The term paha was first applied to isolated knobs and ridges within what we now know as the Iowan drift border by McGee, who refers to them as loess-capped eminences, sometimes elongated to ridges miles in length, sometimes shortened to elliptical hills, and again describes the individual paha as an elongated swell of soft and graceful contour, standing apart on the plain or else connected with its fellows sometimes in long lines, again in congeries, and locally merging to form broad loess plateaus
Some years ago in an article entitled The Loess and Its Fossils, the writer advanced certain opini...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
The southern margin of the main Iowan drift sheet extends in a sinuous line across the central porti...
The loess capped ridges associated with the Iowan glacial drift plain in northeast Iowa have been ca...
Loess is one of the most common geologic materials found on the land surface in the Midwest. This ca...
While exploring Adair County in the interest of the Iowa State Geological Survey, the writer made so...
A narrow band of unusual hills skirts the Missouri River valley along Iowa\u27s western border. The ...
When a stratified, loess-like gumbo, occurring along the Missouri River above Council Bluffs, was fi...
It is exceedingly unfortunate and disturbing that the loess deposits of our state should ever have b...
The narrow ridges and steep bluffs which extend in a narrow band along the Missouri Valley form the ...
One cannot work in the Iowan Drift area and in adjacent areas of older drift without confronting the...
McGee, Calvin, Bain, Todd, and other Iowa geologists, repeatedly direct attention to the occurrence ...
Some years ago in an article entitled The Loess and Its Fossils, the writer advanced certain opini...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
The southern margin of the main Iowan drift sheet extends in a sinuous line across the central porti...
The loess capped ridges associated with the Iowan glacial drift plain in northeast Iowa have been ca...
Loess is one of the most common geologic materials found on the land surface in the Midwest. This ca...
While exploring Adair County in the interest of the Iowa State Geological Survey, the writer made so...
A narrow band of unusual hills skirts the Missouri River valley along Iowa\u27s western border. The ...
When a stratified, loess-like gumbo, occurring along the Missouri River above Council Bluffs, was fi...
It is exceedingly unfortunate and disturbing that the loess deposits of our state should ever have b...
The narrow ridges and steep bluffs which extend in a narrow band along the Missouri Valley form the ...
One cannot work in the Iowan Drift area and in adjacent areas of older drift without confronting the...
McGee, Calvin, Bain, Todd, and other Iowa geologists, repeatedly direct attention to the occurrence ...
Some years ago in an article entitled The Loess and Its Fossils, the writer advanced certain opini...
The literature concerning the Pleistocene deposits of Iowa does not mention the presence of a loess ...
The southern margin of the main Iowan drift sheet extends in a sinuous line across the central porti...