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Articles 61 - 74 of 74

Full-Text Articles in Other Earth Sciences

The Structural Geology Of The Cerrillos Hills Area, New Mexico, Alan E. Disbrow May 1953

The Structural Geology Of The Cerrillos Hills Area, New Mexico, Alan E. Disbrow

Earth and Planetary Sciences ETDs

The earliest major structural deformation recorded in rocks exposed in the Cerrillos area occurred during the Laramie uplift of the Sangre de Cristo Mountains. This resulted in an erosional wedging of Upper Cretaceous strata at a rate of 130 feet per mile. Subsequent deposition of the Eocene Galisteo sand, clay, and gravel overstepped this surface in a sourceward direction.

At the beginning of work on this project the major problem was to determine the geological structure of the Cerrillos Hills. It was felt that a large-scale geologic map of an area extensive enough to reveal the structurally complex center of …


The Huego (Gym) Limestone, Luna County, New Mexico, Lowell E. Bogart May 1953

The Huego (Gym) Limestone, Luna County, New Mexico, Lowell E. Bogart

Earth and Planetary Sciences ETDs

Southwestern New Mexico is characterized by Basin and Range Physiography. Nearly level bolson plains are interrupted irregularly by linear mountain ranges. Sedimentary rocks ranging in age from Cambrian and recent crop out in the mountain areas. Darton (1916) mapped and described a limestone formation, about 1,000 feet thick, which he named Gym limestone. He thought the Gym was restricted in outcrop to Luna County and was distinct from previously described Paleozoic formations. The Gym was originally thought to be Pennsylvanian in age but later on was regarded as Permian. In the restudy of the Gym limestone was the basis of …


Geology Of The Mcrae Canyon Area Sierra County, New Mexico, Hugh P. Bushnell May 1953

Geology Of The Mcrae Canyon Area Sierra County, New Mexico, Hugh P. Bushnell

Earth and Planetary Sciences ETDs

Sedimentary Rocks exposed at the surface in the low area between the north-trending Caballo and Fra Cristobal Mountains of south-central New Mexico include the late Cretaceous Mesaverde formation, the late Cretaceous and early Tertiary McRae formation, and the Miocene-Pliocene Santa Fe formation. A thin veneer of Jordana pediment gravel covers the older rocks on the eastern edge of the area.


Jade: Its Occurrences, Mineralogy, Geology, Uses And Technology, Robert L. Borton May 1952

Jade: Its Occurrences, Mineralogy, Geology, Uses And Technology, Robert L. Borton

Earth and Planetary Sciences ETDs

No abstract provided.


The Study Of An Unusual Augite Near Cabezon Peak, Sandoval County, New Mexico, George Brunton May 1952

The Study Of An Unusual Augite Near Cabezon Peak, Sandoval County, New Mexico, George Brunton

Earth and Planetary Sciences ETDs

When the writer was examining some of the volcanic plugs near Cabezon, New Mexico in the spring of 1951, he discovered in Plug No. 5 (Pl. 2, D.W. Johnson, 1907) some unusual, large vitreous inclusions.


A New Basic Copper Phosphate Mineral From Santa Rita, New Mexico, David B. Givens Dec 1951

A New Basic Copper Phosphate Mineral From Santa Rita, New Mexico, David B. Givens

Earth and Planetary Sciences ETDs

Supergene minerals are not common, nor are they rare at Santa Rita, New Mexico. Kerr (1950,307) reports the presence of cuprite, melaconite, native copper, chrysocolla, machite and azurite. There is also smithsonite present.

The physical appearance of the mineral, coupled with preliminary determinations of the indices of refraction, gave a rough correspondence with dihydrite (Larson and Berman, 1934, 135). However, enough discrepancy existed to warrant taking powder and Weissenberg X-Ray pictures. From these it was evident immediately that the specimen was a new mineral species.


