Bibliografias temáticas / Massachusetts – Cape Cod

Literatura científica selecionada sobre o tema "Massachusetts – Cape Cod"

Autor: Grafiati
Publicado: 25 de julho de 2024
Última modificação: 26 de julho de 2024

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Artigos de revistas sobre o assunto "Massachusetts – Cape Cod"

1

Leatherman, Stephen P. "Barrier Migration of Nauset Beach, Cape Cod, Massachusetts". Journal of Coastal Research 101, sp1 (26 de agosto de 2020): 89. http://dx.doi.org/10.2112/jcr-si101-019.1.

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Uchupi, Elazar, Graham Giese, Neal Driscoll e D. G. Aubrey. "Postglacial Geomorphic Evolution of a Segment of Cape Cod Bay and Adjacent Cape Cod, Massachusetts, U.S.A." Journal of Coastal Research 216 (novembro de 2005): 1085–106. http://dx.doi.org/10.2112/05-765a.1.

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Oldale, Robert N. "A Late Wisconsinan Marine Incursion into Cape Cod Bay, Massachusetts". Quaternary Research 30, n.º 3 (novembro de 1988): 237–50. http://dx.doi.org/10.1016/0033-5894(88)90001-4.

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Reinterpretation of seismic-reflection data from Cape Cod Bay has produced a revised late Wisconsinan history. Acoustically laminated deposits, originally inferred to be glaciolacustrine, are shown to be glaciomarine by tracing them to glaciomarine mud in Stellwagen Basin, north of Cape Cod Bay. A late Wisconsinan marine deposit of nonglacial origin overlies the glaciomarine deposits in Cape Cod Bay. Both deposits indicate that the crust was isostatically depressed below the late Wisconsinan eustatic sea level and that deglaciation and marine submergence occurred simultaneously. Valleys cut into the marine deposits, both glacial and nonglacial, indicate that a low sea-level stand, the result of isostatic rebound, occurred shortly after the marine incursion. A transgressive uncomformity and marine deposits, both mostly of Holocene age, overlie the late Wisconsinan deposits. The marine incursion, regression, and Holocene transgression represent the northward passage of an isostatically induced peripheral bulge following deglaciation. In turn, the bulge, a response to crustal loading and unloading, indicates thick glacier ice in the terminal zone and lends support to arguments for a maximum Laurentide ice model. Evidence for a late Wisconsinan marine incursion, regression, and the passage of a peripheral bulge should be sought in the other bays and sounds of the New England terminal zone.
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Burchsted, J. C. A., e Fred Burchsted. "Lady Crabs, Ovalipes ocellatus, in the Gulf of Maine". Canadian Field-Naturalist 120, n.º 1 (1 de janeiro de 2006): 106. http://dx.doi.org/10.22621/cfn.v120i1.254.

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The Lady Crab (Ovalipes ocellatus), mainly found south of Cape Cod and in the southern Gulf of St. Lawrence, is reported from an ocean beach on the north shore of Massachusetts Bay (42°28'60"N, 70°46'20"W) in the Gulf of Maine. All previously known Gulf of Maine populations north of Cape Cod Bay are estuarine and thought to be relicts of a continuous range during the Hypsithermal. The population reported here is likely a recent local habitat expansion.
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Motzkin, Glenn, Robert Eberhardt, Brian Hall, David R. Foster, Jonathan Harrod e Dana MacDonald. "Vegetation variation across Cape Cod, Massachusetts: environmental and historical determinants". Journal of Biogeography 29, n.º 10-11 (outubro de 2002): 1439–54. http://dx.doi.org/10.1046/j.1365-2699.2002.00800.x.

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Novarino, Gianfranco, Alan Warren, Nancy E. Kinner e Ronald W. Harvey. "Protists from a sewage‐contaminated aquifer on cape cod, Massachusetts". Geomicrobiology Journal 12, n.º 1 (janeiro de 1994): 23–36. http://dx.doi.org/10.1080/01490459409377968.

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Naevdal, G. "Oberservations on the ecology of Western Cape Cod Bay, Massachusetts". Fisheries Research 4, n.º 2 (julho de 1986): 174–76. http://dx.doi.org/10.1016/0165-7836(86)90046-9.

