The Remains of Liangzhu Culture at Jiangzhuang Site in Xinghua and Dongtai Cities, Jiangsu

2017 ◽  
Vol 17 (1) ◽  
pp. 18-31
Keyword(s):  
Yangtze River ◽  
Large Scale ◽  
New Materials ◽  
The West ◽  
Academic Field ◽  
The North ◽  
Main Work ◽  
The People ◽  
Water Wells ◽  
Liangzhu Culture

AbstractIn October 2011 to December 2015, the Institute of Archaeology, Nanjing Museum conducted two terms of excavations to the Jiangzhuang Site located in the administrated areas of Xinghua and Dongtai Cities, Jiangsu Province. The main work was the large-scale uncovering of the settlement of the Liangzhu Culture located in the west zone of the site, the features recovered from which included burials, house foundations, ash pits, water wells, ash ditches, etc. In the cemetery of the Liangzhu Culture in the northeast of the west zone of the site, burials were densely arranged; most of the burials had burial receptacles, and the skeletons were well preserved, the burial positions of which included primary burials and secondary burials. The discovery and excavation of the settlement of Liangzhu Culture at Jiangzhuang Site revised the traditional viewpoint of the academic field that the north border of the Liangzhu Culture was limited by the Yangtze River and provided new materials for the comprehensive and in-depth researches on the civilization and society of the Liangzhu Culture. The large amount of human skeletons unearthed from the burials of the Liangzhu Culture will also effectively improve the indepth researches on the burial custom, social organization and relationship and racial attribution of the people of Liangzhu Culture.

The Dabona Cemetery in Xiangyun County, Yunnan

2016 ◽  
Vol 16 (1) ◽  
pp. 13-26
Keyword(s):  
Large Scale ◽  
Erhai Lake ◽  
Warring States Period ◽  
Social Situations ◽  
The West ◽  
Warring States ◽  
The North ◽  
Lake Region ◽  
The People ◽  
The Social

Abstract In 2014, Yunnan Provincial Institute of Cultural Relics and Archaeology and other institutions conducted large-scale excavation to the Dabona Cemetery located in Dabona Village and to its east of the Liuchang Town, Xiangyun County. The west zone of the Dabona Cemetery had widely distributed early cultural remains, including house foundations, postholes, ash pits, ash ditches, etc. The east zone consisted of two sections distributed in the north-south direction, in the north section of which 25 burials were recovered; among these burials, six were large-sized ones with lengths more than 6m, and the other were medium- and small-sized burials. The grave goods unearthed from these burials reflected that the dates of the remains and burials were roughly in the Warring-States Period to the Qin and Han Dynasties. The area where these remains and burials were located was the main inhabited area of the people of Kunming ethnic group; this excavation provided important materials for the researches on the features and the social situations of the bronze cultures in the Erhai Lake region.

Art. VII.—Notes on Persian Belúchistán. From the Persian of Mirza Mehdy Khán. Published Teheran, July, 1875

1876 ◽  
Vol 9 (1) ◽  
pp. 147-154
Author(s):  
A. H. Schindler
Keyword(s):  
Indian Ocean ◽  
Temperate Climate ◽  
The South ◽  
The West ◽  
The North ◽  
The People ◽  
The Indian Ocean ◽  
The Hill ◽  
Cool Climate

The part of Belúchistán now under Persian rule is bounded upon the north by Seistán, upon the east by Panjgúr and Kej, upon the south by the Indian Ocean, and upon the west by Núrámshír, Rúdbár, and the Báshákerd mountains.This country enjoys a variety of climates; almost unbearable heat exists on the Mekrán coast, we find a temperate climate on the hill slopes and on the slightly raised plains as at Duzek and Bampúr, and a cool climate in the mountainous districts Serhad and Bazmán. The heat at Jálq is said to be so intense in summer that the gazelles lie down exhausted in the plains, and let themselves be taken by the people without any trouble.

