51 results were found for WA 0821 1305 0400 RAB Konblok Taman Cluster Perumahan Terpercaya Penjaringan Jakarta Utara.

Results:

• 11. Earthquake activity offshore North Iceland continues

  of the main cluster where the M5.6 event occurred on Sunday morning. Yesterday's cluster is located slightly closer to the Húsavík Flatey Fault and strongest events were around M3.9 at 05:25 and 05:32. Another M3.5 earthquake at 21:16 on 22. October and an earthquake M4.0 at 05:27 on 23. October were again located in the area of the M5.6 main shock further northwest. These earthquakes are purely /about-imo/news/nr/2558

• 12. Earthquake sequence east of Grímsey

  been manually revised so far are shown as red dots. The M5.5 mainshock is located on a north-south striking left lateral strike-slip fault, see black lines in the map. The M4.7 event around 9 am was located on a normal fault to the north-west. This cluster at about 7.5 km distance to the main cluster was most likely activated due to static stress changes induced by the M5.5 earthquake /about-imo/news/nr/2681

• 13. Earthquake activity east of Grímsey has decreased

  parts of the Grímsey fault system. The events of 2nd April were reported earlier. Later that evening new activity started 15-20 km southeast of the main cluster, and around 23:00 two earthquakes M4.7 and 4.6 were measured in that area and felt widely in North Iceland. Both were on a left lateral strike-slip faulting. The map above shows the activity from 31st March to the late afternoon of 4th /about-imo/news/nr/2685

• 14. Seismic activity through the night

  News The towns of Selfoss and Hveragerdi cannot be seen under the cluster of dots /about-imo/news/nr/1309

• 15. VI_2009_013

  approximately 140 earthquakes between 30 January and 22 April that year. The reason probably being the depth of the seismic cluster, which was near the base of the crust. The purpose of this research is to analyze the seismic activity within Eyjafjallajökull recorded by the SIL network during the period 1991–2006, in order to study the processes that caused the heightened seismicity and uplift /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 16. Further information on the seismicity in Northern Iceland

  were M 3.6 at 03:42 and M 3.2 at 07:47. Since the afternoon of 23 October, a new cluster of earthquakes has occurred about 5 km north-northwest of Gjögurtá on the intersection of the eastern end of Eyjafjarðaráll and the Húsavík-Flatey Fault (HFF). The largest events in this region were M 3.1 at 23:38 on 23 October and 3.2 at 22:20 on 24 October (see the map). Movements on the fault of the M /about-imo/news/nr/2561

• 17. PhD Workshop 2012

  structure, analysis or interpretation of their study). Small clusters of 3 or 4 related dissertation projects will be discussed and reviewed with the aid of experts in parallel sessions. Following acceptance and registration for the Workshop, every PhD student will be allocated a mentor from the pool of experts. Each cluster will receive several assignments for group work. The Workshop will also include 2 /nonam/adaption/phd-workshop-2012/

• 18. norsem_begga

  earthquake locations significantly. Our first step is to test the algorithm on a small subset of 215 earthquakes in year 2001, as reported in the SIL catalog, the earthquakes being located in and around the Geysir region in Southern Iceland. Three small areas were active during the year of 2001, although only one of them was recorded to be active as an earthquake sequence (western cluster; main /media/norsem/norsem_begga.pdf

• 19. norsem_korja

  reactivation type (reverse, normal or strike slip) based solely on their azimuth. The earthquakes in the seismically most active area, close to Skellefteå, Sweden along the western coast of the Gulf of Bothnia and its north-easterly continuation, appear to cluster around the shoreline and along post-glacial faults, which are mostly oriented optimally for reverse or strike slip faulting /media/norsem/norsem_korja.pdf

• 20. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf