The rocks of the Galena Group have proved to be problematic in correlation. This problem is due to a variable lithofacies development. A preliminary investigation, although based upon exposures studied just within Winneshiek County, provides a method for field identification in Iowa of stratigraphic units currently used by the Illinois State Geological Survey within Illinois. Units under consideration at this time are restricted to the Dunleith, Wise Lake, and Dubuque Formations. Methods of identification and correlation employ in part such physical features as sequences of nodular chart bands, discontinuity surfaces, and sparry calcarenite bands. Investigation has disclosed a close relationship of these three features. A composite graphic ...
The Osage Series in southeastern Iowa is composed primarily of cherty carbonate rocks. Thin shale be...
The purpose of this paper is to show the stratigraphic relations of the Greenhorn and Niobrara forma...
In Story County the glacial drift rests directly upon both Pennsylvanian and Mississippian rocks. Th...
The rocks of the Galena Group have proved to be problematic in correlation. This problem is due to a...
During the summer of 1956 the authors undertook an extensive study of the Pennsylvanian rocks expose...
In his report on the geology of Lee county Keyes described a fine-grained, compact limestone at the ...
Iowa geologists have long experienced great difficulty in isolating good key beds in the younger Pen...
In the consideration of the broader taxonomic aspects of the general geologic section of the rocks o...
Use of the Glen Dean limestone as a structural key horizon in the Illinois basin by George V. Cohee....
Formational units of the Meramec Series are present only in the southwestern portion and along the s...
The Dubuque Formation of Upper Ordovician age crops out in the Upper Mississippi Valley. It comprise...
A layer of Wisconsin drift ranging up to 150 feet in thickness mantles the better part of the bedroc...
Much new information concerning the underground geology of Iowa is being accumulated by the Iowa Geo...
In recapitulation: Taxonomic analysis of the problem of the Galena limestone shows that, (1) In conc...
An area in southeast Linn County, Iowa is discussed in which a number of geological units from the C...
The Osage Series in southeastern Iowa is composed primarily of cherty carbonate rocks. Thin shale be...
The purpose of this paper is to show the stratigraphic relations of the Greenhorn and Niobrara forma...
In Story County the glacial drift rests directly upon both Pennsylvanian and Mississippian rocks. Th...
The rocks of the Galena Group have proved to be problematic in correlation. This problem is due to a...
During the summer of 1956 the authors undertook an extensive study of the Pennsylvanian rocks expose...
In his report on the geology of Lee county Keyes described a fine-grained, compact limestone at the ...
Iowa geologists have long experienced great difficulty in isolating good key beds in the younger Pen...
In the consideration of the broader taxonomic aspects of the general geologic section of the rocks o...
Use of the Glen Dean limestone as a structural key horizon in the Illinois basin by George V. Cohee....
Formational units of the Meramec Series are present only in the southwestern portion and along the s...
The Dubuque Formation of Upper Ordovician age crops out in the Upper Mississippi Valley. It comprise...
A layer of Wisconsin drift ranging up to 150 feet in thickness mantles the better part of the bedroc...
Much new information concerning the underground geology of Iowa is being accumulated by the Iowa Geo...
In recapitulation: Taxonomic analysis of the problem of the Galena limestone shows that, (1) In conc...
An area in southeast Linn County, Iowa is discussed in which a number of geological units from the C...
The Osage Series in southeastern Iowa is composed primarily of cherty carbonate rocks. Thin shale be...
The purpose of this paper is to show the stratigraphic relations of the Greenhorn and Niobrara forma...
In Story County the glacial drift rests directly upon both Pennsylvanian and Mississippian rocks. Th...