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SH Soil Parent Materials

AB
Residualsoils formed w/o moving away from original bedrock
colluvualsoils produced from fragments that moved from high to lower elevations
alluvialsoils deposited by moving waters
marinesoils developed from sediments of the seas, where the seas have receded
lacustrinesoils developed from parent materials deposited in glacial lakes
glacialsoils developed by action of glaciers
eoliansoils developed from wind deposits of silt from floodplains, etc
nitrogenpromotes vegetative growth
phosphorusis a part of the plants DNA
potassiumimportant for energy transfer
claysmallest soil particle
sandlargest soil particle



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