@book {51826,
	title = {Physiographic provinces I and II},
	series = {New Mexico in Maps},
	year = {1986},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {1986},
	pages = {23-31},
	publisher = {University of New Mexico Press},
	organization = {University of New Mexico Press},
	edition = {Second Edition},
	address = {Albuquerque, New Mexico},
	abstract = {A physiographic province is a region with a particular pattern of landforms that differs significantly from that of adjacent regions.  Each province has a distinctive geologic framework and particular combinations of topographic and hydrographic features that have evolved through geologic time.  The individual landforms (e.g., mountains, canyons, alluvial fans) that in aggregate make up the varied natural landscapes of a given province reflect a variety of geomorphic processes.  In New Mexico these range from the action of deep-seated (hypogene) forces, including volcanism and tectonism, such as erosion and sedimentation by water or wind.},
	keywords = {book, books, chapter, chapters, geomorphic processes, map,physiographic provinces, physiographic provinces, map, report, reports},
	author = {J. Hawley},
	editor = {Jerry L. Williams (ed.)}
}
@proceedings {52034,
	title = {Overview of geology as related to environmental concerns in New Mexico},
	year = {1981},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {1981},
	pages = {1-10},
	publisher = {New Mexico Bureau of Mines and Mineral Resources},
	abstract = {New Mexico faces a special set of environmental problems associated with rich mineral resources, a dry climate, and vast areas of low population.  Complex interactions between geology and environmental concerns involve geologic processes that have adverse effects on human activities, and modern society{\textquoteright}s use of mineral, land, and water resources.  Geologic processes include moderate-intensity earthquakes, surface subsidence due to rock dissolution, stream floods, debris flows, and landslides.  Geological related human impacts on the environment include surface and subsurface extraction of economic mineral deposits (primarily energy minerals), ground-water development, construction of dams and power plants, disposal of hazardous wastes, and establishment of large-area reserves for military operations and scientific research.     Geologists have a major role in helping solve environmental problems resulting from effects of geomorphic processes and development of mineral, water, and land resources.  Inventories much be made of these processes and resources in order to put complex process-resource-human interactions in proper space and time perspective.  Guidelines can then be formulated for mitigation or prevention of geology-related problems.  For example, mined lands need to be reclaimed, cities need to be planned, and sites need to be selected for hazardous-waste disposal.  Finally, geologists must clearly present available information on relationships between geology and human concerns.  The hallmark of environmental geology should be effective communication with nongeologists.},
	keywords = {abstract, abstracts, conference, conference proceedings, conferences, environment,geology, geology,environmental concerns, geomorphology, processes, proceeding, proceedings},
	author = {J. Hawley and Love, David W.}
}
@proceedings {52207,
	title = {Quaternary stratigraphy in the Basin and Range and Great Plains provinces, New Mexico and western Texas},
	year = {1976},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {1976},
	publisher = {Dowden, Hutchinson and Ross},
	abstract = {The primary objective of this paper is to discuss the present status of Quaternary stratigraphy in the Mexican Highland section of the Basin and Range physiographic province, and the Pecos Valley and southern High Plains sections of the Great Plains province.  Sequences in adjacent areas of southern Arizona and Colorado are also briefly discussed as are relations of some associated units of pre-Quaternary age.  Particular attention is give to the geomorphic settings of these units, the development of present drainage, and the interaction between alluvial processes, tectonism, and volcanism in closed and open basin systems.  Author responsibility is as follows:  north-central New Mexico -- Manley; central New Mexico and Pecos Valley -- Bachman; and southern New Mexico and western Texas -- Hawley.  Detailed field are in progress or have been recently completed by the authors in these areas and a large body of information is available.  Review of published work emphasizes research undertaken since publication of the review papers by Kottlowski, Cooley and Ruhe, and by Frye and Leonard in <i>The Quaternary of the United States </i>(Wright and Frey, 1965).},
	keywords = {abstract, abstracts, conference, conference proceedings, conferences, geomorphology, Quaternary stratigraphy, geomorphology, stratigraphy, proceeding, proceedings},
	isbn = {0-87933-262-X},
	author = {J. Hawley and Bachman, G. O. and Manley, K.},
	editor = {Mahaney, W. C. (ed.)}
}
@proceedings {52232,
	title = {The desert soil-geomorphology project},
	volume = {26th Field Conference},
	year = {1975},
	note = {//LOCAL//NONE//},
	month = {1975},
	pages = {183-185},
