標(biāo)題: Titlebook: Caves and Karst of the Greenbrier Valley in West Virginia; William B. White Book 2018 Springer International Publishing AG 2018 Large Cave [打印本頁] 作者: Weber-test 時間: 2025-3-21 18:08
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書目名稱Caves and Karst of the Greenbrier Valley in West Virginia讀者反饋學(xué)科排名
作者: Homocystinuria 時間: 2025-3-21 23:50
Entscheidungsverhalten im Feld,bsurface either east to Stamping Creek springs or southwest to Locust Spring. However, few parts of the underground are accessible to observation. The caves of the Little Levels are of intermediate size, one to two miles, and many carry active streams which allow some interpretation of the eastern and western edges, but not the central portion.作者: 可行 時間: 2025-3-22 03:03 作者: Arthritis 時間: 2025-3-22 07:06 作者: laxative 時間: 2025-3-22 10:32 作者: 骨 時間: 2025-3-22 12:56 作者: 骨 時間: 2025-3-22 19:20 作者: 未開化 時間: 2025-3-23 00:10 作者: Confidential 時間: 2025-3-23 05:13 作者: critic 時間: 2025-3-23 06:06
The Swago Creek Basin,epresented by Barnes Pit, Tub Cave, and the Carpenters-Swago System. The Carpenter-Swago System has 3.1 miles of surveyed passage, and it is strongly controlled by a N60°E fracture system. Extensive stream tracing in the basin reveals details of drainage pattern which is strongly controlled by the shaly Taggard Formation.作者: Somber 時間: 2025-3-23 11:21 作者: 充滿裝飾 時間: 2025-3-23 14:09 作者: 有罪 時間: 2025-3-23 21:05 作者: CRUMB 時間: 2025-3-23 23:49 作者: Contend 時間: 2025-3-24 03:34
Caves of the Dickson Spring Basin, Monroe County,exception of Haynes Cave, are all in the headwaters (southern) part of the drainage basin and are complex from a geologic and hydrologic viewpoint. Most of these caves have received little attention in the last forty years because of access limitations.作者: ectropion 時間: 2025-3-24 07:01 作者: nautical 時間: 2025-3-24 13:53 作者: 注入 時間: 2025-3-24 17:34
Forschungsdesign und empirisches Feldne contact. The result is a patchwork of large underground drainage systems each discharging through a large spring. Analysis of the profiles of active surface streams and abandoned stream beds gives some insight into the developmental history of the karst.作者: 松果 時間: 2025-3-24 19:49
Innovation und Entrepreneurshipf drainage Systems discharging to two springs 20-km distant from each other with high flows discharge to one and low flows to the other. Drainage patterns have shifted over time as the surface drainage is captured. An estimated age for the entire System is 4.1 million years.作者: 使熄滅 時間: 2025-3-25 01:57
Zeitoptimales Weihnachtsliedersingen,e limestone. The pattern of passages is typically dendritic with an overall trend sub-parallel to the regional strike. Folding and faulting influence passage orientation in some of the passages, but the perching effect of the underlying shale forces the conduits downward along the local dip.作者: Vulnerable 時間: 2025-3-25 04:12 作者: POLYP 時間: 2025-3-25 11:10
The Friars Hole System,f drainage Systems discharging to two springs 20-km distant from each other with high flows discharge to one and low flows to the other. Drainage patterns have shifted over time as the surface drainage is captured. An estimated age for the entire System is 4.1 million years.作者: 空洞 時間: 2025-3-25 14:30
The Contact Caves of Central Greenbrier County,e limestone. The pattern of passages is typically dendritic with an overall trend sub-parallel to the regional strike. Folding and faulting influence passage orientation in some of the passages, but the perching effect of the underlying shale forces the conduits downward along the local dip.作者: BARB 時間: 2025-3-25 19:35
2364-4591 il remains found in these caves.Provides a comprehensive geoThe focus of this book is on the more than 2000 caves of the Greenbrier Valley of West Virginia of which the 14 with lengths greater than 10 km have an aggregate length of 639 km. The major caves form the core part of sub-basins which drain作者: 雪上輕舟飛過 時間: 2025-3-25 20:45 作者: EVICT 時間: 2025-3-26 04:01
The Greenbrier Karst,ded into drainage basins which drain by subterranean routes to big springs. The Greenbrier karst contains more than 2000 caves of which 24 have surveyed lengths exceeding 5?km. The accumulated length of those 24 caves is 503.7?km.作者: CREST 時間: 2025-3-26 05:41
