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STRUCTURE AND COMPOSITION OF EARTH
- 1. Submitted by :- PATEL KIMAL M.Sc. ENVIRONMENTAL SCIENCE Roll no: 312
- 2. On the basis of Relative position, Density, & Composition of the Earth summarize there are three different types of layers of the Earth. Which is identified the structure of the Earth. These three layers are. • Crust • Mantle • Core
- 4. Crust Outermost Thinnest Layer Continental Crust Made of Graniteincl. continents Oceanic crust Made of basaltincl. Ocean floor 5-10 km thick
- 5. The outermost layer of the Earth is the crust. It is also the surface of the earth. This comprises the continents and ocean basins and therefore it has been classified into continental crust and oceanic crust. The oceanic crust extends up to a distance of 5-10 km average. Whereas the continental crust would extend up to 20-70 km average. The oceanic crust is mainly composed of basaltic igneous rocks, mainly of silica and magnesium and therefore also called SIMA layer. The continental crust is composed of crystalline and granitic rocks mainly of silica and aluminum and therefore also called SIAL layer.
- 6. Mantle The biggest layer of the Earth Upper mantle Top part + crust lithosphere 350-670 km Lower mantle Solid hot rock can flow like liquid
- 7. The next layer is the mantle, which is composed mainly of iron and magnesium silicates. It is been referred as FaMa layer. Mantle is also where most of the internal heat of the Earth is located. It is about 2900 km thick. It can be subdivided into four layers namely (1) Lithosphere (70 -100 km) (2) Asthenosphere (100 – 350km) (3) Upper Mantle (350 -670km) (4) Lower Mantle (670 – 2900km)
- 8. The lithosphere is a layer that includes the crust & the upper part most portion of the mantle. It has a part of the tectonic plates that cover surface of Earth. Asthenosphere is the top layer of the upper mantle 100-200 km below surface. It is a low seismic velocity zone where rocks are at or near melting point. It also has a part of tectonic plates. The lower mantle is probably mostly silicon, magnesium and oxygen with some iron, calcium and aluminum. The upper mantle is made up of mostly olivine and pyroxene (iron/magnesium silicates), calcium and aluminum.
- 9. CORE Made mostly of IRON 2 parts Outer core :- Liquid (flows in currents) Inner core :- Solid Megnetic Field
- 10. The outer core is a hot and liquid layer comprising mainly of nickel and (liquid) iron. Therefore it is referred as NiFe layer . The outer core may also contain lighter elements such as Si, S, C, or O. The outer core ranges from 2900km to 5150km and is 2300 km thick. The Earth’s magnetic field is believed to be controlled by the liquid outer core. It is also believed to be the responsible force of earth’s rotation and electric currents. The transition space between outer core and mantle is called Gutenberg discontinuity.
- 11. This layer stretches from 5150 km to 6370 km and is nearly 1200km thick. The inner core is mostly made of solid iron and has little amounts of nickel. It is unattached to the mantle and is suspended in the molten outer core. The inner core is believed to have the extreme temperature and pressure conditions. The transition region between outer core and inner core is called lehmann discontinuity.
- 12. Ocean : the vast body of salt water that cover almost three fourth of the earth surface . Trenches : from when one tectonic plats slides beneath another plates at a subduction zone. Hot spot : a small area with relatively high temperature in a comparison to its surroundings.
- 13. Continent : A continent is one of the earths seven main division of land. Oceanic ridge : Is an under water mountain system for med by tectonic plates. Island arc : an Iceland arc is a type of archipelago often composed of a chain of volcanoes with arc shaped alignment situated parallel and close to a boundary between two converging tectonic plates.