Relevant bibliographies by topics / Cave

Academic literature on the topic 'Cave'

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Published: 4 June 2021
Last updated: 7 July 2024

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Journal articles on the topic "Cave"

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Jacoby, Brianne S., Eric W. Peterson, John C. Kostelnick, and Toby Dogwiler. "Approaching Cave Level Identification with GIS: A Case Study of Carter Caves." ISRN Geology 2013 (August 28, 2013): 1–7. http://dx.doi.org/10.1155/2013/160397.

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Cave passages that are found at similar elevations are grouped together and called levels. The current understanding is that passages within a level are speleogenetically linked to a common static baselevel or stratigraphic control. Cave levels have provided an interpretive framework for deciphering cave development, landscape evolution, and climatic changes. Cosmogenic dating has been successfully used to interpret levels in Mammoth Cave and the Cumberland Plateau; however, this technique is expensive and there are limited funding resources available. Geographic information systems may be used as preliminary procedures to identify cave levels and constrain the timing of level development. A GIS method is applied to the Carter Cave system in northeastern Kentucky. Cave entrance elevations along stream valleys were found by extracting elevation values from a m digital elevation model. Using a histogram generated from the frequency of cave elevations and a natural breaks classifier, four cave levels were identified in the Carter Cave system. This work improves the understanding of the Carter Cave system evolution and contributes toa methodology that can be used to ascertain an erosion history of karst systems.
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Gurgen, Gurcan. "Caves and cave art." New Trends and Issues Proceedings on Humanities and Social Sciences 6, no. 4 (September 24, 2019): 100–105. http://dx.doi.org/10.18844/prosoc.v6i4.4403.

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This paper aims to discuss the impact and importance of the karstic caves, which are effective on the emergence and development of cave art and the rocks that generate them. The origin of cave traces to 40 thousand years and the creation of many more works of art and the importance of the rocks to the present day is very important. In particular, carbonate rocks such as limestone and marble became important spaces and raw materials in terms of art history and development. Carbonate deposits placed in the large ocean bowls during geological periods have been elevated and altered land during orogenesis periods. The fact that the carbonate rocks are soluble due to environmental conditions has led to the formation of a large number of caves depending on the size and distribution of the masses forming them. These karstic caves, which constitute a significant part of the caves in the world, have been the habitat of old people for almost 1-1.5 million years. The caves have been very important shelters for life, which became difficult due to the cold climatic conditions during the glacial periods, which were effective during the last 2 million years (Pleistocene). Under the challenging conditions of the Paleolithic period, human societies have tried to survive on the one hand and, on the other hand, achieved their symbolic thinking skills with their developing brain capacities 100,000 years ago. In the following period, the human communities that continued to develop have left very important ruins, which dates back to 40-10 thousand years ago and are regarded as works of art. Structural features of the caves and the rocks forming them are of great importance in the emergence of these works, which are interesting in their techniques as well as their thought style. Karst caves are very suitable for processing in terms of scraping, embossing and various painting techniques depending on the mineral structure of limestone. Besides, since these caves are difficult to access and are prevented from external dangers and risks, they are of great importance for the emergence of this art and reaching to the present day. Keywords: Cave, Karstic rock, Cave art
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Bowery, Anne-Marie, and Scott Hunter Moore. "Neither Cave nor Cage." Inquiry: Critical Thinking Across the Disciplines 18, no. 4 (1999): 36–54. http://dx.doi.org/10.5840/inquiryctnews199918412.

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Schmalzgruber, Hedwig. "Cave canem." Hermes 149, no. 1 (2021): 83. http://dx.doi.org/10.25162/hermes-2021-0007.

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Lutz, B., and M. Weintke. "Virtual Dunhuang Art Cave: A Cave within a CAVE." Computer Graphics Forum 18, no. 3 (September 1999): 257–64. http://dx.doi.org/10.1111/1467-8659.00346.

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Gomell, Annika K., and Andreas Pflitsch. "Airflow dynamics in Wind Cave and Jewel Cave: How do barometric caves breathe?" International Journal of Speleology 51, no. 3 (October 2022): 163–79. http://dx.doi.org/10.5038/1827-806x.51.3.2437.