	publisher = {New Mexico Bureau of Mines and Mineral Resources},
	abstract = {The Desert Soil-Geomorphology Project refers to a Soil Conservation Service, USDA, investigation between 1957 and 1972, of landscape evolution and soil development in a 400 sq mi area of Dona Ana County, New Mexico (Fig. 1).  Its primary purpose was to gather basic information on soil-geomorphic relationships that would lead to increased accuracy and efficiency of the Soil Survey program in arid and semi-arid regions of the western states.  A team of soil scientists and geologists from the S.C.S. Soil Survey Investigations Division under the direction of Guy D. Smith staffed the project.},
	keywords = {abstract, abstracts, conference, conference proceedings, conferences, Desert Project,publication list, geomorphology, landscape, evolution, list,Desert Project publications, proceeding, proceedings, soil, development, soil-geomorphic relationships},
	author = {J. Hawley}
}
@proceedings {52233,
	title = {Quaternary history of Dona Ana County region, south-central New Mexico},
	volume = {26th Field Conference},
	year = {1975},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {1975},
	pages = {139-150},
	publisher = {New Mexico Bureau of Mines and Mineral Resources},
	abstract = {The region discussed in this paper comprises south-central New Mexico and adjacent parts of Trans-Pecos Texas and Chihuahua, Mexico (Fig. 1).  Emphasis is on Quaternary events and alluvial deposits in the Dona Ana County area of the Mexican Highlands section, Basin and Range province.  Many of the local features mentioned herein are described in the road-log section of this guidebook, particularly at Day 2 and 3 tour stops.  Aspects of Quaternary research in the area are also discussed in companion guidebook papers by Dick-Peddie, Hawley, Hoffer, Fox, Stone and Brown, and King and Hawley.},
	keywords = {abstract, abstracts, conference, conference proceedings, conferences, Desert Project, geology, geology, environmental, geology, Quaternary, geomorphology, alluvial deposits, history,Quaternary, proceeding, proceedings},
	author = {J. Hawley}
}
@proceedings {52336,
	title = {Geologic-geomorphic mapping to serve soil resource development},
	year = {1972},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {August 6-9, 1972},
	pages = {24-30},
	publisher = {Soil Conservation Society of America},
	address = {Hilton Hotel, Portland, Oregon},
	abstract = {A better understanding of the distribution, composition, and genesis of natural features at or near the earth{\textquoteright}s surface increases man{\textquoteright}s ability to develop soil uses that are in closer harmony with the environment.  Field and laboratory studies in geology and its subdiscipline, geomorphology, especially as shown on maps and cross sections, can be particularly helpful in soil resource evaluation and development.},
	keywords = {abstract, abstracts, conference, conference proceedings, conferences, Desert Project, geomorphology,mapping, map,geologic-geomorphic, proceeding, proceedings, soil, resource development, soil,geologic-geomorphic map},
	author = {J. Hawley}
}
@proceedings {52414,
	title = {Notes on the geomorphology and late cenozic geology of northwestern Chihuahua},
	volume = {20th Field Conference},
	year = {1969},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {1969},
	pages = {131-142},
	publisher = {New Mexico Bureau of Mines and Mineral Resources},
	abstract = {<p>The geomorphology and late Cenozoic geology of a 71,500 square kilometer (27,600 square mile) area of northwestern Chihuahua and adjacent parts of Sonora, New Mexico and Texas are discussed. Emphasis is on description of three major physiographic units: The Sierra Madre Occidental, and two subsections of Mexican Basin and Range section. Formal names are proposed for the latter two subdivisions. The larger unit is characterized by broad desert basins and isolated ranges of northern and eastern Chihuahua and is designated the Bolson Subsection. The higher unit, designated the Babicora-Bustillos subsection, occupies a region that is transitional, in terms of terrain and geologic features, between the Bolson unit and the Sierra Madre. Physiographic boundaries were selected on the basis of study of recently-compiled 1:250,000 scale topographic maps and some field work. Control in the northern part of the area was also provided by photos taken from Apollo and Gemini spacecraft. Studies of basin- and valley-fill geology and geomorphology in the New Mexico-Chihuahua border region since 1950 have resulted in considerable elaboration of basic concepts of the late Cenozoic landscape evolution developed notably by Hill, Lee, Baker, Bryan and P. B. King. The fundamental concept of mid- to late Tertiary and Quaternary development and filling of intermontane basins, followed by local establishment of the entrenched Rio Grande Valley system during mid- to late Pleistocene time, appears to be generally applicable to the Basin and Range area under discussion. The important influence of a cyclic climatic change during the Quaternary period on landscape evolution is also recognized.</p>
},
