Cannon Air Force Base, NM: One Pager USAF(Disregard Restriction Header and Footer)

Cannon Air Force Base, NM:Mil Value and Capacity Support Information USAF(Disregard Restriction Header and Footer)

Cannon Air Force Base, NM: COBRA Run USAF(Disregard Restriction Header and Footer)

Cannon Air Force Base, NM: Economic Impact (EIT Run) USAF(Disregard Restriction Header and Footer)

Cannon Air Force Base, NM: Community Infrastructure Assessment USAF(Disregard Restriction Header and Footer)

Cannon Air Force Base, NM: Environmental Impact USAF(Disregard Restriction Header and Footer)

USAF, Holloman AFB, NM, Demographics tables with short descriptions of the area near the installation/activity. Holloman AFB is 88.8 miles from El Paso, TX, the nearest city with a population of 100,000 or more.

Disregard Restriction Header and Footer - RC Transformation in New Mexico - Impacted Sites: Kirtland AFB, NM

Base Visit Book from BRAC Commission Visit to Cannon Air Force Base, NM dtd 23 June 2005. Document includes itinerary, base summary sheet, SECDEF recommendation, military capabilities index, installation review, state map and statistical data, state closure history list, and press articles and correspondence.

Base Visit Report Cannon Air Force Base

Contains notes and Base Visit Book for Cannon Air Force Base, New Mexico.

Book that discusses the ground waters of the Rio Grande Valley as well as tests undertaken at pumping plants along the area. Appendix begins on page 74. Index begins on page 81.

Seismic data were collected in southwestern New Mexico to investigate the sources of the geothermal anomalies and to investigate the potential earthquake hazards of geothermal development. No major crustal structure anomalies have been located related to known geothermal resources, and no areas of continual seismicity have been identified, which is interpreted to indicate a lack of active, or recently active crustal intrusions in southwestern New Mexico. Without a magnetic heat source, the geothermal potential of the known anomalies is probably limited to intermediate and low temperature applications (<180/sup 0/C). The lack of continual seismicity indicates low seismic hazard in the area directly related to geothermal development, although the historic and geologically recent tectonic activity should be taken into consideration during any development in the area. A model of forced groundwater convection is presented to explain the geothermal anomalies in southwestern New Mexico, which is consistent with all available geological and geophysical data from the area.