Answer 1:
Great questions!
As to why Earth is layered, early in its history
it got hot enough (from gravitational compression,
the energy of impacting bodies, and radiation, to
have partially melted. When this happened, the
densest material sank toward Earth's center, while
the less dense stuff rose to the top. It's a
little like a hot chocolate-- foam floats to the
surface, and the heavy syrup settles to the
bottom.
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Answer 2:
The major layers of the Earth, starting from its
center, are the inner core, the outer core, the
mantle, and the crust. These layers formed as the
building blocks of Earth, known as planetesimals,
collided and collapsed under their own gravity
around 4.5 billion years ago. At that time, the
heaviest elements (like iron and nickel) sank to
the core, while the lighter elements (like
silicon, oxygen, and carbon), rose to form the
mantle and crust.
The crust itself is composed of many layers, which
are the ones we can see at the surface. Most
continents have a crystalline core, known as a
'kraton'. Every continental kraton is then draped
in many layers of sedimentary, igneous, and
metamorphic rock. The most dramatic layers, like
those in the mountain ranges above Santa Barbara,
are often sedimentary rocks, which formed as
long-gone mountain ranges eroded away and the
resulting sediments were deposited somewhere else
on the continent. A change in tectonic plate
motion then caused those sedimentary layers to be
brought up to where we can see them today.
When volcanoes erupt, the lava that comes out can
spread across broad areas, forming a layer of
igneous rock within the sedimentary layers. Thus,
most of the layering on the Earth's surface is due
to erosion and deposition of mountain ranges, and
lava flowing out on the surface.
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Answer 3:
Layers of rocks are formed when sediment is
laid down, and flattens out to be as close to the
center of the Earth as possible. Then, a new layer
is laid down, which has to fall onto the older
layer, and thus lies above it.
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