It seems this time Kick’em Jenny is going to do her name honor – today, 23 July 2015, an orange alert has been issued for the submarine volcano.
Kick ’em Jenny and newly identified craters and domes discovered in March 2003. (Image courtesy of NOAA and Seismic Research Institute, 2003 [published in GVN Bulletin]).
The Seismic Research Centre (SRC) of the University of the West Indies has issued an orange alert for the underwater volcano Kick’em Jenny, after strong and sustained signals were recorded in the early hours of this morning suggesting than an eruption could occur with less than 24-hours notice. Instruments monitoring the volcano, located 8km north of Grenada (12.3000° N, 61.6400° W), recorded strong, continuous activity between 1:25 a.m. and 3.am. Grenada, as well as St. Vincent and the Grenadines, Barbados and Trinidad & Tobago are particularly on alert. At the orange alert level, the SRC recommends that the governments of Grenada, St. Vincent, Barbados and Trinidad & Tobago should advise residents of evacuation routes, and put transportation on standby to facilitate evacuation in the event of a tsunami.
Kick’em Jenny, on the steep inner western slope of the Lesser Antilles ridge, was discovered in 1939 when an explosive eruption broke the surface, producing ash columns that reached up to 300 meters above the sea surface (Devas, 1974). There have been at least 11 eruptions since then, with the most recent in 2001. The first detailed survey of the volcano in 1972 revealed a conical structure 1,300 meters high, constructed on the western flank of the arc. The summit crater was found to be at a depth of 190 meters and approximately 180 meters in diameter. The deepest point on Kick ’em Jenny’s crater floor lies at ~264 m depth.
Ocean ground investigation on Kick’em Jenny hydrothermal vents
Recent bathymetric surveys have shown evidence for a major arcuate collapse structure that was the source of a submarine debris avalanche that traveled more than 15 km to the west. Bathymetry also revealed another submarine cone to the SE, Kick ’em Jack, and submarine lava domes to its south. These and subaerial tuff rings and lava flows at Ile de Caille and other nearby islands may represent a single large volcanic complex. Numerous historical eruptions, mostly documented by acoustic signals, have occurred at Kick ’em Jenny since 1939, when an eruption cloud rose 275 m above the sea surface. Prior to the 1939 eruption, which was witnessed by a large number of people in northern Grenada, there had been no written mention of Kick ’em Jenny. Eruptions have involved both explosive activity and the quiet extrusion of lava flows and lava domes in the summit crater; deep rumbling noises have sometimes been heard onshore. Historical eruptions have modified the morphology of the summit crater.
The emission of large quantities of bubbles was observed in 1989 when the submersible Johnson Sealink entered the crater a few months after the 1988 eruption (SEAN 14:05).
A water column containing a significant proportion of rising gas bubbles results in a local lowering of the seawater’s density. (The rising bubbles displace some of the sea water, and at or near the sea surface they provide negligible support to the ship, thus resulting in a loss of buoyancy for ships passing over the volcano.) To account for this hazard, and the risk posed by ejecta, an exclusion zone 1.5 km in radius was created over the volcano (Shepherd, 2004).
UPDATES
UWI Scientific Advisory Jul.25.2015
Kick’em Jenny Update 1
Elevated seismic activity associated with Kick’em Jenny submarine volcano has continued since our last update. Following the hour long eruption signal which started at 01:42am on 23 July 2015 activity continued at an elevated level until 1:30pm. During the period midnight to 4:30pm on 23 July 2015 more than 400 events were recorded. The largest of these was of magnitude 3.3. Seismicity declined from 1:30pm to 5:30pm on 23 July but increased thereafter. At about 2:00am on Friday 24 July an explosion signal was recorded. This signal lasted for about an hour. T-phase from this event was recorded in Montserrat confirming the nature of the activity. The number of earthquakes declined during Friday with only 89 events recorded up to 4:00pm. Overnight this decline continued and between 4:00pm 24 July to 6:30am 25 July less than 20 earthquakes were detected. We will continue to monitor throughout the day to develop a better understanding of the current state of the system. The current alert level remains at Orange.
