yes all triangular pyramids are tetrahedra!!!!!!!!!!!!!
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It is a type of silicates in which all four oxygen atoms of the silicate tetrahedra are shared with neighboring tetrahedra.
Silicon-oxygen tetrahedra with each tetrahedra sharing the oxygen atoms to give it the structure of SiO2 overall.
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Another name is tetrahedra
A bridging oxygen is the oxygen that two SiO4 tetrahedra share in a crystal structure. A non bridging oxygen is any other oxygen that is not shared by two tetrahedra.
tetrahedra (a pyramid with a triangular base)
Not exactly. A tetrahedron is a polyhedron. Many tetrahedra are polyhedra.
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for what number of tereahedra exist kaleidocycle
The simple answer is... Feldspar has a much higher complex and stable tetrahedral orientation in comparison to that of any other Silicate variation higher up on the reation series latter. Feldspar is one of the most stable variations in orientation of, what boils down to, silicate tetrahedra. Because Feldspar is technically a form of silicate tetrahedra orientation, I am assuming you are asking how the silicate tetrahedra orientations vary from its most simple (i.e. Olivine) to its mosts complex (i.e. quartz/FELDSPAR) forms. Esentially a Silicate Ion SiO4^-4 is the most basic building block of FELDSPAR. Knowing this, as you move from the top of Bowen's reaction series, we see a gradual stabilization of the various Silicate tetrahedral orientations. These orientations include (in order of stability/complexity): [TOP OF REACTION SERIES] Individual (Singular form) Silicate Tetrahedra (i.e. Olivine) Chain (Linear form) Silicate Tetrahedra (i.e. Pyroxine) Double Chain (Bilinear form) Silicate Tetrahedra (i.e. amphibole) Sheet Silicate Tetrahedra ('2-D' form) (i.e. Mica: Biotite or Muscovite) Framework Silicate Tetrahedra ('3-D' form) (i.e. FELDSPAR) [BOTTOM OF REACTION SERIES]