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Auteur : Grafiati
Publié le 26 juillet 2024

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1

Fleisher, P. Jay. « Evidence of An Ice-Dammed Lake and Laurentide Readvance Upper Susquehanna Valley, New York State ». Journal of Geography and Geology 14, no 2 (3 novembre 2022) : 52. http://dx.doi.org/10.5539/jgg.v14n2p52.

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Landforms and well logs document a system of ice-contact and proglacial lakes in the upper Susquehanna valley during Laurentide Ice Sheet retreat from the Appalachian Plateau, central New York State.  Recessional moraines formed dams for all lakes, except a newly revealed “Ancestral Goodyear Lake” retained behind an ephemeral ice dam stranded at Colliersville.  A prominent dead-ice sink currently occupies the valley floor at the dam site Ancestral Goodyear Lake held a stable lake level at 1360 feet as represented by thick lake sediments perched in water well logs on the valley wall above Goodyear Lake.  A deltaic terrace at 1250 feet in the same vicinity marks a second, lower lake strand.   In addition, water well logs on the adjacent Portlandville Moraine contain lake sediments bound above and below by ice-contact material deposits thus demonstrating a Laurentide readvance that subsequently dammed the valley to form Glacial Lake Milford as part of the Susquehanna Lake System.
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2

Minderhout, David J. « Native Americans in the Susquehanna River Valley : An Archaeological Summary ». Journal of the Pennsylvania Academy of Science 88, no 1 (1 mars 2014) : 28–39. http://dx.doi.org/10.5325/jpennacadscie.88.1.0028.

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ABSTRACT Native Americans have lived in the Susquehanna River Valley for at least 10,000 years. Archaeological research along the banks of the river has discovered a rich prehistory stretching from the Paleoindian era through the Archaic and Woodland periods up to and through early contact with Europeans. This paper summarizes the major environmental changes that affected the cultural evolution of Native Americans over this long time span and the technological innovations that occurred. Because the same areas in which Native Americans made their camps or villages have also been desirable areas for subsequent European settlement and industrial development, the archaeological record is incomplete and a number of questions remain unanswered and require additional research. Among them are the origins of various archaeological cultures; the size of native populations at in various time periods; and why agriculture/horticulture was so late in developing along the river. A brief discussion of Native American migrations and relocation in the Contact Period is included. Attention is also given to the emergence of organizations over the last two decades in the river basin which claim native descent.
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3

Gardner, Thomas W., Ira D. Sasowsky et Victor A. Schmidt. « Reversed-Polarity Glacial Sediments and Revised Glacial Chronology, West Branch Susquehanna River Valley, Central Pennsylvania ». Quaternary Research 42, no 2 (septembre 1994) : 131–35. http://dx.doi.org/10.1006/qres.1994.1062.

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AbstractA new exposure of glacial and glaciolacustrine sediments at Antes Fort allows for revision of the chronology of pre-Wisconsinan glaciation in central Pennsylvania. Lacustrine sediments from a proglacial lake in the West Branch Susquehanna River valley have reversed remanent polarity with a site mean paleomagnetic declination of 193.8° and inclination of -13.1°. The magnetization is probably a true detrital remanence from the time of deposition and is not significantly affected by postdepositional diagenesis. We propose that the Antes Fort till was deposited during either pre-Illinoian glaciation F or G of G. M. Richmond and D. S. Fullerton (1986, "Quaternary Science Reviews," Vol. 5, 183-196) between 770,000 and 970,000 yr ago. We suggest that it is equivalent to the Penny Hill till in the West Branch Susquehanna River valley and tentatively correlate it westward with the reversed polarity terrace deposits and Minford Silt in western Pennsylvania, West Virginia, and Ohio; the West Lebanon till in Indiana; and the A4 tills (or possible B tills) in Iowa and Nebraska.
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4

Egnal, Marc, et Peter C. Mancall. « Valley of Opportunity : Economic Culture along the Upper Susquehanna, 1700- 1800. » American Historical Review 98, no 1 (février 1993) : 231. http://dx.doi.org/10.2307/2166520.

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5

Mancall, Peter C. « The Revolutionary War and the Indians of the Upper Susquehanna Valley ». American Indian Culture and Research Journal 12, no 1 (1 janvier 1988) : 39–57. http://dx.doi.org/10.17953/aicr.12.1.47685jr4w12x53tn.

