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111 Cards in this Set
- Front
- Back
CHAPTER 1
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CHAPTER 1
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astronomy
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the study of objects beyond Earth's atmosphere
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meteorology
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the study of the air that surrounds our planet
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geology
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the study of materials that make up Earth and the processes that form and change these materials
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oceanography
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the study of Earth's oceans
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lithosphere
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the rigid outer shell of the planet and includes the crust and the mantle
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asthenosphere
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partially molten, plasticlike, flowing layer located below the solid part of Earth's mantle
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hydrosphere
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the water in Earth's oceans, seas, lakes, rivers and glaciers, and the water in the atmosphere
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atmosphere
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the blanket of gases that surrounds our planet
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biosphere
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all organisms on Earth as well as the environments in which they live
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independent variable
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the factor that is manipulated by the experimenter
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dependent variable
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a factor that can change if the independent variable is changed
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control
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used in an experiment to show that the results of an experiment are actually a result of the condition being tested
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Le Systeme International d'Unites (SI)
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a system that is a modern version of the metric system
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law
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a basic fact that describes the behavior of a natural phenomenon
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scientific notation
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a type of shorthand used to express the number as a multiplier and a power of ten
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theory
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an explanation based on many observations during the repeated experiments
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CHAPTER 2
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CHAPTER 2
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cartography
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the science of mapmaking
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equator
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that imaginary line that lies at 0 degrees latitude and circles Earth midway between the north and south poles
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latitude
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the distance in degrees north or south of the equator
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longitude
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the distance in degrees east or west of the prime meridian
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prime meridian
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imaginary line representing 0 degrees longitude, running from the north pole, through Greenwich, ENgland, to the south pole
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International Date Line
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180 degress meridian and serves as the transition line for calendar days
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topographic maps
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show changes in elevation of Earth's surface
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contour line
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connect points of equal elevation
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contour interval
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the difference in elevation between two side-by-side contour lines
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map legend
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explains what the symbols represent on a map
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map scale
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the ration between distances on a map and actual distances on the surface of Earth
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remote sensing
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the process of collecting data about Earth from far above Earth's surface
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electromagnetic spectrum
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the arrangement of electromagnetic radiation according to wavelengths
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frequency
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the number of waves that pass a particular point each second
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Landsat satellite
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information-gathering satellite that uses visible light and infrared radiation to map Earth's surface
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Topex/Poseidon satellite
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data-gathering satellite that uses radar to map features on the ocean floor
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Global Positioning System (GPS)
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Satellite-based navigation system that permits a user to pinpoint his or her exact location on Earth
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sonar
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the use of sound waves to detect and measure objects underwater
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CHAPTER 3
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CHAPTER 3
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element
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a substance that cannot be broken down into simpler substances by physical or chemical means
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atom
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the smallest particle of an element that has all of the characteristics of that element
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nucleus
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made up of protons and neutrons
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protron
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a tiny particle that has mass and a positive electrical charge
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neutron
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a particle with about the same mass as a protron, but it is electrically neutral, has no electrical charge
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atomic number
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the number of protons in an atom's nucleus
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mass number
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the combined number of protons and neutrons
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electron
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has little mass, but has a negative electrical charge that is exactly the same magnitude as the positive charge of a proton
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energy level
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represents the area in an atom where an electron is most likely to be found
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valence electrons
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electrons in the outermost energy level
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isotopes
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atoms of the same element have different mass numbers
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atomic mass
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average of the mass numbers of the isotopes of an element
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radioactivity
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the spontaneous process through which unstable nuclei emit radiation
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compound
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a substance that is composed of atoms of two or more different elements that are chemically combined
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chemical bonds
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the forces that hold the elements together in a compound
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covalent bond
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the attraction of two atoms for a shared pair of electrons that holds the atoms together
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molecule
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two or more atoms held together by covalent bonds
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ion
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an atom that gains or loses an electron and is charged
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ionic bond
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the attractive force between two ions of opposite charge
