Maine's bold coast is one of its distinctive qualities. When I first arrived in Maine, I was surprised, for I had never before seen sedimentary rocks with vertical orientation, as are many rocks along the Maine coast. It is amazing that a quick examination of a site can give you a complex geologic history of the area. For me, this meant exploring the area, and researching how each specific characteristic is formed.
Have you ever noticed the interesting orientation of the rocks along Maine's coast? To many, this looks unnatural. Sedimentary rocks originally form in the ocean as thin layers of sand or mud. Over time, these layer solidify, leaving the ocean floor as layered rock. The layers alternate between the lighter sandstone, and darker mudstone. As it lays on the ocean floor, the rocks are horizontal. The vertical orientation of the rocks are actually formed as a combined result of the sedimentation and the buckling of the ocean's crust with the formation of the Mid-Atlantic ridge (the Mid-Atlantic ridge is an undersea mountain range in the middle of the Atlantic Ocean). With the uplifting of the tectonic plates, a buckling motion occurred, forcing the sedimentary rock onto its side.
Want to know more about Maine's history? Look at the rocks and fossils around you--they'll tell you everything!
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