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Earthquake Details
This is a computer-generated message -- this event has not yet been reviewed by a seismologist.
Magnitude 3.2
Date-Time Tuesday, July 05, 2011 at 03:22:06 UTC
Monday, July 04, 2011 at 09:22:06 PM at epicenter
Location 39.932°N, 111.816°W
Depth 1.3 km (~0.8 mile) (poorly constrained)
Region UTAH
Distances 1 km (1 miles) NE (49°) from Rocky Ridge, UT
5 km (3 miles) SSW (210°) from Santaquin, UT
7 km (4 miles) SSE (166°) from Genola, UT
37 km (23 miles) SSW (201°) from Provo, UT
92 km (57 miles) S (176°) from Salt Lake City, UT
Location Uncertainty horizontal +/- 0.5 km (0.3 miles); depth +/- 4.3 km (2.7 miles)
Parameters NST= 62, Nph= 62, Dmin=5 km, Rmss=0.39 sec, Gp= 54°,
M-type=local magnitude (ML), Version=1
Source University of Utah Seismograph Stations
Event ID uu00007441
Originally posted by MoorfNZ
A 6.5 has just struck 30km west of Taupo on the North Island of New Zealand
150km in Depth
www.geonet.org.nz...edit on 4-7-2011 by MoorfNZ because: (no reason given)
Earthquake Details
This event has been reviewed by a seismologist.
Magnitude 5.3
Date-Time Tuesday, July 05, 2011 at 03:36:25 UTC
Tuesday, July 05, 2011 at 03:36:25 PM at epicenter
Time of Earthquake in other Time Zones
Location 38.597°S, 175.688°E
Depth 161.3 km (100.2 miles)
Region NORTH ISLAND OF NEW ZEALAND
Distances 69 km (42 miles) SW of Rotorua, New Zealand
144 km (89 miles) NW of Napier, New Zealand
209 km (129 miles) SSE of Auckland, New Zealand
310 km (192 miles) NNE of WELLINGTON, New Zealand
Location Uncertainty horizontal +/- 14 km (8.7 miles); depth +/- 6.1 km (3.8 miles)
Parameters NST=139, Nph=148, Dmin=73.5 km, Rmss=1.66 sec, Gp= 47°,
M-type=body wave magnitude (Mb), Version=7
Source USGS NEIC (WDCS-D)
Event ID usc0004n71ex]
Source - USGS
Originally posted by radpetey
There was a 3.7 off the coast of San Diego today at a depth of 0 km. is this a rarity?
Q: What does it mean that the earthquake occurred at a depth of 0 km?
A: An earthquake cannot occur at depth of 0 km. In order for an earthquake to occur, two blocks of crust must slip past one another, and it is physically impossible for this to happen at the surface of the earth. So why do we report that the earthquake occured at a depth of 0 km sometimes? Sometimes it is simply a very shallow event with poor depth resolution, but more often it is not actually an earthquake, but a quarry blast. These explosions are recorded by the seismic network and located by the software. When they are reviewed by a seismic analyst, they are labeled as a quarry blast in the earthquake catalog.
Volcanologist Brad Scott said although the earthquake was centred near Taupo it was more likely felt on the east coast of both islands. There had been reports of it being broadly felt along the east coast in Hawke's Bay and Wairarapa, but not in Taupo, he said. Scott said the earthquake was below the plate boundary, and the volcanic zone of the central North Island would have absorbed much of the energy.
Originally posted by PuterMan
reply to post by Moshpet
There seem to be a few in the usual place and possibly more than usual along the line of volcanoes. In terms of earthquakes in the area 40N-45N, 132.5W-123.5W the activity has been quieter earlier in the year.
Bear in mind also that Alaska has done a little stress relieving with the 7.2