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EARTHQUAKE. 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 : atakan@ifjf.uib.no. Jordskjelv. Vi skal lære om: Hva er et jordskjelv? Hvordan oppstår det?
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EARTHQUAKE 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: atakan@ifjf.uib.no
Jordskjelv • 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’?
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, USASunday, November 3, 2002 at 22:12:41 (UTC)
Large earthquakes (M>7) since 1900 Earthquakes since 1990 Focal mechanisms Earthquake history in Alaska
Secondary effects SESAME EC-RDG EVG1-CT-2000-00026