Relevant bibliographies by topics / Mammoth Cave

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Mammoth Cave'

Author: Grafiati
Published: 4 June 2021
Last updated: 26 July 2025

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Journal articles on the topic "Mammoth Cave"

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Veltre, Douglas W., David R. Yesner, Kristine J. Crossen, Russell W. Graham, and Joan B. Coltrain. "Patterns of faunal extinction and paleoclimatic change from mid-Holocene mammoth and polar bear remains, Pribilof Islands, Alaska." Quaternary Research 70, no. 1 (2008): 40–50. http://dx.doi.org/10.1016/j.yqres.2008.03.006.

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Abstract Cave, a lava tube cave on St. Paul Island in the Pribilofs, has recently produced a mid-Holocene vertebrate faunal assemblage including woolly mammoth, polar bear, caribou, and Arctic fox. Several dates on the mammoth remains converge on 5700 14C yr BP. These dates, ~ 2300 yr younger than mammoth dates previously published from the Pribilof Islands, make these the youngest remains of proboscideans, and of non-extinct Quaternary megafauna, recovered from North America. Persistence of mammoths on the Pribilofs is most parsimoniously explained by the isolation of the Pribilofs and the la
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Niemiller, Matthew L., Kurt Helf, and Rickard S. Toomey. "Mammoth Cave: A Hotspot of Subterranean Biodiversity in the United States." Diversity 13, no. 8 (2021): 373. http://dx.doi.org/10.3390/d13080373.

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The Mammoth Cave System in the Interior Low Plateau karst region in central Kentucky, USA is a global hotspot of cave-limited biodiversity, particularly terrestrial species. We searched the literature, museum accessions, and database records to compile an updated list of troglobiotic and stygobiotic species for the Mammoth Cave System and compare our list with previously published checklists. Our list of cave-limited fauna totals 49 species, with 32 troglobionts and 17 stygobionts. Seven species are endemic to the Mammoth Cave System and other small caves in Mammoth Cave National Park. The Mam
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Cohen, Lara Langer. "“The Blackness of Darkness”." History of the Present 11, no. 1 (2021): 2–22. http://dx.doi.org/10.1215/21599785-8772436.

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Abstract This article considers Kentucky’s Mammoth Cave as an unexpected site for nineteenth-century theorizations of racialized Blackness. Mammoth Cave became a major tourist attraction in the 1840s, generating a host of guidebooks, travel accounts, magazine illustrations, panoramas, newspaper articles, and fiction. Crucial to its fame was the fact that the guides who led visitors through the cave were enslaved men. This article argues that white writers responded to the guides’ knowledge of the cave by reframing it as affinity. In doing so, they transformed Mammoth Cave’s subterranean darkne
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Henrikson, L. Suzann, David A. Byers, Robert M. Yohe, Matthew M. DeCarlo, and Gene L. Titmus. "FOLSOM MAMMOTH HUNTERS? THE TERMINAL PLEISTOCENE ASSEMBLAGE FROM OWL CAVE (10BV30), WASDEN SITE, IDAHO." American Antiquity 82, no. 3 (2017): 574–92. http://dx.doi.org/10.1017/aaq.2017.14.

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The 1960s and 1970s excavations at Owl Cave (10BV30) recovered mammoth bone and Folsom-like points from the same strata, suggesting evidence for a post-Clovis mammoth kill. However, a synthesis of the excavation data was never published, and the locality has since been purged from the roster of sites with human/extinct megafauna associations. Here, we present dates on bone from the oldest stratum, review provenience data, conduct a bone-surface modification study, and present the results of a protein-residue analysis. Our study fails to make the case for mammoth hunting by Folsom peoples. Alth
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Bledsoe, Lee Anne, Chris Groves, and Rick Toomey. "The Mammoth Cave National Park World Heritage Site." Zeitschrift für Geomorphologie, Supplementary Issues 62, no. 3 (2021): 145–93. http://dx.doi.org/10.1127/zfg_suppl/2021/0694.

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Palmer, A. N. "The Mammoth Cave system, Kentucky, USA." Boletín Geológico y Minero 127, no. 1 (2016): 131–45. http://dx.doi.org/10.21701/bolgeomin.127.1.009.

