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Science

Earth crust:

  • The outer layer of the earth.

  • thinnest layer

  • Made up of both continental (land)and oceanic crust(under the ocean).

  • least dense

  • Composed of mostly granite and basalt

    Earth Mantle:

  • Largest layer of the Earth

  • Composed of silicate rocks rich in magnesium and iron

  • Intense heat causes the rocks to rise and then cool and sink.

  • The process is called convection, which causes the crust to move.

  • Average temperature 3000

  • Made up of mostly magma

  • Contains convection currents that move the tectonic plates

Earth outer core:

  • Liquid layer 2,300 km thick, second larges

  • Composed of liquid iron and nickel

  • Lies between inner core and mantle

  • Because the magma moves around the inner core, Earth’s magnetic field is created.

Average temperature 4000o -5000o

Earth Innercore:

  • A solid ball of metal

  • Made of solid nickel and iron

  • Densest layer of the Earth

  • Average temperature 5000-6000

  • Spins at a speed faster than the Earth rotates

  • So hot it melts everything in the outer core

  • a soild

Seismic:

  • Seismic waves are used to determine which layers of the Earth are solid or liquid.

  • Some seismic waves cannot pass through certain layers giving us a clue to the layer’s composition.

    Oceanic Crust:

  • A thin layer of crust that overlies the ocean basins

  • More dense than continental crust

  • Mostly basalt rock

  • Thinner than continental crust.

  • Younger (newer) than continental crust

    Continental Crust

    Continental Crust:

  • Layer of rock which forms the continents

  • Less dense than oceanic crust

  • Mostly granite

  • Thicker than oceanic crust

  • Older than oceanic crust

Science

Earth crust:

  • The outer layer of the earth.

  • thinnest layer

  • Made up of both continental (land)and oceanic crust(under the ocean).

  • least dense

  • Composed of mostly granite and basalt

    Earth Mantle:

  • Largest layer of the Earth

  • Composed of silicate rocks rich in magnesium and iron

  • Intense heat causes the rocks to rise and then cool and sink.

  • The process is called convection, which causes the crust to move.

  • Average temperature 3000

  • Made up of mostly magma

  • Contains convection currents that move the tectonic plates

Earth outer core:

  • Liquid layer 2,300 km thick, second larges

  • Composed of liquid iron and nickel

  • Lies between inner core and mantle

  • Because the magma moves around the inner core, Earth’s magnetic field is created.

Average temperature 4000o -5000o

Earth Innercore:

  • A solid ball of metal

  • Made of solid nickel and iron

  • Densest layer of the Earth

  • Average temperature 5000-6000

  • Spins at a speed faster than the Earth rotates

  • So hot it melts everything in the outer core

  • a soild

Seismic:

  • Seismic waves are used to determine which layers of the Earth are solid or liquid.

  • Some seismic waves cannot pass through certain layers giving us a clue to the layer’s composition.

    Oceanic Crust:

  • A thin layer of crust that overlies the ocean basins

  • More dense than continental crust

  • Mostly basalt rock

  • Thinner than continental crust.

  • Younger (newer) than continental crust

    Continental Crust

    Continental Crust:

  • Layer of rock which forms the continents

  • Less dense than oceanic crust

  • Mostly granite

  • Thicker than oceanic crust

  • Older than oceanic crust

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