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Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle...

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Locating Earthquakes
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Page 1: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Locating Earthquakes

Page 2: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Solid Inner Core

Fluid Outer Core → magnetic field!

Flexible Mantle

Brittle Crust

What's inside the Earth...

Page 3: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Convective motions in Earth’s mantle:

→ heat transfer from the core→ hot spots on the surface→ pressure on tectonic plates

Page 4: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Earth’s Tectonic Plates

Page 5: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

The focus, which is below the Earth’s surface,is where an earthquake occurs.

The epicenter is the point on the Earth’s surfacedirectly above the focus.

Page 6: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Earthquakes send out seismic waves...

...and seismometers detect them on the surface.

Page 7: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Useful characteristics about the waves:

- shear waves- travel up and down- travel slowly- cannot travel through liquid

S Waves

- pressure waves- travel back and forth- travel quickly- can travel through anything

P Waves

Page 8: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Useful characteristics about the waves:

- shear waves- travel up and down- travel slowly- cannot travel through liquid

S Waves

- pressure waves- travel back and forth- travel quickly- can travel through anything

P Waves

Page 9: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...
Page 10: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...
Page 11: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Another useful characteristic about the waves:

Since they travel at different speeds, we canfigure out distance to the earthquake.

Page 12: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Another useful characteristic about the waves:

Since they travel at different speeds, we canfigure out distance to the earthquake.

Page 13: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Another useful characteristic about the waves:

Since they travel at different speeds, we canfigure out distance to the earthquake.

Page 14: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Another useful characteristic about the waves:

Since they travel at different speeds, we canfigure out distance to the earthquake.

Page 15: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

With distance data from 3 cities, we canfigure out where the earthquake occurred.

This is called triangulation.

Page 16: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

This is good for a shallow earthquake.

What if it's not shallow?

Page 17: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

This is good for a shallow earthquake.

What if it's not shallow?

Page 18: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

This is good for a shallow earthquake.

Not as good for a deep earthquake.

Page 19: Locating Earthquakes. Solid Inner Core Fluid Outer Core → magnetic field! Flexible Mantle Brittle Crust What's inside the Earth...

Distance (km) to focus = δt x _____________________(P speed) x (S speed)

(P speed) – (S speed)

(Don't forget to convert to cm on your map!)

To calculate distance to the earthquake...

Arrival times are given in hrs:min:sec For example, 14:35:27.8 and 14:36:19.6

δt is the difference between those times In the above example, δt = 51.8 seconds


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