Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake...

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Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.
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Transcript of Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake...

Page 1: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Page 2: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.
Page 3: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Earth’s Magnetic

Field

Page 4: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.
Page 5: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

http://www.earthweek.com/2011/ew110311/ew110311h.jpg

Page 6: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

http://science.nasa.gov/media/medialibrary/2003/12/22/29dec_magneticfield_resources/nmppath2001_med.gif

Page 7: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.
Page 8: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.
Page 9: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.
Page 10: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Magnetization of Magnetite

Page 11: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Lavas record magnetic reversals

Page 12: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Magnetic reversals

over the past 20 million

years

Page 13: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.
Page 14: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Magnetic time scale • 0-700,000 -- Normal• 700,000 - 2.5 my -- Reversed• > 2.5 my -- Normal• Ko`olau lavas mostly reversed in polarity,

so they must be older than 700,000 yrs, but younger than 2.5 my

• Lavas on Kaua`i and in Wai`anae Range show normal polarity, so they must be older than 2.5 my

Page 15: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

__________ 1. According to the concepts of plate tectonics, the continents of Africa and South America are gradually approaching each other.

__________ 2. Most geologists believe that continents are larger now than they were in the past.

__________ 3. The size of the earth is gradually increasing over time because of seafloor spreading.

__________ 4. Tectonic plates drift in oceans of melted magma just below the surface of the earth.

__________ 5. When two oceanic plates collide, the colder denser older plate is stronger and subducts the newer warmer plate.

Page 16: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Maps recording the locations of earthquakes around the world show that

1. earthquakes are evenly distributed.

2. most earthquakes follow the border of the Atlantic Ocean.

3. most earthquakes occur in the interior of continents.

4. most earthquakes surround the Pacific Ocean.

Page 17: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

The lithosphere is composed of:

1. Core and mantle2. Crust and asthenosphere3. Crust and uppermost mantle4. Core and asthenosphere

Page 18: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Sea-floor spreading suggests that1. the sea floor moves away from the mid-ocean ridge.2. the sea floor moves toward the trenches.3. the sea floor age increases from mid-ocean ridge to the continents.4. all of the above are true.

Page 19: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

Most plates move at an average rate that is best described by which unit rate?1. cm/year.2. m/year.3. km/year.4. plates don’t move.

Page 20: Worldwide seismicity from 1 January 2007 to 1 June 2007. Source: USGS National Earthquake Information Center.

If you dredged a sample of volcanic rock from locality X, the most likely age of the rock (in other words, the amount of time elapsed since the rock cooled from a magma) would be:1. 1 year 2. 1 million years 3. 10 million years 4. 100 million years