Glacial till can be recognized by the distinct layering of different kinds of particles.
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Q42: Even if all the glaciers present today
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Q45: Eluviation of clay,iron,and other materials is the
Q46: In most B horizons one of the
Q48: A soil developed in transported parent materials
Q49: Weathering of rocks usually is most intense
Q50: The C horizons are generally more completely
Q51: A soil developed in residual parent materials
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