Gotowe bibliografie tematyczne / Geology, Stratigraphic Holocene

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Gotowa bibliografia na temat „Geology, Stratigraphic Holocene”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 29 lipca 2024

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Artykuły w czasopismach na temat "Geology, Stratigraphic Holocene"

Boreham, S. "The Geology of the Wicken Vision Area, lower Cam valley, Cambridgeshire, UK." Netherlands Journal of Geosciences - Geologie en Mijnbouw 92, no. 1 (April 2013): 47–59. http://dx.doi.org/10.1017/s0016774600000275.

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AbstractThe geology of the Wicken Vision Area in the lower Cam valley is described with reference to a stacked series of ten cross-sections through Holocene and Pleistocene deposits, and Cretaceous/Jurassic bedrock across the region. A detailed cross-section through a Holocene palaeochannel, with radiocarbon dating and pollen analyses is also presented. The structural geology of the bedrock and the stratigraphic arrangement of the Pleistocene and Holocene deposits are used to describe landscape development for the area. This study offers a new understanding of the stratigraphy and context of t

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Boreham, Steve, and Karolina Leszczynska. "The Geology of the Middle Cam Valley, Cambridgeshire, UK." Quaternary 2, no. 3 (July 12, 2019): 24. http://dx.doi.org/10.3390/quat2030024.

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This study offers a new understanding of the stratigraphy and context of the Pleistocene (including Elsterian and Weichselian) and Holocene deposits of the Middle Cam valley, Cambridgeshire, United Kingdom, and provides a unique and detailed view of the sediment architecture of these valley-fill and interfluve sediments. The new insights into the geology of the area, including dating, pollen analyses, and sediment architecture, are presented with reference to a series of nine cross-sections through Holocene and Pleistocene deposits, as well as Cretaceous bedrock across the region. The structur

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Genov, Ivan. "Comment on “Holocene sedimentation in the southwestern Black Sea: Interplay between riverine supply, coastal eddies of the Rim Current, surface and internal waves, and saline underflow through the Strait of Bosphorus” by O. Ankindinova, A. E. Aksu, R. N. Hiscott [Marine Geology, 420 (2020) 106092]." Review of the Bulgarian Geological Society 81, no. 2 (2020): 77–88. http://dx.doi.org/10.52215/rev.bgs.2020.81.2.6.

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Ankindinova et al. (2020) describe a series of hydrological events that have led to sedimentation and stratigraphic variations in the gradual sinking of the Black Sea shelf during the Holocene. A key aspect of the study is the attempt to provide a reliable stratigraphic basis for proving of a transgression in the basin throughout the Holocene. However, the conclusions of this approach run counter to the stratigraphic rules: redeposition and significant hiatus in the transgressive phase change of depth of sediment core location (M05-03P) – principle of superposition; merging of transgressive an

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Zhou, Weijian, Zhisheng An, and M. J. Head. "Stratigraphic Division of Holocene Loess in China." Radiocarbon 36, no. 1 (1994): 37–45. http://dx.doi.org/10.1017/s0033822200014302.

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Loess deposition within the Loess Plateau of China records the history of environmental change over the last 2.5 Myr. Loess-paleosol sequences of the last 10 ka, which have preserved information of global climate change, relate closely to human occupation of the area. Hence, studies of the deposition and development of Holocene loess are significant for studying environmental change and problems associated with engineering geology. We present here stratigraphic relations among four profiles from the south, west and center of the Loess Plateau. On the basis of 14C radiometric and AMS dates of o

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Latypova, E. K., and B. L. Yakheemovich. "Geochronology of the Pleistocene and Holocene in the Fore-Urals." Radiocarbon 35, no. 3 (1993): 441–47. http://dx.doi.org/10.1017/s003382220006046x.

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The paper presents the results for the 14C dating obtained recently in the Laboratory of the Institute of Geology, Ufa Science Centre, Russian Academy of Science, on the basis of megafaunal bones, peats, wood and mollusk shells. Dates are reported in stratigraphic sequence from the Late Würmian to the Holocene.

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Kurfurst, P. J., and S. R. Dallimore. "Engineering geology of nearshore areas off Richards Island, N.W.T.: a comparison of stable and actively eroding coastlines." Canadian Geotechnical Journal 28, no. 2 (April 1, 1991): 179–88. http://dx.doi.org/10.1139/t91-025.

