This report summarizes existing data on the DeForest Formation (Holocene alluvium) of western Iowa and presents a model aimed at understanding the causative factors behind long-term behavior of the fluvial system in the area. Investigations in six western Iowa watersheds are summarized and results are compared in order to gain an appreciation for both the overall stratigraphic and geomorphic similarity across the region, as well as the degree of local variability resulting from loess thickness patterns, geologic history, and stream size
This paper is a continuation of the work previously reported by Dahl, Handy and Davidson (1), and su...
The narrow ridges and steep bluffs which extend in a narrow band along the Missouri Valley form the ...
Two Pleistocene eolian deposits, the Loveland loess and the Peorian loess, have wide distribution in...
Holocene-age alluvial deposits were studied on the Iowan Surface in a small perennial stream with a ...
This is a guidebook for field conference of a culmination of a long series of cooperative investigat...
The Klein Quarry, in Johnson County, Iowa, exposes a unique section of Quaternary deposits. The sect...
This bulletin reports a 1957-1960 study of landscapes, soils, entrenched streams, and gullies in par...
This bulletin tells how natural erosion has helped shape the landscapes of southwestern Iowa and aff...
The Pleistocene stratigraphy and sedimentology of two quarry exposures near Grand River and Decatur ...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
The Soil Research Laboratory of the Iowa Engineering Experiment Station has been studying areal and ...
As part of a long-range project to investigate the stabilization of loess and glacial till for low c...
Several Wisconsin Loess sections were described before the Iowa Academy of Science in 1953 (1), and ...
This paper describes the type locality and type section for the Honey Creek Member, a stratigraphic ...
The primary purposes of this investigation are: 1) To delineate flood plain deposits with different...
This paper is a continuation of the work previously reported by Dahl, Handy and Davidson (1), and su...
The narrow ridges and steep bluffs which extend in a narrow band along the Missouri Valley form the ...
Two Pleistocene eolian deposits, the Loveland loess and the Peorian loess, have wide distribution in...
Holocene-age alluvial deposits were studied on the Iowan Surface in a small perennial stream with a ...
This is a guidebook for field conference of a culmination of a long series of cooperative investigat...
The Klein Quarry, in Johnson County, Iowa, exposes a unique section of Quaternary deposits. The sect...
This bulletin reports a 1957-1960 study of landscapes, soils, entrenched streams, and gullies in par...
This bulletin tells how natural erosion has helped shape the landscapes of southwestern Iowa and aff...
The Pleistocene stratigraphy and sedimentology of two quarry exposures near Grand River and Decatur ...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
The Soil Research Laboratory of the Iowa Engineering Experiment Station has been studying areal and ...
As part of a long-range project to investigate the stabilization of loess and glacial till for low c...
Several Wisconsin Loess sections were described before the Iowa Academy of Science in 1953 (1), and ...
This paper describes the type locality and type section for the Honey Creek Member, a stratigraphic ...
The primary purposes of this investigation are: 1) To delineate flood plain deposits with different...
This paper is a continuation of the work previously reported by Dahl, Handy and Davidson (1), and su...
The narrow ridges and steep bluffs which extend in a narrow band along the Missouri Valley form the ...
Two Pleistocene eolian deposits, the Loveland loess and the Peorian loess, have wide distribution in...