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1

Bullock, Michelle. "Holocene sediments and geological history, Woolley Lake, near Beachport, South Australia /." Adelaide : Thesis (B. Sc.(Hons)) -- University of Adelaide, Dept. of Geology and Geophysics, 1994. http://web4.library.adelaide.edu.au/theses/09SB/09sbb938.pdf.

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Webb, Robert H. "Late Holocene flooding on the Escalante River, south-central Utah." Diss., The University of Arizona, 1985. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1985_248_sip1_w.pdf&type=application/pdf.

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Huang, Guangqing. "Holocene record of storms in sediments of the Pearl River Estuary and vicinity /." Hong Kong : University of Hong Kong, 2000. http://sunzi.lib.hku.hk/hkuto/record.jsp?B21687808.

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Burbidge, Susan M. (Susan Margot) Carleton University Dissertation Earth Sciences. "Holocene environmental history of lake Winnipeg; thecamoebians and stable lead isotopes." Ottawa, 1997.

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Heine, Jan T. "Glacier advances at the Pleistocene/Holocene transition near Mount Rainier volcano, Cascade Range, USA /." Thesis, Connect to this title online; UW restricted, 1997. http://hdl.handle.net/1773/6748.

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Selby, Katherine. "Late Devensian and Holocene relative sea level changes on the Isle of Skye, Scotland." Thesis, Coventry University, 1997. http://curve.coventry.ac.uk/open/items/0e151cae-7151-0ae4-e4f3-99a45f12ce84/1.

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Five coastal sites have been studies on the Isle of Skye to investigate Late Devensian and Holocene relative sea level changes. In the field, detailed stratigraphical work, geomorphological mapping and levelling were undertaken and representatives cores were sampled. Detailed pollen and diatom analyses were undertaken in the laboratory and samples were submitted for radiocarbon assay where distinct pollen, diatom or lithostratigraphical changes were recorded. Loss on ignition analysis was also undertaken to ascertain the carbon content of the samples. The investigations have revealed that duri
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McGinnis, Benjamin Adam. "Late Holocene evolution of a retrograding barrier : Hutaff Island, North Carolina /." Electronic version (PDF), 2004. http://dl.uncw.edu/etd/2004/mcginnisb/benjaminmcginnis.pdf.

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Lee, Ting Jennifer. "Holocene evolution of a hypersaline lake Lagkor Tso, western Tibet /." Click to view the E-thesis via HKUTO, 2008. http://sunzi.lib.hku.hk/hkuto/record/B39634140.

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Freeman, Andrea Kelly Lee. "Middle to late holocene stream dynamics of the Santa Cruz River, Tucson, Arizona : implications for human settlement, the transition to agriculture and archaeological site preservation." Diss., The University of Arizona, 1997. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1997_349_sip1_w.pdf&type=application/pdf.

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Bridgeman, Jonathan G. "Understanding Mississippi Delta Subsidence through Stratigraphic and Geotechnical Analysis of a Continuous Holocene Core at a Subsidence Superstation." Thesis, Tulane University School of Science and Engineering, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10789629.

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<p> Land-surface subsidence can be a major contributor to the relative sea-level rise that is threatening many coastal communities. Loosely constrained subsidence rate estimates across the Mississippi Delta make it difficult to differentiate between subsidence mechanisms and complicate modeling efforts. New data from a nearly 40 m long, 12 cm diameter core taken during the installation of a subsidence monitoring superstation near the Mississippi River, southeast of New Orleans, provides insight into the stratigraphic and geotechnical properties of the Holocene succession at that site. Stratigr
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Callefo, Flávia 1983. "Análise tafonômica e paleoecológica de estruturas associadas a comunidades microbianas holocênicas e permianas." [s.n.], 2014. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287739.

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Orientador: Fresia Soledad Ricardi Torres Branco<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-25T01:31:00Z (GMT). No. of bitstreams: 1 Callefo_Flavia_M.pdf: 11737292 bytes, checksum: 8072787b62f7e014cd2301d513fc4a17 (MD5) Previous issue date: 2014<br>Resumo: Esteiras microbianas são estruturas organossedimentares laminadas, desenvolvidas a partir do acréscimo de lâminas de sedimentos aprisionados através do metabolismo de microrganismos, que induzem a precipitação de carbonato. Microbialitos são depósitos organ
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Brown, Kendrick Jonathan. "Late quaternary vegetation, climate, fire history, and GIS mapping of Holocene climates on southern Vancouver Island, British Columbia, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/NQ52755.pdf.

