Southern Iran Earthquake

Dangerous earthquake in Southern Iran

Last update: November 10, 2014 at 2:59 pm by By

 

Update 14:24 UTC : We expect the city of Qotbabad to be in the damage zone (radius 20 km from the epicenter)

Update 14:20 UTC : the population density in this desert area is very low and thus only 2700 people can be affected by this dangerous earthquake (radius 20 km). In this area we think that slight damage will be likely

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Iran seismological Agency
25 Km of Fin, Hormozgan
30 Km of Fareghan, Hormozgan
40 Km of Patkuiyeh, Hormozgan

USGS
92km (57mi) NNW of Bandar ‘Abbas, Iran
115km (71mi) NNW of Qeshm, Iran
149km (93mi) E of Lar, Iran
150km (93mi) NW of Minab, Iran
410km (255mi) NNE of Abu Dhabi, United Arab

Most important Earthquake Data:

Magnitude : 5.2

Local Time (conversion only below land) : 2014-11-10 17:22:40

GMT/UTC Time : 2014-11-10 13:52:40

from:    http://earthquake-report.com/2014/11/10/moderate-earthquake-southern-iran-on-november-10-2014/

Ecuador/Colombia Border Earthquake

 

Dangerous earthquake in Northern Ecuador (border with Colombia)

Last update: October 21, 2014 at 8:56 am by By

 

Update : Although we mentioned earlier that this earthquake was not linked to volcanic activity, the Carchi authorities have now confirmed that the earthquake was volcanically triggered.

Image copyright and courtesy El Comercio Ecuador

Important update : INGEOMINAS has raised the alert level of the Chiles – Cerro Negrp volcanoes from yellow to orange at these long-dormant, twin volcanoes as seismicity has surged (over 1500 events!) over the past 24 hours (including a magnitude M5.6 earthquake).

Update : One house was apparently damaged in the capital of Carchi province, Tulcan. No more reports about the fear for a missing person in the landslide. Let’s hope that this was a false alert.

Update : Picture below shows a landslide due to this earthquake (image courtesy Army Ecuador). The governor of the Crachi province in Ecuador may decide to suspend the classes in some schools.

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Update : No reports of damage so far, only an Ecuadorian official report of 1 person missing after a landslide in Cerro Negro.

Update : IGEPN (Ecuador) mentions a Magnitude (Richter) of M5.9 at a depth of 6 km only. Although no direct volcanic link was reported, the epicenter was located in the direct vicinity of the border Colombian volcanoes Cumbal and Chiles.

Screen Shot 2014-10-21 at 06.54.08

Screen Shot 2014-10-21 at 06.54.41 Screen Shot 2014-10-21 at 06.55.03

3km (2mi) WSW of San Gabriel, Ecuador
34km (21mi) SW of Ipiales, Colombia
39km (24mi) NE of Ibarra, Ecuador
49km (30mi) NE of Atuntaqui, Ecuador
117km (73mi) NE of Quito, Ecuador

Most important Earthquake Data:

Magnitude : 5.7

Local Time (conversion only below land) : 2014-10-20 14:33:24

GMT/UTC Time : 2014-10-20 19:33:24

from:    http://earthquake-report.com/2014/10/20/strong-earthquake-colombia-ecuador-border-region-on-october-20-2014/

Sevier COunty, TN Composting Trash

Where Does All the Trash from Dollywood Go? To One of the World’s Best Composting Facilities

Sevier County, Tenn., diverts 70 percent of waste from landfills—and it’s becoming more efficient all the time.

 

All photos by Erin L. McCoy.

 

 

When you think about progressive composting and recycling programs, big cities such as Seattle, San Francisco, and Los Angeles might come to mind—yet one of the most efficient composting facilities in the world is in Appalachian Tennessee.

Because of this plant, the majority of the county’s waste is composted or recycled.

