During a geomorphological field survey on a steep granite hillslope in a humid tropical environment, researchers observed a sudden planar failure where a thick mantle of saturated regolith slid rapidly downslope along a bedrock interface. Which of the following fundamental characteristics distinguishes this mass wasting event from the chemical weathering (hydrolysis) that originally formed the regolith?
- The mass wasting event involves the downslope transportation of rock mantle by gravity, while chemical weathering causes in-situ breakdown of minerals without slope movement.Cevap
- BThe mass wasting event alters the mineral composition of granite into clay, while chemical weathering strictly transports intact soil blocks down slope.
- CThe mass wasting event recrystallizes the regolith into metamorphic slate, while chemical weathering deposits marine sediments along the slope foot.
- DThe mass wasting event occurs purely through wind abrasion on exposed slopes, while chemical weathering is exclusively driven by tectonic uplift.
Cevap
Mass wasting involves the downslope displacement of weathered material under the direct influence of gravity, whereas weathering is the in-situ disintegration or decomposition of rocks without transportation.
Mass wasting refers specifically to the gravitational movement of weathered rock materials and soil down a slope. Weathering, such as hydrolysis operating on granite in humid environments, is an in-situ process that breaks down minerals chemically in place without transporting them downslope.
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Distinction between in-situ weathering breakdown and downslope mass wasting under gravity
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