	keywords = {abstract, abstracts, Cenozoic geology, conference, conference proceedings, conferences, Desert Project, geomorphology, landscape evolution, proceeding, proceedings, soil},
	author = {J. Hawley}
}
@proceedings {52413,
	title = {Quaternary geology of the south-central New Mexico border region},
	volume = {Circular 104},
	year = {1969},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {1969},
	pages = {89-115},
	publisher = {New Mexico Bureau of Mines and Mineral Resources},
	abstract = {In early to mid-Quaternary time, the intermontane basins of the south-central New Mexico border region were still internally drained.  Environments of deposition ranged from alluvial-fan piedmont slopes to broad basin floors that were often sites of lacustrine sedimentation.  In later stages of basin filling, local upland sediment sources were supplemented by the ancestral upper Rio Grande, which extended into the region by early Kansan time.  Studies of vertebrate and invertebrate faunas and correlation of volcanic ash lenses indicate that basin filling in extensive areas adjacent to the Rio Grande Valley culminated in late Kansan to early Illinoian time.  The complex of late Cenozoic basin fills predating Rio Grande Valley entrenchment comprises the Santa Fe Group.  The Jornada and La Mesa geomorphic surfaces cap the Santa Fe sequence.     Cyclic entrenchment of the Rio Grande was initiated after mid-Pleistocene integration of the lower and upper segments of the ancestral Rio Grande.  Subsequently, four major, climatically controlled cycles of valley cutting have taken place.  Aggradation of basin surfaces has continued in broad areas still not integrated with Rio Grande drainage.  Parts of basin floors were occupied by large lakes during late Pleistocene pluvials.     Significant structural deformation of basin- and valley-fill deposits and extrusion of basalts and maare formation in Mesilla bolson represent continuation of deep-seated disturbances in Quaternary time.},
	keywords = {abstract, abstracts, conference, conference proceedings, conferences, geomorphology, Quaternary geology, proceeding, proceedings},
	author = {J. Hawley and Frank E. Kottlowski}
}
@proceedings {52415,
	title = {The Santa Fe group in the south-central New Mexico border region},
	volume = {Circular 104},
	year = {1969},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {1969},
	pages = {52-57},
	publisher = {New Mexico Bureau of Mines and Mineral Resources},
	abstract = {The Santa Fe Group in the south-central New Mexico border region is a complex sequence of piedmont-slope alluvium; playa, lacustrine, and fluvial deposits; and some basaltic volcanic preserved in structural basins within and adjacent to the Rio Grande depression.     The upper limit of the group is the surface of the youngest basin fill predating initiation of the Rio Grande Valley entrenchment.  The lower limit is placed above volcanic and associated sedimentary rocks of Oligocene-early (?) Miocene age that are well exposed in the Caballo-Selden area.  Studies of vertebrate and invertebrate faunas, determination of the potassium-argon age of interbedded basalt, and correlation of volcanic ash lenses have established a general Miocene to mid-Pleistocene age for the Santa Fe Group in the border region.  Early stages of intermontane basin filling occurred in a closed-basin (classic bolson) environment, while later stages were marked by coalescence of basin floors and development of a regional system of through-drainage.  Thus, Santa Fe group deposition in the border region corresponds with Bryan{\textquoteright}s idealized concept of basin filling in the type Santa Fe region to the north.     Important economic resources in the Santa Fe Group include ground water, sand, gravel, clay, and caliche.},
	keywords = {abstract, abstracts, conference, conference proceedings, conferences, geomorphology, piedmont-slope alluvium, geomorphology, Santa Fe Group, basaltic volcanics, geomorphology, Santa Fe Group, fluvial deposits, geomorphology, Santa Fe Group, lacustrine, geomorphology, Santa Fe Group, piedmont-slope alluvium, geomorphology, Santa Fe Group, playa, proceeding, proceedings},
	author = {J. Hawley and Frank E. Kottlowski and W. R. Seager and King, William E. and Strain, William S. and LeMone, David V.}
}
@proceedings {52480,
	title = {Geomorphic surfaces along the Rio Grande Valley from El Paso, Texas to Caballo Reservoir, New Mexico},
	volume = {Sixteenth Field Conference},
	year = {1965},
	note = {//LOCAL//NONE//ProCite field[6]: In},
	month = {1965},
	pages = {188-198},
	publisher = {New Mexico Bureau of Mines and Mineral Resources},
	abstract = {The flood plain of the Rio Grande in southern New Mexico and Texas near El Paso is flanked by an ascending sequence of geomorphic surfaces graded to successively higher and older flood-plain positions of the ancestral river.  These valley-border surfaces represent major cycles of erosion, accompanied by lesser amounts of backfilling, and they are in turn inset below remnants of an early (?) to mid-Pleistocene complex of basin-filled surfaces.},
	keywords = {abstract, abstracts, conference, conference proceedings, conferences, Desert Project, geology,Cenozoic, geomorphology, Cenozoic, proceeding, proceedings, soil, geomorphology relationships},
	author = {J. Hawley}
}
