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  2. Hocking Hills State Park - Wikipedia

    en.wikipedia.org/wiki/Hocking_Hills_State_Park

    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.

  3. Drift Creek Falls - Wikipedia

    en.wikipedia.org/wiki/Drift_Creek_Falls

    Drift Creek Falls is a waterfall formed west of Valley of the Giants, east side of the city of Lincoln City in Lincoln County, Oregon. [1] Access to Drift Creek Falls is located along a trail constructed by the Forest Service in the 1990s and features a 240 foot long suspension bridge crossing Drift Creek. [2]

  4. Devil's Staircase Wilderness - Wikipedia

    en.wikipedia.org/wiki/Devil's_Staircase_Wilderness

    The Devil's Staircase Wilderness is a forested wilderness area adjacent to the Umpqua River in the Southern Oregon Coast Range of the U.S. state of Oregon.It was officially designated in March 2019.

  5. Drift Creek (Siletz Bay) - Wikipedia

    en.wikipedia.org/wiki/Drift_Creek_(Siletz_Bay)

    Drift Creek is a tributary, about 18 miles (29 km) long, of Siletz Bay in the U.S. state of Oregon. [3] The creek begins near Stott Mountain in the Central Oregon Coast Range in Lincoln County and follows a winding course generally west through the Siuslaw National Forest to enter the bay south of Lincoln City on the Pacific Ocean.

  6. Court of Appeals denies proposed Drift Creek Dam but water ...

    www.aol.com/court-appeals-denies-proposed-drift...

    The East Valley Water District, made up of a group of farmers around Mt. Angel, has been seeking to build a dam south of Silverton for a decade.

  7. Falls of the Ohio National Wildlife Conservation Area

    en.wikipedia.org/wiki/Falls_of_the_Ohio_National...

    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.

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