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Originally posted by lordpiney
ive tried to find the info myself, but had no luck so...do any of you know what was the largest number of quakes ever recorded in one day worldwide?
Originally posted by MamaJ
Originally posted by lordpiney
ive tried to find the info myself, but had no luck so...do any of you know what was the largest number of quakes ever recorded in one day worldwide?
Thats a really good question but I have no idea....would like to know myself.
I found this site although I am not sure of the accuracy. Check it out. www.ceri.memphis.edu...
Magnitude 3.1
Date-Time Monday, February 27, 2012 at 04:30:47 UTC Sunday,February26,2012at 10:30:47PM at epicenter Time of Earthquakein otherTimeZones
Location 36.112°N, 100.556°W
Depth 5 km (3.1 miles)
Region TEXAS PANHANDLE REGION
Distances 38 km (23 miles) SE of Perryton, Texas 73 km (45 miles) NNE of Pampa, Texas 78 km (48 miles) S of Beaver, Oklahoma 699 km (434 miles) NNW of AUSTIN, Texas
Location Uncertainty horizontal+/- 14.1 km (8.8miles);depth +/- 3.1km (1.9miles)
Parameters NST= 13, Nph= 13, Dmin=142.5 km, Rmss=0.65 sec, Gp= 65°, M-type="Nuttli" surface wavemagnitude(mbLg),Version=A
Source Magnitude: USGSNEIC (WDCS-D) Location: USGSNEIC (WDCS-D)
Event ID usb00086nc
Originally posted by lordpiney
ive tried to find the info myself, but had no luck so...do any of you know what was the largest number of quakes ever recorded in one day worldwide?
Submarine volcano
Calderas
Cones
Summit Elev: -385 m
Latitude: 24.80°S
Longitude: 177.02°W
A large submarine volcano located at the southern end of the Tonga arc rises to within 385 m of the sea surface. Known informally as Volcano 19, the basaltic to basaltic-andesite seamount contains two calderas, a 3.5 x 2.5 km wide outer caldera and a 1.9-km-wide inner caldera on the west side of the volcano. A central cone complex lies in the center of the outer caldera, east of the inner caldera. Two large hydrothermal fields are located near the summit of the central cone complex and at the base of the southern wall of the western inner caldera. Large high-temperature chimney vents discharge clear fluids and black smoke.
Historic seismicity shows that it's not alone and that since 1990 there've been a few quakes in the area.
I know this thread is really about quakes but we find more and more how interlinked they are and Dutch Sinse here puts out a warning with this recent Japanese Volcano which has been naughty for about a year now but appears to be gearing up for showing off.
Despite the tremendous progress made since Wiechert in understanding the most prominent features in seismic records, long-period ones in particular, we are still well short of reaching the goal he set. In fact, most operators and analysts at seismological observatories, even those who work with the most modern equipment, have not advanced much beyond the mid 20th century with respect to their capability to "understand each wiggle" in a seismic record.
source(www.emsc-csem.org...
Magnitude ML 4.0
Region FRANCE
Date time 2012-02-27 16:31:22.0 UTC
Location 44.49 N ; 6.66 E
Depth 2 km
Distances 100 km NW Nice (pop 338,620 ; local time 17:31:22.1 2012-02-27) 47 km S Briançon (pop 11,577 ; local time 17:31:22.1 2012-02-27) 8 km SW Saint-paul-sur-ubaye (pop 202 ; local time 17:31:22.1 2012-02-27)
1.2.2.1 The magnitude issue
Earthquake magnitude is one of the most widely used parameters in seismological practice,and one that is particularly subject to misunderstanding, even by seismologists. Examples of the way in which changing operational procedures have contaminated a valuable data set haverecently been put forward and discussed in the Seismological Research Letters. After re-examining the earthquake catalogue for southern California between 1932 and 1990, Huttonand Jones (1993) concluded:
•
ML magnitudes (in the following termed Ml with l for “local”) had not been consistently determined over that period;
•
amplitudes of ground velocities recorded on Wood-Anderson instruments and thus Ml were systematically overestimated prior to 1944 compared to present reading procedures;
•
in addition, changes from human to computerized estimation of Ml led to slightly lower magnitude estimates after 1975;
•
these changes contributed to an apparently higher rate of seismicity in the 1930’sand 1940’s and a later decrease in seismicity rate which has been interpreted as being related to the subsequent 1952 Kern County (Mw = 7.5) earthquake;
•
variations in the rate of seismic activity have often been related to precursory activity prior to major earthquakes and therefore been considered suitable for earthquake prediction;
•
the re-determination of ML in the catalogue for southern California, however, does not confirm any changes in seismicity rate above the level of 90% significance for the time interval considered.Similar experiences with other local and global catalogues led Habermann (1995) to state: "...the heterogeneity of these catalogues makes characterizing the long-term behavior of seismic regions extremely difficult and interpreting time-dependent changes in those regions hazardous at best. ... Several proposed precursory seismicity behaviors (activation and quiescence) can be caused by simple errors in the catalogues used to identify them. ... Such mistakes have the potential to undermine the relationship between the seismologicalcommunity and the public we serve. They are, therefore, a serious threat to the well-being of our community."
variations in the rate of seismic activity have often been related to precursory activity prior to major earthquakes and therefore been considered suitable for earthquake prediction;
Originally posted by Hellas
Magnitude mb 5.0
Region CENTRAL IRAN
Date time 2012-02-27 18:48:55.0 UTC
Location 31.47 N ; 56.79 E
Depth 12 km
Distances 133 km NW Kerman (pop 577,514 ; local time 22:18:55.1 2012-02-27)
22 km NW Ravar (pop 40,167 ; local time 22:18:55.1 2012-02-27)
EMSC