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The Secrets of Crab Island: Part I Prehistory: The Secrets of the Stones | ||
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Hundreds of millions of years passed; continents collided, the Earth was in the midst of great This planet is constantly in flux. The time humans have resided here is but an instant in the timeline of Earth's history. For hundreds of millions of years, the region was submerged under vast seas, hemmed in by the loftiest of mountains. Then, some 5 million years ago, the ice came. Massive glaciers covered the region; the change could not have been more profound. Reaching at times to a depth of over a mile, these mighty sheets of ice scoured the earth to bedrock and depressed what earth remained beneath them. Then, a mere 20,000 or so years ago the great ice sheet began to recede. Slowly, the enormous glaciers melted, leaving behind a vast freshwater lake. These melt waters stayed in the region, held back from the sea by the mass of the huge glacier to the north. Some 15,000 years ago, Lake Vermont was formed 2. Lake Vermont wasn't here very long, in a geological sense. Within a couple of thousand years, the glaciers to the north had melted sufficiently to allow sea water to rush in to the area, depressed as it was by the sheer weight of the ice sheet that at one time covered it. The freshwaters of Lake Vermont gave way to the briny depths of the Champlain Sea. The rise of land we know as Crab Island in all likelihood projected out of an ocean once again. Another cataclysmic change was in the making. Human beings would find their way to the shores of the Champlain Sea. Crab Island would hold secrets anew...
Sources/Notes:
1 James G. Bailey, "THE FORGOTTEN GRAVES OF CRAB ISLAND" (The Antiquarian-Fall 1988, Allan Everest, Editor Clinton County Historical Association, Plattsburgh, NY) 1 2 Lake Champlain Maritime Museum, Geological History, <http://www.lcmm.org/site/harbor/resource_pages/timeline/geological.htm > (16 May 2002)
On November 11, 2002, Crab Island was featured in a WPTZ/Lake Champlain Basin Program Champlain 2000 story. The video is no longer available online. However, you can still access the LCBP feature story on the web here. | ||
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