The Schmidt hammer (SH) test on boulders and corestones, suggests three distinctive degree of weathering (from moderately to completely weathered rock), and that biotite content is the major controlling factor of the granite mechanical behaviour.
The variation in the pore volume and the pore-size distribution through a profile of weathered rock can be used as an indicative measure of the variation in the degree of weathering with depth.
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Hardness is a reliable indicator of the degree of weathering of building stone [36].
These units show both lateral and vertical variations in the degree of weathering and porosity.
The properties of residual soils are a function of the degree of weathering.
Lateritization is a process of low-temperature weathering associated with mineralogical breakdown and the degree of weathering diminishes with depth.
This method is a highly efficient and economical technique for determining the degree of weathering of large exposed stone relics.
Mostly, the degree of weathering is determined by simple test results, ignoring simultaneous effects of various weathering factors.
The yield characteristics of wells vary considerably depending on the topographic set-up, lithology, and the degree of weathering.
