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  2. Sheriden Cave - Wikipedia

    en.wikipedia.org/wiki/Sheriden_Cave

    Sheriden Cave is a Paleo-Indian archaeological site from the late Ice age in Wyandot County, Ohio. [1] Glacial deposits sealed off the cave more than 10,000 years ago. Sheriden Cave is a karst sinkhole on a dolomite ridge that crosses Hancock and Wyandot Counties. It is associated with the Indian Trail Caverns that opened in 1927.

  3. Glacial till plains (Ohio) - Wikipedia

    en.wikipedia.org/wiki/Glacial_till_plains_(Ohio)

    The Glacial till plains are a till plain landform in Northern Ohio, located near the shore of Lake Erie and produced by the retreat of the Wisconsin glaciation. Since glacial till is highly fertile soil , agriculture on the glacial till plains is very productive.

  4. Geology of Ohio - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Ohio

    Glacial grooves on Kelleys Island. For 245 million years, spanning the entirety of the Mesozoic in the Paleogene , of the early Cenozoic , Ohio experienced long-running uplift and weathering. Prior to the Pleistocene glaciations, the region was covered in large stream valleys, which are believed to have removed several hundred meters of rock ...

  5. Lake Monongahela - Wikipedia

    en.wikipedia.org/wiki/Lake_Monongahela

    [1] Marine (1997) found five terrace levels along the rivers, but he had to conclude that the lake deposits found on them resulted from only two episodes of glacial damming. Deposits on the fifth and fourth terrace levels represent damming during a pre-Illinoian glaciation, whereas the third- and second-terrace-level deposits represent damming ...

  6. List of National Natural Landmarks in Ohio - Wikipedia

    en.wikipedia.org/wiki/List_of_National_Natural...

    Managed by Ohio University. Fort Hill State Memorial: 1974: Hillsboro: Highland: state Excellent outcrops of Silurian, Devonian, and Mississippian sedimentary bedrock and a natural bridge. Glacial Grooves State Memorial: 1967

  7. Esker - Wikipedia

    en.wikipedia.org/wiki/Esker

    The Irish word was and is used particularly to describe long sinuous ridges, which are now known to be deposits of fluvio-glacial material. The best-known example of such an eiscir is the Eiscir Riada , which runs nearly the whole width of Ireland from Dublin to Galway , a distance of 200 km (120 mi), and is still closely followed by the main ...

  8. Bedford Shale - Wikipedia

    en.wikipedia.org/wiki/Bedford_Shale

    In northern Ohio, the thickness of the Bedford is irregular due to erosion prior to the deposit of the Berea Sandstone, and due to recent glacial and stream erosion. The Bedford thins toward the south; near Columbus in central Ohio it is 95 feet (29 m) thick, and 85 feet (26 m) near Chillicothe 45 miles (72 km) to the south. [28]

  9. Kettle (landform) - Wikipedia

    en.wikipedia.org/wiki/Kettle_(landform)

    A kettle pond in the Hossa hiking area, Suomussalmi, Finland Numerous kettle lakes border the Denali Highway in Alaska. The Kettle Moraine, a region of Wisconsin covering an area from Green Bay to south-central Wisconsin, has numerous kettles, moraines and other glacial features. It has many kettle lakes, some of which are 100 to 200 feet (61 m ...