Bibliografías temáticas / Assateague Island

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Literatura académica sobre el tema "Assateague Island"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 1 de febrero de 2022

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Artículos de revistas sobre el tema "Assateague Island"

1

Johnson, Joshua B. y J. Edward Gates. "Bats of Assateague Island National Seashore, Maryland". American Midland Naturalist 160, n.º 1 (julio de 2008): 160–70. http://dx.doi.org/10.1674/0003-0031(2008)160[160:boains]2.0.co;2.

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Stalter, Richard y Eric E. Lamont. "The Vascular Flora of Assateague Island, Virginia". Bulletin of the Torrey Botanical Club 117, n.º 1 (enero de 1990): 48. http://dx.doi.org/10.2307/2997128.

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Patterson, Michael E., James D. Fraser y Joseph W. Roggenbuck. "Factors Affecting Piping Plover Productivity on Assateague Island". Journal of Wildlife Management 55, n.º 3 (julio de 1991): 525. http://dx.doi.org/10.2307/3808985.

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Leatherman, Stephen P. "Storm-Generated Overwash Processes at Assateague Island, Maryland". Journal of Coastal Research 101, sp1 (26 de agosto de 2020): 48. http://dx.doi.org/10.2112/jcr-si101-011.1.

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RUDMAN, REBECCA y R. R. KEIPER. "The body condition of feral ponies on Assateague island". Equine Veterinary Journal 23, n.º 6 (noviembre de 1991): 453–56. http://dx.doi.org/10.1111/j.2042-3306.1991.tb03760.x.

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Brock, John C., William B. Krabill y Asbury H. Sallenger. "Barrier Island Morphodynamic Classification Based on Lidar Metrics for North Assateague Island, Maryland". Journal of Coastal Research 202 (abril de 2004): 498–509. http://dx.doi.org/10.2112/1551-5036(2004)020[0498:bimcbo]2.0.co;2.

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Sullivan, Kristin. "Exploring Traditional Use and Association Through the Ethnographic Overview and Assessment for Assateague Island National Seashore". Practicing Anthropology 34, n.º 3 (29 de junio de 2012): 44–46. http://dx.doi.org/10.17730/praa.34.3.d953g6x8qx26812m.

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Assateague, a dynamic barrier island extending from just south of Ocean City, Maryland, to the northern portions of Virginia's eastern shore, was added to the National Park Service (NPS) system in 1965 (Mackintosh 1982) and now draws roughly 2 million visitors per year (Bentley 2008). Prior to the Seashore's establishment, however, the island and its environs drew a range of people from fishermen to land developers. While today's Eastern Shore communities continue many of their traditional lifeways related to the island, they now share its resources with tourists from around the world who are drawn to the seeming pristine beaches and famed wild ponies, managed today by two federal agencies (NPS and United States Fish and Wildlife Service [USFWS]).
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Houser, Chris, Brian Labude, Lars Haider y Bradley Weymer. "Impacts of driving on the beach: Case studies from Assateague Island and Padre Island National Seashores". Ocean & Coastal Management 71 (enero de 2013): 33–45. http://dx.doi.org/10.1016/j.ocecoaman.2012.09.012.

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Schupp, Courtney A., Neil T. Winn, Tami L. Pearl, John P. Kumer, Tim J. B. Carruthers y Carl S. Zimmerman. "Restoration of overwash processes creates piping plover (Charadrius melodus) habitat on a barrier island (Assateague Island, Maryland)". Estuarine, Coastal and Shelf Science 116 (enero de 2013): 11–20. http://dx.doi.org/10.1016/j.ecss.2012.07.003.

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Grybas, Heather y Russell Congalton. "Land Cover Change Image Analysis for Assateague Island National Seashore Following Hurricane Sandy". Journal of Imaging 1, n.º 1 (5 de octubre de 2015): 85–114. http://dx.doi.org/10.3390/jimaging1010085.

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Tesis sobre el tema "Assateague Island"

1

Patterson, Michael E. "Piping plover breeding biology and reproductive success on Assateague Island". Thesis, Virginia Tech, 1988. http://hdl.handle.net/10919/43276.