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chemical reaction
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the change of one or more substances into other substances
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solution
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homogeneous mixture whose components cannot be distinguished and can be classified as liquid, gaseous, solid or a combination
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acid
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a solution containing a substance that produces hydrogen ions in water
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crystalline structure
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when particles in a solid are arranged in regular geometric patterns
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glasses
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solids that consist of densely packed atoms arranged at random
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evaporation
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the process of change from a liquid to a gas
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sublimation
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the change of state from a solid to a gas without an intermediate liquid state
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plasmas
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hot, highly ionized, electrically conducting gases
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condensation
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the change from a gas to a liquid
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CHAPTER 4
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CHAPTER 4
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mineral
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a naturally occurring, inorganic solid with a specific chemical composition and a definite crystalline structure
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crystal
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a solid in which the atoms are arranged in repeating patterns
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magma
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molten material found beneath Earth's surface
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silicates
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minerals that contain silicon and oxygen and usually one or more other elements
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luster
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the way that a mineral reflect light from its surface
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streak
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the color of a mineral when it is broken up and powdered
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hardness
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a measure of how easily a mineral can be scratched
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cleavage
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a mineral that splits relatively easily and evenly along one or more flat planes
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fracture
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minerals that break with rough or jagged edges
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specific gravity
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the ratio of the weight of a substance to the weight of an equal volume of water at 4 degrees Celsius
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ore
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a mineral that contains a useful substance that can be mined at a profit
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gems
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valuable minerals that are prized for their rarity and beauty
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CHAPTER 5
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CHAPTER 5
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igneous rocks
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intrusive or extrusive rock formed from the cooling and crystallization of magma; can be classified as felsic, mafic, intermediate, and ultramafic, according to its mineral composition
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lava
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magma that flows out onto Earth's surface
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extrusive
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fine-grained igneous rocks that cool quickly on Earth's surface
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intrusive
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coarse-grained igneous rocks that cool slowly beneath Earth's surface
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partial melting
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the process whereby some minerals melt at low temperatures while other minerals remain solid
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fractional crystallization
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the process wherein different minerals form at different temperatures
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Bowen's reaction series
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illustrates the relationship between cooling magma and mineral formation
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felsic
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light-colored, have high silica contents and contain quartz and the feldspars orthoclase and plagioclase
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mafic
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dark-colored, have lower silica contents and contain plagioclase, biotite, amphibole, pyroxene and olivine and are rich in iron and magnesium
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ultramafic
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have low silica contents and very high levels or iron and magnesium
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porphyritic
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characterized by large, well-formed crystals surrounded by finer-grained crystals of the same mineral or different minerals
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pegmatites
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veins of extremely large-grained minerals
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kimberlites
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rare, ultramafic rocks
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CHAPTER 6
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CHAPTER 6
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sediments
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pieces of solid material that have been deposited on Earth's surface by wind, water, ice, gravity or chemical precipitation
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clastic
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rock and mineral fragments produced by weathering
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deposition
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when sediments are laid down on the ground or sink to the bottoms of bodies of water
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lithification
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the physical and chemical processes that transform sediments into sedimentary rocks
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cementation
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when mineral growth cements sediment grains together into solid rock
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bedding
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horiztonal layering
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graded bedding
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bedding in which the particle sizes become progressively heavier and coarser towards the bottome layers
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cross-bedding
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formed as inclined layers of sediment more foward across a horizontal surface
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clastic sedimentary rocks
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the most common type of sedimentary rocks and are formed from the abundant deposits of loose sediments found on Earth's surface
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porosity
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the percentage of open spaces between grains in a rock
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evaporites
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the layers of chemical sedimentary rocks that oform as a resultregional metamorphism
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regional metamorphism
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when high teperature and pressure affect large regions of Earth's curst, they form large belts of this
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contact metamorphism
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when molten rocks come in contact with solid rock
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hydrothermal metamorphism
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when very hot water reacts with rock and alters its chemistry and mineralogy
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foliated
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wavy layers and bands of minerals
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nonfoliated
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lack mineral grains with long axes in one direction
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porphyroblasts
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large crystals that form in solid rock by the reorganization of atoms during metamorphism
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rock cycle
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the continuous changing and remaking of rocks
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