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Nearshore areas off northern Richards Island can be expected to show considerable variability in lithology, strengths, and geothermal setting both in a temporal and a spatial sense. Drilling and laboratory studies carried out along onshore–offshore transects at a stable coastal site and an actively eroding coastal site have identified six major stratigraphic units of Holocene and pre-Holocene (Wisconsinan) age. The main factors controlling the geotechnical properties of these sediments and their distribution are the occurrence of shallow permafrost beneath areas seasonally covered by landfast

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Wheeler, A. J., and M. P. Waller. "The Holocene lithostratigraphy of Fenland, eastern England: a review and suggestions for redefinition." Geological Magazine 132, no. 2 (March 1995): 223–33. http://dx.doi.org/10.1017/s0016756800011766.

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AbstractThe Fenland basin is filled with unconsolidated Holocene marine and freshwater deposits. Stratigraphic studies of the basin date back to 1877. This paper reviews the various lithostratigraphic schemes which have been proposed. Particular attention is paid to the presently accepted lithostratigraphy. Examples and a case study of a newly surveyed area are used to highlight its failings. Many of the difficulties experienced in Fenland are common to problems of lithostratigraphic classification in coastal lowland environments, as is demonstrated by reference to recent debate in the southea

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Allen, Wai K., Kenneth D. Ridgway, J. A. Benowitz, T. S. Waldien, S. M. Roeske, P. G. Fitzgerald, and R. J. Gillis. "Neogene sedimentary record of the evolution of a translated strike-slip basin along the Denali fault system: Implications for timing of displacement, composite basin development, and regional tectonics of southern Alaska." Geosphere 18, no. 2 (February 8, 2022): 585–615. http://dx.doi.org/10.1130/ges02435.1.

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Abstract Analysis of the late Miocene to Holocene McCallum sedimentary basin, located along the south side of the eastern Denali fault system, provides a better understanding of strike-slip basin evolution, timing of displacement on the Denali fault, and tectonics of the southern Alaska convergent margin. Analysis of the McCallum basin utilizing measured stratigraphic sections, lithofacies analyses, and 40Ar/39Ar tephra ages documented a 564-m-thick, two-member stratigraphy. Fine-grained, lacustrine-dominated environments characterized deposition of the lower member, and coarse-grained, stream

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Thanh, Nguyen Trung, Paul Jing Liu, Mai Duc Dong, Dang Hoai Nhon, Do Huy Cuong, Bui Viet Dung, Phung Van Phach, Tran Duc Thanh, Duong Quoc Hung, and Ngo Thanh Nga. "Late Pleistocene-Holocene sequence stratigraphy of the subaqueous Red River delta and the adjacent shelf." VIETNAM JOURNAL OF EARTH SCIENCES 40, no. 3 (June 4, 2018): 271–87. http://dx.doi.org/10.15625/0866-7187/40/3/12618.

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The model of Late Pleistocene-Holocene sequence stratigraphy of the subaqueous Red River delta and the adjacent shelf is proposed by interpretation of high-resolution seismic documents and comparison with previous research results on Holocene sedimentary evolution on the delta plain. Four units (U1, U2, U3, and U4) and four sequence stratigraphic surfaces (SB1, TS, TRS and MFS) were determined. The formation of these units and surfaces is related to the global sea-level change in Late Pleistocene-Holocene. SB1, defined as the sequence boundary, was generated by subaerial processes during the L

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Malikov, D. G., A. O. Volvakh, N. E. Volvakh, P. Yu Savelyeva, I. Yu Ovchinnikov, and E. L. Malikova. "CHERNOUSOV LOG – THE NEW LOCATION OF LATE PLEISTOCENE AND HOLOCENE MAMMALS IN THE MINUSINSK DEPRESSION (GEOLOGICAL STRUCTURE AND CONDITIONS OF FORMATION)." Geology and mineral resources of Siberia, no. 1 (2023): 12–20. http://dx.doi.org/10.20403/2078-0575-2023-1-12-20.

