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An M4.3 earthquake struck the Mount St. Helens region this morning, 14 February 2011, at 10:35 a.m. PST (18:35 UTC) and was felt widely through southwestern Washington and Northwestern Oregon (earthquake.usgs.gov...). Its exact magnitude may change by a few tenths from this value as records are further analyzed. The earthquake was followed by several aftershocks up to M2.8 over the next few hours (www.pnsn.org...), the three largest of which were also reported felt. All of the earthquakes are located in an area about 8 kilometers (5 miles) north of the crater of Mount St. Helens, near the Johnston Ridge Observatory, at a depth of about 4 to 6 kilometers (2.5 to 4 miles).
Today's earthquakes are in the same place as a small swarm that took place about two weeks earlier, on 29 January. These earthquakes are reminiscent of a swarm that took place about 30 years ago, when a swarm of small earthquakes began in August 1980, a few miles northwest of today's activity. The 1980-1981 sequence climaxed with an M5.5 earthquake on 14 February 1981. Analysis of the 1981 events suggested that they occurred along existing faults in the Mount St. Helens seismic zone, a northwest to southeast trending system of faults in which Mount St. Helens lies. The Mount St. Helens seismic zone exhibits strike-slip motion, with the southwestern rocks slipping horizontally northwest relative to the rocks northeast of the fault zone. The fault zone likely exerts control on the location of Mount St. Helens volcano. Studies following the 1980 eruption suggested that the magma removed during the May 1980 eruption and subsequent lava-dome building caused faults along the seismic zone to slip in response to the magma withdrawal. Similar interaction of volcanic activity and tectonic fault movement is possible in the case of today's earthquakes, but at present there appears to be no signs of unrest in the volcanic system.
The USGS and the Pacific Northwest Seismic Network at University of Washington continue to watch conditions at Mount St. Helens closely.
Originally posted by leaualorin
reply to post by westcoast
well , thank GOD I live in ROMANIA ...
Here we have BIG problems with our evil satanic VERY GREEDY politicians...
But the US guys...
I don't know...
I mean , west coast , CALIFORNIA has daily almost earthquakes and now EAST COAST , washington...
Bad...
Stay close to your car keys and check this site often :
earthquake.usgs.gov...
The second largest earthquake since Mount St. Helen's erupted -- a magnitude 4.3 shaker -- rocked a fault line six miles north of the volcano Monday morning. People felt it as far away as Astoria, Lake Oswego, Hood River and even Bremerton, Wash., near Seattle. The last one, as it happens, was 30 years ago also on Valentine's Day, a magnitude 5.5 temblor. That 1981 earthquake appeared to be the result of the earth's crust readjusting after magma oozed up through the fault and blew the mountain's top on May 18, 1980.
Monday's quake was of the "strike-slip variety," said seismologist Seth Moran of the Cascades Volcano Observatory in Vancouver. The large tectonic Juan de Fuca plate is diving beneath the North American plate. At places, the plates get stuck together. An earthquake occurs when the plates slip past each other, releasing energy, he said. More than 900 people reported feeling the 10:35 a.m. earthquake, posting their responses on the U.S. Geologic Survey's "Did you feel it?" page on its website. No damage was reported. "I felt it, and certainly a lot of people here felt it," Moran said. "It was broadly felt, and, for a 4.3, that's appropriate, it was a decent-sized earthquake." Mount St. Helens has rumbled and belched and quaked nearly every day since the May 1980 eruption, averaging one to two earthquakes a day, Moran said. In late January, a swarm of earthquakes was detected in the same general area as Monday's quake, known as the Mount St. Helen's Seismic Zone.
The zone runs from Mount St. Helen's 30 miles north to Morton, Wash. The largest quake in that January swarm was a modest magnitude 2.6, he said. Monday's quake, like those previous ones, occurred at a relatively shallow depth of about 3.1 miles. The quake doesn't presage another eruption, or another round of dome-building inside the crater like the action that followed a smaller magma eruption in fall 2004, Moran said. This one was simply a result of tectonic plates clashing beneath the earth's surface along the fault. Still, he said: "Anytime a 4.3 earthquake happens in this area, you pay attention because they're not that common. Realistically, we don't know exactly what's going to happen, but there's a reasonable guess that this was the largest event that we're going to see, and that's based on the fact that we've only had one event that's larger in the past 30 years."
Originally posted by Caji316
I can't say they are to blame because I don't have any hard facts..It's just my gut feeling though that they are behind it all.
Analysis of the 1981 events suggested that they occurred along existing faults in the Mount St. Helens seismic zone, a northwest to southeast trending system of faults in which Mount St. Helens lies. The Mount St. Helens seismic zone exhibits strike-slip motion, with the southwestern rocks slipping horizontally northwest relative to the rocks northeast of the fault zone. The fault zone likely exerts control on the location of Mount St. Helens volcano. Studies following the 1980 eruption suggested that the magma removed during the May 1980 eruption and subsequent lava-dome building caused faults along the seismic zone to slip in response to the magma withdrawal. Similar interaction of volcanic activity and tectonic fault movement is possible in the case of today's earthquakes, but at present there appears to be no signs of unrest in the volcanic system.
Monday's quake was of the "strike-slip variety," said seismologist Seth Moran of the Cascades Volcano Observatory in Vancouver. The large tectonic Juan de Fuca plate is diving beneath the North American plate. At places, the plates get stuck together. An earthquake occurs when the plates slip past each other, releasing energy, he said.
This one was simply a result of tectonic plates clashing beneath the earth's surface along the fault. Still, he said: "Anytime a 4.3 earthquake happens in this area, you pay attention because they're not that common. Realistically, we don't know exactly what's going to happen, but there's a reasonable guess that this was the largest event that we're going to see, and that's based on the fact that we've only had one event that's larger in the past 30 years."