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Mok, Ka-man, and 莫嘉敏. "[Delta]¹³C as a palaeo-environmental indicator in a sediment core fromHong Kong." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2012. http://hub.hku.hk/bib/B49770470.

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A study of marine palaeo-landscape development through a sediment core in the western Hong Kong waters has been carried out in this project as the sedimentation record could reflect the environmental changes during the Holocene period. The objectives of this study was to reveal the influences of Holocene post-glacial sea-level fluctuations and the monsoonal freshwater discharge changes to the sedimentation processes in the mouth region of the Pearl River Estuary. These are the two important factors which shape the palaeo-landscape development. Data has been obtained from a ground-truthing v
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Hornsby, Kristofer Tyler. "Constraining the Holocene Extent of the Northwest Meers Fault, Oklahoma Using High-Resolution Topography and Paleoseismic Trenching." PDXScholar, 2017. https://pdxscholar.library.pdx.edu/open_access_etds/3890.

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The Meers Fault (Oklahoma) is one of few seismogenic structures with Holocene surface expression in the stable continental region of North America. Only the ~37 km-long southeastern section of the ~55 km long Meers Fault is interpreted to be Holocene-active. The ~17 km-long northwestern section is considered to be Quaternary-active (pre-Holocene); however, its low-relief geomorphic expression and anthropogenic alteration have presented difficulties in evaluating the fault length and style of Holocene deformation. We reevaluate surface expression and earthquake timing of the northwestern portio
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Bleakley, Nerida Lynn. "Late holocene palaeoecology of Taynaya Bay : the relationships between diatom assemblages and sediment composition in Antarctic coastal environments, and their response to regional climate change. Volume 1." Monash University, School of Geography and Environmental Science, 2003. http://arrow.monash.edu.au/hdl/1959.1/5784.

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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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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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Lee, Ting Jennifer, and 李婷. "Holocene evolution of a hypersaline lake: Lagkor Tso, western Tibet." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B39634140.

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Gates, Edward Breed. "The Holocene Sedimentary Framework of the Lower Columbia River Gorge." PDXScholar, 1994. https://pdxscholar.library.pdx.edu/open_access_etds/4801.

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The Columbia River is the largest fluvially dominated estuary in the Pacific Northwest, yet the Holocene transgressive fill of this system has not previously been studied. Nearly 1500 industry borehole and water well records in the lower Columbia River basin (LCRB) were analyzed. These records document the sedimentary infilling of the lower 120 miles of the drowned river valley that occurred during the Holocene marine transgression (10-0 ka) . Of particular importance is a key stratigraphic marker horizon of volcanic tephra that has been identified throughout the LCRB. INAA was used to determi
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Gudmundsson, Hjalti Johannes. "Holocene glacier fluctuations and tephrochronology of the Öræfi district, Iceland." Thesis, University of Edinburgh, 1999. http://hdl.handle.net/1842/15756.

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The aims of this thesis are to refine the tephrochronology of the Öræfi district, SE Iceland and assess the Holocene glacier fluctuations of the Öræfajökull ice cap. The pattern and timing of glacier fluctuations are determined using glacial geomorphology and tephrochronology, and the implications for palaeoclimate are assessed. Iceland is important to the study of global and regional climatic change because it is located close to both the marine and atmospheric Polar Fronts widely regarded as the key factors in the climate of the North Atlantic region. Six outlet glaciers were studied: Svi
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Sloss, Craig R. "Holocene sea-level change and the aminostratigraphy of wave-dominated barriers estuaries on the southeast coast of Australia." Access electronically, 2005. http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20060306.154507/index.html.

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Schlichting, Robert B. "Establishing the Inundation Distance and Overtopping Height of Paleotsunami from the Late-Holocene Geologic Record at Open-Coastal Wetland Sites, Central Cascadia Margin." PDXScholar, 2000. https://pdxscholar.library.pdx.edu/open_access_etds/3361.

