quiz I: disasters

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34 Terms

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chelyabinsk meteor

  • small meteor traveling about 20x the speed of a bullet

  • exploded in the stratosphere about 23km (15 mi) above the surface

  • people there could feel the intense heat from the fireball as well as the shockwave from the explosion

  • largest known meteor to enter the earth’s atmosphere since the tunguska event

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tunguska event

  • june 30, 1908 fireball exploded over tunguska river valley

  • the blasting force equivalent of 10 megatons of TNT, 10 H-bombs

  • 2,000 km of forest to be flattened and burned

  • at least 1M heard the explosion

  • estimated asteroid 20 to 50m in diameter

  • missed a similar git in 2004 and could happen again

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formation

  1. 13.7 billion years ago: big bang

  2. 13 billion years: formation of first stars (quasars)

  • after 100,000 years quasars died

  • death of quasars gave us the elements and scatters new elements into space

  • H and He collected into what are called a solar nebula

  1. 5 billion years ago: sun grew by buildup of matter from solar nebula

    • after formation of sun, other particles pushed away by solar wind and solar radiation

    • solar radiation and solar winds push unused material away from the newborn sun

    • as particles are pushed away, they’re differentiated by density

    • more dense material (rock and metals) closer to sun

    • lighter material (ice and gases) further from sun

    • particles become trapped in chaotic, unorganized rings around the sun they begin to grow, like dust bunnies into planets

    • rocky material in orbit around the massive sun, collected creating rocky planets (mercury, venus, earth, and mars)

    • gaseous material pushed away from the sun formed the gaseous planets (jupiter, saturn, uranus, and neptune)

  2. 4.56 billion years ago: formation of the earth

  • after formation of the planets, plenty of unused material left flying around

  • periodic drama caused by the impact of material from outer space: asteroids, meteoroids, and comets

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asteroids

  • ranging in size from 10 (30ft) to 1000km (620 mi)

  • most of these reside in asteroid belt between mars and jupiter

  • composed:

    • rocky

    • metallic

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meteroids

  • ranging in size from dust size to 30ft

  • meteoroids are broken up asteroids

  • still in space

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meteor

makes contact with our atmosphere

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meteorite

  • makes contact with surface

  • chunks that fall to earth tell us about the composition of the parent bodies they came from

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comets

  • come in a variety of sizes

  • composed of ice and gaseous material

  • classic glowing tail or two

  • originate in the Kuiper belt and Oort cloud

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airbursts and impacts

  • heat up due to friction as they fall through producing bright light and changing

  • they will either explode into airburst or collude with earth as a meteorite (in Antarctica)

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impact craters

  • barringer crater in arizona

  • bowl shaped depression w upraised rim

  • rim is overlain by ejecta blanket, material blown out of the crater upon impact

  • broken rocks cemented together into breccia

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simple craters

  • typically small less than 4 mi

  • barringer crater

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complex craters

  • larger in diameter greater than 4 mi

  • rim collapses more completely

  • center uplifts following impact

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why earth has so few impact craters

  1. 70% of earth is covered in water

  2. smaller meteors burn up in the atmosphere

  3. eroded by natural processes

  4. plate tectonics recycles crust

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mass extinctions

  • usually involves rapid climate change, triggered by:

    • plate tectonics

    • volcanic activity

    • impacts

  • 5 major mass extinctions:

    • ordovician

    • late devonian

    • permian

    • triassic jurassic

    • cretaceous paleogene (K-Pg)

    • pleistocene

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K-Pg

  • dinosaurs disappeared along with many plants and animals

  • luis alvarez and his son walter discovered that the clay contains an unusually high concentration of iridium

  • yucatan peninsula

  • 112 mi nearly circular as deep as 18 to 25 mi

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inner core

  • radius: 1220 km about the size of the moon

  • material: solid, metallic

  • made of: 90% iron with sulfur, oxygen, and nickel

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outer core

  • thickness: 2180 km

  • material: liquid 10x denser than water

  • made of: same composition as inner core

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mantle

  • thickness: 2900 km

  • material: solid rocky

  • made of: iron and magnesium silicates

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oceanic crust

  • more dense

  • thinner

  • younger

  • basaltic

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continental crust

  • less dense

  • thicker

  • older

  • granitic

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kola borehole

  • 40,200 ft to 12.2 km

  • 19 years to drill

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how we know about earth’s interior

  • seismology

  • seismic waves propagate through the earth

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plate tectonics

  • processes associated with the creation, destruction of “plates”

  • earth’s crust is broken up into several dozen tectonic plates move around spread apart and collide

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geologic processes

  • govern the type, location, and intensity of natural processes and natural disasters

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origin of plate tectonics

  • alfred wegener (1880-1930) noticed similar shapes of continents and hypothesized they were once one giant landmass called urkontinent

  • coined the continental drift in 1912

  • sonar was invented lead to the discovery of mid-atlantic ocean ridge

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paleomagnetism

refers to the magnetism of rocks and the intensity of the direction of magnetic field of earth in the geologic past

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bathymetry

measure of ocean death

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topography

mapping ocean floor

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divergent

  • spreading

  • constructive

  • ridge/rift

  • volcanic activity and earthquakes

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convergent

  • subduction

  • destructive

  • trench

  • volcanic activity

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transform

  • lateral sliding

  • conservative

  • no major effect

  • no volcanic activity but earthquakes

  • san andreas fault

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oceanic oceanic

  • older, denser oceanic crust subducts younger, less dense oceanic crust

  • volcanic island arc, mountains, trenches

  • tsunami, volcanic eruptions, and earthquakes

  • ALeutian Island (Alaska)

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continental oceanic

  • dense oceanic crust subducts less dense continental crust

  • volcanic island arc, mountains, trenches

  • tsunami, volcanic eruptions, and earthquakes

  • cascade mountain range

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continental continental

  • when continental crust collides with continental crust

  • orogenies

  • earthquakes

  • Himalayas