@misc{davis1902river2,
    author = "Davis, W. M",
    title = "River Terraces in New England, in Davis, W. M., ed., Geographical Essays",
    year = "1902",
    howpublished = "Boston, Ginn and Co., p. 514-586",
    note = "talkorigins\_source = {true}; raw\_reference = {Davis, W. M., 1902, River Terraces in New England, in Davis, W. M., ed., Geographical Essays: Boston, Ginn and Co., p. 514-586.}"
}

@misc{davis1909geographical3,
    author = "Davis, W. M",
    title = "Geographical Essays",
    year = "1909",
    howpublished = "Boston, Ginn and Co., 777 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Davis, W. M., 1909, Geographical Essays: Boston, Ginn and Co., 777 p.}"
}

@article{dodge1910geographical,
    author = "Dodge, R. E. and Davis, William Morris and Johnson, Douglas Wilson",
    title = "Geographical Essays",
    year = "1910",
    journal = "Bulletin of the American Geographical Society",
    url = "https://doi.org/10.2307/199164",
    doi = "10.2307/199164",
    number = "4",
    openalex = "W4233739514",
    pages = "300",
    volume = "42"
}

@misc{keilhack1920die5,
    author = "Keilhack, W",
    title = "Die Staumorane bei Guben",
    year = "1920",
    howpublished = "Berlin, Jahrb. Pruess. Geolog. Landesanst",
    note = "talkorigins\_source = {true}; raw\_reference = {Keilhack, W., 1920, Die Staumorane bei Guben: Berlin, Jahrb. Pruess. Geolog. Landesanst.}"
}

@misc{otto1924studien9,
    author = "Otto, A",
    title = "Studien zur Morfologie des Neisstales zwischen Zittau und Gorlitz, 29 of Abhandlungen der Naturforschenden Gesellschaft zu Gorlitz",
    year = "1924",
    howpublished = "Berlin, H.K. Gorlitz, 687 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Otto, A., 1924, Studien zur Morfologie des Neisstales zwischen Zittau und Gorlitz, 29 of Abhandlungen der Naturforschenden Gesellschaft zu Gorlitz: Berlin, H.K. Gorlitz, 687 p.}"
}

@article{mahard1942the7,
    author = "Mahard, R. H",
    title = "The origin and significance of intrenched [sic] meanders",
    year = "1942",
    journal = "Journal of Geomorphology, v. 5, p. 32-44",
    note = "talkorigins\_source = {true}; raw\_reference = {Mahard, R. H., 1942, The origin and significance of intrenched [sic] meanders: Journal of Geomorphology, v. 5, p. 32-44.}"
}

@article{f1947geographical,
    author = "F., W. and Cornish, Vaughan",
    title = "Geographical Essays",
    year = "1947",
    journal = "The Geographical Journal",
    url = "https://doi.org/10.2307/1789931",
    doi = "10.2307/1789931",
    number = "1/3",
    openalex = "W4241084392",
    pages = "133",
    volume = "109"
}

@misc{krygowski1948morfologia6,
    author = "Krygowski, B",
    title = "Morfologia dorzecza Odry",
    year = "1948",
    howpublished = "Poznan, Instytut Zachodni",
    note = "talkorigins\_source = {true}; raw\_reference = {Krygowski, B., 1948, Morfologia dorzecza Odry: Poznan, Instytut Zachodni.}"
}

@article{crossref1954geographical,
    title = "Geographical essays",
    year = "1954",
    journal = "Journal of the Franklin Institute",
    url = "https://doi.org/10.1016/0016-0032(54)90052-6",
    doi = "10.1016/0016-0032(54)90052-6",
    number = "6",
    openalex = "W4233265393",
    pages = "534",
    volume = "258"
}

@article{doi103133pp347,
    author = "Hack, John T. and Goodlett, John C.",
    title = "Geomorphology and forest ecology of a mountain region in the central Appalachians",
    year = "1960",
    journal = "USGS professional paper",
    abstract = "Relation of asymmetry to moisture conditions and Bedrock geology \_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_ \_ 2 the processes of erosion \_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_ \_ Topography \_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_ \_ 5 Erosion and deposition in the flood of June 1949 \_\_\_\_\_\_\_ \_ Topographic forms of first-order mountain valleys \_\_ 5 Description of the flood \_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_\_ \_ Slope profiles",
    url = "https://doi.org/10.3133/pp347",
    doi = "10.3133/pp347",
    openalex = "W176828818",
    references = "doi101029tr035i006p00951, doi1010970001069419381100000011, doi101126science892320559, doi10113000167606194556275edosat20co2, doi101130001676061949601315botp20co2, doi10113000167606195263923dbog20co2, doi10113000167606195667571qsa20co2, doi1023071791828, doi105962bhltitle56969, openalexw1996657273"
}

