Caves and karst of southeastern New Mexico最新文献_第5页

First-day road log, trip 1, from Washington Ranch to Dark Canyon, Mosley Canyon, and Queen Highway, through Indian Basin and Rocky Arroyo, to Azotea Mesa and the McKittrick Hill Caves, and return to Washington Ranch by way of Happy Valley 第一天的道路日志，行程1，从华盛顿牧场到黑暗峡谷、莫斯利峡谷和皇后公路，穿过印第安盆地和洛基阿罗约，到亚索泰梅萨和麦基特里克山洞穴，然后经由欢乐谷返回华盛顿牧场

Caves and karst of southeastern New Mexico Pub Date : 1900-01-01 DOI: 10.56577/ffc-57.1

L. Land, D. Love, V. Polyak

引用次数: 0

Halite depositional cycles in the Upper Permian Salado Formation 上二叠统萨拉多组岩盐沉积旋回

Caves and karst of southeastern New Mexico Pub Date : 1900-01-01 DOI: 10.56577/ffc-.78

R. Holt, D. W. Powers, T. Lowenstein

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Intrastratal karst at the WIPP site, southeastern New Mexico 新墨西哥州东南部WIPP遗址的层内岩溶

Caves and karst of southeastern New Mexico Pub Date : 1900-01-01 DOI: 10.56577/ffc-.233

C. Hill

{"title":"Intrastratal karst at the WIPP site, southeastern New Mexico","authors":"C. Hill","doi":"10.56577/ffc-.233","DOIUrl":"https://doi.org/10.56577/ffc-.233","url":null,"abstract":"— The possibility of intrastratal karst at the WIPP site has been evaluated with respect to karst principles and processes and to dissolution/hydrological studies. While little direct evidence exists for intrastratal karst at the WIPP site, many indirect lines of evidence suggest the possible presence of karst: surface topographic depressions, negative gravity anomalies, lack of surface runoff, collapse breccias, insoluble residue horizons, WIPP-33 sinkholes and caves, anomalous drawdowns, and salinity variations within boreholes. Intrastratal karst, if it exists, would bypass slow matrix flow in the Culebra Dolomite aquifer and be subject to fast flow in cave conduits. *Originally published in: Oklahoma Geological Survey Circular 109, p. 197-209, 2003. Reprinted with permission. FIGURE 1. Map of the Delaware Basin showing location of the Capitan reef, major dissolution depressions (troughs), and western dissolution edge of evaporites. A, B, C, D, E, F, and G correspond to the dissolution troughs of Maley and Huffington (1953), “DOMES” are Vine’s domes/ breccia pipes, CC = Carlsbad Cavern, LC = Lechuguilla Cave, BLS = Bell Lake Sink, MB = Malaga Bend of the Pecos River, and KD = karst domes. Laguna Grande de la Sal (Salt Lake), Nash Draw, and the WIPP site are also shown. From base map of Anderson (1981), modified by Hill (1996).","PeriodicalId":115438,"journal":{"name":"Caves and karst of southeastern New Mexico","volume":"17 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121212463","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Surficial geology in the vicinity of Washington Ranch 华盛顿牧场附近的地表地质

Caves and karst of southeastern New Mexico Pub Date : 1900-01-01 DOI: 10.56577/ffc-.311

D. Love, L. Land

{"title":"Surficial geology in the vicinity of Washington Ranch","authors":"D. Love, L. Land","doi":"10.56577/ffc-.311","DOIUrl":"https://doi.org/10.56577/ffc-.311","url":null,"abstract":"Piedmont slopes and river terraces near Washington Ranch reflect late Neogene geologic history, but are affected by both local and regional solution subsidence of the underlying evaporitic Castile Formation. The Black River currently is a discontinuous stream with local solution sinks and springs. Holocene and late Pleistocene alluvium, marsh, and tufa deposits mark the current river level, whereas two types of older terraces are preserved in the vicinity of Washington Ranch-fluvial gravel terraces, and a fine-grained gypsiferous “terrace” (?) deposit that indicates an episode of no coarse clastic transport along the river. Seven levels of clastic piedmont deposits with preserved surfaces ranging from highest remnants to modern tributary channels reflect changing base levels from the Guadalupe Escarpment toward the Black River and beyond. Older high piedmont levels west and northwest of the Black River cap outcrops of Castile Formation, whereas younger piedmont levels are graded close to the level modern tributaries and the Black River. The underlying Castile Formation is thinned markedly by solution and up to 100 m of coarse alluvium underlie the younger piedmont deposits, reflecting long-term subsidence of the distal parts of the piedmont and Black River. Ovoid karst features cut the piedmont deposits at all levels. Differences in spring and sinkhole water chemistries reflect different aquifers including the piedmont gravel aquifer of Rattlesnake Spring and the gypsic aquifer of Bottomless Lakes.","PeriodicalId":115438,"journal":{"name":"Caves and karst of southeastern New Mexico","volume":"3 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131700010","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 3

Biothems: Biologically influenced speleothems in the caves of the Guadalupe Mountains, New Mexico, USA 生物主题:美国新墨西哥州瓜达卢佩山脉洞穴中受生物学影响的洞穴主题

Caves and karst of southeastern New Mexico Pub Date : 1900-01-01 DOI: 10.56577/ffc-.167

J. Queen, L. Melim

引用次数: 0