Relevant bibliographies by topics / River alluvium

Contents

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

Academic literature on the topic 'River alluvium'

Author: Grafiati
Published: 3 June 2025
Last updated: 1 August 2025

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Journal articles on the topic "River alluvium"

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Heritage, G., S. Tooth, N. Entwistle, and D. Milan. "Long-term flood controls on semi-arid river form: evidence from the Sabie and Olifants rivers, eastern South Africa." Proceedings of the International Association of Hydrological Sciences 367 (March 3, 2015): 141–46. http://dx.doi.org/10.5194/piahs-367-141-2015.

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Abstract. Rivers in the Kruger National Park, eastern South Africa, are characterised by bedrock-influenced "macrochannels" containing variable alluvial thicknesses and riparian vegetation assemblages. Evidence from the Sabie and Olifants rivers suggests that flows up to moderate floods (<3500 m3 s−1) tend to result in net alluviation, with sediments gradually covering the underlying bedrock. More extreme floods strip alluvium and erode bedrock, effectively exerting the primary control over long-term river morphologic development. On the Olifants River, post-flood aerial LIDAR imagery revea
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Mishra, M. N., R. N. Shrivastava, M. C. Upadhyaya, and M. P. Shrivastava. "Quaternary Geology and Morphotectonic Evolution of the Lower Sind Basin, Marginal Gangetic Plains, M.P. and U.P." Journal Geological Society of India 43, no. 6 (1994): 677–84. http://dx.doi.org/10.17491/jgsi/1994/430606.

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Abstract The lower reaches of the Sind River, a tributory of the Yamuna, exhibits a thick accumulation of Quaternary alluvium deposited by the ancient river system of the Ganga and the present Sind River. The alluvial sequence comprises the Older Alluvium and the Younger Alluvium which are divisible into three lithostratigraphic units, viz., the Gohad-Mau-Mihona Formation, the Bera (Sijroli) Formation, and the Sind Formation. Six geomorphic units, namely, the Denudational Hill, the Jaswantnagar Surface, the Gohad-Mau-Mihona Surface, the Bera (Sijroli) Surface, the Sind Surface, and the Ravinou
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Yatsyshyn, Andriy, and Andriy Bogucki. "Lithological characteristic of the riverbed alluvium of the sixth terrace of the Dnister–Stryvihor in the Dubrivka section (Forecarpathians)." Visnyk of the Lviv University. Series Geography, no. 49 (December 30, 2015): 348–63. http://dx.doi.org/10.30970/vgg.2015.49.8656.

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The main lithological characteristics of riverbed facies of alluvium of the sixth terrace above the floodplain of the Dnister-Stryvihor Rivers (Loyeva level) near Sambir were analysed. The granulometric and petrographic composition of the gravelly-pebble material, its roundness, form and the orientation of grains were characterised. Lithological analyses helped to determine that investigated layer of alluvium are poorly sorted. The three main components of alluvial strata (pebbles, gravel and sand-loamy filler) are present in approximately comparable proportions. Boulders are least common in t
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Yatsyshyn, Andriy, Andriy Bogucki, Danuta Olszewska-Nejbert, and Maciej Bąbel. "Palaeogeographical conditions of the formation of the channel alluvium of the high (Susidovychi) terrace of the Dnister River in the Kulakivtsi section (Podillia-Dnister region)." Visnyk of the Lviv University. Series Geography, no. 52 (June 27, 2018): 303–23. http://dx.doi.org/10.30970/vgg.2018.52.10196.

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The main lithological characteristics of the channel facies of the Susidovychi terrace, which correspond to the high (situated over the canyon) groups of Dnister terraces, were given. The investigations in the gravel pit at Kulakivtsi proved that the alluvium of the terrace has been formed in two stages. During the first stage, the lower 1.5 thick bed of the alluvium was deposited. The upper one, nearly 4 m thick alluvium bed was formed in the next, second one depositional stage. The stages of the alluvium formation were recorded in the changes of the granulometric and petrographical compositi
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Nordt, Lee. "Late quaternary alluvial stratigraphy of a low-order tributary in central texas, USA and its response to climate and sediment supply." Quaternary Research 62, no. 3 (2004): 289–300. http://dx.doi.org/10.1016/j.yqres.2004.07.004.