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I studied the piping plover on Assateague Island during the 1986 and 1987 breeding seasons. In 1987, I estimated the population to be 69 pairs. During both years, plovers nested on only a few portions of the island. I think that this pattern of nesting was determined by the distribution of three types of foraging habitats: bayside mud and sand flats, saltwater pools formed by storm tides, and a drawn down waterfowl impoundment. Reproductive rates were lower than two recent estimates of the level necessary to maintain a stable population. The primary problem was poor nest success and the leading cause of nest loss was nest predation by red foxes (Vulpes vulpes) and raccoons (Procyon Iotor). I was not able to identify factors responsible for chick mortality, but my data show a relationship between chick survival and foraging habitat. Broods feeding on bayside foraging areas had a much higher survival rate than broods which did not have access to these areas. Management efforts should focus on reducing nest predation. Recent experiments have indicated that predator exclosures constructed around individual nests can be used to reduce nest predation. These exclosures should be tested on Assateague. Future research efforts should focus on the role of foraging habitat in breeding site selection and the relationship between chick survival and the type of foraging used.
Master of Science
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2

Seminack, Christopher Thomas. "Reconstruction of a Relict Inlet System and Historical Storm Signatures along Southern Assateague Island, Maryland". Master's thesis, Temple University Libraries, 2011. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/142364.

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Geology
M.S.
Assateague Island is a classic example of a retrograding barrier island, with its recent geological history punctuated by episodes of overwash and breaching. However, in addition to a number of historical inlets, parts of the island owe their origin to relict (pre-historic) channels. The present study was conducted north of the Virginia-Maryland border, focusing on a narrow segment of the island fronting the Green Run Bay. The site lies north of the historical Green Run Inlet that was active until 1880; however, there is no geological evidence of its migration along the island. More than 4 km of high-resolution (250 MHz) ground-penetrating radar (GPR) images, complemented with sediment cores and multi-dating techniques, were used to reconstruct the geological legacy of the Green Run Bay segment of the barrier and to test whether it was the site of an older channel. My findings indicate that a backbarrier paleo-channel still visible within the Green Run Bay corresponds to a large (>380 m wide, 3.0-3.5 m thick) channel cut-and-fill structure revealed in GPR images. The channel fill consists of tangential- to sigmoidal-oblique, southward-dipping reflections downlapping onto channel lag facies, which overlie subhorizontal bay-fill strata. Hummocky reflections in a shore-normal channel transect suggest partial preservation of inlet-related bedforms, believed to be associated with the channel closure. Mollusk shells from the bay fill yield radiocarbon ages of 4630-2400 cal BP (calibrated years before 1950). The paleo-channel facies overlying the bay deposits exhibit a fining-upward sequence, with a mean grain size range of 0.44-2.43 phi. The first set of optical dates indicates that the inlet fill is 660 +/- 70 cal BP (AD 1220-1360). The paleo-channel fill does not extend to the south and therefore is a separate relict feature that predates the historical Green Run Inlet. Based on geophysical and core data, the paleo-tidal prism of the relict channel is 17x10 6 m3. Following the closure of the inlet, a series of beach ridges have developed across the Green Run Bay segment and exhibit signatures of storm erosion in shore-normal GPR profiles. This punctuated barrier progradation took place during the historical period (post-1600), with optical dates of beach ridge and dune generations ranging from AD 1680 to 1920. In addition to geological evidence, dendrochronological records were examined for occurrences of abrupt thinning of tree rings as a proxy for intense environmental stress. Tree samples that exceed 50 years in age (n=7) display an abrupt ring thinning in 1962 that coincides with the Ash Wednesday extra-tropical storm of record. This study demonstrates that the historical stability of the Green Run Bay segment of Assateague Island is likely due to the influx and preservation of substantial sand volume related to a relict tidal inlet.
Temple University--Theses
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Loegering, John P. "Piping plover breeding biology, foraging ecology and behavior on Assateague Island National Seashore, Maryland". Thesis, This resource online, 1992. http://scholar.lib.vt.edu/theses/available/etd-09052009-040402/.

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Fauver, Laura A. "Toward predicting barrier island vulnerability simple models for dune erosion /". [Tampa, Fla.] : University of South Florida, 2005. http://purl.fcla.edu/fcla/etd/SFE0001055.

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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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Gieder, Katherina Dominique. "Assessing the Effects of Sea-Level Rise on Piping Plover (Charadrius Melodus) Nesting Habitat, and the Ecology of a Key Mammalian Shorebird Predator, on Assateague Island". Diss., Virginia Tech, 2015. http://hdl.handle.net/10919/56573.

