Add to ORKG1. A valuable series of exposures is now to be found along the, railroad from Des Moines to Allerton. 2. A detailed description of some of the outcrops. 3. General observations and relations
Two Pleistocene eolian deposits, the Loveland loess and the Peorian loess, have wide distribution in...
In the vicinity of Cedar Rapids there are extensive deposits of laminated sands within, and adjacent...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
1. A valuable series of exposures is now to be found along the, railroad from Des Moines to Allerton...
In the early spring of 1921 as the writer was examining the face of the bluff bounding the north sid...
Lying as it does near the border of the Iowan drift sheet, in hilly country deeply eroded by Cedar R...
This paper includes descriptions and interpretations of drift sections which were made available for...
The most significant features that have been revealed by a study of the Pleistocene deposits in many...
The section is located on the line of the Wabash railway about two miles below the little station of...
The Pleistocene exposures on Capitol Hill at Des Moines have become classic through the studies made...
Many new exposures have been made by the Chicago, Milwaukee and St. Paul Railway in the reconstructi...
The finds described in this preliminary report represent skeletal material brought to the surface du...
At the time of the meeting of the Iowa Academy of Science at Drake University, Des Moines, in April,...
While exploring Adair County in the interest of the Iowa State Geological Survey, the writer made so...
The Pleistocene stratigraphy and sedimentology of two quarry exposures near Grand River and Decatur ...
Two Pleistocene eolian deposits, the Loveland loess and the Peorian loess, have wide distribution in...
In the vicinity of Cedar Rapids there are extensive deposits of laminated sands within, and adjacent...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
1. A valuable series of exposures is now to be found along the, railroad from Des Moines to Allerton...
In the early spring of 1921 as the writer was examining the face of the bluff bounding the north sid...
Lying as it does near the border of the Iowan drift sheet, in hilly country deeply eroded by Cedar R...
This paper includes descriptions and interpretations of drift sections which were made available for...
The most significant features that have been revealed by a study of the Pleistocene deposits in many...
The section is located on the line of the Wabash railway about two miles below the little station of...
The Pleistocene exposures on Capitol Hill at Des Moines have become classic through the studies made...
Many new exposures have been made by the Chicago, Milwaukee and St. Paul Railway in the reconstructi...
The finds described in this preliminary report represent skeletal material brought to the surface du...
At the time of the meeting of the Iowa Academy of Science at Drake University, Des Moines, in April,...
While exploring Adair County in the interest of the Iowa State Geological Survey, the writer made so...
The Pleistocene stratigraphy and sedimentology of two quarry exposures near Grand River and Decatur ...
Two Pleistocene eolian deposits, the Loveland loess and the Peorian loess, have wide distribution in...
In the vicinity of Cedar Rapids there are extensive deposits of laminated sands within, and adjacent...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...