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Recent research on air pressure propagation through barometric caves has revealed various speleoclimatological processes, which cause a more complex relationship between surface air pressure changes and resulting pressure gradients between cave and surface air than previously assumed. So far, however, studies on barometric cave airflow have only been based on surface air pressure measurements. Thus, this study investigates and compares airflow at the openings of Wind Cave and Jewel Cave – two major barometric cave systems in South Dakota, USA – as a response to surface air pressure changes and air pressure gradients. Based on high-resolution long-term air pressure measurements from the surfaces and several locations inside the caves, as well as ultra-sonic airflow measurements at the openings, the analysis proves that for both caves, cave airflow velocity can be predicted more accurately by air pressure gradients than by previous surface air pressure changes. An inter-cave comparison also reveals substantial differences in cave airflow dynamics between Wind Cave and Jewel Cave, with the relevant period of surface air pressure variations for cave airflow velocity and the cave reaction times being significantly longer at Jewel Cave compared to Wind Cave. Therefore, the findings of this study demonstrate the effects of cave morphology on airflow and significantly contribute to a better understanding of the speleoclimatological mechanisms and dynamics of compensating airflow at the openings of barometric caves.
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Bahn, Paul G. "Cave art without the caves." Antiquity 69, no. 263 (June 1995): 231–37. http://dx.doi.org/10.1017/s0003598x00064632.

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It is over a decade since Palaeolithic parietal art was first spotted in Europe on exposed open-air surfaces—cave art without the caves. Now the major site in Portugal is threatened by the lake behind a river-dam under construction. Here is a report on what cave art outside the caves amounts to, and of the confrontations over the Côa site that were in the headlines early this year.
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Puşcaş, Cristina M., Ferenc Kristaly, Ciprian C. Stremţan, Bogdan P. Onac, and Herta S. Effenberger. "Stability of cave phosphates: Case study from Liliecilor Cave (Trascău Mountains, Romania)." Neues Jahrbuch f??r Mineralogie - Abhandlungen: Journal of Mineralogy and Geoche 191, no. 2 (February 1, 2014): 157–68. http://dx.doi.org/10.1127/0077-7757/2014/0254.

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Alexandrowicz, Zofia, Jan Urban, and Viacheslav Andreychouk. "Crystal Caves in the ‘Wieliczka’ Salt Mine – unique cave site." Zeitschrift für Geomorphologie, Supplementary Issues 62, no. 3 (March 12, 2021): 235–54. http://dx.doi.org/10.1127/zfg_suppl/2021/0696.

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Kong, Dal-Yong, Seong-Joo Lee, Chang-Pyo Jun, and Yeong-Kyoo Kim. "Mineralogy of Guano Distributed in the Limestone Cave in Korea (Gossi Cave, Baekrong Cave, and Sungryu Cave)." Journal of the Mineralogical Society of Korea 25, no. 3 (September 28, 2012): 131–41. http://dx.doi.org/10.9727/jmsk.2012.25.3.131.

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Dissertations / Theses on the topic "Cave"

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Prieto, Thea. "The Cave." PDXScholar, 2016. http://pdxscholar.library.pdx.edu/open_access_etds/2999.

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Environmental holocaust has driven four people inside of a cave: an elder, holder of stories, a young man poised to assume primacy, a pregnant woman, a child. To escape the desperation of their waning food, water, and health, they tell stories about the past around a diminishing fire. Each character's story draws from a long oral tradition and describes the end of days as a collage of creation myths and historic artifact.
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Brod, Langford Garrett 1927. "Geology and speleogenesis of Colossal Cave, Pima County, Arizona." Thesis, The University of Arizona, 1987. http://hdl.handle.net/10150/558072.

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Miedema, Natalie Margaret. "Non-anthropogenic sources of carbon dioxide in the Glowworm Cave, Waitomo." The University of Waikato, 2009. http://hdl.handle.net/10289/2781.