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Mapping and stratigraphic investigations of back barrier, open-coastal plain sites have been used to establish minimum inundation distances and wave heights of tsunami produced by great subduction zone earthquakes in the central Cascadia margin. Cascadia tsunami deposits have been reported for many coseismic subsidence events in bay marsh settings where tidal-channel features focus tsunami energy. Variable magnitude (8.5±0.5 Mw), frequency (500±300 yr recurrence), and rupture geometry produce widely varying computer model outcomes for Casdcadia tsunami inundation. The results presented in this
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Chiti, Bernardo. "Holocene fluvial and marine influences and settlement interactions in the lower Ribble Valley, Lancashire, U.K." Thesis, University of Stirling, 2004. http://hdl.handle.net/1893/1805.

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The evolution of the lower course and estuary of the river Ribble (Lancashire, U.K.) during the Holocene is the object of study, along with the history of sediment fluxes in them and their influence on past human settlements. Investigation of the valley floor geomorphology and terrace fill stratigraphy and sedimentology, as well as palaeoecological analysis and a number of 14C essays, allowed the reconstruction of Late Pleistocene and Holocene alluvial history and chronology of a reach at the transition point between fluvial and estuarine influences; the archaeological evidence is evaluated in
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Dewey, Felicity Joy. "The sedimentology and palaeoenvironmental significance of vlei sediments on the Winterberg range, South Africa." Thesis, Rhodes University, 1989. http://hdl.handle.net/10962/d1001897.

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Palaeoenvironmental reconstruction of the late Pleistocene and Holocene geological periods for central and southern Africa has been hampered by the erratic distribution of suitable sites, incomplete and inaccurately dated sequences and the limited nature of published data. One geomorphological feature which has supplied valuable evidence for fluctuations in past environmental conditions, is the vlei or dambo. The type-site of these waterlogged features is in south central Africa, but similar features have been described on other continents. The clastic and organic sediments contained within th
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Metcalfe, Elisabet Joan. "Late-glacial through Holocene Stratigraphy and Lake-level Record of Rangely Lake, Western Maine." Fogler Library, University of Maine, 2007. http://www.library.umaine.edu/theses/pdf/MetcalfeEJ2007.pdf.

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Hazard, Colby. "Validity of Holocene Analogs for Ancient Carbonate Stratigraphic Successions: Insights from a Heterogeneous Pleistocene Carbonate Platform Deposit." BYU ScholarsArchive, 2015. https://scholarsarchive.byu.edu/etd/5496.

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Observations of modern carbonate depositional environments and their accompanying depositional models have been used for decades in the reconstruction and interpretation of ancient carbonate depositional environments and stratigraphic successions. While these Holocene models are necessary for interpreting their more ancient counterparts, they inherently exclude important factors related to the erosion, diagenesis, and ultimate preservation of sediments and sedimentary structures that are ubiquitous in shallow marine carbonate environments. Andros Island, Bahamas is an ideal location to examine
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Jones, Nadia Sittara. "Investigating the Holocene History of Eliot Glacier, Mount Hood, Oregon." PDXScholar, 2012. https://pdxscholar.library.pdx.edu/open_access_etds/618.

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This research documents the Holocene glacial history of Mount Hood, Cascade Mountains, Oregon by analyzing a set of three lateral moraines abutting Eliot Glacier, the largest glacier on the mountain. This study seeks to: 1) establish the relative ages of these lateral moraines and 2) determine if these features represent distinct glacial advances. The hypothesis is that the lateral moraines for Eliot Glacier represent three distinct periods of glacial advance based on their position relative to the current glacier and other diagnostic indicators. Soil profiles of three positions (shoulder, bac
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Crowe, Douglas E. "Stratigraphy and geologic history, Bunces Key, Pinellas County, Florida / by Douglas E. Crowe." University of South Florida, 2003. http://purl.fcla.edu/fcla/etd/SFE0000022.

