Etna Week Part 1
Mount Etna - Brief Anatomy of an Exceptional Volcano
By guest blogger Dr. Boris Behncke.
Italy truly deserves to be called "the Cradle of Volcanology" - not only because it hosts virtually all existing types of volcanoes and volcanic rock compositions, and seven of its volcanoes have had confirmed eruptions during the historical period (i.e. the past approximately 2700 years), but also because the earliest surviving eyewitness account of an eruption was written in Italy, the first volcano observatory and the first geothermal power plant were built in Italy, and three volcanological terms denoting styles of eruptive activity - Strombolian, Plinian, and Vulcanian - have their origin in this country. The word "volcano" itself has its origin from the southernmost of the Aeolian Islands, in the Tyrrhenian Sea north of Sicily, Vulcano. Vesuvius, uncomfortably close to Naples and its very densely populated suburbs, is possibly still the most famous volcano worldwide, and certainly one of the most dangerous volcanoes on Earth.
In this exceptionally varied volcanic setting, Mount Etna on the island of Sicily is a volcano of superlatives. It is the most active volcano of Europe and - after KÄ«lauea on Hawai'i - possibly the second most active volcano on Earth, in terms of eruption frequency and long-term average magma output rate. It has the longest record of documented eruptions of all volcanoes worldwide, and can be said to be virtually continuously active, with significant eruptive events occurring almost every year. Its summit stands at 3330 m elevation as of 2010 (Neri et al., 2008), making it the tallest mountain in the Mediterranean basin, and the highest summit in Italy to the south of the Alps. Besides the four nearly continuously active craters at its summit, Etna has approximately 350 craters and minor vents on its flanks, each of which erupts only once, and many of which form sizable cones, like miniature volcanoes, on the flanks of the mountain.
But what makes Etna really unique is its incredible versatility in terms of eruptive styles, eruption magnitudes, and eruption locations. During the historical period, it has produced numerous effusive, Hawaiian to Strombolian style eruptions from vents both at its summit and on its flanks, sometimes purely effusive activity going on for years, countless short-lived episodes of violent Strombolian to sub-Plinian fire fountaining accompanied by voluminous lava and tephra emission, Vulcanian and phreatomagmatic explosions and persistent ash emission sometimes lasting for months (Branca and Del Carlo, 2005). This record is punctuated by a Plinian eruption in 122 B.C. (Coltelli et al., 1998), which caused devastation and hardship to the population of Catania, a city that had been founded more than 600 years earlier by the Greek at the southern base of the volcano. Pyroclastic flows, the most lethal and destructive of all volcanic phenomena, have been observed on a number of occasions in recent years, but luckily affected only the remote summit area (Behncke, 2009).
In spite of its frequent and sometimes violent and hazardous activity, Etna has claimed a surprisingly small number of human victims - less than 80 deaths can be with certainty attributed to the activity of the volcano in the past 2700 years. This figure might be higher because the historical record contains several gaps up to a few hundred years long, like the Arab domination from the 9th to 11th centuries A.D. (all Arab records were lost during the Christian recolonization); yet it is clear that Etna is not a killer volcano, and this is one of the reasons why the people living on its slopes call it "the friendly volcano".
Geological setting and evolution of Etna
Like all things in Italy, the geodynamic setting of Etna is a bit complicated. For this reason, the origin of Etna has been ascribed by various workers to subduction, rifting, and a mantle plume, and more recently, some more exotic factors.
Sicily lies on the boundary between two converging (or colliding) lithospheric plates, the African plate to the south and the Eurasian plate to the north. This convergent margin runs across much of the Mediterranean along a general east-west trend, but shows a marked bend in Italy, where it turns NNW up to the Alps before taking on a SE trend in the Balkans toward Greece. Differently from many convergent plate margins, where one plate consists of oceanic and the other of continental lithosphere (like in the Pacific Northwest of the U.S. where the oceanic Pacific plate runs into, and dives underneath the continental North American plate), the colliding plate margins in Italy are heterogeneous, with bits of oceanic lithosphere alternating with continental lithosphere. The character of convergence therefore changes over short distances from subduction, as in the Calabrian and Aegean arcs, to mountain building as in northern Sicily and along the Apennines and the Alps.
