The Ozarks Mountains are among the oldest mountain ranges on the planet and primitive man arrived here over 7,500 years ago to live in the bluff shelters and caves so numerous to this area and built wattle and daub houses along the banks of the many streams in what is now known as Newton County.
Agriculture appeared later and the cultivation of corn became common throughout the area and the people relied less heavily on hunting and gathering until they subsisted almost entirely on this sweet product of the fields. Corn was ground into meal using sandstone metates, or grinding bowls, and the sand got into the meal and wore away the Indian's teeth, causing severe tooth loss at an early age. Midden deposits in the shelters and caves yield corn cobs, projectile points, bones of food animals and the burials themselves. Some caves have deposits as deep as seventeen feet, indicating thousands of years of occupation. The Indian population was always sparse in this area with never more than one or two families living in any one place. No large villages are found and little or no evidence is noted of warfare. These were simple people living a subsistence life. Hernando DeSoto was the first European to enter Arkansas, doing so in June of 1541. Although he never saw the Ozarks, he inquired of the Tunica Indians (whom he met at a village near the city of Parkin) and was told by them that the area to the north and west was sparsely populated by a nomadic people and that it was a cold climate.
It
is truly amazing how the Ozark Mountains were formed and the
geological studies done in Newton County have shown that this area
was dominated by ancient seas, prehistoric upheavals, and past
climates. The rocks were formed from sediment deposited on the
bottom and along the shoreline of ancient oceans. The structure is
the result of geologic forces that uplifted the region out of the
ocean hundreds of millions of years ago. More recent weathering and
erosion of these rocks sculpted the shape and form of the present
surface. The oldest rocks are Ordovician age (505 to 438 million years ago). They are found in the bluffs, streambeds and flood plains of the major streams in the northern part of the county. These rocks represent lagoons, barrier islands, beaches and shallow ocean environments. The Mississippian Period (360 to 320 million years ago) saw a landscape that was filled with a rich dry-land ecosystem of plants and animals. These rocks represent continental shelf and near shore marine environments. Rocks of the Pennsylvanian Period (320 to 286 million years ago) cap the mountains of the county. They are the result of sediments deposited by ancient deltas and river systems along the margin of a sea. After that, for several million years, a continental fragment collided with the ancestral North America. This collision pushed up the Ouachita Mountains to the south and warped the Ozarks out of the ocean for the last time. Today the Ozarks Mountains in Newton County are a wonderland of beautiful sites to see, exciting things to do, and an authentic experience of natural beauty and rich cultural heritage that one will cherish forever. |
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Excerpts from Newton County Action Team Pathways |
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1-888-ARHOUSE (274-6873) |
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locally 870-446-5900 |
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Email: ARHOUSE@ritternet.com |