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The Waitomo Caves attract approximately 500 000 tourists each year. A requirement of tourist cave management is that the partial pressure of carbon dioxide (PCO₂) is kept below levels that are: hazardous to the health of visitors, hazardous to the glowworms and other natural inhabitants, or potentially corrosive to speleothems. For the Glowworm Cave at Waitomo, the maximum permissible PCO₂ level is 2400 ppm. When exceeded, the tourist operators are required to close the cave. Ten years of monitoring data at the Glowworm Cave was analysed. Most of the variation in PCO₂ could be attributed to CO₂ respired by tourists, and the mixing of cave air with lower PCO₂ outside air. Occasionally, there were periods with high PCO₂ levels while the cave was closed to tourists. The main objective of this study was to investigate the potential role of the Waitomo Stream in contributing CO₂ to the Glowworm Cave atmosphere. Analysis of ten years of Glowworm Cave monitoring data showed that the 2400 ppm PCO₂ limit was, on average, exceeded five times each year, with a total of 48 events between 1998 and 2007. Of the PCO₂ limit exceedences, approximately 31% of events were largely driven by high tourist numbers; 27% of PCO₂ limit exceedences were mainly driven by increased discharge, rainfall, and/or a low temperature gradient between the cave and outside air, whilst 29% of the PCO₂ limit exceedences were due to a combination of tourists and increased discharge, rainfall, and/or a low temperature gradient. The remaining 13% of exceedences were unexplained by tourists or the factors investigated. It may be that the unexplained exceedences were due to the night time closure of the cave door, restricting air exchange. The PCO₂ of the Waitomo Stream was measured by equilibrating air with the streamwater within a closed loop. The air was passed continuously through an infrared gas analyser (IRGA). The streamwater PCO₂ typically ranged between 600 - 1200 ppm. Fluctuations in the PCO₂ of the Waitomo Stream coincided with PCO₂ fluctuations in the Glowworm Cave air, and under most conditions, the stream probably acted as a sink for cave air CO₂. However, following rainfall events, the stream PCO₂ increased, exceeding cave air PCO₂, thus acting as a source of CO₂ to the cave air. High stream PCO₂ often occurred at times when air flow through the cave was restricted, e.g. when the temperature gradient between the cave air and outside air was low, or stream levels were high, thus limiting air movement. The combination of high stream PCO₂ and a low temperature gradient increased the likelihood of high cave air PCO₂. Dripwater was measured to determine whether an increase in dripwater PCO₂ occurred in response to rainfall events. When rainfall events resulted in increased discharge, the dripwater PCO₂ sometimes increased (occasionally exceeding 5000 ppm), however the pattern was not consistent. The chemistry of the Waitomo and Okohua (Ruakuri) Streams was monitored with daily samples collected and analysed for major ions: HCO₃ -, Ca²⁺, Na⁺ and Mg²⁺, and δ¹³C stable isotope. The HCO₃ -, Ca²⁺, Na⁺ and Mg²⁺ concentrations in the streamwater decreased with increased discharge, presumably due to dilution. Increased discharge following rainfall events correlated with increasing PCO₂ in the Waitomo Stream, suggesting that soil atmosphere CO₂ dissolved in soil waters, and carried to the stream by saturated flow, was responsible for the streamwater PCO₂ increase. Ca in the stream showed both an increase and a decrease with respect to rainfall. Increased Ca in the stream occurred at times when the discharged waters were coming from the phreatic zone, and thus sufficient time had lapsed for CO₂ in the discharge waters to react with the limestone (carbonate dissolution reaction). Decreased Ca occurred when the infiltration and percolation of rainwater was rapid, and thus the streamwater was characterised by a higher PCO₂ and a lower Ca concentration, as insufficient time had lapsed for the discharge waters to equilibrate with the limestone. Increased negativity in the δ¹³C of the Waitomo and Ruakuri Streams coincided with increased discharge. During summer low flow, the δ¹³C of Waitomo Stream waters was -11.3‰, whereas during high stream discharge events, the δ¹³C dropped to -12 - -14‰. The δ¹³C of limestone is 0‰, the atmosphere is -7‰, and the soil atmosphere is reported to be about -24‰, thus the decrease in δ¹³C during high flow events supports the contention that soil atmosphere CO₂ is a likely source of the increased CO₂ in flood waters.
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Hubbard, Jackson Durain. "3D Cave and Ice Block Morphology from Integrated Geophysical Methods: A Case Study at Scărişoara Ice Cave, Romania." Scholar Commons, 2017. http://scholarcommons.usf.edu/etd/6712.