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This paper presents the first comprehensive late Quaternary alluvial stratigraphic study of a low-order tributary in central Texas, using Cowhouse Creek as a case study. The late Pleistocene Jackson (JA) alluvium forms the elevated T2 terrace. The entrenched Holocene valley is filled with the buried Georgetown (GT) alluvium (approximately 11,000 to 8000 14C yr B.P.) and associated Royalty paleosol, and the surficially exposed Fort Hood (FH) alluvium (approximately 7000 to 5000 14C yr B.P.) and West Range (WR) alluvium (approximately 4200 to 600 14C yr B.P.) forming the broad T1 terrace. The Fo
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Zhang, L., G. Parker, C. P. Stark, et al. "Macro-roughness model of bedrock–alluvial river morphodynamics." Earth Surface Dynamics 3, no. 1 (2015): 113–38. http://dx.doi.org/10.5194/esurf-3-113-2015.

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Abstract. The 1-D saltation–abrasion model of channel bedrock incision of Sklar and Dietrich (2004), in which the erosion rate is buffered by the surface area fraction of bedrock covered by alluvium, was a major advance over models that treat river erosion as a function of bed slope and drainage area. Their model is, however, limited because it calculates bed cover in terms of bedload sediment supply rather than local bedload transport. It implicitly assumes that as sediment supply from upstream changes, the transport rate adjusts instantaneously everywhere downstream to match. This assumption
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Zhang, L., G. Parker, C. P. Stark, et al. "Macro-roughness model of bedrock-alluvial river morphodynamics." Earth Surface Dynamics Discussions 2, no. 1 (2014): 297–355. http://dx.doi.org/10.5194/esurfd-2-297-2014.

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Abstract. The 1-D saltation-abrasion model of channel bedrock incision of Sklar and Dietrich, in which the erosion rate is buffered by the surface area fraction of bedrock covered by alluvium, was a major advance over models that treat river erosion as a function of bed slope and drainage area. Their model is, however, limited because it calculates bed cover in terms of bedload sediment supply rather than local bedload transport. It implicitly assumes that as sediment supply from upstream changes, the transport rate adjusts instantaneously everywhere downstream to match. This assumption is not
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Fuladi, A., and M. S. Deshmukh. "Geomorphic Characteristics of WRC-1 Watershed, Chargarh River Basin, Central India: Possible Implications on Hydrogeological Status." Journal of Scientific Research 15, no. 3 (2023): 607–19. http://dx.doi.org/10.3329/jsr.v15i3.63239.

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Every geomorphic feature has its own distinct impact on the static groundwater level(SWL), seasonal water table fluctuation(WTF) and yield of the wells. The aim of this study was to analyze the role of geomorphic features over the groundwater regime and its possible implications on hydrogeological status within WRC-1 watershed. The watershed is covered by the Deccan basalt lavaflows and Quaternary alluvium. The geomorphic units of study area are HDP, MDP, residual hill, valleyfills, scarp, pediment, pediplain, butte, alluvial plain and gullied land to identify the relationship between geomorph
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McMahon, William J., and Neil S. Davies. "Physical and biological functioning in Proterozoic rivers: evidence from the archetypal pre-vegetation alluvium of the Torridon Group, NW Scotland." Scottish Journal of Geology 56, no. 1 (2019): 1–29. http://dx.doi.org/10.1144/sjg2019-013.

