Earthquake Cluster North Of Puerto Rico

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In summary, the earthquakes north of Puerto Rico are clustered and appear to be aftershocks from a larger event. There is a possibility that this is the precursor to a larger earthquake.
  • #1
lisab
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I'm a total noob when it comes to geology, so sorry if this is a dumb question.

I live on the Ring of Fire so earthquakes are never far from my thoughts. I go to the USGS earthquake page often just to check out how our Earth is doing.

Lately I've notice a cluster of quakes just north of Puerto Rico. Here's a screen shot I took just now:

35hpkjd.jpg


A couple observations:

These are very small quakes - in the 2.0 to 3.5 range (one 6.4 is buried in there)
They vary in depth - from 3 km to over 90 km.
The screen shot just shows the last 7 days but it's been like this for months.

I don't see any similar thing happening elsewhere on the planet. Maybe Adak comes close, but nowhere near this spot.

So, what's going on north of Puerto Rico??
 
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  • #2
Hi Lisa

The M6.4 was the mainshock, I did record it on my gear here in Sydney, Australia. Not overly large amplitude considering how far it was away from me

What you are seeing is a pretty normal aftershock sequence from any reasonable sized and shallow event.
There were one or two M5 aftershocks in there as well
Seeing an aftershock sequence like this is always valuable in determining the extent of the movement on the fault plane. The pic is in 2D, but if you take the depths of events into account, you can produce a 3D diagram and see any dipping structure of the fault plane

Keep an eye out for future large events and you will see the mass of aftershocks that follow the mainshock.
On occassions you will also see several forshocks to the mainshock.

cheers
Dave
 
  • #3
went into my records for another example for you :)

this one below is from Christchurch, New Zealand, following the M7.1 and several M 6 events of 2010 and 2011. The map as it states covers a 60 day period prior to and including 24 Feb 2011
but doesn't include the initial M7.1 of Sept 04, 2010 and many of its aftershocks, you can see the same clustering of the events

attachment.php?attachmentid=65798&stc=1&d=1390116986.jpg



cheers
Dave
 

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  • #4
The USGS statistics are somewhat skewed because, "starting in January 2009, the USGS National Earthquake Information Center no longer locates earthquakes smaller than magnitude 4.5 outside the United States, unless we receive specific information that the earthquake was felt or caused damage." USGS records all earthquakes in the USGS, but filters those outside the US.

http://earthquake.usgs.gov/earthquakes/eqarchives/year/eqstats.php
http://earthquake.usgs.gov/earthquakes/map/doc_whicheqs.php

In the US, earthquakes of mag 3 or less are quite common, particularly in Hawaii, Alaska, parts of the Cascade range and California.

Indonesia, Japan, New Zealand, and basically the western Pacific 'Ring of Fire' and Sunda extension have frequent earthquakes. Puerto Rico has been particularly active for quite some time.
 
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  • #5
davenn said:
Hi Lisa

The M6.4 was the mainshock, I did record it on my gear here in Sydney, Australia. Not overly large amplitude considering how far it was away from me

What you are seeing is a pretty normal aftershock sequence from any reasonable sized and shallow event.
There were one or two M5 aftershocks in there as well
Seeing an aftershock sequence like this is always valuable in determining the extent of the movement on the fault plane. The pic is in 2D, but if you take the depths of events into account, you can produce a 3D diagram and see any dipping structure of the fault plane

Keep an eye out for future large events and you will see the mass of aftershocks that follow the mainshock.
On occassions you will also see several forshocks to the mainshock.

cheers
Dave

Do you think the dozens (more like hundreds) of little quakes that have been happening there for several months were foreshocks to the 6.4 one? And is it typical for aftershocks and/or foreshocks to vary so much in depth, or does that depend on local conditions?
 
  • #6
Hi Lisa
( will try typing this a second time, browser crashed and I lost a lots of text grrrr )

There are 4 common quake situations

1) A swarm - no significant mainshock
2) A swarm - with a significant mainshock
3) A shallow mainshock - with or without several foreshocks but lots of aftershocks
4) A deep mainshock - very rare foreshocks and few if any aftershocks

Ohhhh and another semi rare event where there are 2 major shocks within a hours or day's of each other
called doublet events. There have been a couple in the last ~ 5 years a pair of M8+ events in the Kuril Isl. north of Japan and a couple of years ago, west of Sumatera, Indonesia, M8.6 and a M8.2 ~ 3 hours apart.

