20 March 2009
I’m finally back from my first attempt at field work in the volcanic highlands of Guatemala, and reasonably alive – no thanks to being laid out flat halfway through the trip by a truly nasty case of food poisoning. There is a distinct disadvantage to doing field work in a developing country, and it’s never more apparent than when you’re so sick you can’t eat for three days. However, aside from a major restructuring of our plan of attack, we were able to collect enough data to keep me busy until the next trip.
The first thing I noticed? Guatemala is FULL of volcanoes. It’s almost impossible to live somewhere on the Pacific coast where you can’t see one. Flying in was incredible – peak after peak went by the window, all beautiful symmetrical cones (except for ‘my’ volcano, of course, but that will come up later). There are more than twenty-five volcanoes (depending on how you count domes), twenty-two that have been active in the Holocene and at least ten in historical times. The capital city has a lovely view of its own stratovolcano, Agua, and Volcáns Fuego, Pacaya and Santa María are currently active.
Guatemala is an interesting place. It’s a developing country, which means that the infrastructure that a lot of us take for granted is much reduced, or even lacking. The government of Guatemala is still struggling to throw off a truly staggering atmosphere of corruption, which also extends to the judicial system and anything meant for infrastructure upkeep. As a result, the country doesn’t have much in the way of sanitation, which means that the first thing you notice is a lot of trash, everywhere. It’s a bit startling until you realize that most people hardly see it anymore. Most people get places by walking, or riding chicken buses – so-called because it’s not unusual to see farm animals on board, along with everything else.
We mainly spent our time away from the capital (which is commonly referred to as Guate – confusing if you’re not sure whether the person is talking about the country or the city). The highland city of Quetzaltenango is about 150 km (or a 3-6 hour drive, depending on your route) away from Guate, and is also called Xela (pronounced Shay-la, short for Xelajú) after the old Mayan name. It’s a very popular place for gringoes to go and study Spanish, and has a charming central park (where I spent some time peoplewatching from a rooftop cafe). Parts of the city are actually quite beautiful – not very much of the actual old colonial architecture is left, since it gets destroyed by earthquakes every so often, but they’ve rebuilt in a sort of neo-Classical style here.
While we were in Xela, we were (lucky?) enough to feel some fairly large earthquakes – a M4.9 about 80 km south of the city, and a M5.3 off the coast south of Guatemala City. One more geological experience for me – being woken up in the middle of the night by the bed shaking!
Guatemala is unlike some other Central American countries (Costa Rica, for example) in that there are many more indigenous people still around, mainly in the highlands. Some of them have adopted the Westernized customs and dress of the Spanish-descended lowland populations, but many still wear traditional dress – mostly the women. They wear an amazing amount of color – in fact, I think they try to wear as much as possible at one time, with some truly eye-popping results. Women and children often carry loads on their heads – something I briefly tried in private, without much success – and it’s common to see a woman throw a folded cloth over her head instead of a hat. (These never fall off, and I couldn’t figure out why not.)
My research is centering around the lava dome complex of Santiaguito at the Volcán Santa María. The volcano and domes are just SW of Xela, in the middle of what are now coffee, banana and macadamia nut plantations (called fincas), and the whole lot sits at the head of several active river drainages that lead directly to the coast.
Santa María first erupted in 1902, creating a huge Plinian column, extensive ash and tephra falls, and blowing a large crater in the flank of the volcano. (Possibly some slumping was also involved, although I’m not entirely sure.) Twenty years later, the first of the Santiaguito lava domes (Caliente) began growing in the crater. The lava domes have been growing ever since, migrating westward with time and eventually returning to the Caliente dome for the last twenty or so years. There have been several major dome collapses (one in 1929 that killed thousands of people and destroyed a number of the coffee plantations that drape the slopes below the domes), and many lahars, some of which destroyed the town of El Palmar in the late 1980s.
There has not, however, been a major dome collapse (involving more than the 3 million cubic meters of the 1929 collapse). My research is focusing on determining the probability of that happening, where it might occur, and what the runout distance of the debris could be. It combines structure mapping, investigations into the hydrothermal system of the domes, and computer simulations, and I eventually hope to turn it all into a new hazard map of the volcano. On this trip we weren’t able to actually make it out to the domes, but I did get to spend a lot of time observing eruptions – something that happens every few hours at Caliente, the active dome. It’s pretty exciting, but also really scary at times, since it makes you realize just how close thousands of people – and you – are to a very active volcano.
Which brings me to a darker side of the work that I’m going to be doing. The populations of the fincas (coffee plantations) live in much the same way they did in 1929 – without paved roads, motorized vehicles, or much communication with people far beyond the local towns. There is probably no one left who remembers the ’29 event, and since nothing major has happened at the volcano since then, they have no way of conceiving of the magnitude of a major collapse event. Perhaps they understand the dangers, but what could they do to avoid them? There is no infrastructure that could initiate, organize or support a large-scale evacuation. Data from seismic stations and from the observatory is transmitted directly to the country’s geological survey, INSIVUMEH, in the capital, and it is by no means a large organization with the clout of, say, the USGS.
It’s a sobering thought. My work may help people in the future – in fact, I hope that it will help give the INSIVUMEH scientists the support they would need to convince people of the need for an evacuation – but it’s a very small chance. More likely is that a major dome collapse will someday happen, and people won’t be able to get away from it even if they have warning.
It’s a pity to end on a depressing note. In the next few posts I’ll talk a little bit about some of the thermal imaging we did with a FLIR (Forward-Looking InfraRed) camera, and show off more of the nifty images you see when you’re watching a volcano that erupts every few hours; I’ll also do a little tour of some of the areas below the volcano, and what happened there in the 20s and 80s.