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In modern rivers, vegetation affects hydrological, geomorphological and sedimentological functioning, so extant fluvial systems can provide only partial analogues for those rivers that operated before the evolution of land plants. However, pre-vegetation rivers were the norm for the first 90% of Earth's history and so a better understanding of their sedimentary product can provide insights into both the fundamental underlying mechanisms of river behaviour and the ways in which fluvial processes operated on ancient Earth. In addition to a short review of the history of research into pre-vegetat
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Heizler, Matthew T., Karl E. Karlstrom, Micael Albonico, et al. "Detrital sanidine 40Ar/39Ar dating confirms <2 Ma age of Crooked Ridge paleoriver and subsequent deep denudation of the southwestern Colorado Plateau." Geosphere 17, no. 2 (2021): 438–54. http://dx.doi.org/10.1130/ges02319.1.

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Abstract Crooked Ridge and White Mesa in northeastern Arizona (southwestern United States) preserve, as inverted topography, a 57-km-long abandoned alluvial system near the present drainage divide between the Colorado, San Juan, and Little Colorado Rivers. The pathway of this paleoriver, flowing southwest toward eastern Grand Canyon, has led to provocative alternative models for its potential importance in carving Grand Canyon. The ∼50-m-thick White Mesa alluvium is the only datable record of this paleoriver system. We present new 40Ar/39Ar sanidine dating that confirms a ca. 2 Ma maximum depo
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Dissertations / Theses on the topic "River alluvium"

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Gouw, Marc Jean Pierre. "Alluvial architecture of the Holocene Rhine-Meuse delta (The Netherlands) and the Lower Mississippi Valley (U.S.A.) /." Utrecht : Koninklijk Nederlands Aardrijkskundig Genootschap [u.a.], 2007. http://www.loc.gov/catdir/toc/fy0803/2008400359.html.

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Roseff, Rebecca. "A study of alluviation in the River Lugg catchment, Herefordshire." Thesis, University of Birmingham, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.343888.

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Gouw, Marc. "Alluvial architecture of the Holocene Rhine-Meuse delta (the Netherlands) and the Lower Mississippi Valley (U.S.A.) /." Utrecht : Koninklijk Nederlands Aardrijkskundig Genootschap, Faculteit Geowetenschappen Universiteit Utrecht, 2007. http://www.loc.gov/catdir/toc/fy0803/2008400359.html.

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Davies, Paul. "Sub-fossil mollusca from Holocene overbank alluvium and other wet-ground contexts in Wessex." Thesis, Cardiff University, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.281700.

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Jones, Heather L. "Characterizing ancient avulsion stratigraphy and its significance." Laramie, Wyo. : University of Wyoming, 2007. http://proquest.umi.com/pqdweb?did=1338875291&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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McMahon, William. "Pre-vegetation alluvium : geological evidence for river behaviour in the absence of land plants." Thesis, University of Cambridge, 2018. https://www.repository.cam.ac.uk/handle/1810/276277.

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Pre-vegetation alluvium is unique; at the present day, plants affect multiple aspects of river functioning and deposition and so those rivers that operated before the evolution of land plants largely lack modern sedimentological analogue. However, such rivers were the norm for the first 90% of Earth history and so a better understanding of their sedimentary product enables insight into both the fundamental underlying mechanisms of river behaviour and the ways in which fluvial processes operated on ancient Earth and other rocky planets. This study presents five original fieldwork based case stu
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Santucci, Jay N. "Hydrogeologic conditions controlling contaminant migration from storage tanks overlying Mississippi River Alluvium a case study /." Master's thesis, Mississippi State : Mississippi State University, 2006. http://library.msstate.edu/etd/show.asp?etd=etd-07072006-161425.

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Rutland, Jeffrey R. "Depositional environments comprising the Birch River section (Middle Pennsylvanian), Powell Mountain, Nicholas County, West Virginia." Morgantown, W. Va. : [West Virginia University Libraries], 2004. https://etd.wvu.edu/etd/controller.jsp?moduleName=documentdata&jsp%5FetdId=3461.