Sevier County, Tennessee, is home to the twin tourist destinations of Gatlinburg and Pigeon Forge, and attracts more than 11 million visitors per year. Gatlinburg is a quaint mountain town packed with quirky stores, restaurants, moonshine shops, and an aquarium. Pigeon Forge is home to the Dollywood amusement park. These towns are poised at the edge of the Great Smoky Mountains National Park, which covers roughly a third of the county.

Perhaps it’s this proximity to the natural world that helped inspire Sevier County’s unique approach to waste disposal. When it opened in 1991, the Sevier Solid Waste Composting Facility was one of the first in the world to use rotating drums, or “digesters,” for breaking down compost. Because of this plant, the majority of the county’s waste is composted or recycled. Today, it’s still a rare breed.

“There’s about 12 or so [composting facilities] in the world like this,” explains Tom Leonard, general manager of Sevier Solid Waste. “Every one of them has gotten some design feature from here, because we’re one of the oldest.”

As we walk around the facility, Leonard points to a grassy rise in the distance. “That back there is our old Class 1 landfill, but we don’t use it anymore.”

Measures of success

About 100,000 tons of solid waste and treated sewage pass through this facility every year—and an astounding 70 percent is diverted from landfills by being composted or recycled. That’s compared to 34.5 percent of all U.S. waste that was diverted in 2012, according to data from the U.S. Environmental Protection Agency. San Francisco, declared the greenest city in America by the Siemens Green City Index, recycled 77 percent of its waste in 2010, but was the only North American city of the 27 listed in the index to recycle more than Sevier County.

The county’s waste diversion rate becomes even more impressive when Leonard explains that 99 percent of the county’s waste is diverted from its Class 1 landfill—the most environmentally harmful type, requiring heavy lining to prevent runoff, careful regulatory oversight, and decades of maintenance. Garbage in these landfills is eventually covered up, but it never really goes away, Leonard says.

“I just don’t like the word ‘forever,’ because that’s a long time. So what we’re doing is, we’re stabilizing the material back down to its form, and our ultimate goal is not to put anything from this plant into a landfill.”

“Our ultimate goal is not to put anything from this plant into a landfill.”

Another unique component to Sevier County’s approach: residents and businesses aren’t required to separate recyclables from their daily waste. There are no recycling bins for home pickup, and the only items people are required to separate are construction and demolition materials, electronics, and tires. The separation of recyclables happens on the back end, as a part of the composting process. (While cardboard can be composted, citizens are asked to separate it because it makes more money for the county as recycled cardboard than as compost.)

In the end, this facility is financially self-sustaining, thanks in part to the money saved by not sending waste to a Class 1 landfill, where most non-recyclable waste in the U.S. ends up. A great deal of money is also saved on transporting garbage to landfills, which are often far away from pickup locations because of the challenges of finding affordable, usable land.

The facility also ensures that waste management is relatively affordable for the county and its cities; the cost of handling waste is $40 per ton, lower than the national average. In Sevier County, these costs are covered in part through a $12-per-month fee for curbside pickup. The Waste Business Journal reported that the average cost to place a ton of municipal solid waste into a landfill in 2012 was $44.23.

Meanwhile, individuals get free compost, with the rest being used for city and county projects such as road maintenance.

The recipe for compost

The tourist industry posed a unique dilemma when Sevier County administrators began seeking new waste disposal options in the late 1980s: “Because so much of our waste stream comes from our millions of visitors that come to the county every year, it’s almost impossible to get them to recycle in the way that we’d need them to,” explains Larry Waters, who has been Sevier County mayor since 1978. The county is home to nearly 94,000 people, a population dwarfed by the huge volume of tourists.

County administrators visited other sites where composting strategies had been implemented and ultimately contracted with Bedminster Bio-Conversion to build the original facility and operate it for the first few years.

Waters says that the county was the first to install a facility of this type. “We were pretty nervous about that—whether or not it was going to meet our needs and do what we needed it to do.”

