Download Layers of the Earth

Survey
yes no Was this document useful for you?
   Thank you for your participation!

* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project

Document related concepts

Geochemistry wikipedia , lookup

Post-glacial rebound wikipedia , lookup

History of geology wikipedia , lookup

Nature wikipedia , lookup

Age of the Earth wikipedia , lookup

History of Earth wikipedia , lookup

Geology wikipedia , lookup

Future of Earth wikipedia , lookup

Large igneous province wikipedia , lookup

Plate tectonics wikipedia , lookup

Geophysics wikipedia , lookup

Mantle plume wikipedia , lookup

Transcript
Layers of the Earth
CRUST
5 to 70 km thick
and up to 400° C (interior)
The crust is the thin, rocky,
outer-layer on which we live.
This is the thinnest layer, but
oceans and continents sit on
the crust. The crust is not
solid—it is actually broken
into pieces we call “plates.”
OUTER CORE
2,300 km thick
and 4,000° C to 5,000° C
Located beneath the mantle,
the outer core is hotter than
the mantle. It is so hot that
the iron and nickel that make
up this layer have melted.
This is the Earth’s only liquid
layer.
MANTLE
2,900 km thick
and up to 4,000° C
Located under the crust, the
mantle is the thickest layer
and is divided into two parts.
The upper mantle is gooey,
heated rock moving slowly
under the crust. The lower
mantle is solid.
INNER CORE
2,400 km in diameter
and up to 7,000° C
The inner core is also made of
iron and nickel. This is the
hottest layer. Due to the
extreme heat and pressure at
the center of the Earth, the
inner core is solid.