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McKelvey, W. "Association between residence on Cape Cod, Massachusetts, and breast cancer". Annals of Epidemiology 14, n.º 2 (fevereiro de 2004): 89–94. http://dx.doi.org/10.1016/s1047-2797(03)00120-0.

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Erwin, R. Michael, Courtney J. Conway e Steven W. Hadden. "Species Occurrence of Marsh Birds at Cape Cod National Seashore, Massachusetts". Northeastern Naturalist 9, n.º 1 (2002): 1. http://dx.doi.org/10.2307/3858572.

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Portniaguine, O., e D. K. Solomon. "Parameter estimation using groundwater age and head data, Cape Cod, Massachusetts". Water Resources Research 34, n.º 4 (abril de 1998): 637–45. http://dx.doi.org/10.1029/97wr03361.

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Teses / dissertações sobre o assunto "Massachusetts – Cape Cod"

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Rolfs, Amy M. (Amy Marie) 1975. "Interactive GIS approach to generate capture curves at the Massachusetts Military Reservation, Cape Cod, Massachusetts". Thesis, Massachusetts Institute of Technology, 1998. http://hdl.handle.net/1721.1/46138.

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Eichler, Hilary J. "Natural attenuation of chlorinated solvents at Ashumet Valley, Cape Cod, Massachusetts". Thesis, Massachusetts Institute of Technology, 1997. http://hdl.handle.net/1721.1/42624.

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Sagintayev, Zhanay. "Relationship between 20th century dune migration and wetland formation at Cape Cod National Seashore, Massachusetts". Virtual Press, 2006. http://liblink.bsu.edu/uhtbin/catkey/1339460.

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Outer Cape Cod (Massachusetts) is dominated by active and stabilizing parabolic and transverse dunes interspersed with numerous inter-dune wetlands. Dune migration has been significantly affected by human activities; conversely, current dune movements are affecting local populations. The objective of the reported research was to assess, using remote sensing and geographic information systems (GIS) technologies, migration of the Cape Cod dunes and the effect of dune movement on distribution of associated wetlands. Aerial photographs from 1938 through 2003 were analyzed to track individual dune movements and subsequent wetland propagation and expansion. Absolute dune movement rates during this period were computed, with a plot of dune movement as a cumulative function. One sub-problem of this study was to quantify `white' areas of active moving sand and `dark' areas of vegetation, in order to quantify changes in vegetative cover with wetland propagation and, conversely, vegetative disappearance with dune movement. Attempts were made to correlate the Palmer Drought Severity Index (PDSI) with dune migration. Based on review of aerial photographs, parabolic dunes have migrated 150 to 250 m since 1938, with 60% of the movement occurring between 1938 and 1977. The relation between absolute parabolic dune migration and corresponding PDSI is approximately logarithmic. Maximum dune migration is associated with PDSI values lower than -2 and reflects moderate drought conditions. Wetlands consistently trailed the dunes, and the distance of wetland movement was related to dune movement distances. Wetland migration was particularly marked from the 1950s to the 1980s. Based on review of georeferenced aerial photographs, it is concluded that marked stabilization of Cape Cod dunes occurred in the 1980s and 1990s, with renewed movement in the 21st Century. This study provides a practical application for assessment of dune migration and vegetative transformations over time using remote sensing and GIS technologies.
Department of Natural Resources and Environmental Management
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Motolenich-Salas, Kenneth M. (Kenneth Michael). "Denitrification as a means of addressing nitrate-contaminated groundwater on Cape Cod, Massachusetts". Thesis, Massachusetts Institute of Technology, 1997. http://hdl.handle.net/1721.1/99607.

