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the theory that the solar system formed from the condensing and accumulation of mass in a nebula (a cloud of gas and dust) |
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the sun in its initial stages |
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small, solid object in space representing first stage in accretion within the solar nebula |
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formation of inner planets |
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gravitational pull/push directed embryos into different orbits which caused them to collided together to form inner planets |
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planetary embryo turns to vaporized debris which is then pulled together to make the moon |
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Earth was partly or mostly molten |
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hypothesis on formation of atmosphere and hydrosphere |
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comets and meteors delivered water to the planet; water-bearing planetary embryos collided with the Earth |
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seismic waves on Earth's surface that decreases in intensity with depth |
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extracted from the mantle by partial melting and crystallization; divergent boundaries |
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formation of continental crust |
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subduction zones and mantle plumes |
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seimic body wave that displaces material in the same direction that the wave is moving which causes alternating squeezing and stretching of the material as the wave passes; travel through any material |
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seismic body waves that displace material at right angles to the direction of wave motion; only travels through solids |
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waves bounce off a boundary |
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bending of a wave caused by a change in wave velocity |
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what are the layers of the Earth? |
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crust, mantle, liquid outer core, iron innor core |
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4 most common components of the Earth |
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iron, oxygen, silicon, & magnesium |
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basic properties of the Earth |
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shape, size, mass, density |
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What is plate tectonic theory? |
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the theory that the Earth's lithosphere is not seamlessly continuous but is broken into discrete pieces that move slowly |
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the part of the Earth's interior that is moving |
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plates colliding compressing the lithosphere and causing subduction one one plate beneath the other |
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plates move apart from each other and new lithosphere forms |
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plates slide against one another which neither creation nor destruction of lithosphere |
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an area of intense volcanic activity not explained by plate tectonics; from where asthenospehere rises beneath lithospheric plates |
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name of super continent when all the continents were connected |
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continental drift hypothesis |
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Alfred Wegener's hypothesis that all the continents were once joined together from which they drifted to their current position |
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Mineral composition (small to large) |
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Definition
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ionic bonds: attraction between positive and negative ions covalent bonds:strongest*;atoms share electrons metallic bonds:electrons roam among several atoms van der Waals: weakest*; |
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physical properties of minerals |
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streak, cleavage vs fracture, hardness, magnetic, reactive |
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contain silicon and oxygen bonded in SiO4; primary rock forming mineral in the crust Example: Quartz |
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melted silicate minerals or liquid rock in the Earth's interior |
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plutonic vs volcanic rocks |
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volcanic rocks: solidify at surface (extrusive) plutonic: solidify beneath surface (intrusive) |
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cinder cone: shield: composite: dome complex: |
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Volcanic Earthquakes Directed Blast Tephra Volcanic Gases Lava Flows Debris Avalanches, Landslides, and Tsunamis Pyroclastic Surge Pyroclastic Flows Lahars |
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suggests that the type of igneous rocks that form from magma solidification depends on the temperature of crystallization and the chemical composition of the originating magma |
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aphanic, porphyric, phaneric, pegmate |
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due to stress from squeezing, stretching, compression, and elongation |
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folds, horst and graben, faults |
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folds: horst: block of crust displaced upward along graben: block of crust displaced downwards faults: a fracture plane along which rock or regolith is displaced |
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primary hazards of Earthquakes |
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secondary hazards of Earthquakes |
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Building Collapse Fires Landslides Liquifaction Seiches Tsunami |
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How is Earthquake magnitude measured? |
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relationship between magnitude and amount of energy released |
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processes associated with the rock cycle |
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melting, crystallization, weathering, transportation, deposition, precipitation, lithification, metamorphism |
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disaggregation of rocks by mechanical means |
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dissolution of some minerals and formation of new minerals and dissolved ions as a result of water and oxygen reacting with the mineral |
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Differences in weather based on rock type (granite vs. gabbro) |
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the process of transforming loose sediment into sedimentary rock by compaction and cementation |
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decrease in volume caused by partial or complete elimination of pore space between sediment usually caused by the weight of overlying sediment |
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the filling of pore spaces with precipitated minerals to produce an interlocking framework with clastic sediment grains; step in lithifaction |
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Clastic sedimentary rocks |
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texture describing particles formed by weathering of preexisting rocks |
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Chemical sedimentary rocks |
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dissolved ions that move away in solution |
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bedding (stratification) mud cracks cross-beds grated beds |
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igneous, sedimentary, metaphoric |
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organic remains preserved in rocks; show ancient pasts |
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change rocks; show the past |
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the process of planetary formation and growth by the gradual accumulation of small objects to make larger ones |
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formation of outer planets |
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solar winds blew light weight gas molecules out of the nebula except where gravity was strong (the outer planets) |
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