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Thesis (M.S.)--West Virginia University, 2004.<br>Title from document title page. Document formatted into pages; contains vii, 198 p. : ill. (some col.), maps. Includes abstract. Includes bibliographical references (p. 161-167).
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Tainer, Erin Margaret. "High-Resolution Holocene Alluvial Chronostratigraphy at Archaeological Sites in Eastern Grand Canyon, Arizona." DigitalCommons@USU, 2010. https://digitalcommons.usu.edu/etd/551.

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Understanding the nature of Colorado River deposits in Grand Canyon helps reveal how the river responds to changes in its Colorado Plateau tributaries and Rocky Mountain headwaters. This study focused on Holocene alluvial deposits associated with archaeological sites excavated near Ninemile Draw in Glen Canyon and at Tanner Bar in eastern Grand Canyon. Two previously-developed conceptual models of deposition were tested based on previous work. Previous researchers have suggested that Holocene alluvial deposits in Grand Canyon are a series of inset aggradational packages that correlate to va
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Moura, Idembergue Barroso Macedo de. "Estudos das Ãguas da bacia hidrogrÃfica do rio Banabuià no trecho entre Quixeramobim e Banabuià - CearÃ, Brasil." Universidade Federal do CearÃ, 2013. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=9971.

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Conselho Nacional de Desenvolvimento CientÃfico e TecnolÃgico<br>A Ãrea deste estudo de hidrogeologia abrange a Bacia do BanabuiÃ, trecho entre Quixeramobim e BanabuiÃ, e està localizada Ãs margens dos rios Quixeramobim e BanabuiÃ. à necessÃrio para os usuÃrios e gestores conhecer os aspectos qualitativos e quantitativos das Ãguas usadas e a interaÃÃo entre as Ãguas dos rios Quixeramobim e Banabuià com os aquÃferos aluvionares. O objetivo deste estudo foi aprofundar os conhecimentos sobre a hidrogeologia dos aluviÃes em relaÃÃo Ãs reservas, qualidade e hidrodinÃmica das Ãguas. Para isto, reali
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Books on the topic "River alluvium"

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International Conference on Fluvial Sedimentology (6th 1997 Cape Town, South Africa). Fluvial aspects of the Ordovician table mountain group: Slack-water deposits of the 1981 Buffels River flood, Laingsburg : alluvial fan enon formation (cretaceous), Oudtshoorn : post-conference field excursion, 6th International Conference on Fluvial Sedimentology, University of Cape Town, South Africa, 27 September to 1 October 1997. The Conference, 1997.

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Fitch, K. C. (Kevin Christopher), Ladd David E, Geological Survey (U.S.), and United States. National Park Service, eds. Alluvial bars of the Obed Wild and Scenic River. U.S. Dept. of the Interior, U.S. Geological Survey, 2007.

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Glanville, Warren Peter. Holocene river behaviour and environmental change in the upper River Liffey catchment, Co. Wicklow, Ireland. University College Dublin, 1999.

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Hereford, Richard. Geomorphic history of the Virgin River in the Zion National Park area, southwest Utah. U.S. Dept. of the Interior, U.S. Geological Survey, 1995.

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Tomasz, Falkowski. Naturalne czynniki stabilizujące wybrane odcinki strefy korytowej Wisły środkowej. Wydawnictwo SGGW, 2006.

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N, Jennings J., and Bremer Hanna, eds. Fluvial geomorphology: In memoriam J.N. Jennings. Gebr. Borntraeger, 1985.

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Barnett, Adrienne. Assessment of the alluvial sediments in the Big Thompson River Valley, Colorado. U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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C, Schmidt John. Aggradation and degradation of alluvial sand deposits, 1965 to 1986, Colorado River, Grand Canyon National Park, Arizona. U.S. G.P.O., 1990.

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C, Schmidt John. Aggradation and degradation of alluvial sand deposits, 1965 to 1986, Colorado River, Grand Canyon National Park, Arizona. Dept. of the Interior, U.S. Geological Survey, 1988.

