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title: There's a message for you if you look up.

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copy: Since they are still preserved in the rocks for us to _see,_ they must have been formed quite recently, that is, geologically speaking. What can explain these striations and their common orientation? Did you ever hear about the Great Ice Age or the Pleistocene Epoch? Less than one million years ago, in fact, some 12,000 years ago, an _ice_ sheet many thousands of feet *thick* rode over Burke Mountain in a *southeastward* direction. The many boulders frozen to the underside of the _ice_ sheet tended to scratch the rocks over which they rode. The scratches or striations seen in the park rocks were caused by these attached boulders. The _ice_ sheet also plucked and rounded Burke Mountain into the shape it possesses today.

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title: As he waited for the shower to warm, he noticed that he could hear water change temperature.

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