However, the Sevier County facility would soon become a model for other, similar composting plants throughout the world. What’s more, the tourist industry proved to be a key advantage, since the high volumes of restaurant food waste are great for compost.

“For us, [composting and recycling] is not only the right thing to do, it financially makes sense for us to do it, so it’s exciting.”

Today, the Sevier Solid Waste Composting Facility receives visitors from around the globe, seeking to gain insights from what Sevier County has learned through trial and error. More efficient processes and technologies have been developed over the lifetime of the facility, and even today operators are always on the lookout for better approaches, Leonard says.

Constant improvement is on Leonard’s mind as he guides me through the facility. We walk inside a huge structure covered with corrosion-resistant plastic, where broken-down materials are pulled from the ends of 185-foot-long cylindrical digesters that rotate slowly.

After three days, materials are pulled out of the digesters and placed onto a conveyor belt, which carries them into the next room. There, they’ll be sifted for glass and recyclables, then laid out into windrows for roughly 37 days. Windrows are narrow, long piles of material that are turned regularly to improve aeration and aid the breakdown into compost.

For all the streamlining this process has undergone, Leonard is today preoccupied with resolving two problems: First, he needs to reduce the moisture in these massive rooms of windrowed compost—not so much that the microorganisms breaking down the compost die, but enough to make it easier to separate glass from the moist compost. It’ll mean more glass recycling in the long run, and will increase the amount and quality of compost the facility can produce.

The second problem is how to make more efficient use of the plastics the facility collects. Many of them can be recycled, but there may be a more financially and environmentally efficient way to put them to use. Leonard believes this problem may soon be resolved with the type of innovative approach that has become the norm here. He hopes to sign a contract with the technology company PHG Energy soon, in the hopes of starting to convert used plastics into fuel within a year.

“We can produce about 6 megawatts of power from just our plastics,” Leonard says, enough to power about 2,400 homes per year.

“For us, [composting and recycling] is not only the right thing to do, it financially makes sense for us to do it, so it’s exciting,” Leonard says.

 

About 300 tons of garbage a day pass through the 188,000-square-foot Sevier Solid Waste Composting Facility in Pigeon Forge, Tenn., and this tipping floor is where that garbage is first collected. The floor is enclosed by a woven, corrosion-resistant plastic. Garbage is funneled through five pits in the tipping floor and into up to five “digesters,” which are long, cylindrical drums that rotate 24 hours a day.

“Paper, food waste, cardboard—anything that’s organic can be broken down in our system,” explains Tom Leonard, general manager of the facility. Biosolids from the local wastewater treatment plant are also mixed in, and help contribute to the microorganisms that will eventually break down waste into compost.

 

Leonard explains how the composting process gets started. The tipping floor is where municipal waste and biosolids from the wastewater treatment plant are first collected before they’re funneled into rotating “digester” drums, which start the composting process.

 

Leading from the tipping floor to another enclosed structure, digesters rotate 24 hours a day. It takes three days for garbage to travel 185 feet along these drums. The three larger digesters are 14 feet in diameter, and two more measure 12 feet in diameter; all are slightly tilted toward the building where compost will eventually be removed.

“Basically, it’s breaking up all those bags and allowing all that stuff to mix together, so now you can get all your organics, all your food waste and paper waste, all mixing together, and then the bugs can start working on that,” Leonard explains. Microorganisms are naturally occurring in the garbage and sewage that enter the digesters. The process is aerobic, so air is blown into the digesters to keep the microorganisms alive and well.

The process of breaking down the waste creates a lot of energy, increasing temperatures in the middle of the digesters to between 160 or 170 degrees.

 

“They turn 24 hours a day, seven days a week, so about one revolution a minute,” explains Leonard, showcasing the digesters that kick-start the composting process. The functionality of these digesters has been improved over the years through trial and error, and now they serve as models for composting plants around the world.

