The peoples of Southern Mozambique: an historical survey

1973 ◽  
Vol 14 (4) ◽  
pp. 565-580 ◽  
Author(s):  
Alan K. Smith
Keyword(s):  
Eighteenth Century ◽  
Central Africa ◽  
Historical Survey ◽  
The South ◽  
Early Date ◽  
The North ◽  
South Central ◽  
Political Units ◽  
Cultural Entity ◽  
The Village

The purpose of this article is to attempt to clarify some of the outstanding controversies in the historical and ethnographic literature on southern Mozambique. It contends that by the eighteenth century, three distinct ethnic groups— the Tsonga, Chopi, and Tonga—lived in the area. It seeks to demonstrate how and why these groups differed from each other, and how these differences affected the ethnographic map. It argues that state formation among the Tsonga began at an early date, largely because of influences emanating from the adjacent western plateau regions of south-central Africa. Most of the neighbouring Tonga peoples, however, were shielded from these influences, and did not evolve political units larger than the village authority. The exception to this generalization occurred in the south of the Tonga-speaking region, where peoples were subject to an invasion by groups of Shona origin. The resultant differences between the two Tonga-speaking groups were to be of extreme importance when both subsequently would be invaded by peoples of Tsonga origin. In the south the arrival of Tsonga speakers resulted in the formation of the Chopi; in the north Tsonga speakers absorbed and assimilated the Tonga, who might have disappeared as a distinct cultural entity had other factors not intervened before the process had been completed.

Firearms in South-Central Africa

1971 ◽  
Vol 12 (4) ◽  
pp. 545-556 ◽  
Author(s):  
Anthony Atmore ◽  
J. M. Chirenje ◽  
S. I. Mudenge
Keyword(s):  
Eighteenth Century ◽  
Southern Africa ◽  
Central Africa ◽  
Political Structure ◽  
Middle Years ◽  
Early Date ◽  
The North ◽  
South Central ◽  
Economic Basis ◽  
White Settlement

Any survey of the effects of the possession and use of firearms among the Tswana and, to the north of them, the Ndebele and Shona peoples, must start with a brief investigation of firearms among the Khoikhoi and the mixed Khoikhoi-white groups. The latter were in some respects the vanguard of the expansions of the white frontier in southern Africa. They originated in unions between Khoikhoi and white hunters, traders and farmers, and probably never existed without firearms; from an early date they also acquired horses. In the middle years of the eighteenth century the Khoikhoi-whites and the Khoikhoi peoples, whose economic basis and political structure had been broken by various aspects of white settlement amongst them, were being armed by the whites to take part in commando expeditions against the San. There is evidence that some Khoikhoi trekked from the colony to avoid this service.

Matronianus, Comes Isauriae: an Inscription from an Early Byzantine Basilica at Yanıkhan, Rough Cilicia

1985 ◽  
Vol 35 ◽  
pp. 93-97 ◽  
Author(s):  
Stephen Hill
Keyword(s):  
The South ◽  
Late Professor ◽  
The Road ◽  
Scrub Oak ◽  
The North ◽  
Wild Olive ◽  
On The Road ◽  
Olive Trees ◽  
The Village ◽  
Early Byzantine

The ruins at Yanıkhan form the remains of a Late Roman village in the interior of Rough Cilicia some 8 kilometres inland from the village of Limonlu on the road to Canbazlı (see Fig. 1). The site has not been frequently visited by scholars, and the first certain reference to its existence was made by the late Professor Michael Gough after his visit on 2 September 1959. Yanıkhan is now occupied only by the Yürüks who for years have wintered on the southern slopes of Sandal Dağ. The ancient settlement at Yanıkhan consisted of a village covering several acres. The remains are still extensive, and some, especially the North Basilica, are very well preserved, but there has been considerable disturbance in recent years as stone and rubble have been removed in order to create small arable clearings. The visible remains include many domestic buildings constructed both from polygonal masonry without mortar and from mortar and rubble with coursed smallstone facing. There are several underground cisterns and a range of olive presses. The countryside around the settlement has been terraced for agricultural purposes in antiquity, and is, like the settlement itself, densely covered with scrub oak and wild olive trees. The most impressive remains are those of the two basilical churches which are of little artistic pretension, but considerable architectural interest. The inscription which forms the substance of this article was found on the lintel block of the main west entrance of the South Basilica.

A Trickle of Authority: The Arid Conditions of Empire in Eighteenth-Century Xinjiang

2021 ◽  
Author(s):  
David Anthony Bello
Keyword(s):  
Eighteenth Century ◽  
Standard Form ◽  
Arid Climate ◽  
Arid Environments ◽  
The South ◽  
Northern Xinjiang ◽  
The North ◽  
Arid Conditions

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.

