MadSci Network: Earth Sciences |
First, we should review the basics of Earth's structure. The crust is the outermost shell. There are two types: ocean crust and continental crust, which have thicknesses of about 5 and 35 km, respectively. Below the crust there is the solid mantle (2885 km thick), the liquid outer core (2270 km thick) and the solid inner core (1216 km thick). Now here's where things get a little complicated: the lithosphere is made of the outermost 100 or so km of Earth and includes the crust and a thin layer at the top of the mantle. The lithosphere is cold and brittle, and is broken up into the tectonic plates. Earthquakes occur only in the lithosphere because it is brittle and can crack under the stresses of plate tectonics.
Before we go on, remember that the mantle is solid rock, but it's a
visco-elastic material that can be deformed, or flow, like
silly putty when put under slow acting stresses over very long periods
of time. The stress is caused by
Oil and coal are resources that we remove from the
shallow crust. They are formed out of formerly living things
like plants and animals that have died and been buried by natural
erosional and depositional processes occuring at Earth's surface. In
fact, for the most part we don't go very deep to get our oil from
under the ground because it's too difficult and expensive; the deepest
oil wells bottom at about 8 to 10 km. There is no oil to be found in
oceanic crust because it does not provide the hosting environment of
continental crust (offshore oil rigs drill into the continental
shelf), but there have been some
attempts
to drill through oceanic crust to the mantle. This drilling is done
in ocean crust because it is very much thinner than continental crust
and intended to find out more about the physical and chemical
properties of the upper mantle.
Try the links in the MadSci Library for more information on Earth Sciences.
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