A 5.5 magnitude earthquake struck the South Sandwich Islands region, situated around 750km south east of South Georgia, in the South Atlantic early Sunday. It was the latest in a series of quakes to hit the Antarctic Region during the past 24 hours.
The moderate quake struck at 9.37am GMT at a depth of 137km and was centred 69 km (42 miles) NNW of Visokoi Island and 330 km (205 miles) NNW of Bristol Island.
The last significant earthquake to be recorded in the South Sandwich Islands region occurred on 08 December 2010 when a magnitude 6.5 quake struck 85 km (55 miles) ENE of Visokoi Island.
The unpopulated islands consist of a chain of eleven volcanic islands, connected by a low submarine ridge, bending in an arc around 400km long. They are an overseas dependency of the UK, but also claimed by Argentina. The 337km islands lie 750 km (470 miles) south east of South Georgia in the South Atlantic Ocean.
This morning’s earthquake was followed by a 4.9 magnitude quake along the Pacific-Antarctic Ridge at 12.05pm. The quake was measured at a depth of 10.3 km (6.4 miles).
Another moderate earthquake struck the Antarctic region early Saturday. The 5.1 magnitude quake which struck the Balleny Islands region 479 km (297 miles) NW of Scott Island, Antarctica, at 5.56am on Saturday. The quake was measured at a depth of 15.8 km (9.8 miles), according to the US Geological Survey (USGS).
The Pacific–Antarctic Ridge (PAR) is a divergent tectonic plate boundary located on the seafloor of the South Pacific Ocean, separating the Pacific Plate from the Antarctic Plate. It is regarded as the southern section of the East Pacific Rise in some usages, generally south of the Challenger Fracture Zone and stretching to the Macquarie Triple Junction south of New Zealand (wiki).
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