Monday, September 15, 2008

Caving in West Virginia

This weekend, I took 14 NOVA students caving in West Virginia. We hit three caves in the vicinity of Franklin, WV, on Saturday. On Sunday, we headed out towards Spruce Knob to experience two terrific caves: Stillhouse and the Sinks of Gandy. Here are some photos (and a video) of those last two caves.

Stillhouse Cave:

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The sinkhole out of which we crawled...
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Whose helmet is that emerging?
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It's Hope!
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A Cecropia caterpillar (according to What's That Bug?) that Tiffany found:caving7

Sinks of Gandy:

The crew poses at the entrance. Gandy Creek flows through the entire cave!
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Exiting into the light and trees and humidity and cows:
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Ricky Q, caver man extraordinaire:
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Video of the final watery exit from the Sinks:


I had a great time on this trip: felt like we all really bonded and had a fun adventure. Thanks to all the students who went and to the Student Activities counselor who co-led the trip with me, Jessie Zahorian! It was fun!

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Wednesday, August 27, 2008

NOVA Caving trip Sept 13-14

NOVA students: This is a reminder that I'm going to be leading a two-day caving trip through the Annandale campus' Office of Student Activities. The trip runs from 8am on Saturday, September 13 to about 7pm on Sunday, September 14. We'll be going to a series of caves near Franklin, West Virginia: Trout, New Trout, Hamilton, and Keys. We'll also drive out to the Spruce Knob area to take in Stillhouse Cave and the Sinks of Gandy (which has a river flowing through it). I've led this caving trip many times over the past 15 years; it's awesome. Last time I took students there was for a GMU GeoClub trip in Fall 2005. Some photos from that trip are available here.

There is space for about 15 students on the trip. The trip has a cost of $35, which covers all food except for Saturday's lunch (bring that in a bag). For dessert on Saturday night at the campground, I'll be fixing Grandma Bentley's famous peach cobbler. If you're interested in going, please contact Jessie Zahorian in the Office of Student Activities at 703-323-3484 or jzahorian [AT] nvcc.edu. First come, first served! Other denizens of the geoblogosphere: sorry, but it's only open to NOVA students.

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Friday, August 8, 2008

NOVA caving trip next month

NOVA students: I'm going to be leading a two-day caving trip through the Annandale campus' Office of Student Activities. The trip runs from 8am on Saturday, September 13 to about 7pm on Sunday, September 14. We'll be going to a series of caves near Franklin, West Virginia: Trout, New Trout, Hamilton, and Keys. We'll also drive out to the Spruce Knob area to take in Stillhouse Cave and the Sinks of Gandy (which has a river flowing through it). There is space for about 15 students on the trip. The trip has a cost of $35, which covers all food except for Saturday's lunch (bring that in a bag). For dessert on Saturday night at the campground, I'll be fixing Grandma Bentley's famous peach cobbler. If you're interested in going, please contact Jessie Zahorian in the Office of Student Activities at 703-323-3484 or jzahorian [AT] nvcc.edu. First come, first served! Other denizens of the geoblogosphere: sorry, but it's only open to NOVA students.

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Wednesday, August 6, 2008

Pictures from Mammoth Cave, Kentucky

Now that I'm back in DC, I can actually start downloading the photos I took all summer. Here's some from the first two days of my summer's travels, in Kentucky at Mammoth Cave.

There was a big cicada emergence happening there. This insect is 17 years old!
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Cicadas weren't the only wildlife. I also saw a Tyrannosaurus rex in the trees near Cave City.
Dinosaur!

On the Wild Cave tour, we entered Mammoth Cave in a roomy passage, but were soon crawling through very small tunnels...
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Caving attire: tres chic.
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Fossil coral weathering out of the roof of the cave...
Fossil coral in ceiling of cave

"Snowball" concretions on the ceiling of the Snowball Room, where there is a subterranean cafe. I had a bowl of soup and a Snickers bar from their extensive menu.
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The Snowball Cafe featured a bathroom, too. I was struck by the contrast between the modern tile and ceramic fixtures and the looming limestone ceiling...
Subterranean cafeteria bathroom

The group of folks (not one of whom I knew) after we got out of the cave and back into the sultry Kentucky summer air.
The group after our Wild Cave Tour

