AP Environmental Science

Geological processes - chapter 16

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I. Plate tectonics

A. Structure of the earth’s interior – fig. 16-2

B. Convection cells within the earth’s mantle drive plate movement (fig. 16-2 and 16-3)

C. Divergent boundaries (fig. 16-5)

1. in ocean - mid-Atlantic ridge (more)

2. on land - rift valleys (Iceland (take a virtual field trip) and east Africa)

  • Lake Baikal in Russia is located on a rift (more)
  • a new ocean is forming in the rift valley of Africa
  • D. Convergent boundaries

    1. subduction zone

    2. trenches and island/volcano (fig. 16-5) arcs in the ocean

    3. mountain building on land

    4. ring of fire (fig. 16-4)

    E. Transform faults

    1. boundary between sections of divergent plates (fig. 16-5)

    2. earthquakes (fig. 16-6 and 16-7)

    Plate Tectonics links

     

    II. Non-tectonic processes produce most surface features

    A. glaciation

    B. mechanical weathering/erosion by wind and water

    C. chemical weathering

                D. The geologic history of the mid-Atlantic

    III. The rock cycle (another link) (fig. 16-9)

    A. igneous rock is formed beneath the earth’s surface in a molten state

    B. sedimentary rock forms from sediments weathered off existing rock/soil and deposited in water

    C. metamorphic rock is produced when existing rock is heated enough to change its form

    IV. Soils

    A. layers – fig. 4-25

    1. Surface layer (O horizon) – surface litter

    2. A horizon – topsoil – mostly organic (varies with soil type)

    3. B horizon – subsoil

    4. C horizon – parent material – lies on the bedrock

    B. soil organisms create soil (fig. 4-26) and add nutrients to it

    C. soil profiles vary in different biomes and are a determining factor for biome types (fig. 4-27, and more later in chap 6)

    D. soil types (more on soil classification) (more here - info on the 12 soil "orders", range maps, etc) (technical info)

    1. clay

    2. sand

    3. silt

    4. soils are a mixture of the three types, which results in a complex assortment of soil texture

    5. soils with roughly-equal mixtures are called loams

    6. differing properties result from varying combinations of the three types

    E. erosion

    1. three types – p. 279

    2. historical examples - dust bowl (p. 281)

    3. seriousness of erosion worldwide – fig. 14-7

    4. desertification is a related problem (fig. 14-9)

    5. solutions to soil erosion problems