Relations of the Wisconsin and Kansan Drift Sheets in Central Iowa, and Related Phenomena

Bain, H. Foster

doi:10.17077/2160-5270.1331

Cited by 6 publications

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“…The "Upper" till of northeast Iowa did not correlate with the up per till at Afton. Bain (1895) correlated the younger till at Afton with McGee's "Lower" till. This led to a revision of the type section at Afton.…”

Section: History Of the Lowan Areamentioning

confidence: 99%

“…The drift to the south was considered Kansan. Bain (1895) studied the relationships of the drift sheets at Afton Junction and traced the drift in southern Polk County southward and concluded that it correlated with the upper drift at Afton.…”

Section: History Of the Lowan Areamentioning

confidence: 99%

“…The upper till became Kansan, the lower till pre-Aftonian, and the peat and gravel retained the name Aftonian (Bain, 1895;Chamberlin, 1896).…”

Section: History Of the Lowan Areamentioning

confidence: 99%

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Characterization of the loamy surficial sediments in a type area of the Iowan Erosion Surface

Wysocki

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Characterization of the Loamy Surficial Sediments within the Study Area 146 Origin of the sediments 148 Geomorphic and time setting 148 Loamy Sediments on the lowan Erosion Surface 150 Ruhe's Model of Landscape Evolution 152 Suggestions for Further Study of the Surficial Loamy Sediments 152 LITERATURE CITED 155 ACKNOWLEDGMENTS 163 APPENDIX A. SOIL PROFILE DESCRIPTIONS 165 List of Abbreviations 165 Texture 165 Mottles 165 Structure 165 Consistence 165 Clay films 166 Transect 4 Clay % = 26.6 e (2.79 X 10)(Distance) 53 Clay Content 20 (5.86 X Clay % = 23.6 e .56 (1.82 X 10)(Distance) Clay % = 21.1

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Section: History Of the Lowan Areamentioning

confidence: 99%

Section: History Of the Lowan Areamentioning

confidence: 99%

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Characterization of the loamy surficial sediments in a type area of the Iowan Erosion Surface

Wysocki

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“…Chamberlin (1895), Calvin (1899Calvin ( , 1911, Bain (1895), Alden and Leighton (1917), and Kay and Apfel (1929) developed the con cept of the lowan drift. showed that the lowan drift did not exist and replaced this concept with the concept of an erosion surface.…”

Section: Summary Of the Introductionmentioning

confidence: 99%

Characterization of the loamy surficial sediments in a type area of the Iowan Erosion Surface

Wysocki

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Pre-Wisconsin glacial stratigraphy of the central plains region in Iowa, Nebraska, Kansas, and Missouri

Hallberg¹

1986

Quaternary Science Reviews

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Relations of the Wisconsin and Kansan Drift Sheets in Central Iowa, and Related Phenomena

Cited by 6 publications

References 0 publications

Characterization of the loamy surficial sediments in a type area of the Iowan Erosion Surface

Characterization of the loamy surficial sediments in a type area of the Iowan Erosion Surface

Characterization of the loamy surficial sediments in a type area of the Iowan Erosion Surface

Pre-Wisconsin glacial stratigraphy of the central plains region in Iowa, Nebraska, Kansas, and Missouri

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