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PLANET EARTH - American Museum of Natural History

PLANET EARTH - American Museum of Natural History

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GLOSSARYatmosphere: the mixture <strong>of</strong> gases (78% nitrogen, 21%oxygen, 0.9% argon, and 0.03% carbon dioxide, byvolume) that surrounds the Earthcarbon cycle: the continuous flow <strong>of</strong> carbon throughliving things (biosphere), the solid Earth (geosphere),the oceans (hydrosphere), and the atmosphereclimate: the weather (including extremes) in a particularregion averaged over a number <strong>of</strong> yearsconvection: the process by which hotter, less densematerial rises and is replaced by colder and densermaterialcontinent: one <strong>of</strong> Earth’s large land massescore: the mass <strong>of</strong> metallic iron and nickel at the center<strong>of</strong> the Earth. The fluid outer core begins at 5100 kmbelow the surface and the solid inner core at 2900 km.crust: Earth’s outermost solid layer, consisting <strong>of</strong> acontinental crust averaging 45 km thick and an oceaniccrust averaging 8 km thickearthquake: a shaking <strong>of</strong> the ground caused by theabrupt release <strong>of</strong> accumulated strain when a faultruptureserosion: the processes that wear down rocks andtransport the loosened sedimentfossil fuels: coal, oil, and natural gas, which formedfrom the remains <strong>of</strong> organisms that lived millions <strong>of</strong>years agogeologist: a scientist who studies Earth, e.g. its history,composition, structure, and the processes that shape itglacier: a large, semi-permanent, slowly flowing river <strong>of</strong>ice formed from compacted snowigneous rock: rock formed when magma (molten rock)solidifiesmantle: the layer between the core and the crust <strong>of</strong>the planet Its properties, such as density and viscosity(resistance to flow), change with depth.metamoprhic rock: rock formed when sedimentary,igneous, or other metamorphic rocks recrystallize intonew rock forms, typically under the influence <strong>of</strong> heatand pressuremineral: any naturally occurring, inorganic solid witha specific composition and an orderly crystallinestructureoutcrop: bedrock exposed at Earth’s surfaceozone layer: the region <strong>of</strong> the upper atmosphere thatcontains about ninety percent <strong>of</strong> Earth’s ozone (moleculesmade up <strong>of</strong> 3 atoms <strong>of</strong> oxygen)plates: the blocks that make up Earth’s rigid, cold,outermost shell, averaging 100 km thick and consisting<strong>of</strong> crust and uppermost mantleradiometric dating: a technique for measuring theage <strong>of</strong> geologic materials based on the decay <strong>of</strong>naturally-occurring radioactive isotopesrock: a naturally occurring aggregate <strong>of</strong> one ormore mineralsrock cycle: the cycle in which sedimentary, igneous,and metamorphic rocks are transformed into other rocktypes through processes such as melting, crystallization,erosion, deposition, lithification (the processby which sediments are turned into rock), andrecrystallizationsedimentary rock: rock formed when sedimentsaccumulate and lithify, or when minerals precipitatedirectly from watervolcano: a vent in Earth’s surface through whichmagma and associated gases and ash erupt. The ejectedmaterials <strong>of</strong>ten form a conical structure.weather: the state <strong>of</strong> the atmosphere at a specific placeand time, characterized by temperature, barometricpressure, wind velocity, humidity, cloud state andprecipitationweathering: the physical and chemical processes thatdiscolor, s<strong>of</strong>ten, and break down rocks exposed to air,water, and organic materialwater vapor: the gaseous state <strong>of</strong> waterwater cycle: the cycling <strong>of</strong> water among oceans andlakes, land, living organisms, and the atmosphere© 2012 <strong>American</strong> <strong>Museum</strong> <strong>of</strong> <strong>Natural</strong> <strong>History</strong>. All rights reserved.

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