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inorganic naturally occurring solids that have specific chemical compositions, an internal crystalline structure, and form through geologic processes.
physically and chemically distinctive.
building blocks of rocks and composititionally inorganic.
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one in which the atoms are arranged in a three-dimensional, regularly repeating orderly pattern.
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the basic building block of the elements.
smallest, electrically neutral assemblies of energy and matter that we know exist in the universe.
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tiny charged particles.
neutralized as they crowd in around a central core of positively charged protons.
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protons and neutrons
protons are +1 charge
neutrons are neutral
electrons have -1 charge
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Term
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Definition
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atoms with the same number of protons but different numbers of neutrons and therefore different atomic masses.
contain different numbers of neutrons but the same number of protons. either stable or unstable. unstavle ones are those in which protons or neutrons are lost from nucleus.
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defined by the number of protons in its nucleus.
oxygen has 8 protons, making that its atomic number.
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electrically charged atom.
positively (cation) or negatively (anion) charged atoms.
protons and electrons are not balanced.
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ionic bonds form between cation and anions due to attraction between positive and negative charges of each
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covalent bonds form through sharing of outer (valence) electrons between atoms
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oxygen combined with silicon.
2nd most abundant element in crust.
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substances that contain silica.
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oxygen is most abundant element in the crust, silicon is second.
iron is most abundant by mass for bulk earth.
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Term
| important crustal minerals |
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Definition
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Most rock-forming minerals are silicates: Feldspars,
Pyroxenes, Amphiboles, Quartz, Micas, Olivine. Some important non-silicates are:
Calcite, Dolomite, Gypsum, oxides and sulfides
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Term
| silicon-oxygen tetrahedron |
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Definition
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basic building block of a crystal.
4 oxygen ions bonded to one silicon ion. -4 net charge.
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Term
| isolated silicate structure |
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Definition
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silicate minerals that are structured so that none of the oxygen atoms is shared by tetrahedrons
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Definition
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two of a tetrahedron's oxygen atoms are shared with adjacent tetrahedrons to form a chain.
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each tetrahedron shares three oxygen atoms to form a sheet
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Term
| framework silicate structure |
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Definition
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all four oxygen ions are shared by adjacent tetrahedrons.
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Term
| physical properties of minerals |
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Definition
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color, hardness, streak, luster, external form, cleavage, density, chemical tests, special properties
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