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Research




The projects listed below are a random selection. Use criteria above to search by keyword, subject, feature, or region. Combining search criteria may provide few or no results.
Geologic Mapping
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Geological Mapping provides the underpinning of most research carried out by our organization. Our goal is to provide state-of-the-art geological maps of sufficient detail to be of benefit for practical applications for the state of New Mexico. These maps can address a wide range specific topics, such as location of geological resources, including mineral and petroleum resources and groundwater, geological hazards, which are all relevant to natural resource use, city planning, and education.

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Hydrogeologic Study of the Plains of San Agustin and the Alamosa Creek Valley
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The AMP initiated a regional hydrogeologic study of the Plains of San Agustin and the Alamosa Creek Valley in October 2009 in response to questions and data needs from state agencies (NM OSE/ISC, NM EMNRD Mining and Minerals Division, and NMED). The issues relate to groundwater availability in the San Agustin basin and possible effects of mineral resource development on water quality in ecologically and culturally sensitive Warm Spring and Alamosa Creek near Monticello.

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Lifetime projections for the High Plains Aquifer in east-central New Mexico
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Several thousand water-level measurements spanning over 50 years, from over a thousand wells, were used to create aquifer lifetime projections for the High Plains Aquifer in east-central New Mexico.

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Hydrogeology of the Questa Area
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The issues are a gap in regional scientific information for deep and shallow, sediment-volcanic aquifers and surface waters in the Questa area; including sustainable sources of drinking water, sources of water to springs and streams that feed fisheries and discharge to the Rio Grande, the character of natural, background water quality, and possible impacts from mine-related waters.

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Uplift of the Tibetan Plateau: Insights from cosmogenic exposure ages of young lava flows
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The Tibetan plateau is a product of the most dramatic tectonic event of recent geological history: the collision of the Indian sub-continent with Eurasia. In spite of the topographic and tectonic implications of the plateau, the mechanisms for its uplift remain controversial. The controversy is in large part a result of poorly constrained uplift history. Types of evidence that have been adduced for the uplift history include paleoecological date, cooling histories of plutonic and igneous rocks, and geomorphic interpretations. Some lines of evidence indicate relatively gradual uplift since the mid-Tertiary, while others support rapid acceleration of uplift during the latest Cenozoic, with the greatest portion during the Quaternary.

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Northeastern Tularosa Basin Regional Hydrogeology Study
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The population centers in Alamogordo, Carrizozo, La Luz, and numerous other small communities, are largely supported by groundwater resources. With few perennial streams in this closed basin, water is sparse. Fresh water resources are limited, and recharge to these areas originates within the high elevation watersheds in the Sacramento Mountains, as precipitation, stream and spring flow. This goal of this study was to improve understanding of the groundwater resources in this region by identifying recharge areas and quantities, determining groundwater flow rates and direction, and to interpret the groundwater/surface water interactions that exist in the region. Methods used in this effort included geologic mapping, groundwater level measurements, and geochemical analyses of the groundwater, springs and streams.

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Statewide Water Assessment: Recharge
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The rate and distribution of groundwater recharge to New Mexico’s aquifers is the least understood aspect of the state’s water budget. Despite a history of precise and distributed measurements quantifying surface water flow, water table elevations, precipitation amounts, as well as current models that describe evapotranspiration, a statewide assessment of recharge has not been completed.

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Scientists Use Ancient Ore Deposits to Predict Ground Water Quality and Paleoclimate
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Two Bureau of Geology scientists, in collaboration with scientists at the United State Geological Survey, have discovered similarities between ground water systems that formed ore deposits 10 million years ago and modern ground water in the Rio Grande Rift. They reported their work in an invited presentation at the 2000 Annual Meeting of the Geological Society of America.

Dr. Virgil Lueth, mineralogist/ economic geologist, and Lisa Peters, senior lab associate at the New Mexico Geochronological Research Lab, have been studying the mineral jarosite in ore deposits from Chihuahua, Mexico, to Albuquerque.

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Southern Taos Valley Hydrogeology
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The southern Taos Valley, located southwest of the town of Taos, has been experiencing high growth over the last few decades. In order to address growing water needs in this region, Peggy Johnson, Dr. Paul Bauer, and Brigitte Felix, completed a technical report summarizing the local geology and hydrogeology.

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Geology and Hydrogeology of the Estancia Basin and East Mountains
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The New Mexico Bureau of Geology and Mineral Resources has a long history of conducting and supporting hydrogeologic investigations in the Estancia Basin of central New Mexico.

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