Geology

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When I was walking to school in the second grade, I found myself behind a group of older kids, arguing about what subjects they hated most. The consensus was geography. At the time I didn’t know what geography was, but I became determined to find out. When I did, two things happened. First, I realized that I loved geography (and along with it, geology). Second, I learned that popularity of anything often meant nothing. And I’ve been passionate about geography ever since.

But not just for myself. Instead I’m interested in feeding scholarship wihin subjects that interest me. For both geography and geology I do that mostly through photography. Toward that end, here are a few recent sets I’ve posted, or updated:

Meanwhile, close to 200 of my shots are now in Wikimedia Commons. Big thanks to the Wikipedians who have put them there. I can’t begin to count how many Wikipedia articles many of these illustrate. currently accompanies eighteen different articles in fourteen different languages.

While we’re on the subject of , I’ll commend to you the new book Good Faith Collaboration by , a fellow at this year. His first chapter is online.

You may notice that most of my links to subjects, both in my online writings and in my photo captions, go to Wikipedia entries. Sometimes people ask me why. One reason is that Wikipedia is the closest we have come, so far, to a source that is both canonical and durable, even if each entry changes constantly, and some are subject to extreme disagreement. Wikipedia is, like the , a set of . Another reason is that Wikipedia is guided by the ideal of a neutral point of view (NPOV). This, Joseph says, “ensures that we can join the scattered pieces of what we think we know and good faith facilitates the actual practice of fitting them together.”

The nature of the Net is to encourage scatterings such as mine, as well as good faith about what might be done with them.

Igor vs. Bermuda

Hurricane Igor

It’s a safe bet that most people don’t know where Bermuda is. Here’s the answer: In the middle of the ocean, close to nothing. It’s not like the Bahamas, or the islands of the Caribbean, which are arranged in chains, or near to a continent. Instead Bermuda pokes above the Atlantic eight hundred fifty miles straight east of Charleston and the same distance south of Halifax. Its nearest neighbor is Cape Hatteras, still close to seven hundred miles away. So there is no land nearby to protect Bermuda, or to which its residents can run for safety.

Bermuda is also tiny, with a land mass is 20.6 square miles. That’s about 4.5 miles square. You could fit two Bermudas in one San Francisco, with room to spare. Its highest point is Town Hill, at about 250 feet above sea level.

Hurricanes usually circle around Bermuda, attacking Caribbean islands or land along the the Gulf or the Atlantic Coast of the U.S. But Hurricane Igor is different. Hurricane Igor is aimed for Bermuda. (Here’s a great looping animation from the National Hurricane Center, showing Igor’s path. And here’s another, with layers you can turn on and off.)

Since what remains of U.S. mainstream media generally don’t give a shit about the rest of the world — especially when the subject is hurricanes (see this Onion story for more on that) — Bermuda remains downgraded as an Area of Interest. Until, of course, it’s obliterated. You know, like Haiti or New Orleans.

But Bermuda is still there, and it does have media, including tweeters and bloggers. (Well, it’s kinda short on bloggers. Look up Bermuda bloggers on Google or Bing and the top results are pretty depressing. At least there’s Global Voices: Bermuda, where I just learned about Bermuda Blog. And there are others I’m sure to hear about, soon as this is posted.)

There’s the Bermua Sun (@BDASun), The Royal Gazette, BermudaNews (@bermudanews.com), Bermuda Online, .bm emergency tweeters (@edenrichardson, @BermudaDCoffice, @smexpress, @Blonde_In_Bda, @CollieBuddz, @FairmontHam, @JImCantore, @letonnerre @shaeyd @jessicanrowe, @amonteleone, @piecesofsleep…) And, of course, everything that shows up in a search for #bermuda, #igor or both.

I can’t find a single radio or TV station in Bermuda that streams on the Web, other than ZBMradio, which doesn’t seem to be working (at that link, which goes to the stream). But here are the Twitter search results for streaming bermuda.

The last major hurricane to strike Bermuda was Fabian, in 2003. That one killed eight and caused $355 million (2010 USD) in damage. Not bad, considering peak sustained winds of 145mph. (See Roland’s comment, below.)

Meanwhile, heres the action plan, via the BDA Sun. I’ll add more below as news comes in.

Last week I flew back and forth from Boston to Reno by way of Phoenix. Both PHX-RNO legs took me past parts of Nevada I hadn’t had a good look at before. One item stood out: a dry lake that looked, literally, like a town had been built on it and blown up. In fact, this was the case. The lake was Frenchman Lake, on Frechman Flat, a valley in a part of the desert known as the Nevada Test Site. The town was nicknamed “Doom Town,” and it was built to see what would happen to it in an atomic blast. Here’s a video that shows the results.

In fact more than a dozen blasts rocked the Doom Town area, starting with Able, in 1951 — the first at the Test Site.

