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The Rough River Lake is a Y-shaped reservoir located in Breckinridge, Hardin, and Grayson counties in Kentucky, United States, about 70 miles southwest of Louisville. [1] This lake was created by the building of a dam, begun in 1955 and completed in 1961, 89.3 miles (143.7 km) above the connection between the Rough River and the Green River .
Rough River Dam State Resort Park. / 37.61083°N 86.50472°W / 37.61083; -86.50472. Rough River Dam State Resort Park is a Kentucky state park encompassing 637 acres (258 ha) [ 1] on Rough River Lake in Grayson county. Rough River Dam of 1959, stretching 1,590 feet (480 m) across and 135 feet (41 m) high, creates Rough River Lake, a ...
Rough River Lake near Leitchfield, Kentucky. The Rough River is a 136-mile-long (219 km) [1] tributary of the Green River in west-central Kentucky in the United States. It's located about 70 miles southwest of Louisville, and flows through Breckinridge, Hardin, Grayson, and Ohio counties. Via the Green and Ohio rivers, it is part of the ...
The tornado reached a peak width of 2,600 yards (2,400 m), and was on the ground for nearly three hours, tracking 165.6 miles (266.5 km) from Woodland Mills to Rough River Dam State Resort Park. [29] [60] [61] The path was the ninth longest in recorded history. [62] It was rated high-end EF4, with an estimated peak wind speed of 190 mph (310 km/h).
Natural Bridge State Park is a member of the Leave No Trace Center for Outdoor Ethics, and offers guided backpacking trips and natural history educational programs. Annual events open to the public include Herpetology Weekend each May, Natural Arches Weekend each February, and the Kentucky Native Plant Society's Wildflower Weekend each April.
Beginning around 11,700 B.C.E., the first indigenous people inhabited the area now known as Arkansas after crossing today's Bering Strait, formerly Beringia. [3] The first people in modern-day Arkansas likely hunted woolly mammoths by running them off cliffs or using Clovis points, and began to fish as major rivers began to thaw towards the end of the last great ice age. [4]
Lake Cumberland was impounded from the Cumberland River by the United States Army Corps of Engineers' construction of the Wolf Creek Dam in 1952. [1] Wolf Creek Dam is the 25th largest dam in the United States, and cost $15 million to construct originally, with an additional $65 million needed almost immediately to fix problems which soon became apparent.
Lake Hitchcock is an important part of the geology of Connecticut. It experienced annual layering of sediments, or varves: silt and sand in the summertime (due to glacial meltwater) and clay in the wintertime (as the lake froze). Analysis of varves along Canoe Brook in Vermont was conducted by John Ridge and Frederick Larsen, including ...