The volcanoes of the Aeolian Islands are believed to be, at least in part, due to the subduction of oceanic lithosphere of the Ionian Sea under the Calabrian arc. However, rather than consistently erupting calc-alkaline magmas as subduction-related volcanoes commonly do, the Aeolian volcanoes also produce more sodium and potassium-rich magmas, which some scientists attribute to magma melting at different depths along a very steeply dipping subducting lithospheric slab (Tommasini et al., 1997).
While out in the Ionian Sea, to the east of Sicily, the northern margin of the African plate consists of oceanic lithosphere subducting underneath the Calabrian arc, on the island itself it is constituted by rather thick continental lithosphere, which makes up the southeast corner of Sicily. Rather than subducting, it bites and pushes into the continental lithosphere of the southern margin of the Eurasian plate. The result is mountain building - much like in the Himalayas or in the Rocky Mountains - going on in the Peloritani, Nebrodi, and Madonie mountain belts, which together constitute the northern backbone of Sicily. Etna lies just north of the plate boundary and away from the Calabrian arc subduction zone, in a rather uncommon place for a volcano to occur, plate tectonically speaking. For this reason, some researchers have invoked a hot spot origin of Etna, and of the older volcanic area of the Monti Iblei to the south, where volcanism has occurred over more than 200 million years (Schmincke et al., 1997; Tanguy et al., 1997; Behncke, 1999). Schiano et al. (2001) present arguments for a transition from a hot spot origin to a more and more pronounced subduction component in Etna's magmas. However, the hot spot model is not plausible because volcanism has shown a northward shift from the Monti Iblei to Etna, which would require movement of the African plate to the south, whereas in reality the contrary is the case (the African plate is moving northward).
A series of recent publications (Gvirtzman and Nur, 1999; Doglioni et al., 2001; Schellart, 2010) places Etna into a context of slab rollback related to the subduction of Ionian oceanic lithosphere below the Calabrian arc. Slab rollback means that the bend where an oceanic plate starts descending into subduction moves gradually away from the subduction zone due to the weight of the subducting plate, and consequently it sort of tears the subduction zone and the overriding plate into the direction of the subducting plate. In the case of the Ionian plate subduction this would mean that the subduction zone migrates southeast, which is well illustrated here at Highly Allochthonous. This leads to the tearing open of a gap between the subduction setting of the Ionian oceanic lithosphere and the Calabrian arc to the east, and the continental collisional setting of Sicily to the west, which in turn causes decompression and the formation of magma in the upper mantle below this opening gap, or "window". The magma rises along the intersection of a number of major regional fault systems and feeds the activity of Etna.
Whatever the geodynamic cause of Etna, it appears to be highly efficient. Throughout its roughly half-million-years-long history, Etnean volcanism has become more and more vigorous and increasingly focused on a large volcanic edifice, eventually leading to the building of the large mountain that dominates Sicily today. The geological evolution of Etna is subdivided into four main phases: (1) the Basal Tholeiitic phase, (2) the Timpe phase, (3) the Valle del Bove centers phase, and (4) the stratovolcano phase.
Geological map of Mount Etna, from the INGV-Catania web site (courtesy of Stefano Branca). Key: (1) Recent alluvial deposits; (2) Mongibello (past 15,000 years) eruptive products (2a) "Chiancone" volcaniclastic debris deposit; (3) Ellittico eruptive products; (4) Valle del Bove centers eruptive products; (5) Timpe phase eruptive products; (6) Basal Tholeiites; (7) Sedimentary basement; "Faglia" = fault, "Orlo della Valle del Bove" = Valle del Bove rim; "Crateri Sommitali" = Summit craters
Distribution of eruptive products of the four main phases of volcanism in the Etna area: (a) Basal Tholeiites; (b) Timpe phase; (c) Valle del Bove eruptive centers; (d) Stratovolcano phase. From Branca et al. (2004)
(1) Basal Tholeiites. The first phase of volcanic activity in the Etnean area occurred about 500,000 years ago, in an area then occupied by a broad bay - referred to as the pre-Etnean gulf - leading to the emission of submarine lava (pillow lava) and associated debris, which is known as hyaloclastite. Some eruptive events lasted long enough to build small volcanic islands, much the same way as the island of Surtsey formed in 1963-1967 off the south coast of Iceland. Outcrops of these earliest products of Etnean volcanism occur along the coast of the Ionian sea immediately to the north of Catania, in the area of the fishing villages of Acicastello and Acitrezza. The castle rock of Acicastello is a world-class geological site (unfortunately not placed under protection as it would certainly deserve) where pillow lavas can be seen next to a typical breccia of small glassy fragments (hyaloclastite) and debris of shattered pillows (pillow breccia or flow-foot breccia).
