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Notes: Layers of the Earth, Lecture notes of Earth Sciences

Outer layer; covers the whole earth; varies in thickness from 5 to ... Chemical composition: rocks rich in calcium and aluminum silicates.

Typology: Lecture notes

2021/2022

Uploaded on 09/12/2022

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Notes: Layers of the Earth
Crust
Outer layer; covers the whole earth; varies in thickness from 5 to
60 Km. Together with the upper mantle, is part of a zone called
the lithosphere.
There are 2 kinds of crust: continental crust and oceanic crust.
Continental Crust
Exists under continents
Average thickness is 30-50 Km (thickest under mountains),
although it can be as thin as 10 Km in places
Chemical composition: rocks rich in calcium and aluminum
silicates
**Note: a silicate contains the molecule, SiO2
Common rock types: granite and rhyolite
Rocks are less dense, lighter in color than oceanic crust
Oceanic Crust
Exists under oceans
Average thickness is 7 Km
Chemical composition: rocks rich in iron and magnesium silicates
Common rock types: basalt, obsidian, gabbro
Rocks are more dense, darker in color than continental crust
Mantle (Chemical Composition: iron & magnesium silicates)
Lies underneath the crust
2900 Km thick
The lithosphere is a zone made of the upper mantle and entire
crust. It is made of cool, hard rock.
Most (but not the very upper part) of the mantle is plastic rock: is
both solid and molten at the same time. This zone is called the
asthenosphere.
Underneath the asthenosphere is the mesosphere, which is solid.
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Notes: Layers of the Earth Crust Outer layer; covers the whole earth; varies in thickness from 5 to 60 Km. Together with the upper mantle, is part of a zone called the lithosphere. There are 2 kinds of crust: continental crust and oceanic crust. Continental Crust  Exists under continents  Average thickness is 30 - 50 Km (thickest under mountains), although it can be as thin as 10 Km in places  Chemical composition: rocks rich in calcium and aluminum silicates **Note: a silicate contains the molecule, SiO 2  Common rock types: granite and rhyolite  Rocks are less dense, lighter in color than oceanic crust Oceanic Crust  Exists under oceans  Average thickness is 7 Km  Chemical composition: rocks rich in iron and magnesium silicates  Common rock types: basalt, obsidian, gabbro  Rocks are more dense, darker in color than continental crust Mantle (Chemical Composition: iron & magnesium silicates)  Lies underneath the crust  2900 Km thick  The lithosphere is a zone made of the upper mantle and entire crust. It is made of cool, hard rock.  Most (but not the very upper part) of the mantle is plastic rock: is both solid and molten at the same time. This zone is called the asthenosphere.  Underneath the asthenosphere is the mesosphere, which is solid.

The asthenosphere has convection currents, where matter rises to the top, cools, then comes back down again, in a continuous cycle. Core Center of the Earth; ~ 3500 Km thick Outer Core  Made of molten iron and nickel  2270 Km thick Inner Core  Made of solid iron and nickel. Is solid because of the extreme pressures it is under.  1220 Km thick As we progress from the exterior to the interior of the Earth:  Temperature increases  Pressure increases  Density increases  Chemical compsition changes Earth may be divided into 3 layers based on chemical composition  Crust  Mantle  Core Earth may be divided into 5 layers based on physical properties  Lithosphere  Asthenosphere  Mesosphere  Outer core  Inner core