 

Leonard points out the ends of the digesters, where garbage is removed after three days of constant rotation. By this time, much of the garbage resembles compost, but large pieces of plastic, metal, and other items that can’t be broken down into compost remain. The material that comes out of the digesters is transported by conveyer belt into the next room, where it’s sifted to remove larger items.

Construction materials such as wire, carpet, hoses, and large pieces of plastic aren’t allowed in everyday trash, since they can clog up the digester.

After the garbage is sifted, “there’s no organics left,” Leonard says. “It’s inert material, so it goes into a Class 3 landfill, which takes construction, demolition, vinyl siding, plastic, glass windows.” Leachate—runoff that has passed through waste and often carries elements and chemicals from that waste as a result—is minimal in Class 3 and Class 4 landfills, meaning these landfills are less harmful to the environment.

 

Most organic materials have started to break down into compost after three days in the digesters, but recyclables such as the metal can that Leonard is pictured with here still need to be sifted out. The conveyer belt to Leonard’s right transports the materials to a primary trommel screen, which sifts the materials that come out of the digesters down to a 1-inch diameter. In this way, items like recyclable cans and plastics are separated.

 

After larger items are filtered out, remaining organics are laid out in windrows—long rows of compost pictured at left. Compost in the windrows will be turned twice a day over a period of about five weeks.

Leonard holds finely sifted compost after it’s passed through a final trommel screen, which sifts down the compost to particles not larger than a quarter-inch in diameter. The sifting process helps to separate glass from the organic material. That glass can be recycled later. One of the biggest challenges the Sevier Solid Waste Composting Facility faces today is managing the moisture in the area of the windrows: it needs to be moist enough to keep the compost breaking down, but dry enough so that glass can be better separated from the compost. The better it separates, the more can be recycled.

 

Though cardboard can break down into compost, Sevier Solid Waste asks customers to separate it, since it has more value when sold for recycling. It can be sold at about $100 to $125 per ton. Sevier County has plenty of cardboard waste, too, because of the many restaurants catering to the county’s large tourism industry.

 

After about 40 days, what was once considered trash has become finely sifted, nutrient-rich compost. “Sixty percent of everything that comes in goes out as compost … and is used on farms, goes back to the earth,” explains Leonard, who is pictured holding the final product here. An added bonus: individuals can come and pick up bags of compost for free.

“That’s one way the citizens can see that we can make something useful out of this waste,” says Larry Waters, Sevier County mayor.

from:    http://www.yesmagazine.org/planet/sevier-county-composting

Volcano Report fr/E. Klemetti

Eruption Update: Copahue, Poás, Sinabung, Kilauea, Holuhraun and Italy

Webcam image of Copahue in Chile, seen on October 16, 2014. A small steam-and-ash plume can be seen along with deposits of fresh, dark grey across on the volcanoes slopes. Image: SERNAGEOMIN.

I apologize for being missing for the last week. The big Geological Society of America meeting is next week in Vancouver BC and not only am I giving a talk and co-chairing a session, but two of my students are presenting posters. Needless to say, things have been busy. My talk centers on what zircon can tell us about the storage conditions and source magmas across the Cascade Range. I have zircon data from four Cascade volcanoes: St. Helens, Hood, South Sister and Lassen, it is a great chance to see how the differences in different parts of the Cascade arc might influence the composition of zircon. My two students are both presenting on their pieces of the Lassen Volcanic Center project, so we’ll be presenting over 800,000 years of zircon data.

Not only that, but I also built a volcano on the Denison campus, so if you missed the video of that, check it out.

