2006 kuril islands earthquake

Depth: 10 km 5.3 magnitude earthquake. Aftershocks of the 6.0 quake Kuril Islands (Russia) 30 September 2006 17:56 GMT More info Based on its magnitude, the fault that was active during the quake ruptured along a surface of approx. The 2006 rupture is located beneath the only region of the Kuril Islands arc with a significant fore-arc basin. The nature of seismic coupling in the gap had been uncertain due to the limited historical record of prior large events and the presence of … Giuseppe Mercalli Peak ground acceleration Seismic intensity scales Earthquake Rossi–Forel scale The 2006-2007 Kuril Islands great earthquake sequence. On 15 November 2006, a great earthquake occurred off the coast near the Kuril Islands. Earthquake Monitoring with Gravity Meters: Case Studies from the November 2006 and January 2007 Kuril Islands Earthquakes Publisher – SEG/EAGE 2010 Summer Research Workshop, Low Frequencies: Their value and challenges, August 15-20, 2010, Snowbird, Utah Map showing regional bathymetry and tectonic features, along with global centroid moment tensor (CMT) solutions for the larger earthquakes in the 2006–2007 Kuril Islands sequence (focal mechanisms), and NEIC epicenters of activity prior to the doublet (gray circles) between the two largest events (yellow circles), and following the 13 January 2007 event (orange circles). 2006-11-15 12:15:23 UTC at 12:15 November 15, 2006 UTC Location: Epicenter at 46.301, 154.407 Northwest Of Kuril Islands. However, the 15 November 2006 Kuril underthrusting event ruptured a region with a relatively strong positive TPGA, conflicting with the typical pattern. Strong currents that persisted over an eight-hour period damaged floating docks and several boats and caused an estimated $9.2 million in losses. Almost 100 events were identified by DASE analysts 21 hours after the main shock (Figure 4). Large seismic slip has 5.3 magnitude earthquake. 2006-11-15 12:15:23 UTC at 12:15 November 15, 2006 UTC Location: Epicenter at 46.301, 154.407 Northwest Of Kuril Islands. The southwestern half of a ̃500 km long seismic gap in the central Kuril Island arc subduction zone experienced two great earthquakes with extensive preshock and aftershock sequences in late 2006 to early 2007. The last major earthquake to hit the Kuril Islands region occurred in 2006. In spite of the quake's large 8.3 magnitude, a relatively small tsunami was generated. 100 km 2 (=39 sqare miles) as a first-order estimate. The main shock of November 15, 2006 occurred at a shallow depth and less than 80 km from the Kuril trench. Shin‐Chan Han, Jeanne Sauber, Fred Pollitz, Postseismic gravity change after the 2006–2007 great earthquake doublet and constraints on the asthenosphere structure in the central Kuril Islands, Geophysical Research Letters, 10.1002/2016GL068167, 43, 7, (3169-3177), (2016). Depth: 10 km Finally, numerous aftershocks occurred (two of which of magnitude above 6.0) in the hour following the main shock. The 2006 Kuril Islands earthquake occurred on November 15 at 8:14:16 pm JST with a magnitude of 8.3 and a maximum Mercalli intensity of IV (Light). On November 15, 2006, Crescent City in Del Norte County, California was hit by a tsunami generated by a M w 8.3 earthquake in the central Kuril Islands.

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