# data[].attributes.body
https://www.nationalgeographic.org/encyclopedia/mantle/
https://www.google.com/search?q=earth%27s+layers+unlabeled&source=lnms&tbm=isch&sa=X&ved=0ahUKEwio1Jqx5oLaAhUFj1kKHaUzBfYQ_AUICigB&biw=1090&bih=489#imgrc=Kdjnb1_zbJv83M:

# data[].attributes.body
-Both the continental and the oceanic crusts are bonded to the mantle to form a layer known as the lithosphere.

-the inner is believed to be as hot as the sun!

-Some parts of the mantle electrical conductivity, not seismic waves.

# data[].attributes.attachment_link.title
Structure of the Earth: Crust, Mantle and Core

# data[].attributes.attachment_link.title
The Earth and its layers  | Educational Video for Kids

# data[].attributes.body
continental crust: Portion of Earth’s crust that makes up the continents.

crust: Thin brittle outer layer of Earth.

oceanic crust: Portion of Earth’s crust that makes up the seafloor.

conduction: Process in which energy moves from a location of higher temperature to a location of lower

temperature as heat; only the heat moves, not the material.

convection: Movement of material due to differences in temperature.

peridotite: Dense, dark igneous rock that makes up the mantle.

Density: this depends in how hot or cold it is. The colder it is the more dense it is.

# data[].attributes.body
Density shows that Earth’s core is metal. Seismic waves let us know that the inner core is solid and the outer core is liquid. Metallic meteorites and the magnetic field also help us find out more about the core.

# data[].attributes.body
The mantle is composed of solid peridotit. Conduction from the core heats the lower mantle. Mantle convection bring hot material up toward the surface of the earth. It brings cooler material down toward the core.

# data[].attributes.body
Oceanic crust is thinner and denser than continental crust. It is also darker in color and denser. Continental crust is lighter and less dense. The crust is very thin compared to Earth’s radius.