The Britons in Southern Scotland

Antiquity ◽  
1955 ◽  
Vol 29 (114) ◽  
pp. 77-88 ◽  
Author(s):  
Kenneth Jackson
Keyword(s):  
Iron Age ◽  
Roman Period ◽  
Anglo Saxon ◽  
Medieval Period ◽  
The West ◽  
Early Medieval Period ◽  
The North ◽  
Dark Ages ◽  
The People ◽  
Northern Portion

The archaeological background of the people of what is now Scotland south of the Forth and Clyde in the Roman period was a La Téne one, and specifically chiefly Iron Age B. This links them intimately with the Britons of southern Britain in the conglomeration of Celtic tribes who called themselves Brittones and spoke what we call the Brittonic or Ancient British form of Celtic, from which are descended the three modern languages of Welsh, Cornish and Breton. To the north of the Forth was a different people, the Picts. They too were Celts or partly Celts; probably not Brittones however, but a different branch of the Celtic race, though more closely related to the Brittones than to the Goidels of Ireland and (in later times) of the west of Scotland. Not being Brittonic, the Picts may be ignored here. Our southern Scottish Brittones are nothing but the northern portion of a common Brittonic population, from the southern portion of which come the people of Wales and Cornwall. Some historians speak of the northern Brittones as Welsh, following good Anglo-Saxon precedent, but this is apt to lead to confusion. The best term for them, in the Dark Ages and early Medieval period, as long as they survived, is ‘Cumbrians’, and for their language, ‘Cumbric’. They called themselves in Latin Cumbri and Cumbrenses, which is a Latinization of the native word Cymry, meaning ‘fellow-countrymen’, which both they and the Welsh used of themselves in common, and is still the Welsh name for the Welsh to the present day. The centre of their power was Strathclyde, the Clyde valley, with their capital at Dumbarton.

Migratory Labour from North-Wester Nigeria

Africa ◽  
1957 ◽  
Vol 27 (3) ◽  
pp. 251-261 ◽  
Author(s):  
R. Mansell Prothero
Keyword(s):  
Large Scale ◽  
Source Area ◽  
Dry Season ◽  
Labour Migration ◽  
Agricultural Activity ◽  
Wet Season ◽  
The North ◽  
The People ◽  
Limited Scale ◽  
Opening Paragraph

Opening ParagraphReaders of Africa will be well aware of population migration as a characteristic feature of a continent where movement between one part and another is largely unrestricted as compared with the more settled parts of the world. There is much evidence of large-scale tribal migrations in the past, of the age-old seasonal wanderings of herders, and of recent labour migration to centres of mineral and industrial production, the last particularly in Central and South Africa. Information is more limited concerning the features of labour migration in West Africa at the present day. In general it is thought that migrants leave their home areas, after the harvest at the commencement of the dry season, to seek work elsewhere for a period of from three to six months and then return to take up farming with the commencement of the next rains. The major source area for these migrants is to the north of the tenth parallel where the wet season is concentrated into a period of about four months, thus severely restricting agricultural activity. Cultivation during the dry season is possible only on a very limited scale. There is thus a considerable period of the year when the primary economic activity of the people is not possible. It is logical that they should seek work elsewhere.

Population Migrations, Colonization, and Social Changes in the Late Prehistoric Lower Yangtze River

2017 ◽  
Author(s):  
Tianlong Jiao
Keyword(s):  
Material Culture ◽  
Yangtze River ◽  
Cultural Landscape ◽  
Yangtze River Delta ◽  
River Delta ◽  
Social Changes ◽  
The North ◽  
Population Migrations ◽  
Lower Yangtze ◽  
Liangzhu Culture

This chapter presents a case study that challenges commonly used approaches in Chinese archaeology to population migration, diffusion, colonization, and material culture change. The dramatic decline of the Liangzhu culture in the Lower Yangtze River Delta around 2000 BC has been extensively investigated. Environmental disasters such as rising sea-level and flooding were suggested by some as the main factors, while others highlighted internal social conflicts or the exhaustive use of jades as the responsible forces. This chapter instead argues that the decline of Liangzhu culture was a dynamic process in which waves of population migrations from the Guangfulin culture in the north was the primary cause. These migrants were organized colonizers who were forced to expand southward by violent conflicts in the Central Plain. Archaeological data suggest the Guangfulin conquered the Liangzhu land and restructured the cultural landscape of the Lower Yangtze River Delta.

