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.

Labels: , , , ,

Monday, May 5, 2008

Tag Crowd for my C&O Canal geology book

I've got a first draft of a book about "Geology Along the C&O Canal" sitting on my computer, and I decided to feed that text into the "Tag Crowd" generator. Why? Because every other geology blogger on the face of the Earth is doing it today, and I don't want to be left out. Also because it's more fun than grading my 47th Billy Goat Trail geology paper...

created at TagCrowd.com

Labels: ,

Saturday, April 26, 2008

Darwin online

You no longer have to trek over to Cambridge University in order to sift through Charles Darwin's notes and papers. Now, it's all online, for anyone to access. The papers are all scanned in, so you can see his actual handwriting, sketches, etc. The image above, for instance, is the first written instance of Darwin's questioning the orthodoxy that species are stable (unchanging) entities over time. If species aren't stable over time, that means they can change over time, and those three words can be condensed into one word: evolution.

Also, NPR did a piece on the material being made web-accessible.

Labels: ,

Monday, April 14, 2008

World Mapper

Here's a cool website that shows different maps of the world based on different data.

For instance, countries scaled to their population sizes:

Or here's the number of preventable deaths per country:

Other keepers include fruit imports per country:

Build your own, or let me know if you find any other interesting ones...

Thanks to Anastassia for tipping me off on this one!

Labels: ,

Sunday, April 6, 2008

Northern Ireland geology website (BBC)

I just got an e-mail from Alan Watson, of Belfast, who read my article in Geotimes about geological travels in Northern Ireland. (This was one of my first topics on this blog, so newcomers may be interested in revisiting some of those old posts in the December and January archives.)

Anyhow, Alan clued me in to a new series from the BBC called "Blueprint," wherein they examine the natural history of the Emerald Isle. There's a cool interactive aspect to the website where you get a map of Ireland and a choice between "Plants/Animals," "Humans," and "Land." Choose "Land" and then select what you want to learn more about. Then you get a series of images, conversations, or videos about different aspects of Northern Ireland's geologic history. It's pretty cool -- there's a really enthusiastic dude (William Crawley) talking about the eruption of the Giant's Causeway, and also examinations of "the Chalk," graptolites, and granite gneiss. They even mention the Iapetus Ocean! (Which was a big focus of the field trip I led today!)

Labels: , , ,

Saturday, March 15, 2008

Unscrew yourself

Unscrew America artUnscrew America art (LED)What would it look like if Napolean Dynamite designed a website to promote energy conservation by switching out lightbulbs? Maybe something like the "Unscrew America" website. The navigation is a bit of a head-spinner, though. Take your Dramamine before you start moving that mouse around.

Labels: ,

Friday, February 29, 2008

Weirdness with a geologic name

On an odd day, a post about an odd place:

Reading David Byrne's blog last week, I was alerted to the existence of The Museum of Jurassic Technology in Los Angeles. When I went to this museum's website, I found a phantasmagoria of odd objects and pseudoscientific farce. It's not supposed to be real; it's supposed to be art. But... why "Jurassic?" Like a lot of McSweeney's works, it seems a little too clever for me to "get." Though not a geologist, Byrne seemed similarly perplexed: "the mixture of the real ... and the imaginary... is a bit of a head twister at first."

Labels: , ,

Wednesday, February 27, 2008

Svalbard's sea monster

National Geographic has an article online about a cool new fossil from Spitsbergen, Svalbard (the Arctic island achipelago belonging to Norway). It's a plesiosaur, a marine reptile from the Jurassic period of geologic time. The front flipper is almost ten feet (3 m) long! The online article includes a picture gallery (the site, the fossils, and National Geographic's beautiful reconstructions).

Labels: , ,

Wednesday, February 13, 2008

Google "My Maps"

A cool feature from Google Maps allows users to create individualized maps with content centered on specific locations. They call them "My Maps." This maps are then viewable in any HTML browser. Check out the "Earth As Art" demonstration map, or this "Oral Histories of Route 66" map for examples of the kind of stuff that you can do with "My Maps." You can also watch the video about how to create them.

It occurs to me that My Maps might be a good way to share geologic knowledge about outcrop locations. One thing that I found frustrating and limiting in my first few years of teaching was that there was no good single source to go to find out about relevant outcrops. It took time and experience to find out where the cool rocks were. Is it a good idea to put this information online in a publicly-accessible format so beginning instructors and interested students/amateurs can visit interesting outcrops? (I sure would have appreciated it four years ago!) Or does that run the risk of letting rockhounds and less-than-ethical geovandals onto previously-secret locations? Is there a benefit to the ancient barriers in outcrop-information flow? Is it better to pass this information on from wise elder to trusted neophyte?