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Scărişoara Ice Cave has been a catalyst of scientific intrigue and effort for over 150 years. These efforts have revealed and described countless natural phenomena – and in the process have made it one of the most studied caves in the world. Of especial interest is the massive ice block located within its Great Hall and scientific reservations. The ice block, which is the oldest and largest known to exist in a cave, has been the focus of multiple surveying and mapping efforts, typically ones utilizing traditional equipment. In this study, the goals were to reconstruct the ice block/cave floor interface and to estimate the volume of the ice block. Once the models were constructed, we aimed to study the relationships between the cave and ice block morphologies. In order to accomplish this goal, three (3) main datasets were collected, processed, and amalgamated. Ground penetrating radar data was used to discern the floor morphology below the ice block. Over 1,500 photographs were collected in the cave and used with Structure from Motion photogrammetry software to construct a texturized 3D model of the cave and ice surfaces. And a total station survey was performed to scale, georeference, and validate each model. Once georeferenced, the data was imported into an ArcGIS geodatabase for further analysis. The methodology described within this study provides a powerful set of instructions for producing highly valuable scientific data, especially related to caves. Here, we describe in detail the novel tools and software used to validate, inspect, manipulate, and measure morphological information while immersed in a fully 3D experience. With this methodology, it is possible to easily and inexpensively create digital elevation models of underground rooms and galleries, to measure the differences between surfaces, to create 3D models from the combination of surfaces, and to intimately inspect a subject area without actually being there. At the culmination of these efforts, the partial ice block volume was estimated to be 118,000 m3 with an uncertainty of ± 9.5%. The volume computed herein is significantly larger than previously thought and the total volume is likely significantly larger, since certain portions were not modeled during this study. In addition, the morphology of ceiling enlargement was linked to areas of high elevation at the base of the ice block. A counterintuitive depression was recognized at the base of the Entrance Shaft. The thickest areas of the ice were identified for future coring projects. And combining all this a new informational allowed us to propose a new theory on the formation of the ice block and to decipher particular speleogenetic aspects.
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Hochstetler, Bethany Irene. "EVALUATION OF CLASTIC CAVE SEDIMENT RECORD VARIABILITY." University of Akron / OhioLINK, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=akron1136495477.

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McCann, Sarah C. "Atmospheric influences on cave meteorology, Jinapsan Cave, Guam| A drip rate analysis." Thesis, Mississippi State University, 2013. http://pqdtopen.proquest.com/#viewpdf?dispub=1536130.

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Temperature, pressure, and relative humidity within Jinapsan Cave on Guam were compiled and analyzed over a five-month period to gain a better understanding of this environment. Temperatures within the cave hover around ~26°C with no apparent influences except the mean annual temperature, with humidity values over 90%. There is high fidelity between outside and internal air pressures indicating no pressure differential exists and pressure changes are a result of kinematic wave flow. A mild correlation exists between a cave speleothem's drip rate and outside pressure. The cave's tidal pool compared to oceanic tides show a lag of 1-2 hours and amplitude dampening. The tidal pool's temperature is 25.7°C, signifying no mass transfer of water occurs. Tropical cave studies are rare, but are important for paleoclimate research using cave speleothems as proxies. This study determined cave meteorological factors that affect speleothem development to allow for more accurate paleoclimate studies.

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FARAUD, MOURARD ISABELLE. "Syndrome cave superieur par thrombose secondaire au catheterisme du reseau cave superieur." Nice, 1989. http://www.theses.fr/1989NICE6555.

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Stephenson, Jason. "Methanotrophy in Movile Cave." Thesis, University of Warwick, 2014. http://wrap.warwick.ac.uk/69299/.