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Thesis: M. Eng., Massachusetts Institute of Technology, Department of Civil and Environmental Engineering, June 1997.
Cataloged from PDF version of thesis. "June 1997." Title as it appears in MIT Commencement Exercises program, June, 1997: Denitrification as a means of addressing vitrate-contaminated groundwater on Cape Cod, MA.
Includes bibliographical references (pages 127-134).
The residents of Cape Cod face a problem of nitrate contamination of their groundwater (their primary source of drinking water) and their coastal and aquatic environments. Groundwater is the only source of drinking water on Cape Cod and the aquifer is defined as a "sole source aquifer" by the Safe Drinking Water Act. While many activities contribute nitrate (NO₃-) contamination to groundwater, nitrate contamination from land application poses the greatest threat on Cape Cod. Only a few small areas on Cape Cod are sewered, and the majority of homes and businesses rely on septic systems. Increased urban development has increased the frequency of installation of septic systems. In many locations, the density of septic systems is greater than the natural ability of the subsurface environment to receive and purify system effluents prior to their movement into groundwater. Many of Cape Cod's environmental resources, including coastal receiving waters, marine embayments threatened with eutrophication, endangered wetlands, and Areas of Critical Environmental Concern (ACECs), are also threatened by nitrate-contaminated groundwater flowing into the coastal waters of Cape Cod, which are extremely sensitive to eutrophication from excess nitrogen loading. In order to address nitrate-contaminated groundwater on Cape Cod, solutions based on biological denitrification should be considered. In this work, these solutions are discussed and explored. First, the major sources of contamination and possible health and environmental effects are discussed. Second, the fate and transport of nitrate in the subsurface environment is analyzed, with a detailed discussion of the factors governing biological denitrification. Third, the current status of groundwater nitrate contamination on Cape Cod is detailed. Fourth, possible options, alternative septic systems and in-situ remedial schemes, which all use biological denitrification as a means of attenuating nitrate in septic system effluent, are presented. Lastly, a proposal for action to deal with nitrate contamination on Cape Cod and suggestions for future study and long-term action for domestic sewage are given, based on my opinion of the scientific and engineering aspects of the circumstances of the contamination.
by Kenneth M. Motolenich-Salas.
M. Eng.
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Gagnon, Judy C. (Judy Claire). "The public perception of drinking treated groundwater from the Massachusetts Military Reservation, Cape Cod, MA". Thesis, Massachusetts Institute of Technology, 1996. http://hdl.handle.net/1721.1/40587.

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Cazayoux, John Patrick. "A resort in Provincetown, Massachusetts rethinking tourism on Cape Cod with a regionalist and sustainable response /". College Park, Md.: University of Maryland, 2007. http://hdl.handle.net/1903/7157.

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Thesis (M. A.) -- University of Maryland, College Park, 2007.
Thesis research directed by: Architecture. Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.
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Lin, Tina L. (Tina Li-Te). "Analysis of geologic parameters on recirculating well technology, using 3-D numerical modeling : Massachusetts Military Reservation, Cape Cod". Thesis, Massachusetts Institute of Technology, 1997. http://hdl.handle.net/1721.1/45485.

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Lopez-Calva, Enrique J. (Enrique Jaiver). "Analysis pumping schemes for the extraction of contaminated groundwater at Cape Cod, Massachusetts, using 3-D numerical modeling". Thesis, Massachusetts Institute of Technology, 1996. http://hdl.handle.net/1721.1/40162.

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Thesis (M. Eng.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 1996.
Includes bibliographical references (leaves 61-65).
by Enrique J. Lopez-Calva.
M.Eng.
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Lee, Ronald Sang. "A physical assessment of Snake Pond of Cape Cod, Massachusetts, including a thermal and surface/ground water model". Thesis, Massachusetts Institute of Technology, 1997. http://hdl.handle.net/1721.1/42686.

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Gutierrez, Benjamin Thomas. "Relative sea-level rise and the development of channel-fill and shallow-water sequences on Cape Cod, Massachusetts". Thesis, Massachusetts Institute of Technology, 1999. http://hdl.handle.net/1721.1/55058.