Climatology and Trends of Climate Extremes of Temperature and Precipitation in Belo Monte Hydropower Plant – Eastern Amazon, Brazil

2021 ◽  
Author(s):  
Wanderson Luiz-Silva ◽  
Pedro Regoto ◽  
Camila Ferreira de Vasconcellos ◽  
Felipe Bevilaqua Foldes Guimarães ◽  
Katia Cristina Garcia
Keyword(s):  
Climate Change ◽  
Climate Extremes ◽  
Annual Rainfall ◽  
The South ◽  
North Central ◽  
Adaptation Capacity ◽  
The North ◽  
South Central ◽  
Daily Data ◽  
Belo Monte

<p>This research aims to support studies related to the adaptation capacity of the Amazon region to climate change. The Belo Monte Hydroelectric Power Plant (HPP) is in the Xingu River basin, in eastern Amazonia. Deforestation coupled with changes in water bodies that occurred in the drainage area of Belo Monte HPP over the past few decades can significantly influence the hydroclimatic features and, consequently, ecosystems and energy generation in the region. In this context, we analyze the climatology and trends of climate extremes in this area. The climate information comes from daily data in grid points of 0.25° x 0.25° for the period 1980-2013, available in http://careyking.com/data-downloads/. A set of 17 climate extremes indices based on daily data of maximum temperature (TX), minimum temperature (TN), and precipitation (PRCP) was calculated through the RClimDex software, recommended by the Expert Team on Climate Change Detection and Indices (ETCCDI). The Mann-Kendall and the Sen’s Curvature tests are used to assess the statistical significance and the magnitude of the trends, respectively. The drainage area of the Belo Monte HPP is dominated by two climatic types: an equatorial climate in the north-central portion of the basin, with high temperatures and little variation throughout the year (22°C to 32°C), in addition to more frequent precipitation; and a tropical climate in the south-central sector, which experiences slightly more pronounced temperature variations throughout the year (20°C to 33°C) and presents a more defined wet and dry periods. The south-central portion of the basin exhibits the highest temperature extremes, with the highest TX and the lowest TN of the year occurring in this area, both due to the predominant days of clear skies in the austral winter, as to the advance of intense masses of polar air at this period. The diurnal temperature range is lower in the north-central sector when compared to that in the south-central region since the first has greater cloud cover and a higher frequency of precipitation. The largest annual rainfall volumes are concentrated at the north and west sides (more than 1,800 mm) and the precipitation extremes are heterogeneous across the basin. The maximum number of consecutive dry days increases from the north (10 to 20 days) to the south (90 to 100 days). The annual frequency of warm days and nights is increasing significantly in a large part of the basin with a magnitude ranging predominantly from +7 to +19 days/decade. The annual rainfall shows a predominant elevation sign of up to +200 mm/decade only in the northern part of the basin, while the remainder shows a reduction of up to -100 mm/decade. The duration of drought periods increases in the south-central sector of the basin, reaching up to +13 days/decade in some areas. The results of this study will be used in the future as an important input, together with exposure, sensibility, and local adaptation capacity, to design adaptation strategies that are more consistent with local reality and to the needs of local communities.</p>

On the Chloride Waters of Great Britain

1945 ◽  
Vol 82 (6) ◽  
pp. 267-273 ◽  
Author(s):  
W. Anderson
Keyword(s):  
Great Britain ◽  
The South ◽  
Very Old ◽  
North East ◽  
The North ◽  
Exact Position ◽  
The Many ◽  
The Village ◽  
Made In

Formerly there were several surface brine springs in the North-East Coalfield; to-day there are none. From the many accounts of their occurrence nothing has been learned of their exact position, and very little of the composition of their waters. The earliest record, made in 1684, described the Butterby spring (Todd, 1684), and then at various times during the next two centuries brine springs at Framwellgate, Lumley, Birtley, Walker, Wallsend, Hebburn, and Jarrow were noted. In particular the Birtley salt spring is often mentioned, and on the 6-in. Ordnance map, Durham No. 13, 1862 edition, it is sited to the south-east of the village. Although no record has been found there must have been either a brine spring or well at Gateshead, for the name of the present-day suburb, Saltwell, is very old, and brine springs are still active in the coal workings of that area.

scholarly journals HA NOI – HUE – SAI GON IN TERRITORY EXPANSION TOWARD THE SOUTH AND UNIFICATION OF THE COUNTRY (1069–1802)

2020 ◽  
Vol 129 (6E) ◽  
pp. 33-43
Author(s):  
Nguyễn Quang Ngọc
Keyword(s):  
Eighteenth Century ◽  
Eleventh Century ◽  
Development Trend ◽  
Early History ◽  
Mutual Support ◽  
The South ◽  
The North ◽  
Starting Point ◽  
Imperial Capital ◽  
The Relationship

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.

scholarly journals “... langt der oppe mot nord.” Bilder av nord i nordnorsk lyrikk – fra Elias Blix til Morten Wintervold

Nordlit ◽  
2015 ◽  
pp. 79
Author(s):  
Henning Howlid Wærp
Keyword(s):  
Eighteenth Century ◽  
The South ◽  
International Orientation ◽  
The North ◽  
North Norway

<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>

scholarly journals The Tsakonian Dialect.—I

1913 ◽  
Vol 19 ◽  
pp. 133-173 ◽  
Author(s):  
C. A. Scutt
Keyword(s):  
East Coast ◽  
Mountain Range ◽  
The South ◽  
The West ◽  
Northern Boundary ◽  
Grazing Land ◽  
Bare Rock ◽  
The North ◽  
Cultivable Land ◽  
The Village

