Lithosphere - Part 2

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21 Terms

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Frost Action

Mechanical Weathering - Break off small grains to large boulders when water expands and freezes in rock pores.

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Granual Disintegration

As water evaporates, crystals grow from the materials dissolved in water which force apart mineral grains.

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Mechanical Weathering

When a rock breaks down into progressively smaller fragments without being altered by chemicals.

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Oxydation

Metallic elements combine with oxygen to form oxides, like iron oxide (rust).heC

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Chemical Weathering

When some or all the minerals in the rock are charged or decaying by agents like water, oxygen, carbon, and other organic acids.

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Biological Weathering

Tree roots can exert pressure on rock.

Bacteria, algae, fungi, and lichen can chemically alter minerals.

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Factors that influence weathering:

Faster weathering:

  • More moisture

  • More heat

  • Cold (frost action)

  • The minerals that make up the rock.

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Igneous Rock

Forms from the cooling and crystallization of the earth’s crust.

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Extrusive Igneous Rock

Formed from lava on the Earth’s surface. Cools fast = fine grain or no crystals

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Intrusive Igneous Rock

Forms from magma beneath the Earths surface (intrusive)

Cools slowly → big crystals

More pressure = darker

Less pressure = lighter

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Lava

Molten rock on Earth’s surface

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Magma

Molten rock under Earth’s surface

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Sediment

Mineral grains broken down from rock

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Sedimentary Rock

Pressure from the weight or material deposited compacts and cements sediments into sedimentary rock.

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Metamorphic Rock

Rocks go through intense pressure and temperature changes without having to melt. Rock is now stronger and more resistant to weathering.

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O horizon

humus, workable, good porosity

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A horizon

topsoil, lots of nutrients and organic material

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E horizon

Extras from the topsoil leached out

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B horizon (subsoil)

Accumulation of leached materials (subsoil)

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R horizon

Regolith, partly broken down parent material

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