In the Land of Nagar: a survey around Tell Brak

Iraq ◽  
1996 ◽  
Vol 58 ◽  
pp. 51-64 ◽  
Author(s):  
J. Eidem ◽  
D. Warburton

During the campaign at Tell Brak in the spring of 1988 the present authors conducted a survey of tells in the vicinity of the site. Although comprehensive, the work was primarily intended to supplement the 1978 survey by K. Fielden, who investigated the sites surrounding the main tell at Brak itself and those on the lower Jaghjagh between the junction with the Wadi Radd and the modern town of Hassake, with a particular view to fourth and third millennium settlement (Fielden 1978/9).Within a rectangle of c. 170 km covered by the survey almost all the ancient settlements are found in a roughly triangular area half this size (its base being the lower Jaghjagh/Radd to the south and its apex immediately south of Tell Barri). Identifying this area as the “hinterland” of Brak is merely a locally suitable generalization, as Brak belongs to several systems, one being the macro-system of large urban centres scattered across the Habur Plains and adjacent areas, and another the micro-system of smaller settlements in the immediate vicinity of Brak itself. Brak was an important centre from prehistoric times until the late second millennium B.C., but its role necessarily changed through time, and the concomitant changes in the extent of the area economically and politically dependent upon it remain difficult to recognize. In this sense the area covered by our survey can be seen as partly arbitrary, partly reflecting some real limits. To the south, the French 1: 200,000 maps indicate further small sites on the southern fringe of the area visited, and further west on the lower Jaghjagh, beyond the area investigated by us, are numerous sites clustering along the banks of the wadi and its small affluents, many fairly large and with material of late fourth millennium and third millennium date. This area is relevant when studying the Brak hinterland, but it cannot be evaluated before the publication of the evidence collected by K. Fielden. The area to the north certainly overlaps, at least for certain periods, the hinterland of Tell Barri. Directly west and east of Brak, the cartographic gaps within and beyond the present survey are real or nearly so. To the west/northwest the modern village may obscure evidence, but apart from sites on the first affluent of the lower Jaghjagh there seems to be a fairly wide area here with little ancient occupation. Finally, to the east our area meets that surveyed by Meijer, and his map shows only two additional tells (Meijer 1986, Fig. 1, Nos. 269a and 269b), both Islamic. The two neighbouring sites (our Nos. 33 and 34) appear to be geomorphological features and not tells. The area covered should thus include most of the sites belonging to the micro-system of settlement around Tell Brak.

1970 ◽  
Vol 36 ◽  
pp. 125-151 ◽  
Author(s):  
John M. Coles ◽  
F. Alan Hibbert ◽  
Colin F. Clements

The Somerset Levels are the largest area of low-lying ground in south-west England, covering an extensive region between the highlands of Exmoor, the Brendon Hills and the Quantock Hills to the west, and the Cotswold and Mendip Hills to the east (Pl. XXIII, inset). The Quantock Hills and the Mendip Hills directly border the Levels themselves, and reach heights of over 250 metres above sea level. The valley between extends to 27 metres below sea level, but is filled to approximately the height of the present sea by a blue-grey clay. The Levels are bisected by the limestone hills of the Poldens, and both parts have other smaller areas of limestone and sand projecting above the peat deposits that cap the blue-grey clay filling. In this paper we are concerned with the northern part of the Levels, an area at present drained by the River Brue.The flat, peat-covered floor of the Brue Valley is some six kilometres wide and is flanked on the north by the Wedmore Ridge, and on the south by the Polden Hills (Pl. XXIII). In the centre of the valley, surrounded by the peat, is a group of islands of higher ground, Meare, Westhay, and Burtle. These islands, which would always have provided relatively dry ground in the Levels, are linked together by Neolithic trackways of the third millennium B.C. Several of these trackways formed the basis of a paper in these Proceedings in 1968 (Coles and Hibbert, 1968), which continued the work of Godwin and others (Godwin, 1960; Dewar and Godwin, 1963).


2021 ◽  
Vol 9 (12) ◽  
pp. 1419
Author(s):  
Xiaolin Ou ◽  
Junjiang Zhu ◽  
Sanzhong Li ◽  
Yonggang Jia ◽  
Zhongjia Jia ◽  
...  

