Presentasjon lastes. Vennligst vent

Presentasjon lastes. Vennligst vent

K.Atakan & K.A.Atakan Institute of Solid Earth Physics University of Bergen Allégt.41, N-5007 Bergen, Norway Tel: +47-55-583413 Fax: +47-55-589669 E-mail:

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Presentasjon om: "K.Atakan & K.A.Atakan Institute of Solid Earth Physics University of Bergen Allégt.41, N-5007 Bergen, Norway Tel: +47-55-583413 Fax: +47-55-589669 E-mail:"— Utskrift av presentasjonen:

1 K.Atakan & K.A.Atakan Institute of Solid Earth Physics University of Bergen Allégt.41, N-5007 Bergen, Norway Tel: Fax:

2 Vi skal lære om: Hva er et jordskjelv? Hvordan oppstår det? Hvilke skader kan vi forvente? Hvordan registrerer vi jordskjelv? Hvordan kan vi lage et ’jordskjelv’? Jordskjelv

3 Denali earthquake of 3 Nov.2002, Alaska, USA

4 Figure Caption:Map showing M7.9 mainshock as a filled white circle and the October 23, 2002, M6.7 foreshock as an open white circle. Shown are events with magnitude greater than or equal 2.0 that occurred between October 22 and November 8, 2002, with a depth of 35 km or less. A total of 415 events are shown. The 2002 Denali Fault earthquake M=7.9 near Denali National Park, Alaska, USA Sunday, November 3, 2002 at 22:12:41 (UTC)

5 Animation of Denali earthquakes in time

6 Denali Fault: Areal view

7 Previous earthquakes along the Denali Fault

8 Earthquake history in Alaska Large earthquakes (M>7) since 1900 Earthquakes since 1990 Focal mechanisms

9 Gravity and aeromagnetic maps

10 Avalanches in the Denali area

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12 Surface ruptures in the Denali area

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22 Secondary effects

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24 Denali aftershocks

25 SESAME EC-RDG EVG1-CT Secondary effects

26 Istanbul urban area development


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