loess, while north of Ashkelon consists of clay.
Attributes | Values |
---|---|
rdfs:label |
|
rdfs:comment |
|
dcterms:subject | |
dbkwik:religion/pr...iPageUsesTemplate | |
abstract |
|