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A set of vocabulary flashcards covering mineral criteria, rock types, common minerals, and bonding concepts discussed in the video lecture.
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Mineral
A solid, naturally occurring, inorganic substance with a definite chemical composition and an orderly internal crystal structure.
Naturally occurring
Formed by geological processes, not manufactured by humans.
Inorganic
Not derived from living matter; minerals formed without biological input.
Chemical composition
The specific combination and proportion of elements that make up a mineral.
Crystal structure
The orderly, repeating arrangement of atoms in a mineral.
Ice
Solid water; ice is a mineral because it has a definite structure, unlike liquid water.
Water
Liquid H2O; not a mineral because it lacks a definite crystalline structure.
Crystalline rock
Rock that contains visible crystals formed by crystal growth.
Clastic rock
Rock made of broken fragments (clasts) of other rocks, often layered.
Thin section
A very thin slice of rock (~4 microns) prepared for microscopic study of minerals.
Scale
The size reference from landscapes to individual grains used when studying rocks.
Luster
The way a mineral's surface reflects light (e.g., metallic or non‑metallic shine).
Hardness
Resistance to scratching on the Mohs scale; higher numbers scratch lower ones.
Streak
The color of a mineral’s powder when rubbed on a porcelain plate.
Cleavage
A mineral’s tendency to break along flat, well‑defined planes.
Specific gravity
A mineral’s density relative to water.
Magnetism
Magnetic property used to identify minerals (e.g., magnetite).
Silicate
A major group of minerals built from silicon‑oxygen tetrahedra; the most common rock‑forming minerals.
Carbonate
Minerals containing carbonate groups (CO3); many fizz in acids (e.g., calcite, dolomite).
Oxide
Minerals composed of oxygen with metals (e.g., magnetite, hematite).
Halide
Minerals formed from halogen salts; halite (NaCl) is a common evaporite halide.
Sulfate
Minerals containing sulfate groups (SO4); gypsum is a common example.
Sulfide
Minerals containing sulfur bound to a metal (e.g., pyrite, galena).
Olivine
A green silicate mineral common in mantle rocks and some crustal rocks.
Feldspar
A group of abundant rock‑forming silicates; common in granitic rocks.
Quartz
A hard, widely distributed silicate mineral; a major building block of many rocks.
Calcite
A carbonate mineral that fizzes with acid; helps distinguish carbonates.
Dolomite
A carbonate mineral similar to calcite; also reacts with acid under certain conditions.
Halite
Sodium chloride; halide mineral that forms cubic crystals from evaporites.
Gypsum
Calcium sulfate; used in drywall; an evaporite mineral.
Magnetite
Iron oxide with strong magnetic properties; important ore.
Hematite
Iron oxide mineral; another major iron ore; typically reddish with metallic luster.
Pyrite
Iron sulfide; known as fool’s gold; common sulfide mineral.
Galena
Lead sulfide; a dense, metallic ore with cubic cleavage.
Diamond
Carbon allotrope with a covalent network; the hardest natural material.
Graphite
Carbon allotrope with a layered structure; softer; used in pencils.
Covalent bonding
Strong bond formed by sharing electrons between atoms.
Ionic bonding
Bonding through electrostatic attraction between oppositely charged ions.
Metallic bonding
Bonding in metals with a 'sea' of electrons; supports conductivity and malleability.
Van der Waals forces
Weak intermolecular forces that influence how minerals interact and stick together.
Weathering vs erosion
Weathering: breakdown of rocks; erosion: movement of the broken material.
Oxygen abundance
Oxygen is the most abundant element in Earth’s crust.
Continental crust vs oceanic crust
Continental crust is less dense and granitic; oceanic crust is denser and mafic (iron‑rich).
Efflorescence
Precipitation of salts on surfaces from moisture moving through rock.
Amethyst
Purple variety of quartz.
Muscovite
Light mica with one plane of cleavage; can be peeled into sheets.
Biotite
Dark mica with one plane of cleavage; common in many rocks.