So, without further ado, here’s some brief updates around the world of volcanoes:

Iceland

The Holuhraun lava field eruption is now one of the largest continuous eruptions in the past few centuries in Iceland here in its second month of activity. Lava flows and fountains are continuing on the plain between Barðarbunga and Askja while the Barðarbunga caldera itself is still subsiding at a rate of 30-40 cm/day. So far, that subsidence is over 0.75 cubic kilometers of lost volume below the caldera floor and large earthquakes are still occurring near the caldera. The biggest danger from this eruption so far has been the copious sulfur dioxide emissions that continue to cause problems for people in Iceland (depending on the winds). If you want to see some stunning images of the eruption, check these out — especially some of the overhead shots of the lava flows. Also, there might be something lost in translation, but Haraldur Sigurðsson make the odd prediction that the eruption would end on March 4, 2015 — a little too specific for my tastes.

Indonesia

Sinabung has entered back into a phase of more intense dome-collapse pyroclastic flows. This crisis at Sinabung has now lasted well over a year and local residents are running into problems with access to food and water. Not only that, but rainfall around the volcano combined with these eruptions has caused the threat of volcanic mudflows (lahars) to increase dramatically. The loose volcanic ash and debris is easily remobilized when heavy rains occur, creating a concrete-like slurry that can be very damaging and dangerous. On the opposite end of the spectrum, some of the pyroclastic flows have also triggered fires in the regions around Sinabung.

Chile/Argentina

Copahue has had a number of moderate explosive eruptions over the last week that prompted some minor evacuations of herders near the volcano. This is the third bout of explosive activity at the volcano since it became restless at the end of 2012. The alert status at Copahue is Orange and if you want to check out what is up there, use the SERNAGEOMIN webcam.

Costa Rica

Poás experienced a number of explosions as well. These mainly steam-driven events closed off the summit of the volcano to tourists for a few days, but access has been reopened after signs of the volcano settling down again – although the overall unrest continues. Be sure to check out the OVSICORI time-lapse video of the explosion as well.

Hawaii

The lava flow headed down the slopes of Kilauea towards Pahoa is still continuing to crawl forward. Now the flows are moving at ~25 meters/day, but the threat still remains for the flows to reach houses and roads if it continues to flow. The current estimate has the flow reaching Apaa Street in Pahoa around November 1. So far, the only damage the flows have caused is to vegetation.

Italy

In case you missed it, be sure to read David Wolman’s coverage of the appeal for the Italian geologists convicted in the aftermath of the L’Aquila earthquake. It still amazes me how much the Italian judicial system is willing to believe in charlatans and find scapegoats for an act of nature.

from:    http://www.wired.com/2014/10/eruption-update-copahue-poas-sinabung-kilauea-holuhraun-italy/#more-1601379

Southern California Earthquake 10/06

Earthquake close to Ridgecrest, Southern California

Last update: October 6, 2014 at 12:41 pm by By

Update : A light shaking is expected to be felt in Ridgecrest.
Screen Shot 2014-10-06 at 14.17.07

14km (9mi) ENE of Ridgecrest, California
73km (45mi) NE of California City, California
96km (60mi) NNW of Barstow, California
98km (61mi) NNW of Barstow Heights, California
435km (270mi) SSE of Carson City, Nevada

Most important Earthquake Data:

Magnitude : 3.7

Local Time (conversion only below land) : 2014-10-06 04:35:21

from:    http://earthquake-report.com/2014/10/06/minor-earthquake-southern-california-on-october-6-2014/

Nevada Earthquake

Earthquake near Enterprise, Nevada (also felt in Las Vegas)

Last update: October 5, 2014 at 10:44 am by By

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Update 10:30 UTC : ER does not immediately expect damage from this earthquake

Screen Shot 2014-10-05 at 12.26.59

14km (9mi) SSW of Enterprise, Nevada
23km (14mi) S of Spring Valley, Nevada
24km (15mi) SSE of Summerlin South, Nevada
25km (16mi) SSW of Paradise, Nevada
399km (248mi) NW of Phoenix, Arizona

Most important Earthquake Data:

Magnitude : 3.58

Local Time (conversion only below land) : 2014-10-05 03:11:26

GMT/UTC Time : 2014-10-05 10:11:26

from:    http://earthquake-report.com/2014/10/05/minor-earthquake-enterprise-nevada-on-october-5-2014/

Anchorage, Alaska Earthquake

Very strong deep and moderately dangerous earthquake at Anchorage, Alaska

Last update: September 26, 2014 at 9:37 am by By

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Final Update : As expected by ER NO structural damage has been detected but a lot of in-house, in-office etc damage like collapsed ceilings, fallen hanging objects, products fallen from shelves etc. Reason : the deep hypocenter. If shallower, structural damage may have been caused.

