Rocks in cold, dry climates resist chemical weathering better than those in hot, wet climates.
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Q23: Physical weathering basically makes small rocks out
Q24: Water, when it freezes, can easily break
Q25: Ordinary rainfall interacting with atmospheric CO2 produces
Q26: Hydrolysis of feldspar into clay depletes the
Q27: The mineral quartz is resistant to weathering
Q29: Fractured rock masses tend to weather more
Q30: Spheroidal weathering is the term applied when
Q31: Spheroidal weathering is a form of physical
Q32: Windblown dust from glaciated areas is called
Q33: In general, dark brown to nearly black
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