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Originally posted by PuterMan
reply to post by boo1981
No, I believe it was actually an earthquake this time.
Rattled the teacups of the old ladies of Worthing!
ENGLISH CHANNEL
July 14, 2011
Time: 13:30:50.6
Lat./Lon.: 50.113 -0.727
National Grid: 491.0 km E, 24.5 km N
Depth: 10.0
Magnitude: 1.8
Originally posted by LexiconV
Buoy activity on both sides of US now.
National Data Bouy Center link
Each DART® station consists of a surface buoy and a seafloor bottom pressure recording (BPR) package that detects pressure changes caused by tsunamis. The surface buoy receives transmitted information from the BPR via an acoustic link and then transmits data to a satellite, which retransmits the data to ground stations for immediate dissemination to NOAA's Tsunami Warning Centers, NOAA's National Data Buoy Center, and NOAA's Pacific Marine Environmental Laboratory. The Iridium commercial satellite phone network is used for communication between 31 of the buoys.[2] When on-board software identifies a possible tsunami, the station leaves standard mode and begins transmitting in event mode. In standard mode, the station reports water temperature and pressure (which are converted to sea-surface height) every 15 minutes. At the start of event mode, the buoy reports measurements every 15 seconds for several minutes, followed by 1-minute averages for 4 hours.[3] The first-generation DART I stations had one-way communication ability, and relied solely on the software's ability to detect a tsunami to trigger event mode and rapid data transmission. In order to avoid false positives, the detection threshold was set relatively high, presenting the possibility that a tsunami with a low amplitude could fail to trigger the station. The second-generation DART II is equipped for two-way communication, allowing tsunami forecasters to place the station in event mode in anticipation of a tsunami's arrival.
Originally posted by summer5
reply to post by LexiconV
Well I just learned some thing new! Thank you, I had no idea
ENGLISH CHANNEL
July 14, 2011
Time: 20:55:09.1
Lat./Lon.: 50.078 -0.600
National Grid: 500.2 km E, 20.8 km N
Depth: 10.0
Magnitude: 1.8
ENGLISH CHANNEL
July 14, 2011
Time: 13:30:50.6
Lat./Lon.: 50.113 -0.727
National Grid: 491.0 km E, 24.5 km N
Depth: 10.0
Magnitude: 1.8
ENGLISH CHANNEL
July 14, 2011
Time: 06:59:10.9
Lat./Lon.: 50.122 -0.743
National Grid: 489.8 km E, 25.5 km N
Depth: 10.0
Magnitude: 3.9
Intensity: 3
FELT S COAST ENGLAND
A network of hidden faults on the outskirts of Christchurch will be the focus of more research to ascertain their earthquake risk.
Seismic surveying by Canterbury University and Calgary University researchers has revealed 10 previously unknown faults west and southwest of the city, including one running from near Lincoln to Halswell.
The survey work is looking at the area between the ends of the Greendale and Port Hills faults, known as "the gap".
At a briefing yesterday, GNS Science natural hazards platform manager Kelvin Berryman said a 30 kilometre line had been surveyed from north of Lincoln across State Highway 1 near Weedons to State Highway 73 just east of West Melton
A cross-section of rocks and sediment to about 1.5km underground showed five faults between about Lincoln and Weedons extending to within about a hundred metres of the surface.
Between there and West Melton there was also evidence of five very old faults in rocks below about 1km, he said.
The surveying had shown there was no obvious connection between the Greendale and Port Hills faults, although the Greendale Fault might extend further east than previously thought.
"There's lots of question marks still. It's complicated down there. There's multiple hidden fault structures."
A fault running from west of Lincoln to northwest of Halswell ran through the "gap" and separated the two other faults.
The magnitude-5.4 earthquake on June 21, centred near Halswell and Prebbleton, was the strongest locally felt earthquake of the 10-month series.
With ground accelerations of up to 60 per cent of gravity, it was felt more sharply than the September 4 magnitude-7.1 shock, Berryman said.
"In the Halswell-Lincoln zone so far, the total amount of energy released on that [fault] is less than that of a magnitude-6.0 earthquake, so that could be one of the candidates if there were to be another magnitude-6.0-plus earthquake.
"We need to be careful and cautious.
"This is quite preliminary. There's no evidence of these things at the surface. It may have done its dash, but there's still a lot of activity going on over there," Berryman said.
"That is a good place to keep working for a few months."
The Boxing Day quake, generated by a small fault under the northern central business district, was still a mystery, he said.
"There has been no further activity on that, which I'm guessing is a really good sign."
The June 13 quake appeared to have been produced by a six to eight-kilometre fault roughly parallel to the coast from north of New Brighton to the Avon-Heathcote Estuary and possibly further south.