Sunday, November 1, 2009

A piece of the rock

Here's an image of my new countertop, inaccurately described by the realtor as "granite":
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It's not felsic, so it can't really be granite, but I'm cool with that. This is the countertop of my kitchen "island" in the new condominium that I spent the past week moving into. For the first time in my life, I'm a homeowner...

...Whoa*.

That's why it's been so quiet around here recently. But... got the internet hooked up today, so I should be back to geoblogging regularly soon.
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* You'll recall that buying a home was one of my resolutions for this year.

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Thursday, October 15, 2009

Summer 2010 classes

I've just submitted a list of the classes I intend to teach for summer 2010. Here they are on NOVA Geoblog, before you can access them in the official Schedule of Classes...

GOL 135 (070N) The Bedrock Geology of Washington, DC. HYBRID COURSE: pre-trip reading, field study and post-trip report. One-day field trip Saturday, June 12. Rain date: Sunday, June 13. Important pre-trip logistical information and preparatory readings located online. This trip will focus on the land upon which the capital city is built, including exposures in Rock Creek Park, Georgetown, and Adams-Morgan. Includes discussion of oceanic sediments, the Rock Creek shear zone, igneous rocks emplaced during Appalachian mountain-building, Cretaceous river gravels, dinosaur bones and recent faulting. Students will be evaluated with a field trip report which will be completed after the trip itself. NOTE: This trip involves moderately strenuous hiking on forest trails. Meet in back of the CT building at 9:00 a.m.; Return by 7:00 p.m. For information about meeting time/place or other questions call (703) 323-3276 or email cbentley@nvcc.edu
HYBRID course
Additional info online

GOL 295 (4 credits) Regional Field Geology of the Northern Rocky Mountains: July 10 to July 25, 2009. Pre-trip meetings Wed. June 9 and Wed. June 23, 6:30pm, in CS 217. Western Montana and Wyoming showcase tectonic, sedimentary, geomorphic, and volcanic features which provide world-class examples of geologic processes. Students in this course will complete field studies of locations in Yellowstone and Glacier National Parks, as well as several other field sites. The course will involve VERY STRENUOUS outdoor physical activity: Students are expected to hike several miles at high elevations in rough mountainous terrain in order to accomplish course objectives. Airfare, lodging, and transportation are covered in the approx. $1400 course fee (does NOT include tuition). For up-to-date information and a complete itinerary, see the course website or contact the instructor at cbentley@nvcc.edu or (703) 323-3276.
Extra fee
Instructor permission required
Additional info online

GOL 299 (071N) (2 credits) Snowball Earth. June 14-19, 2009. HYBRID COURSE: pre-course reading, lab, field study and post-course report. An episode of glaciation 700 million years ago, dubbed Snowball Earth, may have provided for the evolution of multicellular life. The Snowball Earth glaciations stretch our conception of the limits of climate change: the ice apparently reached from the Earth's poles to its equator! Scientists infer that the runaway freezing event was only ended due to volcano-induced global warming. This course examines the geological, chemical, and biological evidence for Snowball Earth, and includes a field trip to local "Snowball" deposits. Course meets four times: three evening sessions (6pm-9pm) in CS 217 and all day on a Saturday (9am-5pm). The schedule is: Monday June 14 (lecture), Wednesday June 16 (lab), Friday June 18 (discussion), and Saturday June 19 (field trip). For further information call (703) 323-3276 or email cbentley@nvcc.edu or go to the course website.
HYBRID course
Additional info online

Anyone in the Northern Virginia area who's interested in any of these classes, drop me a line!

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Wednesday, October 14, 2009

Solar Decathalon

Every two years, the U.S. Department of Energy sponsors a competition called the solar decathalon on the National Mall in Washington, DC. Teams from universities around the country and across the world design low-cost, low-emissions, low-energy-use, architecturally pleasing homes, then bring them to the Mall to assemble them. For two consecutive weekends, folks like you and me can go and tour the innovative shelters. It's really an inspiring experience, and quite popular for that reason.

Here's some photos from last weekend. If you're in the DC area, the homes are open again this Thursday (tomorrow) through Sunday. You should check it out.

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Thursday, September 3, 2009

PSW: Maryland in the Miocene

PALEONTOLOGICAL SOCIETY OF WASHINGTON

Maryland in the Miocene: Paleoenvironmental History of the Calvert Cliffs
Susan Kidwell, Williams Rainey Harper Professor of Geology
Department of Geophysical Sciences, University of Chicago

Wednesday, Sept. 16, 2009
7:00 p.m., in the Cooper Room, National Museum of Natural History (10th St. and Constitution Ave. in NW Washington, DC)

Meet in the Constitution Avenue lobby at 5:00 p.m. if you wish to join the PSW members for dinner at the "Elephant and Castle," NW corner of 12th & Penna. Ave., NW

Non-Smithsonian visitors will be escorted to the Cooper Room at 6:30 and 6:55 p.m.

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Fall 2009 Walkingtown DC

The fall edition of Walkingtown, DC again features my walking tour of DC geology, "History Before History: the Geologic Saga of Washington, DC." It will be on Sunday, September 20, and is free (but reservations are required; sign up with Cultural Tourism DC, the sponsors of the event). Hope you can join us.

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Monday, August 31, 2009

A brush with unakite

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This is another photo from Saturday's hike. Unakite is rumored to be the 'state rock' of Virginia, though it's not in the state code. Regardless of its official status, it sure is a distinctive sight: An epidotized granitoid, unakite is identified by the distinctive pairing of pistachio-green epidote and pink potassium feldspar. There's some grey/purple quartz there too. In the mid-Atlantic states, it's only found in the Blue Ridge geologic province. Here, on the trail below Dark Hollow Falls in Shenandoah National Park, my friends and I encountered this lovely boulder of unakite bearing a vein of milky quartz.

The original granitoid was Grenvillian in age, about 1.1 billion years old. Presumably the metamorphism took place during Alleghanian mountain-building, between 300-250 million years ago. Unakite has been quarried in Virginia for use as a building stone, and can be seen as tiles on the first terrace of the steps leading from the National Mall up to the southern doors of the Smithsonian's National Museum of Natural History in Washington, DC.

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Tuesday, July 28, 2009

Climate Change at Cafe Scientifique

WHAT: Top Ten Things You Should Know About Climate Change

WHEN: Tuesday, August 4, 5:30-8:00 PM; program begins at 6:15 PM.

WHERE: The Front Page Restaurant, 4201 Wilson Blvd., Arlington, VA, Located near Ballston Metro on the ground floor of the NSF building. Parking is available under the NSF building or at Ballston Common Mall.

WHO: Keith Dixon, Research Meteorologist and Climate Modeler, NOAA's Geophysical Fluid Dynamics Laboratory, Joe Witte, Meteorologist, Newschannel 8

HOW: Special 1/2 price burgers start at 5:30 PM. Please come early to order table service and socialize. Short presentation begins at 6:15 PM, followed by Q&A. No science background required—only an interest!

Cafe Scientifique is free and open to the public. Register online here.

ABOUT THE TOPIC: In the coming decades, scientists expect climate change to have an increasing impact on human and natural systems. In a warmer world, accessibility to food, water, raw materials, and energy are likely to change. Climate change will also affect our weather, human health, biodiversity, economic stability, and national security. Come learn the top ten things you should know to know about climate change.

SUPPORT THIS CAFE: The Ballston Science and Technology Alliance, a nonprofit organization, is the sponsor of Cafe Scientifique Arlington. Since April 2006, the goal of Cafe Scientifique has been to make science more accessible and accountable by featuring speakers whose expertise spans the sciences and who can talk in plain English. Cafe is held each month on first Tuesdays at the Front Page in Arlington. Please go to www.arlingtonvirginiausa.com/bsta and contribute. Help keep Cafe open and free to all!

COMING NEXT MONTH: September 1, BioDiversity: How Special We Are! Dave Harrelson and Susan Jewel, Biologists, Endangered Species Program, U.S. Fish and Wildlife Service SPECIAL BSTA PROGRAM: August 25, 4:15 PM at Room 110 NSF, Climate Change Communication 2.0, Ed Maibach, Director of George Mason University's Center for Climate Change Communication. Register online here.

For more information contact Kaye Breen, ballstonscience@yahoo.com, visit www.arlingtonvirginiausa.com/bsta or join us on twitter: http://twitter.com/sciencecafeva or facebook: http://www.facebook.com/pages/Ballston-Science-and-Technology-Alliance/116954825970.

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Sunday, July 26, 2009

Ken Rasmussen takes on George Will

My colleague Ken Rasmussen (the other full-time geology professor at NOVA-Annandale) takes issue with George Will's most recent climate-change-denying column for the Washington Post.

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Friday, July 24, 2009

Geology of Washington, DC video

Student and amateur geologist Greg Willis put together this video instead of writing up the field trip report after June's field courses on the Billy Goat Trail and the Bedrock of D.C. I think it's pretty darned great. I hope you enjoy. Check out Greg's site for more fun stuff.

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Tuesday, July 21, 2009

Two items from this month's Smithsonian

There's an article on the Burgess Shale and another on inventorying all the plants on Plummers Island (home of the Plummers Island Thrust Fault, between DC and the Billy Goat Trail).

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Back in DC

Hey there everyone,

Sorry for the unconformity in my posting. Time has been passing, and events have been occurring, even if they haven't been recorded here. I'll try and compensate for that over the coming month.

My Rockies field trip went well. I think everyone had a good time, and there was clamoring for a similar regional field course next summer. I have some ideas for what that might look like, and undoubtedly I'll start planning that in the coming months. In the meantime, though, it's summer in DC, and time for a bit of R&R.

-CB

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Tuesday, June 16, 2009

A lucky meeting

On Saturday's Bedrock Geology of Washington, DC class, my students and I had the good fortune to stumble upon two geologists out doing field work: Tony Fleming, lead author of the geologic map of the Washington West quadrangle, and Steve Self, senior volcanologist with the Nuclear Regulatory Commission. They were out looking at the Sykesville Formation at Chain Bridge Flats, assessing a potential reinterpretation of the unit.