UWI Scientific Advisory Jul.25.2015
Kick ’em Jenny Update 2
Activity associated with the Kick’em Jenny system continues to decrease. From the 20 events recorded between the period 4:00pm 24th July to 6:30am 25th July, the number of events recorded up to 8:00pm 25th (local time) has consisted of less than 10 below magnitude 2.0. A reconnaissance flight was conducted this afternoon with, volcanologist Dr. Frederic Dondin, one of two of the UWI-SRC team currently in Grenada. Nothing out of the ordinary was observed at the surface above the volcano. Additional instruments were also placed closer to the volcano which reduces the threshold magnitude of events associated with the Kick-‘em-Jenny system that can be identified. We will continue to monitor and update as data come to hand. The current alert level at Kick ’em Jenny still remains at Orange.
Source: http://www.uwiseismic.com/ScientificAdvisories.aspx
Enjoy! -GRANYIA
Sources:
– http://www.uwiseismic.com/NewsDetails.aspx?id=365
– http://www.uwiseismic.com/General.aspx?id=53
– http://volcano.si.edu/volcano.cfm?vn=360160
Yet another interesting article from a part of the world of which I am totally ignorant, thank you! Do you know anything about the history of the weird name(s) of the volcano(es) here ?
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Hi Tom, you’re welcome! This question must have been asked a million times today, as the news of the new activity goes round through the newspapers 😀 The University of the West Indies Seismic research Center has it on first place in their FAQ but even they are not sure of the origin of the name!: “We are not certain of the exact origins of the name ‘Kick ’em Jenny’, but it seems to relate to the fact that the waters in this region are sometimes extremely rough. It may be a corruption of the French: cay que gêne, ‘the turbulent cay (shoal)’, or it may be a reference to a kicking donkey ‘Jenny’.” – This and more answers here:
http://www.uwiseismic.com/General.aspx?id=55#How%20did%20Kick%20%27em%20Jenny%20get%20its%20name?
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Thanks Granyia! I will RTFA properly the next time 😉 The french corruption theory mentioned in the FAQ seems to me to be the most likely origin
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Btw. digging a bit deeper into the site linked, I came over this page http://www.uwiseismic.com/NewsDetails.aspx?id=366 – it mentions that “..A sharp increasing trend was observed during the 21st and 22nd July and between 1:25am and 3:00am on Thursday 23rd July, 2015 the most intense activity, an eruption was observed..” – if this is the case, I wonder why the warning level is only orange?
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Hmm… I have searched very hard, and everywhere else they were saying eruption is possible within a day or two. Could it be that in fact there was a small eruption already, but they decided not to wake the sleeping dogs just yet? There was something itching at the back of my mind when I read the “within 24 hours” statement – that is too narrow a timespan, not the way volcanologists express themselves normally. But the alert level does not need to be red, even if there was a small eruption, it depends on how dangerous they expect it to become. (See for how long Sinabung and Raung in Indonesia have been on Orange; Raung still is, and Sinabung only recently was raised to Red).
Anyway, the official version is this (sorry, I lost the link, it was in a newspaper):
The situation of the submarine volcano Kick’em Jenny has not changed. “Its activity is still quite high,” explains Jean-Marie Saurel, technical director of the Volcanological and Seismological Observatory of Martinique. The island is in orange vigilance since Thursday (July 23) . “It means that there has been a significant upsurge in volcanic activity, with earthquakes, fumaroles, degassing. It suggests that an eruption could occur in the days to come,” believes Jean-Marie Saurel. There is no reason to fear a tidal wave for the moment according to the Observatory of Morne Cadet. “A tsunami is generated once the volcano has an eruption. If there is one, it can occur months or weeks after the onset of activity.”
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Nice post once again, Madam. The bubbling from the deeps has been postulated as one of the mechanisms that the Bermuda Triangle drags its targets / victims from the surface of the Atlantic to the bottom. There is a small amount of truth to that scaremongering as the Triangle is littered with cones on the surface of the ocean indicating methane leaks to the surface. Once the gas is bubbling into the water, its density decreases sometimes to the point where buoyancy goes away for surface craft.
Second observation is that air bubbling out of sinking ships does the same thing to people who jumped off and are furiously swimming away from the point of sinking. This is referred to as being sucked down by the ship.
I think Bob was doing similar things several years ago though nothing entered the region of decreased buoyancy. Cheers –
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Interesting hypothesis – I read somewhere that mass release/melting of methane clathrate deposits also could create such effects in this area. I guess this could be triggered by volcanic degassing and/or hydrothermal activity too.
