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2013 10 6 21 33 20.0 -36.75 -97.75 33.0 6.2 WEST CHILE RISE
2013 10 6 21 18 48.0 -19.75 169.25 33.0 5.1 VANUATU ISLANDS
2013 10 6 17 20 40.0 -53.50 140.50 33.0 5.2 WEST OF MACQUARIE ISLAND
2013 10 6 16 38 16.0 12.25 141.75 33.0 6.2 SOUTH OF MARIANA ISLANDS
2013 10 6 15 10 56.0 17.25 -100.25 33.0 5.1 GUERRERO, MEXICO
2013 10 6 14 27 52.0 17.25 -100.25 33.0 5.0 GUERRERO, MEXICO
2013 10 6 8 3 12.0 -33.50 77.50 33.0 4.7 MID-INDIAN RIDGE
2013 10 6 1 37 28.0 45.50 26.50 33.0 5.5 ROMANIA
2013 10 5 14 35 20.0 -30.75 -177.75 33.0 4.9 KERMADEC ISLANDS, NEW ZEALAND
2013 10 5 8 57 28.0 51.75 -172.75 33.0 4.9 ANDREANOF ISLANDS, ALEUTIAN IS.
2013 10 5 6 31 12.0 -7.50 -13.50 33.0 4.8 ASCENSION ISLAND REGION
2013 10 5 0 27 12.0 36.50 71.50 33.0 5.2 AFGHANISTAN-TAJIKISTAN BORD REG.
2013 10 4 17 26 24.0 -38.75 78.25 33.0 6.5 MID-INDIAN RIDGE
2013 10 4 12 44 16.0 1.75 128.25 33.0 5.2 HALMAHERA, INDONESIA
2013 10 4 11 19 4.0 28.25 -105.25 33.0 4.9 CHIHUAHUA, MEXICO
2013 10 4 10 35 44.0 -11.75 121.75 33.0 5.1 SOUTH OF TIMOR, INDONESIA
2013 10 4 8 32 0.0 -30.75 -178.25 33.0 5.0 KERMADEC ISLANDS, NEW ZEALAND
2013 10 4 1 38 16.0 51.00 157.00 33.0 4.9 NEAR EAST COAST OF KAMCHATKA
2013 10 3 19 58 24.0 14.25 -93.25 33.0 4.8 NEAR COAST OF CHIAPAS, MEXICO
2013 10 3 19 50 0.0 -14.25 -13.75 33.0 4.9 SOUTHERN MID-ATLANTIC RIDGE
2013 10 3 17 46 56.0 55.00 167.00 33.0 5.5 KOMANDORSKIYE OSTROVA REGION
2013 10 3 17 32 48.0 -29.50 -178.50 33.0 5.1 KERMADEC ISLANDS, NEW ZEALAND
2013 10 3 15 24 24.0 -13.75 166.25 33.0 4.9 VANUATU ISLANDS
2013 10 3 6 12 56.0 27.50 88.50 33.0 4.8 SIKKIM, INDIA
2013 10 3 5 23 28.0 -15.75 177.75 33.0 4.9 FIJI ISLANDS
2013 10 3 4 13 52.0 28.00 130.00 33.0 5.2 RYUKYU ISLANDS, JAPAN
2013 10 3 3 51 44.0 14.75 144.25 33.0 4.8 MARIANA ISLANDS
2013 10 2 19 39 28.0 2.25 127.25 33.0 4.8 NORTHERN MOLUCCA SEA
2013 10 2 18 9 36.0 55.25 163.25 33.0 4.9 OFF EAST COAST OF KAMCHATKA
2013 10 2 15 26 32.0 19.00 -65.00 33.0 4.7 PUERTO RICO REGION
2013 10 2 10 7 4.0 -2.25 139.75 33.0 5.2 NEAR NORTH COAST OF IRIAN JAYA
2013 10 2 2 52 56.0 -4.75 123.75 33.0 5.0 BANDA SEA
2013 10 2 1 6 32.0 11.25 57.75 33.0 5.7 OWEN FRACTURE ZONE REGION
2013 10 2 0 58 0.0 0.50 -89.50 33.0 5.5 GALAPAGOS ISLANDS, ECUADOR
2013 10 1 19 41 36.0 56.25 -34.75 33.0 5.6 REYKJANES RIDGE
2013 10 1 14 58 8.0 -3.50 151.50 33.0 5.0 NEW IRELAND REGION, P.N.G.
