Conflict, Population Movement, and Microscale Social Networks in Northern Iroquoian Archaeology

2021 ◽  
Vol 86 (2) ◽  
pp. 350-367
Author(s):  
Jennifer Birch ◽  
John P. Hart

We employ social network analysis of collar decoration on Iroquoian vessels to conduct a multiscalar analysis of signaling practices among ancestral Huron-Wendat communities on the north shore of Lake Ontario. Our analysis focuses on the microscale of the West Duffins Creek community relocation sequence as well as the mesoscale, incorporating several populations to the west. The data demonstrate that network ties were stronger among populations in adjacent drainages as opposed to within drainage-specific sequences, providing evidence for west-to-east population movement, especially as conflict between Wendat and Haudenosaunee populations escalated in the sixteenth century. These results suggest that although coalescence may have initially involved the incorporation of peoples from microscale (local) networks, populations originating among wider mesoscale (subregional) networks contributed to later coalescent communities. These findings challenge previous models of village relocation and settlement aggregation that oversimplified these processes.

1986 ◽  
Vol 1 (20) ◽  
pp. 85
Author(s):  
Cyril Galvin ◽  
Charles J. Rooney ◽  
Gilbert K. Nersesian

Prior to construction at Fire Island Inlet, Fire Island was moving westward at more than 200 feet per year, the north shore of the inlet was eroding severely, and navigation in the inlet was difficult. The Federal Jetty, completed in 1941, and the sand dike, built in 1959, have halted the westward migration, eliminated the severe erosion, and partially improved navigation, with minimal maintenance or repair to the structures. There has been a large net accretion of sand east of the jetty and west of the dike, an unknown part of which is at the expense of shores to the west of the inlet. At the State Park on the south side of the inlet interior, erosion accelerated, probably because of the dike. The middle and ocean segments of the 4750-foot Federal Jetty are now (1987) in good condition, although the design implies a stability coefficient for the quarrystone jetty head at time of construction that would now be considered risky. Stability has been promoted by a stone blanket under and east of the jetty, a thick stone apron seaward of the jetty, a low (8 feet MLW) crest, and armor stone that has been partially keyed in place. Damage due to scour, common at other single-jetty inlets, is absent here because longshore transport, which easily overtops the low crest, keeps the inlet channel away from the jetty. Although the two seaward segments of the jetty remain in good condition, the inshore segment of the jetty is in poor condition, despite its apparently sheltered location. The cumulative effects of waves, possibly channeled to the site along recurved spits during storms, have damaged 1200 feet, and tidal scour has destroyed about 230 feet. The damaged segment has a design cross section which is onefifth and one-twelfth the cross sections of the jetty trunk and head.


1955 ◽  
Vol 11 (3) ◽  
pp. 429-447
Author(s):  
Joaquín Meade

The huasteca region in northeastern Mexico covers sections of the six states of Tamaulipas, Veracruz, San Luis Potosí, Hidalgo, Puebla, and Querétaro. Its boundaries are approximately the following: to the north the river Soto la Marina, known in the sixteenth century as the Rio de las Palmas; to the south the Rio Cazones; to the east the Gulf of Mexico and to the west the mountainous section of the eastern Sierra Madre.The Christian conversion of the Huasteca began, no doubt, in 1518 with the expedition of Juan de Grijalva, who actually sailed as far north as Tuxpan and Tamiahua in the Huastec region of the state of Veracruz. John Diaz, a priest, accompanied this expedition. In 1519 Francisco de Garay, then in Jamaica, sent Alonso Alvarez de Pineda to Tampico and the Río Panuco, where he stayed some time and made contact with the Huastecs who belong to the great Maya family.


1995 ◽  
Author(s):  
Kevin Bryon ◽  

This site is located on North Miami Beach, across from the North Shore Recreational Park (a wooded park along the beach). It is currently a barren strip of eight blocks serving as unused parking and storage for miscellaneous construction equipment. The adjacent context to the west is primarily two- and three-story apartment housing separated from the site by a one-lane service alley. The program given to this area is mixed-use focusing on multi-family housing. The most important issue to address is the connection between the existing residential area and the proposed housing project through contextual response. The intention of this project is to weave these two areas together and create a singular neighborhood condition by reactivating the existing alley system.


2017 ◽  
Vol 16 (02) ◽  
pp. 599-605
Author(s):  
CAROLINE WINTERER

After a generation of grand stories about the rise of modern republican thought (the so-called “republican-synthesis” school epitomized by the works of Gordon Wood and J. G. A. Pocock), James Kloppenberg's new book, Toward Democracy: The Struggle for Self-Rule in European and American Thought, offers a history of democratic thought: what Kloppenberg calls “the idea of self-government.” In the course of nearly a thousand pages of text and notes, Kloppenberg traces democracy's emergence “as a widely shared, albeit still controversial, model of government” over the last four centuries in the North Atlantic world (1). The book is deeply learned and intellectually capacious, covering thinkers from the ancient Greeks, through the sixteenth-century wars of religion, through the American and French Revolutions, ending abruptly at the Civil War. Few intellectual historians writing today could have managed a book of such sweep. The number of authors, texts, and themes discussed is vast—so much so that at times it seems that the book could double as a history of thought in the West.


