Relevant bibliographies by topics / Northeastern North America

Contents

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

Academic literature on the topic 'Northeastern North America'

Author: Grafiati
Published: 4 June 2021
Last updated: 13 February 2022

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Journal articles on the topic "Northeastern North America"

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Zack, Richard S. "Freshwater Macroinvertebrates of Northeastern North America." American Entomologist 37, no. 4 (1991): 247. http://dx.doi.org/10.1093/ae/37.4.247.

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Frank, J. H., N. M. Downie, and R. H. Arnett. "The Beetles of Northeastern North America." Florida Entomologist 79, no. 3 (September 1996): 471. http://dx.doi.org/10.2307/3495601.

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Smith, Douglas, and Paula Martin. "Freshwater Macroinvertebrates of Northeastern North America." Transactions of the American Fisheries Society 120, no. 1 (January 1, 1991): 130–32. http://dx.doi.org/10.1577/1548-8659-120.1.130.

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Lavitt, Tate H., and David L. Wagner. "A New CrypticEupsiliafrom Northeastern North America (Noctuidae)." Journal of the Lepidopterists’ Society 70, no. 3 (August 2016): 238–48. http://dx.doi.org/10.18473/107.070.0310.

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Brothers, Timothy S. "Postsettlement Plant Migrations in Northeastern North America." American Midland Naturalist 128, no. 1 (July 1992): 72. http://dx.doi.org/10.2307/2426414.

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Lothrop, Jonathan C., Darrin L. Lowery, Arthur E. Spiess, and Christopher J. Ellis. "Early Human Settlement of Northeastern North America." PaleoAmerica 2, no. 3 (July 2, 2016): 192–251. http://dx.doi.org/10.1080/20555563.2016.1212178.

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Hough, S. E., K. H. Jacob, and L. Seeber. "High-Frequency Seismic Wave Propagation in Northeastern North America." Seismological Research Letters 61, no. 3-4 (July 1, 1990): 193–208. http://dx.doi.org/10.1785/gssrl.61.3-4.193.

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Abstract A key element in the assessment of seismic hazard is the estimation of how energy propagation from a given earthquake is affected by crustal structure near the receiver and along the more distant propagation path. In this paper, we present data from a variety of sources in eastern North America recorded at epicentral distances of a few to 800 km, and characterize and interpret systematic features. Site effects have been classically considered in terms of amplification either within a sediment-filled valley or from a single topographic feature (Geli et al., 1988). We present evidence of high frequency (5–30 Hz) resonances observed in hard-rock recordings of both body waves and Lg waves, and suggest that site effect should be expanded regionally to include structural and topographic information over sufficiently large areas to include several wavelengths of any features that may interact with seismic waves in the frequency range of interest. A growing body of evidence suggests that ground motions at high frequencies recorded at large epicentral distances in eastern North America are controlled by resonance effects. We hypothesize that a fundamental difference between eastern and western North America spectra stems from a combination of differences in the character of topography and near-surface structure. Active tectonics of western North America gives rise to a complex crust that scatters seismic energy in a random manner and results in very effective attenuation of high frequencies. The older eastern North American crust contains scatterers that are more ordered, with characteristic length scales that give rise to resonance phenomena in the frequency band critical for earthquake hazard. We present preliminary analysis of topographic data from the Adirondack Mountains in New York that demonstrates the existence of characteristic length scales on the order of up to 1–3 kilometers. Features with these length scales will effectively scatter energy at frequencies in the 1 to 10 Hz range.
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Grise, Kevin M., Seok-Woo Son, and John R. Gyakum. "Intraseasonal and Interannual Variability in North American Storm Tracks and Its Relationship to Equatorial Pacific Variability." Monthly Weather Review 141, no. 10 (September 25, 2013): 3610–25. http://dx.doi.org/10.1175/mwr-d-12-00322.1.

