The White Rock Canyon area is in the Rio Grande depression in north-central New Mexico between parallels 35 degrees 33\u27 and 35 degrees 53\u27 and meridians 106 degrees 4\u27 and 106 degrees 21\u27 (Figure 1). It occupies part of western Santa Fe County and eastern Sandoval County. The area was named for White Rock Canyon which has been formed by the Rio Grande. This canyon, called Caja del Rio by the Spanish, meaning box of the river , begins at the town of Buckman and extends southward as a narrow gorge for a distance of 19 miles. The area encloses 316 square miles, including parts of the Cerros del Rio, the Santo Domingo Valley and the Pajarito Plateau, part of which lies within the Bandelier National Monument
The northern part of the Ortiz Mountains of north-central New Mexico consists of a tilted fault bloc...
The area covered in this report lies between Mt. Taylor and the Rio Puerco, and embraces approximate...
Contents: Location and limitation of the District (p.7) -- Topography (p.7) -- The Chinati mountains...
Emphasis has been placed in this work on the structural features of the southern part of the Fra Cri...
The structural complexity of this area provided the initial stimulus for this study. With encouragem...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...
The Rio Puerco fault belt is a transitional feature between the Colorado Plateau and the Rio Grande ...
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 Rio Puerco, in the area of study, occupies a valley eroded in the Santa Fe formation. The silty ...
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
The area included in this report is in the north-central part of Torrance county, central New Mexico...
Pinto Canyon area includes the southern Tierra Vieja Mountains and the northern Chinati Mountains. L...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The northern part of the Ortiz Mountains of north-central New Mexico consists of a tilted fault bloc...
The area covered in this report lies between Mt. Taylor and the Rio Puerco, and embraces approximate...
Contents: Location and limitation of the District (p.7) -- Topography (p.7) -- The Chinati mountains...
Emphasis has been placed in this work on the structural features of the southern part of the Fra Cri...
The structural complexity of this area provided the initial stimulus for this study. With encouragem...
Approximately 5000 ft (1525 m) of strata crop out in the D Cross Mountain quadrangle in west-central...
The Rio Puerco fault belt is a transitional feature between the Colorado Plateau and the Rio Grande ...
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 Rio Puerco, in the area of study, occupies a valley eroded in the Santa Fe formation. The silty ...
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
The area included in this report is in the north-central part of Torrance county, central New Mexico...
Pinto Canyon area includes the southern Tierra Vieja Mountains and the northern Chinati Mountains. L...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The northern part of the Ortiz Mountains of north-central New Mexico consists of a tilted fault bloc...
The area covered in this report lies between Mt. Taylor and the Rio Puerco, and embraces approximate...
Contents: Location and limitation of the District (p.7) -- Topography (p.7) -- The Chinati mountains...