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Naturally occurring solid, formed by geologic processes, that has a crystalline structure and a definable chemical composition. |
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Measure of the relative ability of a mineral to resist scratching. The atoms or ions in crystals of a hard mineral are more strongly bonded that those in a soft mineral. |
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Mineral hardness in relation to common household items. |
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Mineral hardness in relation to common household items. |
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Refers to the shape of a single crystal with well-formed crystal faces. |
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If a mineral breaks to form distinct planar surfaces that have a specific orientation in relation to crystal structure. |
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Oxygen atoms are positioned in the corners of a tetrahedron, a pyramid like shape with four triangular faces. Si has a charge of plus 4 and oxygen a charge of minus 2. |
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The tetrahedral are independent and do not share any oxygen atoms. |
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In a single chain silicate, the tetrahedral link to form a chain by sharing two oxygen atoms. |
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The tetrahedral form a double chain by sharing two or three oxygen atoms. |
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The tetrahedral share three oxygen atoms and therefore link to form two-dimensional sheets. |
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Each tetrahedron shares all four oxygen atoms with its neighbors, forming a three-dimensional structure. |
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At what pressure are rocks most stable? |
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Number of protons found in the nucleus of an atom. |
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Total mass of protons, neutrons and electrons in a single atom. |
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Ion with more electrons than protons. |
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Fewer electrons than protons. |
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Chemical bond formed between a cation and an anion. |
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Chemical bond characterized between the sharing of electrons between atoms. |
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The covalent bonding between atoms in metals, in which the valence electrons move freely. |
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Ability of a solid material to exist in more than one form or crystal structure. |
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Type of chart used to show conditions at which thermodynamically distinct phases can occur at equilibrium. |
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