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The End Result of Weathering Soils Topic 9 Regents Earth Science
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Soils are the end result of both chemical and physical weathering.
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sediments all particles of weathered rock regardless of their size
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ESRT page 6 The dotted lines separate the sizes from each each other
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Sediment Sizes - not kind of material Boulders Cobbles Pebbles Sand Silt Clay Colloids Atoms and ions large small > 25.6 cm 6.4 - 25.6 0.2 - 6.4.006 - 0.2.0004 -.006.00001 -.0004
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soil Tiny bits of inorganic (rock) and organic (humus) matter ranging in size from sand to colloids and ions
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humus organic part of the soil partially weathered plant and animal matter
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Soil profile A side view of a vertical section showing all horizontal layers Develops as a result of weathering and biological processes
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Soil Profile
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Soil profile
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Soil horizons The different layers in a soil profile each with its own characteristic properties such as color, texture, and mineral composition
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Parent material the material from which a soil is formed
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Residual soil soil that has the local bedrock as its parent material
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Transported soil soil that formed from parent material left by winds, glaciers, and rivers, or soil that was itself moved from its original location
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Factors that affect the thickness and composition climate - temperature and precipitation Time longer = thicker parent material -affects the rate of soil formation the soils’s fertility Types of organisms and how many there are Slope of the land
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