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Thesis (M.S.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 1999.
Includes bibliographical references (leaves 60-63).
Channel-fill sediments located in shallow-water off the south shore of Cape Cod, Massachusetts, provide a record of the late-Pleistocene and Holocene geological evolution in a post-glacial setting. Though conventionally difficult to sample adequately and anticipated to have low preservation potential, channel-fill sequences record in some detail differing relative sea-level and sedimentation processes. Two distinct channel-fill sequences record differing sequence stratigraphies, and hence different origins and post glacial histories. These sequences have accumulated in channels eroded into two different late-Pleistocene glacial units. The first fill-type was encountered in channels on the upper portions of the channel network in northern half of the study site. Channels in this portion of the channel system were incised into the late-Pleistocene glacial outwash substrate by spring sapping Uchupi and Oldale, 1994. The channel-fill sequences are comprised of a transgressive systems tract composed of a consistent sequence of coastal embayment and shoreline facies that have succeeded one another in response to Holocene relative sea-level rise. As relative sea-level flooded these paleo-channels, marsh environments were established in response to rising relative sea-level. With continued sea-level rise, the marsh environments migrated farther up channel. The exposed paleo-channels continued to flood, accommodating quiet water coastal embayments, likely protected from wave action by barrier beaches located more seaward. As relative sea-level rise continued, the coastline was driven landward over regions within the paleo-channels that formerly accommodated marsh and embayment sedimentation. The landward migration of the coastline was indicated by beach and barrier facies that covered the fine grained coastal embayment sediments. With further relative sea-level rise, beach and barrier settings were eroded as the shoreface migrated farther landward and nearshore marine deposition by wave and tidal flows ensued. Sedimentary environments similar to those recorded in the channels are found in modern coastal embayments on the south shore of Cape Cod. The second channel-fill type, which forms part of the southern and western portion of the channel network is more difficult to relate to the previously described sequence. The channels that contain fill were not adequately defined in this survey but were probably incised during the late-Pleistocene in response to ice melting and retreat. The sediments that make up this channel-fill are composed mainly of late-Pleistocene glaciolacustrine silts and clays. Sediments that make up the Holocene transgressive systems tract are limited to the upper meter of this channel sequence. They are composed of two sand units that reflect Holocene beach and nearshore sedimentation. The absence of coastal embayment and other paralic facies from the systems tract suggests that these channels did not accommodate protected embayments or that these sediments were not well preserved during the submergence of this region. Changes in the channel orientation or in the rate of relative sea-level rise may have contributed to this difference in sediment fill.
by Benjamin Thomas Gutierrez.
M.S.
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Livros sobre o assunto "Massachusetts – Cape Cod"

1

Orwig, Timothy. Cape Cod Canal. Charleston, S.C: Arcadia Pub., 2013.

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2

Cape Cod. New York, NY: Warner Books, 1991.

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3

Cape Cod. New York, N.Y: Warner Books, 1992.

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4

Bartlett, Ray. Cape Cod, Martha's Vineyard & Nantucket. 3a ed. Berkeley, CA: Avalon Travel, 2013.

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5

Grant, Kim. Cape Cod, Martha's Vineyard & Nantucket. 9a ed. Woodstock, VT: Countryman Press, 2011.

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6

Monbleau, Marcia J. At home--Harwich, Cape Cod, Massachusetts. [Harwich]: M.J. Monbleau, 1993.

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7

Minetor, Randi. Cape Cod National Seashore pocket guide. Guilford, CT: Falcon, 2010.

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8

Tim, Smith, e John Miller. Cape Cod stories: Tales from Cape Cod, Nantucket, and Martha's Vineyard. San Francisco: Chronicle Books, 1996.

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Irish, J. D. Tides of Massachusetts and Cape Cod Bays. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1992.

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Massachusetts. Executive Office of Environmental Affairs. Cape Cod Massachusetts community preservation resource guide. Boston, Mass.]: Executive Office of Environmental Affairs, 2000.

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Capítulos de livros sobre o assunto "Massachusetts – Cape Cod"

1

Portnoy, John W. "Salt Marsh Restoration at Cape Cod National Seashore, Massachusetts". In Tidal Marsh Restoration, 299–314. Washington, DC: Island Press/Center for Resource Economics, 2012. http://dx.doi.org/10.5822/978-1-61091-229-7_18.

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Turner, Jefferson T. "Planktonic copepods of Boston Harbor, Massachusetts Bay and Cape Cod Bay, 1992". In Ecology and Morphology of Copepods, 405–13. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-017-1347-4_51.

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Motzkin, Glenn, William A. Patterson e Natalie E. R. Drake. "Fire History and Vegetation Dynamics of a Chamaecyparis Thyoides Wetland on Cape Cod, Massachusetts". In Ecosystem Management, 116–29. New York, NY: Springer New York, 1993. http://dx.doi.org/10.1007/978-1-4612-4018-1_13.

