On a lawn at No. 629 West Maple Avenue, in Centerville, Iowa, are located two large quartzose conglomerate boulders which are of more than usual interest. These were removed from the glacial till during the process of excavating for the cellar under the dwelling now situated on the same lot and when found were said to be buried beneath several feet of drift material
The discoveries of localities showing glacial scoring in southeastern Iowa have been somewhat numero...
A layer of Wisconsin drift ranging up to 150 feet in thickness mantles the better part of the bedroc...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
The object of this paper is to record the occurrence of four large boulders previously unnoted. Thei...
Large granite erratics, formerly attributed to the Iowan, are believed to be associated with the Kan...
Samples of the large granitic boulders of the Iowan drift were analyzed and features of the boulder ...
An extensive layer of limestone boulders was exposed by the steam shovels in getting out crushed roc...
A large rounded granitic glacial erratic from the Iowa State College campus has several granitic dik...
Throughout the drift mantled surface of Iowa, glaciated boulders of crystalline rocks are of common ...
Until very recently, geologists working in Iowa have been content to refer the various boulder clays...
During the prosecution of field study of the gypsum for the Iowa Geological Survey the writer found ...
Feulner, while mapping the bedrock of Clayton county during the summer of 1951, observed numerous la...
Opening a quarry on the southern edge of a Middle River bluff, the quarryman exposed 20 feet of the ...
The discoveries of localities showing glacial scoring in southeastern Iowa have been somewhat numero...
A layer of Wisconsin drift ranging up to 150 feet in thickness mantles the better part of the bedroc...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
The object of this paper is to record the occurrence of four large boulders previously unnoted. Thei...
Large granite erratics, formerly attributed to the Iowan, are believed to be associated with the Kan...
Samples of the large granitic boulders of the Iowan drift were analyzed and features of the boulder ...
An extensive layer of limestone boulders was exposed by the steam shovels in getting out crushed roc...
A large rounded granitic glacial erratic from the Iowa State College campus has several granitic dik...
Throughout the drift mantled surface of Iowa, glaciated boulders of crystalline rocks are of common ...
Until very recently, geologists working in Iowa have been content to refer the various boulder clays...
During the prosecution of field study of the gypsum for the Iowa Geological Survey the writer found ...
Feulner, while mapping the bedrock of Clayton county during the summer of 1951, observed numerous la...
Opening a quarry on the southern edge of a Middle River bluff, the quarryman exposed 20 feet of the ...
The discoveries of localities showing glacial scoring in southeastern Iowa have been somewhat numero...
A layer of Wisconsin drift ranging up to 150 feet in thickness mantles the better part of the bedroc...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...