ESS 101 Midterm 2 EXAMS WITH FULL
SOLUTIONS
Interest BGin BGalternative BGenergy BGand BGmineral BGsources BGmay BGinvolve BG- BG
BGcorrect BGanswer- BG- BGproducing BGunconventional BGresources
BG- BGmining BGlower BGconcentration BGdeposits
BG- BGrecovering BGresources BGfrom BGwaste BGand BGrecycling BGstreams
BG- BGsourcing BGfrom BGcountries BGwith BGdifferent BGpolitical BGand/or BGenvironmental
BGstewardship BGphilosophies
BG.Which BGof BGthe BGfollowing BGare BGnot BGgoals BGof BGthe BGUSGS
BG- BGUnderstand BGfundamental BGEarth BGprocesses BGthat BGform BGenergy BGand
BGmineral BGresources
BG- BGProvide BGinventories BGand BGassessments BGof BGenergy BGand BGmineral
BGresources
BG- BGUnderstand BGthe BGeffects BGof BGenergy BGand BGmineral BGdevelopment BGon
BGnatural BGresources BGand BGsociety
BG- BGSet BGgovernmental BGpolicy BGon BGoffshore BGdrilling BGin BGthe BGU.S.
, BG- BGUnderstand BGthe BGreliability BGand BGavailability BGof BGenergy BGand BGmineral
BGsupplies BG- BG BGcorrect BGanswer- BGSet BGgovernmental BGpolicy BGon BGoffshore
BGdrilling BGin BGthe BGU.S.
BGThe BGfollowing BGmineral BGis BGused BGto BGfilter BGdrinking BGwater:
BG- BGCadmium
BG- BGDiatomite
BG- BGKaolin
BG- BGTantalum
BG- BGZinc BG- BG BGcorrect BGanswer- BGdiatomite
BGwhat BGare BGthe BGthree BGtypes BGof BGMagma/lava BG- BG BGcorrect BGanswer-
BGmafic-basalt, BGintermediate-andesite, BGfelsic-granite
BGWhy BGdoes BGgranitic BGcomposition BGmagma BGrarely BGmake BGit BGto BGthe
BGsurface? BG- BG BGcorrect BGanswer- BGGranitic BGmagma BGis BGa BGwet BGmelt BGand
BGthe BGmelting BGtemp BGincreases BGwith BGdecreasing BGpressure BGso BGthat BGis
BGsolidifies BGas BGis BGrises BGto BGthe BGsurface, BGas BGpressure BGdecrease
BGwhat BGhappens BGto BGdry BGbasaltic BGmagma BGas BGit BGrises? BG- BG BGcorrect
BGanswer- BGit BGfurther BGmelts BGas BGit BGrises BGto BGthe BGsurface
BGwhere BGdo BGshield BGvolcanoes BGform? BG- BG BGcorrect BGanswer- BGoceanic BGhot
BGspots
BGwhere BGdo BGstrato BGvolcanoes BGform BG- BG BGcorrect BGanswer- BGsubduction
BGzones
BGpyroclastic BGvolcanoes BGare BG- BG BGcorrect BGanswer- BGcinder BGcones BGrelated
BGto BGsmall BGvents BGand BGpresence BGof BGground BGwater
BGfissure BGeruptions BGform BG- BG BGcorrect BGanswer- BGplateau BGbasalts
BGeruptions BGunder BGwater BGform BG- BG BGcorrect BGanswer- BGpillow BGbasalts
BGplutons BGform BGwhen BG- BG BGcorrect BGanswer- BGmagma BGbody BGcrystallizes
BGunderground
BGLarge BGpluton BGexamples BG- BG BGcorrect BGanswer- BGbatholith, BGstock, BGlaccolith
BGand BGlopolith
BGbatholith BG- BG BGcorrect BGanswer- BGa BGvery BGlarge BGigneous BGintrusion
BGextending BGdeep BGin BGthe BGearth's BGcrust.
BGstock BG- BG BGcorrect BGanswer- BGigneous BGintrusion BGthat BGhas BGsurface
BGexposure BGless BGthan BG100 BGkilometers. BGsmaller BGthan BGbatholiths.
