Friday, May 16, 2008

Volcano monitoring: last night's PGS meeting

Last night I attended my first meeting of the Potomac Geophysical Society (PGS). The PGS meets on Thursday nights, and I usually can't make it because I teach on Thursday nights. (I do however attend meetings of the Geological Society of Washington quite regularly, but those are on Wednesday nights.) Now that the semester is over, I was able to make it to the final PGS meeting of the spring.

The meeting was held at Fort Meyer Officer's Club. It's on a military base adjacent to Arlington National Cemetery, and before entering, my Prius had to be searched for bombs (as did all other civilian vehicles). The Officer's Club was about what you would expect, I guess -- kind of 1950's decor, elegant once. I noticed they had compact fluorescent light bulbs in all the sockets, which pleased me. PGS meetings consist of: (1) beer downstairs in the lounge, (2) dinner upstairs in the "Campaign Room," (3) business details, and (4) a talk by a guest speaker.

Last night's speaker was Bill Burton, from the USGS's volcano hazards and monitoring program. Bill's office will be launching a comprehensive new volcano website later this year, and he gave us a brief preview of its features in last night's talk. If you'd like a look for yourself, they have a beta version of the site online now.

Bill reviewed the efforts of his office to monitor a whole lot of volcanoes in U.S. territory (including the protectorate of the Mariana Islands). The map above shows how they've got their work cut out for them.

I was struck by two things about Bill's talk. First, that the volcanoes that the USGS has fully equipped with monitoring instruments (high-precision GPS, seismographs, etc.) provide a wealth of information which makes it relatively easy (relative to say, earthquakes) to predict eruptions. We've learned enough that we can use subtle signals to issue eruption watches and warnings, for both people on the ground and planes in the air.
But the second thing I noted is that they don't have every volcano in their area of responsibility fully instrumented. In fact, they don't even have every "dangerous" volcano in their areas fully instrumented. A striking example of this was a story Bill told while showing us this image:

That's Cleveland Volcano, one of the Aleutians. The photograph was taken by an astronaut, who then called the duty officer in the Alaska Volcano Observatory and told them "Cleveland's erupting." The AVO doesn't have instrumentation on Cleveland, so this phone call (from space!) was the first they knew about the eruption! That's a pretty big gaping hole in the program, it seems to me. We should know at the very least when our volcanoes are already erupting. Even better would be to fully instrument all our potentially-dangerous volcanoes to the fullest possible extent, so we can predict in advance when they will erupt.

At the end of the talk, I asked Bill about this: "How much more money would your office need to outfit the under-instrumented volcanoes to the level you think they need?" Bill estimated $80 million, both for installation and the constant upkeep these instruments require. This morning on the drive into work, I heard that the new farm bill has $450 million set aside for Chesapeake Bay environmental work, so while $80 million seems like a lot to me, I guess it's not all that much in the grand scheme of things. In a post this morning, Nicholas at The Critical Zone examined this issue of huge numbers, and all the science that could get done with that money.
In the wake of the recent tragedies in Myanmar and China, it seems like the US would be wise to invest some money in outfitting our volcanoes with the full suite of monitoring equipment. An ounce of prevention is worth a pound of cure. Who knows how many human lives an ounce of seismograph is worth? When a destructive eruption does happen, we're going to wish we had spent that $80 million when we had the chance.

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Friday, April 25, 2008

The map

Here's a photo of one of the cool things that my Honors students and I got to see on our recent trip up to Buffalo, New York (for the northeastern section meeting of GSA ):

That's an original, signed edition of the William Smith geologic map, brought to the meeting courtesy of the Buffalo Library. It is one of only two in the United States; the other is at the Library of Congress. The map found a home in Buffalo (of all places!) thanks to Chauncey Hamlin, the head of the Buffalo Museum of Science (then called the Buffalo Society of Natural Science) from 1920 to 1948. During his tenure, he assembled a collection of first editions of many seminal scientific works. First editions of Charles Lyell's Principles of Geology and Herbert Hoover's* translation of Agricola's De Re Metallica were also on display at the conference.

* Yes, that Herbert Hoover, at least according to Wikipedia.

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Thursday, April 3, 2008

Some more photos from the Buffalo trip

A few more photos from the Buffalo trip last week... All of these were taken by Victoria, my Honors student.

Here's some malachite in the sandstone of the Whirlpool Formation: the field trip leader suggested this was due to brine flow through these rocks during the Alleghanian ("Alleghenian") Orogeny:

malachite

Herringbone structure ("reverse cross bedding") in the Gasport Formation, overlying the DeCew Formation, which appears flat-lying and calm in this photo, but just below this shows disrupted bedding suggestive of seismic activity:

herringbone

I showcase a sample too big to lug back to the van (ripple marks):

rippleman

Watch where you stand! In the Niagara Gorge, we see some evidence that the Gorge is widening through mass wasting processes. Here's a small gap / scarp opening up as a block of rock to the right slumps down into the Gorge:

scarp

Lastly, on the trip home, we had an obligatory getting-stuck-in-the-mud moment:

mud1

mud2

mud3

Eventually, we got unstuck and headed back down the road!

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Friday, March 28, 2008

Silurian sequence stratigraphy trip

On Wednesday, two students and I participated in an excellent field trip examining the sequence stratigraphy of the Niagara region. We saw uppermost Ordovician rocks (the Queenston Formation) and then a dozen Silurian formations, some of them only 3 meters thick, stacked atop on another in a stereotypical layer cake fashion.

