752 GLACIAL FORMATIONS OF ERIE AND OHIO BASINS. 



County. It there curves around to a course north of east and passes into 

 Wood County near North Baltimore. About a mile north of North Balti- 

 more it turns eastward and passes north of Bardstown and Bloomdale and 

 leaves Wood County about 4 miles north of Fostoria. For 3 or 4 miles 

 in the western part of Seneca County it is ill defined on account of the 

 presence of rock hills, but near Amsden it reappears in strength and leads 

 northeastward past Kansas about to the county line. It there curves 

 abruptly to a southward course and runs out at a creek valley about a 

 mile east of Kansas. 



Faint ti'aces of the shore were found near Angus and thence south- 

 eastward along an angling road to the- Pan Handle Railroad which it crosses 

 at the township line about 3 miles north of Tiffin. The beach then bears 

 eastward near the township line to the Sandusky River, and after crossing 

 the river takes a northeastward course, passing through Watson and about 

 2 miles south and east of the village of Greenspring. It passes about 2 miles 

 east of Clyde and enters Erie County 5 or 6 miles north of Belle^ale. 

 In western Erie County a bay extended back to the north edge of Bellevue, 

 but the border is indistinctly outlined because of the shallowness of the 

 water and the presence of small islands to the north and east. There were 

 also islands iixunediately southwest of Castalia which add to the complexity 

 (see PL XXII). 



At North Monroeville, about 6 miles east of Bellevue, the lake shore 

 becomes reduced to a single definite ridge which leads southward into 

 Huron County past Monroeville and there curves around to the east, cross- 

 ing East Huron River about a mile south of the Lake Shore and Michigan 

 Southern Railway. Its course is then northeastward through Norwalk and 

 East Norwalk into Erie County. For several miles it lies near the Maumee 

 beach and passes with that beach through the village of Berlin Heights. 

 From Berlin Heights eastward to North Amherst it lies 1 to 2 miles north 

 of the Maumee shore. From North Amherst it swings around southward 

 to the city of Elyria. It leads into Elyria from the northwest, but leaves 

 that city in a course north of east and, passing through Ridgeville and 

 Dover, oomes to Rocky River within a mile north of the Maumee shore. t 

 curves around with that shore through West Cleveland and runs through 

 the southwestern part of the city of Cleveland along Dennison avenue. 



Upon crossing the Cuyahoga Valley it passes northward through the 



