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Last Call – The Tracks of My Tears Edition

Robert Emslie November 3, 2010 Last Call

Earthquakes can wreak havoc on buildings, roads, and your adrenal gland. They can also make rail road tracks a total e-ticket ride.

Image source: [Imgur.com]

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Currently there are "29 comments" on this Article:

  1. Fej says:

    Thats a pretty good amount of displacement for one quake. Strike-slip fault for the win!

    • mdharrell says:

      There's no corresponding displacement of the adjacent terrain (note, for example, the undisturbed access road), so this looks more like longitudinal compression of the rails. This could, of course, be a consequence of nearby movement of a strike-slip fault (or dip-slip fault, or oblique fault), but this photo isn't showing the fault itself.

      Yes, I'm a geologist.

      • Fej says:

        Yeah, I realized I was a bit off track right after I posted that. Took me a minute to notice that the "sine wave-ish" pattern of the tracks doesn't really match up with what I've seen strike-slips do. Compression makes a lot more sense.

        In my defense I'm only a Geology major and I'm in the middle of a nasty migraine. I bow to your superior knowledge and judging by the fact you have a geology degree, your superior drinking skills.

        • mdharrell says:

          No problem– I've got three geology degrees and a professional license. I teach undergraduate geology. Mostly, though, it comes down to the drinking skills.

          "…a bit off track…." Heh.

      • OA5599 says:

        I can't find any fault with that analysis.

  2. faster,Tobias! says:

    'Well, we was doing alright but then the peyote kicked in..'

  3. This must be the site of a Molly Hatchet concert. Just got back from their live show downtown and it really shook!

    On a side note, with three motorcycle gangs represented in the crowd, including the legendary Hells Angels, I had hoped some scene might bust out, but nothing happened. Bah, watching too much Sons of Anarchy lately.

  4. Alff says:

    They'll fix it, but not soon enough for Lorenzo Bandini.

  5. I have a picture just like this in a mechanical engineering textbook as the result of thermal expansion of the tracks on a very hot day.

    Basically, they want to get longer, but somewhere farther down there's a bend or otherwise cooler and better anchored section. The compression builds up until this happens.

    • "…and if it snows that stretch down south just won't take the strain."

    • Charles_Barrett says:

      I, too, thought of thermal expansion when I saw that photo. I grew up in earthquake-prone SoCal, and have seen roads that have slid askew, but that sinusoid track does not look like the result of a violent temblor to me.

      • mdharrell says:

        Perhaps, but in the case of thermal expansion on a hot day, how rapidly would the strain progress once the track began to yield? That gravel extending halfway across the road looks like it wasn't just gently pushed aside.

        Besides, in this case there's good reason to blame a quake. I just did some digging:

        http://blogs.agu.org/landslideblog/2010/11/02/the

        Bonus points for the use of "temblor" though.

        • Charles_Barrett says:

          Although my undergraduate degree from Caltech is in electrical engineering, I did take some courses on geology from Prof. Kerry Sieh while I was there. He's a big fan of earthquakes… ;-)

  6. It pretty much matches the heart-trace of any train driver rapidly bearing down on it.

  7. Greg Newman says:

    this was my favourite one from the recent christchurch quake in new zealand

    <img src="http://www.aucklandtrains.co.nz/wp-content/uploads/chch2-533×400.jpg"&gt;

  8. P161911 says:

    Chicanes for trains.

  9. muthalovin says:

    Thomas the Tank Engine is not amused.

  10. Number_Six says:

    These days FIA just puts chicanes wherever the hell they feel like it.

  11. kah says:

    more like the The Tracks of Photoshop Edition

    • Number_Six says:

      Guess you've never experienced an earthquake, huh?

      • kah says:

        nothing bigger that a 5

        A quick google tell me it's from the 7.1 magnitude earthquake that happened near Canterbury New Zealand on September 4th I stand corrected what appears to be the extra track can be easily explained by the simple fact that steel is malleable.

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