The trip was led by Carl Brett, who did a great job. I wanted to showcase here a few of the photos I took that day. Here's Carl showing us Arthophycus trace fossils (interpreted to be the burrows of polycheate worms):

arthophycus

At Outwater Park, we found fossil stromatoporoid reefs. Stromatoporoids were primitive, layered sponges. These ones show glacial striations across their surface, a result of the outcrop being scraped by glaciers during the recent Ice Ages:

striated_stromatoporoids

At another stop (on Lockport Junction Road) , there was a Leperditia ostracode-rich layer. Ostracodes are small arthopods, kind of like krill, but with bean-shaped shells.

ostracodes

At Pekin Hill, we looked at the Goat Island Formation, which showed ripped-up stromatoporoids deposited within it.

stromatoporoids_xsection

Here's a stromatoporoid that tumbled loose from the slope. I'm bringing this one back to Annandale to use as a teaching specimen. Note the upward-bulging dome of the stromatoporoid's internal layers.

stromatoporoid_sample

One of our most amazing stops was hiking up into the Niagara Gorge. This is at the downstream end of the Niagara Escarpment, where the Falls once were. The adjacent town is Lewiston.

artpark

Here's Laura and Victoria in the Gorge, overlooking the Niagara River:

gorge_girls

Now for some fossils from the Rochester Shale and other units exposed in the Gorge. Carl brought these out to show us what we might find. Here's a mouthwatering slab showing Dalmanites trilobites:

dalmanites

And a golf-ball sized cystoid (relative of crinoids, blastoids, and other echinoderms):

cystoid

He had some Lingula dwelling traces, too. Lingula is a common inarticulate brachiopod that dwells / dwelled in vertical burrows beneath the seafloor mud:

lingula_burrows

Here's a shot of a crinoidal grainstone. This limestone is almost entirely made up of "sand" generated by broken up crinoid skeletons:

crinoidal_grainstone

Some spectacular trace fossils (ichno-genus unknown) on a slab that was catching the rays of the sun just right:

traces

And a close-up of the same slab:

traces_closeup

And lastly, a nice slab showing tool marks:

toolmarks

It was really a great trip -- perfect weather, fascinating rocks, good company, and I felt nice and tired at the end of the day.

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Thursday, March 27, 2008

Sedimentary structure photos

On Tuesday afternoon, four students and I drove from Annandale, VA, up to Buffalo, NY, for the NE section meeting of the Geological Society of America. On the way, we crossed the Pennsylvanian Appalachians, and pulled over to examine some beautiful redbed exposures on the Pennsylvania Turnpike. I think these are in the Hampshire Formation, but I could easily be wrong about that, considering I've never been here before. Here's a few photos. First, some beautifully rhythmic alternations between sand and mud, now preserved as alternating layers of sandstone and mudstone:

layers

Then, some nice "ball and pillow" structures, as heavy sand sank downward into squishy mud. In places, the mud skooshes upward in "flames":

ball_and_pillow

And lastly and most amazingly (for me), some awesome exposures of flute casts. These are erosional scours into a layer of sediment by a current, which then fills in the scours (called "flutes") with sand, making these flute casts on the underside of the overlying layer of sand:

flute_casts

The flutes "point" upstream, and open up (and shallow) in the downstream direction. More later!

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Tuesday, March 25, 2008

Other samples from the ultramafics trip

Cool folds (in metamorphic foliation) in this sample:

isoclinal fold

Here's the real prize: a big chunk of peridotite (upper right) that's partly surrounded in a crinkly foliated matrix of chlorite schist (lower left):

ultramafic_annandale

I'm off to Buffalo, NY today with four Honors students to attend the northeastern section meeting of the Geological Society of America. If anyone from the geoblogosphere happens to be up there, I hope you'll say "howdy." Posting may be sporadic over the next few days... we'll see what the Internet connectivity issue is like up there.

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Tuesday, January 8, 2008

Northeastern GSA section meeting

The Northeastern section meeting of the Geological Society of America will be held March 27-29 in Buffalo, New York. I plan on attending it, and I can provide transportation for NOVA students up to the meeting and back. I think it would be awesome to get a whole van-full of people (Honors students and interested others) to take a little roadtrip up there and go to the meeting. The cost for students to attend the 3-day meeting is $45 if you are already a GSA member, or $55 if not. That's a great deal. Other costs: lodging and food. (I'm planning on staying in the hotel where the conference is being held, but there are undoubtedly cheaper options nearby...) I've reserved a NOVA van for us to drive up in, so transportation costs would potentially be zero.

I plan to go up one day "early" for the March 26 field trip to look at the rocks of the field trip: "Silurian - Early Devonian Sequence Stratigraphy, Events, and Paleoenvironments of the Niagara Peninsula Area of New York and Adjacent Ontario, Canada." (Full-day trip, Wed., 26 March. Cost is an additional $30 for students. Lunch provided. Participants must have passports to cross into Canada.)

More information on the meeting is here: http://www.geosociety.org/sectdiv/northe/08mtg/. If you are a NOVA student, let me know as soon as possible whether you want to go up for this meeting/trip. I think it'll be a lot of fun.

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