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Thomas J. Crawford, Charles W. Cressler, 1982. The Talladega “Series” in this area is bounded on the northwest by the Emerson (Cartersville) fault, along which the Talladega was thrust over (1) Valley and Ridge rocks ranging in age from Early Cambrian (Chilhowee Group) to Mississippian (Fort Payne Chert), (2) the Ocoee Supergroup, and (3) the “Corbin granite complex.” The Emerson fault also overrode the Great Smoky fault, which separates Ocoee from Chilhowee rocks in the Cartersville area. An earthquake is caused by a sudden slip on a fault, which results in a release of energy that travels away from the fault surface as seismic waves. During the middle Ordovician Period (about 440 - 460 million years ago), the tectonic plate carrying this area collided with another plate, leading to the creation of a new subduction zone and the beginning of the Appalachians. If you are 13 years old when were you born? In this region, the highest points in Georgia are found, including Brasstown Bald. The thrust fault along the southeastern boundary of the Talladega “Series” is only one of numerous closely spaced imbricate faults within and southeast of the Talladega. Corporate News . [5] Rocks typical of the region include schist, amphibolite, gneiss, migmatite, and granite. The Emerson fault also overrode the Great Smoky fault, which separates Ocoee from Chilhowee rocks in the Cartersville area. Please check your email address / username and password and try again. [1], The Appalachian Plateau geologic region only passes through the extreme northwest corner of Georgia. By continuing to use our website, you are agreeing to our, American Association of Petroleum Geologists, Cushman Foundation for Foraminiferal Research, Mineralogical Society of Great Britain and Ireland, Seismic Detection of Fractured Reservoirs: A Case Study of a Devonian Shale Gas Field in West Virginia: ABSTRACT, Three-Dimensional Structural Interrelationships Within Cambrian-Ordovician Lithotectonic Unit of Central Appalachians: ABSTRACT, A least squares method for earthquake mechanism determination using, Failles de chevauchement acadiennes dans la région de Weedon, Estrie, Québec, Latest Precambrian to Early Cambrian basin evolution, Fortune Bay, Newfoundland: fault-bounded basin to platform, Appalachian thrusting, lithospheric flexure, and the Paleozoic stratigraphy of the Eastern Interior of North America, Lower Cambrian metasediments of the Appalachian Valley and Ridge province, Alabama; possible relationship with adjacent rocks of the Talladega metamorphic belt, Relations between deformation of crystalline basement and sedimentary cover at the basement/cover transition zone of the Appalachian Blue Ridge Province, Relationship between Talladega belt rocks and Ocoee Supergroup rocks near Cartersville, Georgia, Stratigraphy and structure of the central Talladega slate belt, Alabama Appalachians, Paleozoic tectonic evolution of the western Blue Ridge, southern Appalachians: A critical examination of long-standing conflicts in a polydeformed system. Marble and talc are other resources produced in the Blue Ridge in Georgia.[1]. The Coastal Plain in Georgia is part of a geologic region that extends from New Jersey to Texas and consists of sedimentary rocks deposited in the Late Cretaceous to Holocene periods. The Blue Ridge Mountains in Georgia are evidence that in its distant past, the area was at the border of two tectonic plates. runs to Alabama. Oct 20, 2020 read more. [1] The extent of the Valley and Ridge is bound by the Carters Dam fault in the east and the Emerson Fault in the south. The thrust fault along the southeastern boundary of the Talladega “Series” is only one of numerous closely spaced imbricate faults within and southeast of the Talladega. [1] This region is more hilly than mountainous and is marked by lower elevations than the Blue Ridge. [6] It is divided from the Piedmont by the Fall Line, which passes through Georgia from Augusta in the east, then southwestward to Macon, then to Columbus and finally westward to Montgomery, Alabama. Emerson reports its fourth quarter 2020 results prior to market open on Tuesday, Nov. 3. Search for other works by this author on: You do not currently have access to this chapter. Ano ang Imahinasyong guhit na naghahati sa daigdig sa magkaibang araw? The Blue Ridge consists of metamorphic rocks, either metamorphosed equivalents of sedimentary rocks or igneous rocks, and the region includes the metavolcanic rocks of the Georgia Gold Belt. Georgia’s red clay is a product of iron oxidization in the soil and can be seen throughout Bartow, with increased concentrations in the Emerson area. "Talladega ‘Series,’ Great Smoky fault, and Emerson fault: Relationships in the Cartersville area, Georgia", Tectonic Studies in the Talladega and Carolina Slate Belts, Southern Appalachian Orogen, Denny N. Bearce, William W. Black, Stephen A. Kish, James F. Tull. Bulletin of the Seismological Society of America, Tectonic Studies in the Talladega and Carolina Slate Belts, Southern Appalachian Orogen, Geometries and Mechanisms of Thrusting, with special reference to the Appalachians, Linkages and Feedbacks in Orogenic Systems, This site uses cookies.

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