The area covered in this report lies between Mt. Taylor and the Rio Puerco, and embraces approximately 675 square miles. Much of it is readily accessible by either paved highways or improved roads. The general region is a land of numerous mesas, the largest of which is Mesa Chivato. Sandstones form prominent ridges while shales and alluvium form the valleys. Many volcanic plugs stand out as landmarks
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...
The northern part of the Ortiz Mountains of north-central New Mexico consists of a tilted fault bloc...
The White Rock Canyon area is in the Rio Grande depression in north-central New Mexico between paral...
The Rio Puerco, in the area of study, occupies a valley eroded in the Santa Fe formation. The silty ...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
The structural complexity of this area provided the initial stimulus for this study. With encouragem...
The Rio Puerco fault belt is a transitional feature between the Colorado Plateau and the Rio Grande ...
An area of about 1,300 square miles was mapped in parts of Rio Arriba, Sandoval, and McKinley Counti...
Emphasis has been placed in this work on the structural features of the southern part of the Fra Cri...
The Apache Hills, 10 km south of Hachita, New Mexico are a WNW-trending series of low hills, approxi...
p. 297-316, [10] leaves of plates (2 folded) : ill, map ; 24 cm.Includes bibliographical references....
This is a multi-disciplinary study that covers a variety of geoscience topics on both international ...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...
The northern part of the Ortiz Mountains of north-central New Mexico consists of a tilted fault bloc...
The White Rock Canyon area is in the Rio Grande depression in north-central New Mexico between paral...
The Rio Puerco, in the area of study, occupies a valley eroded in the Santa Fe formation. The silty ...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
The structural complexity of this area provided the initial stimulus for this study. With encouragem...
The Rio Puerco fault belt is a transitional feature between the Colorado Plateau and the Rio Grande ...
An area of about 1,300 square miles was mapped in parts of Rio Arriba, Sandoval, and McKinley Counti...
Emphasis has been placed in this work on the structural features of the southern part of the Fra Cri...
The Apache Hills, 10 km south of Hachita, New Mexico are a WNW-trending series of low hills, approxi...
p. 297-316, [10] leaves of plates (2 folded) : ill, map ; 24 cm.Includes bibliographical references....
This is a multi-disciplinary study that covers a variety of geoscience topics on both international ...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...