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The Marietta Earthworks is an archaeological site located at the confluence of the Muskingum and Ohio Rivers in Washington County, Ohio, United States. Most of this Hopewellian complex of earthworks is now covered by the modern city of Marietta. Archaeologists have dated the ceremonial site's construction to approximately 100 BCE to 500 CE.
Map of the Muskingum River watershed Aerial view of the Ohio and Muskingum Rivers at Marietta, Ohio. The Muskingum River (/ m ə ˈ s k ɪ ŋ (ɡ) ə m / mə-SKING-(g)əm; Shawnee: Wakatamothiipi) [4] is a tributary of the Ohio River, approximately 111 miles (179 km) long, in southeastern Ohio in the United States. An important commercial route ...
Hocking Hills State Park is a state park in the Hocking Hills region of Hocking County, Ohio, United States. In some areas the park adjoins the Hocking State Forest. Within the park are over 25 miles (40 km) of hiking trails, rock formations, waterfalls, and recess caves. The trails are open from dawn to dusk, all year round, including holidays ...
It passes Rinard Mills and Dart, and joins the Ohio approximately 5 mi (8 km) southeast of Marietta, Ohio and the mouth of the Muskingum River, which enters the Ohio from the northwest. Duck Creek enters the Ohio between the mouth of the Muskingum and Little Muskingum. All except the last 2 mi (3.2 km) of the river are within Wayne National Forest.
West Virginia lies across the Ohio River to the south: Pleasants County in the far southeast, and Wood County otherwise. Two populated places are located along the Ohio River in Washington Township: most of the city of Marietta, the county seat of Washington County, in the northwest; and the unincorporated community of Reno, in the south.
Muskingum River near its mouth in downtown Marietta. Marietta is a city in and the county seat of Washington County, Ohio, United States.It is located in southeastern Ohio at the confluence of the Muskingum and Ohio Rivers, 11 miles (18 km) northeast of Parkersburg, West Virginia.
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The geology of Ohio formed beginning more than one billion years ago in the Proterozoic eon of the Precambrian. The igneous and metamorphic crystalline basement rock is poorly understood except through deep boreholes and does not outcrop at the surface. The basement rock is divided between the Grenville Province and Superior Province.