The Thames as a Barrier in the Eighteenth Century

2018 ◽  
pp. 26-46
Author(s):  
Derek Morris ◽  
Ken Cozens

Analysis of marriage registers, apprentice records, wills and insurance policies demonstrates that in the eighteenth century, the Thames, downstream from the Tower of London, was a major barrier to the development of strong business and marriage links between the residents on the north bank in Stepney, and those on the south bank in Surrey and Kent. Possible reasons for our findings are examined in the context of London's growth, migration patterns and business opportunities. The importance of Sun Fire Office insurance policies, in examining personal and commercial links between places far apart is emphasised. Suggestions are made for future research.

Author(s):  
David Anthony Bello

This article will explore some of the Qing Empire’s primary adaptations, mainly pastoral and agricultural, to the arid environments of southern, eastern and northern Xinjiang – that is, the Tarim, Hami-Turfan and Zünghar basins respectively. It first examines the region’s arid climate and its constraining implications for, first, agriculture as the empire’s standard form of territorial incorporation in the south and east; and, second, pastoralism and agro-pastoralism in the north. These relations were not purely social, but were conditioned within both human and natural parameters. Xinjiang’s general aridity informed Qing interactions with the territory’s diverse peoples, which presented both cultural and ecological – that is, environmental – obstacles and opportunities.


Author(s):  
Nguyễn Quang Ngọc

Vietnam is a country of an early history establishment with three archaeological centres: Dong Son in the North, Sa Huynh in the Central, and Oc Eo in the South. In the long history, these three centres unite and gather into a unified block, step by step, becoming a mainstream development trend. By the eleventh century, Thang Long capital (Hanoi) is a typical representative, the starting point for the course of advancement to the South of the Vietnamese. Later, Phu Xuan (Hue) from the fourteenth century and Gia Dinh (Saigon) from the seventeenth century directly multiply resources, deciding the success of the course of territory expansion and determining the southern territory of the nation Dai Viet – Vietnam in the middle of the eighteenth century. The Tay Son movement at the end of the eighteenth century starts unifying the country, but the course is not completed with numerous limitations. The mission of unifying the whole country is assigned back to Nguyen Anh. Nguyen Anh continually builds Gia Dinh into a firm basement for proceeding to conquer the imperial capital of Hue and the citadel Thang Long, completing the 733-year journey to expand the southern territory (1069–1802) and unifying the whole country into a single unit. Hanoi – Hue – Saigon in the relationship and mutual support has become the three pillars that determine all successes throughout the long history and in each stage of expansion and shaping of territory and unification of the country.


Nordlit ◽  
2015 ◽  
pp. 79
Author(s):  
Henning Howlid Wærp

<p align="LEFT">The article gives a survey of northern Norwegian poetry from the end of the eighteenth century until the present, focusing on how the north is depicted. Another line in the article follows the shaping of a specific northern Norwegian identity from the launching of the name “Nord-Norge” (North Norway) in 1884. The argument is that the feeling of marginalisation is no longer evident, probably because a new circumpolar identity has emerged, an international orientation replacing the former comparisons and competition with the capital in the south.</p>


1971 ◽  
Vol 51 (2) ◽  
pp. 177-239 ◽  
Author(s):  
G. J. Wainwright ◽  
J. G. Evans ◽  
I. H. Longworth

SummaryExcavations in 1969 within a 35-acre enclosure at Marden on the north bank of the River Avon in the Vale of Pewsey confirmed its association with the Grooved Ware ceramic style and its superficial resemblances to the Durrington Walls enclosure ten miles downstream. A survey of the enclosure produced an unusual plan bounded by a bank with an internal ditch and on the south side by the River Avon itself, whilst the position of the Hatfield Barrow was established by geophysical means. Within the north-entrance causeway a small circular timber structure was recorded in a comparable position to the much larger building at Durrington Walls.


Author(s):  
Peter Thomson

The Barguzin River flows out of the Barguzin Mountains, through the town of Barguzin and then the coastal community of Ust-Barguzin before it finally loses itself in a broad cove of Baikal known as Barguzin Bay. The only way across the river for miles upstream from the lake is a ramshackle little wooden ferry with a tiny, corrugated steel shed with a wood stove in it and room on its deck for about half a dozen cars. The ferry slips noiselessly away from the end of the road on the south bank, and looking west toward the lake, two ghostly, rusting timber loading cranes loom on the horizon while the river spills over into a grassy marsh on its north bank. Turning back to the east, there’s a small motorboat laboring to get upstream—laboring because it’s attached to a tow rope, which is attached to the ferry. The ferry, it turns out, is just a hapless little barge, at the mercy of the river without the guidance of the motorboat pilot on the other end of the towline. Our crossing takes less than five minutes, and connected to it by nothing but that single strand, the pilot directs the barge into place perfectly on the far side. But the deckhand fails to secure it, the ferry swings wide in the current, spins ninety degrees, and slams butt-end into the dock. The pilot scowls as he turns the motorboat around and uses its blunt bow, covered in a tractor tire, to push the barge back into place, where the deckhand finally lashes it to the dock. The Barguzin is Baikal’s third largest tributary, after the Selenga to the south of here and the Upper Angara to the north. It carries about six percent of the water flowing into the lake, along with migratory fish like omul and sturgeon, born in the shallow gravel beds upriver before wandering downstream to spend most of their lives in the lake. And even though it flows through only two towns between its headwaters and the lake, the Barguzin carries a significant pollution load into Baikal, as well, especially organic chemicals from timber operations.


