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Magnitude 7.3 - OFFSHORE EL SALVADOR
2012 August 27 04:37:20 UTC
Details
Summary
Maps
Scientific & Technical
Tsunami
Earthquake Details
This event has been reviewed by a seismologist.
Magnitude 7.3
Date-Time
Monday, August 27, 2012 at 04:37:20 UTC
Sunday, August 26, 2012 at 10:37:20 PM at epicenter
Time of Earthquake in other Time Zones
Location 12.278°N, 88.528°W
Depth 20.3 km (12.6 miles)
Region OFFSHORE EL SALVADOR
Distances 111 km (68 miles) S of Puerto El Triunfo, El Salvador
118 km (73 miles) S of Usulutan, El Salvador
123 km (76 miles) S of San Rafael Oriente, El Salvador
133 km (82 miles) S of Santiago de Maria, El Salvador
Location Uncertainty horizontal +/- 16.1 km (10.0 miles); depth +/- 4.2 km (2.6 miles)
Parameters NST=345, Nph=345, Dmin=130.2 km, Rmss=1.21 sec, Gp= 65°,
M-type=(unknown type), Version=D
Source
Magnitude: USGS NEIC (WDCS-D)
Location: USGS NEIC (WDCS-D)
Event ID usc000c7yw
Originally posted by rbkruspe
Odd enough I did not literally feel this. I might have been preoccupied and or in a place where I could not feel anything vibrate, shake etc.. !
Volcanoes? In the Imperial Valley? At the south end of the Salton Sea, southwest of Mullet Island, are five small volcanic domes. They are oriented along a northeast trend, or perpendicular to the trace of the San Andreas fault system. The domes rise 100 to 150 feet above the valley floor, and collectively are known as Obsidian Butte. They are extruded into the Quaternary alluvium and are thought to be fewer than 20,000 years old. Their composition is rhyolite and pumice, with subordinate obsidian. Obsidian is volcanic glass. It is a volcanic rock that forms when the lava is cooled very rapidly. Mineral crystals do not have time to form in the molten lava, and the noncrystalline mass becomes a glass when it is subject to sudden cooling. Obsidian is often found associated with pumice, often in layers as at Obsidian Butte. Pumice is the hardened residue of volcanic froth, or very liquid rock highly charged with gases. If the gas content is high, then the bubbles "frozen" in place upon hardening can give some buoyancy to the rock. It is commonly thought that pumice rock floats on water. Sometimes it does; usually not. Pumice boulders, because they are light and easily handled, are used extensively for landscaping. The Cerro Prieto volcano, 15 miles south of Mexicali, is a rhyolite dome that is the product of a single eruptive cycle in the late Pleistocene.
Originally posted by MamaJ
reply to post by JustMike
Good morning Mike! I'm just getting done with my first cup of coffee and it seems as if Cali is still ok, never the less still a lot of activity over there including the off shore big one.
Earthquake Report is reporting the off shore quake was coming in so conflicted, even with tsunami info because the quake happened on the oceanic plate and not the North American plate.
Do you mind explaining this in detail for me.
...the hypocenter of the earthquake was located in the oceanic plate and not in the North American plate. This event was in other words an intra-plate event and not a subduction earthquake like most of the earthquakes are in the area.
USGS has located the epicenter of all events in the subduction zone below the continental plate while snet was putting it more into the ocean.
Also, do you think it's possible this is volcanic related, I know we were throwing the idea around yesterday and TA made a thread, but it seems likely to me even more this morning. It's just soooo active and California is basically a huge volcanic state, is it not?? Advise me please. Lol
Thanks!
Jenn
has still a quiet important error margin