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6

Merrell, James H., et Peter C. Mancall. « Valley of Opportunity : Economic Culture along the Upper Susquehanna, 1700-1800 ». Journal of Interdisciplinary History 23, no 4 (1993) : 812. http://dx.doi.org/10.2307/206317.

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7

Aron, Stephen, et Peter C. Mancall. « Valley of Opportunity : Economic Culture along the Upper Susquehanna, 1700-1800 ». Western Historical Quarterly 23, no 3 (août 1992) : 365. http://dx.doi.org/10.2307/971513.

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8

Dennis, Matthew, et Peter C. Mancall. « Valley of Opportunity : Economic Culture along the Upper Susquehanna, 1700-1800. » Journal of American History 79, no 1 (juin 1992) : 240. http://dx.doi.org/10.2307/2078497.

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9

Hood, J. Edward, et Peter C. Mancall. « Valley of Opportunity : Economic Culture Along the Upper Susquehanna, 1700-1800. » Man 27, no 4 (décembre 1992) : 883. http://dx.doi.org/10.2307/2804183.

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10

Leonard, Joseph W., et Peter C. Mancall. « Valley of Opportunity : Economic Culture along the Upper Susquehanna, 1770-1800 ». American Indian Quarterly 17, no 3 (1993) : 443. http://dx.doi.org/10.2307/1184929.

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11

Brooke, John L., et Peter C. Mancall. « Valley of Opportunity : Economic Culture Along the Upper Susquehanna, 1700- 1800. » William and Mary Quarterly 49, no 4 (octobre 1992) : 719. http://dx.doi.org/10.2307/2947187.

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12

Calloway, Colin, et Peter C. Mancall. « Valley of Opportunity : Economic Culture along the Upper Susquehanna, 1700-1800 ». Ethnohistory 39, no 4 (1992) : 521. http://dx.doi.org/10.2307/481971.

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13

April M. Beisaw. « Environmental History of the Susquehanna Valley Around the Time of European Contact ». Pennsylvania History : A Journal of Mid-Atlantic Studies 79, no 4 (2012) : 366. http://dx.doi.org/10.5325/pennhistory.79.4.0366.

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14

Ramage, Joan M., Thomas W. Gardner et Ira D. Sasowsky. « Early Pleistocene Glacial Lake Lesley, West Branch Susquehanna River valley, central Pennsylvania ». Geomorphology 22, no 1 (février 1998) : 19–37. http://dx.doi.org/10.1016/s0169-555x(97)00053-6.

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15

Brown, Matthew R., et Carlos A. Iudica. « Bioaccumulation of Methylmercury in Neovison vison (Schreber, 1777) Populations of the Susquehanna River Valley ». Journal of the Pennsylvania Academy of Science 88, no 1 (1 mars 2014) : 13–19. http://dx.doi.org/10.5325/jpennacadscie.88.1.0013.

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ABSTRACT Being the longest non-navigable river on the eastern coast of the United States, the Susquehanna River and the surrounding areas support a vast number of plants, animals, and other organisms, creating a vast and complex food web within a large and biodiverse ecosystem. One of the most prominent and essential organisms within this food web is the American mink (Neovison vison). In recent years, studies have been conducted to determine the level of biomagnification of methylmercury in terrestrial organisms that reside at higher trophic levels. This particular study has found that American mink populations residing in the Susquehanna River Valley of Pennsylvania are reliable indicators of bioaccumulation of methylmercury due to their role as piscivorous carnivores residing at a high trophic level of the terrestrial food web. Analysis of methylmercury concentrations of 166 hair samples from collected mink specimens yielded 111 samples with concentrations in excess of the toxicity threshold of 1 mg kg-1 body weight. Furthermore, our data suggest that although mercury contamination is a global concern, geographical location of mercury producers, such as coal-burning power plants, and the relationship to the location of mink populations may be a large factor in bioaccumulation of mercury. In particular, samples taken from mink specimens within habitats in the northeastern region of Pennsylvania contained higher concentrations of methylmercury as well as a larger quantity of samples containing concentrations higher than the toxicity threshold than in samples from other regions of the state.
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16

Wennersten, John R. « Valley of Opportunity : Economic Culture Along the Upper Susquehanna, 1700–1800. By Peter C. Mancall ». Environmental History Review 16, no 2 (1992) : 92–93. http://dx.doi.org/10.2307/3984931.

