Earthquakes (ch.4) Flashcards
Seismology
The scientific study of earthquakes
Magnitude
The strength of an earthquake
Earthquake
a series of seismic waves or tremors in the earth’s crust
What causes earthquakes?
Earthquakes are caused when pressure builds up at the edge of the plates as they collide or slide past one another. When this pressure is released a huge amount of energy is released causing the plates to shake. This shaking movement is the earthquake.
Fault lines
long deep cracks in the earth’s crust
Focus
The point where an earthquake begins deep underground
Epicentre
The point on the Earth’s surface directly above the focus
Tremors
Waves of seismic energy which spread out from the focus
Aftershocks
Smaller tremors which may occur hours or days after the original earthquake. They can be extremely dangerous as they may cause already damged buildings to collapse.
Name a fault line
San Andreas Fault, California, USA
- boundary between the Pacific and American plates
Seismograph
an instrument used to measure the strength or force of an earthquake
Richter Scale
registers the scale or magnitude of an earthquake.
How does the Richter Scale work?
The scale ranges from 1 to 10, 1 is the weakest and 10 is the strongest. An increase of one unit on the scales means that an earthquake is 10 times more powerful.
Name three major earthquakes
- Chile - 1960 9.5 magnitude
- Alaska - 1964 9.2 magnitude
- Sumatra - 2004 9.1 magnitude
Explain how a tsunami occurs and include an example.
A tsunami occurs when an earthquake happens under the ocean.
- As the plates move vertically, a huge volume of water is displaced.
- Energy from the earthquake travels through the sea water and creates waves.
- The waves reach the shallow water near the coast and can grow to height as high as 30m.
- The water floods the coastline - huge damage is done to property and the environment and many lives can be lost.
e. g. Japanese Tsunami 2011
- killed 16,000 people