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Teays Valley (/ ˈ t eɪ z / TAYZ [5]) is a census-designated place in Putnam County, West Virginia, United States. The population was 14,350 at the 2020 census . Located about 20 miles (32 km) west of Charleston and 30 miles (48 km) east of Huntington , it is part of the Huntington–Ashland metropolitan area .
Teays River. The Teays River network, which existed before disruption by glaciers during the Pleistocene. Reconstruction is based on the discovery of large buried valleys in West Virginia, Ohio, and Indiana and other evidence. The Teays River / ˈteɪz / [1] (pronounced taze) was a major preglacial river that drained much of the present Ohio ...
Scott Depot, West Virginia. Scott Depot is an unincorporated community in Putnam County, West Virginia, United States. Located along Crooked Creek, it is part of the census-designated place of Teays Valley, which is a part of the Huntington–Ashland metropolitan area. The ZIP code is 25560.
UTC−4 (EDT) The Huntington–Ashland metropolitan area is a metropolitan area in the Appalachian Plateau region of the United States. Referred to locally as the " Tri-State area," and colloquially as "Kyova" (K entuck y, O hio, and West V irgini a), the region spans seven counties in the three states of Kentucky, Ohio, and West Virginia. [ 3 ]
A new US 35 interchange in Teays Valley was started in 2003 and is now complete. A hybrid semi-directional T/diamond interchange connects I-64 to the new US 35 corridor route from Teays Valley to the previous US 35 alignment near Buffalo. In addition, I-64 has been widened to six lanes between this interchange and exit 39 at WV 34.
Teays, written Seays until circa 1884, is an unincorporated community in Putnam County, West Virginia, United States. The town is centered on the former general store / post office on Teays Lane, which sits across from the site of the Teays railroad depot, which was demolished in the mid-1900s. Teays is a namesake and part of the census ...
The glaciers of the Ice Age soon began to block the Teays, effectively damming the river and forming Lake Tight, near what is now Chillicothe, Ohio. The lake has been the repeated topic of research over the past 100 plus years. In geologic terms, the lake's life span was short; the lake appears to have formed in the Lower or Middle Pleistocene.
Designated CP. October 15, 1966. Jefferson Rock is a rock formation on the Appalachian Trail in Harpers Ferry, West Virginia. It consists of several large masses of Harpers shale, [3] piled one upon the other, that overlook the Shenandoah River just prior to its confluence with the Potomac River.
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