. The preglacial drainage of Ohio; comprising the results of researches . THE PREGLACIAL DRAINAGE OF OHIO. 47 Any one walking as I have walked, from Wooster by Hayes-ville and Mansfield to Bellville; and then crossing the profilefrom Ashland to Loudonville: will see this fact demonstratedto convicition. In the first tramp (Wooster to Belleville) you cross all thestreams that drain the eastern face of the plateau; and the eleva-tions, as determined by barometer, may be instructive. WoosterUniversity stands 522 feet above Lake Erie. Killbuck Valley332, Jefiferson, on rock summitt of plateau, 600
. The preglacial drainage of Ohio; comprising the results of researches . THE PREGLACIAL DRAINAGE OF OHIO. 47 Any one walking as I have walked, from Wooster by Hayes-ville and Mansfield to Bellville; and then crossing the profilefrom Ashland to Loudonville: will see this fact demonstratedto convicition. In the first tramp (Wooster to Belleville) you cross all thestreams that drain the eastern face of the plateau; and the eleva-tions, as determined by barometer, may be instructive. WoosterUniversity stands 522 feet above Lake Erie. Killbuck Valley332, Jefiferson, on rock summitt of plateau, 600, the flood plainof Muddy Fork 432, and the divide between this and theJerome Fork 650, while its flood plain is 450. Hayesville,on the summit of the divide between the Jerome and the BlackForks, 700, and the flood plain of the Black Fork at Mifflin is500, the depot at Mansfield 581, and the plateau south of the cityis 800, and above Bellville 900. In the cross section from Ash-land to Loudonville the divide between the Jerome and the BlackForks, independent of glacial
Size: 1451px × 1723px
Photo credit: © Reading Room 2020 / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookdecade1900, booksubjectgeology, bookyear1900