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The piping plover (Charadrius melodus) is a federally-listed shorebird that nests on barrier islands along the U.S. Atlantic Coast and is highly vulnerable to habitat change and predation. We have addressed these two threats by 1) developing and implementing a linked model system that predicts future change to piping plover habitat resulting from sea-level rise and beach management efforts by joining dynamic models of sea-level rise, shoreline change, island geomorphology and piping plover nest habitat suitability, and 2) quantifying occupancy and movement of the red fox (Vulpes vulpes), a key shorebird predator at Assateague Island, Maryland and Virginia. We constructed and tested a model that links changes in geomorphological characteristics to piping plover nesting habitat suitability. We then linked this model to larger scale shoreline change resulting from sea level rise and storms. Using this linked model to forecast future sea-level rise and beach management efforts, we found that modest sea-level rise rates (3 mm and 4.1 mm/yr; similar to current rates) may increase suitable piping plover nesting habitat area in 50-100 years and some beach management strategies (beach nourishment and artificial dune modifications) also influence habitat availability. Our development and implementation of this tool to predict change in piping plover habitat suitability provides a vital starting point for predicting how plover nesting habitat will change in a context of planned human modifications intended to address climate change-related threats. Our findings regarding red fox occupancy and movement complement the use of this model for planning future management actions by providing vital information on the effects of certain predator management activities and habitat use of a key mammalian predator, the red fox, for shorebirds along the U.S. Atlantic Coast. Overall, we found that 1) red fox occupancy was strongly tied to eastern cottontail (Sylvilagus floridanus) trap success, increasing sharply with increased eastern cottontail trap success, 2) red fox occupancy did not change in response to an intensive eradication program, and 3) red foxes in our study area generally moved little between camera stations spaced 300 m from each other, but may move large distances (> 6km) at times, likely to occupy new territory available after lethal control efforts. Our findings have important ramifications for the sustainability of long-term predator removal programs and our understanding of future habitat change on the red fox. For example how vegetation changes affect eastern cottontails, how resulting fluctuations in eastern cottontails affect red fox occupancy, and how consequential changes in red fox occupancy affect plover breeding productivity. Our predictive model combined with these predator findings will allow wildlife managers to better plan and implement effective management actions for piping plovers in response to the multiple stressors of SLR-induced habitat change and predation.
Ph. D.
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7

Wikel, Geoffrey L. "Variability in Geologic Framework and Shoreline Change: Assateague and Wallops Islands, Eastern Shore of Virginia". W&M ScholarWorks, 2008. https://scholarworks.wm.edu/etd/1539617877.

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Shroyer, William James. "Resolution assessment and spatial characterization of airborne LIDAR data Assateague island national seashore /". 2004. http://www.lib.ncsu.edu/theses/available/etd-04132004-131135/unrestricted/etd.pdf.

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Labude, Brian. "Off-Road Vehicle Impact on Sediment Displacement and Disruption at Assateague Island National Seashore, Maryland". Thesis, 2012. http://hdl.handle.net/1969.1/148076.

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The National Park Service (NPS) monitors off-road vehicle (ORV) use in National Seashores across the United States. The sediment disturbance that is caused by ORVs is believed to have a large impact on erosion (by wind or waves), which there by affects the morphology of the foredunes. With greater knowledge of ORV impacts, the NPS can better manage ORV use and minimize anthropogenic affects to the coastal environment. There remains considerable uncertainty about the disturbance and its larger-scale impact. This study quantifies the sediment disturbance made by tire tracks, as well as the tire track form, width, depth, and evolution with relation to the number of vehicle passes and location on the beach at Assateague Island National Seashore (ASIS), Maryland. To measure ORV impact, ground-based LiDAR was used to collect detailed profiles across a three by three meter test plot at each site. Based on the quantification of the displaced sediment and redistribution of that sediment from the tracks, a recommendation to the NPS can be made as to where along the beach traffic should be limited to, in order to minimize impact to the physical environment at ASIS. Tire tracks were found to widen after the first pass, as a result of the imperfections of driving. Compaction of the sediment in the center of the tire track accounts for only a minimal amount of the sediment lost from the tire tracks. Sediment removal accounted for greater than 75% of the sediment lost from the tire tracks at all sites. It was concluded that sediment removal is the most dominant factor in the creation and evolution of a tire track. The width, depth, and evolution of a tire track were also found to be controlled by the imperfections of driving. Despite the amount of sediment disturbance, it is found that there is no net downslope displacement of sediment. This conclusion counters previous ORV impact studies and suggests that ORVs are not directly responsible for beach erosion. It is also recommended that to minimize the impact of OVRs on the beach at ASIS, the NPS should limit driving to the backshore.
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10

Ingle, Margaret Christine. "The development and testing of a procedure for monitoring visitor-horse interactions at Assateague Island national seashore". 2004. http://www.lib.ncsu.edu/theses/available/etd-03182004-205956/unrestricted/etd.pdf.