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Mammoth Cave is the main attraction of Mammoth Cave National Park. For several decades it has been the longest known cave in the world and currently contains 652 km in 2016 of surveyed passages. It is located in the heart of an extensive karst plateau, in which the stratal dip averages only one degree. The cave is part of a drainage basin of more than 200 km². The cave has been known to local inhabitants for several millennia and contains a rich trove of archaeological and historical artifacts. It contains many speleo biota including several rare and endangered species and has been designated
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Mead, Jim I., Larry D. Agenbroad, Owen K. Davis, and Paul S. Martin. "Dung of Mammuthus in the Arid Southwest, North America." Quaternary Research 25, no. 1 (1986): 121–27. http://dx.doi.org/10.1016/0033-5894(86)90048-7.

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The discovery of a unique organic deposit in a dry cave on the Colorado Plateau, southern Utah, permits the first comparison of the physical characteristics and the diet of the dung of the extinct mammoths from the arid Southwest, North America, with that of mammoths from Siberia and northern China, the only other known locations of such remains. The deposit buried beneath sand and rockfall is composed primarily of mammoth dung, estimated at over 300 m3. Radiocarbon dates on dung boluses indicate that the mammoths frequented the cave between approximately 14,700 and 11,000 yr B.P. (the range o
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Bocherens, Hervé, Daniel Billiou, Marylène Patou-Mathis, Dominique Bonjean, Marcel Otte, and André Mariotti. "Paleobiological Implications of the Isotopic Signatures (13C,15N) of Fossil Mammal Collagen in Scladina Cave (Sclayn, Belgium)." Quaternary Research 48, no. 3 (1997): 370–80. http://dx.doi.org/10.1006/qres.1997.1927.

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An isotopic investigation of upper Pleistocene mammal bones and teeth from Scladina cave (Sclayn, Belgium) demonstrated the very good quality of collagen preservation. A preliminary screening of the samples used the amount of nitrogen in whole bone and dentine in order to estimate the preserved amount of collagen before starting the extraction process. The isotopic abundances of fossil specimens from still-extant species are consistent with their trophic position. Moreover, the15N isotopic abundance is higher in dentine than in bone in bears and hyenas, a phenomenon already observed in modern
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Cooper, Martha, and John Cooper. "Observations on the biology of the endangered stygobiotic shrimp Palaemonias alabamae, with notes on P. ganteri (Decapoda: Atyidae)." Subterranean Biology 8 (March 11, 2011): 9–20. https://doi.org/10.3897/subtbiol.8.1226.

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<em>Palaemonias alabamae</em> is endemic to subterranean waters in northern Alabama. Its type locality is Shelta Cave, Madison County, and ostensibly conspecifi c shrimps have been found in Bobcat and two other caves. Pollution and other factors may have extirpated the shrimp from the type locality. In Shelta Cave the species is smaller than the shrimp in Bobcat Cave and <em>P. ganteri</em> in Mammoth Cave, Kentucky. Adult female <em>P. alabamae</em> (s.s.) and <em>P. ganteri</em> are larger than males. Female <em>P. alabamae</em> with visible oocytes or, rarely, attached ova, were observed fr
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Steelman, K. L., M. W. Rowe, V. N. Shirokov, and J. R. Southon. "Radiocarbon dates for pictographs in Ignatievskaya Cave, Russia: Holocene age for supposed Pleistocene fauna." Antiquity 76, no. 292 (2002): 341–48. http://dx.doi.org/10.1017/s0003598x00090426.

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Samples from three charcoal pictographs at Ignatievskaya Cave, in the southern Ural Mountains of Russia, have been radiocarbon dated. An advanced antiquity was expected, with some paintings thought to be more than 10,000 years old, as suggested by the imagery. One charcoal painting, for example, resembles a mammoth. The radiocarbon date of that motif, however, dates only to 7370±50 BP. If that motif actually represents a live mammoth, it places mammoth extinction in the Urals nearer to the present than is currently accepted. A charcoal pigment sample, a drawing of lines radiating from a centra
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Dissertations / Theses on the topic "Mammoth Cave"

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Brunt, Matthew. "Analysis of Mammoth Cave Pre-Park Communities." TopSCHOLAR®, 2009. http://digitalcommons.wku.edu/theses/132.

