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Tuesday October 24 2017, 10:47:47 UTC 41 minutes ago 141km NNE of Palue, Indonesia 6.7 549.2 (km) USGS Feed
Tuesday October 24 2017, 10:47:47 UTC 41 minutes ago Banda Sea. 6.7 562.0 (km) GeoScience Australia
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3 May 2016
Scientists find likely cause for recent southeast U.S. earthquakes
Posted by llipuma
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Compared to earthquakes near plate boundaries, earthquakes in the middle of plates are not well understood and the hazards they pose are difficult to quantify. The new findings could help scientists better understand the dangers these earthquakes present, according to the study’s authors.
Old plates and earthquakes
Tectonic plates are composed of Earth’s crust and the uppermost portion of the mantle. Below that is the asthenosphere: the warm, viscous conveyor belt of rock on which tectonic plates ride.
Earthquakes typically occur at the boundaries of tectonic plates, where one plate dips below another, thrusts another upward, or where plate edges scrape alongside each other. Earthquakes rarely occur in the middle of plates, but they can happen when ancient faults or rifts far below the surface reactivate. These areas are relatively weak compared to the surrounding plate, and can easily slip and cause an earthquake.
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Magnitude Mw 6.5
Region BANDA SEA
Date time 2017-10-24 10:47:47.6 UTC
Location 7.25 S ; 123.06 E
Depth 550 km
Distances 313 km NW of Dili, Timor-Leste / pop: 150,000 / local time: 19:47:47.6 2017-10-24
178 km NE of Maumere, Indonesia / pop: 47,600 / local time: 18:47:47.6 2017-10-24
Global view
Source parameters reviewed by a seismologist
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Compared to earthquakes near plate boundaries, earthquakes in the middle of plates are not well understood and the hazards they pose are difficult to quantify. The new findings could help scientists better understand the dangers these earthquakes present, according to the study’s authors.
Old plates and earthquakes
Tectonic plates are composed of Earth’s crust and the uppermost portion of the mantle. Below that is the asthenosphere: the warm, viscous conveyor belt of rock on which tectonic plates ride.
Earthquakes typically occur at the boundaries of tectonic plates, where one plate dips below another, thrusts another upward, or where plate edges scrape alongside each other. Earthquakes rarely occur in the middle of plates, but they can happen when ancient faults or rifts far below the surface reactivate. These areas are relatively weak compared to the surrounding plate, and can easily slip and cause an earthquake
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