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Minerals yay

QuestionAnswer
Naturally occurring Naturally occurring: Created by nature.
Inorganic Inorganic: Cannot be created using any living thing, only NON-living.
Solid Solid: Minerals have a definite volume, and shape
Crystal Structure Crystal Structure: particles of a mineral lines up in a pattern over and over again
Definite chemical composition Definite chemical composition: A mineral has definite chemical make-up of certain elements.
Mohs hardness scale Mohs hardness scale: Identifies hardness from softest to hardest of ten minerals.
Color Color: Easily observed physical property.
Streak Streak: The color of the minerals powder is easily observed
Luster Luster: Its reflection of light in the minerals surface.
Density Density: How tightly packed the matter is in the mineral.
Crystal system Crystal system: The minerals actual polygon shape, example cube, or hexagon.
Cleavage Cleavage: Mineral breaks along a flat surface, smooth break.
Fracture Fracture: Mineral breaks in an irregular way, jagged and uneven.
Crystallization through melted materials Crystallization through melted materials: form from magma that cools inside the crust or lava that cools on the surface. Magma cools slowly creating large minerals, and lava cools quickly creating small minerals.
Minerals in Hot Water Solution Minerals in Hot Water Solution: Magma heats water to very high temperatures, when the hot water cools the water and leaves the solution that creates the crystallization.
Where minerals are found Where minerals are found: Many rare and valuable minerals are found in or near volcanic activity, mountain building, and bodies of water
Gemstones Gemstones: Using minerals such as rubies and sapphires for jewelry
Metals Metals: Using minerals such as aluminum, iron, copper, and silver, to make other items we use or want.
Ores Ores: a rock that contains metal or useful minerals
Prospector Prospector: someone who looks for ore deposits.
Mining Mining
Rocks 1. Rocks: Make up the earth's crust, that are made of a mixture of minerals and other materials
Mineral Composition Mineral Composition: geologists use a microscope to observe the shape and size of the rock’s crystals.
Sedimentary Sedimentary: forms in layers from sediment
Igneous Igneous: forms from magma or lava
Metamorphic Metamorphic: formed deep underground with heat & pressure
Igneous Rocks Igneous Rocks: formed from intense heat that comes from magma or lava.
Extrusive Rocks Extrusive Rocks: igneous rocks formed from lava that erupted onto Earth's surface
Intrusive Rocks Intrusive Rocks: igneous rocks formed from magma that hardens beneath Earth's surface.
Texture Texture: depends upon the size and shape of the crystals
Porphyritic texture Porphyritic texture: large crystals surrounded by small crystals, which form when magma cools in two stages.
Uses of Igneous Rocks Uses of Igneous Rocks: Used because they are hard, dense, and durable
Basalt Basalt: gravel
Pumice Pumice: cleaning and polishing
Perlite Perlite: soil mixes
Obsidian Obsidian: sharp tools
Granite Granite: building materials
Sedimentary Rocks Sedimentary Rocks: formed from layers of sediment deposited by water and wind;
sediment sediment: small solid pieces of rock or living things.
Changing sediments to rocks: A. Erosion: wind or water carry sediments B. Deposition: when the water or wind stops carrying the sediments C. Compaction: presses sediments together D. Cementation: when dissolved minerals and sediment glue together.
Clastic Rocks Clastic Rocks: formed sedimentary rocks are squeezed together
Examples of clastic rocks: Examples of clastic rocks: shale, sandstone, conglomerate, and breccia
Organic Rocks Organic Rocks: formed when layers of plants and animals are deposited in thick layers
Examples of organic rocks: Examples of organic rocks: coal, and limestone
Chemical Rocks Chemical Rocks: when minerals are dissolved in a solution crystallize
Uses of Sedimentary Rocks: Uses of Sedimentary Rocks: A. Limestone and sandstone: building materials B. Coal: fossil fuel
Metamorphic Rocks: Metamorphic Rocks: formed from heat and pressure deep beneath the earth's surface change sedimentary and igneous rocks into metamorphic
Grains Grains: the arrangement of the grains
Foliated Foliated: grains arranged in parallel layers or bands
Non-foliated Non-foliated: mineral grains are arranged randomly
Marble Marble: building materials
Slate Slate: flooring, roofing, chalkboards
Limestone changes to marble
Sandstone changes to quartzite
Shale changes to slate
Granite changes to gneiss
The Rock Cycle: The Rock Cycle: Forces inside the Earth and at the surface of the Earth produce a rock cycle that builds, destroys, and changes the rocks in the crust.
Subducting Oceanic Plates: Subducting Oceanic Plates: Plate movements (downward) drive the rock cycle by pushing rocks back into the mantle, where they melt and become magma again.
Colliding Continental Plates: .Colliding Continental Plates: Plate movement that causes folds, faulting, and uplifting of the crust that move rocks through the rock cycle.
Created by: user-2003738
 



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