INTRODUCTION. 35 



Bowman, Isaiah, A typical case of stream capture in Michigan: Jour. Geology, vol. 12, 1904, pp. 326-334. 



Discusses the capture of a very small tributary of Huron River near Ypsilanti by the widening of the Huron 

 Valley until it cut into the path of the tributary. 



Flowing wells ana municipal water supplies of Clinton, Eaton, Barry, Ionia, Montcalm, Ottawa, and northern 



Allegan counties, Mich.: Water-Supply Paper TJ. S. Geol. Survey No. 182, 1906, pp. 155-169, 225-226. 



Bownockek, J. A., A deep preglacial channel in western Ohio and eastern Indiana: Am. Geologist, vol. 23, 1899, 

 pp. 178-182, with map. 



Traces a deep channel by borings from Shelby County, Ohio, to Blackford County, Ind. 

 Bradley, F. H., Geology of Vermilion County, Ind.: First Ann. Rept. Geol. Survey Indiana, 1869, pp. 138-141. 



Notes buried soil and distinct sheets of glacial drift. 



Grundy, Will, Kankakee, Iroquois, Vermilion, Edgar, Ford, and Champaign counties, 111.: Illinois Geol. 



Survey, vol. 4, 1870, pp. 190-194, 205-209, 222-230, 236-238, -241-244, 266, 272-274. 



Notes buried soil and distinct drift sheets in several counties. 

 Breeze, F. J., The valley of the lower Tippecanoe River: Proc. Indiana Acad. Sci., 1901, pp. 215-216. 



Presents map and discusses width of valley and of stream. 

 Bretz, J. H., Glacial features of Genesee County [Mich.]: The Schoolmaster (an educational journal published monthly 

 at Saginaw, Mich.), Feb. and Mar., 1907, pp. 482-487 and 530-539. 



Gives a general description of the glacial and lake formations of Genesee County and a map covering most of the 

 county. Discusses the topography and gives a clear account of the recession of the ice sheet and the development 

 of moraines, till plains, eskers, glacial drainage channels, etc., the succeeding lake stages with beaches, deltas, 

 etc., and the relation of all of these features to the present drainage. 

 Brown, R. T., General sketch of geology of Indiana: Third Rept. Board Agri., 1853, pp. 299-322. 



Reports upon counties in Indiana: Fountain County drift and buried channels: Eleventh Ann. Rept. Dept. 



Geology and Nat. Hist. Indiana, 1881, pp. 91-94; Marion County, glacial deposits, terraces, buried channels, post- 

 glacial drainage, well sections, etc.: Twelfth Rept., 1882, pp. 81-96; Morgan County, glacial deposits (including 

 gold and diamonds), drainage features, etc.: Thirteenth Rept., 1883, pp. 79-S3; Hamilton and Madison counties, 

 glacial deposits and postglacial drainage: Fourteenth Rept., 1884, pp. 22-26, 32-37; Hancock County, glacial 

 features, drainage, and soils: Fifteenth Rept., 1886, pp. 1S7-197. 



States that buried soils occur between drift sheets in several of these counties. 

 Burt, W. A., In S. Ex. Doe. No. 1, 31st Cong., 1st sess., 1849, pt. 3, p. 820. 



Notes that Lake Superior was formerly much larger than now. 

 Cable, E. J., Road materials of a portion of central Indiana: Thirtieth Ann. Rept. Dept. Geology and Nat. Res. 

 Indiana, 1905, pp. 656-674, 681-755. 

 The occurrence of gravel deposits in workable quantity in several counties discussed is described in some detail. 

 Campbell, J. L., Report upon the improvement of the Kankakee River and the drainage of the marsh lands in Indiana, 

 34 pp. with map of Kankakee region, Indianapolis, 1883. 



Presents a line of levels along the axis of the Kankakee basin. 

 Campbell, J. T., Topographical phenomena in Indiana: Am. Naturalist, vol. 18, 1884, pp. 367-379. 



Explains low inclination of south-facing drift slopes by a creeping of the deposits, favored by the deposition of 

 drift by a southward-moving current of ice. Distrusts interpretation referring the low inclination to alterna- 

 tions of freezing and thawing on that slope. 



Source of supply to lateral and medial moraines: Abstract in Proc. Am. Assoc. Adv. Sci., vol. 40, 1891, pp. 255- 



256. 



Lower layers of ice are thought to bring up material to higher levels at abrupt bends as streams do. 



Evidence of a local subsidence in the Interior: Jour. Geology, vol. 9, 1901, pp. 437-438. 



Recent levelings of a locality in Indiana where bench marks were established in 18S3 show a southward differ- 

 ential depression which it is thought may have been produced by the Charleston earthquake. 

 Carney, Frank, The metamorphism of glacial deposits: Jour. Geology, vol. 17, 1909, pp. 473-487. 



Discusses induration or cementation, leaching, etc., in Illinoian drift compared with Wisconsin. 



■ Raised beaches of the Berea, Cleveland, and Euclid sheets, Ohio: Bull. Sci. Lab. Denison Univ., vol. 14, 



1909, pp. 262-287. Abandoned shore lines of the Oberlin quadrangle, Ohio: Bull. Sci. Lab. Denison Univ., 

 vol. 15, 1910, pp. 101-117. 



These two papers present results of detailed field study of beaches in several quadrangles on the south shore of 

 Lake Erie. 



Some proglacial lake shorelines of the Bellevue quadrangle, Ohio: Bull. Sci. Lab. Denison Univ., vol. 17, 



March, 1913, pp. 231-246, 4 figs. 



Carr, M. E., and McLandon, W. E., Soil survey of the Saginaw area, Michigan: Field operations Bur. Soils in 1904, 

 U. S. Dept. Agri., 1905, 40 pp. and map. 



Discusses soils, agricultural methods, and conditions in an area of 984 square miles around Saginaw. 

 Chalmers, Robert, Artesian borings, surface deposits, and ancient beaches in Ontario: Summary Rept. Geol. Sur- 

 vey Canada for 1902, pp. 268-279. 



Notes occurrence of two bowlder clays and presents discussion (with map) of several shore lines in southwestern 

 Ontario. Differential uplift is recognized, but the amount of uplift is not determined. 