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Before the creation of Mammoth Cave National Park, this area was home to numerous communities, each with a sense of identity. To prepare for the creation of the National Park, all residents living within these communities were relocated, and many of these communities were lost to the passage of time. Today, public memory of these lost communities is being fostered by the descendents of the pre-park area. Through the use of a Historical Geographic Information System, 1920 Edmonson County manuscript census data, and statistical analysis, the demographic composition of these lost communities was
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Compson, Zacchaeus Greg. "An Isotopic Examination of Cave, Spring and Epigean Trophic Structures in Mammoth Cave National Park." TopSCHOLAR®, 2004. http://digitalcommons.wku.edu/theses/1102.

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AN ISOTOPIC EXAMINATION OF CAVE, SPRING AND EPIGEAN TROPHIC STRUCTURES IN MAMMOTH CAVE NATIONAL PARK Name: Zacchaeus Greg Compson Date: October 15, 2004 Pages: 56 Directed by: Philip Lienesch, Doug McElroy, Michael Stokes and Richard Bowker Department of Biology Western Kentucky University Abstract High-water events in the Green River result in flow-reversals which flush native and introduced fishes into Mammoth Cave, posing threats to indigenous cave fauna. However, little is known about the trophic interactions between
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Jernigan, Jonathan. "Mathematical Modeling of Convective Heat Transfer in Mammoth Cave." TopSCHOLAR®, 1997. http://digitalcommons.wku.edu/theses/787.

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Around two centuries ago, changes were made to the entrances of Mammoth Cave and its passages. Today the Historic Entrance to Mammoth Cave is enlarged and the passage just beyond the entrance known as Houchins' Narrows has been cleared of rubble and filled with sediments. These enlargements have resulted in an increase in airflow throughout the Historic Section of the cave causing environmental conditions such as air temperature and airflow to fluctuate. These fluctuations have negatively impacted inhabitants and contents of the cave system. To restore natural conditions within the cave, Scien
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Taylor, John Edward. "Long-term forest monitoring program for Mammoth Cave National Park." Virtual Press, 1997. http://liblink.bsu.edu/uhtbin/catkey/1041910.

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A long-term forest monitoring program was initiated at Mammoth Cave National Park (MCNP). The objectives of this project were to establish baseline data on the representative forest community types at MCNP based on dominant tree species. Permanent monitoring plots were established in different forest community types throughout the park. A total of 32 permanent plots were established for a combined sample area of 11.4 hectares. All stems larger than 5 cm dbh were measured and mapped within each permanent plot. Data on saplings were also collected. Distributions and abundances were determined fo
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Shell, Melissa K. "Mammoth Cave National Park : distribution and classification of woody vegetation." Virtual Press, 1995. http://liblink.bsu.edu/uhtbin/catkey/941368.

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Mammoth Cave National Park (MCNP) contains a diversity of forest types due to a complex mosaic of landform, rock types and land-use history. The point-centered quarter method was used to collect data for a forested vegetation classification. Stratified random sampling was done in each of the various site types found within the boundaries of MCNP. A classification based on the information available in the matrix of species importance values from each site type was constructed using two-way indicator species analysis (TWINSPAN). Geographic Information System (GIS) analysis was used to devise an
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Warrick, Alyssa Diane. ""Deep" South| Mammoth Cave, Kentucky, and Environmental Knowledge, 1800-1974." Thesis, Mississippi State University, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10642996.

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<p> Mammoth Cave in Kentucky is the longest known cave in the world. This dissertation examines the history of how scientists and non-scientists alike contributed to a growing body of knowledge about Mammoth Cave and how that knowledge in turn affected land use decisions in the surrounding neighborhood. During the nineteenth century visitors traveled through Mammoth Cave along with their guides, gaining knowledge of the cave by using their senses and spreading that knowledge through travel narratives. After the Civil War, cave guides, now free men who chose to stay in the neighborhood, used th
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Jones, Bobette Elaine. "Long-term monitoring program for forest herbs at Mammoth Cave National Park." Virtual Press, 1997. http://liblink.bsu.edu/uhtbin/catkey/1048387.