2002 ◽  
Vol 59 (12) ◽  
pp. 1969-1979 ◽  
Author(s):  
Ashleen J Benson ◽  
Gordon A McFarlane ◽  
Susan E Allen ◽  
John F Dower

The response of Pacific hake (Merluccius productus) to recent changes in ocean conditions has been dramatic, with a larger proportion of the stock moving into Canadian waters in the 1990s. Additionally, after 1994, hake spawned in Canadian waters and a portion of the stock remained year round. The change in distribution corresponded with a change in growth of juvenile hake. These changes were examined in relation to upwelling and temperature. We also examined these changes in relation to changes in the abundance of euphausiids, which are the primary food supply. We propose that the 1989 regime shift differentially affected the availability of euphausiids in the northern and southern Coastal Upwelling Domain, with feeding conditions in the north improved relative to those in the south. This promoted faster growth of juveniles in the northern regions during the 1990s.


1995 ◽  
Vol 26 (1) ◽  
pp. 121-132 ◽  
Author(s):  
Nguyên Thê Anh

The communist take-over of South Vietnam in 1975 presents a certain resemblance to what happened two hundred years before, when the Trinh lords in the North overran the Nguyen's polity in the South by 1775, seizing the territories that had been separate from their control for over two centuries. The similitude of the two situations did seem highly symbolic to the Institute of Historical Studies in Hanoi, which on the pretext of publishing a complete collection of the eighteenth-century scholar Le Quy Don's works, reprinted a former translation of his “Miscellaneous chronicles of the government of the frontiers” as the first volume of this collection. This work was originally composed in 1776, after its author had been ordered south, as a member of the Trinh lords’ bureaucracy, to help restore civil government in the “recovered” areas, and facilitate their reincorporation into the north-centred political system. In its detailed description of the different aspects of southern administration, economy and society, it is tantamount to a survey of the affairs of what the author considered as an irrevocably defeated Vietnamese enemy government. This account of the southern regions at that very moment of national reunification seems also, to some extent, appropriate for the justification of the Tightness of the ideology of a North Vietnam that has just then triumphed over its adversaries.


1987 ◽  
Vol 4 ◽  
pp. 96-114 ◽  
Author(s):  
M.J. Morwood ◽  
L. Godwin

This paper presents the results of survey and excavation in the upper Dawson area of the Central Queensland Sandstone Belt, a sandstone-dominated environment bounded by the townships of Banana in the east, Blackall in the west, Springsure in the north and Injune in the south, and which includes the Central Queensland Highlands (Walsh 1984:1). The work was undertaken as part of the environmental impact study for the Gyranda Weir commissioned by Cameron McNamara for the Queensland Water Resources Commission (Morwood 1985, 1986; Godwin 1985). However, the results of the study, and the potential of the area for future research, have a wider interest.


1970 ◽  
pp. 08-16
Author(s):  
Bokary Allaye Kelly ◽  
Mahesh Poudyal ◽  
Jean-Marc Bouvet

We monitored flowering, fruiting and leafing of Vitellaria paradoxa (shea tree) along the north–south gradient in Mali (West Africa), using three study sites for a period of three years. In each site, adult shea trees were marked and monitored in permanent plots of both field and fallow stands. The chronology of phenophases and their mean length as well as flowering and fruiting were assessed. Our data revealed significant variation according to site and stand. The onset of events starts earlier in the south than in the centre or north, but the period covered by events was almost the same for all sites (3 to 6 months for flowering; 5 to 6 months for fruiting; and 2 to 4 months before full leafing).Flowering and fruiting were more regular in the south, but often as high in the north, with an almost similar trend in both fields and fallows. In the centre, flowering was also high in fields as well as in fallows, while the fruiting was medium to high. We also observed variations in the mean length of phenological events in study sites and stands. Sites in the south showed the highest average length of flowering and leafing (76 days and 44 days, respectively), while the central site showed the greatest length of mean fruiting (110 days).  We observed a significant site*stand interaction and noticeable variation over the years. Our study indicates that phenological events of shea tree could be influenced by several interacting biotic and abiotic factors. A future research challenge in shea phenology would be to discriminate these factors and thus help sustainable management of shea tree parklands.


2010 ◽  
Vol 37 (1) ◽  
pp. 150-160 ◽  
Author(s):  
S. Lundberg ◽  
I. Svanberg

The stone loach (Barbatula barbatula) occurs in three main areas in Sweden. In the north, it is found in Lapland in the River Torneälven. In the south, it is found in Skåne. There are also two populations near the cities of Stockholm and Nyköping. New data suggest that these two populations originate from fish that were kept in ponds. In the 1740s King Frederick I is said to have released stone loaches from German sources in Lake Mälaren, but this cannot explain its occurrence in Igelbäcken near Stockholm. There is also reason to believe that it was kept in ponds at the royal castle Ulriksdal in the mid-eighteenth century. The fish was possibly imported from the king's native Germany, to be eaten as a delicacy. However, historical records tell of pond-keeping of stone loach by the Royal court in the Stockholm area during the 1680s.


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