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  2. Teays River - Wikipedia

    en.wikipedia.org/wiki/Teays_River

    The River's headwaters were near Blowing Rock, North Carolina; it then flowed through Virginia, West Virginia, Ohio, Indiana, and Illinois. (Hansen, 1995). [ 4 ] The largest tributary to the Teays River was the Old Kentucky River (Teller 1991), which extended from southern Kentucky through Frankfort and subsequently flowed northeast, meeting ...

  3. 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 ...

  4. Laurentide ice sheet - Wikipedia

    en.wikipedia.org/wiki/Laurentide_ice_sheet

    The Cordilleran ice sheet covered up to 1,500,000 square kilometres (580,000 sq mi) at the Last Glacial Maximum. [11] The eastern edge abutted the Laurentide ice sheet. The sheet was anchored in the Coast Mountains of British Columbia and Alberta, south into the Cascade Range of Washington. That is one and a half times the water held in the ...

  5. Lake Tight - Wikipedia

    en.wikipedia.org/wiki/Lake_Tight

    The river's path traveled through modern-day West Virginia, Kentucky, Ohio, Indiana, and Illinois, finally emptying into the Gulf of Mexico, which at the time extended to southern Illinois. 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.

  6. Lake Maumee - Wikipedia

    en.wikipedia.org/wiki/Lake_Maumee

    This involved the reversal of drainage in what is now northeastern Indiana and northwestern Ohio as the Maumee River outlet developed by capturing streams that formerly drained into the Wabash. The Great Black Swamp that once occupied much of the land between Sandusky, Ohio , and New Haven, Indiana , was a remnant of the bed of Glacial Lake Maumee.

  7. Till plain - Wikipedia

    en.wikipedia.org/wiki/Till_plain

    Till plains are an extensive flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place, depositing the sediments it carried. Ground moraines are formed with melts out of the glacier in irregular heaps, forming rolling hills.

  8. Tiny Ohio town sees population double with influx of 3,000 ...

    www.aol.com/tiny-ohio-town-sees-population...

    A small Ohio town is the latest victim of the Biden-Harris administration’s open border policy after 3,000 migrants from the West African nation of Mauritania moved in in the past year — lured ...

  9. Valparaiso Moraine - Wikipedia

    en.wikipedia.org/wiki/Valparaiso_Moraine

    The inner border is less than 15 miles (24 km) and at its closest approach is only about 6 miles (9.7 km) from Lake Michigan. The system is from 5 miles (8.0 km) or 6 miles (9.7 km) up to nearly [6] 20 miles (32 km). It is narrowest in LaPorte County, Indiana and widest in Lake County, Indiana. [7]