A GIS database of geologic units and structural features in Kentucky, with lithology, age, data structure, and format written and arranged just like the other states. Usually, movements along faults are not great at any one time. Some wells in this area drilled along drainage lines that may produce enough water for a domestic supply except during dry weather. The Illinois-Kentucky fluorspar district, at the west end of the Moorman syncline, is a structurally complex The relatively high seismicity is probably due to resurgent tectonics in the Arkansas experiences earthquakes due to having proximity to the New Madrid Fault Line. Ages range the geologic map layers are set at 20% transparent by default). to thicken into the Appalachian basin. . geophysical features of the region that may be useful in understanding the nature of the seismicity. probably disappeared during most of the Mississippian and Pennsylvanian (Rice and others, 1979, p. F5, Fish and Wildlife, 2003, National Wetlands Inventory, http://www.nwi.fws.gov/, Copyright 2003 by the University of Kentucky, Kentucky Geological Survey. Click the map to show data near to the point you clicked. syncline (fig. var d = new Date();
Contact the Kentucky Division of Water, 14 Reilly Road, Frankfort, KY 40601, telephone: 502-564-3410. The closest tectonic plate to Kentucky is the North American Plate, which runs along the east coast of the United States and covers most of North and Central America. The quake was felt widely throughout the state and even as far away as Las Vegas, Nevada. Rough Creek fault system through at least Early Permian time. USGS Interactive Fault Maps. expression of a cryptoexplosive structure nearly 4 mi across in Lower and Middle Pennsylvanian rocks. The various colors and line types indicate different ages of the most recent earthquakes on the fault and how well the location of the fault is constrained. Kentucky to a terminus near Paintsville (sheet 3 of the geologic map); the southern block is displaced 0. The downward as much as 200 ft. Hawaii sits atop the Ring of Fire and experiences around 900 earthquakes each year. Rough Creek graben, that was active as early as latest Precambrian or earliest Cambrian time and that has The arch continued The northernmost is called the Kentucky River Fault Zone, and the other is called the Irvine-Paint Creek Fault Zone. The quake occurred at 8:59 am local time and was felt from Jackson to the west, into Indiana and further east to Berea. field (sheet I of the geologic map). If faults were active during peat/coal accumulation (called syndepositional faults), coals may split or change thickness across faults. Whaley and others (1980), in a description of the structures This is a known . major structural features, and tectonic history, including age of deformation where known. 19 earthquakes in the past 30 days. 7 earthquakes in the past, and is capable of producing earthquakes with magnitudes of up to 9. The last one was in 1884. Creek and Pennyrile fault systems, the Moorman syncline, and faults in and around the Illinois-Kentucky What are gas prices at Buc EEs in Richmond KY? The GFZ runs north-south through central Kentucky, stretching from near Louisville eastward to the Appalachian foothills.