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The paper defines a description of geological structure, conditions of formation and paleofaunistic material from two new locations of fossil mammals within the Minusinsk Depression. Three types of sedimentation are determined for the Chernousov Log section. The upper part of the section is represented by subaerial deposits of the Late Holocene. The middle section part is characterised by traces of soil formation of the Holocene optimum. The lower stratum is represented by alluvial deposits of the Late Karginian-Early Sartanian time. Two locations of mammals dating from the Sartanian and Holoc

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Rozprawy doktorskie na temat "Geology, Stratigraphic Holocene"

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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Książki na temat "Geology, Stratigraphic Holocene"

Hummell, Richard L. Holocene geologic history of Mobile Bay, Alabama. Tuscaloosa, Ala: Geological Survey of Alabama, 1995.

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1937-, Davis Richard A., ed. Geology of Holocene barrier island systems. Berlin: Springer-Verlag, 1994.

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Pirazzoli, P. A. World atlas of Holocene sea-level changes. Amsterdam: Elsevier, 1991.

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Kelly, Michael. Quaternary, pre-Holocene, marine events of western Greenland. Copenhagen: Grønlands geologiske undersøgelse, 1986.

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Kelly, Michael. Quaternary, pre-Holocene, marine events of western Greenland. Copenhagen, Denmark: Geological Survey of Greenland, 1986.

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Logan, Alan. Holocene reefs of Bermuda. Miami Beach, Fla. (Fisher Island, Miami Beach 33139): Comparative Sedimentology Laboratory, Division of Marine Geology and Geophysics, Rosenstiel School of Marine and Atmospheric Science, University of Miami, 1988.

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1947-, Fischer Manfred M., ed. Holocene evolution of Zeeland (SW Netherlands). Haarlem, The Netherlands: Nederlands Instituut voor Toegepaste Geowetenschappen TNO, 1997.

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Hummell, Richard L. Holocene geologic history of the west Alabama inner continental shelf, Alabama. Tuscaloosa, Ala: Geological Survey of Alabama, Environmental Geology Division, 1996.

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McCarthy, Francine. Late Holocene water levels in Lake Ontario: Evidence from Grenadier Pond. Toronto: [The Author], 1986.

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R, Dillenburg Sérgio, and Hesp P, eds. Geology and geomorphology of Holocene coastal barriers of Brazil. Berlin: Springer, 2009.

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Części książek na temat "Geology, Stratigraphic Holocene"

AlRefaei, Yaqoub, Ali Najem, Aimen Amer, and Faisal Al-Qattan. "Surface Geology of Kuwait." In The Geology of Kuwait, 1–26. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-16727-0_1.

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AbstractThis chapter represents a comprehensive review of Kuwait’s surface geology and stratigraphy from previous works accomplished by numerous geoscience researchers in the past decades. The surface of Kuwait is characterized by nearly flat topography, featureless to gently undulating, apart from a few tens of meters of escarpments in the north and south, and flat low to moderately elevated hills and ridges. It predominantly consists of siliciclastic sediments and sedimentary rock units ranging in age from Middle Eocene to Holocene. The main stratigraphic exposed successions are located in Jal Az-Zor escarpment, Al-Subyiah (Bahrah) area, Ahmadi Quarry, the Khiran Ridges, and the Enjefa Beach. The oldest exposed rock units are represented by the Middle Eocene Dammam Formation, which is exposed at the Ahmadi Quarry, whereas the youngest recent deposits cover most of Kuwait’s surficial area and lie on top of the Kuwait Group’s deposits. This chapter will illustrate the geology and stratigraphy of Kuwait's surface sediments and sedimentary rock strata. Recommendations and future insights were also documented as part of the way forward to improve the presently available work for the surface geology of Kuwait.

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Kalnina, Laimdota, Eliza Kuske, and Ilze Ozola. "Peat Stratigraphy and Changes in Peat Formation During the Holocene in Latvia." In Springer Geology, 951–56. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_179.

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Rudenko, Olga. "Upper Holocene Stratigraphy and Pollen Case Study of Isfjorden, West Spitsbergen (Svalbard, Norway)." In Springer Geology, 1309–13. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_250.

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Mriheel, Ibrahim, and Mohamed Hamruni. "Upper Pleistocene-Holocene Coastal Depositional Sediments of the Farwah Spit, NW Libya." In Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology and Petroleum Geology, 11–13. Cham: Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-43222-4_3.

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Zalasiewicz, Jan, Mark Williams, and, and Colin Waters. "Anthropocene Patterns in Stratigraphy as a Perspective on Human Success." In Human Success, 207—C9P118. Oxford University PressNew York, 2023. http://dx.doi.org/10.1093/oso/9780190096168.003.0009.

