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  2. Quartzite - Wikipedia

    en.wikipedia.org/wiki/Quartzite

    Quartzite statue of an Egyptian Pharaoh, 14th century BCE [22] Quartzite biface hand axe from Stellenbosch, South Africa. Quartzite is a decorative stone and may be used to cover walls, as roofing tiles, as flooring, and stairsteps. Its use for countertops in kitchens is expanding rapidly. It is harder and more resistant to stains than granite.

  3. Metamorphic rock - Wikipedia

    en.wikipedia.org/wiki/Metamorphic_rock

    Quartzite is sufficiently hard and dense that it is difficult to quarry. However, some quartzite is used as dimension stone, often as slabs for flooring, walls, or stairsteps. About 6% of crushed stone, used mostly for road aggregate, is quartzite. [4] Marble is also prized for building construction [47] and as a medium for sculpture. [6]

  4. Foliation (geology) - Wikipedia

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

    Quartzite, a non-foliated metamorphic rock. Foliation in geology refers to repetitive layering in metamorphic rocks. [1] Each layer can be as thin as a sheet of paper, or over a meter in thickness. [1] The word comes from the Latin folium, meaning "leaf", and refers to the sheet-like planar structure. [1]

  5. List of rock types - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_types

    Epidosite – Hydrothermally altered epidote- and quartz-bearing rock; Felsite – Very fine-grained volcanic rock that sometimes contains larger crystals; Flint – Cryptocrystalline form of the mineral quartz; Ganister – Hard, fine-grained quartzose sandstone, or orthoquartzite; Gossan – Intensely oxidized, weathered or decomposed rock

  6. Texture (geology) - Wikipedia

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

    In geology, texture or rock microstructure [1] refers to the relationship between the materials of which a rock is composed. [2] The broadest textural classes are crystalline (in which the components are intergrown and interlocking crystals), fragmental (in which there is an accumulation of fragments by some physical process), aphanitic (in which crystals are not visible to the unaided eye ...

  7. Slate - Wikipedia

    en.wikipedia.org/wiki/Slate

    The texture of the slate is totally dominated by these pervasive cleavage planes. Under a microscope, the slate is found to consist of very thin lenses of quartz and feldspar (QF-domains) separated by layers of mica (M-domains). [8] These are typically less than 100 μm (micron) thick. [4]

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