The Earth is composed of four main layers: the inner core, outer core, mantle, and crust.
The crust is the outermost layer of the Earth. It is the thinnest layer, ranging from 5 to 70 kilometers in thickness. The crust is divided into continental crust and oceanic crust. The continental crust is thicker and less dense compared to the oceanic crust.
The mantle is the layer beneath the crust and makes up about 84% of the Earth's volume. It is composed of silicate rocks that are solid but capable of flowing over long periods of time. The mantle is divided into the upper mantle and the lower mantle based on differences in physical properties.
The outer core is a liquid layer composed of iron and nickel. It is responsible for generating the Earth's magnetic field through the movement of conductive materials. The outer core is about 2,300 kilometers thick.
The inner core is the Earth's innermost layer, consisting mostly of iron and nickel in a solid state due to high pressure despite extremely high temperatures. It has a radius of about 1,220 kilometers.
When studying the layers of the Earth, it's important to understand the composition and characteristics of each layer. Use diagrams and visual aids to help visualize the structure of the Earth's layers. Practice identifying the differences between the continental and oceanic crust, as well as the properties of the mantle, outer core, and inner core. Additionally, consider conducting experiments or simulations to demonstrate the behavior of materials under high pressure and temperature conditions.
.