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.

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.

The red ball sat proudly at the top of the toybox. It had been the last to be played with and anticipated it would be the next as well. The other toys grumbled beneath. At one time each had held the spot of the red ball, but over time they had sunk deeper and deeper into the toy box.