A Study Of The Breece, New Mexico, Hishikari, Japan And Mino, Japan Meteorites, Louis H. Goldsmith May 1950

A Study Of The Breece, New Mexico, Hishikari, Japan And Mino, Japan Meteorites, Louis H. Goldsmith

Earth and Planetary Sciences ETDs

In this thesis are given the details concerning the falls of three meteorites, as well as information regarding their acquisition, description and mineralogy. These three meteorites are the Breece, New Mexico siderite (E.C.N. = 1083, 353), the Hishikari, Japan achondrite (E.C.N. = 1305, 317) * and the Mino, Japan achondrite (E.C.N. =1367, 354)*


The Geology And Geomorphology Of The White Rock Canyon Area, New Mexico, Robert J. Emmanuel May 1950

The Geology And Geomorphology Of The White Rock Canyon Area, New Mexico, Robert J. Emmanuel

Earth and Planetary Sciences ETDs

The White Rock Canyon area is in the Rio Grande depression in north-central New Mexico between parallels 35 degrees 33' and 35 degrees 53' and meridians 106 degrees 4' and 106 degrees 21' (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 …


Geology Of The Golden Area, Santa Fe County, New Mexico, W. L. Emerick May 1950

Geology Of The Golden Area, Santa Fe County, New Mexico, W. L. Emerick

Earth and Planetary Sciences ETDs

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.


Geology Of The Hagan Coal Basin, Earl P. Harrison Mar 1949

Geology Of The Hagan Coal Basin, Earl P. Harrison

Earth and Planetary Sciences ETDs

This study was undertaken with the foremost objective of determining the stratigraphy and structure of the area, and correlating it with known surrounding areas.

The method of study was through geologic mapping in the field. The formational contacts, faults and other features were studied in the field with the aid of aerial photographs. The sections were measured in the field by hand-leveling with a Brunton compass up across the exposures. The lithology of the formations was studied as the sections were measured. The base map was taken from a planimetric map prepared by the Soil Conservation Service from aerial photos. …


Paleoecology Of The Brachiopoda, Celia Faith Hendren Jan 1949

Paleoecology Of The Brachiopoda, Celia Faith Hendren

Earth and Planetary Sciences ETDs

The immediate concern of the writer in the preparation of this thesis is not so much to give long statistical lists of conclusions (unfortunately this type of material is exceedingly scarce), but to sift the readily available facts in print and prepare a brief history of the work already accomplished on living and fossil Brachipoda. Where possible, there will be a discussion and evaluation of the views presented by different authors.


Correlation Between Electric And Lithologic Characteristics In Four Wells In San Juan County, New Mexico, Edward C. Beaumont Jun 1948

Correlation Between Electric And Lithologic Characteristics In Four Wells In San Juan County, New Mexico, Edward C. Beaumont

Earth and Planetary Sciences ETDs

The primary objective of the problem is to relate electric characteristics to lithologic characteristics in four wells in San Juan County, New Mexico. The secondary objective is to decipher stratigraphic correlations between wells. The wells, in San Juan County, are geologically located in the San Juan Basin, a structural basin in the Colorado Plateau. The formations range in age from Paleozoic Cambrian (?) to Cenozoic Recent. The boundaries of the Basin are ill-defined and have shifted throughout the history of the area.


Geology And Ore Deposits Of The Dunmore Mine, Ouray County, Colorado, Caswell Silver Jun 1946

Geology And Ore Deposits Of The Dunmore Mine, Ouray County, Colorado, Caswell Silver

Earth and Planetary Sciences ETDs

The Dunmore lode is located near Ouray, Colorado in the northwest part of the San Juan Mountains. In structure as well as mineral assemblage it shows a connection between the chimneys and veins of the region. The lode averages about 100 feet wide for 1,200 feet along the Dunmore claim. The fissure zone is over two miles long and displacement along it has offset a folded pre-Cambrian complex 4,500 feet prior to the deposition of 2,400 feet of volcanic tuff. Fissures in the pre-Cambrian rocks controlled in part the intrusion of dikes and the formation of veins. Late Tertiary faulting …


The Paleontology And Stratigraphy Of The Magdalena Group Of Northern And Central New Mexico, Wallace A. Bisbee Jan 1932

The Paleontology And Stratigraphy Of The Magdalena Group Of Northern And Central New Mexico, Wallace A. Bisbee

Earth and Planetary Sciences ETDs

No abstract provided.