askvity

What is the hidden structure inside the Earth?

Published in Earth Structure 2 mins read

The Earth's internal structure is layered, consisting of a crust, mantle, outer core, and inner core, and recently a newly discovered donut-shaped region within the outer core.

Understanding Earth's Layers

The Earth isn't a solid, uniform sphere; instead, it's made up of several distinct layers, each with its own properties:

Layer Description State
Crust The outermost solid layer, relatively thin and brittle. Solid
Mantle A thick layer of hot, semi-solid rock. Semi-Solid
Outer Core A liquid layer of iron and nickel. Liquid
Inner Core A solid sphere of iron and nickel at the Earth's center. Solid

The Newly Discovered Donut

Recent scientific discoveries have revealed a previously unknown structure:

  • Location: Deep within the liquid outer core.
  • Shape: A large, donut-shaped region.
  • Orientation: Aligned parallel to the equator at low latitudes.

This donut-shaped region is a significant discovery that adds to our understanding of the complex dynamics within the Earth's core. It is thought to influence the flow of the liquid iron in the outer core, which in turn affects the Earth’s magnetic field.

Key Aspects of Earth’s Interior:

  • Crust: This is the outermost layer we live on, ranging in thickness from 5km under the oceans to about 70km under mountains. It's composed of various types of rocks and minerals.
  • Mantle: Below the crust is the mantle, a semi-solid layer that accounts for most of the Earth's volume. The mantle’s slow movement drives plate tectonics.
  • Outer Core: The outer core is a liquid layer of iron and nickel, generating Earth’s magnetic field due to its convection.
  • Inner Core: At the very center is the solid inner core, an extremely hot ball of iron and nickel. The immense pressure keeps it solid despite the high temperatures.

In summary, the Earth’s hidden structure is not only layered but also includes unique regions like the recently found donut-shaped area within its outer core. These findings help us comprehend Earth’s magnetic field and internal dynamics better.

Related Articles