The Puerto Rico activity appears to fall into the #2 category above, where there's an active swarm accentuated by the M6.4 mainshock then continuing with many more small events

Hawthorne, Nevada had a similar occurrence back in March and April of 2011. Some 400 small shocks over ~ 8 - 10 weeks ranging from M1 to M3.5. several weeks into the swarm there was a M 4.6 after which it resumed the smaller events till they finally died off and stopped.

Depth variations will largely be controlled by the type and location of fault that has moved
if its continental crustal fault, say like the Christchurch and Nevada events ( away from the main plate boundaries) then there not going to be a great variation in event depths - say ranging over ~ 20 km.
But a subduction fault quake will have a wide range of event depths that could easily range over 100 km or more.

Tectonics around Puerto Rico are quite complex, with Haiti, Dominican Repub. and Puerto Rico sitting between 2 subduction zones.. That area is primarily moving to the NNE and subducting under the North American Plate ( which includes a large section of the North Atlantic seafloor out to the Mid Atlantic Ridge)
http://www.intechopen.com/books/new-frontiers-in-tectonic-research-general-problems-sedimentary-basins-and-island-arcs/the-caribbean-plate-evolution-trying-to-resolve-a-very-complicated-tectonic-puzzle
http://web.ics.purdue.edu/~ecalais/projects/caribbean/dr2003/node3.html

cheers
Dave
 
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  • #7
Lisa, have you ever checked the local earthquake network? I check this daily along with the USGS site.

http://www.pnsn.org/earthquakes/recent

They even have a blog for when we have the local slow slip events in the subduction zone. Fun to follow! What I think is interesting is that we haven't had anything above 4.5 since the Nisqually quake.

the PNSN also has a facebook page, and they are great for asking questions like this. You get responses from the local UW geologists, as well as the local nut cases. *giggle*
 
  • #8
Ms Music said:
Lisa, have you ever checked the local earthquake network? I check this daily along with the USGS site.

http://www.pnsn.org/earthquakes/recent

They even have a blog for when we have the local slow slip events in the subduction zone. Fun to follow! What I think is interesting is that we haven't had anything above 4.5 since the Nisqually quake.

the PNSN also has a facebook page, and they are great for asking questions like this. You get responses from the local UW geologists, as well as the local nut cases. *giggle*

Nice - thanks for the link!
 

1) What causes earthquake clusters to occur?

Earthquake clusters, also known as swarm earthquakes, occur when a series of earthquakes happen in a specific region and within a short period of time. This can be caused by the movement of tectonic plates, volcanic activity, or human activities such as mining or drilling. In the case of the earthquake cluster north of Puerto Rico, it is likely caused by the movement of the North American and Caribbean tectonic plates.

2) How are earthquake clusters different from single earthquakes?

Earthquake clusters are different from single earthquakes in terms of their magnitude and duration. While single earthquakes have a defined magnitude and typically last for a few seconds, earthquake clusters can have multiple earthquakes of varying magnitudes and can last for days, weeks, or even months.

3) Are earthquake clusters a cause for concern?

Earthquake clusters can be concerning because they can cause damage and disruption to communities in the affected region. However, they do not necessarily indicate the occurrence of a larger, more destructive earthquake. Scientists monitor earthquake clusters to better understand the seismic activity in the area and to provide early warning systems for potential future earthquakes.

4) What is the likelihood of a major earthquake following an earthquake cluster?

The likelihood of a major earthquake following an earthquake cluster is difficult to determine. While earthquake clusters can sometimes precede larger earthquakes, there is no guarantee that this will always be the case. It is important for scientists to continue monitoring the seismic activity in the region to better understand any potential risks.

5) Is there a way to predict when an earthquake cluster will occur?

Unfortunately, there is currently no way to predict when an earthquake cluster will occur. While scientists can monitor seismic activity and identify areas that are more prone to earthquakes, it is not possible to accurately predict the timing and magnitude of an earthquake. It is important for communities in earthquake-prone areas to have emergency preparedness plans in place to mitigate potential risks from earthquake clusters.

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