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Abstract Extratropical cyclones play a principal role in wintertime precipitation and severe weather over North America. On average, the greatest number of cyclones track 1) from the lee of the Rocky Mountains eastward across the Great Lakes and 2) over the Gulf Stream along the eastern coastline of North America. However, the cyclone tracks are highly variable within individual winters and between winter seasons. In this study, the authors apply a Lagrangian tracking algorithm to examine variability in extratropical cyclone tracks over North America during winter. A series of methodological criteria is used to isolate cyclone development and decay regions and to account for the elevated topography over western North America. The results confirm the signatures of four climate phenomena in the intraseasonal and interannual variability in North American cyclone tracks: the North Atlantic Oscillation (NAO), the El Niño–Southern Oscillation (ENSO), the Pacific–North American pattern (PNA), and the Madden–Julian oscillation (MJO). Similar signatures are found using Eulerian bandpass-filtered eddy variances. Variability in the number of extratropical cyclones at most locations in North America is linked to fluctuations in Rossby wave trains extending from the central tropical Pacific Ocean. Only over the far northeastern United States and northeastern Canada is cyclone variability strongly linked to the NAO. The results suggest that Pacific sector variability (ENSO, PNA, and MJO) is a key contributor to intraseasonal and interannual variability in the frequency of extratropical cyclones at most locations across North America.
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Behan-Pelletier, Valerie M. "LIMNOZETES (ACARI: ORIBATIDA: LIMNOZETIDAE) OF NORTHEASTERN NORTH AMERICA." Canadian Entomologist 121, no. 6 (June 1989): 453–506. http://dx.doi.org/10.4039/ent121453-6.

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AbstractThe species of Limnozetes of northeastern North America are treated. A new generic diagnosis is given. Eight new species are described: L. latilamellata, L. guyi, L. borealis, L. onondaga, L. amnicus, and L. palmerae on the basis of adults and immatures, and L. lustrum and L. atmetos on the basis of adults. Identification of adults and immatures of these species is presented in tabular format. The range of morphological variation exhibited by these species is discussed. Transformation series for eight character states in Limnozetes are hypothesized on the basis of comparison with Hydrozetes. A key is given to the adults of the nine species of Limnozetes recorded from northeastern North America.
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Wolff, S. L., and R. L. Jefferies. "Taxonomic status of diploid Salicornia europaea (s.l.) (Chenopodiaceae) in northeastern North America." Canadian Journal of Botany 65, no. 7 (July 1, 1987): 1420–26. http://dx.doi.org/10.1139/b87-196.

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The taxonomic status of diploid Salicornia europaea L. (s.l.) in northeastern North America has been evaluated based on morphological and electrophoretic variation within and between populations. Populations of two European diploid micro-species, S. ramosissima J. Woods and S. europaea (s.s.), and populations of the midwestern diploid, S. rubra A. Nels., were also examined, affording a comparison between North American S. europaea (s.l.) and recognized species. Anther length, width of the scarious border of the fertile segment, and floral perianth shape were used to subdivide North American diploid populations into two groups. These groups were morphologically distinct from S. rubra and the European microspecies. The electrophoretic profile was unique in each morphologically distinct group of populations of S. europaea (s.l.) in northeastern North America. Based on morphological, geographical, and electrophoretic differences, diploid populations of S. europaea (s.l.) from this region are assigned to one of the following two new species: S. maritima Wolff & Jefferies, sp.nov., and S. borealis Wolff & Jefferies, sp.nov. The tetraploids are retained in S. europaea (s.l.).
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Dissertations / Theses on the topic "Northeastern North America"

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Miles, William R. "The Royal Navy and northeastern North America, 1689-1713." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ56715.pdf.

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Hertzog, Justin Tyler. "The Upper Mantle Seismic Structure Beneath Northeastern North America." Thesis, Boston College, 2013. http://hdl.handle.net/2345/3401.