The spectacular outcrop of Acicastello, on the coast of the Ionian Sea at the southeast base of Etna, where the earliest eruptive products of the volcano (Basal Tholeiites) are exposed. The left (western) part of the outcrop consists of densely packed pillow lavas, whereas breccias of shattered pillows and hyaloclastite (fragments of volcanic glass altered into yellowish-brown palagonite) make up the right portion of the section. Photos by Boris Behncke.
The products of this earliest phase of volcanism in the Etna area are tholeiitic basalts - virtually the same magma that is currently being erupted from KÄ«lauea (Hawai'i), which is the reason that this phase in the evolution of Etna is referred to as "Basal Tholeiites". Besides the outcrops of Acicastello and nearby locations such as Acitrezza and Ficarazzi, products of this phase occur also further to the west, near the town of Adrano at the southwest base of the volcano.
(2) Timpe phase. The second main phase of Etnean volcanism occurred between >220,000 years ago and about 110,000 years ago in a narrow belt along the Ionian coast along a fault system known as the "Timpe" (the steps). The Timpe faults are marked by conspicuous morphological scarps, and terminate to the NNW near Moscarello and Sant'Alfio on the east flank of Etna. During this phase, numerous fissure eruptions occurred in this relatively restricted elongate belt along the Ionian coast, and led to the growth of a NNW-SSE elongated shield volcano about 15 km long. The internal structure of this shield volcano is today exposed in the Timpe fault scarps between Acireale and Moscarello. During this eruptive period, sporadic volcanism also occurred along the valley of the Simeto river, constructing, amongst others, the large scoria cone that constitutes the hill of PaternÃ² and a number of thin, strongly eroded, lava flows like those cropping out in the northern periphery of Catania at Leucatia-Fasano. The products of this phase showed a shift from tholeiitic to alkali basaltic compositions.
(3) Valle del Bove eruptive centers. About 110,000 years ago, the focus of volcanism shifted from the Ionian coast into the area now occupied by the Valle del Bove. In this period, the character of Etna's activity underwent a profound change, from sporadic fissure eruptions as during the first two phases, to a more centralized activity of both effusive and explosive character. This activity led to the construction of the first composite volcanic edifices in the Etna region, the Rocche and Tarderia volcanoes. The products of these eruptive centers crop out along the base of the southern flank of the Valle del Bove at Tarderia and Monte Cicirello. Subsequently, the activity concentrated in the southeastern sector of the Valle del Bove, at Piano del Trifoglietto, where the main eruptive center of this phase was built up, Trifoglietto volcano, which reached a maximum elevation of about 2400 m. Three minor eruptive centers formed subsequently on the flanks of Trifoglietto, which are named Giannicola, Salifizio and Cuvigghiuni; their activity continued until about 60,000 years ago. This phase marks the formation of a stratovolcano structure in the Etna edifice and the superposition of different eruptive centers.
(4) Stratovolcano phase. About 60,000 years ago, a further shift in the focus of eruptive activity toward northwest marks the end of the Valle del Bove centers, and the start of the building of the largest eruptive center of Etna, now named Ellittico (the elliptical), which constitutes the main structure of the volcano. The Ellittico volcano produced intense effusive and explosive activity, constructing a large edifice, whose summit may have reached a height of 3600-3800 m. Numerous flank eruptions generated lava flows that reached the Simeto river valley to the west of Etna. About 25,000 years ago, the Alcantara river was deviated from its former valley closer to Etna (in correspondence with the towns of Linguaglossa and Piedimonte Etneo) into the present-day Alcantara valley (Branca, 2003). Much of the Ellittico lavas and pyroclastics are present in outcrops in the northern wall of the Valle del Bove.
