magnitude 6.5 kermadec islands

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Magnitude 6.5 KERMADEC ISLANDS Magnitude 5.9 KODIAK ISLAND, ALASKA

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Magnitude 6.5 KERMADEC ISLANDS. Magnitude 5.9 KODIAK ISLAND, ALASKA. Two main groups of seismic waves. Body waves travel through the Earth’s interior. Surface waves are guided by the outer layers of the Earth. Two types of body waves. P-waves = Primary Waves = first arrival - PowerPoint PPT Presentation

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Page 1: Magnitude 6.5 KERMADEC ISLANDS

Magnitude 6.5KERMADEC ISLANDS

Magnitude 5.9KODIAK ISLAND, ALASKA

Page 2: Magnitude 6.5 KERMADEC ISLANDS

Two main groups of seismic waves.

Body waves travel through the Earth’s interior.

Surface waves are guided by the outer layers of the Earth.

Page 3: Magnitude 6.5 KERMADEC ISLANDS

Two types of body waves.

P-waves = Primary Waves = first arrival

S-waves = Secondary Waves = second arrival

Page 4: Magnitude 6.5 KERMADEC ISLANDS

Two types of surface waves.

Rayleigh waves: Discovered by Lord Rayleigh (1887).

Love waves: Discovered by A.E.H. Love (1911).

Page 5: Magnitude 6.5 KERMADEC ISLANDS

Magnitude 6.5KERMADEC ISLANDS

123º

Magnitude 5.9KODIAK ISLAND, ALASKA

52º

Page 6: Magnitude 6.5 KERMADEC ISLANDS
Page 7: Magnitude 6.5 KERMADEC ISLANDS
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Magnitude 6.5KERMADEC ISLANDS

2009 May 16 00:53:46 UTC

Magnitude 5.9KODIAK ISLAND, ALASKA

2009 May 16 18:22:39 UTC

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500 Hz

570 Hz

500 Hz

550 Hz

500 Hz

530 Hz

500 Hz

510 Hz

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1 minute

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Magnitude 6.3 - Fiji 2005 December 13 03:16:09 UTC

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Magnitude 6.3 - Fiji 2005 December 13 03:16:09 UTC

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Plate Tectonics

Page 17: Magnitude 6.5 KERMADEC ISLANDS

Earthquakes

Plate TectonicsEarthquakes correlated with:

* Mid-Ocean Ridges

* Fracture Zones

* Ocean Trenches

1980-2001 (NEIC, M5)

Page 18: Magnitude 6.5 KERMADEC ISLANDS

Mechanism of Plate Tectonics

www.bibliotecapleyades.net

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Directions and Rates of Plate Motion

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QuickTime™ and aTIFF (Uncompressed) decompressor

are needed to see this picture.

QuickTime™ and aTIFF (Uncompressed) decompressor

are needed to see this picture.

U.S. Geological Survey AVO

http://whyfiles.org/031volcano/2.html

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