The area over which the Tsakonian dialect is spoken lies on the east coast of the Peloponnese between the Parnon range and the sea. Its northern boundary is roughly the torrent which, rising on Parnon above Kastánitsa, flows into the sea near Ayios Andréas, its southern the torrent which, also rising on Parnon, passes through Lenídhi to the sea. A mountain range stretches along the coast from end to end of the district, reaching its highest point (1114 metres) in Mt. Sevetíla above the village of Korakovúni. Between Tyrós and Pramateftí, the seaward slopes of this range are gentle and well covered with soil. Behind these coast hills there stretches a long highland plain, known as the Palaiókhora, which, in the north, is fairly well covered with soil, but gradually rises towards the south into a region of stony grazing land, and terminates abruptly in the heights above Lenídhi. The high hill of Oríonda rises out of the Palaiókhora to the west and forms a natural centre-point of the whole district. Behind it stretching up to the bare rock of Parnon, is rough hilly country, cut here and there by ravines and offering but rare patches of cultivable land.

Surface faulting along the Superstition Hills fault zone and nearby faults associated with the earthquakes of 24 November 1987

1989 ◽  
Vol 79 (2) ◽  
pp. 252-281
Author(s):  
R. V. Sharp ◽  
K. E. Budding ◽  
J. Boatwright ◽  
M. J. Ader ◽  
M. G. Bonilla ◽  
...  
Keyword(s):  
Fault Zone ◽  
Lateral Displacement ◽  
Vertical Displacement ◽  
Repeated Measurements ◽  
The South ◽  
Surface Rupture ◽  
Imperial Valley ◽  
The North ◽  
South Central ◽  
The Right

Abstract The M 6.2 Elmore Desert Ranch earthquake of 24 November 1987 was associated spatially and probably temporally with left-lateral surface rupture on many northeast-trending faults in and near the Superstition Hills in western Imperial Valley. Three curving discontinuous principal zones of rupture among these breaks extended northeastward from near the Superstition Hills fault zone as far as 9 km; the maximum observed surface slip, 12.5 cm, was on the northern of the three, the Elmore Ranch fault, at a point near the epicenter. Twelve hours after the Elmore Ranch earthquake, the M 6.6 Superstition Hills earthquake occurred near the northwest end of the right-lateral Superstition Hills fault zone. Surface rupture associated with the second event occurred along three strands of the zone, here named North and South strands of the Superstition Hills fault and the Wienert fault, for 27 km southeastward from the epicenter. In contrast to the left-lateral faulting, which remained unchanged throughout the period of investigation, the right-lateral movement on the Superstition hills fault zone continued to increase with time, a behavior that was similar to other recent historical surface ruptures on northwest-trending faults in the Imperial Valley region. We measured displacements over 339 days at as many as 296 sites along the Superstition Hills fault zone, and repeated measurements at 49 sites provided sufficient data to fit with a simple power law. Data for each of the 49 sites were used to compute longitudinal displacement profiles for 1 day and to estimate the final displacement that measured slips will approach asymptotically several years after the earthquakes. The maximum right-lateral slip at 1 day was about 50 cm near the south-central part of the North strand of Superstition Hills fault, and the predicted maximum final displacement is probably about 112 cm at Imler Road near the center of the South strand of the Superstition Hills fault. The overall distributions of right-lateral displacement at 1 day and the estimated final slip are nearly symmetrical about the midpoint of the surface rupture. The average estimated final right-lateral slip for the Superstition Hills fault zone is about 54 cm. The average left-lateral slip for the conjugate faults trending northeastward is about 23 cm. The southernmost ruptured member of the Superstition Hills fault zone, newly named the Wienert fault, extends the known length of the zone by about 4 km. The southern half of this fault, south of New River, expressed only vertical displacement on a sinuous trace. The maximum vertical slip by the end of the observation period there was about 25 cm, but its growth had not ceased. Photolineaments southeast of the end of new surface rupture suggest continuation of the Superstition Hills fault zone in farmland toward Mexico.

The African Side the Early/Legendary Past

2018 ◽  
pp. 129-138
Author(s):  
Finn Fuglestad
Keyword(s):  
The South ◽  
The North ◽  
Local Traditions ◽  
The Village ◽  
Porto Novo

The village of Tado in the north looms large in some local traditions. It was possibly the first general polity of the region (a theory supported by archaeological findings). What we think we know is that its ruler was a typical sacred king and the society a kinship-type one. But at some stage a group of people known as the Aja or Agasuvi had to flee towards the south. They founded Notsé and Allada. From Allada some groups moved to establish Dahomey in the north and, somewhat later, Porto Novo/Hogbonu in the east. The author argues that all the Ewe of the Western Slave Coast originated from Notsé – a contention modern anthropologists and historians are skeptical of – and that if there was migration, it must have involved few people and short distances. The chapter observes that there is a rival tradition to that of Tado, which underlines the importance of the kingdom of Grand Popo on the coast in the south.

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