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Wednesday, June 11, 2008

Roadtrip update

Howdy folks,

I've been on the road for several days now, and thought it would be time for an update. On my first day, I got up at the crack of dawn and drove from DC out to Winchester, Virginia, where my brother lives, and had breakfast with him and his family. After saying goodbye to my passel of nieces, nephews, and the dogs Cubby and Slick, I hit the road proper. Down the Shenandoah Valley on I-81, then west on I-64 across the wide part of West Virginia. This was the Valley and Ridge province, and it's hell on the gas mileage. I dropped from 54 mpg to 53.5 by the time I got out the Allegheny Plateaus. I also saw the most expensive gas I've seen so far: $4.75 a gallon for regular unleaded. (The lowest I've seen is $3.78.)

After crossing the border into Kentucky, I deviated to the south, and around 8pm EST (7pm CST), I pulled into Mammoth Cave National Park. I got a campsite, set up the tent, and popped a bottle of homebrew. (I brought my last six bottles of Whatchagot Ale with me.) There was a racket coming from the trees: a 17-year cicada emergence was in progress, and the seething insects pulsated as they coordinated their shrill call: positively primordial. For my evening's entertainment, I attended the Park Service's "campfire" program. (Today, "campfire" means "PowerPoint slideshow," which has its advantages and its disadvantages.) It was a hot and humid night's sleep.

The next morning, I got up and made some coffee. After breaking camp, I took a hike down to the "River Styx," an emergent spring where a stream of water flows out of Mammoth Cave and into the Green River (the same Green River, by the way, of John Prine fame). I also passed one of the many entrances to the Mammoth Cave system, and felt an amazing cool breeze oozing out of the hole and flowing down a classic solution valley towards the Green River. At 10am, my tour of the cave began. Mammoth offers multiple tours of different parts of the cave at different activity levels. I signed up for the gnarliest one on offer: the so-called "Wild Cave" tour. (Tuff Cookie presciently recommended this to me, though I had in fact reserved it a couple of weeks ago.) The Wild Cave tour is different from most Mammoth tours because it's real caving, with crawling and mud and tight squeezes, and climbing skills. You've got to be reasonably fit and trim for the Wild Cave tour to work. Joining me where 11 other people with various backgrounds, including seven from the ESPN auto racing circuit. They had a fun, jocular attitude, with a lot of mutual joshing and teasing.

I was struck by a few things about Mammoth: (1) It's really big. But that's why we bother going there, and why it's a national park (it's the longest cave system in the world), so this is no big insight. (2) It's got a lot of gypsum in it. In many places, "flowers" of gypsum crystals sprout from the ceiling and walls. I asked, where's the sulfur coming from? The guides said there was a pyrite rich layer above, which was being leached by rainwater. (3) There's not a lot of stalactites in Mammoth. I've spent a lot of time in caves in West Virginia, and there are many places in them where it's nothing but stalactites. I'm not sure what's up with that, but it was noteworthy to me. (4) There are some HUGE rooms in Mammoth, with ceilings that are easily five or six stories tall. Very impressive; cathedral-like. (5) Mammoth Cave has been a tourist destination for a LONG time. People have been trekking to this destination long before there was a road network to bring them there. Back in the day (late 1700s and early 1800s), people arrived via the river rather than overland. Some of the cave was developed early on to support these visitors. Nowadays, the Park Service continues this tradition with paved walkways, lighting, and even a subterranean cafe in "sacrifice" areas of the cave. My tour passed in and out of these areas throughout our six-hour expedition.

After exiting the cool cave back into the Kentucky afternoon heat, I took a shower (the best $2 I've spent so far on the trip!) and popped into the Prius for some more driving. I headed north again, crossing briefly into Indiana, and then Illinois. I spent the night at a hotel near Mt. Vernon, Illinois. Yesterday morning, I got up and drove west all day, back on I-64 and then on I-70. I crossed the Mississippi River at St. Louis, and then crossed Missouri. Into Kansas after that: it wasn't nearly as flat as I remembered it. Part of the insight into Kansas' topography was courtesy of the Prius, which showed me (via the mpg indicator) when I was going uphill and down. A strong headwind lowered my fuel efficiency significantly, dropping it down to 52.7 mpg by day's end. There's a lot of wind out here! I was also struck by the clouds: such crazy, distinctive forms. I can see how if you were growing up here, you could get into meteorology big time. I saw a massive storm system to my south, and the local NPR affiliate was broadcasting storm warnings and tornado watches all afternoon.

