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earth science mt

earth science mid term

TermDefinition
earth science the study of all the sciences tha help us to understand the planet on which we live.
environment the world in which we live.
physical geology the study of the materials and processes tha form the earth
historical geology study of the possible origins of the earth and changes that have occured since its beginning
oceanography a blend of all the natural sciences as they relate to seawater, seashores, the seafloor,
meteorology the stufy of weather, climates, and the atmosphere
astronomy the study of universe surrounding earth
system set of interacting components
scientific theory well tested, widely accepted, and based on observable facts
the scientific method observation, hypothesis, experimentation, conclusion
composition of earth's "outside" hydrosphere, atmosphere, biosphere, geosphere
composition of earth's "inside" crust, mantle, outer core, inner core
mineral naturally occuring inorganic solid that possesses an orderly crystalline structure and a difinite composition normally made of two or more elements chemically combined as a compound
halite table salt
physical properties of minerals external crystal form, luster, streak, hardness, fracture, cleavage, and specific gravity
silicates most common mineral, always contains oxygen and silicon
rocks peices of the earth's crust which usually contain more than one mineral
types of rocks sedimentary, igneous, metamorphic
rock cycle continual movement of material from one rock type to another
igneous rock formed from magma
sedimentary rocks form from the compaction and cementation of small particles under the pressue of th ematerial above them
metamorphic rock rocks produced form existing sedimentary igneous, and metamorphic rocs.
mechanical weathering very slow process in which rocks are broken into smaller and smaller pieces consisting of the same material as the rock itself
frost wedging (mechanical weathering) repeated cycl of freezing and thawing water in rock cracks
expansion due to unloading (mechanical weathering) result of the top layer of rock eroding away and reduces the pressure on the lower layers causing sheeting, or separation of layers of rock
biological activity (mechanical weathering) plant roots pushing in to rock, splitting the rock, animals burrowing, human blasting
chemical weathering when the minerals in the rock react with other substanses in a chemical reaction thus chaning the make up and stucture of the mineral, 2 important substances, water and oxygen
soil mixture of both mineral and organic material
topography the "lay" or the land
erosion the transport of soil materials due to water, wind or ice
sheet erosion thin layers of water flowing across a surface
sediment soil in water
steam any flowing body of water
laminar slow smooth flow
turbulent flow rough, more common
gradient slope
dissolved load sediment disolved in water, usually not seen
suspended load, "mud" in muddy water
bottom, or bed load sediment that pushes along the bottom
amount of load a stream can carry depends on capacity and competence
ground water all fresh water not frozen in glaciers, and ice sheets(majority in cracks in rock
porosity a measure of how much of a given formation is open space(mostly microscopic)
saturated full (of water)
water table the top of the saturated level
permiability a measure of how easily water can move through rock or soil
aquifer rock layers that are permeable to water, where wells are dug
spring(water) place where the water table level is higher than the ground around it, usually occur on a hillside
artisian wells complex geological system in which the water is actually pushed above the water table twards the surface
potable not drinkable or pure
moraines layers of till which form ridges across the landscape
till large particles left behind by glaciers
kettles depressions left by non moving glaciers that have been buried by the till and then have melted
ephemeral stream stream that carries water only after rainfall
diverging boundaries when plates are moving away from each other
converging boundaries when plates are moving towards each other
subduction when two plates move towards each other and one sinks below the other
transform fault boundaries when two plates are parallel to each other but moving in opposite directions, causing friction between them
fault cracks between two plates
seismograph measures size and direction of earthquake waves
p wave shake earth side to side
s wave shake earth up and down
mercalli scale measures earthquakes based on observable behavior and destruction
richter scale measures amplitude, height of wave
liquification breaking up of soil in to fluid
lithosphere cool shell including crust and upper mantle
moho boundaries between lithosphere and the rest of the inner core
AA flows lava flows with surfaces rough jagged blocks and sharp edges
pahoehoe flows smooth surfaces,like twisted braids of rope, or liquid pored out
pyroclastic material consist of broken rock, ash, dust, and lava bombs, depending upon the eruption
lava bombs blobs of lava ejected in to the atmosphere while still molten, think raindrop
shield volcano gentle slopes formed by flows of low viscosity lava
caldera center of a volcanos eruption
cinder cones form of small pryoclasts building around the vent
composite cone characterized by steep sides, and steep walled crater
nuee arentes glowing avalanches of hot rock, hot gasses, hot ash, and hot dust
lahars mud flows formed from ash, dust, and melted snow and ice
volcanic neck the remains of the original vent tube
batholiths large pieces of rock from lava pooling and cooling below the earths surface
laccoliths molten rock forcibly injected between sedimentary strata, so as to arch the beds above, while leaving the ones below reflectively flat
sills horizontal tubular intrusive bodies that store magma
dikes discordant bodies that cut across bedding surfaces, transport magma
plutons intrusive phenominon
asthenosphere top of the mantle
deformation folding, flowing, fracturing of rocks
ductile deformation folding and flowing, no breaks
synclines represents folds where layers of rock have sagged
anticlnes folds where the layers have been pushed up
normal fault moving away from each other
reveres fault moving towards each other
thrust fault moving towards each other with subduction
slip strike fault parallel moving in opposite directions
joints cracks in rock where no movement has taken place
orogenisis mountain building
Created by: codyknow
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