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Brandywine Falls Provincial Park is a beautiful park centred around the wonderful falls that plunge 70 metres down a vertical wall of glacier fractured rock. The peculiar, angular cubes of rock that the cliffs surrounding the falls is the result of lava rapidly cooling against a glacier. The rapid cooling causes solid rock to fracture in bizarrely angular ways known as columnar jointing. From the viewing platform across from the falls you can make out four distinct layers of columnar jointing separated by glacial till.