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Abstract The human species has deeply impacted the geology of our planet, our current environmental conditions now being very different from the stable interglacial conditions of the Holocene Epoch, in which human civilization flowered. Hence, a new epoch has been proposed, the Anthropocene, starting in tandem with the mid-20th-century Great Acceleration of population, industrialization, and globalization. One of the clearest measures of human impact on our planet is energy use, as reflected by rapidly increasing atmospheric carbon dioxide levels. Through this lens, the large-scale historical patterns of human activity show not gradual change but sudden and massive linked changes to geology and ecosystems. This has been driven by growth of the technosphere, a quasi-autonomous and emergent sphere of human-driven processes that interacts with the other Earth spheres. Consequences include the rapid accumulation of unrecycled waste, increasingly threatening the success of this development and hence of humans too.

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Emery, K. O., and David Neev. "Climate Inferred from Geology and Archaeology." In The Destruction of Sodom, Gomorrah, and Jericho. Oxford University Press, 1995. http://dx.doi.org/10.1093/oso/9780195090949.003.0006.

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Early climatic interpretations for the Lisan and later formations (Late Pleistocene and Holocene—Neev and Emery, 1967, figs. 16, 17) were supported and updated by information from additional coreholes. Although most new and old coreholes bottomed at relatively shallow depths, 20 to 30 m, four of them reached greater depths, 74, 80, 161, and 285 m beneath the 1960 floor of the Dead Sea south basin. The sequences consist of alternating layers of marl and rocksalt. Most marls were deposited from dilute brine during high lake levels and contain alternating laminae of chemical deposits of white aragonite, gray gypsum, and fine-grained detritus consisting of yellowish, brown, green, or dark gray carbonates, quartz, and clay. The detrital fraction is coarser and more dominant toward the deltas, especially near Amazyahu escarpment in the south. Rocksalt layers indicate deposition from more concentrated brine when the levels dropped to about -400 m m.s.l. Lower elevations could have been reached when the sea continued to shrink and when the runoff-to-evaporation ratio diminished, bringing the south basin to complete dessication. As neither the geochemical nature (ionic ratios) of the brines nor the physiography of the terminal water body has changed at least since Late Pleistocene or Lisan Lake time (Katz, Kolodny, and Nissenbaum, 1977), it is probable that through the past 60,000 years rocksalt was precipitated only when the water surface was at or below the critical level of -400 m m.s.l. Gamma-ray logs for some of the new coreholes provide more objective and precise depths of marl and rocksalt layers than do actual samples of sediments. Content of radiogenic minerals in the rocksalt is negligible compared with that in the marl; thus, these layers identify changing physical environments and climates as well as correlating stratigraphy. On gamma-ray logs the peaks or highest intensities of positive anomalies indicate that marl layers or wet climatic subphases and their thicknesses on the logs are proportional to their duration. Presence of negative anomalies or very low levels of gamma radiation show both the existence and thickness of rocksalt layers that denote dry climatic phases.

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Kindinger, Jack L., Shea Penland, S. Jeffress Williams, John R. Suter, Randolph A. McBride, Gregg R. Brooks, and Stan Locker. "Nearshore Holocene Stratigraphy, Northern Gulf of Mexico: Integration of Regional Geologic Studies." In Coastal Depositional Systems in the Gulf of Mexico: Quaternary Framework and Environmental Issues. SEPM Society for Sedimentary Geology, 1991. http://dx.doi.org/10.5724/gcs.91.12.0096.

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Montanari, Alessandro, Marco Peter Ferretti, Maurizio Mainiero, David McGee, Gaia Pignocchi, Stefano Recanatini, and Roberto Zorzin. "Revisiting the archaeological site of Grotta dei Baffoni Cave (Frasassi Gorge, Italy): Integrated stratigraphy, archaeometry, and geochronology of upper Pleistocene–Holocene cave sediments." In From the Guajira Desert to the Apennines, and from Mediterranean Microplates to the Mexican Killer Asteroid: Honoring the Career of Walter Alvarez. Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2557(28).