Chinese Archaeology since 1949

1977 ◽  
Vol 36 (4) ◽  
pp. 623-646 ◽  
Author(s):  
K. C. Chang
Keyword(s):  
Large Scale ◽  
Limited Resource ◽  
The Political ◽  
Unique Combination ◽  
Chinese People ◽  
New Materials ◽  
Chinese Archaeology ◽  
The People ◽  
New Material ◽  
To Come

The second half of the twentieth century may be remembered by Chinese archaeologists as the Golden Age of their discipline. A unique combination of factors and circumstances has produced, and will probably continue to produce for a time, enormous amounts of new material for the study of Chinese prehistory and history. These factors and circumstances include a deep-rooted interest of the Chinese people in their past, not only for its own sake but also for guidance, as lesson; the introduction, in the first half of the century, of Western archaeological science; systematic, large-scale, and sustained national projects to construct roads, canals, reservoirs, and buildings throughout China; and a conscious and conscientious effort to include archaeology as an important part of the political education of the people. This sudden flood of new data—most hitherto unknown, and many unexpected and almost unimaginable—provides unprecedented opportunities for gaining new and much richer knowledge of China's past. China scholars will be busy coping with the new materials for decades to come. They should count themselves extremely lucky, for such opportunities are not likely to arise again after the present century; archaeological relics are a limited resource, even in China.

Structural and metamorphic relationships between the Mount Ida and Monashee Groups at Mara Lake, British Columbia

1982 ◽  
Vol 19 (2) ◽  
pp. 288-307 ◽  
Author(s):  
Kent C. Nielsen
Keyword(s):  
British Columbia ◽  
Large Scale ◽  
Ductile Deformation ◽  
Late Triassic ◽  
Second Phase ◽  
The West ◽  
Late Mesozoic ◽  
The North ◽  
Phase Deformation ◽  
Metamorphic Core

Mara Lake, British Columbia straddles the boundary between the Monashee Group on the east and the Mount Ida Group on the west. Correlation of units across the southern end of Mara Lake indicates lithologic continuity between parts of the groups. Both groups have experienced four phases of deformation. Phases one and two are tight and recumbent, trending to the north and to the west, respectively. Phases three and four are open to closed and upright, trending northwest and northeast, respectively. Second-phase deformation includes large-scale tectonic slides that separate areas of consistent vergence. Slide surfaces are folded by third- and fourth-phase structures and outline domal outcrop patterns. Metamorphic grade increases from north to south along the west side of Mara Lake. Calc-silicate reactions involving the formation of diopside are characteristic. From west to east increasing grade is evident in the reaction of muscovite + quartz producing sillimanite + K-feldspar + water. These prograde reactions are related to relative position in the second-phase structure. The highest grade is located near the lowest slide surface. Greenschist conditions accompanied phase-three deformation. Fourth phase is characterized by hydrothermal alteration, brittle fracturing, and local faulting. First-phase deformation appears to be pre-Late Triassic whereas second and third phases are post-Late Triassic and pre-Cretaceous. The fourth phase is part of a regional Tertiary event. The third folding event is correlated with the development of the Chase antiform and the second-phase folding is related to the pervasive east–west fabric of the Shuswap Complex. The timing of these events indicates that the metamorphic core zone of the eastern Cordillera was relatively rigid during the late Mesozoic foreland thrust development. Ductile deformation significantly preceded thrusting and developed a fabric almost at right angles to the trend of the thrust belt.

