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Pint of Beer - Falls of the Ohio Event Cache

This cache has been archived.

Boreal Walker: Thanks to everyone that showed up and made this one a success. It was nice to meet so many locals. Maybe we will see y'all on the trail someday.

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Hidden : Sunday, October 12, 2014
Difficulty:
1 out of 5
Terrain:
2 out of 5

Size: Size:   other (other)

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Geocache Description:


Where: Buckhead Mountain Grill
When: October 12, 2014 from 1900-2000
Who: Adventurous Cachers
What: A celebration of beer, caching, and the Falls of the Ohio.
Why: To enjoy a pint of beer, swap geocaching stories, and talk about extreme caching.
How: Barge, kayak, paddle boat.

The Ohio River is formed by the confluence of the Allegheny and Monongahela rivers at Point State Park in Pittsburgh, Pennsylvania. From there, it flows northwest through Allegheny and Beaver counties, before making an abrupt turn to the south-southwest at the West Virginia–Ohio–Pennsylvania triple-state line. From there, it forms the border between West Virginia and Ohio, upstream of Wheeling, West Virginia. The river then follows a roughly southwest and then west-northwest course until Cincinnati, before bending to a west-southwest course for most of its length. The course forms the northern borders of West Virginia and Kentucky; and the southern borders of Ohio, Indiana and Illinois, until it joins the Mississippi River near the city of Cairo, Illinois.

The Falls of the Ohio National Wildlife Conservation Area is a national, bi-state area on the Ohio River near Louisville, Kentucky in the United States, administered by the U.S. Army Corps of Engineers. Federal status was awarded in 1981. The falls were designated a National Natural Landmark in 1966. The area is located at the Falls of the Ohio, which was the only navigational barrier on the river in earlier times. The falls were a series of rapids formed by the relatively recent erosion of the Ohio River operating on 386 million-year-old Devonian hard limestone rock shelves. Louisville, Kentucky, and the associated Indiana communities—Jeffersonville, Clarksville, and New Albany—all owe their existence as communities to the falls, as the navigational obstacles the falls presented meant that late 18th Century and early to late 19th Century river traffic could benefit from local expertise in navigating the 26-foot drop made by the river over a distance of two miles. In its original form, the falls could be characterized more as rapids extending over a length of the river, than as a point-like discontinuity in a river such as Niagara Falls. Still, the falls provided a singular, dramatic and daunting obstacle to navigation on this important inland waterway.

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