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Thesis advisor: John E. Ebel
Thesis advisor: John C. Hepburn
Using the seismic refraction technique with a least squares inversion methodology, arrival time data from 1985 to the present are analyzed to delineate, with improved spatial resolution, the upper mantle P-velocity structure throughout northeastern North America (NENA). A total of one hundred and sixty-eight earthquakes are analyzed utilizing over one hundred seismic stations throughout NENA. Seismic data analyzed between 200 - 400 km, 400 - 600 km, and 600+ km throughout NENA are used to study the increase in velocity with depth in the upper mantle. A jackknife analysis was carried out to put constraints on the uncertainties of the velocity measurements. The P-wave velocity of the upper mantle through the New England Appalachians is found to be uniformly 7.94 - 8.07 km/s at depths down to 75 km. Upper mantle Pn velocities throughout the southeastern Grenville Province show velocities ranging from 8.15 km/s to 8.54 km/s as epicentral distances increase. Uncertainties of P velocities range from 0.01- 0.12 km/s. Based on laboratory measurements of simulated upper mantle conditions and the orogenic history of the Grenville Province and northern Appalachians, upper mantle mineral compositions of eclogite (Grenville Province) and pyroxenite (northern Appalachians) are proposed to be the factor controlling seismic velocity variation in the upper mantle. Variations in upper mantle temperatures between the Grenville Province and northern Appalachians are ruled out as affecting the difference in upper mantle velocities between southeastern Canada and New England
Thesis (MS) — Boston College, 2013
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Geology and Geophysics
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Fortin, David. "Paleoclimatic and instrumental records of environmental variability in northeastern North America." Kingston, Ont. : [s.n.], 2008. http://hdl.handle.net/1974/1636.

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Shook, Beth Alison Schultz. "Ancient DNA and the biological history and prehistory of northeastern North America /." For electronic version search Digital dissertations database. Restricted to UC campuses. Access is free to UC campus dissertations, 2005. http://uclibs.org/PID/11984.

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Vermaire, Jesse. "Reconstructing macrophyte biomass dynamics in temperate lakes of northeastern North America using paleolimnology." Thesis, McGill University, 2011. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=97004.

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Submerged macrophytes are known to influence the structure and function of lake ecosystems. Despite their importance, long term monitoring records of macrophytes are rare and thus relatively little is know regarding how human activities have altered macrophyte abundance in lakes. Paleolimnological reconstructions may provide the best approach for examining long-term trends in macrophyte abundance. This thesis evaluates the potential of sedimentary diatoms as indicators of macrophyte abundance and examines the long-term effects of human activities on ecosystem stability and macrophyte abundance. A novel analysis of an existing dataset showed that there were significant differences in the sedimentary diatom assemblage of lakes with either high or low macrophyte cover, and that these differences in the diatom assemblages can be used to infer the macrophyte cover of lakes. I further examined the influence of macrophytes on diatoms using a continuous measure of whole-lake macrophyte biomass in 41 lakes located in southern Quebec, Canada, and showed that diatoms can be used to detect substantial changes in macrophyte abundance through time. An analysis of the effects of external phosphorus (P) inputs to the lake showed that increasing P inputs resulted in greater diatom dissimilarity through time, providing empirical evidence for the idea that P inputs increase ecosystem variability. Finally, I show a widespread trend of a relative reduction in benthic diatoms and an inferred decline in macrophyte abundance between pre-1850 and present-day conditions, which is significantly related to modern land use. Together, this thesis advances our ability to track long-term changes in macrophyte abundance and demonstrates that human activities over the past ~150 years have altered ecosystem stability and reduced macrophyte abundance in southern Quebec lakes.
Les macrophytes submergées influencent la structure et les fonctions des écosystèmes lacustres. Étant donné que les programmes de surveillance à long terme (décennie ou plus) des macrophytes sont rares, l'impact des activités humaines sur l'abondance des macrophytes dans les lacs est relativement peu connu. La reconstruction paléolimnologique pourrait être la meilleure approche pour examiner les tendances à long terme de l'abondance des macrophytes. Cette thèse évalue le potentiel des diatomées sédimentaires comme indicateur de l'abondance des macrophytes et examine les effets à long terme des activités humaines sur la stabilité des écosystèmes et sur l'abondance des macrophytes. Une nouvelle analyse d'un jeu de donnée existant a montré qu'il y a une différence significative entre les assemblages des diatomées sédimentaires de lacs ayant de faibles ou de larges couvertures de macrophytes. Ces différences d'assemblage peuvent être utilisées afin d'inférer la couverture de macrophytes dans les lacs. Par la suite, j'ai examiné l'influence des macrophytes sur les diatomées en utilisant une mesure continue de la biomasse du lac total de macrophyte pour 41 lacs situés dans le sud du Québec, Canada. Cette étude a montré que les diatomées peuvent être utilisées pour détecter des changements substantiels dans l'abondance des macrophytes à travers le temps. Une analyse de l'effet des apports externes en phosphore (P) aux lacs a montré que l'augmentation des apports en P résulte en un accroissement de la dissimilarité des diatomées dans le temps, ce qui fourni une preuve empirique que les apports en P augmentent la variabilité des écosystèmes. Finalement, je montre la tendance répandue de la réduction relative des diatomées benthiques et le déclin inféré de l'abondance des macrophytes entre les conditions d'avant 1850 et de nos jours, ce qui est significativement relié à l'utilisation du territoire moderne. En résumé, cette thèse fournie une nouvelle méthode pour retracer les changements à long terme de l'abondance des macrophytes et démontre que les activités humaines des quelques 150 dernières années ont altéré la stabilité des écosystèmes et réduit l'abondance des macrophytes dans les lacs du Sud du Québec.
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Triplett, Linda A. (Linda Ann). "A radiocarbon assessment of the projectile point typology for the archaic period of the Northeast of North America /." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65554.