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A monitoring program of forest herbs was initiated at Mammoth Cave National Park (MCNP). The objectives of this project were to produce a quantitative description of the current forest herb communities which can be used as a baseline for monitoring future change as well as a foundation for making informed management decisions. Herbaceous vegetation in previously established permanent forest monitoring plots was characterized during the summers of 1993-94. In the future, these baseline data can be used to detect changes in forest herb communities that might result from natural succession, manag
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DeWildt, Chris. "Conservation Studies of Insect Cave Faunas in Mammoth Cave National Park and Ghana, West Africa." TopSCHOLAR®, 2007. http://digitalcommons.wku.edu/theses/393.

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As part of a long term ecological monitoring effort at Mammoth Cave National Park, a blind cave beetle, Neaphaenops tellkampfi, was collected and data on populations trends gathered from September 2005 through December 2006 in Great Onyx Cave. The sex and age of each individual in each of 15 sites were determined and density trends of the entire population was measured. The species was chosen due to its role as an indicator species, since potential anthropogenic threats to the environment can be detected via population response. This was the initial implementation of a new monitoring method an
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Slunder, J. Scott. "Field Test of a Calcite Dissolution Rate Law: Fort’s Funnel Cave, Mammoth Cave National Park." TopSCHOLAR®, 1993. http://digitalcommons.wku.edu/theses/1415.

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The laboratory-derived calcite dissolution rate law of Plummer et al. (1978) is the most widely used and mechanistically detailed expression currently available for predicting dissolution rates as a function of water chemistry. Such rate expressions are of great use in understanding timescales associated with limestone karst development. Little work has gone into the field testing of the rate law under natural conditions. This work compared measured dissolution rates measured by a crystal weight loss experiment in Buffalo Creek within Fort’s Funnel Cave, which lies within a pristine, foreste
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Kipper, Chelsey. "Influence of Spring Flow Reversals on Cave Dissolution in a Telogenetic Karst Aquifer, Mammoth Cave, KY." TopSCHOLAR®, 2019. https://digitalcommons.wku.edu/theses/3158.

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An often overlooked connection between karst groundwater systems and surface water is spring flow reversal, the flow of river water into karst springs caused by changes in hydraulic gradient. Karst aquifers are subject to the intrusion of river water when the hydraulic head of a base level river is higher than the hydraulic head of a base level spring. When this occurs, the flow out of the spring reverses, allowing river water to enter base level conduits. River water thus becomes a source of recharge into karst basins, transporting both valuable nutrients and harmful contaminants into karst a
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Books on the topic "Mammoth Cave"

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Hobbs III, Horton H., Rickard A. Olson, Elizabeth G. Winkler, and David C. Culver, eds. Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4.

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D, Cutliff Lewis, Clark Chip, and Eastern National Park and Monument Association., eds. Mammoth Cave. Interpretive Publications, 1985.

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L, Van Camp Mary, ed. Mammoth cave. KC Publications, 1991.

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United States. National Park Service, ed. Mammoth Cave, Mammoth Cave National Park, Kentucky: Official map and guide. The Service, 1994.

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Burnham, Brad. Mammoth Cave: The world's longest cave system. Rosen Pub. Groups's PowerKids Press, 2003.

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

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Olson, Colleen O'Connor. Nine miles to Mammoth Cave: The story of the Mammoth Cave Railroad. Cave Books, 2012.

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Olson, Colleen O'Connor. Scary stories of Mammoth Cave. Cave Books, 2002.

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French, Vivian. Cave-baby and the mammoth. ReadZone, 2015.

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1932-, Watson Patty Jo, ed. Archeology of the Mammoth Cave area. Cave Books, 1997.

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Book chapters on the topic "Mammoth Cave"

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Greb, Stephen F. "Mammoth Cave." In Carboniferous Geology of the Eastern United States: St. Louis, Missouri to Washington, D.C. June 28–July 8, 1989. American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft143p0050.

