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  2. Snowflake - Wikipedia

    en.wikipedia.org/wiki/Snowflake

    In colder air down to −8 °C (18 °F), the crystals form as hollow columns, prisms or needles. In air as cold as −22 °C (−8 °F), shapes become plate-like again, often with branched or dendritic features. At temperatures below −22 °C (−8 °F), the crystals become plate-like or columnar, depending on the degree of saturation.

  3. Ice crystal - Wikipedia

    en.wikipedia.org/wiki/Ice_crystal

    Ice crystals create optical phenomena like diamond dust and halos in the sky due to light reflecting off of the crystals in a process called scattering. [1] [2] [15] Cirrus clouds and ice fog are made of ice crystals. [1] [16] Cirrus clouds are often the sign of an approaching warm front, where warm and moist air rises and freezes into ice ...

  4. Crystallization - Wikipedia

    en.wikipedia.org/wiki/Crystallization

    The crystals are captured, stored, and sputter-coated with platinum at cryo-temperatures for imaging. The crystallization process appears to violate the second principle of thermodynamics. Whereas most processes that yield more orderly results are achieved by applying heat, crystals usually form at lower temperatures – especially by ...

  5. Crystal - Wikipedia

    en.wikipedia.org/wiki/Crystal

    Likewise, if a substance can form crystals, it can also form polycrystals. For pure chemical elements, polymorphism is referred to as allotropy . For example, diamond and graphite are two crystalline forms of carbon , while amorphous carbon is a noncrystalline form.

  6. Crystal structure - Wikipedia

    en.wikipedia.org/wiki/Crystal_structure

    In crystallography, crystal structure is a description of ordered arrangement of atoms, ions, or molecules in a crystalline material. [1] Ordered structures occur from intrinsic nature of constituent particles to form symmetric patterns that repeat along the principal directions of three-dimensional space in matter.

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  8. Fractional crystallization (geology) - Wikipedia

    en.wikipedia.org/wiki/Fractional_crystallization...

    Fractional crystallization, or crystal fractionation, is one of the most important geochemical and physical processes operating within crust and mantle of a rocky planetary body, such as the Earth. It is important in the formation of igneous rocks because it is one of the main processes of magmatic differentiation . [ 1 ]

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