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  2. Microcracks in rock - Wikipedia

    en.wikipedia.org/wiki/Microcracks_in_rock

    Microcracks in rock, also known as microfractures and cracks, [1] are spaces in rock with the longest length of 1000 μm and the other two dimensions of 10 μm. In general, the ratio of width to length of microcracks is between 10 −3 to 10 −5. [1] Due to the scale, microcracks are observed using microscope to obtain their basic characteristics.

  3. Lithic fragment (geology) - Wikipedia

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

    Lithic fragments, or lithics, are pieces of other rocks that have been eroded down to sand size and now are sand grains in a sedimentary rock. They were first described and named (in their modern definitions) by Bill Dickinson in 1970. [1] Lithic fragments can be derived from sedimentary, igneous or metamorphic rocks.

  4. Rock (geology) - Wikipedia

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

    Metamorphic rocks are formed by subjecting any rock type—sedimentary rock, igneous rock or another older metamorphic rock—to different temperature and pressure conditions than those in which the original rock was formed. This process is called metamorphism, meaning to "change in form". The result is a profound change in physical properties ...

  5. Discontinuity (geotechnical engineering) - Wikipedia

    en.wikipedia.org/wiki/Discontinuity...

    A discontinuity may exist as a single feature (e.g. fault, isolated joint or fracture) and in some circumstances, a discontinuity is treated as a single discontinuity although it belongs to a discontinuity set, in particular if the spacing is very wide compared to the size of the engineering application or to the size of the geotechnical unit.

  6. Grain size - Wikipedia

    en.wikipedia.org/wiki/Grain_size

    Grain size (or particle size) is the diameter of individual grains of sediment, or the lithified particles in clastic rocks. The term may also be applied to other granular materials . This is different from the crystallite size, which refers to the size of a single crystal inside a particle or grain.

  7. Tessellation - Wikipedia

    en.wikipedia.org/wiki/Tessellation

    Any one of these three shapes can be duplicated infinitely to fill a plane with no gaps. [6] Many other types of tessellation are possible under different constraints. For example, there are eight types of semi-regular tessellation, made with more than one kind of regular polygon but still having the same arrangement of polygons at every corner ...

  8. The 16-person journey mounted in September 2023 from Tarawa, Kirbati, a port near Howland Island, and the team’s unmanned submersible scanned 5,200 square miles of ocean floor.

  9. Plate scale - Wikipedia

    en.wikipedia.org/wiki/Plate_scale

    The plate scale of a telescope connects the angular separation of an object with the linear separation of its image at the focal plane. If focal length f {\displaystyle f} is measured in mm, the plate scale in radians per mm is given by angular separation θ and the linear separation of the image at the focal plane s , or by simply the focal ...