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Toomey, Rickard S., Horton H. Hobbs, and Rickard A. Olson. "An Orientation to Mammoth Cave and This Volume." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_1.

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Olson, Rickard A. "Mammoth Cave Meteorology." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_10.

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Colburn, Mona L. "Under Foot: The Paleontology of Mammoth Cave." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_11.

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Olson, Rickard A. "Landscape Ecology of Mammoth Cave: How Surface and Cave Ecosystems Influence Each Other." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_12.

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Poulson, Thomas L. "Terrestrial Cave Ecology of the Mammoth Cave Region." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_13.

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Helf, Kurt L., and Rickard A. Olson. "Subsurface Aquatic Ecology of Mammoth Cave." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_14.

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Culver, David C., and Horton H. Hobbs. "Biodiversity of Mammoth Cave." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_15.

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Lavoie, Kathleen H. "Mammoth Cave Microbiology." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_16.

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Thomas, Steven C., and Rickard S. Toomey. "Bats of Mammoth Cave." In Mammoth Cave. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53718-4_17.

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Conference papers on the topic "Mammoth Cave"

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Brucker, Roger W. "Can the Transpark Contaminate Mammoth Cave?" In Ninth Multidisciplinary Conference on Sinkholes and the Engineering and Environmental Impacts of Karst. American Society of Civil Engineers, 2003. http://dx.doi.org/10.1061/40698(2003)33.

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Nelson, Shakarah, Rickard S. Toomey, Thomas D. Byl, Benjamin V. Miller, and De'Etra Young. "RESPONSE OF MAMMOTH CAVE CYANOBACTERIA TO ULTRAVIOLET LIGHT." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358620.

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Hilgenhurst, Callie. "CHARACTERIZING MICROPLASTIC POLLUTION IN MAMMOTH CAVE NATIONAL PARK." In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-395913.

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Kambesis, Patricia. "MAPPING THE "INCROPS" OF THE MAMMOTH CAVE SYSTEM." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-369675.

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Hilgenhurst, Callie, Eli Kane, Tom Byl, Rickard S. Toomey, and Jessica Oster. "CHARACTERIZING MICROPLASTIC POLLUTION IN MAMMOTH CAVE NATIONAL PARK." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-382329.

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Palmer, Arthur N. "MAMMOTH CAVE AS A RECORD OF REGIONAL GEOMORPHIC EVOLUTION." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321444.

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Osburn, Magdalena, Matthew J. Selensky, Andrew L. Masterson, Rickard S. Toomey, Rickard A. Olson, and Glenn R. Osburn. "GEOMICROBIOLOGY OF MAMMOTH CAVE USING AN ISOTOPE GEOBIOLOGY APPROACH." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-369748.

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Tholen, Jake Michael, Patricia N. Kambesis, Rickard S. Toomey, and Alan E. Kehew. "SUB-BASIN DELINEATION NEAR TURNHOLE BEND, MAMMOTH CAVE NATIONAL PARK." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-290373.

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Davis, Donald G. "The First Decade in Snowy River: Stalking the Mammoth Cave of the West." In 2022 New Mexico Geological Society Annual Spring Meeting & Ft. Stanton Cave Conference. New Mexico Geological Society, 2022. http://dx.doi.org/10.56577/sm-2022.2852.

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Wolf, S., N. Ebinger-Rist, C. J. Kind, and K. Wehrberger. "NEW PERSPECTIVES ON THE LION MAN FIGURINE OF HOHLENSTEIN-STADEL CAVE (SOUTHWESTERN GERMANY)." In Знаки и образы в искусстве каменного века. Международная конференция. Тезисы докладов [Электронный ресурс]. Crossref, 2019. http://dx.doi.org/10.25681/iaras.2019.978-5-94375-308-4.32.