We processed the raw multi-beam bathymetry data acquired in the central and northeastern part of the South China Sea by eliminating noise and abnormal water depth values caused by environmental factors, and a high resolution bathymetric map with a 20-m grid interval was constructed. Various scales of seafloor geomorphological features were identified from the data, including an image of Shenhu canyon, which is located in the northern continental margin of the South China Sea; submarine reticular dunes in the north of the Dongsha atoll; submarine parallel dunes in the northeast of the Dongsha atoll; and several seamounts in the southwest sub-basin and in the east sub-basin. In the processing step, various anomalies in the multi-beam bathymetry data were corrected. The optimal swath filtering and surface filtering methods were chosen for different scales of seafloor topography in order to restore the true geomorphological features. For the large-scale features with abrupt elevation changes, such as seamounts (heights of ~111–778 m) and submarine canyons (incision height of ~90–230 m), we applied swath filtering to remove noise from the full water depth range of the data, and then surface filtering to remove small noises in the local areas. For the reticular dunes and parallel dunes (heights of ~2–32 m), we applied only surface filtering to refine the data. Based on the geometries of the geomorphological features with different scales, the marine hydrodynamic conditions, and the regional structure in the local areas, we propose that the Shenhu submarine canyon was formed by turbidity current erosion during the Sag subsidence and the sediment collapse. The submarine reticular dunes in the north of the Dongsha atoll were built by the multi-direction dominant currents caused by the previously recognised internal solitary waves around the Dongsha atoll. The submarine parallel dunes in the northeast of the Dongsha atoll were built by the repeated washing of sediments with the influence of the tidal currents and internal solitary waves. The conical, linear and irregular seamounts identified from the bathymetry data were formed during the spreading of the southwest sub-basin and the east sub-basin. The identified seamounts in the multi-beam bathymetry data are correlated to deep magmatic activities, the Zhongnan transform fault and the NE-trending faults.


Author(s):  
Luigi Guiso ◽  
Paolo Pinotti

This chapter documents a sharp reversal in electoral participation between the North and the South of Italy after the 1912 enfranchisement which extended voting rights from a limited élite to (almost) all adult males. When voting was restricted to the élite, electoral turnout was higher in the South but falls significantly below that in the North after the enfranchisement. This gap has never been bridged over the following century and participation remains lower in the South despite the enrichment of democratic institutions and extension of voting rights to women during the post-war democratic republic. This pattern is consistent with a simple theoretical framework in which individuals' voting in political elections is affected by private benefits and civic duty. Only elites can grab private benefits from participation in politics, and civic culture differs across communities. Extension of voting rights to non-elites results in a significant transfer of power to their political organizations only among populations with a high sense of civic duties. Together with the gap in participation between North and South our findings suggest that democratization can benefit non-elites only when the latter have already a high sense of civic capital and is unlikely to induce norms of civic behavior.


1986 ◽  
Vol 52 ◽  
pp. 31-51 ◽  
Author(s):  
Peter Drewett ◽  
C. Cartwright ◽  
S. Browne ◽  
K. D. Thomas ◽  
A. Thompson ◽  
...  

An extensively plough-damaged oval barrow of the third millennium bc was excavated. The entire mound had been removed by ploughing. No burials were found under the site of the mound but disarticulated human skeletal material was found in the ditches. The main flanking ditches appear to have silted in naturally with evidence of Beaker activity and Romano-British agriculture in the higher levels. Some evidence of deliberate back-filling, including the burial of carved chalk objects, was found in the ditches at the east end. A single Saxon hut was excavated in the north-east corner of the barrow and a rubbish deposit containing Middle Saxon pottery was found in the upper levels of the ditch in the south-west corner of the barrow.


Author(s):  
Semerhei-Chumachenko A. B. ◽  
Agayar E. V. ◽  
Zhuk D. O.

Tornadoes and strong squalls are dangerous for almost all spheres of human life and the economy of the region. The degree of negative impact depends on their type, quantity, intensity, area of formation and geographical features of the territory. The article defines the dynamics of the number of tornadoes and strong squalls in the North-Western Black Sea region (Odessa, Nikolayev and Kherson regions of Ukraine) from 2006 to 2020.Geographical position of the south-west of Ukraine, synoptic processes and a variety of climatic conditions contribute to the frequent occurrence of severe convective phenomena and creating the extraordinary complexity of their space-time distribution. The study revealed current trends in the formation of dangerous convective phenomena in the south-west of Ukraine. One of the most squall-prone regions of Ukraine is the territory of the North-Western Black Sea region. During 2006-2020 there was an increase in the number of squalls and tornadoes in the North-Western Black Sea region in comparison with previous years.


