Chapter 1: Matter and Minerals Vocabulary

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Vocabulary practice flashcards generated from Foundations of Earth Science Chapter 1 lecture notes on matter, atomic structure, mineral properties, and mineral classifications.

Last updated 11:50 PM on 9/1/26
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31 Terms

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Mineralogy

The scientific study of minerals.

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Mineral

A naturally occurring, inorganic solid that possesses an orderly crystalline structure and a definite chemical composition.

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<p>Rock</p>

Rock

A naturally occurring solid mass of mineral, or mineral-like matter, usually consisting of an aggregate of several different minerals.

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Atom

The smallest particle of matter that cannot be chemically split.

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Proton

A subatomic particle found in the nucleus of an atom that carries a charge of +1+1.

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Neutron

A subatomic particle located in the nucleus of an atom that possesses no charge (00).

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Electron

A subatomic particle with a charge of 1-1 and a mass approximately 1/20001/2000 that of a proton or neutron, surrounding the nucleus in a cloud.

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Valence Electrons

The electrons located in the outermost principal shell of an atom that interact with other atoms to form chemical bonds.

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Atomic Number

The number of protons in the nucleus of an atom, which determines its chemical nature.

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Element

A substance composed of atoms that all have the same atomic number and identical chemical properties.

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Octet Rule

A chemical principle stating that atoms tend to gain, lose, or share electrons until they are surrounded by eight valence electrons.

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Chemical Bond

The transfer or sharing of electrons that lowers the total energy of atoms and results in a full valence shell.

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Ionic Bond

A chemical bond formed when valence electrons are transferred from one atom to another, producing oppositely charged ions that attract each other.

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Covalent Bond

A chemical bond produced when electrons are shared between atoms.

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Metallic Bond

A chemical bond created when valence electrons are free to move from one atom to another among all available atoms.

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Luster

The quality of light reflected from the surface of a mineral, classified as metallic, submetallic, or nonmetallic.

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Streak

The color of a mineral in powdered form, determined by rubbing the sample on an unglazed porcelain streak plate.

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Crystal Shape or Habit

The characteristic shape of individual mineral crystals or aggregates of crystals.

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Hardness

A mineral's resistance to abrasion or scratching.

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<p>Mohs Scale</p>

Mohs Scale

A relative scale ranging from 11 to 1010 used to measure mineral hardness against ten standard index minerals.

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<p>Cleavage</p>

Cleavage

The tendency of a mineral to break along planes of weak chemical bonding, producing smooth, flat surfaces.

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Fracture

The pattern of breakage in a mineral with chemical bonds equal in strength in all directions, forming irregular or smooth curved (conchoidal) surfaces.

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Tenacity

A mineral's resistance to breaking, bending, cutting, or deforming under stress.

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Specific Gravity

A ratio describing density, equal to the weight of a mineral divided by the weight of an equal volume of water.

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<p>Rock-Forming Minerals</p>

Rock-Forming Minerals

The few dozen abundant minerals that compose the majority of Earth's crust.

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Silicates

The most common mineral group in Earth's crust, comprising over 90%90\% of the crust and built from silicon and oxygen.

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<p>Silicon-Oxygen Tetrahedron</p>

Silicon-Oxygen Tetrahedron

The fundamental building block of all silicate minerals, consisting of four oxygen atoms (O2O^{2-}) covalently bonded to a central silicon atom (Si4+Si^{4+}), forming the complex ion SiO44SiO_4^{4-}.

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Feldspars

The most plentiful group of silicate minerals, making up over 50%50\% of Earth's crust.

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Quartz

The second-most-abundant mineral in continental crust, composed entirely of silicon and oxygen (SiO2SiO_2).

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Dark Silicate Minerals

Silicate minerals containing iron and magnesium, characterized by dark color and high specific gravity.

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<p>Nonsilicate Minerals</p>

Nonsilicate Minerals

Mineral groups lacking silicon-oxygen tetrahedra, making up about 8%8\% of Earth's crust and classified by their common negative ions into groups such as carbonates, halides, oxides, sulfides, sulfates, and native elements.