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Title from PDF of title page.<br>Document formatted into pages; contains 113 pages.<br>Thesis (M.S.)--University of South Florida, 1983.<br>Includes bibliographical references.<br>Text (Electronic thesis) in PDF format.<br>ABSTRACT: Bunces Key, a narrow, linear, barrier island on the west-central coast of Florida, was formed in 1961. Its growth and development since that time is well documented by aerial photography. Cores taken from the Key and surrounding areas reveal a stratigraphic succession of facies reflecting rapid vertical aggradation. Sedimentation began on a gently sloping platform
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Dittmers, Klaus Hauke. "Late Weichselian to Holocene sedimentation in the inner Kara Sea : qualification and quantification of processes = Sedimentationsprozesse in der inneren Kara-See (Spät-Weichsel bis Holozän) /." Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 2006. http://www.gbv.de/dms/goettingen/510037178.pdf.

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Campo, Bruno <1984&gt. "The Pleistocene-Holocene Transition in the Po Plain (Italy): Stratigraphic Architecture and Sequence Stratigraphy from a Highly-Subsiding Basin." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7540/1/Tesi_dottorato_XXVIII_ciclo_Bruno_Campo_Esame_Finale_2016.pdf.

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This work focuses on the Late Pleistocene-Holocene transition in the southern Po Basin. Five areas were investigated, with the aim of unraveling the role of different allogenic factors (climate, eustacy, sediment supply) on stratigraphic architecture in the last 45 ky. The study starts from the distal portion of the basin (the coastal plain deposits) and then moves towards increasingly internal areas: the alluvial sector characterized by the Po channel belt deposits, and the mud-prone interfluvial succession between the Apenninic margin and the Po channel belt. In the coastal sector, high-reso
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Campo, Bruno <1984&gt. "The Pleistocene-Holocene Transition in the Po Plain (Italy): Stratigraphic Architecture and Sequence Stratigraphy from a Highly-Subsiding Basin." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7540/.

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This work focuses on the Late Pleistocene-Holocene transition in the southern Po Basin. Five areas were investigated, with the aim of unraveling the role of different allogenic factors (climate, eustacy, sediment supply) on stratigraphic architecture in the last 45 ky. The study starts from the distal portion of the basin (the coastal plain deposits) and then moves towards increasingly internal areas: the alluvial sector characterized by the Po channel belt deposits, and the mud-prone interfluvial succession between the Apenninic margin and the Po channel belt. In the coastal sector, high-reso
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Stoneman, Rob. "Holocene palaeoclimates from peat stratigraphy : extending and refining the model." Thesis, University of Southampton, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.317945.

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Gonthier, Nicole. "Holocene stratigraphy and sedimentation off the Great Whale River entrance, southeastern Hudson Bay." Thesis, McGill University, 1992. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=61215.

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The regional distribution of Holocene sediments of eastern Hudson Bay off the Great Whale River mouth was mapped using a grid of reflection seismic lines over 60 km long and covering an area of approximately 800 km$ sp2$ and data from eight piston cores. A larger data base and a greater area of study than that used in previous studies significantly increases our understanding of the sedimentation and deglaciation processes that have occurred in the area since the last deglaciation. Based on the seismic records and piston cores, four stratigraphic units overlying the Proterozoic bedrock (unit 1
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Maike, Christopher A. "A Flood-Tidal Delta Complex, The Holocene/Pleistocene Boundary, and Seismic Stratigraphy in the Quaternary Section off the Southern Assateague Island Coast, Virginia, USA." University of Toledo / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=toledo1408097363.

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Dal, Bo Patrick Francisco Fuhr. "Mecanismos deposicionais e processos pedogenéticos em lençóis de areia eólica = a Formação Marília, Neocretáceo da Bacia Bauru, Brasil, e La Salina, Holoceno da Bacia Tulum, Argentina." [s.n.], 2011. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287349.

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Orientador: Giorgio Basilici<br>Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-19T17:33:24Z (GMT). No. of bitstreams: 1 DalBo_PatrickFranciscoFuhr_D.pdf: 16255266 bytes, checksum: aeb871c6c13a2eecaa543a21baa19f06 (MD5) Previous issue date: 2011<br>Resumo: Lençóis de areia eólica são áreas morfodeposicionais caracterizadas por morfologias planas e ausência de dunas com faces de avalancha. Exemplos atuais e antigos de lençóis de areia eólica são conhecidos em todos os continentes e descritos na literatura desde o Paleoprote
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Summa, Michelle Carlene. "Geologic Mapping, Alluvial Stratigraphy, and Optically Stimulated Luminescence Dating of the Kanab Creek Area, Southern Utah." DigitalCommons@USU, 2009. https://digitalcommons.usu.edu/etd/506.

