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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
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
formation
13.7 billion years ago: big bang
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
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)
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
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
meteroids
ranging in size from dust size to 30ft
meteoroids are broken up asteroids
still in space
meteor
makes contact with our atmosphere
meteorite
makes contact with surface
chunks that fall to earth tell us about the composition of the parent bodies they came from
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
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)
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
simple craters
typically small less than 4 mi
barringer crater
complex craters
larger in diameter greater than 4 mi
rim collapses more completely
center uplifts following impact
why earth has so few impact craters
70% of earth is covered in water
smaller meteors burn up in the atmosphere
eroded by natural processes
plate tectonics recycles crust
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
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
inner core
radius: 1220 km about the size of the moon
material: solid, metallic
made of: 90% iron with sulfur, oxygen, and nickel
outer core
thickness: 2180 km
material: liquid 10x denser than water
made of: same composition as inner core
mantle
thickness: 2900 km
material: solid rocky
made of: iron and magnesium silicates
oceanic crust
more dense
thinner
younger
basaltic
continental crust
less dense
thicker
older
granitic
kola borehole
40,200 ft to 12.2 km
19 years to drill
how we know about earth’s interior
seismology
seismic waves propagate through the earth
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
geologic processes
govern the type, location, and intensity of natural processes and natural disasters
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
paleomagnetism
refers to the magnetism of rocks and the intensity of the direction of magnetic field of earth in the geologic past
bathymetry
measure of ocean death
topography
mapping ocean floor
divergent
spreading
constructive
ridge/rift
volcanic activity and earthquakes
convergent
subduction
destructive
trench
volcanic activity
transform
lateral sliding
conservative
no major effect
no volcanic activity but earthquakes
san andreas fault
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)
continental oceanic
dense oceanic crust subducts less dense continental crust
volcanic island arc, mountains, trenches
tsunami, volcanic eruptions, and earthquakes
cascade mountain range
continental continental
when continental crust collides with continental crust
orogenies
earthquakes
Himalayas