The Humboldt stages, like the Algona stages consist of a series of recessional moraines some of which are smaller than others, and some of which are poorly defined and irregular or missing in places. They are somewhat concentrically parallel to each other and are disposed at distances varying from two to eight miles apart along a main axial direction which extends southward near the east branch of the Des Moines river from southern Kossuth county to Humboldt, and along the Des Moines river south of Humboldt to Fort Dodge. Toward the places of union with the Gary moraine both eastward and westward the several moraines of this group converge to some extent
The purpose of this paper is to show the stratigraphic relations of the Greenhorn and Niobrara forma...
The Iowan lobe of the Wisconsin glaciation is located in northeastern Iowa. Evidence is summarized w...
Iowa and the upper Mississippi basin are, as is now quite generally known, in possession of the most...
The Humboldt stages, like the Algona stages consist of a series of recessional moraines some of whic...
The principal moraine of this Wisconsin group in Iowa extends from the northeastern corner of Winneb...
The city of Algona is the best known locality near the maximum southern extent of these recessional ...
This map shows the positions of the margin, of the recessional stages and of the substages respectiv...
A definite moraine extends southeastward across the southwestern township of Butler County to centra...
Immediately following the time that the Altamont moraine was formed there was an intermittent retrea...
The several major and many more minor recessional moraines are discussed with respect to their locat...
With the lower Minnesota valley blocked with ice, drainage from the waning Keewatin glacier, in sout...
There is one glaciation that did not reach Iowa, the absence of which throws all into confusion. Thi...
The gravels related to the Iowan glaciation of northeastern Iowa have been studied in the field and ...
Calculated upon the basis of Bruckner climatological cycle of 33 years, the retreat of the Des Moine...
From the angle of genesis we lately have to modify some of our ideas on our Glacial till-sheets. Rea...
The purpose of this paper is to show the stratigraphic relations of the Greenhorn and Niobrara forma...
The Iowan lobe of the Wisconsin glaciation is located in northeastern Iowa. Evidence is summarized w...
Iowa and the upper Mississippi basin are, as is now quite generally known, in possession of the most...
The Humboldt stages, like the Algona stages consist of a series of recessional moraines some of whic...
The principal moraine of this Wisconsin group in Iowa extends from the northeastern corner of Winneb...
The city of Algona is the best known locality near the maximum southern extent of these recessional ...
This map shows the positions of the margin, of the recessional stages and of the substages respectiv...
A definite moraine extends southeastward across the southwestern township of Butler County to centra...
Immediately following the time that the Altamont moraine was formed there was an intermittent retrea...
The several major and many more minor recessional moraines are discussed with respect to their locat...
With the lower Minnesota valley blocked with ice, drainage from the waning Keewatin glacier, in sout...
There is one glaciation that did not reach Iowa, the absence of which throws all into confusion. Thi...
The gravels related to the Iowan glaciation of northeastern Iowa have been studied in the field and ...
Calculated upon the basis of Bruckner climatological cycle of 33 years, the retreat of the Des Moine...
From the angle of genesis we lately have to modify some of our ideas on our Glacial till-sheets. Rea...
The purpose of this paper is to show the stratigraphic relations of the Greenhorn and Niobrara forma...
The Iowan lobe of the Wisconsin glaciation is located in northeastern Iowa. Evidence is summarized w...
Iowa and the upper Mississippi basin are, as is now quite generally known, in possession of the most...