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At the turn of the century, Kanab Creek incised 30-meters into its alluvium, leaving behind fluvial terraces and thick basin fill sediments exposed along arroyo walls. Research objectives were to determine the timing and causes of past valley-filling and arroyo-cutting episodes along a 20 km-long reach of Kanab Creek in southern Utah. Fluvial deposits were mapped at the 1:12,000 scale and sediments were described and dated using Optically Stimulated Luminescence (OSL) and radiocarbon dating. The Kanab Creek valley can be divided into a narrow, upper terraced reach and a broad lower basin f
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Griffiths, Ann Hilary. "A stratigraphical, sedimentological and palaeoenvironmental analysis of Holocene and present-day coastal sedimentation : Wigtown Bay, S.W. Scotland." Thesis, University of Glasgow, 1988. http://theses.gla.ac.uk/1455/.

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Evidence of Holocene marine transgression and regression in South-West Scotland is exhibited in the stratigraphical record of present and former coastal deposits. Remnant areas of Holocene coastal (including marine) sediments are preserved at the head of marine inlets and estuaries along the northern shore of the Solway Firth and may extend up to 10km inland, indicating significant changes in coastal configuration as a result of marine transgression and regression during the last 10,000 years.At the head of Wigtown Bay, former Holocene coastal deposits are well exposed along the incised meande
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Russell, Paul. "Tsunami Stratigraphy in a Salt Pond on St. Croix, US Virgin Islands." The Ohio State University, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=osu1524156328491204.

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Levesh, Jarrett Leigh. "Middle Miocene to Holocene History of the Delacroix Island Fault System." ScholarWorks@UNO, 2019. https://scholarworks.uno.edu/td/2623.

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An in-depth field study of the Delacroix Island producing field illustrates the evolution of the east-trending Delacroix Island Fault during the last 13 My. Well log correlations and 3-D seismic interpretation of 22 subsurface bio-stratigraphic horizons across the fault reveal variable stratigraphic thicknesses and displacement. Wells, with well log curve data as shallow as 31 m (100 ft) below the surface, were used to calculate interval thicknesses, expansion indices, sediment accumulation rates, burial history and magnitudes of displacement. Through these analyses, a correlation was found be
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Partin, Judson Wiley. "Stalagmite reconstructions of western tropical pacific climate from the last glacial maximum to present." Diss., Georgia Institute of Technology, 2008. http://hdl.handle.net/1853/22556.

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The West Pacific Warm Pool (WPWP) plays an important role in the global heat budget and global hydrologic cycle, so knowledge about its past variability would improve our understanding of global climate. Variations in WPWP precipitation are most notable during El Niño-Southern Oscillation events, when climate changes in the tropical Pacific impact rainfall not only in the WPWP, but around the globe. The stalagmite records presented in this dissertation provide centennial-to-millennial-scale constraints of WPWP precipitation during three distinct climatic periods: the Last Glacial Maximum (LGM)
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Giacomelli, Serena <1974&gt. "The Remote Sensing-Stratigraphic Approach Applied to the Reconstruction of Holocene Sedimentary Evolution in Coastal Areas: Case Studies from Arno and Po Delta Plains (Italy)." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2017. http://amsdottorato.unibo.it/8109/1/Giacomelli_Serena_tesi.pdf.

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The growing availability of open-access databases, made the RS data and analyses to be increasingly employed in several geological research areas, including Quaternary and Environmental Geology. Despite the frequent use of the RS in alluvial-coastal plains paleohydrographic reconstruction, especially to identify stagnant versus well-drained areas (i.e., past wetlands and paleochannels, respectively) by means of brightness contrasts on images, the relationship between surface RS-derived traces and shallow subsurface stratigraphy remains underexplored. The present PhD thesis represents a contri
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Monjanel, Anne-Lise. "Les diatomées oligocènes à holocènes de l'Atlantique Nord et de la Méditerranée occidentale : biostratigraphie et paléoceanographie." Brest, 1987. http://www.theses.fr/1987BRES2035.

