Earth Space Science Review – Flashcards

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theory that the plates that move due to convection currents
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Theory of Plate Tectonics
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credited with the theory of continental drift
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Alfred Wegener
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credited with the theory of plate tectonics
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Harry Hess
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when two oceanic plates pull apart, magma rises and new crust is formed
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sea floor spreading
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circular movement of a substance due to changes in temperature and density
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convection currents
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large pieces of earths crust that move due to convection currents
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plates
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earths crust located under the ocean
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oceanic crust
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earths crust made of land
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continental crust
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large supercontinent that existed 250 million years ago
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pangea
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when two plates pull apart
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divergent boundary
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when two plates come together
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convergent boundary
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when two plates grind past each other
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transform boundary
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formed when two plates pull apart and land falls downard
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rift valley
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a chain of volcanic islands formed at an ocean-ocean convergent boundary
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island arc
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formed at an ocean-continental convergent boundary
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volcanic arc
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the more dense plate us pulled into the mantle under the less dense plate
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subduction zone
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divergent boundary in the middle of the Atlantic Ocean
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mid atlantic ridge
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depression formed at a subduction zone
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trench
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another name for the crust
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lithosphere
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another name for them mantle
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aesthenosphere
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outer layer of the Earth
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crust
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thickest layer of the Earth, part liquid part solid where convection currents are found
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mantle
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very dense solid spinning layer of the Earth
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inner core
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very dense liquid spinning layer of the Earth
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outer core
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created from the opposite spinning of the inner and outer core
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magnetic field source
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form at continental-continental convergent boundaries
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mountain range
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oxygen and silicon
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crust elements
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iron and magnesium
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mantle elements
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iron and nickel
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inner core elements
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iron and nickel
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outer core elements
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increases with depth
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earths temperature
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increases with depth
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earths pressure
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quartz and feldspar
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crust minerals
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a break in the earths crust that moves rocks
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fault
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rock formed from tiny pieces of other rocks or shells that have been compacted together
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sedimentary rock
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determines absolute age
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radioactive dating
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a fossil that occured for a short time in history
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index fossil
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ROY G BIV
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colors of visible light
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RMIVUXG
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types of electromagnetic radiation
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longest waves
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radio waves
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speed up atoms, detect weather
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micro waves
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heat waves
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infrared waves
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cause skin cancer and eye damage
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ultraviolet waves
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the distance between the crests of sucessive waves
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wavelength
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the number of waves that pass a point in an amount of time
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frequency
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see through skin
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x waves
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gamma waves
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shortest waves
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reflecting telescopes
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most common large telescopes
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depends on size and temperature
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brightness of stars
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OBAFGKM
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spectral class letters
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how bright objects seem from here on Earth
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apparent brightness
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how bright objects would be if they were all the same distance from Earth
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absolute brightness
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when objects appear to move because they are viewed from different locations
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parallax
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used to calculate the distance to stars
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using parallax
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classifies stars by temperature and absolute brightness
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HR Diagram
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stars that are in the main part of their lifecyle
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main sequence stars
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when big stars expand as they die
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supergiant
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when small stars expand as they die
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red giant
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when big stars explode as they die
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supernova
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when small stars explode as they die
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planetary nebula
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cloud of gas and dust where stars are born
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nebula
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when small stars collapse as they die
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white dwarf
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when big stars collapse as they die
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black hole
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gravity
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force that holds stars together
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plasma
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state of matter of stars
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nuclear fusion
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source of stars energy
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hydrogen and helium
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composition of the sun
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fusing of light atoms into heavy new atoms, releases energy
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nuclear fusion
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4.6 billion years
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age of sun
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small stars burn slower and longer
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life of stars
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color that is reflected
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color you see
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all 7 colors combined
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white light
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white
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all colors reflected
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black
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all colors absorbed
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14.7 billion years
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age of universe
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theory of how the universe formed
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big bang theory
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the farther away a galaxy is, the faster it is moving away from us
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Hubble's Law
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the radiation leftover from the big bang
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cosmic background radiation
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baby star
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protostar
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cosmic background radiation and Hubble's law
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evidence of big bang
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shift of light to a longer wavelength as it moves away
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redshift
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waves have lower frequency as an object moves closer
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blueshift
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expanding outward
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direction of universe
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hydrogen and helium
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first elements formed
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huge stars
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size of first stars
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supernova
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where heavy elements are created
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during the big bang
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when light elements were created
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carbon, oxygen, nitrogen
