https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp Made in China en-us 2022-02-28 20:11:49 UTC 2022-03-22 21:17:40 UTC hello@padlet.com dofiiakazanovska https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2070361461 The geosphere is the rocky part of our planet.
It made of: minerals and rocks.
It contains three layers inside: Crust, mantle and core.]]> 2022-02-28 21:52:20 UTC https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2070361461 dofiiakazanovska https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2070364120 Is the layer in where we live, it is about 70km wide.
There are two tipes of cust:

]]> 2022-02-28 21:54:57 UTC https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2070364120 dofiiakazanovska https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2070372963 The mante is the middle layer of the geosphere, it is about 2830 km wide. It starts in the kilometre 70 and Finnish in the kilometre 2900 approximately.
There are two tipes of mantle: upper mantle(solid but elastic) and outer mantle (plastic).]]> 2022-02-28 22:04:10 UTC https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2070372963 dofiiakazanovska https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2108347149 Earth's outer core is a liquid layer.
About 2,260 km thick.
Composed of mostly iron and nickel that lies above Earth's solid inner core and below its mantle.
The outer core begins approximately 2,889 km beneath Earth's surface at the core-mantle boundary and ends 5,150 km beneath Earth's surface at the inner core boundary.]]> 2022-03-22 20:26:36 UTC https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2108347149 dofiiakazanovska https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2108360816 Earth's inner core is the innermost layer of planet Earth. 
It is primarily a solid Earth's inner core is the innermost layer of planet Earth. 
It is primarily a solid ball with a radius of about 1,220 km  which is about 20% of Earth's radius, about 20% of Earth's radius or 70% of the Moon's radius]]> 2022-03-22 20:37:47 UTC https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2108360816 dofiiakazanovska https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2108379230 Continental crust: Continental crust is the layer of igneous, sedimentary, and metamorphic rocks that forms the continents. This layer is sometimes called sial because its bulk composition is richer in aluminium silicates and has a lower density compared to the oceanic crust, called sima which is richer in magnesium silicate minerals and is denser. There is a reasonably sharp contrast between the more felsic upper continental crust and the lower continental crust, which is more mafic in character.

]]> 2022-03-22 20:53:36 UTC https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2108379230 dofiiakazanovska https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2108380469 Oceanic crust: Oceanic crust is the uppermost layer of the oceanic portion of the tectonic plates. The crust overlies the solidified and uppermost layer of the mantle. The crust and the solid mantle layer together constitute oceanic lithosphere.]]> 2022-03-22 20:54:30 UTC https://padlet.com/dofiiakazanovska/7axdk9m9uk2aialp/wish/2108380469