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Climatic Geomorphology
Figure 13.14. Large inter-rill areas separated by small gullies formed in Quaternary clay materials.
The slopes are affected by intense cracking and unequal rills development. The Bardenas Reales of
Navarra, Spain, in the Ebro Basin.
Figure 13.15. Intense rill formation in Miocene clays similar to badlands. The Bardenas Reales, Navarra,
Spain, in the Ebro Basin.
Climatic Geomorphology
Figure 13.14. Large inter-rill areas separated by small gullies formed in Quaternary clay materials.
The slopes are affected by intense cracking and unequal rills development. The Bardenas Reales of
Navarra, Spain, in the Ebro Basin.
Figure 13.15. Intense rill formation in Miocene clays similar to badlands. The Bardenas Reales, Navarra,
Spain, in the Ebro Basin.