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FitzGerald, Duncan M., e Todd M. Montello. "Backbarrier and inlet sediment response to the breaching of Nauset spit and formation of New Inlet, Cape Cod, Massachusetts". In Coastal and Estuarine Studies, 158–85. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/ce044p0158.

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Chalfa Ruyter, Nancy Lee. "New York, Cape Cod, San Antonio". In La Meri and Her Life in Dance, 203–37. University Press of Florida, 2019. http://dx.doi.org/10.5744/florida/9780813066097.003.0009.

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This chapter tells of La Meri’s last years in New York City (1956-1960) and her next new beginning in Cape Cod, Massachusetts, with her sister Lilian Newcomer. There, she established a school, Ethnic Dance Arts, and an annual ethnic dance festival that presented artists from the United States and other countries. Gopal contacted La Meri sometime in 1958, asking her to join him in the performances he was giving in Trinidad, and she lists rehearsals and other meetings she had with him in June and August of that year. In her last years, she was cared for by William J. Adams, a former student and dancer. In 1984, she moved back to San Antonio with Adams and died there in 1988.
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Fisher, John J., e Stephen P. Leatherman. "Glacial and coastal geology, Cape Cod National Seashore; Massachusetts". In Centennial Field Guide Volume 5: Northeastern Section of the Geological Society of America, 213–20. Geological Society of America, 1987. http://dx.doi.org/10.1130/0-8137-5405-4.213.

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Uchupi, Elazar, G. S. Giese, D. G. Aubrey e D. J. Kim. "The Late Quaternary Construction of Cape Cod, Massachusetts: A Reconsideration of the W. M. Davis Model". In The Late Quaternary Construction of Cape Cod, Massachusetts: A Reconsideration of the W. M. Davis Model. Geological Society of America, 1996. http://dx.doi.org/10.1130/0-8137-2309-4.1.

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Stanford, James N. "Focus on Subgroups within the Hub". In New England English, 182–208. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190625658.003.0007.

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This is the second of two chapters (Chapters 6 and 7) that analyze the Dartmouth-based fieldwork data in eastern Massachusetts. This chapter “zooms in” to focus on particular subgroups within the Hub data set. First, the chapter provides statistical and graphical comparisons of traditional New England dialect features by contrasting two nearby groups: White speakers in the traditional working-class South Boston neighborhood, and Black/African American speakers in nearby Dorchester, Hyde Park, and other neighborhoods. The chapter concludes with a fieldwork project in Cape Cod. In each case, the chapter provides detailed plots of dialect features and statistical analyses with respect to age, gender, social class, ethnicity, and other factors
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Gura, Philip F. "The Mashpee Revolt { 1833–1834 }". In Life of William Apess, Pequot, 77–99. University of North Carolina Press, 2015. http://dx.doi.org/10.5149/northcarolina/9781469619989.003.0005.

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This chapter focuses on William Apess's involvement in the Mashpee Revolt of 1833–4. While he was preaching in Scituate and Kingston on the South Shore of Massachusetts, Apess heard conflicting accounts of the Mashpee Indians' situation. Some evidently were content with the government-appointed overseers' protection of their tribal rights, while others vehemently opposed the paternalism and corruption that such oversight encouraged. Apess knew of the tribe's various petitions to the Massachusetts legislature. In May 1833, Apess traveled to Cape Cod to learn more about this situation as well as to preach to them. He met Phineas Fish, the minister assigned to the Mashpees. With Apess's assistance, the Mashpees drafted a memorial to Governor Levi Lincoln in which, among other things, they expressed their desire for self-government. The rest of this chapter examines the events leading up to the Mashpee Revolt and the aftermath of the Natives' action, including the trial of Apess and his confederates and his incarceration, along with the Mashpee's eventual incorporation as a state-recognized district.
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Gaskell, Ivan. "Joining the club: a Tongan ‘akau in New England". In Curatopia, 176–90. Manchester University Press, 2019. http://dx.doi.org/10.7228/manchester/9781526118196.003.0012.