Caves and Karst of the Greenbrier Valley in West Virginia978-3-319-65801-8Series ISSN 2364-4591 Series E-ISSN 2364-4605 作者: 背信 時間: 2025-3-26 11:24 作者: Conflagration 時間: 2025-3-26 13:00
Erfolgskontrolle der Online- Kommunikationl Creek, a tributary of Indian Creek and thus of the New River. The underground route of Laurel Creek passes through Laurel Creek Cave, Rimstone-Crossroads Cave, and Greenville Saltpeter Cave. The caves are in nearly flat bedding near the crest of the Abbs Valley Anticline.作者: 陶器 時間: 2025-3-26 20:40
William B. WhitePresents detailed descriptions of some of the largest caves in eastern United States.Explores the aquatic fauna, terrestrial fauna, and fossil remains found in these caves.Provides a comprehensive geo作者: SHRIK 時間: 2025-3-26 21:35
Cave and Karst Systems of the Worldhttp://image.papertrans.cn/c/image/222682.jpg作者: 惡心 時間: 2025-3-27 03:32
The Culverson Creek Cave System, springs along Spring Creek. Because of the large surface catchment and some partial blockages along the passages, the cave is subject to flooding. There are ten entrances, large passages, and numerous streams, with a total surveyed length of 20.1 miles (32.4?km).作者: 相反放置 時間: 2025-3-27 08:16
The Laurel Creek Basin and Greenville Saltpeter Cave,l Creek, a tributary of Indian Creek and thus of the New River. The underground route of Laurel Creek passes through Laurel Creek Cave, Rimstone-Crossroads Cave, and Greenville Saltpeter Cave. The caves are in nearly flat bedding near the crest of the Abbs Valley Anticline.作者: monopoly 時間: 2025-3-27 11:27 作者: Morose 時間: 2025-3-27 14:35 作者: restrain 時間: 2025-3-27 17:53
Berücksichtigung von Ressourcenverbindungentensive use of water-tracing techniques and cave mapping in the USA. The carbonate aquifer is about 400 ft (120?m) thick in the Swago Creek area west of Marlinton (Pocahontas County) increasing to 1000 ft (300?m) in southern Monroe County. The basic hydrogeologic setting for the region consists of r作者: 委托 時間: 2025-3-27 22:37
Forschungsdesign und empirisches Feld Greenbrier, and Monroe Counties, West Virginia. The geologic setting is conducive to the development of long caves but not deep caves. Within the Greenbrier Karst are 24 caves with surveyed lengths greater than 5?km of which nine have lengths greater than 20?km for a total of 500?km of cave passage作者: 拋物線 時間: 2025-3-28 04:22
https://doi.org/10.1007/978-3-8349-8690-00s, through the War of 1812, and the American Civil War. Technical descriptions of the caves began in the late 1940s with the work of William E. Davies. Exploration by cavers began in the 1950s and expanded rapidly thereafter. Exploration and survey were greatly enhanced by the organization of the N作者: 熱情的我 時間: 2025-3-28 09:16
https://doi.org/10.1007/978-3-8349-8690-0rainage but relatively little expression of surface karst. Swago Creek heads in two large cave-entrance springs: Overholt Blowing Cave and Cave Creek Cave. The Overholt Blowing Cave stream can be explored nearly to the head of the Dry Creek Valley but the upstream segment of the valley is pirated ea作者: 膠狀 時間: 2025-3-28 13:19
Entscheidungsverhalten im Feld,westward dipping Greenbrier Limestone. The underlying Maccrady Shale, an effective aquiclude is exposed at the land surface along the southeastern edge, forming a groundwater dam between the karst and the deeply incised Greenbrier River. All drainage in the central portion of the Little Levels is su作者: syring 時間: 2025-3-28 15:00 作者: Adrenal-Glands 時間: 2025-3-28 19:19 作者: 好忠告人 時間: 2025-3-28 23:35 作者: 稀釋前 時間: 2025-3-29 04:38
Zeitoptimales Weihnachtsliedersingen,tween the town of Lewisburg and Spring Creek in central Greenbrier County. The total combined surveyed passage is just over 128?km (80 miles). The Hole is the northernmost of the contact caves and drains north to Spring Creek. Ludington, McClung, Maxwelton Sink, Benedict, and Wades caves drain south作者: Rustproof 時間: 2025-3-29 08:29 作者: Critical 時間: 2025-3-29 14:26
Rainer Krumm,Christian Geissler Levels karst surface bounded by the Greenbrier River to the north, Second Creek to the south and west, and shales and sandstones to the east. Organ Cave is a contact cave with the active drainage cut into the underlying Maccrady shale. It displays a dendritic drainage system with multiple streams m作者: 持續(xù) 時間: 2025-3-29 17:01