Fortunately, they were willing to take a little time and discuss their findings with the students. Here's a couple shots of Steve talking to the group:
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I joined Steve and Tony in the field yesterday (Monday) too, looking at some outcrops on the other side of the river, and trying to make sense of them. Fun stuff! More on that at a later date...

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Tuesday, June 9, 2009

Time warp dreams

As a high school student in Arlington County, Virginia, I used to take regular hikes down a path called Windy Run, and then walk along the south shore of the Potomac River, upstream. It was in the days before I knew anything about rocks, and I was mainly appreciating other aspects of nature, like the plant life, the birds, the bugs, the salamanders, and occasionally something really cool like a raccoon. But I was aware that the scene I observed and enjoyed was not the same scene that had always persisted.

I heard rumors from my uncle about patches of woods inside the DC Beltway that preserved virgin forest -- giant trees that gave a hint of the former majesty of this eastern hardwood forest. I read about an eastern herd of bison that would migrate north and south through the Piedmont and Coastal Plain, crossing the Potomac near Alexandria (before we killed them all). I noticed a gazillion deer, and had it explained to me that the lack of predators like cougars and wolves resulted in the herbivores' population explosion. We used to have elk here, but European colonists had extirpated them. The last of the bison were killed off by 1800, and the final elk met a bullet around 1850. This used to be a pretty wild place!

I observed trash nearly constantly, often mixed obscenely with natural debris, sheathed in mud, or woven into birds' nests. Every few minutes, a jet airplane on its approach to National Airport would thunder overhead. Those of us who lived in the flight path would learn to automatically put conversations on "pause" during the 30 seconds it took for the planes to pass. Visitors didn't know what to do about the noise; it was too pervasive to be ignored. But live here long enough, and you learned to ignore it. You adapted, like the birds adapted by putting aluminum foil and plastic bags into their nests.

And the river itself? It's gross. In the modern day, it's constantly muddy and silty, with a foul-smelling sewage/sediment biofilm all over the rocks and logs in the water. There's scummy flotsam and rumors that you'll get a rash if you swim in it. There's people fishing down by Teddy Roosevelt Island, and you have to wonder why... They're not going to eat the fish they catch out of this polluted stream, are they?

The theme of this month's Accretionary Wedge is "time warp." The Wedge is a geoblog 'carnival,' though it's been inactive for a while, this month sees its return to 'accreting.' For those of you who are new readers to NOVA Geoblog, it's probably a great opportunity to check out some of the dozens of other interesting geoblogs out there. So what does this have to do with my reflections on the local woods, and the Potomac River? This month's Wedge host is Lockwood from Outside the Interzone. He asked geobloggers, "Where and when would you most like to visit to witness and analyze an event in Earth's history?"

I'm going to use my time travel experience to go back in time right here, in Washington, DC. I want to go back to 1491*. I want to see what my home looked like before European settlers showed up and brought their particular brand of industrialization / civilization / land use changes / ecological perturbations to the Potomac River valley. It may surprise readers to learn that I'd opt for this -- a simple experience of pre-colonization North American nature -- over something tectonic and structural, but that's what calls to me on a deep, emotional level. I want to see a vibrant ecosystem with big trees. I want to see the water of the Potomac River look like water; I want to go swimming in it. I want to see what bird migration looked like before it dropped off so precipitously. I want to see a passenger pigeon, a carolina parakeet. I want to see for myself what a healthy amphibian population looks like. And bison fording the Potomac in Alexandria... perhaps emerging from the clear water with the autumn colors ablaze on the far side of the river? That would just be... awesome.

* Note that there's a good book by this same name, on this same theme, 1491. The book makes the case that there was already a lot of landscape/ecological modification playing out before Europeans arrived: that native Americans played a significant role in messing with natural systems and we shouldn't imagine an ecological paradise, just less of an ecological disaster.

Of course, going back to 1491 may have some negative aspects to it: there would be malaria endemic to DC at that time, and the native tribes might not take kindly to a time traveler popping in to ogle their forested homes. But I'll take those risks (they exist today in other places I've visited), since the pay-off would be such a profound deepening of perspective.

If I had the ability to go back in time, I'd use it to gain experience with pre-colonial North America. I'd check out the same river banks I would walk 500+ years later, and see what we've lost.

...And, once I've seen that former world, I can't guarantee that I'd come back.

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Monday, June 8, 2009

Ordering contest ANSWER

A couple of days ago, I asked for someone to tell me the geologic history of this boulder, in correct chronological order. To make it easier, I labeled the relevant rock units with letters. I promised that the first person to post the correct sequence of events in the comments would win a GEOLOGY ROCKS bumper sticker.

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From first to last, the correct sequence of events is X, D, R, M, F.

Thomas Donlon got it right! Congratulations, Thomas -- I'll mail you a bumper sticker.

So let's delve into more detail: what actually happened with this rock?

First, a mafic source rock was weathered, generating chunks of rock "X." Then those clasts were mixed in with a bunch of sand and mud to generate the graywacke that makes up most of the boulder. This was later metamorphosed (not shown with a letter) to generate rock "D." Later, rock "D" with inclusions of "X" was split open, and granitic magma intruded into that fracture to make the dike labeled as "R." Later still, another cross-cutting event took place, cutting across everything that had come so far, to generate the vein of milky (hydrothermal) quartz labeled as "M." Finally, these rocks were uplifted and exposed, and various fractures, including "F," liberated this boulder from its source area. Now it is free, adrift on the Chain Bridge Flats, and posing for geologists. The final event was me discovering and gracing it with a quarter before snapping its portrait.

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Saturday, June 6, 2009

Ordering exercise: CONTEST

Inspired to give those Californians a run for their money with their cool examples of relative dating exercises, I took this photo last week down at Chain Bridge Flats, the westernmost corner of Washington, DC:

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Your assignment, should you choose to accept it: tell me the geologic history of this boulder, in correct chronological order. To make it easier for you, I've labeled the relevant rock units with letters here. (The letters were chosen randomly, and do not by their alphabetic nature imply any sort of order. Note that "F" is the fracture surface defining the planar outer edge of the boulder.) First person to post the correct sequence of events in the comments area below wins a GEOLOGY ROCKS bumper sticker.

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Answer in a couple of days. Good luck!

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Tuesday, June 2, 2009

Walkingtown, DC photos

Here's a few shots from Sunday's "History before history: The geologic saga of Washington, DC" tour for Walkingtown, DC. We had ~forty people show up; I was glad to have the NOVA Geology megaphone system so I could broadcast to a crowd that size.

Thanks to Michelle Arsenault (NSF) for playing caboose to our group (and taking these photos), and to Laura Moore (volunteer for Cultural Tourism DC) for keeping us safely out of the road.

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Classic "subduction" arm pose:
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Pondering garnets in the Laurel Formation:
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(note the cyclist above, running the gauntlet of interested geologists!)

Checking out the Clydesdale Fault:
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What's up with this limestone? Why is it gray higher than about seven feet or so?
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And the lovely quarry where we can see the various members of the Georgetown Intrusive Suite (arm-waving to indicate boudinage):
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Friday, May 29, 2009

Soapstone Valley, DC

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I've been meaning to go check out the Soapstone Valley for years, but finally got around to it on Memorial Day. The park is a valley that shoots off to the east from Rock Creek Park, with an eastern terminus at Connecticut Avenue:



I didn't have far to walk before I found my first cobble of soapstone. It felt soapy in my hand, and was easily scratched by my fingernail. (Fingernail = 2.5 on the Mohs scale of hardness; talc = 1) I found it interesting that the soapstone cobbles had less algae growing on them than the other cobbles in the stream... Hmm. Because they slough off their outer layers more easily? Or because there's something chemical going on that prevents algae growth?
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Why does anyone care about soapstone? Well, people who care about prehistory are interested in soapstone because it was easily carved to make various artifacts. As a geologist, I'm more interested in it because it's a metamorphic rock that implies an ultramafic protolith. In other words, as the various rocks that would become DC's bedrock were squished and squeezed and heated during Taconian mountain-building, one of the ingredients in the mix may have been a peridotite. As the graywacke around it metamorphosed to metagraywacke, the putative peridotite metamorphosed into soapstone.

The stuff I found in Soapstone Valley is a talc schist with porphyroblasts or relict phenocrysts of something dark and chunky in it:
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Here's a close-up. The big crystals were dark green, like augite, but they had a texture that looked more like hornblende. Not sure as to their identity. I'll put one under the microscope later to try and suss out the relationship between the cleavage planes.
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They're definitely mafic though! Here's an example where the large crystals are rusted out:
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So there was plenty of soapstone float, but no bedrock outcrops. At first, I was in the highly foliated metagraywacke schist of the Rock Creek Shear Zone...
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...but as I headed upstream I found boulders of the Kensington Tonalite, implying exposures of the KT further up the valley...
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... and sure enough, that's what I found. This is the Kensington Tonalite, a late Ordovician granitoid.
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Where I first crossed the contact, I thought it looked a little odd, and then a later look at the geologic map of the Washington West quadrangle (Fleming, et al., 1995):
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Fleming, et al., list it as a sheared biotite tonalite of the Georgetown Intrusive Suite, which I guess explains its appearance as distinct from the Kensington Tonalite.

When I got up to the eastern edge of the park, I saw the source of the stream:
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The valley widens out here, almost as if the rock is weaker... And where concrete has been poured (to stabilize the slope??) the underlying rock is etched away: it's the super-soft soapstone...
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Here's a boulder of soapstone (my fingernail scratches it to demonstrate that it's soft):
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Here's the geologic map of the area. You can see Soapstone Valley cutting an east-west swath across the strike of the structures. ("ss" means "soapstone"...)

My annotations on Tony Fleming's map (reference below).

Reference:
Geologic map of the Washington west quadrangle, District of Columbia, Montgomery and Prince Georges Counties, Maryland, and Arlington and Fairfax Counties, Virginia. Anthony H. Fleming, Lucy McCartan, and Avery Ala Drake. U.S. Geological Survey (Reston, VA), 1995.
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A quick tangent to note a milestone: this is my 700th post on NOVA Geoblog. Thanks to everyone for reading. Looking forward to 700 more...