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Movile Cave is an isolated cave ecosystem that receives no input of photosynthetically fixed carbon. Instead, carbon is primarily fixed through light- independent bacterial processes such as chemolithoautotrophy and methanotrophy. Distinctive microbial floating mats appear at the surface of groundwater flooding the cave, at the redox interface between the oxygenated air above (7-10%) and the anaerobic water below. Methane, of geological origin, bubbles up into the cave and is present in the cave atmosphere (0.5-1%). The in situ methanotroph community of Movile Cave microbial floating mat was determined by examination of metagenomic sequencing and pmoA gene microarray data sets. The metagenonomic sequencing approach indicated a Methylococcus capsulatus -like organism to be the most abundant methanotroph in Movile Cave. pmoA microarray analysis indicated a high abundance of Methylocystis pmoA gene sequences with Methylococcus capsulatus-like pmoA gene sequences being relatively abundant. The methane oxidising bacterium Methylomonas strain LWB was isolated from a sample of lake water from Movile Cave. Phylogenetic analysis of the genes encoding 16S rRNA and the soluble and particulate methane monooxygenase functional gene markers pmoA and mmoX, respectively, confirmed that strain LWB belongs to the genus Methylomonas. Methylomonas LWB has a second putative copy of the particulate methane monooxygenase pXM which displays an unusual gene orientation. The Methylomonas LWB genome contains all genes encoding the typical Type I methanotroph ribulose monophosphate pathway for formaldehyde assimilation and all genes required for a complete TCA cycle. Active methane oxidisers in Movile Cave were identified by DNA Stable-isotope probing. Organisms belonging to the genera Methylomonas, Methylocystis, Methylococcus and Methylobacter- were identified from 13C-enriched DNA. Cross-feeding of the 13C label into non-methanotrophic organisms identified from the 13C-enriched DNA indicated that methanotrophs provide a carbon source for other microorganisms in Movile Cave.
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Kolčárek, Michal. "Augmented Reality in CAVE." Master's thesis, Vysoké učení technické v Brně. Fakulta informačních technologií, 2013. http://www.nusl.cz/ntk/nusl-236405.

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Tato práce se zaměřuje na technologii Cave Automatic Virtual Environment a konkrétně pak na využití principů rozšířené reality v tomto prostředí. Dává si za cíl odpovědět na otázku, zdali je možné použít v prostředí CAVE existující frameworky pro rozšířenou realitu, konkrétně ty, pracující na platformě iOS. Hlavní důraz je kladen na rozpoznávání markerů v tomto prostředí a na zvýšení přesnosti jejich rozpoznání. Práce odpovídá na množství otázek z této oblasti, jako jaké markery je vhodné použít, jaké jsou omezení a největší obtíže. Výstupem je demonstrační aplikace, pracující na platformě iOS, která v je prostředí CAVE otestovaná a plně použitelná. Tato aplikace by měla vylepšit uživatelský vjem z prostředí CAVE tím, že mu poskytne dodatečné informace a také základní možnosti interakce se zobrazenými objekty.
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Elmore, Clinton. "Comparing Structure from Motion Photogrammetry and Computer Vision for Low-Cost 3D Cave Mapping: Tipton-Haynes Cave, Tennessee." Digital Commons @ East Tennessee State University, 2019. https://dc.etsu.edu/etd/3608.

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Natural caves represent one of the most difficult environments to map with modern 3D technologies. In this study I tested two relatively new methods for 3D mapping in Tipton-Haynes Cave near Johnson City, Tennessee: Structure from Motion Photogrammetry and Computer Vision using Tango, an RGB-D (Red Green Blue and Depth) technology. Many different aspects of these two methods were analyzed with respect to the needs of average cave explorers. Major considerations were cost, time, accuracy, durability, simplicity, lighting setup, and drift. The 3D maps were compared to a conventional cave map drafted with measurements from a modern digital survey instrument called the DistoX2, a clinometer, and a measuring tape. Both 3D mapping methods worked, but photogrammetry proved to be too time consuming and laborious for capturing more than a few meters of passage. RGB-D was faster, more accurate, and showed promise for the future of low-cost 3D cave mapping.
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Books on the topic "Cave"

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Fiol, Bartomeu. Cave Carmina, cape canes. Mallorca: Editorial Moll, 1998.

