How do we know that the crust, the mantle, outer core and inner core makes up the Earth, when nobody has been down there?
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Answer:
"The inner core and crust are solid; the outer core and mantle layers are plastic or semi-fluid. The various layers are separated by discontinuities which are evident in SEISMIC DATA; the best known of these is the Mohorovicic discontinuity between the crust and upper mantle." "The core is probably composed mostly of iron (or nickel/iron) though it is possible that some lighter elements may be present, too. Temperatures at the center of the core may be as high as 7500 K, hotter than the surface of the Sun. The lower mantle is probably mostly silicon, magnesium and oxygen with some iron, calcium and aluminum. The upper mantle is mostly olivene and pyroxene (iron/magnesium silicates), calcium and aluminum. We know most of this only from SEISMIC TECHNIQUES; samples from the upper mantle arrive at the surface as lava from VOLCANOES but the majority of the Earth is inaccessible. The crust is primarily quartz (silicon dioxide) and other silicates like feldspar." Source (contains other very interestin information): http://seds.lpl.arizona.edu/nineplanets/nineplanets/earth.html Other interessant information: http://mediatheek.thinkquest.nl/~ll125/en/struct.htm http://en.wikipedia.org/wiki/Structure_of_the_Earth http://www.seismo.unr.edu/ftp/pub/louie/class/100/interior.html Some articles on modern issues: Earth's Core Rotates Faster than Surface: http://www.livescience.com/forcesofnature/050825_earthcore.html Hole Drilled to Bottom of Earth's Crust, Breakthrough to Mantle Looms: http://www.livescience.com/technology/050407_earth_drill.html Finally, a Solid Look at Earth's Core: http://www.livescience.com/forcesofnature/050414_earth_core.html About a new exploring technique with neutrinos: "The heart of our planet is largely a mystery because scientists can't go there or see what's inside. Geologists have just one tool, seismology, with which to probe the inner Earth." "There are still lots of theories about what's really inside the Earth" "For the first time, researchers have detected tiny particles called geoneutrinos coming from deep within the Earth. The discovery is expected to shed light, almost literally, on the contents and processes of the planet's insides." http://www.livescience.com/forcesofnature/050727_earth_neutrinos.html
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Other answers
they know of the inner earth because of the ocean.by digging in the oil rigs, sciencetists have discovered the plates that shift. and by discovering that they had some mind teasing questions that were itching for answers. they pput long scopes down the top of the volcanoes and go as deep as they can before the scope starts to melt from the pressure.the scope has a spoon like shape at the end of it. when they bring the scope up from the volcanoe they put what they have gathered from the magma samples.also they use radars at some specific spots on the earth's crust which activates when there is an earthquake.
rolly_polly_bug
Scientest know because the deeper we dug the hotter it got. The inner core is a solid circle of fire made up of nickel and iorn that makes the magnetic fieled. The outer core is made up of iorn and nickel also. Mantel is liquid and very hot. I don't knoe how we know this but somehow we do. The crust is what we are on. The crust is moving right now. You can't feel it because it is going very so-low. Can you feel your fingernail grow? No you can't. That is how slow our crust is moving.
hoe monkey
By usin P and S waves. P waves can travel throgh liqid, S waves cant. When we pass the waves trough the Earth, the S waves curve roud that liquid core. Thats just some evidence I know of.
Gonzo
"The layering of the Earth has been inferred indirectly using the time of travel of refracted and reflected seismic waves created by earthquakes. The core does not allow shear waves to pass through it, while the speed of travel (seismic velocity) is different in the other layers. The changes in the seismic velocity between the different layers causes refraction owing to Snell's law. Reflections are caused by an large increase in seismic velocity and are similar to light reflecting from a mirror." Source: http://en.wikipedia.org/wiki/Structure_of_the_Earth
xprofessor
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