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Sunday, May 24, 2009

Osprey flies over field area

Last week, I was geologizing down at the Chain Bridge area (far western corner of DC), and this Osprey aircraft flew over. A few minutes later, I heard it returning, and I shot this little video. What a weird looking airplane!

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Tuesday, May 19, 2009

NAGT field trip photos

Whew!

Sorry I haven't posted much here in the past week. I've been swamped.

The good news is that my biggest task is now off my plate (just turned in the first draft of my MSSE capstone to my advisor), and that means I've got some spare attention left for the blog.

I thought I would take the opportunity to share some images from this past weekend's NAGT (National Association of Geoscience Teachers) Eastern Section conference, held at the NOVA Loudoun campus. On Saturday, I led a version of my "Bedrock Geology of Washington, DC" trip for a group of eight conference attendees.

All these photos are from Randy Newcomer, Director of Training and Services for Complete Safety Solutions of Lititz, Pennsylvania, and are posted with his permission... and my annotations!

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If you're interested in seeing (most of) these rocks, join next Sunday's Walkingtown, DC tour!

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Sunday, May 10, 2009

Walkingtown, DC announcement

Just a heads-up for DC-area readers: The spring 'edition' of Walkingtown, DC is coming up, and once again I'll be leading my "History Before History" tour. This three-hour walking tour of Adams-Morgan, the Zoo, and Rock Creek Park covers the geologic saga which formed the bedrock of the nation's capital city. We'll look at the Rock Creek Shear Zone, Cretaceous-aged river gravels, a faulted unconformity, and the Georgetown Intrusive Suite. It's free and open to the public. More information is on the Walkingtown website. Please join us!

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Sunday, April 26, 2009

BCNH

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That's a black-crowned night heron I saw on a little post-coffee, pre-work walk in Rock Creek Park the other day.

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Monday, April 13, 2009

Bonnie Bassler talk at Carnegie

Bonnie Bassler, whose TED talk I featured here on Sunday, will be speaking Thursday evening at the Carnegie Institution in northwest DC, as part of their "Capitol Science" lecture series. As in the TED talk, she will be discussing "Cell-to-Cell Communication in Bacteria." The talk begins at 6:45pm. Enjoy!
Hat tip to Diego H. for letting me know about this!

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Friday, April 10, 2009

Ptygmatic folding in a granite dike

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Ptygmatic folding is a style of folding characterized by an "intestine-like" appearance. The folded item (in this case, a granite dike) folds back on itself, and the cross-cut material (in this case, a schist) flows out of the way. In other words, there's a viscosity contrast between the relatively-stiff granite dike and the relatively-weak schist.

This particular ptygmatically-folded dike is in a boulder outside of the National Museum of the American Indian, in Washington, DC. That's a quarter at the top of the photo, for scale.

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Tuesday, March 31, 2009

Cherry tree + great blue heron

A shot from DC's Tidal Basin this weekend:
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Tuesday, March 24, 2009

Boom! tomorrow in DC

Passing on some excitement:

For the filming of a TV pilot, there will be a simulated explosion on Wednesday, March 25 between 9:30 a.m. (tomorrow morning) and noon near Key Bridge in the District.

The explosion will produce a 20 to 30' fireball that will last for approximately 2 minutes.

Please pass along this information to others appropriate. The Department of Homeland Security and D.C. Police and Fire departments have been notified, along with the Washington Airports Authority. The Virginia State Patrol and Arlington Police Department will be contacted. If you have additional questions, contact Kathy Hollinger or Burt Warner with the DC Film Office at 202-727-6608.

The explosion will take place on the Potomac River just north of the Key Bridge and Jack's Boathouse (K / Water Street, NW under the Whitehurst Freeway). In the scene to be filmed, there will be six (6) sculling boats on the Potomac River and one of them blows up. CBS Paramount television is filming a pilot titled "Washington Field." This is a new television series about the elite Washington field office of the FBI and a team of agents with exceptional and diverse skills who are called together for only the most critical cases.

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Tuesday, March 17, 2009

Lil' Rockhounds

Tuesday, March 10, 2009

Mike Kaas on the Silver Hill Mine

Sorry for the late notice... this is for today at lunchtime.

The Sliver Hill mine:
America's First Silver Mine and Supplier of Lead to the Confederacy

L. Michael Kaas

Abstract: The Silver Hill Mine in Davidson County, North Carolina was the first important underground silver mine in America. Discovered in 1838, it produced significant quantities of silver and lead into the mid-1840's. As the oxidized ores were depleted, abundant, rich, lead-zinc sulfide ores were encountered. These complex primary ores presented the mine operators with difficult metallurgical problems. Mine development and production slowed. Nearly a decade passed as the owners experimented with new processing and smelting technologies. These efforts were largely unsuccessful and the mine closed in the early 1850's. The Civil War created an urgent need for lead to supply Southern troops. The Confederate government operated the Silver Hill Mine to provide an alternate source of lead in case the mines at Austinville, Virginia should fall into Northern hands. Lead concentrates with high silver values were shipped from Silver Hill to the newly constructed Confederate smelter in Petersburg, Virginia. After the War, the mine continued to operate for several years but the problems of the refractory sulfide ores were not solved and the mine closed again. For more than a century after production stopped, the Silver Hill Mine was the repeated target of both mining companies and stock promoters.

Where: Pier 7 Restaurant, 650 Water Street, SW, Washington, DC (within walking distance of the Waterfront Metro on the Green Line) Free parking with validation from Pier 7 Restaurant.

11:30 - Social 12:00 - Lunch 12:30 - Speaker

Meeting cost: $20.00 for Washington, DC Section SME members $25.00 for non-members

Contact Steve Stokowski with questions

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Saturday, March 7, 2009

Revelle lecture announced

The National Academies' Ocean Studies Board would like to announce that Dr. Paul G. Falkowski, Board of Governors' Professor at Rutgers University, will be the speaker for the tenth annual Roger Revelle Commemorative Lecture, scheduled for Tuesday, March 17, 2009 at 5:30pm. It will be held in the Baird Auditorium in the Smithsonian's National Museum of Natural History (10th Street and Constitution Avenue). Dr. Falkowski's talk is entitled:

The Once and Future Ocean

The ocean has been a feature of Earth's surface for at least 4 of the past 4.5 billion years, and has provided the primary environment for the evolution of microbes that drive the biogeochemical cycles on Earth. Over this long period of time, the ocean has witnessed extreme changes, ranging from complete coverage with ice to extensive periods when there was no ice at all; periods of extraordinary extinction of animal life, to periods of dramatic evolutionary radiation of animals. Throughout all of Earth's history, the ocean has served as the primary backbone of life on the planet; and the core metabolic processes have been successfully transferred across vast stretches of geological time. Humans, in contrast, evolved only about 200,000 years ago, and in that short period of time have come to successfully outcompete and plunder many of Earth's living resources. Over the past 100 years, in particular, we have increasingly altered the trophic structure of the ocean as well as its physical circulation and chemical properties. While human impacts will surely alter ecosystem functions the core metabolism of the ocean will go on. Rather, ironically, humans are the fragile species that will lose capabilities of using the ocean as a source of food and novel molecules. Our future is intimately tied to that of the ocean. We have to begin viewing the oceans as a key component of the Earth system; one that we cannot live without.

This event is free and open to the public. For planning purposes, please complete this brief registration form. You are encouraged to post the event flyer or to forward it to your colleagues. For more information, contact Pamela Lewis.

Please visit Roger Revelle Lecture Series for information on Roger Revelle and on previous lectures.

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Wednesday, February 18, 2009

Saprolitic dikes in my 'hood

Walking to my car the other day, I looked up at the embankment on my street, and noticed some geology there I hadn't seen before. Yesterday, with my camera, I climbed up the embankment (~15 feet) to investigate. Fortunately there were some trees to hold onto.

Sure enough, it was as I suspected: dikes of granite (subvertical in orientation) that, along with the schistose bedrock they cut across, had totally weathered to saprolite.

Keys for scale:
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Originally, these dikes were emplaced during the late-Ordovician eastern-North American episode of mountain-building called the Taconian ("Taconic") Orogeny. Later, when they got exposed at the surface (or close to it) they began to "rot."

Hand for scale:
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Here's a video showing how readily these dikes formerly known as granite deform by crumbling into pieces:



The main chemical weathering process that has happened here to make this possible is the hydrolysis of feldspar to produce kaolinite, a clay mineral. Large single crystals of potassium feldspar in the granite are now large amorphous masses of kaolinite, which has no strength when stressed.

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Wednesday, February 11, 2009

2/18 PSW meeting

PALEONTOLOGICAL SOCIETY OF WASHINGTON

Institutional Memories: The Paleo Art of National Geographic and the Smithsonian Institution
by Angela Botzer (National Geographic) and Mary Parrish (Scientific Illustrator, Dept. of Paleobiology, National Museum of Natural History, Smithsonian Institution)

Paleo art has been an important part of the dissemination of the science of paleontology for two important Washington, DC institutions and their audiences for more than 150 years. The presenters will detail fascinating histories of paleo art via the material housed in the collections of their respective organizations.

Wednesday, Feb. 18, 2009
7:00 p.m., in the Cooper Room, National Museum of Natural History
10th St. & Constitution Ave. Meet in the Constitution Avenue lobby at 5:00 p.m. if you wish to join some fun paleontologists for dinner, at the "Elephant and Castle," NW corner of 12th & Penna. Ave., NW. Non-Smithsonian visitors will be escorted to the Cooper Room at 6:30 and 6:55 p.m.

Remaining Dates for 2008-2009 Season: March 18, April 15, May 13

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Bird guide for the iPhone

Coyote Crossing alerted me to this awesome-looking application for the iPhone: a field guide to the birds of North America. On my way back home to the apartment last night, I parked my car in Mt. Pleasant and was walking up the hill to my building, when I saw two of my neighbors pointing a flashlight into the woods (yes, we have woods in DC). "What have you got?" I asked. It was an owl, and they obligingly pointed it out to me. I identified it as a barred owl, and explained the field marks that would allow them to distinguish it from our other big eastern owl, the great horned owl. As we talked, the barred owl flushed and silently swooped through the tree branches and into the darkness. Anyhow, if my neighbors had the iBird Explorer Plus, they wouldn't have needed to rely on an ex-ornithologist walking by at that moment. Pretty cool!

