Exploring the Foundations of Our Planet
A Comprehensive Overview of Earth Sciences
Geology is the primary Earth science, focusing on the solid Earth, the rocks of which it is composed, and the processes by which they change over time.
Rigid outermost shell, 5-70km thick.
Viscous layer comprising 84% of volume.
Liquid iron and nickel, creates magnetic field.
Solid ball of iron at 5,400 °C.
Rocks are constantly being recycled through three primary states:
Formed from the cooling of magma or lava (e.g., Basalt, Granite).
Formed by the accumulation of minerals or organic particles (e.g., Sandstone, Shale).
Created by the transformation of existing rock types through heat and pressure (e.g., Marble, Slate).
Weathering, erosion, deposition, lithification, and melting.
The theory that Earth's outer shell is divided into several plates that glide over the mantle.
These movements are responsible for earthquakes, volcanoes, and mountain building.
Geological time scales allow us to understand the vast history of Earth (approx. 4.54 billion years).
Understanding geology is vital for our modern society:
Thank You for Exploring Geology!