From the angle of genesis we lately have to modify some of our ideas on our Glacial till-sheets. Realizing that the continental ice-masses do not emanate from a single center, it is found that our Iowa tills come from what is known as the Keewatin center, on the west of Hudson Bay; while the tills on the east side of the Mississippi River originated mainly from the Labradoran center. The only invasion of ice from the last mentioned center is a slight one by the Illinoian ice, in the extreme southeastern part of our state
Johnson County offers a field of phenomena that are strikingly applicable to the theme of our late P...
Iowa has been repeatedly and so thoroughly planed off and worked over by continental glaciers of no ...
The observations from which these data were obtained were made in an excavation opened for the basem...
From the angle of genesis we lately have to modify some of our ideas on our Glacial till-sheets. Rea...
There is one glaciation that did not reach Iowa, the absence of which throws all into confusion. Thi...
The interglacial deposits of northeastern Iowa embrace the peat and forest bed which has been known ...
Iowa and the upper Mississippi basin are, as is now quite generally known, in possession of the most...
The discoveries of localities showing glacial scoring in southeastern Iowa have been somewhat numero...
The gravels related to the Iowan glaciation of northeastern Iowa have been studied in the field and ...
Opening a quarry on the southern edge of a Middle River bluff, the quarryman exposed 20 feet of the ...
In the third annual report of the Iowa Geological Survey Dr. C. R. Keyes has treated, at considerabl...
With the larger perspective of the Cretaceous formations recently opened out to the west of us, betw...
With the lower Minnesota valley blocked with ice, drainage from the waning Keewatin glacier, in sout...
The long period intervening between the deposit of the Cretaceous rocks of Iowa and the advent of th...
Organic remains in glacial drifts and interglacial deposits are relatively abundant in Iowa and serv...
Johnson County offers a field of phenomena that are strikingly applicable to the theme of our late P...
Iowa has been repeatedly and so thoroughly planed off and worked over by continental glaciers of no ...
The observations from which these data were obtained were made in an excavation opened for the basem...
From the angle of genesis we lately have to modify some of our ideas on our Glacial till-sheets. Rea...
There is one glaciation that did not reach Iowa, the absence of which throws all into confusion. Thi...
The interglacial deposits of northeastern Iowa embrace the peat and forest bed which has been known ...
Iowa and the upper Mississippi basin are, as is now quite generally known, in possession of the most...
The discoveries of localities showing glacial scoring in southeastern Iowa have been somewhat numero...
The gravels related to the Iowan glaciation of northeastern Iowa have been studied in the field and ...
Opening a quarry on the southern edge of a Middle River bluff, the quarryman exposed 20 feet of the ...
In the third annual report of the Iowa Geological Survey Dr. C. R. Keyes has treated, at considerabl...
With the larger perspective of the Cretaceous formations recently opened out to the west of us, betw...
With the lower Minnesota valley blocked with ice, drainage from the waning Keewatin glacier, in sout...
The long period intervening between the deposit of the Cretaceous rocks of Iowa and the advent of th...
Organic remains in glacial drifts and interglacial deposits are relatively abundant in Iowa and serv...
Johnson County offers a field of phenomena that are strikingly applicable to the theme of our late P...
Iowa has been repeatedly and so thoroughly planed off and worked over by continental glaciers of no ...
The observations from which these data were obtained were made in an excavation opened for the basem...