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Wednesday, February 4, 2009

"We are all Smith Islanders"

Because he's coming to campus tomorrow (Thursday), last weekend I watched Mike Tidwell's movie We are all Smith Islanders. It's a 35-minute long documentary about how climate change is effecting the states of Maryland and Virginia, and the District of Columbia. Though it is a political document (and not a scientific documentary), I think it's a worthwhile enterprise because it connects the global to the local. We hear a lot about climate change, but when someone actually walks through Ocean City, Maryland, pointing out what three feet of sea level rise would look like, it fosters a connection based on shared landmarks.

Thanks to archive.org, you can actually watch the movie in low resolution on the Internet. Google video also keeps a copy available.

Or, if you'd prefer it in higher resolution (on DVD), you can find it at the NOVA library.

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Wednesday, January 28, 2009

Snow in DC

Yesterday was our first big snowfall (well, "big" by DC standards) of the year. We got around 3 inches total, but then last night that got covered and compacted by a layer of freezing rain. Here's the scene yesterday morning around 8am from my apartment, looking west over Beach Drive, Rock Creek Park, and the National Zoo (movie is 30 seconds long):




The College was open, though, so in we all trooped. Here's the campus as viewed from Little River Turnpike:

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And a few shots of the snow-laden campus...
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The snow continued into the afternoon, with predictions of freezing rain for the evening. I had my Physical Geology class, but then the word came down from on high* that NOVA would be closing at 2pm. So, no lab, and no Environmental Geology. We all trooped home to our various classes.

* NOVA has put together an impressive new emergency alert system. It automatically sends e-mails, sends text messages to our cell phones, and (as I found out yesterday in the middle of my Physical Geology lecture) causes a window to open up on all campus computers saying "ALERT: The College will be closing today at 2pm due to snow." I was in the middle of a PowerPoint slide showing why weak bonding in mineral crystal lattices cause cleavage, and BAM suddenly there was a flashing alert up on the screen. Instantaneous notification for the entire class. Another one was open on my computer when I got back to my office. Pretty effective, I think.

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Wednesday, January 21, 2009

A hike in Rock Creek Park

The day before Inauguration, I decided to celebrate George Bush's last day in charge of my country by taking a walk in the woods. Okay... that wasn't really my motivation. I was just procrastinating writing up my Structural Geology labs for the coming semester. Anyhow, for one reason or another, I took a stroll in the woods.

I brought my rootin' tootin' new camera with me, and took a few photos. I've got four things to show you: (1) some differential weathering, (2) some kink banding, (3) some cool effects in frozen soil, and (4) a critter.

(1) To start, check out this close-up photo of a stone bridge where the Klingle Valley merges with the Rock Creek Valley:
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Several of the (local) stones used in the bridge are weathering at a faster rate than the mortar (cement) that holds them together. As a result of this differential erosion, the less-stable rocks are recessed into the face of the bridge:

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Here's another one, where you can see that not all minerals are equally stable at Earth surface conditions. The large central quartz augen stands out in high relief as the micaceous & feldspathic schist around it weathers away.

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Yet another: recessed about an inch into the bridge:

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That's not all I saw. I also re-discovered the location of some kink bands along the Rock Creek Park bike path:

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These kink bands are similar to the ones that Spring 2008 Honors student Victoria measured and analyzed in Broad Branch (also in Rock Creek Park), but these ones are in a different location, further south in the park.

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What's worth noting about these kink bands is that they overprint the regional foliation of these schistose rocks. In order to do that, the force that generated the foliation must have been coming from one direction (call it east-west), causing the mineral grains to line up at right-angles to that stress. That allignment is what we call foliation. Later, a new generation of deformation came in from a different direction (call it north-south, approximately parallel to the foliation), kinking the pre-existing foliation. For more on kink bands in DC, see my "DC rocks" page.

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(4) One of the disadvantages to hiking in Rock Creek Park in the winter is that it's pretty monochromatic. One of the advantages is that with all the leaves off the trees, it's a lot easier to see new stuff. It's great woodpecker-watching weather, for instance. I saw five woodpeckers of two species that day. Also, it makes it a lot easier to see where the trails are. I saw a new trail that I had never walked before, and so I decided to check it out. I'm glad I did. One thing that I saw that is pretty cool is this effect in frozen soil:

rc_hike_01_19_0908

When water freezes, it expands in volume by about 9%, and that shows up here as the upper layer of wet soil froze, it expanded in all directions, pulling away uniformly from two large cobbles of quartzite. It almost makes it look like the quartzite cobbles shrunk in their "sockets," but really it's the "sockets" that got larger.

(4) Lastly, I was doubly glad to have taken the new trail because it was a "road less travelled" kind of deal. I was the only one there. As I trod along, suddenly I heard a scampering noise. It was a critter! It ran up a little gully and then paused as still as a stump, looking at me:

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Can't see it? Try this zoomed-in shot:

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It's a red fox! Vulpes vulpes, one of two wild canids we have in Rock Creek Park. Pretty good sighting -- only the fourth time I've seen one here (and I spend a lot of time in this park). And every one of those times was in the winter. Again, it's having those clean leaf-less views that allows hikers to see stuff like this.

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Inauguration photo... from space

Those aren't insects swarming all over the ground: those are people!
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From the GeoEye satellite, via Google Earth, via the Google Earth blog.

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Tuesday, January 20, 2009

Live photos from the Inauguration


I'm hosting a couple of Obama campaign workers this week, giving them a free futon as an expression of gratitude for their work on the campaign. One of them, Laura D., is uploading images and short twitteresque updates from the Mall at zannel.com.

Check it out for the latest from the action downtown!

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Obama motorcade

Here's the view from my apartment yesterday (the day before Inauguration):



Happy Inauguration, everyone!

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Sunday, January 18, 2009

D.C. area energy consumption down 2%

According to a study by the Washington Post, our area's electricity consumption dropped by a small but perceptible amount in the first nine months of 2008, as compared to 2007. The article linked to above describes the sources of data as being a mix of home audits in Arlington County, Virginia (40 out of 89,000 total), government figures for the number of miles driven on local roads, and utility billing information. Overall, the Post estimates a 2% reduction for the study period in 2008 as compared to the previous year. Now, the question is, Why? By their reckoning, it's likely to be a mix of increased consciousness of "green" energy practices, increased use of compact fluorescent light bulbs, and perhaps most importantly: mild weather.

One thing I can say about that lattermost factor: this year, 2009, is so far not really of the "mild weather" variety. It's dang cold here!

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Monday, January 12, 2009

Back, safe and sound

Just a quick note to say: I'm back!

I left Quito this morning at 10am, and just got back to my apartment in DC around 8pm. Feels good to be back home. I had a fun trip, and I'll tell you all about it, but probably not 'til the semester gets underway. First classes are at noon tomorrow!

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Friday, December 19, 2008

GeoCorps position at CUE

Students! What will you do next summer? I've done some work with the good folks at the Center for Urban Ecology in DC, which works with the national parks in the National Captial Region. I was notified today that they're in search of a GeoCorps participant to complete a paleontological inventory of the area's parks.

Could be fun! The relevant info is below, or you can see it all on the GeoCorps site.

Public Land Name: Center for Urban Ecology, National Capital Region, National Park Service
Position Title: Geosciences Research Assistant / Paleontologist
Position ID Number: 208
Location: Washington, DC
Position Description: The work of the GeoCorps participant will build upon a paleontological inventory of the National Capital Region’s parks conducted in 2004 which revealed remarkable assemblages containing vertebrate, invertebrate, and plant fossils distributed in four distinct physiographic regions. The participant will conduct paleontological resource site condition assessments, complete documentation, and help establish a monitoring program for fossil sites in the Chesapeake and Ohio Canal National Historic Park (MD, DC), Manassas National Battlefield (VA), and National Capital Parks-East (MD, DC). The position will include both office and field work. Most of the time will be spent conducting field paleontological surveys to fully document localities and to undertake site condition assessments. Site visits will be conducted by vehicle and on foot. While working in the field, the participant will ensure that NPS regulations and safety procedures are being followed. Office duties will include reviewing literature, preparing documentation for entering into NPS databases, building a photographic library, and drafting recommendations for site monitoring. Participants may have an option to use a portion of their time for self-directed research after approval from regional and park staff. Prior to starting this position a government security background clearance will be required. This position is offered through the Geological Society of America's GeoCorps America Program in partnership with the National Park Service's Geoscientists-in-the-Parks Program.
Qualifications: Undergraduate/graduate coursework and/or field experience in paleontology, with preference given to knowledge of the Mid-Atlantic region. Applicant must have completed at least three years of college-level coursework. Graduates students, faculty, and active and retired professionals are also welcome to apply. Experience in the field, discovery and evaluation of paleontological resources, particularly trace fossils, is important. The applicant should be able to work well independently, both in the office and in the field, have basic map reading and GPS skills, and must be comfortable both working outdoors and negotiating a busy city. Basic computer skills are required. Applicant must have a valid driver’s license and a good driving record.
Position Dates: 12 weeks with flexible starting dates in April-May
Payment: $2,750.00
Housing Available: Housing will be provided at no cost to the participant most likely at Brookmont House (George Washington Memorial Parkway) in Washington, D.C. This is a 3-bedroom house shared with up to two other people. There is public transportation available but grocery shopping and other services are limited in this area, so having a personal vehicle is highly recommended.
Physical/Natural
Environment:
Parks of the National Capital Region (NCR) encompass numerous sites ranging in size from less than one to over six thousand hectares that provide a diversity of experiences and landscapes. The 15 national parks of the National Capital Region lie within four physiographic provinces: Coastal Plain, Piedmont, Blue Ridge, and Ridge and Valley, and contain significant geological resources. These parks include areas with national icons (the National Mall), national battlefields (Antietam, Manassas, Monocacy, Harpers Ferry), and natural forests (Catoctin Mountain Park and Prince William Forest Park), all amidst the rapidly growing metropolitan Washington, D.C. This unique setting provides great opportunities to gain insights into issues related to urban ecology and integrated management of cultural and natural resources.
Work Environment: The Center for Urban Ecology (CUE) houses the Natural Resources and Science Division, which is an interdisciplinary team that provides scientific guidance, technical assistance, and education for the preservation and enhancement of park resources in the National Capital Region, National Park Service. Working with resource managers, researchers, and the public, CUE strives to discover and incorporate new ways to understand, preserve, and enhance natural communities within and around the national parks in the metropolitan Washington, D.C. area. CUE is located in the Georgetown area of Washington, DC, in a Rock Creek Park facility. Laboratories at CUE are fully equipped to support research in botany, plant health (pathology), entomology, hydrology, aquatic biology, soils, and wildlife biology.
# of current Applicants: 0