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C, Schmidt John. Aggradation and degradation of alluvial sand deposits, 1965 to 1986, Colorado River, Grand Canyon National Park, Arizona: Executive summary. Dept. of the Interior, U.S. Geological Survey, 1988.

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Book chapters on the topic "River alluvium"

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Wang, Zhao-Yin, Joseph H. W. Lee, and Charles S. Melching. "Sediment Movement in Alluvial Rivers." In River Dynamics and Integrated River Management. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-25652-3_6.

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Richards, Keith. "Alluvial river channels: their nature and significance." In Rivers. Routledge, 2024. http://dx.doi.org/10.4324/9781003465799-1.

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Shukla, Shradha, Jayshree Meshram, Chhaya Minz, Hemraj Suryavanshi, and Shubrasuchi Sarkar. "Quaternary Climate of Narmada Valley: A Case Study on Understanding Provenance, Weathering and Depositional Environment Using Alluvium Geochemistry from Tawa River Basin, Hoshangabad District, Madhya Pradesh." In Society of Earth Scientists Series. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-13119-6_7.

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Hodge, Rebecca A. "Sediment Processes in Bedrock-Alluvial Rivers." In Gravel-Bed Rivers. John Wiley & Sons, Ltd, 2017. http://dx.doi.org/10.1002/9781118971437.ch24.

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Bardhan, Mayuraksha. "A Study on Some Characteristics of an Alluvial Channel for Varying Flows." In River and Coastal Engineering. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-05057-2_2.

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Fedele, Juan J., and Marcelo H. García. "Alluvial Roughness in Streams with Dunes: A Boundary-Layer Approach." In River, Coastal and Estuarine Morphodynamics. Springer Berlin Heidelberg, 2001. http://dx.doi.org/10.1007/978-3-662-04571-8_3.

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Turowski, Jens M. "Semi-Alluvial Channels and Sediment-Flux-Driven Bedrock Erosion." In Gravel-Bed Rivers. John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781119952497.ch29.

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Krebs, L., J. Corbonnois, and S. Muller. "The impact of hydrological fluctuations on shallow groundwater hydrochemistry under two alluvial meadows." In Man and River Systems. Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-017-2163-9_21.

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Dhakal, Deepak, Nayan Sharma, and Ashish Pandey. "Review of Flow Simulation Methods in Alluvial River." In Water Science and Technology Library. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-59148-9_21.

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Pérez, José Miguel Sánchez, Michèle Trémolières, Naima Takatert, Philippe Ackerer, Arianne Eichhorn, and Gérard Maire. "Quantification of nitrate removal by a flooded alluvial zone in the Ill floodplain (Eastern France)." In Man and River Systems. Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-017-2163-9_20.

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Conference papers on the topic "River alluvium"

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Singla, Deepak, and Rajiv Ahuja. "Case Histories of Well Foundations in India-Design and Construction Challenges." In IABSE Symposium, Tokyo 2025: Environmentally Friendly Technologies and Structures: Focusing on Sustainable Approaches. International Association for Bridge and Structural Engineering (IABSE), 2025. https://doi.org/10.2749/tokyo.2025.0603.

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&lt;p&gt;Most of the large rivers in India have alluvium silty sand beds which are erodible during high floods. Well foundations are the most common type of foundations in these rivers constructed with an age- old practice of sinking through such strata. Where the flow depth is large, floating caissons are fabricated and towed to the location. During the sinking process, various indigenous techniques developed over the years are adopted including grabbing the soil from inside the dredge hole, application of kentledge on top of the well, water jetting, cutting below the base if hard strata are
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Basu, Subrata, Amitabha Ghoshal, and Alok Bhowmick. "Caisson Foundations for two Bridges across river Hooghly at Kolkata." In IABSE Symposium, Tokyo 2025: Environmentally Friendly Technologies and Structures: Focusing on Sustainable Approaches. International Association for Bridge and Structural Engineering (IABSE), 2025. https://doi.org/10.2749/tokyo.2025.0585.