Chinese Communist Treatment of the Origins and the Foundation of the Chinese Empire

1965 ◽  
Vol 23 ◽  
pp. 78-105 ◽  
Author(s):  
A. F. P. Hulsewé
Keyword(s):  
Yangtze River ◽  
Fourth Century ◽  
Fifth Century ◽  
The Yangtze River ◽  
The South ◽  
The West ◽  
Warring States ◽  
North East ◽  
The North ◽  
Chinese Empire

In antiquity, China was far from being the China we know today, neither in extent, nor in political and social organisation. To the south it did not extend beyond the Yangtze River, to the north it stopped short of the Mongolian steppe, to the north-east, only a small part of the south Manchurian plain was included, whereas in the west it merely went up to the easternmost part of what is now Kansu Province; the Szechwan plain was only included at the end of the fourth century B.C. Politically, the King of Chou was theoretically the overlord of most of this area, but in actual practice, independent rulers reigned over a congeries of larger and smaller states. As a result of wars of conquest, seven large states had come to be formed by the middle of the fifth century B.C. and these were engaged in a ceaseless struggle for supremacy. The time between the middle of the fifth century and 221 B.C., when the western state of Ch'in finally conquered all its rivals, is known as the period of the Warring States.

scholarly journals 'The worst disaster suffered by the people of Scotland in recorded history': climate change, dearth and pathogens in the long 14th century

2015 ◽  
Vol 144 ◽  
pp. 223-244
Author(s):  
Richard Oram
Keyword(s):  
Cultural Change ◽  
Large Scale ◽  
Environmental Data ◽  
Historical Discourse ◽  
Proxy Records ◽  
The North ◽  
Political Upheaval ◽  
The People ◽  
Large Scale Change

Informing historical and archaeological discourse with environmental data culled from documentary and climate proxy records is transforming understanding of political, social economic and cultural change across the North Atlantic and European Atlantic regions generally. Limited record evidence and region-specific proxy data has hindered engagement by historians of medieval Scotland with the exploration of environmental factors as motors for long term and large scale change and adoption of the interdisciplinary methodologies involved in their use. This paper seeks to provide an overview of the potential for such data and methodologies in providing context for the well-rehearsed narratives of political upheaval and socio-economic realignment that have characterised much past Scottish historical discourse.

scholarly journals Pemanfaatkan Potensi Lokal Melalui Pembuatan Susu Jagung Guna Mencegah Stunting Pada Desa Gejugan

2020 ◽  
Vol 1 (1) ◽  
pp. 18-21
Author(s):  
Agus Edi Setiyono ◽  
Ngatimun Ngatimun ◽  
Titik Musriati
Keyword(s):  
Food Source ◽  
Local Potential ◽  
North Coast ◽  
Socialization Process ◽  
The West ◽  
The North ◽  
Agricultural Produce ◽  
The People ◽  
Hands On ◽  
Good Nutrition

Gejugan Village is one of the villages in Probolinggo district on the north coast. Gejugan Village is in the west bordering Klaseman Village and Karangpranti Village, Pajarakan District. Gejugan village has local potential that can be developed from their agricultural produce, namely corn. Corn is an alternative food source that contains many nutrients. But the people here still don't have the knowledge to be able to use it. The Socialization Activity for Making SUJU (Corn Milk) to Prevent Stunting and Utilizing Local Potential is expected to provide more knowledge to the Gejugan community in utilizing existing local potential, especially processing corn into corn milk. Besides having good nutrition, corn milk also has more value in the economy. If it is processed properly and properly, this product can be sold in the market. The socialization of making corn milk was attended by 25 residents of Gejugan Village. Material for making corn milk was given by providing materials and hands-on practice during the event. Participants in the socialization of making corn milk enthusiastically listened to and practiced directly making corn milk during the socialization process. From the results of the socialization, the practiced corn milk resulted in 6 bottles of corn milk measuring 360 ml. Participants listened well and the material presented was well received by all participants present. Keywords: Local Potential, Corn Milk, Stunting

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