Rainer Krumm,Christian Geisslertton Limestone. Eight significant caves are reported within this basin, and all of the passages are developed in the Patton, Sinks Grove, and Hillsdale units. Several of the entrances receive small streams and are at the contact of the Hillsdale Limestone and the Maccrady Shale. The caves, with the 作者: 公司 時間: 2025-3-29 20:54
Online-Medien und Personalmanagement,tion of the cave was controlled by a combination of structural and hydrologic factors. Geologic structure provided a pre-solutional network of faults, joints, and bedding planes in the bedrock that was later exploited by groundwater flux. The cave is situated on the western limb of the Sinks Grove A作者: GLOOM 時間: 2025-3-30 00:09
Online-Medien und Personalmanagement,eloped conduit system transports waters through this upland basin via a series of branchwork passages. The main underground stream, the Mystic River, flows 10.4?km (6.5 miles) and has both eastern and western tributaries, fed by a combination of concentrated and diffuse recharge. Upper-level passage作者: Juvenile 時間: 2025-3-30 04:24
Erfolgskontrolle der Online- Kommunikationl Creek, a tributary of Indian Creek and thus of the New River. The underground route of Laurel Creek passes through Laurel Creek Cave, Rimstone-Crossroads Cave, and Greenville Saltpeter Cave. The caves are in nearly flat bedding near the crest of the Abbs Valley Anticline.作者: 非秘密 時間: 2025-3-30 12:03 作者: Fallibility 時間: 2025-3-30 15:43
https://doi.org/10.1007/978-3-8349-8897-3a is dominated by crustaceans and especially amphipods of the genus ., and they primarily occupy vadose streams and the epikarst, but are notably absent from phreatic waters. . is the most widely distributed, found in 59 caves. The segmented worm . and the salamander . are both endemic to single sit作者: 鴕鳥 時間: 2025-3-30 19:22
https://doi.org/10.1007/978-3-319-65801-8Large Caves; Cave Organisms; Caves and Karst; Cave Exploration; Greenbrier Karst; Greenbrier River; Greenb作者: fibroblast 時間: 2025-3-30 21:26
978-3-319-88110-2Springer International Publishing AG 2018作者: 瑪瑙 時間: 2025-3-31 04:11
Hydrology of the Greenbrier Karst,ch of the flow through the aquifer is through conduits under open channel conditions much like a surface stream with a roof. Discharge is concentrated at large springs that typically display rapid response to storm events, and the ratio of maximum to minimum discharge exceeds 100:1 for most of the s作者: 愛管閑事 時間: 2025-3-31 07:42 作者: ABYSS 時間: 2025-3-31 12:41 作者: abreast 時間: 2025-3-31 15:17 作者: NICHE 時間: 2025-3-31 19:37
Scott Hollow Cave,by regional flexures resulting from Alleghenian compressive stress and an unmapped thrust fault. Tributaries joining the Mystic River from the east generally trend down dip along bedding planes, while western tributaries follow steeper, more complex paths, at least partially controlled by a thrust f作者: 憤慨一下 時間: 2025-3-31 22:43 作者: innate 時間: 2025-4-1 05:01 作者: GULP 時間: 2025-4-1 07:37
Berücksichtigung von Ressourcenverbindungench of the flow through the aquifer is through conduits under open channel conditions much like a surface stream with a roof. Discharge is concentrated at large springs that typically display rapid response to storm events, and the ratio of maximum to minimum discharge exceeds 100:1 for most of the s作者: Cantankerous 時間: 2025-4-1 10:15
Innovation und Entrepreneurship during floods. Three stalagmites were used to study local climates over the past 7,000?years. The most detailed time series record multiple dry periods lasting centuries. The “droughts” coincided with Bond Events, which were episodic periods of enhanced ice-rafting in the North Atlantic Ocean belie作者: Apraxia 時間: 2025-4-1 16:24 作者: Pruritus 時間: 2025-4-1 20:55
Online-Medien und Personalmanagement,canyons at their origin, and contain some active water. The middle level comprises mainly large phreatic passages, but with substantial clastic fills. The lower levels are well-developed canyon passages that run down dip and crosscut and incise below the main level of the cave. Conduit cross-section
