Exam 2: Formation of Soils From Parent Materials

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Residual parent materials have formed in place and have not been transported from one area to another.

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True

Igneous rocks can best be characterized as:

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A

Glacial till can be recognized by the distinct layering of different kinds of particles.

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False

Exfoliation is caused by changes in _________.

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Granite is an example of a(n) ________.

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Silicate clay accumulation is most common in the ____.

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Which of the following statements is not correct?

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Alluvial fans are usually characterized by ???______ soils.

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A soil developed in residual parent materials will likely have properties related to the properties of the rock below the C horizon.

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The transformation of gneiss into mica, quartz, and feldspar crystals is an example of:

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Weathering of rocks usually is most intense in the center of a rock fragment, and gradually decreases toward the outside.

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Glacial till is a term used to describe parent materials that:

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Sapric and fibric are terms used to describe peat parent materials.

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Organic deposits are most common in areas where water flow over the soil surface is restricted.

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The C horizons are generally more completely weathered than the other horizons.

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The reaction: mica + H2O K+ + OH- + acid clay is an example of ________.

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Chemical weathering is accelerated by water, oxygen, and organic and inorganic acids moving down through the regolith.

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The topmost horizon in most humid region forest soils is the A horizon.

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Secondary minerals are recrystallized products of the chemical breakdown and/or alteration of primary minerals.

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If you wanted to find a soil where physical weathering dominated over chemical breakdown you would be most apt to find it in ______.

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