SOLUTIONS
Interest BGin BGalternative BGenergy BGand BGmineral BGsources BGmay BGinvolve BG- BG
BGcorrect BGanswer- BG- BGproducing BGunconventional BGresources
BG- BGmining BGlower BGconcentration BGdeposits
BG- BGrecovering BGresources BGfrom BGwaste BGand BGrecycling BGstreams
BG- BGsourcing BGfrom BGcountries BGwith BGdifferent BGpolitical BGand/or BGenvironmental
BGstewardship BGphilosophies
BG.Which BGof BGthe BGfollowing BGare BGnot BGgoals BGof BGthe BGUSGS
BG- BGUnderstand BGfundamental BGEarth BGprocesses BGthat BGform BGenergy BGand
BGmineral BGresources
BG- BGProvide BGinventories BGand BGassessments BGof BGenergy BGand BGmineral
BGresources
BG- BGUnderstand BGthe BGeffects BGof BGenergy BGand BGmineral BGdevelopment BGon
BGnatural BGresources BGand BGsociety
BG- BGSet BGgovernmental BGpolicy BGon BGoffshore BGdrilling BGin BGthe BGU.S.
, BG- BGUnderstand BGthe BGreliability BGand BGavailability BGof BGenergy BGand BGmineral
BGsupplies BG- BG BGcorrect BGanswer- BGSet BGgovernmental BGpolicy BGon BGoffshore
BGdrilling BGin BGthe BGU.S.
BGThe BGfollowing BGmineral BGis BGused BGto BGfilter BGdrinking BGwater:
BG- BGCadmium
BG- BGDiatomite
BG- BGKaolin
BG- BGTantalum
BG- BGZinc BG- BG BGcorrect BGanswer- BGdiatomite
BGwhat BGare BGthe BGthree BGtypes BGof BGMagma/lava BG- BG BGcorrect BGanswer-
BGmafic-basalt, BGintermediate-andesite, BGfelsic-granite
BGWhy BGdoes BGgranitic BGcomposition BGmagma BGrarely BGmake BGit BGto BGthe
BGsurface? BG- BG BGcorrect BGanswer- BGGranitic BGmagma BGis BGa BGwet BGmelt BGand
BGthe BGmelting BGtemp BGincreases BGwith BGdecreasing BGpressure BGso BGthat BGis
BGsolidifies BGas BGis BGrises BGto BGthe BGsurface, BGas BGpressure BGdecrease
BGwhat BGhappens BGto BGdry BGbasaltic BGmagma BGas BGit BGrises? BG- BG BGcorrect
BGanswer- BGit BGfurther BGmelts BGas BGit BGrises BGto BGthe BGsurface
BGwhere BGdo BGshield BGvolcanoes BGform? BG- BG BGcorrect BGanswer- BGoceanic BGhot
BGspots
BGwhere BGdo BGstrato BGvolcanoes BGform BG- BG BGcorrect BGanswer- BGsubduction
BGzones
BGpyroclastic BGvolcanoes BGare BG- BG BGcorrect BGanswer- BGcinder BGcones BGrelated
BGto BGsmall BGvents BGand BGpresence BGof BGground BGwater
BGfissure BGeruptions BGform BG- BG BGcorrect BGanswer- BGplateau BGbasalts
BGeruptions BGunder BGwater BGform BG- BG BGcorrect BGanswer- BGpillow BGbasalts
BGplutons BGform BGwhen BG- BG BGcorrect BGanswer- BGmagma BGbody BGcrystallizes
BGunderground
BGLarge BGpluton BGexamples BG- BG BGcorrect BGanswer- BGbatholith, BGstock, BGlaccolith
BGand BGlopolith
BGbatholith BG- BG BGcorrect BGanswer- BGa BGvery BGlarge BGigneous BGintrusion
BGextending BGdeep BGin BGthe BGearth's BGcrust.
BGstock BG- BG BGcorrect BGanswer- BGigneous BGintrusion BGthat BGhas BGsurface
BGexposure BGless BGthan BG100 BGkilometers. BGsmaller BGthan BGbatholiths.
