there are 7 layers of earth’s inner workings these layers include crust, upper mantle, transition...
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EARTH’S STRUCTURE AND HEAT TRANSFER
There are 7 layers of Earth’s inner workings
These layers include crust, upper mantle, transition region, lower mantle, lithosphere, outer core, and the inner core
The innermost part of Earth is measured at between 9,000 and 13,000 degrees Fahrenheit
The Layers of Earth’s Core
The Crusto The crust is about 5 miles deep into the
Earth from the bottom of the ocean, but 25 miles from the surface of a continent
o At the deepest part of the Earth’s crust, the temperature is about 1600 degrees Fahrenheit
o The Earth’s crust is broken into many different plates, which move around on the surface of Earth
THE LITHOSPHERE
The lithosphere is a section of the Earth in which
the crust and upper mantle meet
The lithosphere is comprised of rigid brittle rock
Right beneath the lithosphere is the
asthenosphere, which is the portion of the Earth
that causes plate movement
The transition layer of Earth is around 250-406 miles deep
Made of mainly basaltic magmas, but also contains amounts of calcium, aluminum, and garnet
The layer becomes dense when the garnet is cooled, but buoyant and light when it is heated
TRANSITION LAYER
THE UPPER MANTLE
The upper mantle and lower mantle together make up the largest portion of Earth
Both mantles are extremely hot and plastic in texture
The upper mantle is made up of olivine and pyroxene
This layer is not entirely solid but is also partially liquid
LOWER MANTLE
This layer is also sometimes referred to as the D’’ layer
The lower mantle is between 660 and 2890 km. deep
The lower mantle’s chemical composition consists of silicon, magnesium, and oxygen
This layer is also believed to have iron, calcium, and/or aluminum in it
The outer core of Earth is around 125 to 188 miles thick and is sometimes included as part of the lower mantle because of its geographical nature
Scientists say that the outer core of Earth is made of mostly iron and nickel
This layer of Earth can heat to temperatures between 7,200 and 9,000 degrees Fahrenheit
This would normally cause the iron and nickel to melt, but the pressure from the rest of the planet keeps it mostly solid
THE OUTER CORE
Lower mantle
The INNER CORE
The inner core is a solid portion of Earth that isn’t physically attached to the mantle, but is suspended by the molten outer core
The constant rotational motion of Earth creates electrical currents, giving our planet its magnetic field
Scientists also confirmed that 10% of this layer is oxygen and/or sulfur
Transfer of HeatIn the core of the Earth, all three forms of the transfer of heat are used. Radiation from the inner core heats most of the planet, as does conduction from the touching of each layer (excluding the inner core). Convection currents take place inside the outer core and the mantle where the molten magmas move around. Finally, the crust, upper mantle, and transitional layers are all mostly or entirely solid, so heat passes between them from conduction.
Our Earth is not only heated by its molten inner core, but also by the distant sun, which radiates heat all the way back to Earth
The sun’s heat causes temperature changes in the atmosphere, which is how we feel the different seasons on Earth- because we are either closer or farther away from the sun
Earth’s axis is on a tilt of about 23.5 degrees, causing one half of the world to be closer to the sun, then rotating away so the other half is in the same position
When we absorb energy from the sun, it passes through our atmosphere, causing a loss in heat, before making its way to us on land. In the ocean, it receives even less heat at a time because it must heat a larger body than one section of land
Temperature and The Sun
http://www.universetoday.com/73597/what-is-lithosphere/
http://www.science.nationalgeographic.com http://
www.eduweb.com/portfolio/earthsystems/plate_tectonics/tectonics1.html
http://www.mnh.si.edu/earth/text/4_1_5_0.html http://www.whoi.edu/NobleMetals/Fproject2.html http://
volcano.oregonstate.edu/vwdocs/vwlessons/lessons/Earths_layers/Earths_layers4.html
http://library.thinkquest.org/28327/html/universe/solar_system/planets/earth/interior/layers_of_earth.html
Sources Cited
http://www.vlab.msi.umn.edu/projects/natLowerMant.shtml
http://education.nationalgeographic.com/education/encyclopedia/core/?ar_a=1
http://www.oup.co.uk/oxed/children/oise/pictures/earth/earthcore/
Sources Cited