he Aftonian deposits of southwestern Iowa have peculiar interest in that within the area is the type locality for the Aftonian. So far neither the drift of the region nor the Aftonian as a unit has received a general discussion. The references to the beds extant are merely incidental to broader studies. The type locality and several other critical exposures have been visited by many geologists but no one has presented a complete account of the beds in question
McGhee, in the map accompanying his Pleistocene History of Northeastern Iowa, makes the Upper Till ...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
The entire surface of Audubon County is covered with a thick deposit of glacial drift, loess, etc. E...
Until very recently, geologists working in Iowa have been content to refer the various boulder clays...
Organic remains in glacial drifts and interglacial deposits are relatively abundant in Iowa and serv...
Union County already occupies a notable place in the annals of the Pleistocene geology of our State....
The interglacial deposits of northeastern Iowa embrace the peat and forest bed which has been known ...
The long period intervening between the deposit of the Cretaceous rocks of Iowa and the advent of th...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
This paper includes descriptions and interpretations of drift sections which were made available for...
Johnson County offers a field of phenomena that are strikingly applicable to the theme of our late P...
One cannot work in the Iowan Drift area and in adjacent areas of older drift without confronting the...
Many new exposures have been made by the Chicago, Milwaukee and St. Paul Railway in the reconstructi...
In making an excavation through a low ridge just east of Oelwein, in Fayette county, the workmen of ...
The work of Professor Shimek, of the Iowa Geological Survey, in western Iowa, has brought to light m...
McGhee, in the map accompanying his Pleistocene History of Northeastern Iowa, makes the Upper Till ...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
The entire surface of Audubon County is covered with a thick deposit of glacial drift, loess, etc. E...
Until very recently, geologists working in Iowa have been content to refer the various boulder clays...
Organic remains in glacial drifts and interglacial deposits are relatively abundant in Iowa and serv...
Union County already occupies a notable place in the annals of the Pleistocene geology of our State....
The interglacial deposits of northeastern Iowa embrace the peat and forest bed which has been known ...
The long period intervening between the deposit of the Cretaceous rocks of Iowa and the advent of th...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
This paper includes descriptions and interpretations of drift sections which were made available for...
Johnson County offers a field of phenomena that are strikingly applicable to the theme of our late P...
One cannot work in the Iowan Drift area and in adjacent areas of older drift without confronting the...
Many new exposures have been made by the Chicago, Milwaukee and St. Paul Railway in the reconstructi...
In making an excavation through a low ridge just east of Oelwein, in Fayette county, the workmen of ...
The work of Professor Shimek, of the Iowa Geological Survey, in western Iowa, has brought to light m...
McGhee, in the map accompanying his Pleistocene History of Northeastern Iowa, makes the Upper Till ...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
The entire surface of Audubon County is covered with a thick deposit of glacial drift, loess, etc. E...