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Magnitude M 4.1
Region SONORA, MEXICO
Date time 2016-12-01 02:26:22.0 UTC
Location 30.86 N ; 109.32 W
Depth 5 km
Distances 287 km W of Ciudad Juárez, Mexico / pop: 1,513,000 / local time: 19:26:22.0 2016-11-30
255 km NE of Hermosillo, Mexico / pop: 596,000 / local time: 19:26:22.0 2016-11-30
87 km SE of Bisbee, United States / pop: 5,600 / local time: 19:26:22.0 2016-11-30
30 km NE of Esqueda, Mexico / pop: 6,200 / local time: 19:26:22.0 2016-11-30
Magnitude M 4.2
Region OAXACA, MEXICO
Date time 2016-11-30 08:18:18.0 UTC
Location 17.05 N ; 95.47 W
Depth 94 km
Distances 364 km SE of Puebla de Zaragoza, Mexico / pop: 1,591,000 / local time: 02:18:18.0 2016-11-30
133 km E of Oaxaca de Juárez, Mexico / pop: 263,000 / local time: 02:18:18.0 2016-11-30
38 km E of San Miguel Quetzaltepec, Mexico / pop: 3,700 / local time: 02:18:18.0 2016-11-30
Why are there “missing” earthquakes?
There is an earthquake on another website; why is it not here?
We may not rapidly locate earthquakes smaller than 5.0 outside the US unless they have caused significant damage or are widely felt. Earthquakes this small rarely cause significant damage. At times, some other agency may report an earthquake with a larger magnitude than what we compute from our data, especially for non-US events near magnitude 5.0. If our magnitude for the event is less than magnitude 5.0, we may not issue a rapid report for it.
Earthquakes occurring outside the US and smaller than about magnitude 4.5 can be difficult for the USGS to locate if there are not enough data. The USGS continues to receive data from observatories throughout the world for several months after the events occur. Using those data, we add new events and revise existing events in later publications. For a description of these later publications and the data available, see Data.
The 2010–2014.3 global earthquake rate increase
Tom Parsons 1 and Eric L. Geist 1
1 U. S. Geological Survey, Menlo Park, California, USA
...
1. Introduction
Obvious increases in the global rate of large (M ≥ 7.0) earthquakes happened after 1992, 2010, and especially during the first quarter of 2014 (Table 1 and Figure 1). Given these high rates, along with suggestions that damaging earthquakes may be causatively linked at global distance [e.g., Gomberg and Bodin, 1994; Pollitz et al., 1998; Tzanis and Makropoulos, 2002; Bufe and Perkins, 2005; Gonzalez-Huizar et al., 2012; Pollitz et al., 2012, 2014], we investigate whether there is a significant departure from a random process underlying these rate changes. Recent studies have demonstrated that M ≥ 7.0 earthquakes (and also tsunamis) that occurred since 1900 follow a Poisson process [e.g., Michael, 2011; Geist and Parsons, 2011; Daub et al., 2012; Shearer and Stark, 2012; Parsons and Geist, 2012; Ben-Naim et al., 2013]. Here we focus on the period since 2010, which has M ≥ 7.0 rates increased by 65% and M ≥ 5.0 rates up 32% compared with the 1979 – present average. The first quarter of 2014 experienced more than double the average M ≥ 7.0 rate, enough to intrigue the news media [e.g., www.nbcnews.com...]. We extend our analysis to M ≥ 5.0 levels, as many of these lower magnitude events convey significant hazard, and global catalogs have not generally been tested down to these thresholds.
2. Methods and Data
We work with the Advanced National Seismic System (ANSS) catalog of M≥ 5.0 global earthquakes for the period between 1979 and 2014.3 with a primary focus on the recent interval between 2010 and 2014.3 that shows the highest earthquake rates (Table 1 and Figure 1). A variety of tests suggest that the catalog is complete down to magnitudes between M=4.6 and M=5.2, depending on the method used to assess it (see supporting information). We examine a range of lower magnitude thresholds above M =5.0 to account for this uncertainty.
...
originally posted by: jadedANDcynical
...
Don't forget the "US" part of "USGS."
...
originally posted by: GoShredAK
Does it show a 4.3 in Alaska from yesterday?