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Etude de la flore des diatomees de forages oceaniques et de coupes situees a terre: site 647 de l'odp pour l'oligocene; formation des moronites et coupes de cobatillas en espagne, coupes de saint-laurent la vernede et d'uzes dans le gard, coupes du "tripoli di contignaco" en italie et forages dsdp des sites 116, 334, 335 et 545 pour le miocene; site 646 de l'odp pour le plio-pleistocene. L'interpretation biostratigraphique permet de mettre en evidence des hiatus de la sedimentation ,lies a la circulation oceanique profonde et a la presence d'upwellings cotiers
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Valentine, David W. "Late Holocene stratigraphy, Humboldt Bay, California evidence for late Holocene paleoseismicity of the southern Cascadia subduction zone /." 1992. http://catalog.hathitrust.org/api/volumes/oclc/285528147.html.

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Oatney, Emily M. "Geology and paleoseismology of the Trans-Yamuna active fault system, Himalayan foothills of northwest India." Thesis, 1998. http://hdl.handle.net/1957/33684.

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Satellite image interpretation, geologic mapping, and paleoseismic trenching are used to investigate the Trans-Yamuna active fault system in the northwestern Doon Valley of the Indian Himalayan foothills. This east-west fault system is subparallel to and crosses the Main Boundary thrust near the structural transition from the Nahan salient to the Dehra Dun reentrant. The Trans-Yamuna active fault system may terminate to the east at a lateral ramp of the Main Boundary thrust. A south-side-up, relatively linear fault trace with variable fault dips suggests that the fault system is high-angle rev
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Higgs, Caldin Grant. "Geochemical insights into the influence of Holocene sea level change on the evolution of the Mkhuze River Delta, Lake St Lucia, northen KwaZulu- Natal." Thesis, 2017. https://hdl.handle.net/10539/23745.

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Thesis submitted in fulfilment of the academic requirements for the degree of Master of Science. Department of Chemistry University of Witwatersrand, Johannesburg April 2017.<br>The Mkhuze River discharges into the most northern part of Lake St Lucia, via a contemporary bayhead delta. The delta formed in response to sea level rise during the last deglaciation and today exerts great influence on the functioning of Lake St Lucia, one of the largest estuarine systems in Africa and a globally important conservation area. A sediment core (11.5 m) was extracted from the distal end of th
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Krentz, Sarah. "Potentially tsunamigenic event layer in late Holocene Great South Bay, Long Island, New York constraints on origins, processes, and effects /." Diss., 2009. http://etd.library.vanderbilt.edu/available/etd-07232009-175830/.

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Evans, Mary Yvonne. "The geology, sedimentology, geochronology and palaeo-environmental reconstruction of the Heelbo hillslope deposit, Free State Province, South Africa." Thesis, 2016. http://hdl.handle.net/10539/19373.

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Thesis submitted in fulfillment of the requirements for the Degree of Doctor of Philosophy University of the Witwatersrand South Africa 2015<br>A multidisciplinary sedimentological, stratigraphic, mineralogical and geochronological analysis of a small, fossil-bearing, Holocene hillslope deposit, flanking a mesa, has enabled a reconstruction of the palaeo-environmental history of the region. The hillslope deposit, located on the farm Heelbo in the eastern Free State Povince, South Africa, overlies Jurassic mudrock and sandstone of the Elliot Formation, Karoo Supergroup. The deposit is locat
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Mee, Aija C. "Origin, formation and environmental significance of sapropels in shallow Holocene coastal lakes of Southeastern Australia." 2007. http://hdl.handle.net/2440/57295.

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Title page, contents and abstract only. The complete thesis in print form is available from the University of Adelaide Library.<br>The aims of this investigation on the Holocene carbonate successions of three shallow, ephemeral lakes from the Cooring coastal plain were: to determine the timing of the sapropel ’events’ in the three lakes; to determine the origin of the sapropelic organic matter and evaluate changes; to establish whether sapropel deposition in these shallow, coastal lakes primarily reflects increased organic matter delivery to the sediments during periods of enhanced terrestrial
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Grossman, Eric E. "Holocene sea level history and reef development in Hawaii and the Central Pacific Ocean." 2001. http://wwwlib.umi.com/dissertations/fullcit/3017398.

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Shulmeister, James. "Late Quaternary and Holocene environmental history of Groote Eylandt, Northern Australia." Phd thesis, 1991. http://hdl.handle.net/1885/140901.

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