Labels: , , , ,

Friday, January 25, 2008

New article up at Geotimes

Today my piece for Geotimes on geological travels in Northern Ireland went up on their website. You can check it out here.

Labels: ,

Sunday, January 20, 2008

Geology of Maine

The Maine Geological Survey maintains a terrific website with lots of information about the state's umpteen gazillion geological locales.

I feel like you could run a virtual field trip to Maine with the wealth of quality information and and images they have on this site. It's all well illustrated with lots of photos of structures and geologic contacts.

Learn more about the granite dikes at Pemaquid Point Lighthouse.

Or learn about where to find pillow basalts.

Or check out the giant purple crystals at Mount Apatite.

Or check out the distinctive dark feldspars of Maine's only "shonkinite".

It's all there, plus much, much more! Enjoy.

Labels: , ,

Wednesday, January 9, 2008

iTunes U?

I got an e-mail the other day from NOVA's VP for Instructional & Information Technology. He informed the faculty that later this month we'll have the option of putting our lectures & course materials up on iTunes, as part of something called iTunes U. Thomas Nelson Community College, another community college in Virginia, is already participating, as are a great many 4-year universities, including Ivy Leaguers.

I like this idea, but wonder how much time it's going to take. In general, I am super-duper excited over the advent of increased sharing online, and the decline of barriers to sharing. One of my pet peeves has been academic journals. Many are published by huge publishing companies like Elsevier, who make money off of them. For many years, scientists (and other scholars) who wanted to publish their research were forced to give up the copyright to their work and turn it over to one of these companies. Other scientists (or other scholars) who wanted to read about the research then had to pay OUTRAGEOUS subscription fees for these journals. I'm talking thousands of dollars a year -- far beyond the means of anyone who doesn't have a massive academic bureaucracy backing them up. To me, this seems massively unjust. It's the scientists who produce and consume the research; and publishing companies appear to make crazy profits off of all that stressful labor by others. ...Reminds me of slavery!

However, the Internet has the potential to change all that. With the net, anyone can publish their research online, and someone else on the other side of the world can access it 2 seconds later. With this, of course, comes the potential for lousy scholarship and fakery in research. At least that's the line touted by Elsevier and their ilk. Peer review is still essential, and it's going to be cool to see which journals get on board with the new reality. One I checked out recently is PLoS One. (They had a research article on really cool jellyfish fossils from the Cambrian, which is how I found out about them.) Somewhat more basic is the Journal of the Virtual Explorer, where my thesis advisor and some colleagues published an article (about kink banding) in 2004.

And while you're talking about the distribution of online information, it would be remiss not to mention Wikipedia. Wikipedia is HUGE among my students. I frequently use it myself as a handy reference. But handy doesn't mean accurate. Because anyone can edit the entries on Wikipedia, it's not guaranteed to be peer reviewed. A competitor, Citizendium, hopes to out-wiki Wikipedia with fully-refereed articles written by identifiable authors. WIRED explored their competing styles in their recent "Geekipedia."

More information about the iTunes U / online lecture phenomenon is available in a Washington Post article from the end of December.

Labels: , ,

Historical paleontology art at the Smithsonian

The Smithsonian's department of paleobiology has a webpage devoted to displaying some art that was used in some old scientific papers on fossils. There's a beautiful variety of images there, like this frontal view of a Triceratops skull that was used to prepare a lithograph, which then appeared in a paper by legendary paleontologist Othniel Charles Marsh (archnemesis of Edward Drinker Cope). Check out the full variety of art here.

Labels: , , ,

Monday, December 24, 2007

Astronomy picture of the day

The "Astronomy Picture of the Day" web site showcases a different image of the Cosmos every day. Nice! I've got it on my RSS feed, so everyday when I log into my Google account, I've got an image like this one greeting me. Clicking on the image takes you to a larger version and a more detailed description of the pic.
Here, for instance, is what they have to say about this shot: "Sprawling across hundreds of light-years, emission nebula IC 1396 mixes glowing cosmic gas and dark dust clouds. Stars are forming in this area, only about 3,000 light-years from Earth. This detailed view was created in light primarily emitted by hydrogen gas, recorded through a filter that narrowly transmits a wavelength characteristic of glowing hydrogen atoms in the nebula." Check it out!

Labels: ,