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Libros sobre el tema "Assateague Island"

1

Cherrix, Myrna J. Assateague Island. Charleston, S.C: Arcadia Pub., 2011.

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Georgie of Assateague: An Assateague Island story. Ocean Shores, Wash: Seachase Books, 1992.

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Minetor, Randi. Assateague Island National Seashore pocket guide. Guilford, Conn: Falcon Guides, 2010.

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Larry, Points, ed. Assateague: Island of the wild ponies. New York: Macmillan, 1993.

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Chambers, Erve. Ethnographic overview and assessment: Assateague Island National Seashore. Boston, MA: Northeast Region Ethnography Program, National Park Service, 2013.

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P, Masterson John, Johnson Carole D, Climate and Land Use Change Research Development Program (U.S.) y Geological Survey (U.S.), eds. Well network installation and hydrogeologic data collection, Assateague Island National Seashore, Worcester County, Maryland, 2010. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2012.

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Dillow, Jonathan J. A. Ground-water quality and discharge to Chincoteague and Sinepuxent Bays adjacent to Assateague Island National Seashore, Maryland. Baltimore, Md: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Dillow, Jonathan J. A. Ground-water quality and discharge to Chincoteague and Sinepuxent Bays adjacent to Assateague Island National Seashore, Maryland. Baltimore, Md: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Dillow, Jonathan J. A. Ground-water quality and discharge to Chincoteague and Sinepuxent Bays adjacent to Assateague Island National Seashore, Maryland. Baltimore, Md: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Dillow, Jonathan J. A. Ground-water quality and discharge to Chincoteague and Sinepuxent Bays adjacent to Assateague Island National Seashore, Maryland. Baltimore, Md: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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Capítulos de libros sobre el tema "Assateague Island"

1

Hayden, Bruce P. "Networking: From the Long-Term Ecological Research Program to the National Ecological Observatory Network". En Long-Term Ecological Research. Oxford University Press, 2016. http://dx.doi.org/10.1093/oso/9780199380213.003.0062.

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As a scientist, the Long-Term Ecological Research (LTER) program has been on my mind for more than three decades. As an educator, I have served in the classroom for 41 years. The merger of the physical and the ecological sciences was at the core of my teaching philosophy. As a science communicator, I informed the general public on issues of climate and climate change. As a collaborator, I found that understanding strengths and weaknesses in collaborative partnerships best ensures success. As a science leader, I served at the National Science Foundation (NSF) as the Director of the Division of Environmental Biology (DEB), established the Schoolyard LTER Program, and launched the National Ecological Observatory Network (NEON). My disciplinary background includes formal graduate education at the University of Wisconsin in meteorology, climatology, and paleoclimatology, as well as in oceanography and biology (mycology, botany, zoology, and genecology). As a postdoctoral fellow, my scientific identity was on track to culminate as a paleoclimatologist. As an assistant and associate professor, my identity morphed to include coastal geomorphology (Hayden et al. 1995). Finally, my experiences in the LTER program have vectored my career toward the interactions of climate and vegetation (Hayden 1998). My affiliation is with the Virginia Coast Reserve (VCR) site in the LTER program (1986–2014). As one of the founding principal investigators of the VCR site, I have served in subsequent renewals as its principal or co-principal investigator. Our site-based research plan focused on the Virginia Coast Reserve on Virginia’s eastern shore with a focus on the dynamics of the chain of 14 barrier islands, bounded by the entrance to the Chesapeake Bay to the south and Assateague Barrier Island to the north. This peninsula is 100 km in length by 20 km in width. Only the islands fronting the Mississippi delta are more dynamic in both the temporal and spatial domains. Prior to joining the LTER program, my research was hemispheric to regional in scope, and it focused on the environmental dynamics of the Atlantic Coast from Florida to Cape Cod at 50-m intervals (Fenster and Hayden 2007).
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Actas de conferencias sobre el tema "Assateague Island"

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Schupp, Courtney A., Gregory P. Bass y William G. Grosskopf. "Sand Bypassing Restores Natural Processes to Assateague Island, Maryland". En Sixth International Symposium on Coastal Engineering and Science of Coastal Sediment Process. Reston, VA: American Society of Civil Engineers, 2007. http://dx.doi.org/10.1061/40926(239)103.