Are you one of the people who felt the shaking of this earthquake AND/OR are you aware of any damage (at your place or elsewhere)? If yes, may we kindly request you to let us know what you have felt and if you have damage or not. Please use the form below.

Update 18:40 UTC : Below the first damage pic from Alaska. Bill Falsey will not be the only one posting such images.

Screen Shot 2014-09-25 at 20.39.51

Update 18:25 UTC  : The theoretical Pager expects a MMI VI strong shaking (updated) for the Anchorage area, which reflects better what we receive as IHFI reports.

Screen Shot 2014-09-25 at 20.25.03 Screen Shot 2014-09-25 at 20.25.16

Update 18:09 UTC : Based on the first received experience reports we fear that slight damage will be possible. Max. theoretical shaking should be MMI V (moderate shaking). Moderate shaking is mostly harmless.

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Update 18:07 UTC : ER is not expecting any damage from this earthquake mainly for 2 reasons: a) a too deep hypocenter (breaking point) which makes that the earthquake is felt in a wide radius but b) the distance from populated areas

A TSUNAMI IS NOT EXPECTED (below land and too deep)

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97km (60mi) WNW of Willow, Alaska
127km (79mi) WNW of Knik-Fairview, Alaska
131km (81mi) NW of Anchorage, Alaska
381km (237mi) SW of Fairbanks, Alaska
905km (562mi) WNW of Whitehorse, Canada

Most important Earthquake Data:

Magnitude : 6.2

Local Time (conversion only below land) : 2014-09-25 09:51:17

GMT/UTC Time : 2014-09-25 17:51:17

from:    http://earthquake-report.com/2014/09/25/very-strong-earthquake-willow-alaska-on-september-25-2014/

Tectonic Plate Movement Faster than Before

 
Tectonic Plates Moving Faster: Study September 12, 2014
San Andreas Fault from the air
This aerial view of the San Andreas Fault shows how an untold number of slips have altered the landscape.

Scientists say they have found that Earth’s tectonic plates are now moving faster than at any other point in the last 2 billion years.Plate tectonics is the prevailing geologic process that shapes the planet.

It triggers most of the world’s strongest earthquakes and many volcanic eruptions, along with building mountains and moving continents.

While earlier research seemed to reveal that the massive tectonic plates are actually slowing down as Earth’s core cools, New Mexico Institute of Mining and Technology geochemist Kent Condie and colleagues say they have evidence of faster plate movements.

Writing in the journal Precambrian Research, the team says they looked at how often new mountain belts form when plates collide, and compared it to magnetic data from volcanic rocks.

That allowed them to determine where the rocks formed and how quickly the continents had moved.

Photo: U.S. Geological Survey

from:    http://www.earthweek.com/2014/ew140912/ew140912a.html

Eruptions at Mayon Volcano in Phillipines

New Eruptions at Mayon in the Philippines Prompts Evacuations

The conical summit of Mayon in the Philippines. Paths of previous lava flows and pyroclastic flows can be seen on the steep slopes of the volcano.

Quick post before I take off for the Department of Geosciences Fall Field Trip. If you’re looking for the current status of the eruption in Iceland, be sure to check out the Icelandic Meteorological Office.

