Achehnese Control over West Sumatra up to the Treaty of Painan, 1663

1969 ◽  
Vol 10 (3) ◽  
pp. 453-479 ◽  
Author(s):  
J. Kathirithamby-Wells
Keyword(s):  
Fifteenth Century ◽  
Coastal Region ◽  
Central Control ◽  
Central Administration ◽  
Royal Family ◽  
Important Distinction ◽  
The North ◽  
Northern Border ◽  
West Sumatra ◽  
Central Sumatra

The west Sumatran coast between Barus in the north and Inderapura in the south, which came under Achehnese rule, was originally part of the Minangkabau kingdom which developed in the fourteenth century and reigned supreme in central Sumatra up to about the end of the following century The Padang lowlands and the coastal region up to the northern border of Silebar were considered in the Alam Minangkabau as part of the rantau, or acquired territories, as different from the darat, or nucleus of the kingdom formed by the 3 luaks (or districts) of Agam, Tanah Data and Lima Puloh Kota. The important distinction between the darat and the rantau was that the former was administered on genealogical principles with a penghulu at the head of each negeri in the luak while the rantau was divided into several parts and was under the territorial rule of various rajas who were members of the royal family.2 Beneath the rajas appointed by the central administration at Pagarruyong were minor rajas and penghulus selected from amongst the local inhabitants who were in charge of the various districts. In return for the help and protection provided by the darat, especially in times of trouble, the negeris in the rantau were obliged to pay homage and tribute to Pagarruyong, a duty which they evaded during periods of weak central control, as at the end of the fifteenth century.

Ketilidian structure and the rapakivi suite between Lindenow Fjord and Kap Farvel, South-East Greenland

2000 ◽  
pp. 50-59
Author(s):  
Brian Chadwick ◽  
Adam A. Garde ◽  
John Grocott ◽  
Ken J.W. McCaffrey ◽  
Mike A. Hamilton
Keyword(s):  
Coastal Region ◽  
Field Work ◽  
Natural Environment Research Council ◽  
East Greenland ◽  
The North ◽  
Tectonic Processes ◽  
Field Investigations ◽  
North Eastern ◽  
Bad Weather ◽  
North Eastern Part

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Chadwick, B., Garde, A. A., Grocott, J., McCaffrey, K. J., & Hamilton, M. A. (2000). Ketilidian structure and the rapakivi suite between Lindenow Fjord and Kap Farvel, South-East Greenland. Geology of Greenland Survey Bulletin, 186, 50-59. https://doi.org/10.34194/ggub.v186.5215 _______________ The southern tip of Greenland is underlain by the Palaeoproterozoic Ketilidian orogen (e.g. Chadwick & Garde 1996; Garde et al. 1998a). Field investigations in the summer of 1999 were focused on the structure of migmatites (metatexites) and garnetiferous granites (diatexites) of the Pelite Zone in the coastal region of South-East Greenland between Lindenow Fjord and Kap Farvel (Figs 1, 2). Here, we first address the tectonic evolution in the Pelite Zone in that region and its correlation with that in the Psammite Zone further north. Then, the structure and intrusive relationships of the rapakivi suite in the Pelite Zone are discussed, including particular reference to the interpretation of the controversial outcrop on Qernertoq (Figs 2, 8). Studies of the structure of the north-eastern part of the Julianehåb batholith around Qulleq were continued briefly from 1998 but are not addressed here (Fig. 1; Garde et al. 1999). The field study was keyed to an interpretation of the Ketilidian orogen as a whole, including controls of rates of thermal and tectonic processes in convergent settings. Earlier Survey field work (project SUPRASYD, 1992–1996) had as its principal target an evaluation of the economic potential of the orogen (Nielsen et al. 1993). Ensuing plate-tectonic studies were mainly funded in 1997–1998 by Danish research foundations and in 1999 by the Natural Environment Research Council, UK. The five-week programme in 1999 was seriously disrupted by bad weather, common in this part of Greenland, and our objectives were only just achieved. Telestation Prins Christian Sund was the base for our operations (Fig. 2), which were flown with a small helicopter (Hughes MD-500).

scholarly journals Mitigating natural events to avoid disaster in public school buildings: seismic retrofitting of SDN 42 Korong Gadang

2018 ◽  
Vol 229 ◽  
pp. 02021
Author(s):  
James Mwangi ◽  
Laura Putri ◽  
Listhbeth Collins
Keyword(s):  
School Facilities ◽  
Seismic Retrofitting ◽  
Building Structures ◽  
National Agency ◽  
Electrical Grid ◽  
The North ◽  
Australian Plate ◽  
West Sumatra

