Speleology

@article{crossref1866mammoth,
    title = "Mammoth cave of Kentucky",
    year = "1866",
    journal = "Notes and Queries",
    url = "https://doi.org/10.1093/nq/s3-ix.212.61b",
    doi = "10.1093/nq/s3-ix.212.61b",
    number = "212",
    pages = "61-61",
    volume = "s3-IX"
}

@article{vestal1870the,
    author = "VESTAL, TILGHMAN B.",
    title = "The Mammoth Cave and the Cave Regions of Kentucky",
    year = "1870",
    journal = "Scientific American",
    url = "https://doi.org/10.1038/scientificamerican06251870-412",
    doi = "10.1038/scientificamerican06251870-412",
    number = "26",
    pages = "412-413",
    volume = "22"
}

@article{stevens1882the,
    author = "Stevens, W. LeConte",
    title = "The Mammoth Cave of Kentucky",
    year = "1882",
    journal = "Science",
    url = "https://doi.org/10.1126/science.os-3.80.3",
    doi = "10.1126/science.os-3.80.3",
    number = "80",
    pages = "3-6",
    volume = "os-3"
}

@article{hovey1891mammoth,
    author = "Hovey, Horace C.",
    title = "Mammoth Cave, Kentucky",
    year = "1891",
    journal = "Journal of the American Geographical Society of New York",
    url = "https://doi.org/10.2307/196576",
    doi = "10.2307/196576",
    pages = "47",
    volume = "23"
}

@misc{fisher1934growth1,
    author = "Fisher, L. W",
    title = "Growth of stalactites",
    year = "1934",
    howpublished = "American Mineralogist, v. 19, p. 429-431",
    note = "talkorigins\_source = {true}; raw\_reference = {Fisher, L. W., 1934, Growth of stalactites: American Mineralogist, v. 19, p. 429-431.}"
}

@article{jones1965algological,
    author = "Jones, H.",
    title = "Algological investigations in Mammoth Cave, Kentucky",
    year = "1965",
    journal = "International Journal of Speleology",
    url = "https://doi.org/10.5038/1827-806x.1.4.6",
    doi = "10.5038/1827-806x.1.4.6",
    number = "4",
    pages = "491-516",
    volume = "1"
}

@article{vanlandingham1965diatoms,
    author = "Van Landingham, Sam",
    title = "Diatoms from Mammoth Cave, Kentucky",
    year = "1965",
    journal = "International Journal of Speleology",
    url = "https://doi.org/10.5038/1827-806x.1.4.7",
    doi = "10.5038/1827-806x.1.4.7",
    number = "4",
    pages = "517-539",
    volume = "1"
}

Clastic sediment deposits found within the caves of Mammoth Cave National Park have yielded a magnetostratigraphic pattern of magnetic polarity reversals which indicates-that they were deposited over a range of at least 1 million and most likely 2 million years.

@article{schmidt1982magnetostratigraphy,
    author = "Schmidt, Victor A.",
    title = "Magnetostratigraphy of Sediments in Mammoth Cave, Kentucky",
    year = "1982",
    journal = "Science",
    abstract = "Clastic sediment deposits found within the caves of Mammoth Cave National Park have yielded a magnetostratigraphic pattern of magnetic polarity reversals which indicates-that they were deposited over a range of at least 1 million and most likely 2 million years.",
    url = "https://doi.org/10.1126/science.217.4562.827",
    doi = "10.1126/science.217.4562.827",
    number = "4562",
    pages = "827-829",
    volume = "217"
}

@misc{schmidt1982magnetostratigraphy2,
    author = "Schmidt, V. A",
    title = "Magnetostratigraphy of sediments in Mammoth Cave, Kentucky",
    year = "1982",
    howpublished = "Science, v. 217, p. 827-829",
    note = "talkorigins\_source = {true}; raw\_reference = {Schmidt, V. A., 1982, Magnetostratigraphy of sediments in Mammoth Cave, Kentucky: Science, v. 217, p. 827-829.}"
}

@incollection{brucker2012mammoth,
    author = "Brucker, Roger W.",
    title = "Mammoth Cave System, Kentucky",
    year = "2012",
    booktitle = "Encyclopedia of Caves",
    url = "https://doi.org/10.1016/b978-0-12-383832-2.00067-0",
    doi = "10.1016/b978-0-12-383832-2.00067-0",
    pages = "469-474"
}

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 a World Heritage Site and an International Biosphere Reserve (UNESCO). Its many passage levels and sediments contain a record of the fluvial history of most of southeastern North America.

@article{palmer2016the,
    author = "Palmer, A. N.",
    title = "The Mammoth Cave system, Kentucky, USA",
    year = "2016",
    journal = "Boletín Geológico y Minero",
    abstract = "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 a World Heritage Site and an International Biosphere Reserve (UNESCO). Its many passage levels and sediments contain a record of the fluvial history of most of southeastern North America.",
    url = "https://doi.org/10.21701/bolgeomin.127.1.009",
    doi = "10.21701/bolgeomin.127.1.009",
    number = "1",
    pages = "131-145",
    volume = "127"
}

@incollection{brucker2019mammoth,
    author = "Brucker, Roger W.",
    title = "Mammoth Cave System, Kentucky",
    year = "2019",
    booktitle = "Encyclopedia of Caves",
    url = "https://doi.org/10.1016/b978-0-12-814124-3.00080-7",
    doi = "10.1016/b978-0-12-814124-3.00080-7",
    pages = "669-677"
}