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  2. Rectangular cuboid - Wikipedia

    en.wikipedia.org/wiki/Rectangular_cuboid

    its volume is the product of the rectangular area and its height: =. its surface area is the sum of the area of all faces: = (+ +). its space diagonal can ...

  3. Soma cube - Wikipedia

    en.wikipedia.org/wiki/Soma_cube

    The pieces of a Soma cube The same puzzle, assembled into a cube. The Soma cube is a solid dissection puzzle invented by Danish polymath Piet Hein in 1933 [1] during a lecture on quantum mechanics conducted by Werner Heisenberg.

  4. Cube - Wikipedia

    en.wikipedia.org/wiki/Cube

    The volume of a cuboid is the product of its length, width, and height. Because all the edges of a cube are equal in length, the formula for the volume of a cube as the third power of its side length, leading to the use of the term cubic to mean raising any number to the third power: [ 7 ] [ 6 ] V = a 3 . {\displaystyle V=a^{3}.}

  5. Tetragonal crystal system - Wikipedia

    en.wikipedia.org/wiki/Tetragonal_crystal_system

    An example of the tetragonal crystals, wulfenite Two different views (top down and from the side) of the unit cell of tP30-CrFe (σ-phase Frank–Kasper structure) that show its different side lengths, making this structure a member of the tetragonal crystal system.

  6. Close-packing of equal spheres - Wikipedia

    en.wikipedia.org/wiki/Close-packing_of_equal_spheres

    Illustration of the close-packing of equal spheres in both HCP (left) and FCC (right) lattices. In geometry, close-packing of equal spheres is a dense arrangement of congruent spheres in an infinite, regular arrangement (or lattice).

  7. Disphenoid - Wikipedia

    en.wikipedia.org/wiki/Disphenoid

    A tetrahedron is a disphenoid if and only if its circumscribed parallelepiped is right-angled. [9]We also have that a tetrahedron is a disphenoid if and only if the center in the circumscribed sphere and the inscribed sphere coincide.

  8. Dilatancy (granular material) - Wikipedia

    en.wikipedia.org/wiki/Dilatancy_(granular_material)

    A sample of a material is called dilative if its volume increases with increasing shear and contractive if the volume decreases with increasing shear. [7] [8] Dilatancy is a common feature of soils and sands. Its effect can be seen when the wet sand around the foot of a person walking on beach appears to dry up.