@article{carlston1965the1,
    author = "Carlston, C. W",
    title = "The relation of free meander geometry to stream discharge and its geomorphic implications",
    year = "1965",
    journal = "American Journal of Science, v. 263, p. 864-885",
    note = "talkorigins\_source = {true}; raw\_reference = {Carlston, C. W., 1965, The relation of free meander geometry to stream discharge and its geomorphic implications: American Journal of Science, v. 263, p. 864-885.}"
}

@article{clayton1966essays,
    author = "Clayton, Keith M. and Dury, G. H.",
    title = "Essays in Geomorphology",
    year = "1966",
    journal = "The Geographical Journal",
    url = "https://doi.org/10.2307/1792584",
    doi = "10.2307/1792584",
    number = "4",
    openalex = "W2040930588",
    pages = "555",
    volume = "132"
}

@article{birkenmajer1968essays,
    author = "Birkenmajer, Krzysztof",
    title = "Essays in geomorphology",
    year = "1968",
    journal = "Palaeogeography, Palaeoclimatology, Palaeoecology",
    url = "https://doi.org/10.1016/0031-0182(68)90051-5",
    doi = "10.1016/0031-0182(68)90051-5",
    number = "3",
    openalex = "W215552957",
    pages = "227-229",
    volume = "4"
}

@misc{moore1968speleothems8,
    author = "Moore, G. W",
    title = "Speleothems, in Fairbridge, R. W., ed., Encyclopedia of Geomorphology",
    year = "1968",
    howpublished = "New York, Reinhold Book Co., p. 1040-1041; 1295 pp",
    note = "talkorigins\_source = {true}; raw\_reference = {Moore, G. W., 1968, Speleothems, in Fairbridge, R. W., ed., Encyclopedia of Geomorphology: New York, Reinhold Book Co., p. 1040-1041; 1295 pp.}"
}

@phdthesis{garner1974the4,
    author = "Garner, H. F",
    title = "The Origin of Landscapes",
    year = "1974",
    publisher = "Synthesis of Geomorphology: New York, Oxford University Press, 734 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Garner, H. F., 1974, The Origin of Landscapes: Synthesis of Geomorphology: New York, Oxford University Press, 734 p.}"
}

@misc{smart1979determinism10,
    author = "Smart, J. S",
    title = "Determinism and randomness in fluvial geomorphology",
    year = "1979",
    howpublished = "Eos, v. 60, no. 36, p. 651-655",
    note = "talkorigins\_source = {true}; raw\_reference = {Smart, J. S., 1979, Determinism and randomness in fluvial geomorphology: Eos, v. 60, no. 36, p. 651-655.}"
}

@incollection{bianchi2006origin,
    author = "Bianchi, Thomas S.",
    title = "Origin and Geomorphology",
    year = "2006",
    booktitle = "Biogeochemistry of Estuaries",
    abstract = "Geologically speaking, estuaries are ephemeral features of the coasts. Upon formation, most begin to fill in with sediments and, in the absence of sea level changes, would have life spans of only a few thousand to tens of thousands of years (Emery and Uchupi, 1972; Schubel, 1972; Schubel and Hirschberg, 1978). Estuaries have been part of the geologic record for at least the past 200 million years (My) BP (before present; Williams, 1960; Clauzon, 1973). However, modern estuaries are recent features that only formed over the past 5000 to 6000 years during the stable interglacial period of the middle to late Holocene epoch (0–10,000 y BP), which followed an extensive rise in sea level at the end of the Pleistocene epoch (1.8 My to 10,000 y BP; Nichols and Biggs, 1985). There is general agreement that four major glaciation to interglacial periods occurred during the Pleistocene. It has been suggested that sea level was reduced from a maximum of about 80 m above sea level during the Aftoninan interglacial to 100 m below sea level during the Wisconsin, some 15,000 to 18,000 y BP (figure 2.1; Fairbridge, 1961). This lowest sea level phase is referred to as low stand and is usually determined by uncovering the oldest drowned shorelines along continental margins (Davis, 1985, 1996); conversely, the highest sea level phase is referred to as high stand. It is generally accepted that low-stand depth is between 130 and 150 m below present sea level and that sea level rose at a fairly constant rate until about 6000 to 7000 y BP (Belknap and Kraft, 1977). A sea level rise of approximately 10 mm y−1 during this period resulted in many coastal plains being inundated with water and a displacement of the shoreline. The phenomenon of rising (transgression) and falling (regression) sea level over time is referred to as eustacy (Suess, 1906). When examining a simplified sea level curve, we find that the rate of change during the Holocene is fairly representative of the Gulf of Mexico and much of the U.S. Atlantic coastline (Curray, 1965).",
    url = "https://doi.org/10.1093/oso/9780195160826.003.0008",
    doi = "10.1093/oso/9780195160826.003.0008",
    openalex = "W3103478702"
}