Term 4 Exam Year 8 Semester 2 Flashcards
What causes earthquakes?
Earthquakes are caused by the build up and release of stress within strata.
What is elastic rebound?
As stress accumulates in ricks either side of the fault the rocks bend and distort until the earthquake occurs and the rocks snap back to their original state releasing energy that produces seismic waves.
What is the epicentre?
The epicentre is the place in the earths surface where the earthquake is first felt.
What is the focus?
The focus is the place inside the earth where the earthquake originates.
What are seismic waves?
Seismic waves are energy released during an earthquake.
What are the three different types of seismic waves?
P Wave - Primary Waves
S Wave - Secondary Waves
L Wave - Surface Waves
What is a P Wave?
Primary Waves Fastest Compressional Weakest Travels through fluids and solids
What is an S Wave?
Secondary Waves Slower Shearing (pulls rocks in opposite directions) Stronger Only travels through solids
What is an L Wave?
Surface waves Slowest Compressional and shearing Strongest Travels through solids only
What is the asthenosphere?
The layer of slow flowing hot semi-solid rock in the upper mantle.
What is a seismograph?
A machine that records earthquake activity.
What is a seismogram?
A record of earthquake activity.
What are the different types of plate boundaries?
Transform
Divergent
Convergent (oceanic oceanic, continental continental and oceanic continental)
What is a transform plate boundary?
When two plates slide against each other, these don’t make mountains or volcanoes but do produce lots of earthquakes. An example in real life is Los Angeles close to San Francisco (extra marks) where the North American plate is slowly moving downwards and the Pacific plate is slowly moving upwards, causing a transform boundary.
What is a divergent plate boundary?
A divergent plate boundary is where two plates move away from each other causing constant creation of new land. Plates move apart and the crust expands. When two pieces of crust move away from each other, molten rock rises into the opening. An example of this in real life is Iceland because Iceland is constantly growing in size due to it being in the middle of the North American plate and the Eurasian plate.