2013 9 30 22 41 12.0 -21.25 -174.25 33.0 5.2 TONGA ISLANDS
2013 9 30 20 21 12.0 55.50 -34.50 33.0 4.9 REYKJANES RIDGE
2013 9 30 12 25 28.0 -5.00 149.00 33.0 5.6 NEW BRITAIN REGION, P.N.G.
2013 9 30 8 16 8.0 49.25 -28.25 33.0 5.7 NORTHERN MID-ATLANTIC RIDGE
2013 9 30 5 56 0.0 -30.75 -178.25 33.0 6.4 KERMADEC ISLANDS, NEW ZEALAND
2013 9 30 3 44 40.0 26.25 60.25 33.0 4.9 SOUTHERN IRAN
BobAthome
reply to post by muzzy
" iridium, a heavy metal rare " is this one of those ,,"rare earth metals?",, cause just curious,
BobAthome
For Graph-aholics
taken 2:59 Atlantic Canada time,,
amazing timing
Localisation
Solomon Islands
Latitude : 10.09 °S
Longitude : 160.89 °E
Depth : 91 Km
Description
Date : 06/10/2013 16:37:05 (UTC)
Magnitude : 4.5 mb
Phase count : 17
RMS residual :1.68
Seismic event of 2013/10/06 at 16:36:58.8 UTC
Local time : 2013/10/07 at 03:36:58
in Solomon Islands
Magnitude : M 4.5
Depth : 10 km
Latitude : 10.00 S
Longitude : 160.85 E
Detected in : 3 min 58 sec
muzzy
BobAthome
reply to post by muzzy
" iridium, a heavy metal rare " is this one of those ,,"rare earth metals?",, cause just curious,
Yep, because its not from Earth
Wiki
Dianec
How I understand it - these sorts of faults are unlikely to have catastrophic earthquakes mainly because even bigger ones aren't as likely to be as destructive as they would be on another type of fault. That doesn't mean they aren't a concern. For example, it can place pressure in its neighbor San Andreas.
Dianec
I don't know if they are also seeing deformation at Joshua Tree (currently) but that could mean magma movement or it could mean more creeping (most likely the later). Regardless - as it rips apart magma will move up. Same for mammoth mountain and the rest of them. I am not reading that harmonic tremors are present yet am reading of possible magma intrusion. That tells me it is a result of the tearing - very deep down there is some pressure from magma (maybe).
Thebel
Tjörnes Fracture Zone in Iceland is getting calm, very few earthquakes happen. Is it over? Its almost like tremor in this:
If you want to destroy a car, you can do it with TNT. But more energy could be obtained by feeding an equal weight of chocolate chip cookies to a group of people and giving them sledgehammers.
Chile
A large seismic event struck the Chilean coast at 19.10:40 UT on May 22, 1960 (Plafker and Savage, 1970; Cifuentes, 1989; Cifuentes and Silver, 1989). The hypocenter was at 38.05°S – 72.34°W and the focal depth was estimated around 35 km, similar to the Sumatra earthquake. A recent relocation (Krawczyk and the SPOC Team, 2003) provides a more western and slightly deeper hypocenter > 73° 05’ W, 38° 15’ S, H = 38.5 km).
…
The records suggest that a large slow and silent foreshock took place on the deepest portion of the fault 15 minutes before the main shock, with a seismic moment comparable to that of the main event (Plafker and Savage, 1970; Kanamori and Cipar, 1974; Lund, 1982; Cifuentes, 1989; Cifuentes and Silver, 1989).
…
In this case, the rupture would have to nucleate in the subcrustal ductile lithosphere where the stress produced by the subducting slab would dissipate.
…
Alaska
In the late afternoon of March 27, 1964, the second largest earthquake (but eventually the largest on recent reassessment of magnitude by Okal – seminar at INGV headquarters) ever experienced by mankind struck the gulf of Alaska, with epicentre (61.0°N, 147.7°W) about 150 km east of Anchorage, near College Fiord (Anonymous, 1964). In the map attached to the first available report (Anonymous, 1964) a delineation of the uplifted and subsided zones is drawn (Figure 10b).
As in the Sumatra earthquake, in the Alaska seismic event a long belt – at least 500 km – of subsided crust followed an inner zone from near Anchorage to Kenai Peninsula and Kodiak Island. A subsidence of up to 2.0 m was recorded. An emergence zone with a peak uplift of 8 m was recognized in the external region facing the Pacific. It was probably of the same length as the subsided one.