If you have questions about the application and selection process, please contact Anny Jones. If you have questions about any aspect of the position - description, qualifications, housing, dates - please contact the primary or secondary contact below:

PRIMARY CONTACT INFORMATION
Contact Name: Giselle Mora-Bourgeois
Title: Science Education Coordinator
Address: 4598 MacArthur Blvd, NW
City/State/Zip: Washington, DC 20007
Phone: 202-342-1443 Ext 220
Email: Giselle_Mora-Bourgeois@nps.gov
Website: http://www.nps.gov/cue/
SECONDARY CONTACT INFORMATION
Contact Name: Vincent L. Santucci
Title: Chief Ranger
Address: George Washington Memorial Parkway
Turkey Run Park
City/State/Zip: McLean, VA 22101
Phone: (703) 289-2531
Email: vincent_santucci@nps.gov
Website: http://www.nps.gov/gwmp/

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Thursday, December 18, 2008

Giant map of DC

Check this out: planners of next month's inauguration are using a giant map to figure all the logistics out.

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Wednesday, November 19, 2008

Watch the fall foliage change...

...from my apartment window!

Here's a series of photographs I've taken over the last month and a half to document the change in the leaves on the trees. I'm a big fan of repeat photography to document changes like these.

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Maybe I'll do the reverse of this project in the spring to watch it greening up again...

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Thursday, November 13, 2008

Red ink

It's that time of the semester, when the field trips are over, and the field trip essays start rolling in. These papers I assign are intended to be syntheses of the field trips I take my students on. I want them to interpret the landscape as a geologist would, and support each claim about geologic events in the past with supporting evidence observed or discussed on the trip.

I offer my students the opportunity to submit a rough draft of their field trip paper, and then I give them feedback about both content and formatting/writing style, so they have a chance to revise before submitting a final draft. Each semester, about a quarter of the students avail themselves of this opportunity for feedback before the "real" paper is due. Giving them quality feedback is a time-consuming process, but I feel it's important both to cement geologic concepts in their minds, and to guide them in developing their writing skills.

Accordingly, it's been a slow week for posting on this blog. I've been too busy with work. However, this morning it occurred to me that I could capitalize on my grading efforts by sharing a student essay with you all, edits and all. Why do I think you'll be interested in such a thing? (A) I think it gives some insight into the practice of teaching geology at the introductory college level, and (B) I think this is an excellent rough draft for an essay about Washington, DC's geologic history. The student's name, of course, has been redacted:

essay_1001
essay_2001
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Tuesday, November 4, 2008

Vote: cast!

8:30am: Just got back from voting. As with 4 years ago, the line stretched around the block: awesome to see so many of my neighbors and fellow citizens participating. It gave me the warm fuzzies.

Today's the day, people! Let's make it happen.

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Saturday, November 1, 2008

Recent field trips

Last week was field trip week for me. I led trips to the Billy Goat Trail on Tuesday and Thursday, and to Washington, DC, on Saturday.

On the Physical Geology field trip to the Billy Goat Trail, we saw rocks like amphibolite, metagraywacke, and migmatite:







Hope and Ana checking out the migmatite:


The group poses with the migmatite, to show how close anatexis is to their hearts...


Jane examines lamprophyre in a weathered-out dike:


Noting the characteristics of metagraywacke:




Traversing 'Pothole Alley'... Joel looks chilly...


Our lunch spot... Alex pretends to dive into the Potomac River...


Traversing 'The Traverse':


On the Historical Geology field trip to DC on Saturday, we were amused to find a jack-o-lantern that had facial hair resembling mine...



But that's not all! We also saw some geology. While you can get a more complete picture at my "DC Rocks" webpage, I'll post a few new photos of new outcrops here...

Here's a nice slab of granite (very angular) set in metagraywacke matrix (metamorphosed accretionary wedge complex)...
DC_FT_2008_1

Here's two members of the Georgetown Intrusive Suite, showing the (earlier) gabbro stoping xenoliths into the (later) granite:
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I love field trips. I love seeing my students light up at being outside, at getting a handle on the stuff we talk about all semester in class. I think field trips are super duper important.

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The rock that I hate

As a geologist, I love most rocks I encounter. But yesterday morning, I went out to my car and saw this:

car (2)

Can you tell what's missing? Hint: here it is, all over the front seats:

car (3)

My car had been broken into over night. Bummer. I live in the city, so this happens sometimes in the city, but I've learned never to leave anything of value in the car, and certainly never to leave anything of value in plain view. The people who broke into my car last night must therefore be classed as vandals, not thieves, since they didn't steal anything. Grrr...

Then, in the course of calling the insurance company, I opened up the driver's side door, and saw this:

car (1)

See the rock there, between the driver's seat and the driver's door? That rock came through the passenger window, from the other side of the car, with enough force to slam into the other side of the vehicle. And it left its mark on the panel on the interior of the driver's door:

car

So, the poor little Prius is now in the shop, getting a new door panel and a new window. Major bummer. And now I know that there is at least one rock in this world that I do not like.

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Monday, October 27, 2008

Sunset imagery

Here's some recent sunset photos. Sunsets are one of my favorite natural phenomena. I love how beautiful they are.

One from my apartment window, with the National Cathedral to the right:
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One from my car, driving back from a friend's farm a couple weeks ago (pear-gathering expedition):
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Video from the same post-pear-pre-prandial peregrination:


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Sunday, October 12, 2008

Bridge mystery revealed!

Yesterday I noted that there's an interesting pattern to be seen as one crosses DC's Duke Ellington Bridge:

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After sharing these photos yesterday, I posed question for you: What's up with the coloration of these exposures? Why are they black on top and white on bottom? It's the same rock (Indiana limestone), so why the difference in color?

The answer has two parts. First, the calcite (calcium carbonate) which comprises the limestone is sitting out there in the air, and is subject to rain and what-not. Some of that rain has sulfuric acid in it, and that dilute sulfuric acid reacts with the calcite, producing a thin layer of gypsum (calcium sulfate). Those itty-bitty crystals of gypsum have bladed habits, and those bladed crystals are really good at trapping soot and dust. So while the calcite underneath isn't as effective as a soot-trap, the thin layer of chemically-altered gypsum on the surface of the blocks rapidly accumulates dark-colored particulate matter.

So that explains the dark color, but what about the lighter-colored lower portions? Is it simply that they aren't exposed to as much acid rain? Perhaps because they're further down on the "outcrop"? Nope... though that's clearly a consideration (note the thin white vertical lines below some of the stars), it wouldn't explain the abrupt transition from dark colored above to light-colored below. So: what gives?

It's here that context plays an important role. This is an urban location, an outcrop in the city. Like many flat surfaces in the city, it's subject to being tagged with graffiti. Periodically, the City sends along a crew to power-wash the bridge's graffitied surfaces. When they do this, they strip away not only the spray-paint, but also the gypsum and its trapped soot! Because graffiti artists can only reach so high, the city only power-washes so high, and the upper portion of the bridge "outcrop" is both unmolested by graffiti and uncleaned by the City. It records a continual accumulation of gypsum and soot, but the lower portion has its proverbial slate cyclically wiped clean!

I'm on a field trip this weekend (I wrote this post on Thursday and set it to publish while I was away), so I don't know who won the prize (a "GEOLOGY ROCKS" bumper sticker!) but as soon as I get back, I'll settle up with the clever winner. In advance, I'll congratulate you: Nice job!

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Saturday, October 11, 2008

Geo-Mystery on the Duke Ellington Bridge

To walk from the Woodley Park neighborhood of DC to my neighborhood (Adams-Morgan), you have to cross the deep gorge of the Rock Creek Valley. To do this, walk east on Calvert Street over the Duke Ellington Bridge.

Here's something you might notice as you walk over the bridge:

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My question for you: What's up with the coloration of these exposures? Why are they black on top and white on bottom? It's the same rock (Indiana limestone), so why the difference in color?

First person to post the correct answer in the comments section below gets a "GEOLOGY ROCKS" bumper sticker as a reward. Full answers tomorrow in a separate post...

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Friday, October 10, 2008

A lurid sunset

This was the view from my apartment window last night:

lurid_sunset

(That's the National Cathedral on the right.)

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Wednesday, October 8, 2008

Upcoming lectures at the Carnegie

Capital Science Lectures upcoming at the Carnegie Institution in northwest DC:

Thursday 10/16/2008 - 6:45pm
Cooperation and Collective Behavior, from Bacteria to the Global Commons
Simon Levin, Princeton University,
Department of Ecology and Evolutionary Biology, Center for BioComplexity
A sustainable future for humanity will require finding a way to share our complex environment. Learn about the evolution of cooperation in non-human populations, and what must change in our own behaviors if we are to have a common future.

Wednesday 11/12/2008 - 6:45pm
Geysers of the Solar System
Susan Kieffer, University of Illinois at Urbana-Champaign,
Center for Advanced Studies, Department of Geology

What would Old Faithful look like if it erupted on Io, the hot moon of Jupiter, or on Enceladus, the frigid moon of Saturn? What can the towering geysers on Io and Enceladus tell us about the interiors of these moons?

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Monday, October 6, 2008

Upcoming talks

Here's two events you might be interested in, if you live in the DC area and are into the Earth sciences...

