The area under consideration has a dimension of 8 miles east-west and 4 miles north-south, and includes the canyons of Spring Creek and Hobble Creek, Utah County, Utah. These streams flow off the west flank of a southern portion of the Wasatch Range, and have cut canyons to a depth of over 3,000 feet, exposing sections of upper Paleozoic sediments. Pennsylvanian rocks in the vicinity of the southern Wasatch Mountains have received little attention from stratigraphers. In this paper an attempt is made to describe the sequence of Pennsylvanian rocks in the region
Sections have been measured at Crystal River Ranch, Thompson Creek, Mount Sopris, Coal Creek and Sch...
The Canyon Group comprises an alternating sequence of limestone and shale formations, with sandstone...
The Paradox Basin of southeast Utah is characterized by a Late Pennsylvanian stratigraphic sequence ...
The area under consideration has a dimension of 8 miles east-west and 4 miles north-south, and inclu...
The Pennsylvanian strata of North Central Texas are divisible into three main lithostratigraphic uni...
Abstract: The Oquirrh Group of Pennsylvanian and Permian age in the southern East Tintic Mountains, ...
In 1948 Williams subdivided the Jefferson Formation of northeastern Utah into two formations. The up...
The strata of Pennsylvanian age in north-central Texas dip gently and uniformly to the northwest. Th...
The geological column in northern Utah has had very little detailed study. Those who have made repor...
The stratigraphic section in the report are begins with the Arapien shale, Upper Jurassic in age and...
A detailed geologic investigation was made of the eastern part of the Dairy Ridge Quadrangle and the...
The Swan Peak Formation in north-central Utah thickens westward, from zero feet near Logan to 687 fe...
thesisThe Promontory Range, Box Elder County, Utah,, is the first mountain range west of the north-c...
The strata of Pennsylvanian age in north-central Texas dip gently and uniformly to the northwest. Th...
The Summer Ranch and North Promontory Mountains have not been studied in detail geologically, althou...
Sections have been measured at Crystal River Ranch, Thompson Creek, Mount Sopris, Coal Creek and Sch...
The Canyon Group comprises an alternating sequence of limestone and shale formations, with sandstone...
The Paradox Basin of southeast Utah is characterized by a Late Pennsylvanian stratigraphic sequence ...
The area under consideration has a dimension of 8 miles east-west and 4 miles north-south, and inclu...
The Pennsylvanian strata of North Central Texas are divisible into three main lithostratigraphic uni...
Abstract: The Oquirrh Group of Pennsylvanian and Permian age in the southern East Tintic Mountains, ...
In 1948 Williams subdivided the Jefferson Formation of northeastern Utah into two formations. The up...
The strata of Pennsylvanian age in north-central Texas dip gently and uniformly to the northwest. Th...
The geological column in northern Utah has had very little detailed study. Those who have made repor...
The stratigraphic section in the report are begins with the Arapien shale, Upper Jurassic in age and...
A detailed geologic investigation was made of the eastern part of the Dairy Ridge Quadrangle and the...
The Swan Peak Formation in north-central Utah thickens westward, from zero feet near Logan to 687 fe...
thesisThe Promontory Range, Box Elder County, Utah,, is the first mountain range west of the north-c...
The strata of Pennsylvanian age in north-central Texas dip gently and uniformly to the northwest. Th...
The Summer Ranch and North Promontory Mountains have not been studied in detail geologically, althou...
Sections have been measured at Crystal River Ranch, Thompson Creek, Mount Sopris, Coal Creek and Sch...
The Canyon Group comprises an alternating sequence of limestone and shale formations, with sandstone...
The Paradox Basin of southeast Utah is characterized by a Late Pennsylvanian stratigraphic sequence ...