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What on earth

Deep earthquakes

The best estimate for the deepest known earthquake is 684 km deep, under the Fiji Islands in the Southwest Pacific, on 17 June 1977.

Yesterday, Thursday 2 February 2006, a strong earthquake, magnitude 6.6, occurred in the Fiji region at an estimated depth of 595.6 km.
http://earthquake.usgs.gov/eqcenter/recenteqsww/Quakes/usiram.php
Deep earthquakes even of this magnitude do not cause any (severe) damage.

Looking at the lower half of the map of historical seismicity http://neic.usgs.gov/neis/bulletin/neic_iram_h.html in this area it is easy to follow the inclination of the Benioff zone from shallow earthquakes, 0 – 36 km deep, to the deepest earthquakes 500 – 800 km deep. The earthquake foci normally plot along a dipping plane at an angle of 33 to 60 degrees and such a plane is called a Benioff zone. Earthquakes along Benioff zones define a lithospheric plate that descends into the mantle beneath another, overlying plate – in this case the Pacific Plate in the east sliding under the Australian Plate in the west. The zone is named after Hugo Benioff, a US seismologist who first described this feature.

Ole

Carbon flow in soilClay -> Oxygen -> Animals

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