Africa ◽  
1948 ◽  
Vol 18 (4) ◽  
pp. 259-271
Author(s):  
F. J. Pedler

The Province of Zaria, in Northern Nigeria, has a population of some 540,000.The central portion of the Province, covering the largest part of the area, is sparsely populated and contains some pagan tribes who have little to do with the economy of their Hausa neighbours to the north. There is a southern fringe, more thickly peopled, where Christian missions are established and where the people buy and sell with neighbouring communities to the south. This paper is not concerned with these parts. We shall deal only with the northern part of the Province. Its area is about 7,400 square miles. The African population of this area which we are considering amounts to some 323,000, of whom about 40,000 are Fulani cattle people, about 10,000 southern clerks and workmen, and the rest Hausa farmers and traders. The European and Syrian population, comprising about 360 civilians and about 120 military personnel, is fairly evenly divided between the two towns of Zaria and Kaduna. The country stands on the northern edge of the ‘middle belt’ of orchard bush, and extends in places into the southern fringe of the great savannah belt of the western Sudan. Its climate is therefore a good deal kinder than that of the barer lands of Kano and Sokoto, and more suitable for intensive peasant cultivation than the wetter countries to the south where the tsetse and other insect pests have held back indigenous development. The economic activities of the African population will be described in detail hereafter.


The paper now presented to the Royal Society is a sequel to one on the same subject read here on April 27, 1893, and published in the Transactions for that year. In that paper the subject was explained at some length; it will, therefore, be unnecessary in this to repeat more than a very few explanatory observations. The aim of this inquiry is to deduce the date of the foundation of a Greek (or Egyptian) temple from its orientation, but I confine myself entirely to Greek temples, in which, however, the same practice was followed which had previously been reduced to a system in Egypt ( vide ‘ Dawn of Astronomy,’ by Sir J. N. Lockyer). Almost all the temples in Greece and its Colonies had an Easterly frontage, and the principal religious function in each temple took place on the morning of the day when the sun, as it rose above the visible horizon, shone through the open Eastern door directly upon the sanctuary, where there was usually a statue of the deity in the centre. As some time was requisite for the priests to prepare for the ceremony, the orientation of the temple was so directed as to combine with the sunrise the previous heliacal rising or setting of some conspicuous star which could also be observed from the sanctuary. In the absence of clocks the heliacal rising or setting of stars was very greatly observed by the ancients—the meaning of the term being that the star, when very slightly above the horizon, should just be visible in the twilight, before being extinguished by the dawn. The angle of the orientation depended primarily on the time of year chosen for the principal festival, but it would be liable to a slight modification for the sake of combining an heliacal star with the sunrise, and it is the latter consideration which offers the means of determining the date of foundation, because the stars, owing to the precession of the equinoxes, are affected by a slow, but steady movement, which alters the amplitude, as it is called, of their rising or setting—viz., the angular distance from the true East or West as the case may be, and which is reckoned positive if towards the North, and negative if towards the South.


2002 ◽  
Vol 30 (1) ◽  
pp. 31-36
Author(s):  
George J. Sefa Dei ◽  
Alireza Asgharzadeh

Defined primarily in terms of the exodus of the highly talented from the Southern countries to the North, the phenomenon known as “brain drain” has gained in importance during recent decades and years. Changing global conditions, unprecedented developments in information and electronic technology, globalization, and widening of the gap between the South and the North have focused attention on the brain drain. We begin this article by discussing the nature of the brain drain, briefly noting that it occurs in three settings: internal, regional, and global. Our argument here is that brain drain occurs in almost all societies, initially from poorer and impoverished rural areas to relatively rich and developing urban centers within national boundaries and later (or sometimes concurrently) to more developed and wealthy regions and neighboring countries.


2000 ◽  
Vol 179 ◽  
pp. 201-204
Author(s):  
Vojtech Rušin ◽  
Milan Minarovjech ◽  
Milan Rybanský

AbstractLong-term cyclic variations in the distribution of prominences and intensities of green (530.3 nm) and red (637.4 nm) coronal emission lines over solar cycles 18–23 are presented. Polar prominence branches will reach the poles at different epochs in cycle 23: the north branch at the beginning in 2002 and the south branch a year later (2003), respectively. The local maxima of intensities in the green line show both poleward- and equatorward-migrating branches. The poleward branches will reach the poles around cycle maxima like prominences, while the equatorward branches show a duration of 18 years and will end in cycle minima (2007). The red corona shows mostly equatorward branches. The possibility that these branches begin to develop at high latitudes in the preceding cycles cannot be excluded.


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