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However, the Kentucky Geological Survey estimated a cumulative total of 200,000 wells in 1992, with 23,000 oil wells and 11,000 gas wells producing in 1989. The Eastern Coal Field and Western Coal Field have been the mine sites of production, with little exploration in the Jackson Purchase and Bluegrass regions.
USGS physiographic map of Kentucky showing the location of the Knobs. The Knobs Region or The Knobs is located in the US state of Kentucky. It is a narrow, arc-shaped region consisting of hundreds of isolated hills. The region wraps around the southern and eastern parts of the Bluegrass region in the north central to northeastern part of the state.
Mud and debris surround a playground outside Robinson Elementary School near Ary in Perry County, Ky., on Tuesday, Aug. 2, 2022. Flood waters devastated many communities in Eastern Kentucky last week.
The Department of Defense Education Activity (DoDEA) operates schools for military dependents at two major United States Army bases in Kentucky, Fort Campbell and Fort Knox. DoDEA has organized a Kentucky-specific district to administer the schools on those bases (although some of the Fort Campbell schools are physically located in Tennessee).
In addition to the above schools, one school located in Tennessee is a member of the Kentucky High School Athletic Association, the state's governing body for high school sports. Fort Campbell High School is located in the Tennessee portion of the Fort Campbell Army base, but has always competed against Kentucky schools. Most of the base ...
The Field Elementary School at 120 Sacred Heart Lane in Louisville, Ky. on July 10, 2023. Field, the district's fourth-oldest school, opened in 1915 with five teachers and 155 students in ...
The Lexington Limestone is a prominent geologic formation that constitutes a large part of the late Ordovician bedrock of the inner Bluegrass region in Kentucky.Named after the city of Lexington, the geologic formation has heavily influenced both the surface topography and economy of the region.
The Clinton Group (also referred to as the Clinton Formation or the Clinton Shale) is a mapped unit of sedimentary rock found throughout eastern North America. [1] [2] The interval was first defined by the geologist Lardner Vanuxem, who derived the name from the village of Clinton in Oneida County, New York where several well exposed outcrops of these strata can be found.