I decided to stop for the night in Hays, Kansas, home of fellow geoblogger Ron Schott. As it turns out, Ron is not actually in town this week, but I may be able to hook up with him for some Kansas chalk scouting on my way back east in late July. But there's a lot to do in Hays. For dinner, I went to the Lb. Brewing Company, a craft brewery and brewpub downtown. I got a sampler of eight (small glasses) of their various beers, and enjoyed them all. Most unusual was a lemon beer which tasted a lot like lemonade. After dinner (reading Oceans of Kansas with my turkey panini), I watched another massive storm system pass to the north, with towering gray clouds and sporadic pulses of lightning. Wow.

This morning, I'm off for a run (need to stretch those legs!) and then to the Sternberg Museum of Natural History here in Hays (an affiliate of Ron's university, Fort Hays State University). The Sternberg has a reputation as having awesome fossils from the area's sedimentary strata laid down in the Western Interior Seaway. Looking forward to it.

Next stop: Denver, hopefully by 7pm so I can attend the "Geography Goes Digital" event at the Denver Museum of Nature and Science. More later...

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Thursday, March 6, 2008

Is the Grand Canyon 17 million years old?

The talented science writer Joel Achenbach has a piece on the Washington Post website about new research which suggests the Grand Canyon as an erosional feature is much older (~17 Ma) than we previously thought (~6 Ma). Achenbach's article is based on a study published in today's Science by Victor Polyak, Carol Hill, and Yemane Asmerom, of the University of New Mexico. These researchers* calculated the ages of cave mammillaries (rounded speleothems that form in caves near the water table) with U/Pb isotopic dating to infer when the water table had dropped in the past, implying a deep canyon.

* With all the talk in the geoblogosphere about death-defying geological research, it should be noted these folks were rappelling hundreds of feet down the canyon's cliffs to get to some of these caves...

Anyhow, dates from the calcite deposits suggest that the water table dropped more slowly (and hence the erosion rate must have been slower) in the western canyon than in the eastern section. The western part of the canyon yields inferred erosion rates of 55 to 123 m/Ma, while the eastern canyon's caves yield inferred rates of 166 to 411 m/Ma (about 3 times as fast). The authors interpret this to mean the Grand Canyon formed in two pieces: one started slowly propagating from the west, then another formed from the east (relatively rapidly working its way westward), and the two broke through and met in the middle, yielding the Canyon we know and love.

The photo above is a view from one of the sampled caves. [Photo is by Art Palmer, taken from the "Achenblog" site (Joel Achenbach's blog).]

Check out more details here. Or see the NYT's treatment here.

Main reference:
Victor Polyak, Carol Hill, and Yemane Asmerom, 7 March 2008. "Age and Evolution of the Grand Canyon Revealed by U-Pb Dating of Water Table-Type Speleothems." Science, Vol. 319. no. 5868, p. 1377 - 1380. DOI: 10.1126/science.1151248

Commentary in the same issue of Science:
Tim Atkinson and Mike Leeder. 7 March 2008. "Canyon Cutting on a Grand Time Scale." Science, Vol. 319, no. 5868, p.1343-1344. DOI: 10.1126/science.1155286

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Thursday, January 10, 2008

Blind cave fish can produce sighted offspring

An article in the current issue of Current Biology describes a fascinating experiment with profound results. Like the best science, the experiment is simple and elegant. Researchers took blind cave fish from two different cave systems and mated them. The offspring had fully functional eyes. It turns out that different parts of the developmental system had broken down in the eye-producing mechanisms of these two different fish populations. In essence, they represented two different evolutionary trajectories. Technically, a certain spot in the genes for making one part of the eye mutated in one population of cave fish, and another spot (or "locus") mutated in a second population. The fish were both blind, but they were blind for different reasons. What was wrong with one was right with the other, and by breeding them good genes cancelled out bad, at least in some of the offspring. The remarkable implication is that researchers produced sighted fish from two populations that hadn't seen in over a million years! It's a powerful confirmation of their independent origins in different cave systems -- basically a subterranean example of how evolution takes populations of organisms in different directions based on their own individual circumstances and histories.

A summary of the work is found at National Geographic's website, for those of you who don't subscribe to Current Biology.

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