Lithosphere

1. Crust                  :   The crust is very thin (average 20Km). This does not sound very thin but if you were to imagine the Earth as a football, the crust would be about ½millimetre thick
2. Oceanic Crust     :   contained Silicon and magnesium. The thinnest parts are under the oceans (OCEANIC CRUST) and go to a depth of roughly 10 kilometres
3. Continental Crust   :    contained Silium and alumunium. The thickest parts are the continents (CONTINENTAL CRUST) which extend down to 35 kilometres on average
4. Lithosphere   :   Has two layer, they are SiAl (Silium-alumunium) dan SiMa (Silikon Magnesium).It has the thickness about 40-60 kilometres. Lithosphere has Silicon-oksida until 59,12 %, and it also called Silicat layer. It has the deep 1.200 kms
5. Asthenosphere     :     The between is the nicel and ferum. It’s the liquid layer. It has the deep 1700 kms and it has the very high temperature
6. Mohorocivic   : it’s stronger due to high pressure. It layed between mantle and Lithosphere
7. Mantle           :  It’s the layer of hard rock. Its temperature is 3000⁰ C. And the thickness is 2900 kms
8. Outer core    :    The outer core is the layer beneath the mantle. It is made of liquid iron and nickel. Complex convection currents give rise to a dynamo effect which is responsible for the Earth's magnetic field. Its thickness is 2200 kms
9. Inner core   :   The inner core is the bit in the middle!. It is made of solid iron and nickel. Temperatures in the core are thought to be in the region of 5000-6000°c and it's solid due to the massive pressure. Its thickness is 1250 kms