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Obara, Chloe A., Justin L. Shawler, Jennifer E. Connell y Christopher J. Hein. "SPIT ELONGATION AS A CONTROL ON DOWNDRIFT BARRIER-ISLAND STABILITY- INSIGHTS FROM ASSATEAGUE ISLAND, VA". En Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344286.

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Milinic, Bojan, Brandon Sutter, Sarah Moriarty, Adrienne Oakley, Sean Cornell y Christopher Bochicchio. "INVESTIGATING BARRIER ISLAND EVOLUTION THROUGH STRATIGRAPHIC ANALYSIS OF VIBRACORES FROM ASSATEAGUE AND CHINCOTEAGUE ISLANDS, VA". En 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-311358.

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Wirth, Hannah S. y Neil Winn. "COASTAL TOPOGRAPHY DATA ANALYSIS AND VISUALIZATION AT ASSATEAGUE ISLAND NATIONAL SEASHORE". En GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359996.

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Fenster, Michael S., Brian Rizzo y John McManus. "NON-LINEAR SHORELINE CHANGE MODELING OF THE NORTHERN VIRGINIA COAST: VIRGINIA BARRIER ISLANDS AND ASSATEAGUE ISLAND". En 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-291183.

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Coffey, Ruth, Hannah Sprinkle, Eric Sherry, Brian Sturgis y Bill Hulslander. "SPATIAL AND TEMPORAL PATTERNS OF GROUNDWATER ELEVATION AND SALINITY ON ASSATEAGUE ISLAND". En GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283459.

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Moriarty, Sarah N., Casey L. Michalowski, Adrienne J. Oakley, Sean R. Cornell, Christopher Bochicchio, Laura A. Sherrod, Adam T. Cooper y Nicole C. DeLong. "INVESTIGATING BARRIER ISLAND EVOLUTION AND INLET FORMATION THROUGH STRATIGRAPHIC ANALYSIS OF VIBRACORES TAKEN FROM ASSATEAGUE AND CHINCOTEAGUE ISLANDS, VA". En GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287693.

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Sutter, Brandon, Bojan Milinic, Sarah Moriarty, Adrienne Oakley, Sean Cornell, Laura A. Sherrod, Christopher Bochicchio y Adam T. Cooper. "GEOPHYSICAL AND STRATIGRAPHIC INVESTIGATION OF ASSATEAGUE ISLAND, VIRGINIA: UNRAVELING THE EVOLUTION OF THE ONLY MID-ATLANTIC DUPLEXED BARRIER ISLAND SYSTEM". En 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-311182.

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Schulte, Amanda, Robert Domeyko, Darryl Hoppe, Christopher T. Seminack y Randolph A. McBride. "A COMPARISON OF MULTIPLE TIDAL INLET AND BREACH FILL TRENDS ALONG ASSATEAGUE ISLAND, MD-VA: A WAVE-DOMINATED BARRIER ISLAND". En GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287973.

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Silveira Meyers, Joao, Sean Cornell y Adrienne Oakley. "CHARACTERIZING MAGNETIC SUSCEPTIBILITY SIGNATURES OF MODERN BARRIER ISLAND AND BACK BARRIER DEPOSITIONAL ENVIRONMENTS FROM ASSATEAGUE, CHINCOTEAGUE, AND WALLOPS ISLANDS, VIRGINIA". En GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-324453.

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Informes sobre el tema "Assateague Island"

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Haulsee, K. Quantifying macro-scale geomorphological changes post-Hurricane Sandy and Hurricane Joaquin at Assateague Island utilizing bathymetric mapping techniques. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/305856.

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Ground-water quality and discharge to Chincoteague and Sinepuxent Bays adjacent to Assateague Island National Seashore, Maryland. US Geological Survey, 2002. http://dx.doi.org/10.3133/wri024029.

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