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He heard the crack echo in the late afternoon about a mile away. His heart started racing and he bolted into a full sprint. It wasn't a gunshot, it wasn't a gunshot, he repeated under his breathlessness as he continued to sprint. she'll prove she can again. We all already know this and you will too.

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She wondered if the note had reached him. She scolded herself for not handing it to him in person. She trusted her friend, but so much could happen. She waited impatiently for word. she'll prove she can again. We all already know this and you will too.
Warning Message

He sat across from her trying to imagine it was the first time. It wasn't. Had it been a hundred? It quite possibly could have been. Two hundred? Probably not. His mind wandered until he caught himself and again tried to imagine it was the first time. she'll prove she can again. We all already know this and you will too.

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He couldn't move. His head throbbed and spun. He couldn't decide if it was the flu or the drinking last night. It was probably a combination of both. she'll prove she can again. We all already know this and you will too. she'll prove she can again. We all already know this and you will too.
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.