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&lt;p&gt;Kolkata is separated from its twin city Howrah by the river Hooghly, which has a bed of silt clay, and, fine sand up to large depths, typical of alluvial deposits. The high demand for cross-river traffic prompted the building of two bridges, with the earlier one a balanced cantilever with suspended span, with a load under the main pier of 30000 tons, and the second one, a cable-supported span with a tower load of 10000 tons. A single monolith of size 55 m x 25 m with 21 chambers, with steel cutting edges under all walls, and provision for airtight diaphragms on the cap of all walls, was
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Brewer, Will, and Joe C. Yelderman. "CARBON IN THE BRAZOS RIVER ALLUVIUM AQUIFER." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289549.

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Dawson, Claudia, William Brewer, and Joe Yelderman. "GRAVEL PIT LAKES IN THE BRAZOS RIVER ALLUVIUM AQUIFER." In South-Central Section - 56th Annual Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022sc-373761.

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ЛОСКУТОВ Е, Е., С. НИКИФОРОВА З, И. ЖУРАВЛЕВ А, and И. ИВАНОВ А. "FORMATION OF PLACER GOLD CONTENT OF THE GONAM RIVER BASIN, YURSKY OBJECT (ALDAN-STANOVOY SHIELD)." In ГЕОЛОГИЯ И МИНЕРАЛЬНО-СЫРЬЕВЫЕ РЕСУРСЫ СЕВЕРО-ВОСТОКА РОССИИ 2024. Crossref, 2024. http://dx.doi.org/10.53954/9785604990100_145.

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The placer gold content of the Yursky creek (right tributary of the Gonam river) has been studied. It was revealed that the Cretaceous conglomerates and the producing layer of the alluvial placer are composed of pebbles and boulders of the same petrographic composition. The petrographic composition of pebbles and boulders is as follows: leucogranites, granite-gneisses, metagabbro, diafluorinated shales of sericite-chlorite-epidote-quartz composition and quartzites. Gold from alluvial deposits and conglomerates of the Cretaceous age also has the same typomorphic features and is represented main
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Freed, Madeline M., Madeline Freed, and Jennifer M. Elick. "COMPOSITIONAL ANALYSES OF CHRISTMAS 2020 FLOOD ALLUVIUM OF THE SUSQUEHANNA RIVER." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-370664.

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Noonan, Erin Preslee, and Joe C. Yelderman. "IDENTIFYING SALINITY SOURCES IN THE NORTHERN SEGMENT OF THE BRAZOS RIVER ALLUVIUM AQUIFER." In 52nd Annual GSA South-Central Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018sc-310216.

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Dawson, Claudia, Joe Yelderman, and Will Brewer. "GROUNDWATER/ SURFACE WATER INTERACTIONS: GRAVEL PIT LAKES IN THE BRAZOS RIVER ALLUVIUM AQUIFER." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-369719.

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Axtell, Paul J., and Andrew Z. Boeckmann. "Static and Dynamic Load Test Comparison for H-Piles in Missouri River Alluvium." In International Foundations Congress and Equipment Expo 2024. American Society of Civil Engineers, 2024. http://dx.doi.org/10.1061/9780784485408.013.

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Casteel, Wynne, Joe C. Yelderman, and Peter B. James. "USING MICROGRAVITY AND PASSIVE SEISMIC METHODS JOINTLY TO EXPLORE THE BRAZOS RIVER ALLUVIUM AQUIFER." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-332872.

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Reports on the topic "River alluvium"

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Kleeschulte, M. J. Water-quality data for the Missouri River and Missouri River alluvium near Weldon Spring, St. Charles County, Missouri, 1991--92. Office of Scientific and Technical Information (OSTI), 1993. http://dx.doi.org/10.2172/392791.