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ABSTRACT In this paper, we present old and new data about our integrated interdisciplinary stratigraphic study of sedimentary deposits preserved in the Grotta dei Baffoni Cave of the Frasassi hypogenic cave complex, including sedimentological, paleontological, archaeometric, and radiometric analyses. This research work allowed us to reconstruct the geologic, environmental, and human history of this part of the northeastern Apennines of Italy for the past 200,000 years, from the late Middle Pleistocene to the Present. Accumulation of alluvial sediment began in this cave ~200,000 years ago, when an entrance was breached by the Sentino River during its process of incision and deepening of the Frasassi Gorge coupled with regional tectonic uplift. Flooding of the cave went on until the entrance sill of the cave was lifted up to an elevation that could no longer be reached by the river, sometime in the mid–Late Pleistocene. After this, windblown dust (i.e., loess) and coarser carbonate clasts derived from the disintegration of the vaults due to cryogenic processes and/or seismically induced collapses of the limestone vaults, accumulated on this now-dry underground environment. The stratigraphy of an ~4-m-thick sedimentary deposit accumulated in the vast atrium room of the cave was measured, sampled, and documented in two excavation trenches in 1952 by archaeologist Anton Mario Radmilli. By collecting a dozen stratigraphically located osteological finds for 14C dating, and revisiting artifacts collected by Radmilli, which are archived respectively in the Museum of Natural History of Verona and in the National Museum of Archaeology of Ancona, we assessed that the cave was frequented by wild animals, such as cave bear and ibex, starting in the mid–Late Pleistocene. Dating of charcoal particles from subsurface sediments in the inner part of the cave suggested that fires were lit in this cave by Epigravettian visitors during the Younger Dryas cold period. Scarce archaeological evidence nevertheless suggests that man began using this underground environment for worship practices probably in the early Neolithic. Human bones in the lower part of one of Radmilli’s excavations yielded early Eneolithic ages. No other human bones were found in overlying levels of this excavation, but the typology of animal bones and associated ceramic artifacts, corroborated by our 14C dates, suggest that this cave was utilized as a worship or ritual place until the early Middle Bronze Age. After that, the cave was sporadically used as a shelter for herders until recent times.

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"A Review of the Stratigraphy of Eastern Paratethys (Oligocene—Holocene), With Particular Emphasis on the Black Sea." In Regional and Petroleum Geology of the Black Sea and Surrounding Region, 39–51. American Association of Petroleum Geologists, 1997. http://dx.doi.org/10.1306/m68612c4.

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Kindler, Pascal. "New data on the Holocene stratigraphy of Lee Stocking Island (Bahamas) and its relation to sea-level history." In Terrestrial and shallow marine geology of the Bahamas and Bermuda. Geological Society of America, 1995. http://dx.doi.org/10.1130/0-8137-2300-0.105.

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Streszczenia konferencji na temat "Geology, Stratigraphic Holocene"

Ballarin, Matteo, and Nadia D'Agnone. "Paesaggio, suolo, tempo: la rappresentazione dei tempi geologici nella citta' di Catania." In International Conference Virtual City and Territory. Roma: Centre de Política de Sòl i Valoracions, 2014. http://dx.doi.org/10.5821/ctv.8041.

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Parlare di tempo geologico è un modo di contestualizzare i processi materiali della terra nella sua storia. La scala dei tempi geologici suddivide la lunga storia della terra in eoni, ere, periodi ed epoche, non omogenei tra loro, ma in relazione l'un l'altro a seconda di ciò che emerge dall'analisi dei dati stratigrafici o dallo studio della stratificazione dei diversi livelli della crosta terrestre. Recentemente negli studi relativi a territorio e paesaggio è stata introdotta l'idea che l'epoca dell'Olocene, iniziata circa 11.700 anni fa, sia terminata e c

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Fisher, James E., Saba Esmailzadeh, and Jacob N. Fillingham. "Geological and Geotechnical Considerations for Floating Offshore Wind Infrastructure within the U.S. Atlantic OCS." In Offshore Technology Conference. OTC, 2023. http://dx.doi.org/10.4043/32578-ms.

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Abstract Current offshore wind activities within the Atlantic Outer Continental Shelf are within water depths suitable for fixed-bottom foundations, generally considered as water depths shallower than 60 m. Recent BOEM designated call areas within the Central Atlantic include two areas on the continental slope in water depths greater than 200 m that will require floating offshore wind turbines. The objective of this study is to expand upon a previously completed BOEM-funded desktop study and focus on the geological and geotechnical conditions and the engineering constraints for the deep-water

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