Rocks And Minerals Flashcards
Rocks
Naturally occuring aggregate of minerals. Building blocks of lithosphere!
Rock Types
Igneous, sedimentary, metamorphic
Igneous
From “ignis” or fire. Formed by volcanic activity.
Examples, basalt or obsidian, granite or gabbro.
Classified into extrusive and intrusive.
Extrusive Igneous
Solidifies at Earth’s surface.
Lava is extrusive.
Intrusive Igneous
Solidifies before it breaks the surface.
Magma is intrusive.
Sedimentary
Lithification= sediments to sedimentary rock.
Sediments are uplift and weathering of rocks, transported and deposited elsewhere.
Classified into clastic and chemical.
Ex. Sandstone or conglomerate, halite or limestone.
Clastic Sedimentary
Formed by accumulation, compaction and cementation of particles from weathering. Particles are different shapes and sizes.
Chemical Sedimentary
Contains materials formed by chemical precipitation of minerals as a direct result of physical processes, or indirect result of life processes of water-dwelling animals.
Metamorphic Rocks
Came from pre-existing rocks that undergo changes in mineralogy, texture, and chemical composition. Pressure forces spaces between mineral grains to close, producing higher density, mor compact rock. At greater depth, may recrystallize and form into new mineral contained in rock.
Classified into foliated and non-foliated.
Ex. Gneiss or slate, quartzite or marble.
Foliated Metamorphic
Exhibits parallel alignment of minerals
Non-foliated Metamorphic
Produced when there is very little deformation and when parent rock has equidimensional crystals.
Mineralogy
Study of chemistry, crystal structure, and physical properties of minerals and mineralized artifacts.
Minerals
Building blocks of rocks! INORGANIC.
Naturally occuring chemical compounds
Homogenously solid
Each mineral has definite chemical composition
Each mineral has regular crystalling structure.
Properties of Minerals
Color, caused by reflection of visible light. Unreliable because impurities affect it.
Streak, color of powdered mineral and less variable than body color, often used in identification. Rubbing mineral on unglaze porcelain.
Crystal structure, individual orderly geometrical spatial arrangement of atoms.
Cleavage, tendency to split along weak points.
Luster, metallic or non-metallic shine
Specific gravity, relative density. May differ in different colors.
Hardness, if it can scratch or be scratched by another mineral.
Limestone use!
Cement, chalk