The tan-colored clastic rocks in these photos are the pyroclastic-flow deposits emplaced during the climactic explosive eruptions at the end of the Ellittico stage of Mount Etna, about 15,000 years ago. These deposits occur in outcrops near the town of Biancavilla on the lower southwest flank of the volcano. Photos taken in August 2001 by Boris Behncke
The Ellittico stage ended about 15,000 years ago with a series of powerful explosive (Plinian) eruptions (Coltelli et al., 2000), which destroyed the summit of the volcano leaving a caldera about 4 km in diameter. Intense eruptive activity continued during the past 15,000 years, largely filling the Ellittico caldera, and building up a new summit cone. This current summit edifice is called Mongibello. About 9000 years ago, a portion of the upper east flank of Etna underwent gravitational collapse, generating a catastrophic landslide (the Milo debris avalanche), and forming the huge collapse depression of the Valle del Bove, which still today bites deeply into the eastern sector of the volcano (Calvari et al., 2004).
Aerial view of the Valle del Bove, a huge collapse depression formed by a massive sector collapse of Etna's eastern flank about 9000 years ago. Much of the depression has been filled by more recent lava flows; the original depth must have been significantly greater. This view is from the southeast, showing the summit craters in the upper center. Photo taken in August 2007 by Boris Behncke
Following the Valle del Bove sector collapse, remobilization of the debris avalanche deposit by alluvial processes led to the generation of a detritic-alluvional deposit, known as Chiancone, which crops out between Pozzillo and Riposto along the Ionian coast. This huge collapse of the eastern flank of the Mongibello edifice has exposed a large portion of the internal structure of both the Valle del Bove eruptive centers and of the Ellittico volcano, which crop out in the walls of the depression. The eruptive activity of the Mongibello is strongly controlled by structures of weakness in the volcanic edifice, where most intrusions occur along a number of main trends.
These predominant trends are characterized by three main rift zones, the Northeast, South and West rift zones. Although much of the activity of the Mongibello volcano is effusive, numerous strongly explosive events are known as well, mostly from the summit craters (Coltelli et al, 2000). The most powerful eruption of this eruptive phase occurred in historical time, in 122 B.C. (Coltelli et al., 1998). This eruption, which occurred from the summit of the volcano, produced a large volume of pyroclastics (ash and lapilli), which fell in a sector on the southeast flank of the volcano, causing heavy damage in the city of Catania.
(Part 2 to follow later this week.)
Thanks, Boris Behnke, for this interesting and clear explanation of the Mt. Etna.
Bevor I came on this blog I didn't realise that here in Europe we have " real" volcanos und how interesting they are!
Looking forward to Part 2.
Hello Boris Behncke, thank you,this is great stuff, especially for this neophyte who has been training on the EyjafjallajÃ¶kull eruption! Lots of information clearly expressed and building on what we have already learned. Looking forward to the next installments.
Etna is ... huge.
I am amazed at how much detail has been gathered about the history of the volcano. But when you conciser the size, there is probably a lot of information to be found.
Terrific write-up on Etna Boris! Thank you for bringing us "up-to-date" on current thoughts about the history and behaviour of la Etna!
Thanks folks - and there's quite a bit more to follow later this week!
In the meantime Sicily's geodynamics continue to be alive. This afternoon (16 August 2010) we had a magnitude 4.6 earthquake in the Aeolian Islands, the epicenter being near Vulcano island. There has been damage to buildings and infrastructures on Lipari, Vulcano, and Salina, landslides, and 7 people have been reportedly injured.
No way saying whether this earthquake is related to Vulcano, which last erupted 1888-1890.
Some more info at www.flickr.com/photos/etnaboris/
Approximate timing of Etna's eruptive phases appears to correspond to Northern Hemispheric IceAge mass changes.
See Temp Figs, Sediment Records (temps) and pattern of temperature and IceAge volume changes, section on Glacials and Interglacials.
