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Originally posted by muzzy
reply to post by The Great Day
said on the TV News here in New Zealand that there had been 200 aftershocks (and that was 3.5 hrs ago).
only 27 shown on Philippine Institute of Volcanology and Seismology @ this point in timeedit on 7-2-2012 by muzzy because: (no reason given)
Originally posted by muzzy
maybe it was just update time, surely they didn't just have 400 odd more in 10 minutes
here be the 30 day the map
well it was
Is there anyone who knows Japanese.
Originally posted by MoorfNZ
Magnitude 5.3, Tuesday, February 7 2012 at 11:21 pm (NZDT), 30 km west of Taumarunui, North Island, New Zealand
Depth 250km
Felt Map: www.geonet.org.nz...
Magnitude mb 5.0
Region SVALBARD REGION
Date time 2012-02-07 23:37:03.0 UTC
Location 77.05 N ; 7.24 E
Depth 2 km
Distances 1210 km NW Murmansk (pop 319,263 ; local time 02:37:03.3 2012-02-08)
898 km NW Tromsø (pop 52,436 ; local time 00:37:03.3 2012-02-08)
201 km SW Barentsburg (pop 576 ; local time 00:37:03.3 2012-02-08)
In particular, the epicentral distance limits (in km) are calculated according to the formula..........[formula does not print]...............
The aftershock zone sizes are 4.6 km for m4 and 46 km for m6.5. For the time limits we use the following formula, a variant..........[formula does not print]...............
Equation (6) yields a time limit of 3.33 days for m=4 and 33.3 days for m=5.5. If an earthquake is in the time-distance window of another larger preceding event, it is deleted from the declustered catalog.
MOLCHAN et al. (1996, 1997, p. 1223) propose the following windows for removing aftershocks: for m 6.5 the time range is 2 years. The spatial window radius is 50, 60, 70, 100, and 200 km for the earthquake magnitude ranges 5.5–6.5, 6.5–7.0, 7.0–7.5, 7.5–8.0, and >=8.0, respectively.
We use the results of the likelihood analysis of earthquake catalogs (KAGAN, 1991c) as a third declustering method. We approximate an earthquake occurrence by a multidimensional Poisson cluster process, i.e., origin time, earthquake size, and centroid location are modelled. In this model mainshocks are distributed according
to the Poisson distribution, whereas dependent events in earthquake sequences are controlled by a distribution which is characterized by a few adjustable parameters.
Originally posted by diamondsmith
The death tall from Filipino earthquake is rising,and very strange they had large waves that hit some towns.
source(blogs.voanews.com...
TextFilipino officials say a strong earthquake has rocked the central Philippines, killing at least 43 people and causing widespread damage and power outages.officials say there is no concern of a tsunami, although some coastal towns nearby were hit by large waves.
7.1 2012/02/02 13:34:41 -17.766 167.134 23.1 VANUATU
6.0 2012/02/03 03:46:23 -17.376 167.278 21.7 VANUATU
6.1 2012/02/05 00:15:41 -18.935 168.923 163.4 VANUATU
6.0 2012/02/05 16:40:40 -17.952 167.230 10.3 VANUATU
6.7 2012/02/06 03:49:17 9.964 123.246 11.0 NEGROS - CEBU REGION, PHILIPPINES
6.0 2012/02/06 10:10:24 9.874 123.070 15.0 NEGROS - CEBU REGION, PHILIPPINES
Originally posted by berkeleygal
7.1 2012/02/02 13:34:41 -17.766 167.134 23.1 VANUATU
6.0 2012/02/03 03:46:23 -17.376 167.278 21.7 VANUATU
6.1 2012/02/05 00:15:41 -18.935 168.923 163.4 VANUATU
6.0 2012/02/05 16:40:40 -17.952 167.230 10.3 VANUATU
6.7 2012/02/06 03:49:17 9.964 123.246 11.0 NEGROS - CEBU REGION, PHILIPPINES
6.0 2012/02/06 10:10:24 9.874 123.070 15.0 NEGROS - CEBU REGION, PHILIPPINES
big week - what's next?
Originally posted by jadedANDcynical
reply to post by zworld
Is there anyone who knows Japanese.
I sent a link to this post and the one wih the japanese site to it to a friend of mine who is majoring in Japanese and Chinese, will let you know when she replies.