With over 50 million students, Indonesia has the fourth largest education system in the world. The first twelve years of education are compulsory for all citizens. The students, together with over 3 million teachers spend six (or five in some cases) days a week at over 300,000 schools, typically from 6:30 AM to 2 (or 3) PM. Geographically, Indonesia is traversed by the infamous “ring of fire” and prone to natural events resulting from the tectonic plate movements of the Australian Plate from the South, the Eurasian and Sunda Plates from the North and the Philippine Plate from the East. Left unmitigated, these natural events would lead to natural disasters emanating from resulting earthquakes and leading to tsunamis, landslides, the collapse of building structures and failure of lifelines (roads, pipelines, electrical grid, etc.). In an effort to provide disaster-safe schools, the National Agency for Disaster Management has required that school facilities be a community center in case of disasters and serve as emergency shelters. Retrofit of existing buildings will be needed to comply with government guidelines. This paper presents a case study of the determination of structural deficiencies of an existing school building in SDN 42 Korong Gadang, Padang, West Sumatra and implementation of a seismic retrofit (design and construction) at the same building to mitigate potential earthquake disaster.

Literary Conduits for ‘Consent’

2016 ◽  
Vol 19 (2) ◽  
pp. 322-350 ◽  
Author(s):  
Pankaj Kumar Jha
Keyword(s):  
Sixteenth Century ◽  
Fifteenth Century ◽  
North India ◽  
Indian Society ◽  
Historical Process ◽  
The North ◽  
Literary Cultures

The making of the imperial subjects is as much a matter of historical process as the emergence of the empire. In the case of the Mughal state, this process started much before its actual establishment in the sixteenth century. The fifteenth century in North India was a period of unusual cultural ferment. The emergence of the Mughal imperial formation in the next century was intimately related to the fast congealing tendency of the north Indian society towards greater disciplining of itself. This tendency is evident in the multilingual literary cultures and diverse knowledge formations of the long fifteenth century.

scholarly journals A Study of the Surface Air Temperature Variations in Nigeria

2017 ◽  
Vol 11 (1) ◽  
pp. 54-70 ◽  
Author(s):  
Najib Yusuf ◽  
Daniel Okoh ◽  
Ibrahim Musa ◽  
Samson Adedoja ◽  
Rabia Said
Keyword(s):  
Air Temperature ◽  
Cloud Cover ◽  
Coastal Region ◽  
Surface Air Temperature ◽  
The South ◽  
Climate Type ◽  
Temperature Variations ◽  
North Central ◽  
North East ◽  
The North

Background: Simultaneous measurements of air temperature were carried out using automatic weather stations at 14 tropical locations in Nigeria. Diurnal variations were derived from the 5-minute update cycle initial data for the years ranging between 2007 and 2013. The temperature trends in Nigeria revealed a continuous variability that is seasonally dependent within any particular year considered. Method: The analysis was carried out using available data from the network and the results are presented with a focus to characterize the temperature variations at different locations in the country using the mean, maximum and minimum temperatures from the north which is arid in nature to the south, which is a tropical monsoon climate type and a coastal region. Result: In overall, temperature variations in Nigeria were observed to have higher values in the far north, attributed to the influence of Sahara Desert, which has less cloud cover and therefore is more transparent to solar irradiance and lowers values in the south, where there are more cloud cover and abundant vegetation. Conclusion: Measured maximum and minimum temperatures in Nigeria are respectively 43.1°C at Yola (north-east part of Nigeria) and 10.2°C for Jos (north-central part of Nigeria). The least temperature variations were recorded for stations in the southern part of the country, while the largest variations were recorded in the north-central region of the country.

Clerical Poverty in Early Sixteenth-Century England: Some East Anglian Evidence

1986 ◽  
Vol 37 (3) ◽  
pp. 389-396 ◽  
Author(s):  
John Pound
Keyword(s):  
Sixteenth Century ◽  
Social Status ◽  
Fifteenth Century ◽  
Average Salary ◽  
The North ◽  
High Social Status

The economic standing of the English parochial clergy in the early sixteenth century has been re-examined recently by Michael Zell, and the evidence at his disposal suggests that many of them were poverty-stricken in the extreme. He points to the large surplus of unendowed curates, chaplains and the like, and to the fact that when employment was available it was neither rewarding, in a monetary sense, nor necessarily secure. Stipends were officially regulated by an early fifteenth-century statute which set a maximum of £5 6s. 8d. per annum, and ‘evidence from all regions of England indicates that very rarely were curates and chaplains given more than that’. It was not uncommon for areas in the north to pay even less than this. In Lancashire, for example, the average salary of about 100 curates and chaplains in 1524 was £2 9s. 6d. In the East Riding of Yorkshire a year later it was £4. On the basis of such evidence, Mr Zell reasonably concludes that the unbeneficed clergy must have found it very difficult to survive, and that ‘the average country priest could not have been a person of high social status’.

scholarly journals Preface

1857 ◽  
Vol 65 ◽  
pp. v-xi
Author(s):  
Lambert B. Larking
Keyword(s):  
Fifteenth Century ◽  
Public Library ◽  
The Public ◽  
The North

