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Localised zones of deeper weathering also exist at the NW area and at the SW floodplain regions where saprolite thickness exceeds 22.0 m (Fig. 7b).
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We suggest that deep unroofing of basement structures in many parts of Europe has been mainly accomplished by deep weathering and stripping of pre-weathered rock.
Also, tropical rocks tend to experience deep weathering, rarely poking above the ground as outcrops.
The moist, hot climatic conditions lead to deep weathering of rock and the development of deep, typically reddish soil profiles rich in insoluble sesquioxides of iron and aluminum, commonly referred to as tropical red earths.
Deep weathering is prevalent in tropical and sub-tropical areas.
Tropical chemical weathering produces extensive lateritization and formation of deep weathering profiles.
Because of deep weathering and thick vegetation, exposures of faulted rocks are scarce.
The phenomenon of deep weathering has been very important for geomorphology.
Higher-level bedrock areas were subjected to deep weathering and tor-formation.
Although dating of weathering mantles is often circumstantial, it appears sufficiently precise to argue for various ages of deep weathering.
This is an indication of a fairly deep weathering development with resistivities 100 600 Ωm across the study area.
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