scholarly journals Surface uplift above the Jemez mantle anomaly in the past 4 Ma based on40Ar/39Ar dated paleoprofiles of the Rio San Jose, New Mexico, USA

Geosphere ◽  
2015 ◽  
Vol 11 (5) ◽  
pp. 1384-1400 ◽  
Author(s):  
Michael A. Channer ◽  
Jason W. Ricketts ◽  
Matthew Zimmerer ◽  
Matthew Heizler ◽  
Karl E. Karlstrom
Keyword(s):  
New Mexico ◽  
San Jose ◽  
The Past ◽  
Surface Uplift

Historic Churches of New Mexico Today

2019 ◽  
Author(s):  
Frank Graziano
Keyword(s):  
New Mexico ◽  
San Francisco ◽  
San Jose ◽  
Pueblo Indians ◽  
New Mexican ◽  
Cultural Legacy ◽  
Attachment To Place ◽  
The Village ◽  
The Church ◽  
Previous Scholarship

Historic Churches of New Mexico Today is an interpretive ethnography based on fieldwork among hispanic villagers, Pueblo Indians, and Mescalero Apaches. The fieldwork was reinforced by extensive research in archives and in previous scholarship. The book presents scholarly interpretations in prose that is accessible, often narrative, at times lyrical, and crafted to convey the experience of researching in New Mexican villages. Descriptive guide information and directions to remote historic churches are provided. Themes treated in the book include the interactions of past and present, the decline of traditions, a sense of place and attachment to place, the church as a cultural legacy, the church in relation to native traditions, resistance to Catholicism, tensions between priests and congregations, maintenance and restoration of historic buildings, and, in general, how the church as a place and devotion as a practice are important (or not) to the identities and everyday lives of individuals and communities. Among many others, the historic churches discussed in the study include the Santuario de Chimayó, San José de Gracia in Las Trampas, San Francisco de Asís in Ranchos de Taos, the village churches of Mora County, St. Joseph Apache Mission in Mescalero, and the mission churches at Laguna, Acoma, and Picurís Pueblos.

Eyeworm infections ofOxyspirura petrowi, Skrjabin, 1929 (Spirurida: Thelaziidae), in species of quail from Texas, New Mexico and Arizona, USA

2016 ◽  
Vol 91 (4) ◽  
pp. 491-496 ◽  
Author(s):  
N.R. Dunham ◽  
R.J. Kendall
Keyword(s):  
New Mexico ◽  
Population Decline ◽  
Northern Bobwhite ◽  
Cellular Damage ◽  
Scaled Quail ◽  
Callipepla Squamata ◽  
The Past ◽  
New Research ◽  
Gambel's Quail ◽  
Historical Range

AbstractNorthern bobwhite (Colinus virginianus) and Scaled quail (Callipepla squamata) have been declining steadily throughout much of their historical range over the past few decades. Even the Rolling Plains of Texas, historically rich with wild quail and one of the last remaining quail strongholds, has been suffering a population decline, most notably since 2010. Gambel's quail (Callipepla gambelii) have also been experiencing their own decline throughout their respective range, but not as significant as that of other species of quail. Eyeworms (Oxyspirura petrowi) in quail have been recognized for years but not thoroughly studied until recently. New research reveals thatO. petrowiinfection can cause inflammation, oedema, and cellular damage to the eye of the quail host. The objective of this research was to better understand the prevalence of the eyeworm infection in different quail species, expand on known distribution, and determine if there is a relationship between location and species infected with eyeworms. Northern bobwhite, Scaled quail and Gambel's quail were hunter-donated from one county within Texas, New Mexico and Arizona, and examined for the prevalence, mean abundance and mean intensity of eyeworm infection from November 2013 to February 2014. Quail from every location were found to have individuals with a varying degree of eyeworm infection. This is the first study to document eyeworm infection in Gambel's quail and in quail in New Mexico and Arizona, and reports the highest eyeworm infection found in Northern bobwhite and Scaled quail.

