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  2. Jet erosion test - Wikipedia

    en.wikipedia.org/wiki/Jet_erosion_test

    The test consists of mounting a jet tube inside of an enclosed cylinder and releasing a turbulent downpour of water onto a soil specimen at a constant hydraulic head.If the shear stress applied by the jet stream exceeds the critical shear stress for erosion of the soil, the jet will erode soil particles, causing a scour hole to form.

  3. Weathering - Wikipedia

    en.wikipedia.org/wiki/Weathering

    Thermal stress weathering is an important mechanism in deserts, where there is a large diurnal temperature range, hot in the day and cold at night. [13] As a result, thermal stress weathering is sometimes called insolation weathering, but this is misleading. Thermal stress weathering can be caused by any large change of temperature, and not ...

  4. Soil mechanics - Wikipedia

    en.wikipedia.org/wiki/Soil_mechanics

    Download as PDF; Printable version; In other projects ... Soil produced and transported by intense weathering and erosion ... The field Plate Load Test is commonly ...

  5. Hole erosion test - Wikipedia

    en.wikipedia.org/wiki/Hole_erosion_test

    The hole erosion test (HET) is a method used in geotechnical engineering to quantify the resistance of a soil to erosion, and is specifically relevant to the topic of internal erosion in embankment dams. The test can be performed in a laboratory on a remolded soil sample, and provides estimates of both the critical shear stress for erosion of ...

  6. Soil production function - Wikipedia

    en.wikipedia.org/wiki/Soil_production_function

    A general model suggests that the rate of physical weathering of bedrock (de/dt) can be represented as an exponential decline with soil thickness: / = ⁡ [] where h is soil thickness [m], P 0 [mm/year] is the potential (or maximum) weathering rate of bedrock and k [m −1] is an empirical constant. [1]

  7. Rock cycle - Wikipedia

    en.wikipedia.org/wiki/Rock_cycle

    Weathering and erosion break the original rock down into smaller fragments and carry away dissolved material. This fragmented material accumulates and is buried by additional material. While an individual grain of sand is still a member of the class of rock it was formed from, a rock made up of such grains fused together is sedimentary.

  8. Sedimentology - Wikipedia

    en.wikipedia.org/wiki/Sedimentology

    Clastic rocks are composed of particles derived from the weathering and erosion of precursor rocks and consist primarily of fragmental material. Clastic rocks are classified according to their predominant grain size and their composition. In the past, the term "Clastic Sedimentary Rocks" were used to describe silica-rich clastic sedimentary ...

  9. Joint (geology) - Wikipedia

    en.wikipedia.org/wiki/Joint_(geology)

    Joints have a profound control on weathering and erosion of bedrock. As a result, they exert a strong control on how topography and morphology of landscapes develop. Understanding the local and regional distribution, physical character, and origin of joints is a significant part of understanding the geology and geomorphology of an area.

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