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  2. Pyrargyrite - Wikipedia

    en.wikipedia.org/wiki/Pyrargyrite

    Pyrargyrite is a sulfosalt mineral consisting of silver sulfantimonite, Ag 3 SbS 3. Known also as dark red silver ore, ruby blende, garnete blende or ruby silver, it is an important source of the metal. It is closely allied to, and isomorphous with, the corresponding sulfarsenide known as proustite or light red silver ore.

  3. Chlorargyrite - Wikipedia

    en.wikipedia.org/wiki/Chlorargyrite

    Chlorargyrite is the mineral form of silver chloride (AgCl). [5] Chlorargyrite occurs as a secondary mineral phase in the oxidation of silver mineral deposits. It crystallizes in the isometric–hexoctahedral crystal class. Typically massive to columnar in occurrence it also has been found as colorless to variably yellow cubic crystals.

  4. Roundness (geology) - Wikipedia

    en.wikipedia.org/wiki/Roundness_(Geology)

    The degree of roundness points to the range and mode of transport of clastic material, and can also serve as a search criterion in mineral exploration, especially for placer deposits. Alluvial debris in major rivers tend to exhibit a high degree of roundness. Alluvium from small rivers is less rounded.

  5. Sibilant - Wikipedia

    en.wikipedia.org/wiki/Sibilant

    The main distinction is the shape of the tongue. Most sibilants have a groove running down the centerline of the tongue that helps focus the airstream, but it is not known how widespread this is. In addition, the following tongue shapes are described, from sharpest and highest-pitched to dullest and lowest-pitched:

  6. Lustre (mineralogy) - Wikipedia

    en.wikipedia.org/wiki/Lustre_(mineralogy)

    Lustre (British English) or luster (American English; see spelling differences) is the way light interacts with the surface of a crystal, rock, or mineral.The word traces its origins back to the Latin lux, meaning "light", and generally implies radiance, gloss, or brilliance.

  7. Tridymite - Wikipedia

    en.wikipedia.org/wiki/Tridymite

    Two of the most common at standard pressure are known as α and β. The α-tridymite phase is favored at elevated temperatures (above 870 °C) and it converts to β-cristobalite at 1,470 °C. [4] [5] However, tridymite does usually not form from pure β-quartz, one needs to add trace amounts of certain compounds to achieve this. [6]

  8. Zonohedron - Wikipedia

    en.wikipedia.org/wiki/Zonohedron

    In geometry, a zonohedron is a convex polyhedron that is centrally symmetric, every face of which is a polygon that is centrally symmetric (a zonogon).Any zonohedron may equivalently be described as the Minkowski sum of a set of line segments in three-dimensional space, or as a three-dimensional projection of a hypercube.

  9. 4-polytope - Wikipedia

    en.wikipedia.org/wiki/4-polytope

    Just as a 3D shape can be projected onto a flat sheet, so a 4-D shape can be projected onto 3-space or even onto a flat sheet. One common projection is a Schlegel diagram which uses stereographic projection of points on the surface of a 3-sphere into three dimensions, connected by straight edges, faces, and cells drawn in 3-space. Sectioning