In the vicinity of Cedar Rapids there are extensive deposits of laminated sands within, and adjacent to the valley of the Cedar River and its tributaries. These lie above the till of the Iowan Substage and are associated for the most part with the highest terrace found along the Cedar River and its tributaries in Linn County. The presence of the laminated sediments has been noted by others, but no detailed study appears to have been made of them in the region of Cedar Rapids. During the active building program in Cedar Rapids many exposures were made in basement excavations and furnished a good opportunity for study
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
Linn is a junction of the Chicago, Rock Island and Pacific Railway, situated four miles northwest of...
In the vicinity of Cedar Rapids there are extensive deposits of laminated sands within, and adjacent...
Lying as it does near the border of the Iowan drift sheet, in hilly country deeply eroded by Cedar R...
In the early spring of 1921 as the writer was examining the face of the bluff bounding the north sid...
The most significant features that have been revealed by a study of the Pleistocene deposits in many...
The Pleistocene stratigraphy and sedimentology of two quarry exposures near Grand River and Decatur ...
Exposures of the Cedar Valley limestone adjacent to Iowa City show a wide variation from the conditi...
The Klein Quarry, in Johnson County, Iowa, exposes a unique section of Quaternary deposits. The sect...
1. A valuable series of exposures is now to be found along the, railroad from Des Moines to Allerton...
This paper includes descriptions and interpretations of drift sections which were made available for...
Two Pleistocene eolian deposits, the Loveland loess and the Peorian loess, have wide distribution in...
The entire surface of Audubon County is covered with a thick deposit of glacial drift, loess, etc. E...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
Linn is a junction of the Chicago, Rock Island and Pacific Railway, situated four miles northwest of...
In the vicinity of Cedar Rapids there are extensive deposits of laminated sands within, and adjacent...
Lying as it does near the border of the Iowan drift sheet, in hilly country deeply eroded by Cedar R...
In the early spring of 1921 as the writer was examining the face of the bluff bounding the north sid...
The most significant features that have been revealed by a study of the Pleistocene deposits in many...
The Pleistocene stratigraphy and sedimentology of two quarry exposures near Grand River and Decatur ...
Exposures of the Cedar Valley limestone adjacent to Iowa City show a wide variation from the conditi...
The Klein Quarry, in Johnson County, Iowa, exposes a unique section of Quaternary deposits. The sect...
1. A valuable series of exposures is now to be found along the, railroad from Des Moines to Allerton...
This paper includes descriptions and interpretations of drift sections which were made available for...
Two Pleistocene eolian deposits, the Loveland loess and the Peorian loess, have wide distribution in...
The entire surface of Audubon County is covered with a thick deposit of glacial drift, loess, etc. E...
Previous investigations in Pleistocene geology in Iowa have resulted in the development of the conce...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
Linn is a junction of the Chicago, Rock Island and Pacific Railway, situated four miles northwest of...