This report represents a detailed study of the geology of a small area in the vicinity of Golden, Santa Fe County, New Mexico. The area is one of low hills, dissected by numerous small arroyos, lying between the Ortiz Mountains on the north and the San Pedro Mountains on the south. To the west the area merges into the Hagan Coal Basin, and to the east the low pass between the mountains descends into the headwaters of Galisteo Creek and into the Estanica Valley
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
Northeastern New Mexico is one of the most diverse natural landscapes in the state. Large volcanic v...
The Summit Mountains and surrounding region is on the Arizona-New Mexico state line about 25 km nort...
The area included in this report is in the north-central part of Torrance county, central New Mexico...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The structural complexity of this area provided the initial stimulus for this study. With encouragem...
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...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
The Ladron Mountains are in a fault-block range consisting in large part of Pre-Cambrian rocks. They...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
The Lone Star deposit is located in La Bajada Canyon in western Santa Fe County, New Mexico. The exp...
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...
This report summarizes the geology and geomorphology of 12 small watersheds in the Peloncillo Mounta...
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
Northeastern New Mexico is one of the most diverse natural landscapes in the state. Large volcanic v...
The Summit Mountains and surrounding region is on the Arizona-New Mexico state line about 25 km nort...
The area included in this report is in the north-central part of Torrance county, central New Mexico...
The field investigation for this report was initiated in October 1952 and was continued intermittent...
The structural complexity of this area provided the initial stimulus for this study. With encouragem...
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...
This report includes about seven square miles of the central front of the Fra Cristobal Mountains. T...
The Ladron Mountains are in a fault-block range consisting in large part of Pre-Cambrian rocks. They...
The northern part of the Fra Cristobal Range contains rocks of Precambrian, Cambrian, Pennsylvanian,...
The Lone Star deposit is located in La Bajada Canyon in western Santa Fe County, New Mexico. The exp...
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...
This report summarizes the geology and geomorphology of 12 small watersheds in the Peloncillo Mounta...
The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred d...
Northeastern New Mexico is one of the most diverse natural landscapes in the state. Large volcanic v...
The Summit Mountains and surrounding region is on the Arizona-New Mexico state line about 25 km nort...