Heck, maybe I can make her an ATS convert
source(earthquake.usgs.gov...
TextMagnitude 5.6 Date-Time Wednesday, February 08, 2012 at 10:54:43 UTC Wednesday, February 08, 2012 at 05:54:43 AM at epicenter Time of Earthquake in other Time Zones Location 0.682°N, 79.187°W Depth 69.8 km (43.4 miles) Region NEAR THE COAST OF ECUADOR Distances 65 km (40 miles) ESE of Esmeraldas, Ecuador 102 km (63 miles) N of Santo Domingo de los Colorados, Ecuador 124 km (77 miles) WNW of Ibarra, Ecuador 125 km (77 miles) NW of QUITO, Ecuador Location Uncertainty horizontal +/- 16.8 km (10.4 miles); depth +/- 8.5 km (5.3 miles) Parameters NST=396, Nph=411, Dmin=95.7 km, Rmss=0.83 sec, Gp= 90°, M-type=body wave magnitude (Mb), Version=8
source(earthquake.usgs.gov...
TextMagnitude 5.6 Date-Time Wednesday, February 08, 2012 at 12:01:37 UTC Wednesday, February 08, 2012 at 09:01:37 PM at epicenter Time of Earthquake in other Time Zones Location 37.838°N, 138.099°E Depth 9.7 km (6.0 miles) Region NEAR THE WEST COAST OF HONSHU, JAPAN Distances 84 km (52 miles) W of Niigata, Honshu, Japan 132 km (82 miles) N of Nagano, Honshu, Japan 148 km (91 miles) NNE of Toyama, Honshu, Japan 280 km (173 miles) NNW of TOKYO, Japan Location Uncertainty horizontal +/- 14.2 km (8.8 miles); depth +/- 6.3 km (3.9 miles) Parameters NST=413, Nph=413, Dmin=143.6 km, Rmss=0.66 sec, Gp= 97°, M-type=regional moment magnitude (Mw), Version=7
Magnitude mb 5.0
Region OFFSHORE CHIAPAS, MEXICO
Date time 2012-02-08 13:06:47.0 UTC
Location 15.05 N ; 94.03 W
Depth 60 km
Distances 190 km W Tapachula (pop 197,961 ; local time 07:06:47.7 2012-02-08)
112 km SW Pijijiapan (pop 15,101 ; local time 07:06:47.7 2012-02-08)
106 km SW Tres picos (pop 4,881 ; local time 07:06:47.7 2012-02-08)
New stratigraphic evidence from Cascadia demonstrates that 13 earthquakes ruptured the entire margin from Vancouver Island to at least
the California border since the eruption of the Mazama ash 7700 years ago. The 13 events above this prominent stratigraphic marker have an average repeat time of 600 years, and the youngest event » 300 years ago coincides with the coastal record.
The turbidite event stratigraphy shows a clear record for the northern » 600 km of the Cascadia Basin, the entire length of the subduction zone offshore from Washington and Oregon has ruptured 18 times in great earthquakes during the past » 9800
Around Mag 8.5 to 9
The Bradley Lake record is based only on tsunami deposited sands, exhibits a relatively greater number of events per unit time than the estuary records, and has 12 events requiring a tsunami inundation of > 5.5 m.
The uppermost turbidite event returns a "modern" age, which we interpret is likely the 1906 San Andreas earthquake. The penultimate event returns
an intercept age of AD 1663 (2 ¾ range 1505–1822). The third and fourth events are lumped together, as there is no hemipelagic sediment between them. The age of this possible couplet event is AD 1524 (1445–1664). The 5th event age is AD 1204 (1057–1319), and the sixth event age is AD 1049 (981–1188). These results are in relatively good agreement with the onshore work to date, which indicates an age for the penultimate event in the mid-1600s (Figure 7), the most likely age for the third event is » AD 1500–1600, and a fourth event » AD 1300.
The Cascadia subduction zone, which extends 1100 km along the Pacific coast of North America (Figure 1), produces infrequent earthquakes of moment magnitude (M w ) 8 or larger. The possibility of these great earthquakes was first inferred from geodesy [Savage et al.,
1981] and from geophysical and tectonic similarities with other subduction zones [Heaton and Kanamori, 1984]. The past occurrence of great Cascadia earthquakes, at intervals averaging about 500 years, was then shown by paleoseismology [Clague, 1997].
I never realised how different Japanese is from English