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Does anybody know if there have been past eruptions that created ashfall on land for Kickem Jenny?
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Hi Cbus, the first and biggest recorded eruption was that in 1939 (funny that it happened exactly the same day, 23 July), which was described as very similar to those of Surtsey or Kavachi. Up to 300 m high fountains of mud and seawater, but no ash mentioned. The volcano was only discovered that year, so previous visible eruptions must have been before living memory. (see http://www.uwiseismic.com/General.aspx?id=26)
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I am still pondering your question… is it possible at all for a submarine volcano to create an ash plume (as opposed to a mud fountain) before it almost reaches the water surface? How would the ash stay dry enough to be dispersed by wind for over 8 km; if it has travelled 180 m through water it surely would come out as mud and act rather like lapilli or bombs? What made you ask?
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Turns out, my feeling was right – there seem to have been two small eruptions in Kick ‘em Jenny already. The first before they raised the alert level (as it was mentioned in the report) and the second a night after.
Another one of the zillions of newspaper reports on Friday said:
“ST GEORGE’S, Grenada — The Seismic Research Centre (SRC) at the University of the West Indies recorded a second small eruption during the night of Thursday at the Kick ‘em Jenny submarine volcano… The alert level was increased to Orange on Thursday, which remains in effect, and therefore means that all ships must strictly observe the five kilometer exclusion zone of Kick ‘em Jenny.”
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A few thoughts, mostly from looking at the GVP page. First; the 1988 eruption, which produced minor surface activity (SRU) or none at all (GVP) apparently involved the violent destruction of a fairly substantial summit dome. Given the demonstrated suppressive effect of about 190m of water, this suggests that for the 1939 eruption to generate a 300m plume it must have been a real lulu of an explosive event, no?
Second, re the name. Both interpretations relate to the unusually rough and turbulent water noted by old sailing-ship crews in the area. Is it, perhaps, possible that buoyancy-reducing eruptions or vigorous degassing from the then-unsuspected submarine volcano might have been a contributory factor?
On a more frivolous note, Georges Boudon of the Pelee Observatory heard the submarine explosion signals in 1988 …while scuba-diving off Martinique. Volcanology has its compensations.
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Today’s Picture of the Day on NASA’s Earth Observatory website is the “Nighttime View of Raung Volcanic Plume” – seen with CAT’s eyes…
“When it comes to seeing what’s going on in the atmosphere after dark, CATS has an advantage. From a perch on the outside of the International Space Station, the Cloud-Aerosol Transport System (CATS) recently observed part of a plume streaming from Raung Volcano, even though the plume was not apparent in imagery from other spaceborne instruments.” Continue reading: http://earthobservatory.nasa.gov/IOTD/view.php?id=86286
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Substantial earthquake here in Anchorage some 0+15 ago. About 110 km NW town at a depth of 130 km. Preliminary magnitude of 5. I expect it to be revised upward. The initial shaking was somewhat muted. Surface wave was a pretty good jolt that kept going for a while as it tailed off. No loss of power, utilities, or damage. Nothing fell off shelves. That area of Alaska has had a number of similarly sized and located quakes for the last couple months. Might ask AVO if anything is going on next week. Closest volcano is Hayes which has been quiet for around 500 years. Last series of major eruptions out of it was some 4,000 years ago. Cheers –
http://wcatwc.arh.noaa.gov/?p=PAAQ/2015/07/25/ns27g6/1/SEAK71
http://www.volcanodiscovery.com/hayes.html
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Isn’t that too deep for anything volcano-related? How deep were the others before this, similar?
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Depths have been similar. Not active volcano related, but I worry about precursor events – magma on the move thru recently opened fault lines into inactive chambers slowly crystallizing. Cheers –
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Is this to be believed or just a hoax?
Tolbachik Diamonds
http://www.meteovesti.ru/news.n2?item=63573574972
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I have added two updates (Scientific Advisories from UWI) at the end of the post!
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An M 7.2 Earthquake just happened in Papua/Indonesia! Depth 60 km. USGS has it a M7.0 / 33 km.
http://www.emsc-csem.org/Earthquake/earthquake.php?id=452489
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