New Mexico Tech Seismological Observatory
New Mexico Tech Seismological Observatory
Recent Earthquakes |
This list will be updated once a week with felt earthquakes being added within 24 hours. Felt earthquakes are in boldface type.
UTC Day |
UTC Time |
Lat (deg) |
Lon (deg) |
Depth (km) |
STD epicenter (km) |
Region | NEIC Report | ||
20120131 |
22:35:51.75 |
34.332 |
-106.733 |
5.00 |
-0.1 |
0.21 |
0.85 |
SNWR |
|
20120131 |
04:34:56.89 |
34.064 |
-106.717 |
5.00 |
0.0 |
0.85 |
2.70 |
Quebradas |
|
20120130 |
09:23:15.51 |
34.027 |
-107.012 |
5.00 |
0.4 |
0.59 |
0.35 |
Socorro Peak |
|
20120129 |
20:21:07.78 |
35.766 |
-107.046 |
5.00 |
1.8 |
2.10 |
10.63 |
SE of Laventana |
|
20120129 |
09:18:15.70 |
36.666 |
-104.822 |
5.00 |
1.9 |
2.39 |
11.43 |
SW of Raton |
|
20120129 |
05:20:01.93 |
34.058 |
-106.606 |
5.00 |
0.0 |
0.36 |
1.21 |
Quebradas |
|
20120128 |
16:05:58.00 |
34.326 |
-107.86 |
5.00 |
1.2 |
0.99 |
0.90 |
NE of Pie Town |
|
20120128 |
00:58:58.41 |
34.053 |
-106.576 |
5.00 |
-0.1 |
0.49 |
1.25 |
Quebradas |
|
20120128 |
00:34:14.80 |
33.917 |
-105.248 |
5.00 |
2.3 |
4.70 |
10.25 |
NE of Carrizozo |
|
20120127 |
15:53:25.04 |
34.076 |
-106.648 |
5.00 |
0.1 |
0.37 |
1.05 |
Quebradas |
|
20120126 |
16:32:09.12 |
33.937 |
-106.774 |
12.15 |
-0.2 |
0.25 |
0.91 |
Quebradas |
|
20120123 |
15:11:41.15 |
34.235 |
-107.051 |
5.00 |
0.5 |
4.33 |
1.65 |
Polvadera Peak |
|
20120123 |
09:09:17.57 |
34.001 |
-106.754 |
5.00 |
-0.1 |
1.04 |
1.67 |
Quebradas |
|
20120119 |
06:34:52.96 |
33.241 |
-105.091 |
5.00 |
2.0 |
0.82 |
4.41 |
E of Roswell |
|
20120117 |
17:53:24.78 |
34.158 |
-105.818 |
5.00 |
1.6 |
0.69 |
1.39 |
SW of Corona |
|
20120117 |
07:53:29.36 |
34.347 |
-106.721 |
9.74 |
-0.4 |
0.38 |
1.10 |
SNWR |
|
20120116 |
16:42:19.50 |
34.061 |
-106.616 |
5.00 |
-0.4 |
0.19 |
1.27 |
Quebradas |
|
20120116 |
09:15:28.49 |
33.869 |
-106.649 |
5.37 |
0.1 |
0.18 |
1.30 |
E of Carthage |
|
20120115 |
14:31:30.75 |
34.255 |
-106.883 |
5.00 |
0.1 |
0.19 |
0.39 |
San Acacia |
|
20120115 |
04:55:29.55 |
34.100 |
-106.753 |
5.00 |
0.0 |
0.20 |
0.42 |
Quebradas |
|
20120114 |
23:33:42.09 |
33.868 |
-106.665 |
5.00 |
0.3 |
0.31 |
0.91 |
E of Carthage |
|
20120114 |
23:33:26.80 |
33.873 |
-106.692 |
5.00 |
n/a |
0.26 |
0.99 |
E of Carthage |
|
20120114 |
23:32:52.11 |
33.862 |
-106.669 |
5.00 |
-0.1 |
0.36 |
0.97 |
E of Carthage |
|
20120114 |
23:32:23.68 |
33.863 |
-106.645 |
5.07 |
0.2 |
0.30 |
1.30 |
E of Carthage |
|
20120114 |
23:12:14.70 |
33.873 |
-106.651 |
6.41 |
0.4 |
0.33 |
1.29 |
E of Carthage |
|
20120112 |
18:03:55.56 |
35.099 |
-106.546 |
5.00 |
0.7 |
0.23 |
2.10 |
Albuquerque |
|
20120109 |
15:15:44.13 |
34.012 |
-106.675 |
8.81 |
-0.7 |
0.05 |
2.58 |
Quebradas |
|
20120109 |
09:25:47.85 |
34.461 |
-107.082 |
5.70 |
0.5 |
0.25 |
0.77 |
Sierra Ladrones |
|
20120109 |
08:28:31.60 |
34.005 |
-106.97 |
5.00 |
0.3 |
0.35 |
0.34 |
S of Socorro Peak |
|
20120107 |
03:31:38.05 |
34.261 |
-106.776 |
5.00 |
-0.4 |
0.05 |
0.66 |
Quebradas |
|
20120107 |
00:07:12.80 |
34.246 |
-106.918 |
3.21 |
0.0 |
0.62 |
0.39 |
SW of San Acacia |
|
20120105 |
08:55:04.86 |
34.058 |
-106.615 |
5.00 |
-0.2 |
0.17 |
1.27 |
Quebradas |
|
20120105 |
04:30:36.21 |
34.179 |
-106.575 |
5.00 |
-0.8 |
0.45 |
2.02 |
E of Quebradas |
|
20120104 |
01:30:34.30 |
34.059 |
-106.615 |
5.00 |
-0.3 |
0.23 |
1.27 |
Quebradas |
|
20120103 |
17:04:29.40 |
35.394 |
-101.958 |
5.00 |
2.4 |
0.87 |
6.58 |
NW of Amarillo, TX |
|
20120102 |
11:55:59.02 |
34.133 |
-106.516 |
5.61 |
-0.1 |
0.00 |
5.94 |
E of Quebradas |
Can't be determined.
Depth to the earthquake source in kilometers. Default, unconstrained, value is 5 km.
The coordinates of the epicenter of the earthquake in degrees latitude and degrees longitude. The epicenter is the location on the surface directly above the actual rupture point of the earthquake, which is below the surface.
The magnitude indicates the size of the earthquake. The NMTSO calculates magnitude based on the duration of the event.
National Earthquake Information Center
Earthquakes noted as having an NEIC report will have a link to the report for 30 days. After that, the event is archived in an NEIC database that is not easily linked to, so the link will be changed to the NEIC earthquake catalog search page.
Measure of the final earthquake location fit.
Measure of the solution variation.
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Last Updated: January 29, 2012 by Jana Pursley |