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Out Of Mind » SOLAR & PLANETARY ALERTS & INFO » EARTH CHANGES » QUAKE ALERTS ~12/20/2016

QUAKE ALERTS ~12/20/2016

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1 QUAKE ALERTS ~12/20/2016 on Tue Dec 20, 2016 8:31 pm

PurpleSkyz

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M 6.7 - KEPULAUAN BARAT DAYA, INDONESIA - 2016-12-21 00:17:17 UTC













MagnitudeM 6.7
RegionKEPULAUAN BARAT DAYA, INDONESIA
Date time2016-12-21 00:17:17.4 UTC
Location7.70 S ; 128.20 E
Depth220 km
Distances305 km E of Dili, Timor-Leste / pop: 150,000 / local time: 09:17:17.4 2016-12-21
2030 km SE of Bandar Seri Begawan, Brunei Darussalam / pop: 64,500 / local time: 08:17:17.4 2016-12-21
2098 km W of Port Moresby, Papua New Guinea / pop: 284,000 / local time: 10:17:17.4 2016-12-21
Source parameters not yet reviewed by a seismologist


More information at:

 Badan Meteorologi, Klimatologi, dan Geofisika Djakarta, Indonesia
 USGS/NEIC Denver, USA
 GeoForschungsZentrum (GEOFON) Potsdam, Germany

Thanks to: http://www.emsc-csem.org



  

2 Re: QUAKE ALERTS ~12/20/2016 on Tue Dec 20, 2016 8:36 pm

PurpleSkyz

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At least 3 dead, 47 injured after strong earthquake hits Ecuador



Posted by TW on December 19, 2016 



 

At least 3 people have been killed and more than 47 injured after a strong and shallow earthquake registered by Ecuador's Geophysical Institute (IGEPN) as M5.7 hit Ecuador on December 19, 2016. The quake occurred at 07:11 UTC at a shallow depth of 5.2 km (3.2 miles).  USGS registered it as M5.4 at a depth of 10 km (6.2 miles). EMSC is reporting M5.5 at the same depth.
According to the USGS, the epicenter was located 18.5 km (11.5 miles) SSW of Esmeraldas (population 165 2016), 38.4 km (23.9 miles) NE of Muisne (population 13 393), 61.6 km (38.3 miles) NNW of Rosa Zarate (population 42 121), and 96.9 km (60.2 miles) WSW of Valdez (population 11 441), Ecuador.
IGEPN recorded the quake off the coast of Atacames in Esmeraldas province, about 175 km (108.7 miles) NW of Quito, the capital. It was followed by 15 lesser-magnitude aftershocks (M3.4 - 4.5).
A tsunami alert was not issued but the institute warned that aftershocks could be expected.
This region was devastated by a massive M7.8 earthquake on April 16, 2016. That quake killed about 670 people.

President Rafael Correa said all three victims suffered heart attacks.
More than 700 families were forced to evacuate their homes.
Authorities said three hotels in the area, a popular tourist destination, were destroyed, and other buildings sustained substantial damage.

Estimated population exposure to earthquake shaking




Seismotectonics of South America (Nazca plate region)

