. Bulletin of the scientific laboratories of Denison University. 136 Biilleiin of Laboratories of Denison University Vol. XIII] Furthermore, westward from I lanover the vaUey j^rows broader; at Newark, a (hstance of seven miles, it is aliout two miles between the rock walls. Consequently as the margin of the east- ern side of the Scioto lobe assumed new positions in its declineâ a long" halt has been noted in the vicinity of Newark'âthis valley dependency persisted. The details of the drift south and southwest of Claylick have been studied for two miles, showing that the retreat of the ma
. Bulletin of the scientific laboratories of Denison University. 136 Biilleiin of Laboratories of Denison University Vol. XIII] Furthermore, westward from I lanover the vaUey j^rows broader; at Newark, a (hstance of seven miles, it is aliout two miles between the rock walls. Consequently as the margin of the east- ern side of the Scioto lobe assumed new positions in its declineâ a long" halt has been noted in the vicinity of Newark'âthis valley dependency persisted. The details of the drift south and southwest of Claylick have been studied for two miles, showing that the retreat of the main body of the ice was gradual, and apparently maintaining positions parallel to the convex margin mapped by Leverett. SUMMARY. A study of the Illinoian drift in this broken topography of the coarser-textured and more resistant formations of the Mississip- pian and Pennsylvanian periods estal)lishes the existence of tongue-like dependencies of the Scioto lobe reaching out into the eastward trending valleys. Gcologlca] Dcpartuictit. Denison Uni-i'crsify, Granville, O., April, 1906. ^ F. Leverett. loc. cit., Plate II. e5' 1 1 Z^^ â1 >.y^' ^^ .f-âf4-/! ^0^ ) \ V - \l / ^ â >Aâ ---'\T^-f *"*â *""* //- A* V^ / y [^ V ^ , ^ â x^ ^a* J f r ^ V^" ;,>^^*Y^-/ ^" 1 4 1 iickin,)Co\y ^ â ty RMuSkim^umCo *>2/ m Hanoror Dam I' J TOWNSHIPS I. Eden i Fa//s6urfh 3. Mary Ann 4 Perry SMa cf/ sen 6, Hanc ver 7 FranM/in BHo/^ewell J Bow/inif Crei. LICKING COUNlV, 0 Bcrt/orofXIIinoianJce ancwmif va//ey c^ependencea. F, ,. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Denison University; Denison Scientific Association. Granville, Ohio : [The University]
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