Nine stratigraphic sections of the Cedar Valley Formation were studied in Black Hawk, Buchanan and Benton counties in an attempt to better interpret the environment of deposition of the formation. Key environmental criteria for the interpretation of shallow water carbonate environments were recognized in the Cedar Valley Formation in the study area. The environment of deposition of the Solon Member is interpreted as entirely subtidal. The environment of deposition of the Rapid Member ranged from shallow subtidal to intertidal. The Coralville Member is interpreted as having been deposited in an environment that ranged from very shallow subtidal to intertidal and supratidal
The Osage Series in southeastern Iowa is composed primarily of cherty carbonate rocks. Thin shale be...
The Klein Quarry, in Johnson County, Iowa, exposes a unique section of Quaternary deposits. The sect...
A study of well samples from central Iowa shows that a distinct rock-stratigraphic unit is present b...
Nine stratigraphic sections of the Cedar Valley Formation were studied in Black Hawk, Buchanan and B...
Exposures of the Cedar Valley limestone adjacent to Iowa City show a wide variation from the conditi...
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....
The hydrogeology of the Devonian-Silurian carbonate aquifer was investigated at a hazardous waste si...
This is a guidebook for field conference of a culmination of a long series of cooperative investigat...
A layer of Wisconsin drift ranging up to 150 feet in thickness mantles the better part of the bedroc...
Recent quarry operations at Glory (N. E. ¼ Sec. 36 Spring Creek Twp., Black Hawk County, about 6 mil...
In a report recently made to the State Geological Survey, the writer communicates in detail some fac...
This paper is a renewal of a practice carried on by L. W. Wood in the 1930s, that of presenting each...
This is the first of a two-part report dealing primarily with the Devonian strata in the subsurface ...
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 Klein Quarry, in Johnson County, Iowa, exposes a unique section of Quaternary deposits. The sect...
A study of well samples from central Iowa shows that a distinct rock-stratigraphic unit is present b...
Nine stratigraphic sections of the Cedar Valley Formation were studied in Black Hawk, Buchanan and B...
Exposures of the Cedar Valley limestone adjacent to Iowa City show a wide variation from the conditi...
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....
The hydrogeology of the Devonian-Silurian carbonate aquifer was investigated at a hazardous waste si...
This is a guidebook for field conference of a culmination of a long series of cooperative investigat...
A layer of Wisconsin drift ranging up to 150 feet in thickness mantles the better part of the bedroc...
Recent quarry operations at Glory (N. E. ¼ Sec. 36 Spring Creek Twp., Black Hawk County, about 6 mil...
In a report recently made to the State Geological Survey, the writer communicates in detail some fac...
This paper is a renewal of a practice carried on by L. W. Wood in the 1930s, that of presenting each...
This is the first of a two-part report dealing primarily with the Devonian strata in the subsurface ...
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 Klein Quarry, in Johnson County, Iowa, exposes a unique section of Quaternary deposits. The sect...
A study of well samples from central Iowa shows that a distinct rock-stratigraphic unit is present b...