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Slightly damaging earthquake near the coast of Guatemala - June 22, 2017
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Update Friday 07:00 UTC: Latest CONRED statistics as per 16:00 (4 PM) local time
65 incidents reported, 122 affected persons, 21 people with damaged properties, 4 injured, 5 houses with slight damage, 15 houses with moderate damage, 1 house with serious damage, 8 affected roads, 11 affected schools, 7 affected churches, 14 affected buildings, 1 destroyed bridge.
Update 22:22 UTC: Understanding the M6.8 Guatemala earthquake
The June 22, 2017 M 6.8 earthquake offshore of Guatemala occurred as the result of shallow thrust faulting on or near the subduction zone interface in the region. At the location of this earthquake, the Cocos plate converges with the Caribbean plate at a rate of 69 mm/yr towards the northeast, and subducts beneath Central America at the Middle America Trench, 110 km to the southwest of this earthquake. The June 22nd event is located near to the triple junction between the Cocos, Caribbean, and North America tectonic plates; just to the northwest of this earthquake, the Cocos plate subducts beneath the North America plate at the slightly faster rate of 79 mm/yr, accommodating left-lateral strike-slip motion between the Caribbean and North America plates near the surface in south-central Guatemala. The location, depth, and focal mechanism solution of the June 22nd earthquake are all consistent with the event occurring on the subduction zone interface.
Central America is very seismically active, and the region within 250 km of the June 22, 2017 event has experienced 35 other M 6.5+ earthquakes over the preceding century. Most also occurred on the shallow plate interface in this region. The largest was a M 7.7 earthquake in August 1942, 25 km to the northwest of today’s earthquake, which caused 38 fatalities and triggered many landslides along the coast of Guatemala. A M 6.8 in October 1979, 15 km to the northeast of the June 22, 2017 earthquake, resulted in 7 fatalities.
The June 22nd, 2017 earthquake also follows a series of 16 events of M 4.0-5.5 on or near the subduction thrust interface about 150-250 km to the northwest, between late May 2017 and as recent as June 19, 2017. On June 14, 2017, a larger M 6.9 normal faulting, intermediate depth earthquake occurred within the subducting Cocos plate 175 km to the northwest of today’s event. The June 14th earthquake has been reported to have caused 5 fatalities.
Source: USGS
Update 22:22 UTC:
Probably the best scientific explanation of today's earthquake by Jay Patton. Click on the poster to connect to his great webpage.
Update 22:00 UTC: Another update with unfortunately more numbers from CONRED at 13:00 local time
52 incidents reported, 52 affected persons, 9 people with damaged properties, 4 injured, 5 houses with slight damage, 4 houses with moderate damage, 8 affected roads, 9 affected schools, 6 affected churches, 11 affected buildings, 1 destroyed bridge.
Update 16:18 UTC: Overview of the inspections of CONRED at 07:00 Local Guatemala time.
27 incidents reported, 4 houses with slight damage, 8 affected roads, 6 affected buildings, 2 affected bridges.
Update 15:23 UTC: CONRED reports landslides and slight structural damage in Sacatepéquez, Totonicapán, Chimaltenango, Suchitepéquez and Escuintla
Photo: CONRED Guatemala
Update 15:18 UTC: At the moment of writing this update we have only found some limited damage as shown on the picture below. Luckily no reports of injuries or fatalities.
Update 14:10 UTC: CONRED teams (civil defense Guatemala) are currently inspecting infrastructure and will help were needed.
Update 14:05 UTC: Based on theoretical calculations USGS expects a max. strong shaking felt by 333,000 people. Nearly 17 million may have felt a light shaking.
Update 13:58 UTC: Professor Max Wyss, who specializes in theoretical prognoses of injuries and fatalities expects : 0 fatalities and 0 to 70 injured people
Update 13:48 UTC: Below the focal mechanism of this earthquake. The main movement is "thrust" due to the Caribbean plate pressing in opposite direction into the heavier Cocos oceanic plate who subducts the Caribbean plate.
Do beach balls looks like Chinese or Latin to you, check this article "Understanding Beach Balls"
The main movement as described above can be seen better on this image. We presume that Fault Plane 2 will be the one today (although in this case difficult to distinguish)
Main earth movement based on the current focal mechanism. Image courtesy Observatoire Geoscope
Update 13:46 UTC: NO tsunami alert for the North American coastal area's. Some strong currents and local tsunami possibility close to the epicenter is still possible. Inhabitants of the area will be locally informed about the danger.
Update : Based on the present earthquake parameters (Magnitude, Depth, Population, etc) and our experience with earthquake damage impact, earthquake-report.com calls this earthquake dangerous and expects some injuries and possibly serious damage
Update 13:45 UTC: Due to the epicenter closer to the coast we now think that the strong shaking at the coast meybe more dangerous than initially thought.
Puerto San José, Guatemala, 23.7 km (14.7 mi) SWPopulation: 18,655
La Gomera, Guatemala, 38.2 km (23.7 mi) SSEPopulation: 24,001
Masagua, Guatemala, 51.0 km (31.7 mi) SSWPopulation: 10,045
Nueva Concepción, Guatemala, 62.4 km (38.7 mi) SEPopulation: 11,121
Escuintla, Guatemala, 63.6 km (39.5 mi) SSWPopulation: 103,165
Most important Earthquake Data:
Magnitude : 6.8
Local Time (conversion only below land) : Unknown
GMT/UTC Time : 2017-06-22 12:31:01
Depth (Hypocenter) : 32 km
Depth and Magnitude updates in the list below.
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