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Terms for ESS Final

AB
stressforce applied to a given area
compressional stressshortens and thickens crust
tensional stressthins and stretches crust
strainactual change in shape or size of a rock body due to stress
ductile deformationrock deep in the ground flows/folds in response to stress
brittle deformationrock body near the surface fractures/faults in response to stress
anticlineformed by upfolding (arching) of rock layers
synclineformed by downfolds, or rock troughs
normal faulthanging wall moves down relative to the footwall in response to tensional stress
reverse faulthanging wall moves up relative to the footwall in response to compressional stress
thrust faulta reverse fault with a dip angle of less than 45 degrees
isostasyvertical movement of earth's plates based on gravitational balance of land mass vs. asthenosphere depression
jointvertical fracture in a rock body with no offset
weatheringthe disintegration and decomposition of rock at or near Earth's surface
erosionthe transport of weathered rocks by a mobile agent
frost wedgingphysical weathering caused by the expansion of water as it freezes within a rock body
talus slopeslarge piles of rock rubble at the base of rock outcrops
sheetinglarge slabs of igneous rock break loose in layers
mass wastingdownslope movements of soil and unconsolidated materials (rock fragments) without the use of a transport medium
competencemaximum size of particles a stream is capable of carrying based on its velocity (energy)
capacitymaximum load (amount of sediment) a stream can carry
meanderswide, sweeping bends in an older stream
calvingwhen large pieces of ice break off the front of a glacier; form icebergs at sea
pluckingwhen a glacier loosens and lifts blocks of rock as it moves over a fractured surface
driftdeposits of sediment left by a retreating glacier
saltationrolling and skipping of larger grains of sand along the surface of the desert by the force of winds
desert pavementstony surace of coarse pebbles and cobbles formed as the final result of longterm deflation
loessa blanket of fine, windblown silt over a broad area
physical oceanographystudy of the physical properties of the ocean, such as temperature, depth, and waves and currents
geological oceanographystudy of the shape, composition, and evolution of the seafloor and its sediments
oceanan immense body of saltwater with a well-defined basin
bathymetrystudy of the depth and topography of the ocean floor
abyssal plaindeep, extremely flat features formed by thick accumulations of fine sediment from turbidity currents
diurnalone high and low tide per day
semidiurnaltwo equal sets of high and low tides per day
geostrophic flowwarm currents directed away from the equator, and cool ones toward it
Coriolis Effectthe apparent deflective force of Earth's rotation on all free-moving objects; deflection to right in northern hemisphere and to left in southern
Ekman Spiralvertical spiraling effect on ocean water due to the combination of the coriolis effect and the drag of deflected surface water on the underlying water
upwellingthe vertical movement of cold, nutrient-rich, deep water to the surface to replace warmer surface water that has been moved away, such as by continental deflection
El Ninoname given to periodic warming of the central and eastern Pacific Ocean
La Ninaname given to the periodic cooling of the eastern Pacific Ocean
thermoclinelayer of water in which there is a rapid change in temperature with depth
planktonincludes all organisms that drift in the ocean
nektonincludes all animals capable of moving independent of the ocean currents
benthosorganisms living on or in the bottom of the ocean
pelagic zoneopen zone of the ocean at any depth
benthic zonemarine-life zone that includes any sea-bottom surface regardless of its distance from shore
terrigeneous sedimentformed from eroded continental rocks that are transported to the ocean by rivers and runoff
biogeneious sedimentformed from shells and skeletons of marine animals and algae
chemosynthesisprocess whereby microorganisms create energy without the use of light
bycatchunintentional harvest
ocean acidificationaddition of inorganic carbon sources into the ocean, driving the production of carbonic acid and lowering the pH
eutrophicationprocess where oxygen is lost from the water column as a direct result of the decay of algal blooms formed by the addition of nitrate sources
photophoreslight producing adaptations found in deep sea fish
barbellong, skinny extension from the chin of a deep sea fish, usually tipped with a photophore, and used like a fishing lure
weatherstate of the atmosphere at a particular time and a particular place
climatelong-term state of the atmosphere at a particular location
solar insolationmeasure of the portion of the sun's energy that reaches Earth's surface
albedosolar energy reflected by the Earth's surface
tropospherelayer of the atmosphere closest to the Earth's surface where almost all weather occurs
stratospherelayer above troposphere that contains the ozone layer and jet streams
temperature inversionindicates that the temperature is increasing with height in the atmosphere
isobarcountour line drawn connecting areas of equal pressure
anemometermeasures wind speed
relative humidityactual ratio of how much water vapor is present vs. how much the air is capable of holding for that temperature and pressure
sling psychrometertype of hygrometer using 2 thermometers, one with a wet bulb and one dry, and a table
dew pointthe temperature at which a parcel of air has to be cooled to reach saturation
station modelsymbolic illustration showing weather occurring at a given reporting station
air massa large body of air with uniform temperature and moisture
frontplace where 2 air masses interact
cold frontfast moving front associated with violent weather activity that occurs directly at the front
warm frontassociated with steady precipitation that generally happens ahead of the front
cold front map symbolblue line with triangles pointing in the direction of movement
warm front map symbolred line with half circles pointing in the direction of movement
jet streamstrong pressure gradient create high winds at high altitudes where polar air masses meet tropical air masses
monsoonseasonal reversal of wind direction associated with large continents
high pressure systempressure increases as you move toward the center of the system and winds move clockwise; also called an anticyclone
low pressure systempressure increases as you move away from the center of the system and winds move counterclockwise; also called a cyclone
condensation nucleivery fine particles in the atmosphere that provide a surface for water to condense and form a cloud
renewable energy sourcegenerally one that can be replenished by nature within a 100 year period
cryospherethe frozen part of the Earth's surface


IPC, Earth/Space Science & AP Environmental Science Instructor
Friendswood High School
Friendswood, TX

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