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Recurrence Interval Estimates For The July 2022 Eastern Kentucky Floods, North Fork Of The Kentucky River, William C. Haneberg
Recurrence Interval Estimates For The July 2022 Eastern Kentucky Floods, North Fork Of The Kentucky River, William C. Haneberg
Open File Reports--KGS
July 2022 flood recurrence interval calculations for three gages along the North Fork of the Kentucky River—Whitesburg, Hazard, and Jackson, Kentucky—based upon both empirical distributions and theoretical log-Pearson Type III distributions yield a range of results from 851 years for the Whitesburg gage near the headwaters of the North Fork to about 2 years for the Hazard gage to 94 years for the Jackson gage. While the log-Pearson Type III approach worked well for the Whitesburg and Hazard gages, it produced an unrealistically low estimate for the Jackson gage because the empirical and theoretical curves diverge significantly for large floods …
Surficial Geologic Map Of The Hadley 7.5-Minute Quadrangle, Warren County, Kentucky, Matthew Massey, Meredith Swallom, Antonia Bottoms, Wes Buchanan, Bailee Nicole Hodelka, Emily Morris
Surficial Geologic Map Of The Hadley 7.5-Minute Quadrangle, Warren County, Kentucky, Matthew Massey, Meredith Swallom, Antonia Bottoms, Wes Buchanan, Bailee Nicole Hodelka, Emily Morris
Contract Reports--KGS
The Hadley 7.5-minute quadrangle is located in Warren County northwest of Bowling Green, Kentucky. Regionally, the quadrangle is entirely within the Mammoth Cave plateau, which is located in the Mississippian Plateaus physiographic region (McDowell, 1986). The Mammoth Cave plateau is a regional west-dipping cuesta, that has been extensively incised by the Green and Barren Rivers and their tributaries. The area is underlain by Upper Mississippian to Lower Pennsylvanian (Rainey, 1963): the lowest fluvial valleys are underlain by Ste. Genevieve Limestone; Girkin Formation is exposed on the steep slopes between the lower valleys and higher plateau; the plateau is underlain by …
Surficial Geologic Map Of The Bowling Green North 7.5-Minute Quadrangle, Warren County, Kentucky, Meredith Swallom, Matthew Massey, Wes Buchanan, Bailee Nicole Hodelka, Hannah Hayes, Charles Wells Iii, Emily Morris
Surficial Geologic Map Of The Bowling Green North 7.5-Minute Quadrangle, Warren County, Kentucky, Meredith Swallom, Matthew Massey, Wes Buchanan, Bailee Nicole Hodelka, Hannah Hayes, Charles Wells Iii, Emily Morris
Contract Reports--KGS
The Bowling Green North 7.5-minute quadrangle is located in Warren County immediately north of Bowling Green, Kentucky. Regionally, the quadrangle includes parts of the Pennyroyal and Mammoth Cave plateau, both within the Mississippian Plateaus physiographic region (McDowell, 1986). The Dripping Springs escarpment, which separates the lower-elevation Pennyroyal from the higher-elevation Mammoth Cave plateau is highly dissected in the quadrangle. Topography in the Pennyroyal is characterized by pervasive sinkhole development across the low-relief Pennyroyal, which is mostly underlain by the Mississippian St. Louis Limestone, Ste. Genevieve Limestone, and Girkin Formation (Shawe, 1963). Higher-relief topography is restricted to the slopes of the …
Surficial Geologic Map Of The Rockfield 7.5-Minute Quadrangle, Warren, Logan, And Simpson Counties, Kentucky, Wes Buchanan, Meredith Swallom, Antonia Bottoms, Matthew Massey, Bailee Nicole Hodelka, Emily Morris
Surficial Geologic Map Of The Rockfield 7.5-Minute Quadrangle, Warren, Logan, And Simpson Counties, Kentucky, Wes Buchanan, Meredith Swallom, Antonia Bottoms, Matthew Massey, Bailee Nicole Hodelka, Emily Morris
Contract Reports--KGS
The Rockfield 7.5-minute quadrangle is located west of Bowling Green, Kentucky situated mostly in Warren County, but also includes small areas of Simpson and Logan Counties in its southwestern corner. Regionally, the quadrangle includes parts of the Pennyroyal and Mammoth Cave plateau within the Mississippian Plateaus physiographic region (McDowell, 1986). The Dripping Springs escarpment, which separates the lower-elevation Pennyroyal from the higher-elevation Mammoth Cave plateau is highly dissected in the quadrangle. Topography in the Pennyroyal is characterized by pervasive sinkhole development across a low-relief plain, which is mostly underlain by the Mississippian Ste. Genevieve Limestone. Higher-relief topography is restricted to …
Surficial Geologic Map Of The Flaherty 7.5-Minute Quadrangle, Kentucky, Ann Hislop, Matthew Massey, Maxwell L. Hammond Iii, Antonia E. Bottoms, Michele Mchugh, Emily Morris
Surficial Geologic Map Of The Flaherty 7.5-Minute Quadrangle, Kentucky, Ann Hislop, Matthew Massey, Maxwell L. Hammond Iii, Antonia E. Bottoms, Michele Mchugh, Emily Morris
Contract Reports--KGS
The Flaherty 7.5-minute quadrangle is located southwest of Louisville and northwest of Elizabethtown along the boundary between Hardin and Meade Counties. The quadrangle includes mostly the Pennyroyal region of the Mississippian Plateau and also smaller areas of the Mammoth Cave plateau and the highly dissected Dripping Springs escarpment in the western half of the map area (McDowell, 1986). Topography is mostly characterized by pervasive sinkhole development in a lower elevation and low-relief plain, and high-relief plateaus, ridges, and knobs of the Dripping Springs escarpment scattered along the west side of the quadrangle. Swadley (1963) mapped the bedrock geology of the …
Surficial Geologic Map Of The Patriot 7.5-Minute Quadrangle, Kentucky, Maxwell L. Hammond Iii, Antonia E. Bottoms, Steven L. Martin
Surficial Geologic Map Of The Patriot 7.5-Minute Quadrangle, Kentucky, Maxwell L. Hammond Iii, Antonia E. Bottoms, Steven L. Martin
Contract Reports--KGS
The Patriot 7.5-minute quadrangle is located in Boone, Gallatin, and Grant Counties of northern Kentucky in the Outer Bluegrass physiographic province (McFarlan, 1943). Broad to narrow ridges, steep hillsides, and the Ohio River Valley characterize the topography of the quadrangle. The Ohio River has been made navigable by a series of high-level dams, and the Markland Locks and Dam controls the river level in this area (Ray, 1974). The bedrock geology, originally mapped by Swadley (1969), consists, from oldest to youngest, of the Point Pleasant Formation, the Kope Formation, the Fairview Formation, the Bellevue Tongue of the Grant Lake Limestone, …