1) I'll be giving next week's Science Seminar at NOVA Annandale. I'll be discussing my geological experiences out west this summer in a talk called "Two Months of Rock and Road." It starts at 12noon on Friday, October 17 in the CE Building Forum, and will conclude by 1pm. Light refreshments served starting at 11:45am. Free and open to the public.

2) American Meteorological Society Environmental Science Seminar Series: "Ecosystem Health in a Climatically-Altered World: Is 'Species Rescue' Part of the Prognosis for the Future?" by Dr. Camille Parmesan, University of Texas, Austin, Texas. Friday, October 10, 2008; New Time - 10:00 AM - 12:00 PM, in the Russell Senate Office Building, Room 253 Washington, DC. Free and open to the public.

What sorts of climate-related and compound stresses are various wild ecosystems encountering? What impact are these stresses having on these various ecosystems? How might one characterize the resilience, or lack thereof, of these ecosystems to these stresses. For those with the capacity to do so, how are ecosystems adapting to changes brought about by climate change and other stresses such as development? What is happening to those ecosystems that are showing signs of being incapable of either adapting in place or moving elsewhere? How do the rates of climate change and other stresses affect the odds that certain ecosystems will adjust and ultimately, survive? Are there ecosystems that now require, or will require, special human interventions in order to prevent their collapse and/or demise? What would these interventions look like and are they governed by existing national policy?

Buffet Reception Following; More information online at http://www.ametsoc.org/seminar

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Monday, September 29, 2008

Joel Achenbach on the new Ocean Hall

Joel Achenbach reports in today's Washington Post about the Smithsonian Institution's newest addition: the Sant Ocean Hall, which opened this weekend at the National Museum of Natural History. I plan to go check it out myself this week, but until I get the chance to report, consider Mr. Achenbach's words.

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Thursday, September 25, 2008

Old, old rock


This just in! The New York Times reports that a rock from Quebec may be the new title-holder in the "Oldest Rock On Earth" competition, unseating its fellow countryrock, the Acasta Gneiss of the Northwest Territories. In a study today in Science, Rick Carlson of the Carnegie Institution of Washington (a local boy!) and colleagues report a 4.28 Ga date for the rock (which appears to be a gneiss, though the article didn't say for sure, and I can't yet access the original paper). More after I read the original article by Carlson, et al. ...

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Monday, September 22, 2008

GSW reminder

Geological Society of Washington
Meeting 1424
Wednesday, September 24, 2008

Sarah Penniston-Dorland, University of Maryland, College Park - "Multiple sulfur isotopes reveal a magmatic origin for the Platreef PGE deposit, Bushveld Complex, South Africa"

Callan Bentley (me!), Northern Virginia Community College - "Rise of the geoblogosphere"

Matthew Jackson, Department of Terrestrial Magnetism (Carnegie Institution) - "The fate of subducted continental crust in the Earth's mantle"

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Refreshments start at 7:30 p.m. The formal program starts at 8:00 p.m.
Free and open to the public.

Meetings are held at the John Wesley Powell Auditorium (go in via the fenced-in parking lot on the corner of Florida Ave and Massachusetts Ave, NW) of the Cosmos Club, 2170 Florida Avenue NW, Washington, D.C.

GSW Web Site address: http://www.gswweb.org/
Future meetings: Oct. 22, Nov.12, and Dec. 10

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Cougars in Virginia?

CNN reports on cougar sightings in the town of Blackstone, Virginia, a bit southwest of Richmond. The official line goes that since mountain lions (Felis concolor) were wiped out along the eastern seaboard in the early 1900s, they haven't been found anywhere except for a relict population in the Florida Everglades (where they are called "panthers"). But this one little town in the Virginia Piedmont has had more than the average number of sightings. I think it would be great if mountain lions reestablished themselves in the hills of the Old Dominion. Our deer population is out of control, and while it's unsettling to not be at the top of the food chain, ecosystem coherence takes a higher priority in my mind. Along similar lines, in 2004 it was reported that coyotes had moved back into Rock Creek Park, the large national park that runs through the heart of northwest Washington, DC. Park officials have suggested they wouldn't be surprised if black bears moved back in too.

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Sunday, September 21, 2008

Georgetown Intrusive Suite

I led my "History Before History: The Geologic Saga of Washington, DC" tour twice this weekend as part of the twice-annual "Walkingtown, DC" weekend. The folks attending the tour both days were really cool, and were full of good questions. We covered the sedimentary origins of DC's rocks at the bottom of the Iapetus Ocean, their metamorphosis during Taconian mountain building, the intrusion of plutonic rocks, the erosion of those ancient mountains, the deposition of river gravels during the Cretaceous (together producing an unconformity), and the faulting of that unconformity sometime post-Cretaceous (probably Miocene). I'm kind of tired after all that geologic history, especially repeated twice in two days!

georgetown_boulder

The photo above is of a boulder in Rock Creek Park showing all three members of the Georgetown Intrusive Suite, a series of igneous plutons that were intruded into the crust during late-Ordovician mountain-building. I like this boulder because it illustrates well two of the principles of relative dating: the gabbro must be older than the diorite, because there are xenoliths of the gabbro in the diorite (inclusions). You can't break off a piece of gabbro unless it already exists. The granite dike must be younger than the diorite, because it cuts across the diorite (cross-cutting relationships). You can't crack open diorite unless it already exists.

Just thought I'd share an informative little outcrop like this. Please ignore the white graffiti that mars the central part of the exposure. A pen at the top is circled to give a sense of scale.

I hope everyone had a relaxing weekend!

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Thursday, September 11, 2008

New Hall of Oceans at the Smithsonian

Just a few weeks left until the National Museum of Natural History (Smithsonian Institution) opens the doors of its new Ocean Hall to the public (Saturday morning, September 27). I'm particularly excited that it contains an exhibit on ancient seas, including a Basilosaurus skeleton!

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Thursday, August 14, 2008

Upcoming events in DC geology

Fellow DC metro area residents -- there are a bunch of geology events coming up in the next couple of months that you may be interested in. Everything* listed here is free and open to the public.

Next Sunday, August 24, I'll be leading an event called "Geology Along the C&O Canal," at the Lock 8 River Center from 10am until 11am. My plan is to give an overview of the Appalachian mountain belt, then focus on the Piedmont "chapter" of that story, using local outcrops to illustrate the rock types produced. I'm not sure if you need to reserve a spot or not; Call Bridget Chapin at the Potomac Conservancy (number at link above) to inquire about details.

Friday, September 5: "Geology Along the Billy Goat Trail," I'll lead this hike along the famous Billy Goat Trail, examining its exquisite display of metamorphic geology and geomorphology. 12:30pm-4:30pm. Reserve a spot through the good folks at the Great Falls Tavern Visitor Center.

Wednesday, September 10: first Geological Society of Washington meeting of the fall. Beer served at 7:30pm, and the formal program begins at 8pm. At the Cosmos Club in Dupont Circle.

Saturday, September 20: I'll be leading my "History Before History: the Geologic Saga of Washington, DC" walking tour as part of Walkingtown, DC. The tour runs from 1pm until about 4pm, and involves about 2.5 miles of walking from Adams-Morgan to Georgetown. Limit of 30 people; interested walkers should reserve a spot with Cultural Tourism, DC, the nonprofit group that sponsors Walkingtown, DC each spring and fall.

Sunday, September 21: For those who can't make it Saturday, I'll again be leading my "History Before History: the Geologic Saga of Washington, DC" walking tour as part of Walkingtown, DC. The tour runs from 1pm until about 4pm, and involves about 2.5 miles of walking from Adams-Morgan to Georgetown. Limit of 30 people; interested walkers should reserve a spot with Cultural Tourism, DC, the nonprofit group that sponsors Walkingtown, DC each spring and fall.

Wednesday, September 24: Another Geological Society of Washington meeting, but I'll be delivering a talk at this one. My talk's title is "Rise of the geoblogosphere."

Sunday, October 5: I'll be delivering a talk called "A Geologist's Perspective on Climate Change" at the Chinn Park Regional Library in Woodbridge, Virginia. 2pm-3pm.

Friday & Saturday, October 10-11: The Virginia Geological Field Conference, in Marion, VA. "Geology of the Saltville and Pulaski Fault Blocks" is this year's topic. *This is the one item on the list that is not in the immediate DC metro area, and also the one item on the list that costs money -- registration is $45 for professionals, $20 for students. Transportation, lunch, and guidebook will be provided. See more details on the website. If you're interested in comparing and contrasting two Valley and Ridge fault blocks shoved westward during Alleghenian mountain-building, this might be of interest to you.

Thursday, October 23: the Earth's birthday, according to James Ussher. 4004 BC to 2008 AD; does that make it 6012 years old? Or is it 6011 years old, since there was no year "0"? Tricky... Regardless, I'll be serving lithosphere/asthenosphere cake/pudding to NOVA students in celebration of the day. (I posted on visiting Archbishop Ussher's church here.)

Wednesday, October 22: Another GSW meeting. Same time, same place, but this time I'll be back where I belong: in the audience.

Friday, October 24: "Geology Along the Billy Goat Trail," I'll lead this hike along the infamous Billy Goat Trail, examining its exquisite display of metamorphic geology and geomorphology. 12:30pm-4:30pm. Reserve a spot through the good folks at the Great Falls Tavern Visitor Center.

If you're into geology and you'll be around, I hope you'll join us on one or more of these events.

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Tuesday, August 12, 2008

Some great unconformities

This summer, I saw "the Great Unconformity" in a couple of locations.

An unconformity is a break in the local geologic record -- a period of time which elapsed without being recorded by the deposition of rock units. Often unconformities mark places where erosion has erased part of the local rock record, but sometimes they just mark periods of non-deposition. (Analogy: You can get a blank page in your diary two ways. You can either take a day off from writing, or you can write that day's entry and then later go back and erase it. Either way, you end up with a day going by and no journal entry.) People call the major break between metamorphic and igneous "basement" rocks and overlying sedimentary layers the "Great" Unconformity, though it's not the same age everywhere. It's just shorthand, really.