Magnitude ML 3.4
Region SOUTHERN ALASKA
Date time 2016-12-01 23:55:55.0 UTC
Location 61.87 N ; 150.28 W
Depth 7 km
Distances 2188 km NW of Vancouver, Canada / pop: 1,838,000 / local time: 15:55:55.0 2016-12-01
824 km W of Whitehorse, Canada / pop: 23,300 / local time: 15:55:55.0 2016-12-01
69 km NW of Palmer, United States / pop: 6,000 / local time: 14:55:55.0 2016-12-01
19 km NW of Willow, United States / pop: 2,200 / local time: 14:55:55.0 2016-12-01
Magnitude MD 2.4
Region NORTHERN CALIFORNIA
Date time 2016-12-01 23:48:17.2 UTC
Location 38.79 N ; 122.79 W
Depth 21 km
Distances 665 km NW of Los Angeles, United States / pop: 3,793,000 / local time: 15:48:17.2 2016-12-01
115 km W of Sacramento, United States / pop: 467,000 / local time: 15:48:17.2 2016-12-01
30 km S of Lakeport, United States / pop: 4,800 / local time: 15:48:17.2 2016-12-01
7 km SW of Cobb, United States / pop: 1,800 / local time: 15:48:17.2 2016-12-01
Magnitude MD 2.0
Region SAN FRANCISCO BAY AREA, CALIF.
Date time 2016-12-01 19:02:34.8 UTC
Location 37.32 N ; 122.11 W
Depth 0 km
Distances 504 km NW of Los Angeles, United States / pop: 3,793,000 / local time: 11:02:34.8 2016-12-01
150 km S of Sacramento, United States / pop: 467,000 / local time: 11:02:34.8 2016-12-01
19 km W of San Jose, United States / pop: 946,000 / local time: 11:02:34.8 2016-12-01
4 km S of Loyola, United States / pop: 3,300 / local time: 11:02:34.8 2016-12-01
Magnitude ML 2.2
Region GREATER LOS ANGELES AREA, CALIF.
Date time 2016-12-01 16:51:47.9 UTC
Location 34.19 N ; 118.84 W
Depth 28 km
Distances 57 km W of Los Angeles, United States / pop: 3,793,000 / local time: 08:51:47.9 2016-12-01
43 km E of Ventura, United States / pop: 96,800 / local time: 08:51:47.9 2016-12-01
2 km N of Thousand Oaks, United States / pop: 127,000 / local time: 08:51:47.9 2016-12-01
Moderate earthquake - Anchor Point, Alaska on November 30, 2016
Magnitude : 4.5 Local Time (conversion only below land) : 2016-11-30 09:57:07 GMT/UTC Time : 2016-11-30 18:57:07 Depth (Hypocenter) : 98.2 km
earthquake-report.com...
Magnitude ML 4.4
Region SOUTHERN ALASKA
Date time 2016-11-30 18:57:07.5 UTC
Location 60.01 N ; 152.68 W
Depth 99 km
Distances 2225 km NW of Vancouver, Canada / pop: 1,838,000 / local time: 10:57:07.5 2016-11-30
973 km W of Whitehorse, Canada / pop: 23,300 / local time: 10:57:07.5 2016-11-30
203 km SW of Anchorage, United States / pop: 292,000 / local time: 09:57:07.5 2016-11-30
54 km NW of Anchor Point, United States / pop: 2,000 / local time: 09:57:07.5 2016-11-30
The 2010–2014.3 global earthquake rate increase
Tom Parsons 1 and Eric L. Geist 1
1 U. S. Geological Survey, Menlo Park, California, USA
...
1. Introduction
Obvious increases in the global rate of large (M ≥ 7.0) earthquakes happened after 1992, 2010, and especially during the first quarter of 2014 (Table 1 and Figure 1). Given these high rates, along with suggestions that damaging earthquakes may be causatively linked at global distance [e.g., Gomberg and Bodin, 1994; Pollitz et al., 1998; Tzanis and Makropoulos, 2002; Bufe and Perkins, 2005; Gonzalez-Huizar et al., 2012; Pollitz et al., 2012, 2014], we investigate whether there is a significant departure from a random process underlying these rate changes. Recent studies have demonstrated that M ≥ 7.0 earthquakes (and also tsunamis) that occurred since 1900 follow a Poisson process [e.g., Michael, 2011; Geist and Parsons, 2011; Daub et al., 2012; Shearer and Stark, 2012; Parsons and Geist, 2012; Ben-Naim et al., 2013]. Here we focus on the period since 2010, which has M ≥ 7.0 rates increased by 65% and M ≥ 5.0 rates up 32% compared with the 1979 – present average. The first quarter of 2014 experienced more than double the average M ≥ 7.0 rate, enough to intrigue the news media [e.g., www.nbcnews.com...]. We extend our analysis to M ≥ 5.0 levels, as many of these lower magnitude events convey significant hazard, and global catalogs have not generally been tested down to these thresholds.
2. Methods and Data
We work with the Advanced National Seismic System (ANSS) catalog of M≥ 5.0 global earthquakes for the period between 1979 and 2014.3 with a primary focus on the recent interval between 2010 and 2014.3 that shows the highest earthquake rates (Table 1 and Figure 1). A variety of tests suggest that the catalog is complete down to magnitudes between M=4.6 and M=5.2, depending on the method used to assess it (see supporting information). We examine a range of lower magnitude thresholds above M =5.0 to account for this uncertainty.
...