Continental/oceanic crust / earthquakes

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Continental/oceanic crust

Last updated 12:23 PM on 5/20/26
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8 Terms

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Oceanic crust

  • found beneath oceans

thinner than continental / more dense

10 km deep

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continental crust

found under land - forming continent

thicker than oceanic

  • 25-30 km thick

  • CC not as dense as oceanic crust

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tectonic plate

  • l = crust + top part of mantle

  • lithosphere = made up of huge pieces called tectonic platees

  • fit together like a jigsaw

  • most of earth is covered by 7 major plates

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impacts of earthquakes

Wide spread infrustruture damage - loss of service and access

  • roads + bridges + airports +

  • water + gas + electricity= damaged / inaccessable

Human impact

  • injury / death of ppl

  • After disaster - chlorea ongoing outbreaks years later

Impacted economic + development

loss of job + workplace / number in workforce

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Earthquakes

Where tectonic plates meet

  • over time pressure builds up pressure release

  • when pressure releaseenergy release(shockwaves)

  • most earthquakes = human causes - high pressures inc. large dam, underground nuclear explosion

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Haiti earthquake 2010 impacts

Caused by enriquillo plantain

tansform boundary b/t caribbean + north american plates to cause destructive earthquakes

  • many buildings collapsed = many killed pr trapped from lack of building codes

Loss of critical infrustructrue

  • loss of electricity + communication lines + roads clocked = reduce ability to offer aid to all areas

1 mill left homeless

hospitals = unusable - days waiting for treatment

increasing crimes - looting + escaped prisoners

Hospitals unusable

infected signifcant amoutn of ppl / water contaminated

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short term impacts earthquake

many buildings collpased = lack of building codes - many trapped or killed

  • loss acess to services like hospitals

  • electricity + communication lines

  • water gas electricity = damaged + inaccessable

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design earthquake proof buildings

Flexibal foundation = pads + reinforced concrete/ sand cushions = stable

  • pendulum swings opposite earth movement - earthquake movement = dissipate energy

  • shock absorbers - absorb seismic energy

  • base isolation = seperate base of building from ground using spring - building feel less shaking

  • cross bracing = transfer earthquake force to foundation

  • prevent building collapsing