Archaeologia ◽  
1874 ◽  
Vol 44 (2) ◽  
pp. 242-258
Author(s):  
Richard Henry Major

On the 14th of March last I had the honour of laying before this Society some new facts which had fallen under my notice in connection with the early discoveries of the great continental Island of Australia. One of these new facts was the very promising circumstance that there had been found in the Royal Burgundian Library in Brussels, by M. Ruelens, one of the Conservators of the Library, who had obligingly communicated to me the fact, the original autograph report to King Philip III. of a discovery of Australia in 1601 by a Portuguese named Manoel Godinho de Eredia, which discovery I had been the first to make known to the world in a paper read before this Society on the 7th of March, 1861. The report was accompanied by maps and views and portraits, and as at the time of my announcing its discovery to you I had received through M. Ruelens an obliging promise from the Chevalier d'Antas, the Portuguese Minister in Brussels, that an extract should be sent me of that portion with which I was immediately concerned, I begged that the printing of my paper should be postponed until I should possess the opportunity of incorporating into it the translation of the said extract. My reason for appearing before you without waiting till I had examined the Report with my own eyes was, that, while I had no reason to entertain the shadow of a doubt as to the corroborative nature of its contents, I had a still more important announcement to make to you respecting a yet earlier discovery of Australia in the first half of the sixteenth century. Since then I have received the promised extract, and I am sorry to have to report to you that a more unsatisfactory document has never fallen under my notice. But, in order that you may rightly estimate both it and the case to which it refers, it will be necessary that I repeat to you the leading facts and circumstances of the whole story. Up to 1861, the earliest visit to the coasts of Australia known in history in connection with the name of any ship or captain, was that made by the Dutch yacht the “Duyphen,” or “Dove,” about the month of March, 1606. This vessel had been despatched from Bantam on the 18th of November, 1605, to explore the islands of New Guinea. Her course from New Guinea was southward along the islands on the west side of Torres Strait to that part of Terra Australis a little to the west and south of Cape York, but all these lands were thought to be connected and to form the west coast of New Guinea. The Commander of the “Duyphen,” of whose name we are ignorant, was of course unconscious of the importance of his discovery. Indeed, of the discoveries made subsequently by the Dutch on the coasts of Australia, our ancestors of a hundred years ago, and even the Dutch themselves, knew but little. That which was known was preserved in the “Relations de divers Voyages curieux,” of Melchisedeck Thevenot (Paris, 1663-72, fol.); in the “Noord en Oost Tartarye,” of Nicolas Witsen (Amst. 1692-1705, fol.); in Valentyn's “Oud en Nieuw Oost Indien” (Amst. 1724-26, fol.); and in the “Inleidning tot de algemeen Geographie” of Nicolas Struyk (Amst. 1740, 4to.). We have, however, since gained a variety of information, through a document which fell into the possession of Sir Joseph Banks, and was published by Alexander Dalrymple (at that time hydrographer to the Admiralty and the East India Company) in his collection concerning Papua. This curious and interesting document is a copy of the instructions to Commodore Abel Jansz Tasman for his second voyage of discovery. That distinguished commander had already, in 1642, discovered not only the island now named after him, Tasmania, but New Zealand also; and, passing round the east side of Australia, but without seeing it, sailed on his return voyage along the northern shores of New Guinea. In January, 1644, he was despatched on his second voyage, and his instructions, signed by the Governor-General Antonio Van Diemen and the members of the Council, are prefaced by a recital, in chronological order, of the previous discoveries of the Dutch. Prom this recital, combined with a passage from Saris, given in Purchas, vol. i. p. 385, we derive the above information respecting the voyage of the Duyphen, the date of which constituted it the first authenticated discovery of Australia with which a vessel's name could be connected. In 1861, however, I ventured to dispute this priority, and I think I cannot do justice to you and to myself better than by reciting the grounds on which I did so in the very words with which I then addressed you. They are as follows: “Within the last few days I have discovered a MS. Mappemonde in the British Museum, in which on the north-west corner of a country, which I shall presently show beyond all question to be Australia, occurs the following legend: Nuca antara foi descuberta o anno 1601 por mano (sic) el godinho de Evedia (sic) por mandado de (sic) Vico Rey Aives (sic) de Saldaha,” (sic) which I scarcely need translate, Nuca Antara was discovered in the year 1601, by Manoel Godinho de Eredia, by command of the Viceroy Ayres de Saldanha.


1982 ◽  
Vol 19 (9) ◽  
pp. 1836-1850 ◽  
Author(s):  
M. E. Brookfield ◽  
Q. H. J. Gwyn ◽  
I. P. Martin

We describe six major stratigraphic units from the hitherto neglected Quaternary sequences along the north shore of Lake Ontario between Oshawa and Port Hope. These units, from the base upwards, consist of the following: a lowermost unit of silt till, apparently overlying bedrock; a complex unit of lacustrine and glaciofluvial sediments with several thin silt tills, usually unconformable on the lowermost unit; a glaciofluvial sand unit, filling valleys cut into the underlying units; a unit of two sandy pebbly tills; a silt till; and varved clays and sands of glacial Lake Iroquois.Though the sections show more erosional intervals, the above units can be correlated with the better known Scarborough sections as follows: the lowest unit with the Sunnybrook Till; the overlying complex unit with the Meadowcliffe Till and associated sediments; the two sandy pebbly tills with the lower Leaside Till; and the overlying silt till with the Halton Till.The inferred geological history is similar to that of the Scarborough area.


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