Add to ORKGNumerous low mounds of irregular shape in the v1cm1ty of Grand Mound and De Witt, Iowa, are glacial features coming under the category of kames. Twenty-two kames have been identified within an oblong area about two or three miles wide and 12 miles long, lying immediately south of the Chicago, Northwestern railroad and U. S. Highway 30 (see Figure l). The area extends eastward from about two miles east of the town of Calamus, passing south of the town of Grand Mound and continuing two miles southeast of the city of De Witt. Parts of the kame field lie in Olive, Orange and De Witt townships, Clinton county
An extensive road surfacing program in all the counties of northern Iowa for the past ten years or m...
At the last meeting of the Academy I called attention to an extension of the Wisconsin drift south, ...
Among the many interesting surface features of Iowa, there are few, if any, that have attracted more...
Numerous low mounds of irregular shape in the v1cm1ty of Grand Mound and De Witt, Iowa, are glacial ...
The object of this paper is to record the occurrence of four large boulders previously unnoted. Thei...
There is in eastern Iowa one short journey which shows a more interesting variety of land forms in s...
It is commonly understood that the Raccoon River, where it flows through Des Moines, lies just south...
McGhee, in the map accompanying his Pleistocene History of Northeastern Iowa, makes the Upper Till ...
Many new exposures have been made by the Chicago, Milwaukee and St. Paul Railway in the reconstructi...
When a boy, living on the border between the Iowan and the Loess-Kansan drift sheets, the great diff...
Union County already occupies a notable place in the annals of the Pleistocene geology of our State....
This paper includes descriptions and interpretations of drift sections which were made available for...
During the summer of 1936 a well was drilled for a municipal water supply at Larchwood, Lyon County....
The loess capped ridges associated with the Iowan glacial drift plain in northeast Iowa have been ca...
The principal moraine of this Wisconsin group in Iowa extends from the northeastern corner of Winneb...
An extensive road surfacing program in all the counties of northern Iowa for the past ten years or m...
At the last meeting of the Academy I called attention to an extension of the Wisconsin drift south, ...
Among the many interesting surface features of Iowa, there are few, if any, that have attracted more...
Numerous low mounds of irregular shape in the v1cm1ty of Grand Mound and De Witt, Iowa, are glacial ...
The object of this paper is to record the occurrence of four large boulders previously unnoted. Thei...
There is in eastern Iowa one short journey which shows a more interesting variety of land forms in s...
It is commonly understood that the Raccoon River, where it flows through Des Moines, lies just south...
McGhee, in the map accompanying his Pleistocene History of Northeastern Iowa, makes the Upper Till ...
Many new exposures have been made by the Chicago, Milwaukee and St. Paul Railway in the reconstructi...
When a boy, living on the border between the Iowan and the Loess-Kansan drift sheets, the great diff...
Union County already occupies a notable place in the annals of the Pleistocene geology of our State....
This paper includes descriptions and interpretations of drift sections which were made available for...
During the summer of 1936 a well was drilled for a municipal water supply at Larchwood, Lyon County....
The loess capped ridges associated with the Iowan glacial drift plain in northeast Iowa have been ca...
The principal moraine of this Wisconsin group in Iowa extends from the northeastern corner of Winneb...
An extensive road surfacing program in all the counties of northern Iowa for the past ten years or m...
At the last meeting of the Academy I called attention to an extension of the Wisconsin drift south, ...
Among the many interesting surface features of Iowa, there are few, if any, that have attracted more...