Of particular interest is the timing of 100KY climate cycles, at ~500KY, where benthic O-18 shows large fluctuations.
Expanded map showing the collision interface between African and Eurasian plates.
Thank you, Boris, for the interesting first installment of Etna info. Sounds to me as if Sicily and the surrounding area is just about as complex as Island. I am still trying to wrap my head around slap rollback. I think I have an understanding of it, but I am not sure so I will be reading that again to see if I can make sense out of it. From the interpretative sketch, it looks very complicated and the geo community is really not all that sure what is the cause of Etna's activity because it "isn't supposed to be there" sort of thing.
Thanks for posting a picture of the Valle de Bove because that has given me a perspective of what that area looks like and where the lava flows were going in 2006. That was the time my DH and I watched the Etna Treking cam for six hours! That was awesome.
I look forward to your next post to learn more. You know, I miss your reports that you used to do on you web site. So much has changed!
Yay.... I found data.
INGV Centro Nazionale Terremoti
Gathered all quakes from 2010 to present and plotted.
Note: This plot goes down to 600 km, which is about 20 times deeper than my Icelandic plots.
And a zoomed in perspective view. Colors adjusted to reflect shallower depth limits.
Boris, what (if any) significance is there about tholeiitic basalt being the first eruptive products of etna, changing to alkalic?
Does it imply more of a mantle component in the initial products?
Also, given the large amount of melt that rises through etna, has there been any thought about whether the area might be prone to hosting a shallow magma chamber? What leads to that sort of thing? Is it a more diffuse area where intrusions take place vs the established magma path to the surface that etna posesses?
Boris' website page on Etna References, per citations referenced in his Etna introductory material.
Passerby (#11) rightly noted that there were no references in this first Etna bit - they will come with the third part (I placed them at the end of the whole thing I submitted to Erik). So with a few days of patience you'll also get the whole bunch of references (there are many recent ones included, which are not on my old "Etna references" page) ...
Meanwhile, we're getting the happy information that today afternoon's M 4.6 earthquake near Vulcano has, as it seems, not caused any injuries to people. However, it's the Big News tonight in Italy, though there's a tendency to downplay a little bit on the side of Lipari's administration, we're at the apex of the tourist season!
I think you just got your coordinates wrapped around your head... ;)
This should be on East longitude, ie. increasing from left to right when viewing North, and a northward plot should show longitudes, while the eastward plot has lats growing from right to left.
(Yeah, me too: the same head all the year round...)
Funny thing: when I started typing this comment, the keyboard was Chinese - never happened before; English pops up rather often, but this was the first spontaneous Chinese pop-up.
It's possible. I generated two of them when I saw the issue, I may have linked the wrong one. I'll go check.
"increasing from left to right"
Which one are you looking at? That's what I'm seeing. "View North" has the low numbers on the left (west)
The "View East" has north to the left (high numbers)
If you are seeing something different please let me know.
Woops! My bad (partially); what you have are mixed longitude/latitude texts.
Thanks, Boris for an informative look at Etna and its effects on the area surrounding it. I only wish I had read this before when I went up to Etna in 2006 and saw the lava flow from the 2003(?) eruption. It looked like the beginning of a 4 lane asphalt highway leading down from the summit almost to Linguaglossa (one lucky town). I was in Acireale. I wish I had known about the geologic area of Acicastello. For anyone interested in volcanoes their impact on culture and history, Sicily is a great place to visit.
I'm a fan of the INGV webcams. When are they going to fix the Stromboli webcams? And would you explain the thermal imaging webcam and what that is supposed to be telling us. I understand the thermal webcam for Stromboli but not the one for Etna.
Fantastic article Boris I enjoyed reading it.
Now what are the chances of you resuming the updates to Italy's Volcano's???? An excellent site and I've had withdrawal symptoms since you stopped updating it.
Thanks for the article Boris. Its very interesting to read.
Have you ever considered writing your own blog about Etna and whats going on there? Something like the style of your Flickr Postings today. I think there would be interest for it.
@Kultsi, Askola, FI
Okay, now I see it. The labels are backwards.