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ill, McLoughlin Wayne, ed. Cave. New York: HarperCollins, 2000.

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Cave. New York: F. Watts, 1989.

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Cave. Paris]: Gallimard, 2021.

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ill, Wynne Patricia, ed. Cave. New York: Scientific American Books for Young Readers, 1993.

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Spilsbury, Richard. Cave. Chicago, Ill: Capstone Heinemann Library, 2013.

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von Ehrenfried, Manfred "Dutch." From Cave Man to Cave Martian. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-05408-3.

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Boer, Roland. Cave droppings: Nick Cave and religion. Oakville, CT: Equinox Pub., 2012.

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1927-, Sullivan G. Nicholas, and National Speleological Society, eds. Speleology: Caves and the cave environment. 3rd ed. St. Louis: Cave Books, 1997.

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Judi, Thompson, ed. Mammoth Cave and the Kentucky cave region. Charleston, SC: Arcadia, 2003.

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Book chapters on the topic "Cave"

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Chirienco, Mirona, and Aurel Perşoiu. "Cave." In Encyclopedia of Planetary Landforms, 1–5. New York, NY: Springer New York, 2014. http://dx.doi.org/10.1007/978-1-4614-9213-9_32-1.

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Chirienco, Mirona, and Aurel Perşoiu. "Cave." In Encyclopedia of Planetary Landforms, 227–31. New York, NY: Springer New York, 2015. http://dx.doi.org/10.1007/978-1-4614-3134-3_32.

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Spellman, Frank R. "Cave to Allegorical Cave to Present." In The Science of Waste, 7–18. Boca Raton: CRC Press, 2021. http://dx.doi.org/10.1201/9781003252665-2.

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Hunt, Chris O. "Niah Cave." In Encyclopedia of Geoarchaeology, 547–48. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-1-4020-4409-0_100.

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Karkanas, Panagiotis, and Paul Goldberg. "Cave Settings." In Encyclopedia of Geoarchaeology, 108–18. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-1-4020-4409-0_151.

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Haaland, Magnus M., and Christopher S. Henshilwood. "Blombos Cave." In Encyclopedia of Geoarchaeology, 75–76. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-1-4020-4409-0_188.

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Goldberg, Paul. "Kebara Cave." In Encyclopedia of Geoarchaeology, 453–55. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-1-4020-4409-0_88.

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Shidrang, Sonia, Marcel Otte, and Jean-Guillume Bordes. "Yafteh Cave." In Encyclopedia of Global Archaeology, 11389–96. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-30018-0_3270.

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Lucas, Philip C. "Helictite Cave." In The Caves of Burnsville Cove, Virginia, 205–36. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-14391-0_12.

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Niemiller, Matthew L., and Daphne Soares. "Cave Environments." In Extremophile Fishes, 161–91. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-13362-1_8.

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Conference papers on the topic "Cave"

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Petzold, Frank, Oliver Bimber, and Christian Tonn. "CAVE without CAVE." In eCAADe 2007: Predicting the Future. eCAADe, 2007. http://dx.doi.org/10.52842/conf.ecaade.2007.161.

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"Cave." In 2018 11th International Conference on Human System Interaction (HSI). IEEE, 2018. http://dx.doi.org/10.1109/hsi.2018.8430952.

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Ali-Eldin, Ahmed, Chirag Goel, Mayank Jha, Bo Chen, Klara Nahrstedt, and Prashant Shenoy. "CAVE." In MMSys '22: 13th ACM Multimedia Systems Conference. New York, NY, USA: ACM, 2022. http://dx.doi.org/10.1145/3534088.3534350.

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Park, Sung Kyu, Youngwoo Park, Gyudong Shim, and Kyu Ho Park. "CAVE." In the 2011 ACM Symposium. New York, New York, USA: ACM Press, 2011. http://dx.doi.org/10.1145/1982185.1982262.