In a communication from Mr. Milward to the Archælogical Journal, December, 1850, the following statement occurs, with reference to the charters, &c. preserved in the Eecord Office at Malta.“There is also a volume of the fifteenth century, containing the accounts of the Commanderies. It is a continuation of an older and still more interesting volume which has, by some means, found its way into the Public Library. The latter gives the accounts of the property belonging to the Order in England and Scotland. Unfortunately these accounts are very difficult to decipher. I remember, however, looking over it, in company with a Scotch gentleman, who had edited various antiquarian works, and with another gentleman from Northumberland. The Scotchman read the MS. with tolerable facility; my friend from the North repeatedly identified certain allusions with property that he knew, and felt much interest in the book. There is also much that is valuable in the statement of the different prices paid for commodities, labour, &c.”

Identifying the Country of Meilugudun and the Significant Value of Zhou Qufei’s Lingwai daida

2017 ◽  
Vol 21 (1) ◽  
pp. 1-43
Author(s):  
Victoria Almonte
Keyword(s):  
Fifteenth Century ◽  
Song Dynasty ◽  
Social Differences ◽  
Political Consequences ◽  
Southern Song ◽  
The North ◽  
Maritime Silk Road ◽  
Chinese Texts ◽  
The Relationship ◽  
The City

Abstract During the last century, considerable interest arose regarding Chinese knowledge of western territories, with a long list of works being published on the topic. Joseph Needham’s Science and Civilisation in China (1959) states that Arab thinking had clearly influenced the Chinese conception of geography over the centuries. Zhang Xinglang analyses the relationship between the Chinese empire and countries overseas, focusing on Islamic countries and particularly those in the north of Africa. Feng Chengjun’s western territories toponyms and Gudai nanhai diming huishi have provided two powerful and even fundamental tools for the research presented here. The first gathers together a large collection of toponyms from various literary works; these are written in western language with their relative transcription or translation in Chinese. The second, the Gudai nanhai diming huishi, is divided in two volumes analysing many Chinese toponyms and their use in several geographical works. Li Qingxin’s Haishang Sichou zhilu, focuses on the development of the Maritime Silk Road and its economic-political consequences for China’s empire. Gabriele Foccardi’s research focuses instead on the motives for Chinese travellers and their expeditions, highlighting the historical and social differences between the different dynasties. Friedrich Hirth and William Rockhill provide a crucial literary resource with their translation of Zhao Rukuo’s work, Zhufanzhi (1966), as does J.V.G. Mills with his annotated translation of Ma Huan’s Yingya shenglan, a journey work of the fifteenth century. Yang Wuquan’s research into Zhou Qufei’s work, published in 1999, identifies several toponyms used by Zhou and compares several foreign geographical works. Zhou Qufei and Zhao Rukuo were both imperial officials during the Southern Song dynasty. They spent many years in the border territories of China: Zhou Qufei in Qinzhou, Guangxi province, and Zhao Rukuo in Quanzhou, Fujian province. Their works mention several toponyms never used before in Chinese texts: ‘Meilugudun’, or ‘Meilugu’ (as written by Zhao Rukuo), is one of these. The identification of this toponym has not been determined until now. Therefore, the aim of this paper is to determine which kingdom was identified with the ‘Meilugudun’ toponym during the Song Dynasty. Two different questions are here discussed and resolved. First, can the land of Meilugudun be identified with the city of Merv in Turkmenistan? Second, do Zhou’s ‘Meilugudun’ and Zhao’s ‘Meilugu’ both stand for the same place? This paper can be divided into four sections. The first section focuses on Zhou Qufei, the second on Zhao Rukuo. The third analyses and compares previous scholars’ studies. The fourth proposes the new identification of the Meilugudun kingdom.

Etude tectonique du secteur Pradoluengo-Alarcia, Sierra de la Demanda (chaines iberiques, Espagne)

1963 ◽  
Vol S7-V (7) ◽  
pp. 1068-1075
Author(s):  
Michel Colchen
Keyword(s):  
Basement Complex ◽  
Direction Parallel ◽  
The North ◽  
Basement Rocks ◽  
Northern Border ◽  
Tectonic Study

Abstract A tectonic study of the area northwest of Sierra de la Demanda (Spain) revealed Tertiary orogenic phases represented by overlaps and overturnings. Towards the northern border, the Cambrian overrides Carboniferous, Triassic and Jurassic formations; the Carboniferous-Triassic units appear overturned under the Cambrian; and the Jurassic formations are affected locally by a system of dislodged slices of nappes associated with imbricate basement rocks. Two major directions of deformation suggest the presence of two successive orogenic phases. The first phase, older than the Oligocene conglomerates, folded the units above the basement in a NW-SE direction, parallel to the north oriented horst in the basement complex. In the post-Oligocene phase NE-SW imbrication affected the conglomerates as well as the basement and overlying units.

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