Layers of the Earth

• Crust: The Earth's outermost layer, made up of solid rock and soil.
• Mantle: The layer beneath the crust, composed of hot, semi-solid rock.
• Outer Core: A liquid layer of molten iron and nickel.
• Inner Core: The Earth's innermost layer, consisting of solid iron and nickel.

Inner Core

The inner core of the Earth is composed of solid iron and nickel. It is the hottest and most dense part of our planet, with temperatures reaching up to 5,500 degrees Celsius. Despite its extreme heat, the immense pressure keeps the inner core solid. It plays a crucial role in generating Earth's magnetic field.

Journey to the Center

• Heat Transfer in the Mantle (you need to know)

  • the Layers of the Earth

  • Understand the Mantle's Role in tectonics

  • Convection in the mantle

  • Implications for Earth's Dynamic Changes

Heat Transfer in the Mantle

Trivia: The main method of heat transfer in the mantle is convection. Convection occurs when hot material rises, cools, and then sinks back down. This process creates a continuous cycle of heat transfer, helping to drive the movement of tectonic plates on Earth's surface. Fun Fact: The mantle is the layer between the Earth's crust and core, and it makes up about 84% of the Earth's volume.

The Moho: Boundary

• The Moho is the boundary between the Earth's crust and mantle.

• It was discovered by Andrija Mohorovičić in 1909.

• The Moho is characterized by a significant increase in seismic wave velocity.

• It separates the rigid crust from the more ductile mantle.

• Understanding the Moho helps us study the Earth's structure and tectonic processes.

Moho Discovery

Trivia: The Moho, or Mohorovičić discontinuity, was discovered by Andrija Mohorovičić. It is the boundary between the Earth's crust and mantle. This discovery revolutionized our understanding of the Earth's structure. It was discovered using seismic waves in October of 1909.