P8.3.5 Flashcards
What are the 4 components of our Earth’s structure?
Inner core - solid
Outer core - liquid
Mantle - almost solid
Crust - solid, what we live on
What type of waves do earthquakes produce and how are they detected?
Seismic waves - used to detect the Earth’s structure
Seismometers
What are the 2 types of seismic waves and their properties?
P - waves (primary) - longitudinal, can travel through solids and liquids
S - waves (secondary) - transverse, can’t travel through liquids
Why do seismic waves take a curved path through the earth?
They bend due to the changing density.
How do we know the outer core is liquid?
The S-wave shadow zone is large and shows that the S-waves cannot penetrate part of the centre of the Earth, and since they are transverse, they cannot travel through liquids.
Why are there P-wave shadow zones?
P-waves travel faster in solids than liquids, when they enter the outer core, they refract and then refract when they leave, leaving a gap where there are no p-waves between those p-waves in the mantle and those coming from the outer core.
What do faint P-waves tell us?
They are found in the P-wave shadow zone, they show us that the inner core is solid.