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17

Midtrød, Tom Arne. « “A People before Useless” : Ethnic Cleansing in the Wartime Hudson Valley, 1754–1763 ». Early American Studies : An Interdisciplinary Journal 21, no 3 (juin 2023) : 428–59. http://dx.doi.org/10.1353/eam.2023.a904222.

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abstract: This article investigates the issue of ethnic cleansing against Native peoples in early America and the relationship between ethnic cleansing and genocide. It examines the efforts of colonial officials in New York and New Jersey to remove Native groups in the Hudson Valley region during the Seven Years’ War. In an atmosphere of suspicion and animosity, colonial authorities first sought to exert control over local Natives through surveillance and internment in colonial towns. Then, following an outburst of genocidal violence from ordinary colonials, they began to encourage the Natives to leave their homelands, first for refuge among the Mohawk allies of the British and then for Native settlements in the distant Susquehanna country. Cast as an effort at paternalistic protection of vulnerable Natives, the official effort at ethnic cleansing worked in tandem with indiscriminate violence from ordinary colonial, as officials both exploited and exaggerated the genocidal attitudes of the colonial population to encourage Native removal. Though colonial officials abandoned this ethnic cleansing program after the return of peace to the region in 1758, the evidence presented here shows that largely nonviolent efforts at removal or ethnic cleansing cannot easily be disentangled from the threat of genocide or extermination.
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18

Bloomquist, J. « DIALECT DIFFERENCES IN CENTRAL PENNSYLVANIA : REGIONAL DIALECT USE AND ADAPTATION BY AFRICAN AMERICANS IN THE LOWER SUSQUEHANNA VALLEY ». American Speech 84, no 1 (1 mars 2009) : 27–47. http://dx.doi.org/10.1215/00031283-2009-003.

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19

Hart, John P., et C. Margaret Scarry. « The Age of Common Beans (Phaseolus vulgaris) in the Northeastern United States ». American Antiquity 64, no 4 (octobre 1999) : 653–58. http://dx.doi.org/10.2307/2694210.

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AbstractA radiocarbon date of A.D. 1070 ± 60 was linked to the remains of maize (Zea mays), beans (Phaseolus vulgaris), and squash (Cucñrbita pepo) at the Roundtop site in the Susquehanna River valley of New York by William Ritchie in 1969 and 1973 publications. This date established the presence of beans in the Northeast at an earlier time than in most other areas of the eastern United States, where they are generally rare before A.D. 1300. Subsequently beans have been reported in pre-A.D.1300 contexts from at least eight other sites in the Northeast. Recent calibrated AMS dates on beans from Roundtop are no earlier than A.D. 1300 (Hart 1999a). Given that the original Roundtop date was responsible for the acceptance of early beans in the Northeast, the AMS dates suggested that beans may not become archaeologically visible there until ca. A.D. 1300. AMS dates on beans from four other sites, reported here, substantiate the Roundtop results. Beans and by extension maize-beans-squash intercropping are not evident in the Northeast before ca. A.D. 1300.
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20

Wickert, Andrew D. « Reconstruction of North American drainage basins and river discharge since the Last Glacial Maximum ». Earth Surface Dynamics 4, no 4 (8 novembre 2016) : 831–69. http://dx.doi.org/10.5194/esurf-4-831-2016.

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Abstract. Over the last glacial cycle, ice sheets and the resultant glacial isostatic adjustment (GIA) rearranged river systems. As these riverine threads that tied the ice sheets to the sea were stretched, severed, and restructured, they also shrank and swelled with the pulse of meltwater inputs and time-varying drainage basin areas, and sometimes delivered enough meltwater to the oceans in the right places to influence global climate. Here I present a general method to compute past river flow paths, drainage basin geometries, and river discharges, by combining models of past ice sheets, glacial isostatic adjustment, and climate. The result is a time series of synthetic paleohydrographs and drainage basin maps from the Last Glacial Maximum to present for nine major drainage basins – the Mississippi, Rio Grande, Colorado, Columbia, Mackenzie, Hudson Bay, Saint Lawrence, Hudson, and Susquehanna/Chesapeake Bay. These are based on five published reconstructions of the North American ice sheets. I compare these maps with drainage reconstructions and discharge histories based on a review of observational evidence, including river deposits and terraces, isotopic records, mineral provenance markers, glacial moraine histories, and evidence of ice stream and tunnel valley flow directions. The sharp boundaries of the reconstructed past drainage basins complement the flexurally smoothed GIA signal that is more often used to validate ice-sheet reconstructions, and provide a complementary framework to reduce nonuniqueness in model reconstructions of the North American ice-sheet complex.
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21