Anyhow, here it is in the Grand Canyon (photos provided below are both unadorned and annotated versions):

unconformity_01

unconformity_02

Give or take, there's about 1.2 billion years missing along this ancient erosional surface. Intuitively, this probably makes sense, since metamorphic rocks like schist and 'distilled' intrusive rocks like granite are characteristics of mountain belts, where they form at depth. In order to get those interior-mountain-belt rocks to the surface takes lots of erosion over lots of time (though not necessarily that long -- in DC, for instance, we have interior-mountain-belt rocks exposed that 'only' took 360 million years to make it to the surface). In the above photos, the metamorphic rocks and granites below the unconformity formed about 1.7 billion years ago, during the Mazatzal Orogeny, and the sedimentary layers on top (both quartz sandstones) were deposited in the Cambrian period, about 543-488 million years ago. They represent passive margin sedimentation along an ancient transgressive seashore, something like modern day beach sands along the east coast of North America. So, to get something like the Great Unconformity, take something like coastal Maine (Acadia National Park, say), and bury it beneath something like Virginia Beach.

And here "it" is again, in Wyoming's Wind River Canyon (between Thermopolis and Shoshoni):

unconformity_03

unconformity_04

A zoomed-in look at this same outcrop:

unconformity_05

unconformity_06

This time, however, the rocks below the unconformity are much older* metamorphics (schist & amphibolite) and granite. According to Maughan (1987), these are the oldest rocks exposed in Wyoming, having formed about 2.9 billion years ago. They were then metamorphosed at 2.75 billion years ago. These truely ancient rocks (Archean) were then eroded and exposed at the surface, where quartz-rich sand was laid down atop their burnished roots. Aside from the difference in the age of the underlying basement rocks, the story is very similar to the one at the Grand Canyon.

* Thanks very much to Kim, who pointed out my error in under-stating their age in an earlier, more-poorly-researched version of this post.

Reference:
Maughan, E.K. (1987) "Wind River Canyon, Wyoming." In: Geological Society of America Centennial Field Guide - Rocky Mountain Section. S.S. Buess, ed. p. 191196.

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Monday, May 26, 2008

Audubon geology class goes to DC

Yesterday, I took my Audubon Society / USDA Grad School "Natural History Field Studies" students on a field trip to examine the bedrock geology of Washington, DC. We had a good time: beautiful weather, great attitudes, and even luck with parking! I guess because it's Memorial Day weekend, a lot of people have left town. One of the great challenges of urban geologizing is finding room for those infernal cars...

Here's a photo of the group at Chain Bridge, DC, on Sunday morning:

NHFS_chain_bridge

That class ends on Monday night, bridging the gap between my NOVA spring and summer semesters. It's been a good run -- thanks, folks!

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Friday, May 16, 2008

Scary map du jour

This map was in this morning's Washington Post. The red dots are currently-existing coal-fired power plants. The black dots with the central stars are proposed future coal-fired power plants.
Coal is relatively cheap energy, but it's got some signficant environmental problems associated with it (the accompanying article was about reduced air quality in national parks like Shenandoah). Another recent Washington Post article investigated the effects of mountaintop-removal methods of getting at the coal out in neighboring West Virginia.
More significant than the air quality issue to me is the lunacy of investing more in fossil fuel infrastructure. We should be moving away from these old, dirty technologies, not entrenching ourselves in them. Burning coal generates CO2. The writing is on the wall in regards to the effect of this anthropogenic CO2 on our planetary climate system. But the vast majority of DC's energy comes from coal. Enter the hypocrite: I'm bummed that every time I post to this blog, I'm using electricity that adds carbon to the atmosphere. And if this map is prophetic, it looks like it's going to stay that way for some time to come.

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Wednesday, May 14, 2008

The Palisades Museum of Prehistory

This is how good it is to be a professor on summer break: Yesterday afternoon, after composing yesterday morning's epic account of my Massanutten trip, I toodled on over to the Palisades Museum of Prehistory to (a) drink beer and (b) talk rocks with the museum's curator, Doug Dupin.

The Palisades Museum of Prehistory is in far western Northwest DC, near the Dalecarlia Reservoir and Sibley Hospital. There, you'll find a neighborhood called the Palisades, and in the Palisades, you'll find Doug Dupin's house. In Doug's backyard, you'll find what appears to be a nice shed. Turns out, this is the museum. It's a long story, but basically it boils down to this: Doug was a cartographer, but a contract went sour, and so he was staying at home with a lot of time on his hands. He decided to grow some grapes to make wine, and store that wine in a self-dug wine cellar. He started digging the hole, and encountered arrowheads, pot sherds, and other artifacts. He got intrigued, and decided to showcase the findings atop the wine cellar in a self-made museum.

If you want more details, the Washington DC CityPaper profiled Doug in a 2006 article. A good read; I recommend it.

Doug is a great guy -- pursues what he's interested in, be it homebrew, viniculture, skateboarding (he once rode the length of the C&O Canal on a self-made board -- read about it in this New York Times Magazine article), or archaeology.

Doug attended my "Walkingtown, DC" walking tour of DC's geologic history, and brought along a few odd rocks for me to identify. At the end of the tour, he invited me over to see his museum. Yesterday, I finally got the chance to do that. We cracked open a couple bottles of Dogfish Head 60-minute IPA and started browsing his collection of found prehistoric objects. Doug was very interested in my analysis of rock types (apparently archaeologists use a different set of terminology for describing what rock types projectile points are made out of).

On his own property and in neighboring areas of the Palisades, Doug has found hundreds and hundreds of objects, many of them beautifully worked arrowheads of flint, quartzite, and rhyolite. There are also some oddballs that don't fit with the human prehistory theme: a 1791 coin bearing the image of Louis XVI, crystals of amethyst and gypsum, old glass bottles, rounded river cobbles, and anything else that caught his attention. One of the most astounding things I saw yesterday was a huge woolly mammoth tooth. Doug told me a friend of his found it in the Potomac River while canoing (I think he said near Seneca Creek, but that was a beer and a half in, so maybe I've got that wrong). But there it was, a fully ridged mammoth molar; unmistakable. I hadn't heard of previous mammoth finds in our area, but I guess it's not surprising they were here.

Anyhow, I had a great time, and I recommend that everyone in the DC area make an appointment with Doug to go check out his collection and support his project.

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Monday, May 12, 2008

Rain, rain

Latest gage information from the Potomac River near Little Falls. Looking out my window at Rock Creek this morning, I can see the water is way up, moving fast, and the color of teh tarik.

DC (and many other surrounding municipalities) are under flood warnings this morning as a result. The Washington Post's Capital Weather Gang is impressed by it all.

(Fortunately Saturday's field trip happened to be scheduled between downpours.)

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Sunday, May 11, 2008

Pangea day - DC bedrock

Morning, folks. I awake to a challenge from Chris at GoodSchist, to show where my local bedrock was at the time of Pangea's incipient breakup. (I think Chris chose the late Triassic, 220 Ma, since Ron Blakely's map of that time shows New Zealand clearly in the south.) It's an interesting time for the rock beneath Washington, DC. After have just experienced ~50 million years of crunching between North America and Africa, DC's tortured bedrock is now being stretched as Africa begins to pull away again. A series of rift valleys mark the stretching of the crust, shown clearly in the map as a series of NE-SW oriented lakes along the axis of the Appalachian orogen.

DC's future location is between two of those rift valley lakes: one to the east, one to the west. If I owned DC real estate during the Triassic, I'd be very interested in this process, because one of those rift valleys is going to become a new ocean basin, and one isn't. The one that isn't is destined to stop opening and fill in with dirt. It will be a failed rift valley, an aulacogen of sorts.

The question is: which one is the weakest link? If the one to the west breaks open, that will be the new Atlantic Ocean basin, and DC will stay hitched to Africa. If the one to the east breaks open, that will be the site of the Atlantic, and DC will stay hitched to North America.

As it turned out, the eastern rift was the one that connected up with other rifts to the northeast and southwest, and became the young Atlantic. The western rift, known as the Culpeper Basin, stopped stretching open, and got filled in with sediment. DC stayed attached to North America, and that's the way it is.

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Tuesday, May 6, 2008

Earthquake in NOVA / DC area : UPDATED

Three-quarters of the way through my Physical Geology final exam this afternoon, the room shook and a low rumble propagated through our building. The students, many of whom were in the area on 9/11, instantly looked up with a very concerned "Was that a bomb?" look on their faces. To assuage their fears, and because I've previously heard similar rumbles coming from our HVAC ducts, I told them that it was just the cooling system, and not to worry.

Turns out I was wrong: it was a small earthquake with an epicenter about 1 km from here (we're about 1 km west of Annandale proper, and the USGS suggests it was 2km southwest of Annandale; see map below).

Almost on the epicenter of our own little quake! For us east-coasters, that's a big deal!

WTOP reported on it (Thanks to Ron Schott for forwarding me this link).

Here's the USGS quake page on the event.

Here's the Maryland Geologic Survey's seismometry. (source of image above, which is in Eastern Standard Time, not Daylight)

Here's the Washington Post's (brief) treatment of it.

I've gotta say, Ron Schott's up on it -- within an hour of the seismic event, he had e-mailed Tuff Cookie and I to ask about it. Pretty prompt! Thanks, Ron.