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Baker, Martha C. "Defining the relationship of self-care agency to spirituality and cultural affiliation in Northeastern Oklhoma [sic] native American and Euro-American groups." free to MU campus, to others for purchase, 1999. http://wwwlib.umi.com/cr/mo/fullcit?p9946240.

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Allitt, Sharon. "STABLE ISOTOPIC INSIGHTS INTO THE SUBSISTENCE PATTERNS OF PREHISTORIC DOGS (CANIS FAMILIARIS) AND THEIR HUMAN COUNTERPARTS IN NORTHEASTERN NORTH AMERICA." Diss., Temple University Libraries, 2011. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/136922.

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Anthropology
Ph.D.
There are four goals to this study. The first is to investigate the diet of prehistoric dogs (Canis familiaris) in the Northeast region of North America using stable isotope analysis. The second goal of this study is to generate independent data concerning the presence or absence of C4 resources, such as maize, in the diets of dogs. Third, this study investigates the use of dog bone as a proxy for human bone in studies assessing the presence of C4 resources at archaeological sites. The fourth goal of this study is to provide a check on existing interpretations of the material, macro- and micro-botanical records as it concerns the presence or absence of C4 resources at the sites involved in this study. Stable isotope analysis is a science that allows the measuring of the abundance ratio of two stable isotopes of a particular element. Stable isotope analysis can differentiate C4 and C3 plants, as well as terrestrial and marine resources in material such as bone where the chemistry of diet becomes recorded. Given the importance of C4 plants to many prehistoric populations, in the absence of direct evidence identifying their presence at archaeological sites, an alternate method for identification is needed. Maize played an important role in changing human behaviors during prehistory including: decisions to increase sedentism, abuse of power structures, and stratification of gender roles within human populations. Additionally, an overall decrease in health is seen in prehistoric populations who focused their subsistence practices on maize. Dogs were chosen as the focus of this study because related research suggests that their diet tends to mimic human diet. Prehistoric dogs were scavengers, but they were also intentionally fed companions. The suggestion that dog diet in some way mimics human diet means that stable isotope ratios from their bone will reflect the type of resources available for consumption by their human counterparts. As such, this investigation may also indirectly inform on the diets of the American Indian inhabitants of the settlements in which these dog remains originate. Thirty samples of dog bone, dating from the Early Ceramic Period, ca. 3000 B.P. to the Late Woodland and Early Historic Period, were obtained from museum and personal collections, and from ongoing archaeological excavations throughout the Northeast region of North America. Stable isotope analysis was conducted at Notre Dame's Center for Environmental Science and Technology. The results of this analysis indicates that these prehistoric dogs consumed the types of resources represented in the archaeological record with one important exception: consumption of C4 resources, possibly maize, was occurring at several sites where no other evidence of C4 exploitation exists. Of the dogs sampled ten were from pre-agricultural sites in Maine and their stable isotope ratios indicated a diet of marine and terrestrial resources. Nineteen dogs were excavated from components dating to the Late Woodland or Historic Period. During the Late Woodland and Historic Period the C4 plant maize was exploited by many human groups in the study region. Interpretation based on stable isotopes from bone collagen indicates that six of these dogs had isotopic signatures within the range of significant C4 resource consumption. Stable isotope ratios from the remaining dogs indicate a smaller contribution of C4 resources to diet. According to 13C ratios from carbonate three dogs, two from New Jersey (DB2, DB8) and one from Maryland (DB11), had a significant C4 plant component to their diet. The remaining Late Woodland and Historic period dogs most likely consumed minor amounts of C4 resources. In addition to identifying C4 resources in the diet of dogs, the value of assessing isotope data from both collagen and carbonate is investigated. The sample size for this study was small in comparison to the size of the region assessed. Despite the small sample size, this analysis contributes to our knowledge of past dog and human subsistence patterns. Our understanding of the utility of stable isotope studies of human companion species has also expanded. In addition to investigating the presence of C4 resources in the diet of prehistoric dogs, this research provides an alternate line of inquiry to re-assess current interpretations, especially in areas where direct evidence of isotopically identifiable C4 plants, such as maize are currently lacking. The results of this study are applicable first and foremost to the consumption patterns of the individual animals sampled. However, that these dogs were consuming particular resources provides at least a clue of what was under consideration by their human counterparts.
Temple University--Theses
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Hughes, Stephen. "Crustal structure of northeastern North America : results from the Ontario-New York-New England seismic refraction/wide-angle reflection experiment." Thesis, University of Leicester, 1992. http://hdl.handle.net/2381/35043.