This shot shows Yucca Lake and Yucca Flat, which has many dozens of subsidence craters where underground blasts have gone off. This Google Maps view shows the same from above. All the blasts look like rows of dimples in the desert. But some are hundreds of feet across. Before reading about underground nuclear testing, I had thought that all the tests were deep enough to avoid surface effects.

This shot looks across the Test Site to Area 51. Amazing place. Some of what they say about it may even be true. By the way, that shot was taken (I just checked) from almost 100 miles away. I used a Canon 5D and a zoom telephoto lens set to 200mm.


While walking around Paris for the last month, I’ve became fascinated by the highly fossiliferous limestone that comprises so many of its iconic structures. At one point I thought, Hmm… The City of Light is built with materials of death. I had no idea how much farther that thought would take me.

Without abundant death we wouldn’t have asphalt, concrete, marble, travertine, chert, oil, gas, coal, asphalt, limestone, dolomite, and countless other requirements of civilization. So, given the unusual abundance of limestone in use here, I wondered where it came from. Naturally, from my 21st-century perspective, I assumed that all of it had been quarried in some other place: hills outside of town, perhaps. Lutetian limestone, it’s called, and it’s a relatively new rock: only a few dozen million years old. Younger than dinosaurs. It’s also known as “Paris stone”, and has become quite the fashion item lately.) What I hadn’t figured was that nearly all of this building stone, for many centuries, was extracted from beneath Paris itself: a sum large enough to build a Great Pyramid.

I didn’t learn any of that until we visited the Catacombes a couple days ago.

The Catacombes are bone banks called ossuaries. They occupy abandoned quarries beneath Paris and contain the remains of more than six million people. Many of the deceased were likely the same men (and women? probably) who carved out the quarries, mostly in the first several centuries of the last millennium. It must have been quite a project since these withdrew enough rock to assemble Notre Dame, thousands of other churches large and small, bridges, city walls, and homes—and left beneath the streets of Paris more than 300 kilometers (100 miles) of tunnels, including rooms and vaults that together comprise a vast man-made cave system. Top to bottom, a vertical cross-section of Paris looks like this:

  • Surface — streets, buildings, parks
  • Metro tunnels
  • Sewers
  • Quarries

Fossils are bones of stone, I explained to my kid. And limestones are stones of bone. Here in the Catacombes, down hallways that go on and on and on and on, the bones of dead Parisians are stacked into walls, with an artistry that makes one wonder what was going on in the heads of the masons. The walls facing the visitors are built mostly with femurs and skulls. The femurs are stacked and interlocked, with the knee knuckles outward, course after course forming a pattern like stitches in cloth. These are interrupted by horizontal lines of skulls, and usually topped with a final row: a crowning course of human heads. No concrete, grout, or other adhesive material anywhere. Here and there some arm bones might be used, but femurs and skulls were clearly the preferred structural material. Behind these walls behind lie loosely the rest of the bones: remains of remains.

The masons were priests. The bones were gathered from the city’s cemeteries, which had become rotten with an abundance of corpses as the end of the 18th century approached. That’s when it was decided to move the bones down into deeper graves. The quarries were empty, so the bones came down. The whole project went in stages, running from the late 1700s to the middle 1800s. The priests, whose jobs already required exceptional respect for the dead, were conscripted for the work.

The pictures in my collection (e.g. the one above) aren’t the best I’ve taken. Most of the light was provided by dim illumination in the catacombes itself, or by cell phones. If you wish to know more (and I recommend it), here is a pile of fascinating links:

Since one walks through the tunnels in the company of guides and other people, it is less creepy than you might think. After a while, endless aisles of bones also tend to make the bones themselves ordinary. Yet one wonders: Is this skull Robespierre’s? Danton’s? Both lost their heads to the guillotine, but down here all heads are equally ordinary and anonymous, fully respected, but still just building material.

A lesson: different as we are in life, we are remarkably identical in death. Skulls tend to all look the same. So do other bones. One can say, These were babies once. Then laughing children. They grew up, learned about life, and lived long enough to produce more babies and get work done. And what they’ve left is no different than what everybody else leaves.

What makes us animals is that we eat other living things. (We need their carbon.) We live on things that lived. And we build with them too. Death supplies us. In turn, we supply as well.

What makes us different is who we are, and what we do when we’re alive. Life is for the living. And so, it turns out, is death.

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The California is serpentine (correct name, serpentinite), which comes in many varieties, some which contain asbestos, which doesn’t get dangerous unless you grind it up and spread it into the air. Just sitting there, as it does through much of California and in other parts of the world, serpentine is mostly a greenish grace on the landscape.

