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Luster
The way a mineral reflects light, categorized as metallic or nonmetallic.
Streak
The color of a mineral when it is powdered; often more reliable than surface color.
Hardness
A measure of a mineral's resistance to scratching, assessed using tools like a fingernail or glass.
Cleavage
The tendency of a mineral to break along flat planes.
Fracture
The irregular or curved breakage of a mineral, not along flat planes.
Density
The mass of a mineral per unit volume, often used for identification.
Magnetism
The property of attracting or repelling certain materials, helpful in mineral identification.
Acid Reaction
A mineral's response to acid, indicated by fizzing if carbonates are present.
Intrusive
Igneous rocks formed from slow cooling magma beneath the Earth's surface, resulting in coarse texture.
Extrusive
Igneous rocks formed from fast cooling lava at the Earth's surface, typically fine-grained.
Felsic
A composition of igneous rocks that are light-colored and high in silica.
Mafic
Igneous rocks that are darker in color and rich in iron and magnesium.
Clastic Sedimentary Rocks
Rocks formed from the accumulation and lithification of fragments of pre-existing rocks.
Grain Size
A classification criterion for sediments and sedimentary rocks, indicating particle diameter.
Sorting
A measure of the uniformity of grain sizes in sediment, indicating the energy of transportation.
Foliation
The alignment of minerals within a metamorphic rock, indicative of pressure during metamorphism.
Superposition
A principle stating that in undisturbed sedimentary rock layers, the oldest layer is on the bottom.
Cross-Cutting Relationships
Geological principle that states that an intrusion or fault is younger than the rocks it cuts through.
Bowen’s Reaction Series
A sequence that explains the order of mineral crystallization from cooling magma.
Fractional Crystallization
A process where early formed crystals are removed from the melt, changing the composition of the remaining liquid.
Index Fossils
Fossils used to identify and date the specific time frame of the rock in which they are found.
Contact Metamorphism
Metamorphism that occurs when rocks are heated by nearby molten rock.
Regional Metamorphism
Metamorphism that occurs over large areas due to heat and pressure.
Sedimentary Structures
Features in sedimentary rocks, such as fossils and mud cracks, that provide insights into the depositional environment.
Mineral Identification
The process of identifying minerals using multiple properties such as hardness, streak, and luster.