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The Ontario-New York-New England seismic refraction/wide-angle reflection profile was acquired to investigate the deep structural interrelationships between the southeastern Grenville province and the western New England Appalachians. The Grenville province is characterized by 45 km thick crust, with an average crustal seismic velocity of 6.6 km/s and a Poisson's ratio of 0.28+0.01. In the mid-crust a laminated dome-like body is inferred to be composed of mafic cumulate sills on the basis of its high velocity (7.1 km/s) and Poisson's ratio (0.27). The lower crust is characterized by a velocity of 7.0 km/s which suggests a strongly mafic composition such as garnet pyroxene granulite. The Moho is a variable feature, characterized by en-echelon reflections suggestive of compositional interlayering. An anomalous mantle layer with a velocity of 8.6 km/s is proposed to represent an eclogized basaltic layer added to the lithosphere during Grenvillian orogenesis. The boundary between the Grenvillian craton and the western New England Appalachians is marked by an eastward dipping ramp structure which penetrates to a depth of 25 km where it soles out above a transitional mid-lower crustal interface. The New England Appalachians are characterized by an average crustal velocity of 6.4 km/s and a sharply reflective Moho delineating crustal thinning from 41 km to 37 km towards the Atlantic margin. The lower crustal velocity is 6.8 km/s, with a Poisson's ratio of 0.26+0.01. In contrast to the Grenvillian craton the seismic properties of the Appalachian lower crust are consistent with an intermediate composition interlaced with mafic sills related to extensional underplating and intrusion during the rifting of the Atlantic Ocean.
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Mohow, James August. "Paleo-Indian and early archaic settlement patterns of the Maumee River Valley in northeastern Indiana." Virtual Press, 1989. http://liblink.bsu.edu/uhtbin/catkey/544133.

