This is the first of a two-part report dealing primarily with the Devonian strata in the subsurface of extreme southeastern Iowa. In this portion, the 1ithostratigraphic relationships between three cores from Des Moines and Lee Counties are discussed (see fig. 1). The second part of this report will be concerned primarily with the biostratigraphic aspects of the examined cores
A recently discovered exposure of fossiliferous beds of Upper Devonian age in Iowa County, Iowa, con...
Nine stratigraphic sections of the Cedar Valley Formation were studied in Black Hawk, Buchanan and B...
Recent grading of a road in Jackson county, Iowa, led to the uncovering and subsequent discovery of ...
Rock samples were collected from the Bertram Member of the Wapsipinicon Formation in six quarries in...
In a report recently made to the State Geological Survey, the writer communicates in detail some fac...
The Devonian System, in Iowa, is exposed in a belt about 50 miles wide extending along a line from M...
The principal exposures of the Upper Devonian Shell Rock Formation occur along the Shell Rock River ...
The most important geological discovery in Iowa in recent years is the revelation that our Devonic d...
This paper is a renewal of a practice carried on by L. W. Wood in the 1930s, that of presenting each...
The great Devonic limestone succession in Iowa was long treated as if it were a single stratigraphic...
Numerous spore-like bodies have been observed in the Cedar Valley formation of Late Devonian age dur...
In examining the rock exposures in a quarry near the village of Robins, Linn County, Iowa, Mr. R. B....
It is a well-known characteristic of the Devonian limestones that to an extraordinary degree they ha...
During a temporary employment period (May 16 - September 15, 1980) with the Iowa Geological Survey, ...
A recently discovered exposure of fossiliferous beds of Upper Devonian age in Iowa County, Iowa, con...
Nine stratigraphic sections of the Cedar Valley Formation were studied in Black Hawk, Buchanan and B...
Recent grading of a road in Jackson county, Iowa, led to the uncovering and subsequent discovery of ...
Rock samples were collected from the Bertram Member of the Wapsipinicon Formation in six quarries in...
In a report recently made to the State Geological Survey, the writer communicates in detail some fac...
The Devonian System, in Iowa, is exposed in a belt about 50 miles wide extending along a line from M...
The principal exposures of the Upper Devonian Shell Rock Formation occur along the Shell Rock River ...
The most important geological discovery in Iowa in recent years is the revelation that our Devonic d...
This paper is a renewal of a practice carried on by L. W. Wood in the 1930s, that of presenting each...
The great Devonic limestone succession in Iowa was long treated as if it were a single stratigraphic...
Numerous spore-like bodies have been observed in the Cedar Valley formation of Late Devonian age dur...
In examining the rock exposures in a quarry near the village of Robins, Linn County, Iowa, Mr. R. B....
It is a well-known characteristic of the Devonian limestones that to an extraordinary degree they ha...
During a temporary employment period (May 16 - September 15, 1980) with the Iowa Geological Survey, ...
A recently discovered exposure of fossiliferous beds of Upper Devonian age in Iowa County, Iowa, con...
Nine stratigraphic sections of the Cedar Valley Formation were studied in Black Hawk, Buchanan and B...
Recent grading of a road in Jackson county, Iowa, led to the uncovering and subsequent discovery of ...