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This chapter examines the place of Oceanic clubs in New England collections. During the nineteenth century, they occupied an equivocal position in the New England mental repertory as indices of savage sophistication, and as souvenirs of colonial childhood or travel. Focusing on a Tongan ‘akau tau in the collection of the Chatham Historical Society on Cape Cod, Massachusetts, this chapter traces what can be known of its history as a highly regarded prestige gift item among New Englanders from the middle of the nineteenth century until its entry into the museum. As a thing that an early owner could alienate legitimately, its presence in Chatham is not unethical, yet it nonetheless imposes stewardship responsibilities—consultation with the originating community—that such a small institution is poorly placed to meet. This requires understanding and patience rather than disapprobation.
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Trabalhos de conferências sobre o assunto "Massachusetts – Cape Cod"

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Clement, William P., e Allen M. Gontz. "SEISMIC REFLECTIONS FROM OFFSHORE OF PROVINCETOWN, CAPE COD, MASSACHUSETTS". In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272429.

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Schneiderman, Jill S. "MICROPLASTICS IN DUNE SANDS FROM OUTER CAPE COD, MASSACHUSETTS". In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282703.

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Carnevale, Mario, e Jutta Hager. "GPR Survey to Characterize Lake Bottom Sediments, Cape Cod, Massachusetts". In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2003. Environment and Engineering Geophysical Society, 2003. http://dx.doi.org/10.4133/1.2923234.

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Carnevale, Mario, e Jutta Hager. "Gpr Survey To Characterize Lake Bottom Sediments, Cape Cod, Massachusetts". In 16th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.190.lak03.

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Johnson, Carole, Jason Sorenson, Denis R. LeBlanc e John Lane. "NUCLEAR MAGNETIC RESONANCE LOGGING -- LESSONS LEARNED AT THE MASSACHUSETTS MILITARY RESERVATION, CAPE COD, MASSACHUSETTS". In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2014. Society of Exploration Geophysicists and Environment and Engineering Geophysical Society, 2014. http://dx.doi.org/10.4133/sageep.27-032.

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Johnson, Carole, Jason Sorenson, Denis R. LeBlanc e John Lane. "NUCLEAR MAGNETIC RESONANCE LOGGING -- LESSONS LEARNED AT THE MASSACHUSETTS MILITARY RESERVATION, CAPE COD, MASSACHUSETTS". In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2014. Society of Exploration Geophysicists and Environment and Engineering Geophysical Society, 2014. http://dx.doi.org/10.1190/sageep.27-032.

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GIESE, GRAHAM S., MARK B. ADAMS, STACY S. ROGERS, S. LAWRENCE DINGMAN, MARK BORRELLI e THERESA L. SMITH. "COASTAL SEDIMENT TRANSPORT ON OUTER CAPE COD, MASSACHUSETTS: OBSERVATION AND THEORY". In The Proceedings of the Coastal Sediments 2011. World Scientific Publishing Company, 2011. http://dx.doi.org/10.1142/9789814355537_0176.

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Singha, Kamini, Andrew M. Binley, John W. Lane e Steven M. Gorelick. "Electrical Imaging of Tracer Migration at the Massachusetts Military Reservation, Cape Cod". In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2003. Environment and Engineering Geophysical Society, 2003. http://dx.doi.org/10.4133/1.2923190.

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Horgan, Julianna S., e Cynthia R. Domack. "COASTAL EROSION AND LIGHTHOUSE RELOCATION ON CAPE COD AND MARTHA’S VINEYARD, MASSACHUSETTS". In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-290107.

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Singha, Kamini, Andrew M. Binley, John W. Lane Jr. e Steven M. Gorelick. "Electrical Imaging Of Tracer Migration At The Massachusetts Military Reservation, Cape Cod". In 16th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.190.ele04.

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Relatórios de organizações sobre o assunto "Massachusetts – Cape Cod"

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Whitmore, Jessica. Cape Cod National Seashore 2021 shorebird monitoring and management report. National Park Service, 2024. http://dx.doi.org/10.36967/2301299.