However, today’s post is about the renewed activity at Mayon in the Philippines. It appears that lava is now actively extruding at the summit of the volcano, producing rock falls of incandescent blocks of lava. Seismic activity has increased dramatically over the last week and the style of earthquakes suggests to geologists at PHIVOLCS that magma is ascending inside the volcano. They have increased the alert status at Mayon from 2 to 3 (on a 5 level scale) and say that the potential for a “hazardous eruption” within weeks is high.

What this means in a practical scene is that over 24,000 people are now being evacuated from an 8-km radius around Mayon. The Philippine government is establishing refugee camps for the first evacuees* and readying more if the situation at the volcano suggests that a larger evacuation is needed. The largest hazard posed by Mayon is that of pyroclastic flows generated by the collapse of the new lava dome forming at the summit (or possibly from any explosive eruptions that might occur). Mayon is definitely one of the most active volcanoes in the Philippines — and even when it is not in an active eruption period, steam explosions at the summit can be deadly. The Philippine government is watching the activity closely to determine if and when more evacuations are needed.

As I mentioned with the eruption of Rabaul, this activity at Mayon has the potential to have much more direct consequences on people than the activity in Iceland. In the Western Pacific and Southeast Asia, hundreds of thousands of people live within a few tens of kilometers of these potentially highly explosive volcanoes. At Mayon, that number is over 250,000 people within 10 kilometers! Keeping a close eye on these eruptions is definitely a necessity to protect those lives.

* AUTHOR’S NOTE: This article from the Philippine Star quotes a PHIVOLCS volcanologist as saying that Mayon is “overdue” for a large explosive eruption. This is based on a grand total for 2 prior eruptions in 1814 and 1897. I wouldn’t believe this sort of talk as 2 data points cannot be used to set such a pattern, even if it existed.

from:    http://www.wired.com/2014/09/new-eruptions-mayon-philippines-prompts-evacuations/#more-1565563

Earthquake Close to Guam

Very strong, deep earthquake very close to Guam

Last update: September 17, 2014 at 9:13 am by By

Update 08:45 UTC: Only light damage as broken glass, falling shelves and unsecured objects or damaged transformers reported.  No important damage or injuries currently.Update 08:40 UTC: Power is reported out at Mount Santa Rosa, Yigo and also in Dandan area were crews are working to safely fix a line as a result of the earthquake. In southern villages power has been mostly restored.

Update 08:25 UTC: A landslide was reported in East Agama, Uttam. Guam Police Department and Department of Public Works have been dispatched to follow up on the situation.

Update 07:27 UTC: The earthquake was downgraded to Magnitude 6.7. This makes it less dangerous.

Update 07:11 UTC: Pacific Daily News is reporting power outages from Talofofo to Malojloj and down to Bear Rock in Inarajan.
– Some residents have reported losing phone service after the quake.

Update 06:37 UTC
As reported by our readers, the USGS ShakeMap gives a strong intensity for the whole island. This can cause moderate damage to buildings. So far, no reports indicate any damage or destruction.

A magnitude 7.1 earthquake occurred only a few km north of Guam, according to preliminary USGS data. The hypocenter was located in a depth of approx. 130 km. This makes the earthquake less dangerous and reduces the chance for a tsunami. NO warnung was issued, althouth small, non-destructive waves along the coast of Guam can not be excluded.

The shaking of the earthquake was felt very strongly on Guam, according to reports we received.

Guam ShakeMapNearby cities:

  1. 45km (28mi) NW of Piti Village, Guam
  2. 51km (32mi) NW of Tamuning-Tumon-Harmon Village, Guam
  3. 54km (34mi) WNW of Dededo Village, Guam
  4. 55km (34mi) NW of Mangilao Village, Guam
  5. 49km (30mi) NW of Hagatna, Guam

Most important Earthquake Data:

Magnitude : 6.7

Local Time (conversion only below land) : Unknown

GMT/UTC Time : 2014-09-17 06:14:49

from:    http://earthquake-report.com/2014/09/17/very-strong-earthquake-mariana-islands-on-september-17-2014/