Rocks, weathering and soils

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課程筆記

Geological Time

  • Geological time refers to the vast timescales over which Earth's rocks and landscapes have formed and changed.
  • Processes like weathering and erosion act over millions of years, shaping the land we see today.
  • Understanding geological time helps explain why some rocks are much older than others.

Types of Rock

  • Igneous rocks form when molten rock (magma or lava) cools and solidifies.
  • Sedimentary rocks are made from layers of sediment that become compacted and cemented over time.
  • Metamorphic rocks form when existing rocks are changed by heat and/or pressure.
  • Examples include granite (igneous), limestone (sedimentary) and slate (metamorphic).

The Rock Cycle

  • The rock cycle describes how rocks are continually formed, broken down and reformed over geological time.
  • Weathering and erosion break down existing rocks into sediment.
  • Sediment can be transported, deposited and lithified to form sedimentary rock.
  • Heat and pressure can change rocks into metamorphic rocks, and melting can produce magma for igneous rocks.

Weathering: Physical Processes

  • Physical weathering (also called mechanical weathering) breaks rocks into smaller pieces without changing their chemical composition.
  • Freeze-thaw weathering occurs when water freezes in cracks, expands by 9.2%, and exerts pressure that can fracture rock.
  • Thermal stress weathering results from repeated expansion and contraction of rock due to temperature changes, leading to cracking.
  • Onion-skin weathering (exfoliation) is the peeling of outer rock layers due to repeated heating and cooling.
  • Biological weathering includes plant roots prying apart rocks and burrowing animals disintegrating rock.

Weathering: Chemical Processes

  • Chemical weathering involves reactions between rock minerals and water, atmospheric gases (like oxygen and carbon dioxide), or biologically produced chemicals.
  • Water is the principal agent of chemical weathering.
  • Chemical weathering can dissolve minerals or alter them into new minerals.
  • Biological weathering can also be chemical, for example when lichens produce acids that break down rock.

Soil Formation

  • Soil forms from the breakdown products of rocks mixed with organic material (humus).
  • Weathering is the first step in soil formation, creating loose rock fragments.
  • Organic matter from dead plants and animals enriches the soil.
  • Soil formation is a slow process that can take thousands of years.

Soil Horizons

  • A soil profile is a vertical section through soil, showing distinct layers called horizons.
  • The O horizon is the top layer of organic matter (leaf litter, humus).
  • The A horizon (topsoil) is a mixture of organic material and minerals, where most plant roots grow.
  • The B horizon (subsoil) accumulates minerals leached from above.
  • The C horizon is made of weathered parent rock fragments.
  • The R horizon is the underlying solid bedrock.

Why Soils Differ

  • Soils vary because of differences in parent rock, climate, relief (slope), organisms and time.
  • Climate affects weathering rates and the amount of organic matter.
  • Steep slopes may have thin soils due to erosion.
  • Different parent rocks produce soils with different mineral contents and textures.

UK Rock Landscapes

  • Granite landscapes, such as Dartmoor, form from igneous rock that is resistant to weathering, often creating high moorland with tors.
  • Limestone landscapes, such as the Peak District or Yorkshire Dales, are shaped by chemical weathering, producing features like caves and pavements.
  • The type of rock influences the landscape's shape, drainage and vegetation.

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練習題

免費預覽——60 題中的 8 題。註冊即可查看全部。
  1. 1.What is the term for the breakdown of rocks in their original place, without movement?

    Easy
    • AErosion
    • BWeathering
    • CTransportation
    • DDeposition
  2. 2.Which of the following is the main agent of both physical and chemical weathering?

    Easy
    • AWind
    • BWater
    • CSunlight
    • DGravity
  3. 3.Which of the following are types of physical weathering? (Select all that apply.)

    Medium
    • AFreeze-thaw weathering
    • BThermal fracturing
    • CPressure release
    • DCarbonation
    • EHydrolysis
  4. 4.Weathering involves the transport of rocks and minerals by agents such as water, ice, wind, and gravity.

    Easy

    True or false?

  5. 5.Match each weathering process with its correct description.

    Medium
    • Frost wedging
    • Ice segregation
    • Thermal fatigue
    • Expansion of freezing water in cracks
    • Growth of ice lenses that pry rock apart
    • Repeated stress cycles gradually weaken rock
  6. 6.Put the following steps of the rock cycle in the correct order.

    Medium
    • Weathering breaks down existing rock into sediments
    • Sediments are transported and deposited
    • Sedimentary rock is formed
    • Heat and pressure change rock into metamorphic rock
  7. 7.Which type of weathering is most important in subarctic or alpine environments?

    Medium
    • AChemical weathering
    • BPhysical weathering
    • CBiological weathering
    • DErosion
  8. 8.Which of the following statements about frost weathering are true? (Select all that apply.)

    Medium
    • AFrost wedging is most effective in small tortuous fractures.
    • BIce segregation is likely the more important mechanism of frost weathering.
    • CFrost wedging is most effective in the tropics.
    • DFrost weathering is a form of chemical weathering.
    • EIce segregation occurs when supercooled water migrates to ice lenses.

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