He stared out the window at the snowy field. He'd been stuck in the house for close to a month and his only view of the outside world was through the window. There wasn't much to see. It was mostly just the field with an occasional bird or small animal who ventured into the field. As he continued to stare out the window, he wondered how much longer he'd be shackled to the steel bar inside the house.
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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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The bridge spanning a 100-foot gully stood in front of him as the last obstacle blocking him from reaching his destination. While people may have called it a "bridge", the reality was it was nothing more than splintered wooden planks held together by rotting ropes. It was questionable whether it would hold the weight of a child, let alone the weight of a grown man. The problem was there was no other way across the gully, and this played into his calculations of whether or not it was worth the risk of trying to cross it.
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