Geophysical prospecting for new cave passages: Fort Stanton Cave, New Mexico, USA

被引:0
作者
Lewis Land
机构
[1] National Cave and Karst Research Institute,
[2] and New Mexico Bureau of Geology and Mineral Resources,undefined
[3] New Mexico Institute of Mining and Technology,undefined
来源
Carbonates and Evaporites | 2012年 / 27卷
关键词
New Mexico; Fort Stanton Cave; Snowy River; Resistivity;
D O I
暂无
中图分类号
学科分类号
摘要
Geophysical surveys have been used to predict extensions of newly discovered sections of Fort Stanton Cave, the third-longest cave in New Mexico. Because air-filled caves have almost infinite resistivity, the electrical resistivity (ER) method is a very effective tool for detection of subsurface conduits in the unsaturated zone. Resistivity profiles have been used for several years by local cavers to guide exploration in Fort Stanton Cave. However, the most recent discoveries approach the limits of the depth of investigation of the resistivity equipment used by the cavers. The National Cave and Karst Research Institute has begun conducting resistivity profiles over these deeper portions of the cave system using a SuperSting™ R-8 resistivity meter coupled with longer 112-electrode arrays. These ER tools have been very successful at identifying extensions of known passage in Fort Stanton Cave.
引用
收藏
页码:97 / 102
页数:5
相关论文
共 4 条
[1]  
Andrews JE(2006)Palaeoclimatic records from stable isotopes in riverine tufas—Synthesis and review Earth-Sci Rev 75 85-104
[2]  
Davis DG(2008)Return to Snowy River—Fort Stanton Cave goes on Rocky Mt Caving 25 24-31
[3]  
Kelley VC(1971)Geology of the Pecos country, southeastern New Mexico: New Mexico Bureau of mines and mineral resources Memoir 24 78-102
[4]  
Worthington SRH(2007)Groundwater residence times in unconfined carbonate aquifers J Cave Karst Stud 69 94-undefined