It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
M6.4 - 116km NE of Bathsheba, Barbados
13.829°N 58.641°W depth=5.6 km (3.5 mi)
Time
2015-07-16 15:16:31 (UTC)
2015-07-16 10:16:31 (UTC-05:00) in your timezone
Times in other timezones
Nearby Cities
116km (72mi) NE of Bathsheba, Barbados
132km (82mi) NE of Bridgetown, Barbados
252km (157mi) E of Bisee, Saint Lucia
254km (158mi) ESE of Riviere-Pilote, Martinique
256km (159mi) E of Castries, Saint Lucia
"1881 12 31 INDIA: ANDAMAN I,NICOBAR I
" Estimated Rupture Parameters of the 31 December 1881 (M 7.9) Car Nicobar Earthquake. Southern segment (main rupture) 8.52 N, 92.43 E. Northern segment 10.75 N, 92.43 E. (reference #4104) December 31, 1881, morning 7:55 hr. Burmese coast. An earthquake, which is believed to have originated in the Bay of Bengal, west of the Andaman Islands, was felt over a area of 2 million square miles. Besides affecting a large portion of the Indian Peninsula and Bengal, it was also felt on the Burmese coast, including some of the islands in the Mergui Archipelago and caused much damage in the Adaman and Nicobar Islands. The surface of the ocean was greatly disturbed and waves were formed which continued to roll against the coastlines for several hours after the cessation of the earth waves, which lasted only for a few seconds.. Port Blair is the only place where any damage was done to masonry buildings, and it is to be regretted that the damage should be so little instructive, as is the case... In the Car Nicobar extensive damage was done to the coconut groves and huts of the natives and vents similar to those described in connection with the Cachar earthquake of 1869 were opened in the sandy soil. (reference #1185)
The 31 December 1881 Mw = 7.9 Car Nicobar earthquake. This earthquake caused minor damage in the Andaman Island Penal colony and generated a tsunami that was observed throughout the Bay of Bengal but not along the Burmese coast. The tsunami did no damage around the Bay of Bengal where tide gauges recorded a maximum amplitude of 0.8 m (Oldham, 1884). An analysis of five tide gauge records reveals that the earthquake was Mw = 7.9 +0.2 and occurred on an east-dipping thrust fault below and to the west of Car Nicobar, an island at 9 deg N midway between the Andaman and Nicobar islands (Ortiz and Bilham, 2003). GPS measurements at Port Blair indicate oblique convergence of the plate boundary (Paul et al., 2001). The earthquake is believed to have occurred on the interface between the Indian and Andaman Plates and the inferred mechanism of westward slip of the hanging wall slip is consistent with slip partitioning between the dipping subduction zone, and the strike-slip west Andaman fault east of Car Nicobar. A feature of this earthquake is the inferred presence of a region of minor slip NE of the main rupture zone. This may have been a secondary secondary earthquake triggered by the mainshock. Its timing would have to have occurred within a few minutes of the mainshock for it to have produced the sea wave observed at Port Blair. Local populations were concentrated in only two islands and therefore there is no corroboration of this inferred northern region of submarine faulting which occurred between them. It is probable that offshore corals may be of use in reconstructing an extended history of earthquakes in the Andaman-Nicobar Islands. The island of Car Nicobar is believed to have been raised and tilted during the 1881 event. Deformation models that do not include this uplift result in an inappropriate estimate of the observed tsunami runup on the island (Ortiz and Bilham, 2003). (above from reference #4084)
Epicentre in Bay of Bengal; waves recorded in Ceylon and Gangetic Delta in Bengal. (reference #3927) December 31, 1881. Epicenter in western central part of the Bay of Bengal. Tsunami waves from Sri Lanka to Ganges delta. Tsunami on Andaman and Nicolar Islands. Tsunami amplitudes: Port Blair 0.92 m, False Point 0.05 m, Nagapatam 1.22 m, Camicobar 0.7 m. (reference #96)
December 31, 1881. Bay of Bengal. Epicenter supposedly near the center of the Bay. Waves were reported from Ceylon northward along the east shore of the bay to the Ganges Delta and along the Andaman and Nicobar islands as far south as Sumatra. Four waves were noted at some locals. No waves were recorded at the tide stations on the Burma coast. (reference #42) The surface of the ocean was greatly disturbed and waves were formed which continued to roll against the coastlines for several hours after the cessation of the earth waves, which lasted only for a few seconds. The first tidal wave (tsunami) was recorded at Port Blair at 8:10 a.m. followed by others in succession at about 15 min interval, with a height of about 3 ft from crest to hollow. They continued til 9 p.m. The velocity of the waves varied from 2 to 6.9 miles per minute. ... The sea-wave broke on this island [Car Nicobar] and it is recorded that the water penetrated into the houses of the Burmese residents which stood on platforms of less than 2.5 ft high, while those on higher platforms escaped. (reference #1185)
Magnitude mb 5.7
Region FIJI REGION
Date time 2015-07-17 18:49:53.9 UTC
Location 18.12 S ; 178.16 W
Depth 544 km
Distances 360 km E of Suva, Fiji / pop: 77,366 / local time: 06:49:53.9 2015-07-18
322 km SE of Lambasa, Fiji / pop: 24,187 / local time: 06:49:53.9 2015-07-18