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All 69 terms

TermDefinition
glacier definitionthick mass of compacted and re-crystalized snow. forms on land and shows from form of movement.
continentallargest glacier, 1000 miles wide and deep. only two on earth today covering antarctica and greenland.
alpinesmaller glacier. less than 100 mi wide/deep. over 1000 found around the world.
icecapsmedium size. about 10 around the world. found in high plateaus like tibet.
formationsglaciers can take at least 100 years to form. no ice ages now.
firncompacted snow' very icy and formed when snow doesn't melt in summer time.
glacial icecompacted/re-crystalized firn. light blue color. heavier than ice and an icebergs made of glacial ice.
glacial movementmost of the time, glaciers move slowly . few inches a day.
basil slidingglacial slips/slides on a think layer of mud at the bottom of a glacier.
surgesany quick/sudden movement of glaciers, happens with alpine glaciers. expecially during the summer (melting season).
zone of fractureupper 1/3 of a glacier where the ice is very brittle & will crack as the glacier moves.
crevassesdeep cracks found in the zone of fracture about 200-300 ft. deep. -especially dangerous to mountain climbers.
zone of flowthe lower 2/3s of a glacier, where the ice will bend as the glacier moves, like thick caramel/molasses.
zone of accumulationupper half of a glacier, usually at a higher elevation where snowfall is greater than melting.
zone of wastagelower 1/2 of a glacier where melting is greater than snowfall.
advancing glacierany glacier that's growing in size in 2009, there are few advancing glaciers.
retreating glacierany glacier that's shrinking in size. 2009: most are retreating, meaning the climate is warming up.
calvingprocess of forming icebergs. spectacular and loud process & occurs when glaciers flow into the ocean.
fjordu-shaped valley that's underwater. they're formed when a glacier retreats from a coastline. famous in norway, sweden &alaska.
striationsvery small scratches found in the bedrock produced by the erosion of a glacier.
groovessame as striations; formed by the erosion of a glacier but are much much bigger. kelley's island: lake erie ; famous for glacier grooves.
quarryingwhen a glacier breaks off and crushes large boulders as it goes over a cliff or a ledge.
roche montonneerock formation formed by quarrying action in the glacier: famous in yosemite national park.
driftterm referring to any gravel or boulders thats left behind after a glacier melts. sr. rock: glacial drift called a glacial eratic.
outwashtype of drift that's found in layers & produces a very flat landscape like what's found in w. ohio.
tillalso drift but it's unlayered; produces a hilly landscape. KHS is built on glacial till.
morainesa ridge of rill. they form long hills and are found anywhere there used to be a glacier.
alpine featureshorn : sharp mountain peak. tourn : mountain lake. pater : two or more mountain lakes. U shaped valleys. hanging valley. "waterfall" arete : long & sharp mt. peak.
continental featureskame: made of glacier till. kettle: depressents that have water (geauga/punderson). marines: hills of ridges of till. drumlin: teardropped shape hill. esker: made of sand and is like a marine.
ice ages.periods of time where all the glaciers are advancing. many ice ages in history of earth only takes a 10 degree drop in temperature to go into the ice age.
interglacial featureswarmer periods of time btwn ice ages currently are living in an interglacial period and the earth should naturally warm for the next 80,000 years.
ice corestubes of glacial ice that are drilled and removed from a glacier in order to study past climates.
milankovitch cycletheory that says every 100,000 years the earth naturally cools down and goes into an ice age caused by the wobble of the earth's axis and change of shape of earth orbit.
glacial advancesfour glaciers that have come down from canada during the past half million years. each advance is named after a state with most evidence. (nebraska, kansas, illinois, wisconsin)
glacial map: ohio.2/3 covered by glacier during each one.
structural geologistlooks at surface map. draws in rock layers underground highest paid find oil and gas.
compressant (type of stress)rock layers are pushed tgthr occurs when large crustal plates collide.
tensional (type of stress)pulled apart causes rock layers to break and move along fault lines, produces rift valleys.
shear (type of stress)multidirectional stress produces most distractive earthquakes on the earth.
foldbend in a rock later caused by compressional stress, high temperature and pressure.
anticlinea fold that bends upward
synclinea fold that bends downward
recumbent foldanticlines and synclines combined tgthr.
dipangle a rock layers tilted from horizontal, the rock beneath KHS is dipping at about seven degrees.
strikealways measured at ninety degrees to the dip & is measured in a north/south or east/west direction.
rules for mapping folds1. oldest rock layers will always be found at the center of an anticline. 2. youngest rock layers found at center of a syncline. 3. never change the thickness of an underground rock layers.
faulta break in the rock layers along which there must be movement on each side. there are no surface faults in ohio.
hanging wallalso an old gold-mining term that refers to the side of the fault that's above your head and you'd hang your lantern on that side of the fault.
footwallalso an old gold-mining term and it's the side of the fault your feet would be on if you tunneled/dug into the fault.
fault planesmiddle of the fault and it's the imaginary line that divides hanging wall and foot wall.
normal faultwhen the hanging wall side moves down compared to the footwall side. always caused by tensional stress.
reverse faultwhen the hanging wall side moves up compared to the footwall caused by compressional stress.
transcurrent faulta horizontal movement fault so there's no hanging wall or footwall. san andreas fault in california is a famous one.
rift valleyspecial type of valley that's produced by tensional stress & to normal faults.
isostasybalance of the earth's crust which means if one area, the cause is sinking, another area, the crust is rising. isostatic rebound - man cause for earthquakes in ohio.
formation of oiloil is a gross smelly very thick liquid, almost pitch black in color. formed by the decay of microscopic marine life. millions of years of heat and pressure to produce a chemical.
anticline or dome oil traprichest and most productive of traps. produce millions of gallons of raw oil.
faultssecond most productive of traps. when we find oil nxt to normal/reverse faults.
stratagraphicmost common oil map in NE Ohio also produces the least amount of oil.
density scanwhen a structural geologist calculates the density of the surface rocks looking for a value of above 26g/cm. ohio passes this test.
core samplingwhen they look for certain fossils at the surface and underground that are usually found with oil deposits. example: pelecypod. ohio passes this test.
seismic blastingwhen structural geologists set off a series of dynamite charges and record bound back time of the sound waves made by the explosions. ohio fails this test.
oil wells.1. the first well was drilled in PA and oil was struck @ 100 ft down. 2. 2009: average cost for drilling an oil well: $7 mil. av. depth; 7000 ft. 3. a gusher is when oil pours out of an oil well under high pressure. it's a bad thing because you lose and pollute the landscape.
fractional distillationprocess of boiling the raw oil that comes out of the ground in order to make something useful w/it. like gasoline, kerosene, diesel fuel, motor oil, asphault & cosmetics. -takes place @ an oil refinery which employs 1000s of people but is done away from civilization.
coalblack sedimentary rock full of a chemical compound called hydrocarbons and since the US is the saudi arabia of coal, we burn it by the tons everyday to produce electricity.
four grades of coalanthrocite: burns clean - very hot. bituminous and sub-bituminous : US burn these two. lignite : worst grade - smokes - burns cooler.
underground miningwhen we dig mine-shafts or tunnels in order to reach the coal considered very dangerous because of cave-ins, explosions & the black lung disease.
strip miningpreferred way to mining coal and it's when we dig a huge pit to reach the coal. it's big drawback is that is leaves a large erosional scar on the earth.
scrubbersa method used to remove sulfur from coal so it burns clearer and you don't produce acid rain. the method is expensive and you pay for it in your electric bill.
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Terms 69
Creator nelia_bucholz
Created March 23, 2009
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