Serpentine’s provenance is also remarkable (at least to geology types like me). It’s formed deep in the planet’s crust, under the spreading centers of oceans, where sea water penetrates mantle rock and, under great heat and pressure, lends lustrous colors and textures to what would otherwise become the plain old peridodite.

Anyway, have found a friend in , who is working to dump serpentine as the state rock. You know, like it matters. (Only 27 states bother having a state rock.) Read more in Burrito Justice and in the many posts that come up when you search for. Or you can skip all that and go to ‘s Speak Up for Serpentine at .

Here’s the opposing (anti-serpentine) view.

My home state, (also that of my nonfictionist hero, ) has no state rock, mineral or gem. How about asphalt, rhinestone and dirt? Just trying to help.

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Or let the paleontologists dig it for you. That’s what a team led by Yale researchers did last year in southeastern Morocco’s Lower and Upper Fezouata Formations. The result is covered by LiveScience in Oldest Soft-Bodied Marine Fossils Discovered . Specifically, “The animals represented by these newly discovered fossils, including sponges, annelid worms, mollusks, and horseshoe crabs, lived during the Ordovician period between 480 million and 472 million years ago, making them the oldest ever discovered during this period.”

So, while I have your attention on that, let me redirect you to Ron Schott’s Road Trip: An Experiment in Social Geology. He begins,

With your help, dear readers and fellow geobloggers, I’d like to run an experiment in social geology this summer. My hypothesis is that real-time/live-web tools and social networking can be applied to geology-focused road trips in ways that enrich the experience for both the road-tripper and the audience of active participants. This blog post is a call for collaborators, and a starting point for discussion and refinement of this hypothesis. I hope that it evolves into much more than that.

Me too. While Ron traverses The West, I’ll be heading to France for much of June and July. But I’ll keep up with him and enjoy vicarious digging of hard rock landscapes, many of which I already know but haven’t seen. Sez Ron,

The response to my blog posts two weeks ago using excerpts from John McPhee’s Annals of the Former World has inspired me to attempt to GigaPan at least four more of his I-80 geologic localities on my way out to San Francisco. Tentatively, and subject to tight restrictions imposed by the vagaries of weather and the need to arrive at the conference on time, I’m aiming to GigaPan the Gangplank/Summit area of the Laramie Range, roadcuts in the Rawlins, WY area, something in the Rock Springs/Overthrust area of western Wyoming, the Wasatch Front/Great Salt Lake, the Golconda Thrust, and an ophiolite in the Sierra Foothills.

The only thick book I’ve picked up nearly as often as McPhee’s Annals is Tolstoy’s War and Peace (though the latter not in the last couple of decades, I regret to admit). The Gangplank and the Overthrust sites I have visited dozens of times in re-readings of Rising from the Plains, my favorite of the four prior books that Annals combines (with a bonus section called Crossing the Craton). The Wasatch, Salt Lake, Golconda thurst and Sierra Foothills ophiolites star in Basin and Range and Assembling California, which Annals also includes. Been to all of those many times as well.

Ron is a Gigapanner of the first water. Here’s the latest, shown with a Canon 5D like my own (though with a better lens than any that I have). Can’t wait to see what he shows. (Some samples from his professional work as a geology professor.)

Good to see by his tweets (he’s @rschott) that he’s still cruising the West Coast (after getting some gigapans in Utah en route ). While he’s still out there, here a few possible side trips I’d like to suggest :

  • Love Ranch, where David Love grew up. Love was the geologist who guided McPhee through Wyoming. The title of the resulting book, Rising from the Plains, comes from a diary of David’s mother, Ethel Waxham Love, a writer whose prose was equal to McPhee’s, and who carries much of the book’s narrative burden. Dr. Love and the ranch buildings are all gone, but not the landscape, nearly all the features of which were named by the Love family.
  • Red Bluff Ranch, near Lander and west of the Gas Hills, amidst red Triassic features raised to weather when the Wind River Range, said David Love to John McPhee, “just pooched out.” Red Bluff Ranch is where Ethel Waxham (years away from becoming a Love) arrived when she — as McPhee loves to put it — came into the country by stagecoach.
  • The Powder River Basin strip coal mines, where the land celebrated by “Home on the Range” is classed as “overburden” and peeled off by the square mile to extract coal. This is featured in the “Coal Train” chapters McPhee’s Uncommon Carriers.

I can think of many more, but those are a start. I’ll add more later. Right now I gotta take the kid to the dentist.

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I just learned by Eric Martindale’s comment to my Borg’s Woods post in February that the March 13 storm knocked down many of the trees in the old growth urban forest that was our neighborhood playground when I was a kid. For more here’s a post in the NJUrbanForest blog, and here are some pictures as well.

Storms are as much a part of nature as old growth forests, even when the former reduces the latter. Sad to read, however, that mosquito abatement has involved the draining of the woods’ pond, where generations of kids learned to skate in a beautiful setting.