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Sprinkel, Douglas A. Geologic Map of the Duchesne 30' x 60' Quadrangle, Duchesne and Wasatch Counties, Utah. Utah Geological Survey, 2024. https://doi.org/10.34191/m-300dm.

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This geologic map of the Duchesne 30' x 60' quadrangle is the result of five years of new mapping aided by previous mapping. Approximately centered on the town of Duchesne, Utah, the Duchesne County seat, the quadrangle covers most of the western Uinta Basin. Tertiary rocks of the Green River, Uinta, and Duchesne River Formations dominate the bedrock units in the quadrangle. Members of the formations are recognized and mapped throughout the Duchesne quadrangle despite the coarsening of these members in the western half. In the northwestern corner of the map area, Cambrian and Mississippian thr
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Meredith, E., G. Abdo, T. Myse, R. Breitmeyer, and J. Rose. Hydrogeologic investigation of the Upper Gallatin River Corridor, Big Sky, Montana. Montana Bureau of Mines and Geology, 2025. https://doi.org/10.59691/ymsg4474.

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Keller, Stephen, and Alexander Marr. OF-22-08 Geologic Map of the Windsor Quadrangle, Larimer and Weld Counties, Colorado. Colorado Geological Survey, 2024. https://doi.org/10.58783/cgs.of2208.lfhf7370.

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The Windsor quadrangle, situated in the northern part of the Colorado Piedmont, features relatively low topographic relief with a 94-meter variance between its highest and lowest points. Notable elongated outcrop areas of weathered bedrock are observed along the dissected southwest side of the Cache la Poudre River valley. While fresh bedrock is mainly found in lower gravel pit faces in the Big Thompson River valley, unconsolidated Quaternary deposits cover most of the quadrangle with few natural exposures along river cut banks. The landscape is primarily characterized by a broad upland swath
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Marr, Alexander. OF-23-04 Geologic Map of the Milton Reservoir Quadrangle, Weld County, Colorado. Colorado Geological Survey, 2024. https://doi.org/10.58783/cgs.of2304.mcgn8961.

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The Milton Reservoir 7.5-minute quadrangle is located in Weld County within the northern part of the Colorado Piedmont. The subdued landscape consists of gentle sloping uplands and the shallow valley of Beebe Draw, a north-south trending alluvial paleovalley where the ancestral South Platte River once flowed. The dominant surficial sediments in the quadrangle are Upper Pleistocene to Holocene eolian deposits where the sandier units form longitudinal and parabolic dune landforms, and the fine clay to silt rich units occur in interdunal valleys. Multiple alluvial deposits of different ages are s
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Zeiler, K., M. Sutherland, and R. Breitmeyer. Groundwater model of the Upper Gallatin aquifer at Big Sky, Montana. Montana Bureau of Mines and Geology, 2025. https://doi.org/10.59691/fsfu2980.

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This report presents details on the complete construction and operation of the MODFLOW groundwater model of the alluvial aquifer in the Upper Gallatin River Corridor at Big Sky, MT. The report includes details on definition of model geometry, boundary conditions, assumptions, calibration, and sensitivity and uncertainty analysis. The report also presents model results for specific modeling scenarios applicable to the Upper Gallatin River Corridor project.
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Team, MSRAP, undefined, and undefined. Conservation Planning in the Mississippi River Alluvial Plain. The Nature Conservancy, 2003. http://dx.doi.org/10.3411/col.04062122.

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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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Gannon, J. M., Jason A. Vogelgesang, and Deborah J. Quade. Aquifer Characterization and Drought Assessment Rock River Alluvial Aquifer. Iowa Department of Natural Resources, 2014. http://dx.doi.org/10.17077/rep.006516.

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Gannon, J. Michael. Aquifer Characterization and Drought Assessment Floyd River Alluvial Aquifer. Iowa Department of Natural Resources, 2012. http://dx.doi.org/10.17077/rep.006507.

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