In the general section of the coal measures of Iowa, Missouri and Kansas there are two unconformities which are really quite notable in our stratigraphy. One of these, the one at the base of coal measures, receives wide consideration from earliest days, albeit its sedimental equivalency and time-expression is little regarded. That there is another unconformity within the Carbonic section, hardly less notable than the first one mentioned, at the base of the Bethany limestones bevelling all the productive coal section is a very much more recent realization
The principal coal-bearing formation of Iowa and other parts of the western interior basin is the lo...
The shallow synclinal disposition of the coal measures of southwestern Iowa is a theme of much past ...
The district at hand is one somewhat remote from any known field of productive Coal Measures, but be...
In the general section of the coal measures of Iowa, Missouri and Kansas there are two unconformitie...
In Missouri the base of the Henrietta group is drawn at the base of the Lower Fort Scott limestone. ...
On the general geological map of Iowa there are three peculiarities in the areal distribution of the...
For a long time it has been known that in Iowa and the neighboring states to the south a break in se...
Several years ago while studying the coal measures of Iowa and the neighboring states, it was sugges...
The exposed stratified rocks of central Iowa are made up chiefly of Lower Coal Measure clays, shales...
Recent diastatic analyses of our Des Moines coal measures, particularly of the great Arkansan centru...
The lower measures of the Iowa-Missouri coal field consist of a series of sandstones, shales, fire c...
Late studies of the Mississippian formations of southeastern Iowa for the Iowa Geological Survey hav...
Iowa geologists have long experienced great difficulty in isolating good key beds in the younger Pen...
A detailed discussion of problems and ambiguities of stratigraphic nomenclature and terminology as i...
In its broader, or continental, relationships, the chronologic position of our Iowa Productive coal ...
The principal coal-bearing formation of Iowa and other parts of the western interior basin is the lo...
The shallow synclinal disposition of the coal measures of southwestern Iowa is a theme of much past ...
The district at hand is one somewhat remote from any known field of productive Coal Measures, but be...
In the general section of the coal measures of Iowa, Missouri and Kansas there are two unconformitie...
In Missouri the base of the Henrietta group is drawn at the base of the Lower Fort Scott limestone. ...
On the general geological map of Iowa there are three peculiarities in the areal distribution of the...
For a long time it has been known that in Iowa and the neighboring states to the south a break in se...
Several years ago while studying the coal measures of Iowa and the neighboring states, it was sugges...
The exposed stratified rocks of central Iowa are made up chiefly of Lower Coal Measure clays, shales...
Recent diastatic analyses of our Des Moines coal measures, particularly of the great Arkansan centru...
The lower measures of the Iowa-Missouri coal field consist of a series of sandstones, shales, fire c...
Late studies of the Mississippian formations of southeastern Iowa for the Iowa Geological Survey hav...
Iowa geologists have long experienced great difficulty in isolating good key beds in the younger Pen...
A detailed discussion of problems and ambiguities of stratigraphic nomenclature and terminology as i...
In its broader, or continental, relationships, the chronologic position of our Iowa Productive coal ...
The principal coal-bearing formation of Iowa and other parts of the western interior basin is the lo...
The shallow synclinal disposition of the coal measures of southwestern Iowa is a theme of much past ...
The district at hand is one somewhat remote from any known field of productive Coal Measures, but be...