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In 1987, the Archaeological Resources Management Service (AXM6) at Ball State University conducted a sampling survey of a seven mile section of the Maumee River Valley in Allen County, Indiana. In addition to the primary survey, the project conducted an experiment in resurveying previously surveyed sample units, interviewed local collectors, and analyzed and tabulated data from a local collection with site level provenience. The project also reevaluated data previously collected from an adjacent section of the river valley and tested four sites in the latter study area.This study summarizes the data from the Maumee Grant Project and presents a general chronology of prehistoric habitation in the study area based upon that data. More specifically, this study has formulated provisional settlement models for the:PaleoIndian and Early Archaic habitation of the Upper Maumee River Valley, circa-10,000 to 6,000 B.C.The data indicate that the earliest peoples to inhabit the study area were Paleo-Indian bands with a preference for floodplain habitation and a subsistence strategy that emphasized hunting. As the post-glacial climate of the region ameliorated, the Early Archaic peoples that followed adapted a more diverse subsistence strategy, thus drawing upon a wider variety of terrace and floodplain resources. In contrast to their PaleoIndian forerunners, Early Archaic groups in the Upper Maumee Valley generally exhibited a preference for terrace habitation. In addition to the general Early Archaic occupation of the valley, three specific lithic traditions, the Kirk, the Bifurcate, and the Thebes, were identified and their settlement practices compared. While the origins of the earliest PaleoIndian bands in the region remained unclear, subsequent groups seem to have extended from and/or been influenced by Late Pleistocene and Early Holocene populations to the north, west, southwest, south, and east. By contributing to the regional data base and formulating provisional settlement models, this report provides a foundational basis for future research in the region.
Department of Anthropology
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Books on the topic "Northeastern North America"

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Bessette, Alan. Mushrooms of northeastern North America. Syracuse, N.Y: Syracuse University Press, 1997.

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Indians of northeastern North America. Leiden: E.J. Brill, 1986.

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Downie, N. M. The beetles of northeastern North America. Gainesville, Fla: Sandhill Crane Press, 1994.

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Nicholas, George P., ed. Holocene Human Ecology in Northeastern North America. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4899-2376-9.

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A, Long Dana, ed. The Archaic of northeastern Ohio. Kent, Ohio: Distributed by the Kent State University Press, 1986.

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Peterson, Roger Tory. A field guide to wildflowers: Northeastern and North-central North America. Boston: Houghton Mifflin, 1987.

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Margaret, McKenny, ed. A field guide to wildflowers, northeastern and north-central North America. Boston: Houghton Mifflin, 1996.

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Seabrooke, Leckie, ed. Peterson field guide to moths of northeastern North America. Boston: Houghton Mifflin Harcourt Pub. Company, 2012.

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Peterson, Roger Tory. Peterson first guide to wildflowers of northeastern and north-central North America. Boston: Houghton Mifflin, 1986.

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Margaret, McKenny, National Audubon Society, National Wildlife Federation, and Roger Tory Peterson Institute, eds. A field guide to wildflowers of Northeastern and North-central North America. Boston: Houghton Mifflin, 1996.

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Book chapters on the topic "Northeastern North America"

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Snow, Dean R., Nancy Gonlin, and Peter E. Siegel. "The Northeastern Forests." In The Archaeology of Native North America, 140–60. Second edition. | Milton Park, Abingdon, Oxon; New York, NY: Routledge, 2019.: Routledge, 2019. http://dx.doi.org/10.4324/9781315101156-8.

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Colburn, Elizabeth A., and Aram J. K. Calhoun. "Vernal Pools of Northeastern North America." In The Wetland Book, 1–17. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6173-5_283-1.

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Colburn, Elizabeth A., and Aram J. K. Calhoun. "Vernal Pools of Northeastern North America." In The Wetland Book, 651–66. Dordrecht: Springer Netherlands, 2018. http://dx.doi.org/10.1007/978-94-007-4001-3_283.

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Hancock, R. G. V. "European Glass Trade Beads in Northeastern North America." In Modern Methods for Analysing Archaeological and Historical Glass, 459–71. Oxford, UK: John Wiley & Sons Ltd, 2013. http://dx.doi.org/10.1002/9781118314234.ch22.

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Baron, William R. "Historical Climates of the Northeastern United States." In Holocene Human Ecology in Northeastern North America, 29–46. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4899-2376-9_3.

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Nicholas, George P. "Introduction: Human Behavior and Holocene Ecology." In Holocene Human Ecology in Northeastern North America, 1–7. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4899-2376-9_1.

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Gaudreau, Denise C. "The Distribution of Late Quaternary Forest Regions in the Northeast." In Holocene Human Ecology in Northeastern North America, 215–56. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4899-2376-9_10.

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Nicholas, George P. "Ecological Leveling." In Holocene Human Ecology in Northeastern North America, 257–96. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4899-2376-9_11.

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Nicholas, George P. "Afterword." In Holocene Human Ecology in Northeastern North America, 297–304. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4899-2376-9_12.