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In the Hohlenstein-Stadel Cave in 1939 excavators uncovered nearly 200 mammoth ivory fragments, which were refitted as a therianthrope figurine with the head and torso of a cave lion but with the legs of a human being. It was thus named the Lion Man. During recent excavations in the Stadel Cave between 2008 and 2013, a stratigraphic sequence was discovered that extended from the Middle Palaeolithic to the Aurignacian. It became clear that the location of the Lion Man during the excavations of 1939 corresponded to layer Au of the recent 2008-2013 excavations part of the excavation back dirt fro
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Reports on the topic "Mammoth Cave"

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Remensnyder, Katie, Elaine Robinson, Katie Beck, Sarah Reyes, John Rasmussen, and William Hunter. Mammoth Cave National Park Historic Resource Study. National Park Service, 2023. https://doi.org/10.36967/2309606.

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In 2022 the National Park Service (NPS) contracted Commonwealth to conduct an HRS of Mammoth Cave National Park. Funding for the project was provided by the NPS Cultural Resources, Partnerships, and Science Cultural Resources Fund Source. This HRS, the second conducted for the cultural resources in the Park, accounts for changes to the Park’s built environment since the original HRS, incorporates additional research, and reanalyzes and reevaluates resources documented in the first HRS. Of the 290 surveyed cultural resources, 57 have been previously listed in the NRHP either as individual listi
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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, 2021. http://dx.doi.org/10.36967/nrr-2286525.

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Toomey, Rickard, Vincent Santucci, Justin Tweet, Vincent Santucci, Rickard Toomey, and Justin Tweet. Mammoth Cave National Park: Paleontological resource inventory (sensitive version). National Park Service, 2024. http://dx.doi.org/10.36967/2306041.

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Mammoth Cave National Park (MACA) in south-central Kentucky protects one of the most famous and extensive cave systems in the world. Fossils, both in the bedrock of the cave system and as much more recent remains that date to the cave era, have been reported since at least the first half of the 19th century, but have rarely been a focus of investigation. In 2019, following a report of shark fossils in the wall of a cave passage, a team of MACA staff and volunteers, members of the National Park Service (NPS) Paleontology Program, and paleontological specialists from outside the NPS began a pale
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Toomey, Rickard, Vincent Santucci, Justin Tweet, Vincent Santucci, Rickard Toomey, and Justin Tweet. Mammoth Cave National Park: Paleontological resource inventory (public version). National Park Service, 2025. https://doi.org/10.36967/2308457.

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Mammoth Cave National Park (MACA) in south-central Kentucky protects one of the most famous and extensive cave systems in the world. Fossils, both in the bedrock of the cave system and as much more recent remains that date to the cave era, have been reported since at least the first half of the 19th century, but have rarely been a focus of investigation. In 2019, following a report of shark fossils in the wall of a cave passage, a team of MACA staff and volunteers, members of the National Park Service (NPS) Paleontology Program, and paleontological specialists from outside the NPS began a pale
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5

Herring, Theodore, Justin Tweet, and Vincent Santucci. Wind Cave National Park: Paleontological resource inventory (public version). National Park Service, 2023. http://dx.doi.org/10.36967/2299620.

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Wind Cave National Park (WICA), the first cave in the world to become a national park, is famous for the park’s namesake feature. Wind Cave, named for the noticeable wind-flow patterns observed as air moves in and out of the natural cave entrance, is currently the third longest cave system in the United States and seventh longest in the world. Wind Cave formed when groundwater dissolved buried layers of the fossiliferous Madison Limestone, which were deposited during the Mississippian subperiod approximately 359 to 347 million years ago. In addition to the Madison Limestone, several other form
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6

Henderson, Tim, Vincent Santucci, Tim Connors, and Justin Tweet. National Park Service geologic type section inventory: Southern Plains Inventory & Monitoring Network. National Park Service, 2022. http://dx.doi.org/10.36967/nrr-2293756.

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Type sections are one of several kinds of stratotypes. A stratotype is the standard (original or subsequently designated), accessible, and specific sequence of rock for a named geologic unit that forms the basis for the definition, recognition, and comparison of that unit elsewhere. Geologists designate stratotypes for rock exposures that are illustrative and representative of the map unit being defined. Stratotypes ideally should remain accessible for examination and study by others. In this sense, geologic stratotypes are similar in concept to biological type specimens, however, they remain
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