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Cape Cod National Seashore (CACO) manages the protection of federal and state listed beach-nesting shorebirds (piping plover [Charadrius melodus], least tern [Sternula antillarum], and American oystercatcher [Haematopus palliatus]), and various migrating shorebird species following procedures outlined in the 2018 Shorebird Management Plan/EA and associated Finding of No Significant Impact (FONSI) (NPS 2018), as well as the 2021 Biological Opinion. This report summarizes monitoring results from the 2021 field season. Piping plover, least tern, and American oystercatcher nesting and brood-rearing behaviors were monitored on over 43 miles of coastline from Provincetown to Orleans, Massachusetts.
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Campbell, David, William D. Ritchie, Stephanie Syler, David Kource, Stephen Mellin e Jeanette Bonito. Construct Troop Formation Center Environmental Assessment Cape Cod Air Force Station, Massachusetts. Fort Belvoir, VA: Defense Technical Information Center, setembro de 2005. http://dx.doi.org/10.21236/ada636783.

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John K. Steckel Jr. CLIMATE CHANGE FUEL CELL PROGRAM UNITED STATES COAST GUARD AIR STATION CAPE COD BOURNE, MASSACHUSETTS. Office of Scientific and Technical Information (OSTI), junho de 2004. http://dx.doi.org/10.2172/836828.

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Grant, Marcus, e Alan Hale. Stored Radioactive Material Landfill Site no. 7 (LF-7), Massachusetts Military Reservation, Cape Cod, MA. Fort Belvoir, VA: Defense Technical Information Center, março de 2013. http://dx.doi.org/10.21236/ada582303.

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Nikula, Blair, e Robert Cook. Status and distribution of Odonates at Cape Cod National Seashore. National Park Service, 2024. http://dx.doi.org/10.36967/2303254.

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Odonates are significant components of most wetland habitats and important indicators of their health. At Cape Cod National Seashore (CACO), we compiled odonate records dating back to the 1980s and, based partly on that data, identified 41 wetland sites for sampling, representing six freshwater habitats (kettle pond, inter-dune pond, dune slack, riparian marsh, vernal pool, and bog). We surveyed these sites for adult odonates during the 2016?2018 field seasons. Ten sites were surveyed all three years (total 19-20 surveys/site); all ten had at least some historical data. The remaining 31 sites were surveyed for one field season, a total of 6-8 times each. We conducted 391 surveys, recording 53,435 individuals and 74 species (45 dragonflies and 29 damselflies); not all individuals were identified to species. Abundance and species richness varied significantly between habitats. For all individuals recorded, abundance was greatest at vernal pools and kettle ponds. Riparian sites had the lowest abundance. Species richness was highest at kettle ponds, including several species of conservation concern, two listed as Threatened by the state of Massachusetts. Riparian marshes and dune slacks had relatively low richness. Among the 10 sites surveyed three years, we found significant annual variation in abundance and species richness. There was significant and generally greater between-site variation in abundance within a year than between years at sites. Community analysis found pond depth, habitat type, and presence of predaceous fish were significant factors explaining between-site variation in community composition. Habitats also differed significantly in community composition. Multidimensional scaling showed sites tend to cluster together by habitat type. Vernal ponds have the highest average community similarity to all other habitats (53.5%), with dune slack (52.9%), bog (52.0%) and inter-dune (51.5%) close behind. In contrast, riparian sites (46.3%) and kettle ponds (39.5%) are least similar to other habitats. Overall, 86 species of odonates have been recorded at CACO, a rich and diverse assemblage reflecting the variety and quality of freshwater habitats present. Although these habitats are relatively well-protected, stressors include climate change, nutrient inflow from adjacent development, road runoff, and trampling of emergent vegetation. A plan for monitoring is beyond the scope of this project. Ideally, it would be best to use the insight into odonate variation obtained from these surveys to develop a monitoring program designed to meet standards of statistical confidence and power currently employed in NPS monitoring programs.
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Ground-water resources of Cape Cod, Massachusetts. US Geological Survey, 1986. http://dx.doi.org/10.3133/ha692.

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Hydrogeologic framework of western Cape Cod, Massachusetts. US Geological Survey, 1997. http://dx.doi.org/10.3133/ha741.

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Delineation of groundwater recharge areas, western Cape Cod, Massachusetts. US Geological Survey, 2000. http://dx.doi.org/10.3133/wri004000.

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Geologic map of Cape Cod and the Islands, Massachusetts. US Geological Survey, 1986. http://dx.doi.org/10.3133/i1763.

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Distribution and Structure of Holocene Sediments in Cape Cod Bay, Massachusetts. US Geological Survey, 2002. http://dx.doi.org/10.3133/i2729.

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