Update: Here's the Google Map showing the epicenter (green arrow). I've circled the building where I was giving the exam in the green circle:


Also: Here's the intensity map as it looked after I logged on and completed the "Did You Feel It?" survey:

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Tuesday, April 22, 2008

Rain in the river

It started raining in DC on Sunday, and it basically hasn't quit since then. Rock Creek is running high and frothy, and the Potomac has about seven times as much water in it today as it did 36 hours ago. The USGS has only one gauging station on the Potomac in the Piedmont -- at Little Falls, approximately on the DC/Maryland border. Here's what that gage's data (available free online from the Survey) tells us (as of last evening) about the river's recent discharge trend:

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Saturday, April 12, 2008

Walkingtown, DC

Later this month, I'm leading a tour for "Walkingtown, DC" a twice-annual event sponsored by Cultural Tourism DC, a nonprofit organization. My tour is called "History Before History: the geologic saga of Washington, DC." I'll be leading the tour on both Saturday, April 26, and Sunday, April 27, from 1-4pm. If you're in the area, consider coming along. We'll be discussing the deposition of sediments in the Iapetus Ocean, generation of an accretionary wedge, the Taconian Orogeny, the Rock Creek Shear Zone, emplacement of the Georgetown Intrusive suite, and finally the erosion of the young Appalachian mountains and the deposition of dinosaur-fossil-bearing river gravels atop the unconformity: the Potomac Group. As a bonus, we'll even visit a thrust fault which ruptures the unconformity at the intersection of Adams Mill Road and Clydesdale Place, NW. It's a nice little jaunt through prehistory. However, this hike was extremely popular last year: we had ~300 people show up! So I've asked Cultural Tourism DC to institute a reservation system this time around: I'm limiting participation to 30 people per day. Act now to reserve your place by calling or e-mailing Cultural Tourism DC.

Here's two pictures of the mad crowds last spring. I get the heebie-jeebies just thinking about it:

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Friday, March 21, 2008

Honors students' field work, Part 3

I've already introduced you to two of my Honors students' field projects. Now for the last of the three -- Jason's project on the strained metaconglomerate of Klingle Road. Klingle Road is a "road" in D.C. that was damaged by a storm some years back, and never repaired. Some people have started using it as a park, while others clamor for the road to be fixed. Geologically, it's interesting because it exposes a rock unlike any other nearby: a distinctly foliated metaconglomerate. Because I am so clever, I call it the Klingle Road Metaconglomerate. It's part of the "Laurel Formation," which is one of many flavors of metagraywacke / accretionary wedge complex that make up the bulk of the Piedmont in this area. Here's some of the squished clasts that Jason is interested in:

metacong_klingle

We know these rocks got heated up a fair bit. How do we know this? Well, they flowed out into elongated shapes all oriented in the same direction for one (see the additional photos here). The outcrop is peppered with clusters of little plus-shaped protuberances: they are clusters of sericite (cryptocrystalline muscovite) in the shape of staurolite porphyroblasts. Staurolite is a reasonably high grade metamorphic mineral, and when we see the three-dimensional shape of staurolite, but it's been turned into relatively-low-grade sericite, it's an indication of "retrograde metamorphism." Basically, after hitting the peak of its particular metamorphic conditions (high temperature and pressure, growing staurolite), the rock is readjusting to lower temperatures and pressures, and those staurolite crystals are reacting to a mineral that's more stable at those lower temperatures and pressures: sericite.


staurolite_pseudomorph

But anyhow -- back to the metaconglomerate. It's made of clasts, and those clasts have been stretched. The question is: how much have they been stretched. Sometimes when strain estimates are made, we assume an initial sphere shape, and then measure the lengths of the various axes of the resulting ellipsoidal shape (the "strain ellipsoid"). But is the assumption of initial sphericity valid? Jason is testing this issue by measuring the axes of cobbles and pebbles from the metaconglomerate as well as loose cobbles and pebbles found in nearby Rock Creek. We want to get a sense of how ellipsoidal cobbles are before they experience orogenic shortening/stretching. Here's a shot of Jason, Spencer, and Victoria measuring cobble axis lengths on a gravel bar near the National Zoo:

rock_creek_clasts

And a shot of the crew close-up:

clast_measure

And, just for fun, here's one more shot from Victoria's field area on Broad Branch. We hiked up to the contact with the Kensington Tonalite (a ~464 Ma felsic intrusive rock -- essentially a granite) and found a series of small waterfalls over this resistant rock unit. In the sequence of cascades were a series of deep pools. I submerged myself in one of them:

deep

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Monday, March 17, 2008

Honors students' field work, Part 2

Picking up with my series of posts introducing the work my Honors students are doing this semester: today we'll take a look at Spencer's project, which involves field work on a bedrock terrace (strath) of the Potomac River near Chain Bridge (which can be seen in the background of this photo). As before, ignore the datestamp in the lower-right of the photo. These pictures were taken last week, not in 2004.

chainbridge

This is in the westernmost corner of DC's "diamond" shape. The bridge leads across the river into Arlington, Virginia. As you can see, there's a lot of rock exposure here -- the sort of thing we go crazy over here in the east. As noted before, this is metagraywacke (sometimes metamorphosed to schist, sometimes to gneiss, sometimes just strongly foliated, and sometimes so lightly metamorphosed / deformed that it even preserves original sedimentary structures like graded bedding. The interesting thing about the Chain Bridge locality is that in amongst the metagraywacke are big chunks of other rock types. I'll refer to these as "clasts." Some geologists have interpreted them as sedimentary deposits; others as "olistoliths" (tectonically emplaced chunks in an accretionary wedge complex). Spencer is in charge of documenting the variety of these clasts, in hopes that it may tell us something about their ultimate source. Here's a big elongate clast of gneiss:

clast1

We had a good little field routine going: Victoria and Jason would go scout out clasts, and then mark their location with a chalk arrow. Then Spencer would document each clast's lithology and characteristics (e.g. foliation at an angle to regional foliation) and then photograph it. Once he'd photograph it, he "checked it off" with chalk. All of this chalk graffitti gets washed away with the next big rainstorm.

clast2

Some of the clasts are no longer in their original condition. The one below, for instance, bears a multitude of garnets, metamorphic minerals which reflect how the clast's original composition reacted to the higher temperatures and pressures of Appalachian mountain-building.

garnet-rich clast

Another thing we saw a lot of in the Chain Bridge locality is erosional features related to the incision of the Potomac River into bedrock. Here's Jason showing off a pothole that drilled all the way through one outcrop:

pothole

Next time, we'll take a look at Jason's project.

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Thursday, March 13, 2008

DC Environmental Film Fest

It's almost cherry blossom season, so that means it's also time for the annual DC Environmental Film Festival. For two weeks, lots of interesting films are hosted by dozens of libraries, theaters, embassies, NGOs, and the like. Many of them are free. If you live in the DC area, this is an excellent opportunity to see some movies that you won't otherwise get access to. Even if you're not in the Capitol area, you can check out some of these films: this year, several of the films (like tonight's snow leopard movie) are available for watching free via the Internet. Enjoy!

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Wednesday, March 12, 2008

Billy Goat Trail geology hike dates

DC Metro area residents, you're hereby invited to join me (NOVA) or Phil Justus (NRC) or Michelle Arsenault (NSF) on a geology hike along the Billy Goat Trail, a popular and rugged hiking trail upstream from DC on the Potomac River, downstream from Great Falls. Michelle and Phil and I take turns leading this excellent hike. You'll learn about the Iapetus Ocean, Appalachian mountain-building, and the incision history of the Potomac River. You'll see potholes, amphibolites, metagraywacke, migmatite, and the mysteriously-straight Mather Gorge. The Park Service has just posted the spring schedule online here. Reserve your space today!

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Sunday, March 2, 2008

"The Last Iceberg"

Today was the artist's reception at the National Academies of Science for Camille Seaman's exhibit of photographs entitled "The Last Iceberg." I took a break from writing a paper for my MSSE class and went down to check it out.

One of my geology honors students, Spencer, showed up too, and we checked out Seaman's glowing icebergs set against dark backgrounds. There were some really stunning images, but the exhibit was rather small -- only fifteen or so separate pictures.

If you're not in the DC area, you can check out a slideshow of images from the exhibit at Seaman's website. Enjoy!

Also, while I was there, I went upstairs to see the excellent "Monkey Portraits" exhibit by Jill Greenberg. As with "The Last Iceberg," only a selection of images was shown -- a total of ten or so. But man, what an amazing ten images! I'll put just one up here, entitled "Undecided":

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Wednesday, February 20, 2008

Biofuels cartoon

After last week's CO2 smackdown on corn ethanol and other biofuels as a "cure" for global warming, Washington Post cartoonist Tom Toles scratched out this killer cartoon:

Thanks to John Weidner for calling this gem to my attention!

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Thursday, February 14, 2008

Valentine's Day at the Zoo

In the spirit of the day, check out this article about mating at the National Zoo, here in DC (and a literal stone's throw from my apartment window).

Among the information featured:
when two females cheetahs are housed together, one or both females will shut down their ovulation, which makes it impossible to breed them until they are again separated.

Shanthi, the baby Asian elephant (who's now almost as big as her mom), was the result of artificial insemination. I remember visiting the Zoo shortly after Shanthi was born, and seeing video footage of her birth. Wow! Kablooey! That's a big package to drop!

The male Panamanian golden frog (pictured), which is extinct in the wild, will attach itself to the female for up to 120 days to make sure he's the one to fertilize her. Talk about clingy!

Also, you may be interested to know that some lowland gorillas will mate face-to-face, as the Wildlife Conservation Society reported this week, and was subsequently promoted by National Geographic.

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Monday, February 11, 2008

DC crime camera locations

Starting today, DC police are monitoring live images from surveillance cameras in many parts of the city. The District has 73 cameras, with live feeds from 54. The Washington Post published this map showing where they are (supposedly the locations were chosen in historically high crime areas). They also have an article about the new system. My 'hood of Adams-Morgan gets two, it looks like...

Anyhow, I always love maps, so I thought I'd share this one.

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Thursday, January 31, 2008

Moon over the National Cathedral

Here's a shot from last week of the almost-full moon hanging over DC's National Cathedral. The view is to the west, which I guess means that I must have taken this picture in the morning, since the moon's face is being illuminated by the Sun. The Sun, of course, rises in the east. And if I can't specifically remember, that probably means I hadn't had my coffee yet, so that definitely makes it a morning shot.

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Monday, January 28, 2008

Snow at the Zoo

We had some snow the week before last in DC. Here's the view from my apartment out over the National Zoo, draped in a lovely layer of white.

That's Rock Creek in the foreground, a major waterway cutting through DC along a pre-existing zone of weakness called the Rock Creek Shear Zone. Rock Creek Park is the largest urban national park in the United States (twice as large as Central Park, and about 5/3 the size of Golden Gate Park).

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