Main, Gloria L. « Valley of Opportunity : Economic Culture along the Upper Susquehanna, 1700–1800. By Peter C. Mancall. Ithaca and London : Cornell University Press, 1991. Pp. xviii, 253. $29.95. » Journal of Economic History 52, no 2 (juin 1992) : 509–10. http://dx.doi.org/10.1017/s0022050700011207.

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22

Marcus Gallo. « “Fair Play Has Entirely Ceased, and Law Has Taken Its Place” : The Rise and Fall of the Squatter Republic in the West Branch Valley of the Susquehanna River, 1768–1800 ». Pennsylvania Magazine of History and Biography 136, no 4 (2012) : 405. http://dx.doi.org/10.5215/pennmaghistbio.136.4.0405.

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23

Bush, David R. « Prehistoric Farmers of the Susquehanna Valley : Clemson Island Culture and the St. Anthony Site. R. Michael Stewart Occasional Publications in Northeastern Anthropology No. 13. Archaeological Services, Bethlehem, Connecticut, 1994. vi + 225 pp., plates, figures, tables, references cited. $30.00 (cloth). » American Antiquity 62, no 1 (janvier 1997) : 156–57. http://dx.doi.org/10.2307/282394.

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24

Custer, Jay F. « Correlation of regional late woodland triangle projectile point variation and native American ethnic group territories in the central middle Atlantic ». North American Archaeologist, 29 mars 2022, 019769312210905. http://dx.doi.org/10.1177/01976931221090596.

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The shapes and sizes of 983 Late Woodland triangular projectile points from four indigenous Native American different ethnic groups of the central Middle Atlantic region (Unami Lenapi – Lower Delaware Valley, Munsee Lenape – Upper Delaware Valley, Susquehannock – Lower Susquehanna Valley, Nanticoke – Lower Delmarva Peninsula) and one archaeological complex (Shenks Ferry – Lower Susquehanna Valley) were compared using various univariate statistical analytics, including the difference-of-mean and difference-of proportion tests, to see if there were any statistically significant morphological differences among them. There were none, even though earlier studies of small samples with anecdotal observations and comparisons stated that there were observable differences among the projectile points of the various ethnic groups. This study's findings refute the axiomatic assumption of traditional normative culture approaches that there must be identifiable stylistic variation in projectile points among different ethnic groups. In the case of Late Woodland triangular projectile points in the central Middle Atlantic region, the technological prerequisites of shock hunting with bows and stone-tipped arrows limited inter-ethnic group variation in projectile point forms. However, use of poisons may have affected overall projectile point sizes.
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25

Rieth, Christina B. « Analyzing Style and Technology in the Eastern Woodlands ». MRS Proceedings 712 (2002). http://dx.doi.org/10.1557/proc-712-ii4.8.

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ABSTRACTTrace element analysis was used to assess the provenance of manufacture of ceramic vessels recovered from six Early Late Prehistoric sites (A.D. 700-1300) in the Susquehanna Valley of New York and Pennsylvania. The compositional profiles of 93 sherds were recorded and compared with the profiles of known clays in the valley. The results of this project suggest that the vessels from these sites form five different clay groups with most vessels manufactured from local clays. Some non-locally manufactured pots were also identified and may represent interaction between neighboring groups.
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26

« Valley of opportunity : economic culture along the Upper Susquehanna, 1700-1800 ». Choice Reviews Online 29, no 06 (1 février 1992) : 29–3521. http://dx.doi.org/10.5860/choice.29-3521.

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27

« Susie Susquehanna & ; The River Valley Blues by Clara Mae Barnhart (review) ». American Book Review 44, no 1 (mars 2023) : 157–60. http://dx.doi.org/10.1353/abr.2023.a902846.

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28

« Peter C. Mancall. Valley of Opportunity : Economic Culture along the Upper Susquehanna, 1700–1800. Ithaca : Cornell University Press. 1991. Pp. xviii, 253. $29.95 ». American Historical Review, février 1993. http://dx.doi.org/10.1086/ahr/98.1.231-a.

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