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Barber, Russell J. "The Use of Land Snails from Prehistoric Sites for Paleoenvironmental Reconstruction." In Holocene Human Ecology in Northeastern North America, 11–28. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4899-2376-9_2.

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Conference papers on the topic "Northeastern North America"

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Li, Yiran, Vadim Levin, and Zhenxin Xie. "FABRIC OF THE LITHOSPHERE IN NORTHEASTERN NORTH AMERICA." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328049.

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Cipar, John J., and John E. Ebel. "P-WAVE TRAVEL-TIME RESIDUAL MAP FOR EASTERN NORTH AMERICA." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328490.

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Amidon, William H., and Mary Roden-Tice. "THE CASE FOR LATE CRETACEOUS COMPRESSIONAL REJUVENATION IN EASTERN NORTH AMERICA." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272633.

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Washington, Paul A. "EVIDENCE FOR POST-ALLEGHANIAN N-S CONTRACTIONAL DEFORMATION IN EASTERN NORTH AMERICA." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310846.

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Ver Straeten, Charles, William E. Stein, and Rose-Anna Behr. "DEVONIAN TERRESTRIAL SYSTEMS, EASTERN NORTH AMERICA: WHERE WE'RE AT; WHAT IS NEXT?" In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-309924.

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Ebel, John E., and Martin C. Chapman. "EASTERN NORTH AMERICA PASSIVE MARGIN EARTHQUAKES AND MESOZOIC RIFT STRUCTURES." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-343949.

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Li, Cong, Haiying Gao, Michael L. Williams, and Xiaotao Yang. "MODIFICATION OF THE CONTINENTAL CRUST IN EASTERN NORTH AMERICA REVEALED BY PS CONVERTED WAVES." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328190.

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Pease, Allison, and James Davis. "SEA LEVEL BUDGET ALONG THE EAST COAST OF NORTH AMERICA." 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-289898.

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Menke, William, Dallas Abbott, and Vadim Levin. "THE INFLUENCE OF MANTLE UPWELLING AT THE PASSIVE CONTINENTAL MARGIN OF EASTERN NORTH AMERICA ON THE CRUST." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-327907.

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Fowler, Brian K., P. Thompson Davis, Jeremy D. Shakun, Paul R. Bierman, Lee B. Corbett, Peter Mattison, and Rebecca Mattison. "A NEW COSMOGENIC EXPOSURE AGE FOR EMPLACEMENT OF NEW HAMPSHIRE'S MADISON BOULDER, REPUTEDLY THE LARGEST ERRATIC IN NORTH AMERICA." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-327778.

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Reports on the topic "Northeastern North America"

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Ascoli, P. Mesozoic-Cenozoic foraminiferal, ostracod and calpionellid zonation of the north Atlantic margin of North America: Georges Bank-Scotian basins and northeastern Grand Banks [Jeanne d'Arc, Carson and Flemish Pass basins] and biostratigraphic correlation of 51 wells. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/130500.

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Adams, J., P. W. Basham, and S. Halchuk. Northeastern North American earthquake potential - new challenges for seismic hazard mapping. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205110.

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Marks, David R. Mute Swans. U.S. Department of Agriculture, Animal and Plant Health Inspection Service, February 2018. http://dx.doi.org/10.32747/2018.7208745.ws.

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Abstract:
Mute swans (Cygnus olor) are an invasive species originally brought to the United States in the late 19th and early 20th centuries for ornamental ponds and lakes, zoos and aviculture collections. Original populations were located in northeastern states along the Hudson Valley but have since expanded to several Midwestern states and portions of the western U.S. and Canada. Mute swan damage includes competing with native waterfowl, destroying native plants, spreading disease, and colliding with aircraft. They are also considered a nuisance in some areas due to their abundant fecal droppings and aggressiveness towards people. Some have questioned the status of mute swans as an introduced species, but multiple reviews by scientists and the U.S. Fish and Wildlife Service clearly support the conclusion that mute swans are not native to North America. The Migratory Bird Treaty Act, therefore, does not protect mute swans, and management authority falls under jurisdiction of the states and Tribes.
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