The observations from which these data were obtained were made in an excavation opened for the basement of Wesley Foundation building just south of the athletic field of Iowa State College on Lincoln Way. The uppermost deposit which is found everywhere on the upland in the vicinity of Ames, is the Wisconsin till, most of which at this place had been removed by erosion prior to the beginning of the work. A zone of red soil about two feet thick just beneath this till serves as an unmistakable indicator of the plane of separation between it and the Kansan till below
Organic remains in glacial drifts and interglacial deposits are relatively abundant in Iowa and serv...
Five rock bodies and four major erosional surfaces are recognized in the subsurface; these are a low...
A large rounded granitic glacial erratic from the Iowa State College campus has several granitic dik...
The observations from which these data were obtained were made in an excavation opened for the basem...
Opening a quarry on the southern edge of a Middle River bluff, the quarryman exposed 20 feet of the ...
Until very recently, geologists working in Iowa have been content to refer the various boulder clays...
The long period intervening between the deposit of the Cretaceous rocks of Iowa and the advent of th...
In the third annual report of the Iowa Geological Survey Dr. C. R. Keyes has treated, at considerabl...
During the past summer the author made a series of observations, at the request of Prof. S. Calvin, ...
From the angle of genesis we lately have to modify some of our ideas on our Glacial till-sheets. Rea...
Some of the larger valleys of pre-glacial and inter-glacial topography have been located and describ...
The discoveries of localities showing glacial scoring in southeastern Iowa have been somewhat numero...
In June, 1960, a 2-ft. post-Kansan peat deposit was exposed in a building excavation in Grinnell (Po...
The gravels related to the Iowan glaciation of northeastern Iowa have been studied in the field and ...
The object of this paper is to record the occurrence of four large boulders previously unnoted. Thei...
Organic remains in glacial drifts and interglacial deposits are relatively abundant in Iowa and serv...
Five rock bodies and four major erosional surfaces are recognized in the subsurface; these are a low...
A large rounded granitic glacial erratic from the Iowa State College campus has several granitic dik...
The observations from which these data were obtained were made in an excavation opened for the basem...
Opening a quarry on the southern edge of a Middle River bluff, the quarryman exposed 20 feet of the ...
Until very recently, geologists working in Iowa have been content to refer the various boulder clays...
The long period intervening between the deposit of the Cretaceous rocks of Iowa and the advent of th...
In the third annual report of the Iowa Geological Survey Dr. C. R. Keyes has treated, at considerabl...
During the past summer the author made a series of observations, at the request of Prof. S. Calvin, ...
From the angle of genesis we lately have to modify some of our ideas on our Glacial till-sheets. Rea...
Some of the larger valleys of pre-glacial and inter-glacial topography have been located and describ...
The discoveries of localities showing glacial scoring in southeastern Iowa have been somewhat numero...
In June, 1960, a 2-ft. post-Kansan peat deposit was exposed in a building excavation in Grinnell (Po...
The gravels related to the Iowan glaciation of northeastern Iowa have been studied in the field and ...
The object of this paper is to record the occurrence of four large boulders previously unnoted. Thei...
Organic remains in glacial drifts and interglacial deposits are relatively abundant in Iowa and serv...
Five rock bodies and four major erosional surfaces are recognized in the subsurface; these are a low...
A large rounded granitic glacial erratic from the Iowa State College campus has several granitic dik...