Emphasis has been placed in this work on the structural features of the southern part of the Fra Cristobal Range in order to extend the studies in the Caballo Mountains area and the McRae Canyon area. By mapping in detail the structure of the Fra Cristobal range it is hoped that a better understanding of the adjoining Rio Grande and Jornada del Muerto depressions may be reached. As an added contribution, a Permian section was measured as these rocks are relatively undeformed and very well exposed in some parts of the range. The field mapping was done in the spring and summer of 1954. Field data were plotted on aerial photographs to a scale of 1:31, 680 and subsequently transferred to a base map made from U.S. Soil Conservation Service P...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The Ladron Mountains are in a fault-block range consisting in large part of Pre-Cambrian rocks. They...
The area covered in this report lies between Mt. Taylor and the Rio Puerco, and embraces approximate...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
The White Rock Canyon area is in the Rio Grande depression in north-central New Mexico between paral...
The structural complexity of this area provided the initial stimulus for this study. With encouragem...
The Sangre de Cristo Mountains of Colorado and New Mexico are, geologically speaking, relatively unk...
The Rio Puerco fault belt is a transitional feature between the Colorado Plateau and the Rio Grande ...
The northern part of the Ortiz Mountains of north-central New Mexico consists of a tilted fault bloc...
The area included in this survey is that part of New Mexico between (and adjacent to) U. S. Highways...
This report represents a detailed study of the geology of a small area in the vicinity of Golden, Sa...
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
The Rio Puerco, in the area of study, occupies a valley eroded in the Santa Fe formation. The silty ...
The recent visits of a number of the members of the Academy to the Tulerosa district and contiguous ...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The Ladron Mountains are in a fault-block range consisting in large part of Pre-Cambrian rocks. They...
The area covered in this report lies between Mt. Taylor and the Rio Puerco, and embraces approximate...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
The White Rock Canyon area is in the Rio Grande depression in north-central New Mexico between paral...
The structural complexity of this area provided the initial stimulus for this study. With encouragem...
The Sangre de Cristo Mountains of Colorado and New Mexico are, geologically speaking, relatively unk...
The Rio Puerco fault belt is a transitional feature between the Colorado Plateau and the Rio Grande ...
The northern part of the Ortiz Mountains of north-central New Mexico consists of a tilted fault bloc...
The area included in this survey is that part of New Mexico between (and adjacent to) U. S. Highways...
This report represents a detailed study of the geology of a small area in the vicinity of Golden, Sa...
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
The Rio Puerco, in the area of study, occupies a valley eroded in the Santa Fe formation. The silty ...
The recent visits of a number of the members of the Academy to the Tulerosa district and contiguous ...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The Ladron Mountains are in a fault-block range consisting in large part of Pre-Cambrian rocks. They...
The area covered in this report lies between Mt. Taylor and the Rio Puerco, and embraces approximate...