Earth Science Flashcards
Theory of Plate Tectonics:
The lithosphere is broken into large plates that interact and cause geological events
Tectonic Plates
Large plates that float slowly on a layer of fluid-like rock in the Earth’s Mantle
Layers of the Earth and their Order
Crust, Upper Mantle, Lower Mantle, Outer Core, Inner Core
Primary Wave 4 Aspects
Cause rock particles to move forward and backward
(compress and expand like an accordion),
Move the fastest,
Are the first ones detected
in an earthquake,
Can travel through liquids and solids (Earth’s
interior)
Secondary Wave 3 Aspects
Move slower than P waves, faster than surface waves, Causes rock particles to move up and down or side to side, Can only travel through solids
Surface Wave 4 Aspects:
On the surface and often cause, the greatest damage Cause rock particles to move up and down, and side to side, Slowest of the three waves, Can travel along the surface of Earth (not through Earth’s interior)
Mid Ocean Ridges
Mountain Ridges on the ocean floor
Sea Floor Spreading
The process of magma rising to the surface at mid ocean ridges to from new crust.
Divergent Plate Boundaries
When two tectonic plates move away from each other
Convergent Plate Boundaries
When two tectonic plates move towards each other
Transform Boundaries
When two tectonic plates slide past each other
Mantle Convection
the process of the mantle heating up and rising to the surface where it cools and sinks down once more, repeating the process
Hot Spots
hot regions of Earth’s
mantle where magma rises to the
surface by breaking through weak parts
of the lithosphere
Hot Spot Volcanoes
Tectonic plates can move over fixed
areas called hot spots, creating a trail
of volcanic islands, Volcanoes can form above hot spots as the
magma rises and melts through the crust
Fault
Fractures (cracks) in the Earth’s
crust. They can be as small as a
few millimeters and as large as
several kilometers.