WHAT CAUSES EARTHQUAKES AND VOLCANOES Chapter 8 Section 4.
-
Upload
augustus-brown -
Category
Documents
-
view
215 -
download
0
Transcript of WHAT CAUSES EARTHQUAKES AND VOLCANOES Chapter 8 Section 4.
WHAT CAUSES EARTHQUAKES AND VOLCANOES
Chapter 8 Section 4
Earthquakes
Plate movement occurs slowly so you can’t see or feel it.
The rocks jagged edges catch and pressure builds up
If the pressure is too strong then an earthquake happens
Earthquakes
The point underground of an earthquake is the FOCUS
The point directly above the focus on Earth’s surface is the EPICENTER
The energy of an earthquake is carried in waves The waves can move up or down The waves can move back and forth The waves can roll or move in a circular
fashion
Earthquake magnitude
The greatest damage occurs near the focus and epicenter
As the waves move out- they lose energy
Almost all the largest earthquakes have occurred in California and Alaska
The boundary between the Pacific Plate and the North American plate
Richter Scale
The magnitude of an earthquake is measured on the Richter scale
Each increase of 1 on the Richter scale means a 31 times more energy is released
Volcanoes
A volcano- an opening in the surface of one of Earth’s plates through which magma rises.
Ash cloud- tiny bits of rock spew out the opening
Crater- steep-sided depression at the top of a volcano
Caldera-crater that is at least 1.6 km wide
Volcanoes
Most often occur when one plate sinks beneath another
Most volcanoes occur on the ocean floor
Detecting an Earthquake or volcano
Seismometers- detect shaking or tremors in Earth’s crust
Magma rising or Earth’s plates moving Tiltmeter- detects changes in the slope
of the land Seismograph- records the movement or
tremors at faults