Characteristic Seismic Waves Associated with Cryosphere Dynamics in Eastern Dronning Maud Land, East Antarctica

Table 2

  Source parameters for 14 detected plausible glacial earthquakes in Antarctica during 1993–2008 (modified after 2010 [12]). Origin times and epicenters are determined by the surface-wave detection algorithm.

Date	Time	Latitude	Longitude	𝑀
1996/07/14	19 : 05 : 52	−62.25	−55.75	4.8^C
1998/05/11	23 : 17 : 44	−67.00	109.00	4.9^C
1999/06/27	15 : 37 : 52	−77.75	−47.25	4.8^C
2000/04/09	23 : 25 : 36	−66.25	110.75	4.9^B
2000/06/22	23 : 10 : 48	−67.00	109.00	4.9^C
2001/11/24	03 : 20 : 48	−67.00	109.00	4.9^E
2002/03/18	08 : 22 : 40	−65.25	−62.75	4.7^C
2002/03/30	04 : 15 : 28	−67.00	109.00	4.8^C
2004/01/24	08 : 38 : 24	−68.00	150.00	4.8^C
2004/01/31	04 : 31 : 52	−67.00	111.00	4.9^C
2007/10/14	02 : 10 : 08	−66.75	109.75	4.9^B
2008/05/18	08 : 35 : 04	−65.50	124.50	4.8^C
2008/06/18	00 : 04 : 00	−68.75	151.25	4.8^B
2008/07/21	07 : 34 : 48	−69.75	−67.75	4.8^C

The letter code following the magnitude M:  indicates the quality of the detection and location: B: isthe highest quality and C/E: is the lowest.