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Layng, Kris, Ken Perlin, Sebastian Herscher, Corinne Brenner, and Thomas Meduri. "Cave." In SIGGRAPH '19: Special Interest Group on Computer Graphics and Interactive Techniques Conference. New York, NY, USA: ACM, 2019. http://dx.doi.org/10.1145/3306211.3320138.

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Williams, Abigail, and Patricia N. Kambesis. "CAVE SEDIMENT ANALYSIS IN CAVE VALLEY CAVE, NEVADA: IMPLICATIONS FOR DESERT HYDROLOGY." In 68th Annual GSA Southeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019se-327214.

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Tan, Liangcheng, Jingyao Zhao, Dong Li, and Yongli Gao. "Cave air CO2 monitoring in Shenqi Cave, southwest China." In National Cave and Karst Research Institute Symposium 8. National Cave and Karst Research Institute, 2020. http://dx.doi.org/10.5038/9781733375313.1006.

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Becker, Sascha, Shawn Greenlee, Dmitri Lemmerman, Morgan McGuire, Nicholas Musurca, and Noah Wardrip-Fruin. "Cave writing." In ACM SIGGRAPH 2005 Sketches. New York, New York, USA: ACM Press, 2005. http://dx.doi.org/10.1145/1187112.1187248.

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Hocking, Rodney, Glen Balog, Tessa Ormerod, and Heather Pearce. "Early cave management at the Carrapateena sublevel cave." In Fourth International Symposium on Block and Sublevel Caving. Australian Centre for Geomechanics, Perth, 2018. http://dx.doi.org/10.36487/acg_rep/1815_32_hocking.

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Steele, Nicholas E. "CAVE CLIMATE CHARACTERIZATION AND EXAMINING THE EFFECTIVENESS OF CAVE MANAGEMENT PRACTICES - TIMPANOGOS CAVE NATIONAL MONUMENT." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283887.

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Reports on the topic "Cave"

1

Prieto, Thea. The Cave. Portland State University Library, January 2000. http://dx.doi.org/10.15760/etd.3000.

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Rosse, Anine. Cave water quality monitoring for Wind Cave National Park: 2021 data report. National Park Service, November 2022. http://dx.doi.org/10.36967/2295296.

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Weissinger, Rebecca, Andy Armstrong, Kirsten Bahr, and Chris Groves. Trends in water quality of cave pools at Timpanogos Cave National Monument, July 2008–September 2018. Edited by Alice Wondrak Biel. National Park Service, October 2020. http://dx.doi.org/10.36967/nrr-2279316.

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Spela Goricki, Spela Goricki. Through a glass darkly: assessing population size of an endangered cave salamander from samples of spring and cave water. Experiment, October 2016. http://dx.doi.org/10.18258/8166.

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Reger, D. R., and C. R. Campbell. Preliminary report, 1985, Sakie Bay Cave, CRG-230. Alaska Division of Geological & Geophysical Surveys, 1985. http://dx.doi.org/10.14509/1129.

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Schwemm, Catherin, and Donna Shorrock. Natural resource condition assessment: Timpanogos Cave National Monument. National Park Service, November 2020. http://dx.doi.org/10.36967/nrr-2279634.

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Markus Friedrich, Markus Friedrich. Exploring the temperature tolerance of a cave beetle. Experiment, October 2016. http://dx.doi.org/10.18258/8137.

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Groves, Chris, Autumn Singer, Lee Anne Bledsoe, Rickard Toomey, Katie Algeo, and Cathleen Webb. Natural resource condition assessment: Mammoth Cave National Park. National Park Service, May 2021. http://dx.doi.org/10.36967/nrr-2286525.

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Reger, D. R., and C. R. Campbell. Early historic use of Sakie Bay Cave, CRG-230. Alaska Division of Geological & Geophysical Surveys, 1986. http://dx.doi.org/10.14509/1223.

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Herring, Theodore, Justin Tweet, and Vincent Santucci. Wind Cave National Park: Paleontological resource inventory (sensitive version). National Park Service, May 2023. http://dx.doi.org/10.36967/2299199.

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