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elements necessary for life
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red star
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coldest color star
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blue star
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hottest color star
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main sequence
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stage of life the sun is in
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change in frequency as an object moves
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doppler effect
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measure movement of stars
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use of doppler effect
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expand, explode, collapse
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stages of all stars dying
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supergiant, supernova, black hole
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stages of large star dying
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giant, planetary nebula, white dwarf
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stages of small star dying
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depends on its mass
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length of a stars life
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hydrogen
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element that most stars are made of
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magnitude
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another term for brightness
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uses mirrors
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reflecting telescope
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uses convex lenses
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refracting telescope
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small/medium star
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size of our sun
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G2
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spectral class of our sun
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time it takes for half of the atoms to break down into a new element
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half life
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igneous rock pushes into a body of existing rock
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intrusion
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igneous rock covers a body of existing rock
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extrusion
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in a body of sedimentary rocks, the oldest rocks are on the bottom
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law of superposition
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in a body of sedimentary rocks, the rocks formed lying horizontally
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law or original horizontality
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age of two or more things compared to each other
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relative age
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exact age of something
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absolute age
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when older rocks are in direct contact with much younger rocks
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unconformity
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intrusion or weathering
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causes of unconformity
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younger than the rock around it
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age of fault
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younger than the rock around it
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age of intrusion
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living thing preserved in sediment
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fossil
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sedimentary rock
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rock where fossils are found
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relative age
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age of sedimentary rocks
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absolute age
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age of igneous and metamorphic rocks
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break down of radioactive elements into stable elements
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radioactive decay
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5730 years
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half life of Carbon 14
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rock made of cooled lava
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igneous rock
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an existing rock that was exposed to heat or pressure
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metamorphic rock
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sediment being deposited after being moved
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deposition
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rocks breaking down by wind and water
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weathering and erosion
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crust
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thinnest layer of earth
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mantle
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thickest layer of earth
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ocean crust
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more dense crust
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where magma continually pushes through the crust
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hot spot
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cities where earthquakes and volcanoes are likely to happen
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high risk cities
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cities where earthquakes and volcanoes are not likely to happen
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low risk cities
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rocks, fossils, climate, puzzle fit, glaciers, sea floor spreading
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evidence for plate tectonics
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5 cm/year
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rate of plate movement
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rocks, climate, fossils
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Wegener' evidence
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how the continents moved
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Wegener's flaws
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spectral class
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another term for temperature of stars
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gamma wave
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highest energy wave
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radio wave
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lowest energy wave
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hotter stars are brighter
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relationship between magnitude and spectral class
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# of waves/time
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frequency units
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gamma and xray
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waves used in medicine
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all waves
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waves produced by stars
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radio waves
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waves used in TVs
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related to star temperature
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star color
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protects Earth from solar winds
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Earths magnetic field
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particles of rock are cemented together
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cementation
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igneous rocks
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rocks found at the Mid Ocean Ridge
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age increases with distance
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age of rocks at the Mid Ocean Ridge
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objects that are closer
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objects with graeter parallax
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hydrogen fused into helium
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fusion reaction in stars
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yellow
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color of Sun
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weather, erosion, deposition, cementation
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how sedimentary rocks form
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heat and pressure
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how metamorphic rocks form
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cooling of magma
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how igneous rocks form
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increase of average atmospheric temperature
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global warming
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3.5 billion years old
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age of oldest fossils
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4 billion years old
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age of oldest rocks
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400 million years ago
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first land animals appear
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200 million years ago
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Pangea breaks apart
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1.5 million years ago
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major glaciers cover North America
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65 million years ago
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dinosaurs go extinct
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atmosphere
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Earths most vulnerable sphere
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13,000 years ago
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end of last ice age in New England
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compaction of living organisms
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how fossil fuels form
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500 million years
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time it takes for fossil fuels to form
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oil, coal, natural gas
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3 fossil fuels
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solar, hydro, wind
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3 renewable energy sources
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intense heat from Earths interior
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geothermal energy
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an unlimited resource
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renewable resource
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petroleum
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another name for oil
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a resource with a limited quanity
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nonrenewable resource
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increasing CO2 levels
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recent atmospheric CO2 pattern
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atmospheric temperature
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levels of CO2 directly effect
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300 ppm
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highest atmospheric CO2 in past 400,000 years
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380 ppm
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current atmospheric CO2 level
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related to star's temperature
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star color
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absorb all colors
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black objects
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reflect all colors
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white objects
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