June 15th, 2010

Mountain Time 179

That last panel was supposed to be people on the opposite side of the planet wondering why they were stuck 10 feet below ground, but I didn’t spin the Earth hard enough and landed on a lighthouse scene somewhere in the middle instead. Sorry.

Happy Tuesday! Today marks 490 years since Philip II declared William the Silent an outlaw. William has yet to comment.

^ 7 Comments...

  1. Marty

    Both of the characters have nice hair. I want hair like that.

  2. ColdFusion

    I don’t think solids float atop more dense solids.. that’s sort of why solids are different from fluids.. herrnn…
    That little bird looks lonely :C

  3. isto

    It’s more that both plates are floating atop the semi-solid asthenosphere, and when they collide and have nowhere else to go, the denser plate sinks and assimilates into the asthenosphere, while the other just continues to float.

    For the bathtub-fun-time equivalent, float something like a baking sheet into a block of styrofoam.

    In contrast, when two continental plates collide, they’re simply unable to sink, and instead bunch up and form big ol’ folded mountains. It’s interesting to note that such mountains go down just as far as they go up, but remain solid because their buoyancy kinda pushes the asthenosphere further down.

  4. Wiesel

    good thing they’re always mindful of their bouyancy

  5. isto

    Amen.

  6. ColdFusion

    hmm.. plausible. Applause.

  7. Dougie

    Mindfully buoyant…that’s a great name for a band.

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