Evaporite Dissolution Relevant to the Wipp Site, Northern Delaware Basin, Southeastern New Mexico

1982 ◽  
Vol 15 ◽  
Author(s):  
Steven J. Lambert
Keyword(s):  
New Mexico ◽  
High Rate ◽  
Late Cenozoic ◽  
Time Intervals ◽  
Near Surface ◽  
Waste Isolation Pilot Plant ◽  
Delaware Basin ◽  
The Past ◽  
Geomorphic Features ◽  
Geologic Record

ABSTRACTEvaluation of the threat of natural dissolution of host evaporites to the integrity of the Waste Isolation Pilot Plant (WIPP) in southeastern New Mexico has taken into consideration (1) the volume of “missing” rock salt, (2) the occurrence (or not) of characteristic dissolution brines, (3) geomorphic features, some of which are unrelated to dissolution, and (4) the time intervals over which dissolution may have been active. Even under the assumption that all “missing” halite was originally present and has been removed by dissolution, there is no evidence of active preferential removal of the lower Salado Formation halite by any geologically reasonable process. The geologic record contains evidence of dissolution in the Triassic and Jurassic; to constrain all removal of basinal halite to the late Cenozoic yields an unrealistically high rate of removal. Application to the lower Salado of a stratabound mechanism known to be active in Nash Draw, a near-surface feature within the Basin, allows a minimum survival time of 2,500,000 years to be predicted for the subsurface facility for storage of radioactive waste at WIPP. This calculation is based on an analysis of all known dissolution features in the Delaware Basin, and takes into account the wetter (pluvial) climate during the past 600,000 years.

A Basketmaker III Site in Canyon Largo, New Mexico

1944 ◽  
Vol 9 (4) ◽  
pp. 381-385 ◽  
Author(s):  
Frank C. Hibben ◽  
Herbert W. Dick
Keyword(s):  
New Mexico ◽  
Chaco Canyon ◽  
San Juan ◽  
The Past ◽  
Field School ◽  
Mesa Verde ◽  
Four Seasons ◽  
Basketmaker Iii ◽  
Cultural Connections ◽  
The University

One of the activities of the University of New Mexico's 1939 field school at Chaco Canyon was a reconnaissance excavation in the vicinity of Largo Canyon, to the northeast of the Chaco, proper. This was a continuation of the survey and excavations of the past four seasons, as a part of the project for outlining chronologically and geographically the culture known as Gallina. The extent of the Gallina manifestation to the east and south has already been fairly accurately delineated, but its western and northwestern boundaries are unknown. Since the San Juan and Mesa Verde centers lie to the northwest, it was deemed imperative that the cultural connections in that direction be determined. Typical Gallina unit houses are common on the headwaters of the Largo and in the Llegua Canyon area which heads in the same region. The extremely rugged area lying between this district and the San Juan and Mesa Verde region, however, is not only difficult of access, but is practically unknown archaeologically.

scholarly journals A TRYPETID BRED FROM GALLS ON BIGELOVIA

1893 ◽  
Vol 25 (2) ◽  
pp. 48-52
Author(s):  
C. H. Tyler Townsend
Keyword(s):  
New Mexico ◽  
The Past ◽  
Westerly Direction ◽  
Past Summer

A round, white, woolly gall was found on stems of Bigelovia (sp. probably graveolens)in several localities in western New Mexico the past summer, from June 19 to 22. Those found June 19 were old galls, and were met with near Luera Spring, in Socorro county. On June 21 the fresh galls were found in numbers near Gallo Spring. Sometimes two or three were found near each other on the same stem or twig of the plant, and in one case three galls were found joined together, forming a triple gall. On June 22 they were found extremely common west of Apache Spring, thus seeming to increase in number in a westerly direction, as did also the patches of Bigelovia, every plant of which was full of them.

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