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  2. Ophiolite - Wikipedia

    en.wikipedia.org/wiki/Ophiolite

    Ordovician ophiolite in Gros Morne National Park, Newfoundland Chromitic serpentinite, Bay of Islands Ophiolite, Lewis Hills, Newfoundland. An ophiolite is a section of Earth's oceanic crust and the underlying upper mantle that has been uplifted and exposed, and often emplaced onto continental crustal rocks.

  3. Orogenic belt - Wikipedia

    en.wikipedia.org/wiki/Orogenic_belt

    An orogenic belt, orogen, or mobile belt, [a] is a zone of Earth's crust affected by orogeny. [2] An orogenic belt develops when a continental plate crumples and is uplifted to form one or more mountain ranges ; this involves a series of geological processes collectively called orogenesis .

  4. Smartville Block - Wikipedia

    en.wikipedia.org/wiki/Smartville_Block

    Geologic map depicting the Smartville Complex (in brown) and other accreted terranes in California. [1]The Smartville Block, also called the Smartville Ophiolite, Smartville Complex, or Smartville Intrusive Complex, is a geologic terrane formed in the ocean from a volcanic island arc that was accreted onto the North American Plate during the late Jurassic (~160–150 million years ago).

  5. Category:State parks of Ohio - Wikipedia

    en.wikipedia.org/wiki/Category:State_parks_of_Ohio

    Pages in category "State parks of Ohio" The following 71 pages are in this category, out of 71 total. This list may not reflect recent changes. ... Mobile view ...

  6. Climate zones updated for first time since 2012. What it ...

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  7. Hueston Woods State Park - Wikipedia

    en.wikipedia.org/wiki/Hueston_Woods_State_Park

    The state bought the land in 1941, but the park did not open until 1957. The state used the land initially as a prison camp. [citation needed] In 1956, Four Mile Creek was dammed to form Acton Lake, named for Clyde Acton, the member of the Ohio General Assembly who persuaded the legislature to buy the property. [4]

  8. Geology of Ohio - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Ohio

    Ohio's State Invertebrate Fossil, is a trilobite found in the formation. The Southern Hemisphere where Ohio was located at the end of the Ordovician experienced a widespread glaciation, around 438 million years ago. Sea level dropped due to the glaciation, accompanied by a subsidence of the land.

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