Earthquake information

rms	-- s
N° phases used for the localisation	33
N° stations used for the localisation	33
Gap	79.0 °
95% confidence ellipse
semi major	--
semi minor	--
Azimuth	-- °
Location Type	manual

Download data for this event

Note: links can take up to 20 minutes from the earthquake to become available

code	Distance°	EvAz	A/M	Phase	Pick time	Residual	T	Reporting network
OUR	0.170	350	M	P	2013-05-12 13:23:19.7	0.2	T	THE
OUR	0.170	350	M	S	2013-05-12 13:23:22.4	0.1	T	THE
PAIG	0.350	228	M	P	2013-05-12 13:23:22.8	0.1	T	THE
PAIG	0.350	228	M	S	2013-05-12 13:23:27.8	-0.2	T	THE
PLG	0.490	296	M	P	2013-05-12 13:23:25.3	0	T	THE
PLG	0.490	296	M	S	2013-05-12 13:23:32.2	-0.3	T	THE
THAS	0.690	50	M	P	2013-05-12 13:23:28.4	-0.6	T	THE
THAS	0.690	50	M	S	2013-05-12 13:23:39.9	0.7	T	THE
HORT	0.830	302	M	P	2013-05-12 13:23:31.2	-0.3	T	THE
HORT	0.830	302	M	S	2013-05-12 13:23:42.8	-0.8	T	THE
SOH	0.830	322	M	P	2013-05-12 13:23:31.5	0	T	THE
SOH	0.830	322	M	S	2013-05-12 13:23:43.4	-0.3	T	THE
KAVA	0.910	24	M	P	2013-05-12 13:23:33.0	-0.1	T	THE
KAVA	0.910	24	M	S	2013-05-12 13:23:46.2	-0.2	T	THE
LIA	0.930	106	M	P	2013-05-12 13:23:33.7	0.2	T	THE
LIA	0.930	106	M	S	2013-05-12 13:23:47.2	0.1	T	THE
THE	0.930	300	M	P	2013-05-12 13:23:34.3	0.8	T	THE
SRS	1.000	341	M	P	2013-05-12 13:23:34.5	-0.1	T	THE
SRS	1.000	341	M	S	2013-05-12 13:23:49.3	0.1	T	THE
AOS	1.000	186	M	P	2013-05-12 13:23:34.5	-0.4	T	THE
AOS	1.000	186	M	S	2013-05-12 13:23:49.3	-0.2	T	THE
XOR	1.020	219	M	P	2013-05-12 13:23:35.8	0.7	T	THE
XOR	1.020	219	M	S	2013-05-12 13:23:50.1	0.1	T	THE
SKIA	1.090	203	M	P	2013-05-12 13:23:36.7	0.4	T	THE
SKIA	1.090	203	M	S	2013-05-12 13:23:51.9	-0.2	T	THE
FYTO	1.120	228	M	P	2013-05-12 13:23:37.0	0	T	THE
LIT	1.180	267	M	P	2013-05-12 13:23:37.6	-0.3	T	THE
SMTH	1.190	75	M	P	2013-05-12 13:23:37.8	-0.3	T	THE
SMTH	1.190	75	M	S	2013-05-12 13:23:54.5	-0.9	T	THE
KNT	1.310	320	M	P	2013-05-12 13:23:40.1	0.3	T	THE
KNT	1.310	320	M	S	2013-05-12 13:23:58.9	0.6	T	THE
GRG	1.460	303	M	P	2013-05-12 13:23:42.7	0.8	T	THE
ALN	1.710	64	M	P	2013-05-12 13:23:45.5	0.2	T	THE