I'm currently working on extracting terrain data for Etna/Sicily in order to get a better view. I'll be correcting those labels then... if I don't decide to lash out at the guy who coded this PoS Ladserf software package in Java. (It should not take this long to save a [expletive deleted] file).
Boris, thank you for the discussion chock full of wonderful nuggets about Etna. I have to admit, I'm still a beginner, and it will take me longer to fully appreciate your information. I'm adding it to my "to read after more study" file. ;-)
@Dr. Boris Behncke
Never thought it could be sooooo interesting and enlightening to go through your article, specially the geodynamics part. I got stuck, like Diane, around the "slap rollback", but for what I could understand, it provides a very reasonable explanation which is not "mantle-plume"-related. The idea of a "window" tearing that subducting slab is amazing. It's like "rifting" in the middle of a subduction boundary, if I got it right. And Lurking plots show deep focus earthquakes typical for subduction zones, which denies the "hotspot" version.
I've been to Italy many times and my friends always wanted to drag me to Sicily, and I declined it for other historical locations, but next time this won't happen. Thank you very much indeed!
#9 #13 @Lurking
I've noticed the shifted labels too. Your plots go N through all Italian volcanoes and seismic zones up to Firenze, I think. Which makes it very interesting, because you can "see" magma rising to Stromboli, Vesuvius, etc.
M 4.5 - SICILY, ITALY - 2010-08-16 12:54 UTC
I forgot to thank you for the amazing link on Lake Kivu's methane harvesting, on the other thread. Very good "mood-stimulating" effect to me.
Thanks, Boris, my wife went to Etna when she visited back in the 70's. Erupting then. Amazing system.
Would like to see it and Sicily sometime...
Okay... a redo. Been fighting and cursing the terrain extraction program most of the day.
This is a pretty wild view, not real pretty, but its all of Sicily with the quakes planted under it. Perspective view.
And these two are closer in views with the terrain of Etna plotted over top of it.
Copy paste these two. (the forum monster will get me if I make them into links)
Caveat: If I have hosed up the lat-lon labels again, I'm going to go out back and kick something.
Hydrothermal vents rising from the same aesthenosphere source, under Sicily?
Mount EtnaâIblean volcanism caused by rollback-induced upper mantle upwelling around the Ionian slab edge: An alternative to the plume model. Schellart (2010) Geology.
#25 @Lurking: You did it again! Latitudes are supposed to be between 36Âº and 38Âº and longitudes between 12Âº5 - 16 Âº. :)
Well, then prove that this one is wrong...
The North-South and East West things are just right. Good job!
BTW what was that spoofing all about on the other thread?
Some one was using my moniker and posting stuff using it. I noticed that they put some URL in their sig. I didn't follow it since it's usually some advert when the Intruder Bots strike. A lot of times it's a script that wanders around to make random but believable posts to drum up traffic or customers.
It looks like Katla is starting to stir again this morning, it seems that the activity is going in waves starting on the North fault line and slowly moving South, it almost seems that the fault line has a pulse.
Wow.... Etna rocks...!!
As a Frenchman, I don't get too often my fix of active volcanism (or I would have to go to La RÃ©union, which would be interesting by the way ;), and I'm absolutely delighted to have such a volatile neighbor not too far away... (unless it does what Eyjaf did this spring and grounds every aircraft for two weeks..)
Kudos to Boris Behnke for such a master piece of information.... To everybody who run this blog, Keep on the good work!!
Now, for everything to go insanely cool, I would love to have it erupt.... Oh nothing big, just the pyrotechnics we all know and love, without disturbing anything nearby!
@RH #32... check the depths. All 1km. Nothing to remotely get excited about it!
love these articles, but could we get access to higher resolution images, please
WOW! I am amazed at how much detail has been gathered about the history of the volcano. But when you conciser the size, there is probably a lot of information to be found.
A wonderfull articles you have written here, I know a little bit about Etna when I was a master degre student and visited Etna in 2001. I have seen one unexpected eruption then I was in Sommitali crater, dangerous but stronger than a real thriller. Therefore, after your explaination, I now understand some detail better than in 2001.
A advised man staleness skin a move of revenge without tantalising foolery
Could the developer of this site contact me a.s.a.p - I may be able to help you out.