Minerals/Mining Quiz Unit 7
5 characteristics of minerals
Must occur naturally in the earth
Must be inorganic
Are always solids
Definite chemical composition
Have atoms that are arranged in a definite repeating pattern (crystal structure)
6 physical properties of minerals
Color
Luster
Hardness
Streak: The color of the powder scraped off a mineral when it is rubbed against a hard, rough surface.
Density: mass/volume
Cleavage and Fracture
Cleavage: Breaking along certain lines
Fracture: jagged, rough breaks
Mohs scale
1 is the softest (talc) and 10 is the hardest (diamond)
5 examples of how minerals used in everyday life
Food, Buildings, Cosmetics, Electronics, Jewerly
Pg 8-Stratigraphy, uniformitarianism, how would you determine the most recent rock layer formed
Stratigraphy: the study of how rock layers are formed
Uniformitarianism: the same processes of erosion, deposition, and subterranean heat that were currently observable had formed the current land forms slowly over millions of years
Pg 10-Know the characteristics of igneous rock types (felsic, mafic, ultra mafic, intermediate)
Felsic: Low in Iron and High in silica, made of light colored materials (EX: Granite)
Mafic: High in Magnesuem and Iron, made of darker colored materials and are heavier (EX: Basalt)
Ultra Mafic: 90% of mafic materials and are low in silica
Intermediate: Composition between mafic and felsic (EX: andesite)
Pg 10-Know the 4 textures of igneous rocks (porphyritic, fine grained, coarse grained, glassy)
Porphyritic: Large and small crystals combined because of slow cooling then eventually rapid cooling when getting closer to the surface
Fine Grained: Made of small interlocking crystals because the magma hardened and cooled rapid once reaching the earth’s surface (Basalt)
Coarse grained: Interlocking mineral crystals that are bigger because it hardens slowly
Glassy: A shiny/polished look, magma hardened quick so there was no time for crystals to form. EX: obsidian
Pg 11-Know the 4 types of metamorphism (contact, dynamic, regional, hydrothermal)
Contact: Magma comes in contact with an existing rock
Dynamic: From mountain formations, huge pressure bends, folds, and crush the existing rock
Regional: Large amounts of rock are altered because of the high pressure+temperature as they are pushed deep within the earth
Hydrothermal: Rock comes into contact with hot fluids near ocean vents
Pg 12-Know the 3 types of sedimentary rocks (clastic-shale, chemical-gypsum, organic-coal)
Clastic-shale: formed from weathering or erosion of any preexisting rock. Running water rounds the fragments. They get deposited because the water begins to slow and the sediments get sorted to later become different sedimentary rocks
Chemical-Gypsum: can be found at the bottom of dried up lakes, swamps, or the sea. Minerals have fallen out of solution/water has evaporated and left behind the mineral sediments
Organic-Coal: remains of plants and animals(fossils)
Pg 13-Know the rock cycle diagram
Weathering and Erosion
Deposition
Cementation: materials broken down by weathering, transported by erosion, and then glued together to make sedimentary rocks
Metamorphism: rocks are buried deep, heat/pressure/ chemical reactions change them into metamorphic rocks
Magma: Igneous rocks from cooling and hardening of magma
Crystallization
Pg 14-Mining process:
Prospecting/Surveying:
Exploration
Design/Planning
Development
Production
Reclamation
Pg 15-Surface versus subsurface mining
Surface
Pros: Less Expensive, Safer
Cons:Alters large portions of the landscape, increased erosion, destruction of habitats
Subsurface
Pros: Less Surface Damage
Cons: More expensive, Additional safety concerns, Acidic Water conditions
Pg 16-Restoration and reclamation of mines
Restoration: A legal term that involves returning a disturbed site to a more or less natural state
Reclamation: The rehabilitation of a disturbed site for a useful and desirable purpose