Very shallow M6.6 earthquake hits Ogasawara region, Japan
A very shallow earthquake registered by the JMA as M6.6 hit Japanese Ogasawara Archipelago at 18:22 UTC (03:22 JST) on August 16, 2018. The USGS is reporting M6.4 at a depth of 11.5 km (7.1 miles) at 18:21 and M6.0 at 18:22 UTC. EMSC is reporting M6.4 and M5.9 at a depth of 10 km (6.2 miles). According to the USGS, the epicenter was located 251 km (156 miles) SE of Iwo Jima, 420.9 km (261.5 miles) SSW of Ogasawara, Japan and 945.4 km (587.5 miles) NNW of Saipan, Northen Mariana Islands. There are no people living within 100 km (62 miles). Although there may be slight sea-level changes in coastal regions, this earthquake has caused no damage to Japan, JMA said. The closest volcanoes are Minami-Hiyoshi and Nikko, both submarine. They have located roughly 100 km (62 miles) W of the epicenter. Periodic water discoloration and water-spouting have been reported over Minami-Hiyoshi since 1975 when detonations and an explosion were als…

Earthquake swarm detected near Herðubreið, Askja volcanic area, Iceland

Earthquake swarm detected near Herðubreið, Askja volcanic area, Iceland

A notable amount of earthquakes occurred near Herðubreið, Iceland's Askja volcanic area on Tuesday, November 28, 2017, with magnitudes ranging from 0.4 to 2.0 and depths between 2.5 and 12.8 km (1.5 - 8 miles).
In total, the Icelandic Met Office (IMO) registered 45 earthquakes in the area over the past 48 hours. The first, M0.8 at a depth of 8.2 km (5 miles), was registered at 14:45 UTC on November 26 and was followed by M0.4 (at 7.7 km / 4.8 miles), M0.9 (at 6.2 km / 4.8 miles) and M0.8 at (at 7.8 km / 4.8 miles) on November 27.
Quakes intensified after 05:00 UTC on November 28, with 40 quakes by 11:48 UTC (M0.4 - 2.0; depths 2.5 - 12.8 km / 1.5 - 8 miles).
IMO geologists say this is not unusual and does not point to any volcanic unrest.

Geological summary

Askja is a large basaltic central volcano that forms the Dyngjufjöll massif. It is truncated by three overlapping calderas, the largest of which is 8 km (5 miles) wide and may have been produced primarily from subglacial ring-fracture eruptions rather than by subsidence. A major rhyolitic explosive eruption from Dyngjufjöll about 10 000 years ago was in part associated with the formation of Askja caldera.
Many postglacial eruptions also occurred along the ring-fracture. A major explosive eruption on the SE caldera margin in 1875 was one of Iceland's largest during historical time. It resulted in the formation of a smaller 4.5-km-wide (2.8 miles) caldera, now filled by Öskjuvatn lake, that truncates the rim of the larger central caldera. The 100-km-long (62 miles) Askja fissure swarm, which includes the Sveinagja graben, is also related to the Askja volcanic system, as are several small shield volcanoes such as Kollatadyngja. Twentieth-century eruptions have produced lava flows from vents located mostly near Öskjuvatn lake.

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