For perspective perhaps it is helpful to note that the boggy parts of Borg’s Woods are among the few vernal remnants of glacial Lake Hackensack, which pooled over most of the Hackensack River watershed when the last ice age began to end around 15,000 years ago. The lake lasted several millennia, then drained around 11,500 years ago, when the terminal moraine near Perth Amboy broke. Back then the sea was still far outside the current borders of New York and New Jersey. Only when the rest of the ice cap melted did the oceans reach their current level — which, as we know, is still rising.

weathermap

The mudslides we feared in Southern California didn’t materialize when I posted about the topic on January 21st. Now they are feared again, as a new wave of winter rainstorms passes through. Some slides have already happened. More will. Count on it. (And if you’re at serious risk, really please do GTFO.)

Meanwhile, back here in Boston, a winter snowstorm is headed our way, after treating D.C., Maryland and the surrounding regions to another heavy layer of snow, atop the deepest in memory, which hasn’t had a chance to melt. (One relative there went for many hours without power, looking out on a scene where his car appeared only as a low hill in snow through which only trees and houses protruded.)  We’ve mostly been spared this winter, as have the ski areas to the north. Those will probably be spared again, since this storm is expected to do its heaviest dumping south of here. Bummer, that.

On Friday we fly back to Santa Barbara for The Kid’s winter school break. There are mudslide risks there too, though not as severe as in Los Angeles. (Our hills are mostly rock. L.A.’s are mostly dirt. Think of L.A.’s hills as sponges — because that’s what they are. Place a dry sponge on a steep incline, drip water on it, and see what happens when it fills.)

Maybe, if we’re lucky, we’ll miss the rain there, and get treated to some of those sunsets we’ve been missing. Hope so.

[Later…] I just got a call from my wife, awakened at 3:3oam in California by a call from the school here. A snow day has been declared. Doesn’t look like it yet, though. There are details in the clouds, like scales on a mackerel. But, as we can see from the radar, it’s coming.

[Later still…] It’s now 2:30 in the afternoon, not long before school gets out, and there has been approximately no snow at all. Just a mix of light flakes and drizzle. Good, I guess.

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spypondhockey

For most of Winter in the Northeast, skating is possible only during the somewhat rare times when the ice is thick and not covered with snow or other unwelcome surface conditions. And bad skating has been the story, typically, for most of this Winter around Boston. After an earlier snow, there were some ad hoc skating rinks cleared by shoveling, but those were ruined by rains, more snow, more rains, and intermittent freezes that made a hash of the surface. But recent rains and hard freezes have formed wide paths between remaining islands of ruined snow. On most ponds there aren’t enough open spaces for real hockey games, but there’s plenty enough for skating, and for hockey practice, anyway. (A note to newbies and outsiders: nearly all lakes here are called ponds. Dunno why yet. Maybe one of ya’ll can tell me. Still a bit of a noob myself.)

Hockey practice is what I saw when I paused to take a sunset shot with my phone at Spy Pond, which I passed it late this afternoon on a long walk along the Minuteman Bikeway, which is one of my favorite walking paths (and thoroughfares — at least when it’s warm and clear enough to bike on). As it happens, Spy Pond ice has some history. There was a period, in the mid- to late-1800s, after railroads got big, but before refrigeration came along, when New England was a source for much of the world’s shipped ice. And Spy Pond itself was one of the most productive sources. This picture here…

spypond_history2

… shows ice being harvested for storage in ice houses beside the railroad which is now the Bikeway. I stood near the left edge of this scene when I took the picture at the top, and the boy and his dad playing hockey were about where at the center left, where a horse is shown pulling what looks like a man with a plow. (That last shot is from this historical display alongside the bikeway.)

The brainfather of Boston’s ice industry was Frederic Tudor, about whom I have learned a great deal from The Ice King: Frederic Tudor and His Circle. Highly recommended, if you’re into half-forgotten New England history. The book came as a bonus with membership in Mystic Seaport, a terrific maritime museum down the road on the Connecticut coast.

[Later…] The industry you see depicted above can also serve as a metaphor. For that a hat tip goes to Robin Lubbock (@RLma), New Media Director of WBUR, who pointed me to this piece by Michael Rosenblum. Nails it. (I also love Rosenblum’s Maybe monetizing is not the answer and Edward III, Crecy and Local TV Newsrooms, also via Robin.)

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saltpond_smFour more of my aerial photos now illustrate their subjects in Wikipedia: Nebraska National Forest and the nearby town of , both in the region; and and Salina (a micro algae that colors salt ponds, such as those on the left), both in the Bay Area.

There are now 120 of my shots in Wikimedia Commons. I put none of them there. I just tag shots aggressively and describe them the best I can (and have time for), and let nature take its course. In these cases nature was PDTillman. Hats off to him.

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