2. Earth is composed of rock – both solid and molten – as well as
various metallic elements.
This solid part of the Earth, as well as the soil and loose rock
on the exterior, makes up the geosphere.
The geosphere may be taken as the collective name for
the lithosphere, the hydrosphere, the cryosphere, and
the atmosphere.
The geosphere consists of an outer solid layer composed of
rocks and minerals that make up rocks, soil and sediments.
3. The Earth’s geosphere is divided into three
chemical sections:
a) The Crust, composed almost entirely of
light elements, like silicon.
b) The Mantle, which is 68% of the Earth’s
mass.
c) The Core, the innermost layer; it is
composed of very dense elements, such as
nickel and iron.
4. The crust is the outer hard layer of the Earth. It is a part of
the lithosphere.
The crust is the thin outermost layer of the geosphere. It is
divided into plates that move slowly over earth surface.
The crust has two different parts. One is the continental
crust (under the land) and the other is oceanic crust (under
the ocean). The continental crust is thicker, and the oceanic
crust is thinner. Thicknesses of the crust can be anywhere
from 5–70 km.
The crust is made up of different types of rocks; igneous,
metamorphic, and sedimentary rocks.
The crust and the upper mantle make up the lithosphere.
5. The mantle is about 2900 km thick.
It is made up of dense materials, which
are rich in iron.
The mantle is semifluid; the molten rock
flows very slowly, which lets the solid
plates move on top (Much like cereal
flows on top of syrup!).
6.
7. The Earth can also be divided into five layers,
based on its physical properties.
They are:
Lithosphere – rigid and solid earth
Asthenosphere – plastic; made of molten rock
Mesosphere – Lower mantle, transitions to the
liquid outer core
Outer Core – made of dense, molten iron and
nickel
Inner Core – made of solid iron and nickel
8. The lithosphere is cool, solid and
rigid.
It is divided into many smaller
pieces called Tectonic plates.
9. The asthenosphere is semi-fluid,
molten rock.
This allows the tectonic plates to
move on top.
This motion is essential to our
Earth‘s appearance.