The South American arc extends over 7,000 km, from the Chilean margin triple junction offshore of southern Chile to its intersection with the Panama fracture zone, offshore of the southern coast of Panama in Central America. It marks the plate boundary between the subducting Nazca plate and the South America plate, where the oceanic crust and lithosphere of the Nazca plate begin their descent into the mantle beneath South America. The convergence associated with this subduction process is responsible for the uplift of the Andes Mountains, and for the active volcanic chain present along much of this deformation front. Relative to a fixed South America plate, the Nazca plate moves slightly north of eastwards at a rate varying from approximately 80 mm/yr in the south to approximately 65 mm/yr in the north. Although the rate of subduction varies little along the entire arc, there are complex changes in the geologic processes along the subduction zone that dramatically influence volcanic activity, crustal deformation, earthquake generation and occurrence all along the western edge of South America.
Most of the large earthquakes in South America are constrained to shallow depths of 0 to 70 km resulting from both crustal and interplate deformation. Crustal earthquakes result from deformation and mountain building in the overriding South America plate and generate earthquakes as deep as approximately 50 km. Interplate earthquakes occur due to slip along the dipping interface between the Nazca and the South American plates. Interplate earthquakes in this region are frequent and often large, and occur between the depths of approximately 10 and 60 km. Since 1900, numerous magnitude 8 or larger earthquakes have occurred on this subduction zone interface that were followed by devastating tsunamis, including the 1960 M9.5 earthquake in southern Chile, the largest instrumentally recorded earthquake in the world. Other notable shallow tsunami-generating earthquakes include the 1906 M8.5 earthquake near Esmeraldas, Ecuador, the 1922 M8.5 earthquake near Coquimbo, Chile, the 2001 M8.4 Arequipa, Peru earthquake, the 2007 M8.0 earthquake near Pisco, Peru, and the 2010 M8.8 Maule, Chile earthquake located just north of the 1960 event.
Large intermediate-depth earthquakes (those occurring between depths of approximately 70 and 300 km) are relatively limited in size and spatial extent in South America, and occur within the Nazca plate as a result of internal deformation within the subducting plate. These earthquakes generally cluster beneath northern Chile and southwestern Bolivia, and to a lesser extent beneath northern Peru and southern Ecuador, with depths between 110 and 130 km. Most of these earthquakes occur adjacent to the bend in the coastline between Peru and Chile. The most recent large intermediate-depth earthquake in this region was the 2005 M7.8 Tarapaca, Chile earthquake.
Earthquakes can also be generated to depths greater than 600 km as a result of continued internal deformation of the subducting Nazca plate. Deep-focus earthquakes in South America are not observed from a depth range of approximately 300 to 500 km. Instead, deep earthquakes in this region occur at depths of 500 to 650 km and are concentrated into two zones: one that runs beneath the Peru-Brazil border and another that extends from central Bolivia to central Argentina. These earthquakes generally do not exhibit large magnitudes. An exception to this was the 1994 Bolivian earthquake in northwestern Bolivia. This M8.2 earthquake occurred at a depth of 631 km, which was until recently the largest deep-focus earthquake instrumentally recorded (superseded in May 2013 by a M8.3 earthquake 610 km beneath the Sea of Okhotsk, Russia), and was felt widely throughout South and North America.
Subduction of the Nazca plate is geometrically complex and impacts the geology and seismicity of the western edge of South America. The intermediate-depth regions of the subducting Nazca plate can be segmented into five sections based on their angle of subduction beneath the South America plate. Three segments are characterized by steeply dipping subduction; the other two by near-horizontal subduction. The Nazca plate beneath northern Ecuador, southern Peru to northern Chile, and southern Chile descend into the mantle at angles of 25° to 30°. In contrast, the slab beneath southern Ecuador to central Peru, and under central Chile, is subducting at a shallow angle of approximately 10° or less. In these regions of “flat-slab” subduction, the Nazca plate moves horizontally for several hundred kilometers before continuing its descent into the mantle, and is shadowed by an extended zone of crustal seismicity in the overlying South America plate. Although the South America plate exhibits a chain of active volcanism resulting from the subduction and partial melting of the Nazca oceanic lithosphere along most of the arc, these regions of inferred shallow subduction correlate with an absence of volcanic activity. (USGS) More information on regional seismicity and tectonics
Featured image credit: USGS

Thanks to: https://watchers.news



  

3 Re: QUAKE ALERTS ~12/20/2016 on Wed Dec 21, 2016 11:37 am

PurpleSkyz

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https://youtu.be/SKfob3uD7_o

Published on Dec 20, 2016
This stream is showing the past 48 hours of USGS reported earthquakes + the last 50 EMSC reported earthquakes internationally.

No voice in this video unless a large earthquake strikes.

Marker height off the globe = depth into the Earth.

The feed may show double earthquakes in some locations due to both USGS + EMSC agencies reporting the events.

When an earthquake strikes, you will hear a rumble, ding, and a bell toll. The bell will toll the number of times = to the earthquake which occurs. (example : M4.0 will ring 4 times).

The most recent earthquake has a green placemark / flag on it.

Blue flag / placemark = the last earthquake which was looked up

______

Download the full version of earthquake3D here (cost: $20 USD):

http://www.wolton.net/quakes.html

Free version here:

http://www.wolton.net/quake.html

_______

I now have a PO Box if viewers want to mail questions, donations, or mail packages / products they recommend to unbox on camera!



  

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