scholarly journals Decolonizando Tarteso en el estudio de la Protohistoria mediterránea.

Anduli ◽  
2021 ◽  
pp. 159-177
Author(s):  
Pablo González-Zambrano
Keyword(s):  
Historical Narrative ◽  
The South ◽  
The Past ◽  
The North ◽  
East And West ◽  
The Mediterranean

Tartessus has been one of the most controversial subjects in Spanish historiography for the last five centuries, although its mentions date back to the 7th century BC. In this work we analyze how the concept of Tartessus has been extrapolated to each context of historiographic production, and the different uses that have been made of it. To do this, we examine works that deal with the theme and context of Tartessus and analyze the discourse to understand how the historical narrative of the present has been colonizing the past of the southern peninsula. Such analysis has led us to discern that Tartessus, with its colonial connotations, has functioned as a hinge between the north and the south of the peninsula and as the scene of the struggle between east and west within the Mediterranean framework. Hence, Andalusian protohistory has served as a legitimizing basis for claims of the north over the south.

Ino-Leukothea between East and West

2006 ◽  
Vol 6 (1) ◽  
pp. 105-121 ◽  
Author(s):  
Margalit Finkelberg
Keyword(s):  
Bronze Age ◽  
Complex Network ◽  
Near East ◽  
Mediterranean Coast ◽  
Native Population ◽  
The South ◽  
The North ◽  
East And West ◽  
The Mediterranean ◽  
Of Greece

AbstractUntil recently it has generally been taken for granted that cultural contacts between the Aegean and the Near East invariably proceeded in one direction, from East to West. It seems, however, that recent archaeological discoveries are about to change this picture. As these discoveries demonstrate, with the collapse of the Mycenaean civilization some Bronze Age populations of Greece migrated to the Levant and settled along the Mediterranean coast from Tarsos in the north to Ashkelon in the south, eventually to be assimilated into the native population. This fact suggests a much more complex network of relations between the Aegean and the Near East than the simple one-sided cultural dependence which has usually been postulated.

Prehistoric Galilee

Antiquity ◽  
1927 ◽  
Vol 1 (3) ◽  
pp. 299-310 ◽  
Author(s):  
F. Turville Petre
Keyword(s):  
Sea Level ◽  
Coastal Plain ◽  
Limited Extent ◽  
The South ◽  
Jordan Valley ◽  
Central Plateau ◽  
The North ◽  
East And West ◽  
The Mediterranean ◽  
Western Side

The district with which we are concerned constitutes the northern section of Galilee between the Nahr-el-Kasmiyeh and the Merj Ayun to the north, and the plains of Haifa and Asochis (Sahel-el-Buttauf) and the Wadi Hammam to the south; to the east and west its boundaries are respectively the Jordan and the Mediterranean. The greater part of the region is occupied by a central limestone massif, the Galilean highlands, which rise in a series of terraces from the Jordan valley to a height of nearly 4000 feet above sea level, and then descend steeply to the Mediterranean coastal plain. Much of this country, especially on the western side of the watershed, is barren and uncultivable, but the high central plateau in the north from Yarun to Tibnin and the lower plateaux of Kades and Safsaf include some of the most productive corn-growing districts west of the Jordan. The beds of the larger valleys also, which even in summer are not entirely waterless, provide fertile garden land and are mostly highly cultivated. The more rocky parts of the region provide scant pasturage for flocks of goats, and in most places the olive is cultivated to a limited extent.

scholarly journals ‘Et pour les Belges la même chose’?

2021 ◽  
Vol 136 (2) ◽  
pp. 24-41
Author(s):  
Marc Boone ◽  
Tom Verschaffel
Keyword(s):  
The South ◽  
Historical Scholarship ◽  
Half Century ◽  
The Past ◽  
The North ◽  
Past Half Century ◽  
University History ◽  
Past Half

Bijdragen en Mededelingen betreffende de Geschiedenis der Nederlanden was en is een Nederlands-Belgisch project. Belgische, in de realiteit enkel Vlaamse, historici hebben een rol gespeeld in de redactie en als auteurs van bijdragen. Het aandeel van het Zuiden is altijd kleiner geweest dan dat van het Noorden. Het tijdschrift poogde via een (meestal) paritaire samenstelling van de redactie en initiatieven, zoals comparatief opgezette themadossiers, de balans te herstellen. Aangezien het tijdschrift, zeker wat het Zuiden betreft, nauw verbonden was met de universitaire historische vakgroepen, in het bijzonder die van Gent en Leuven, weerspiegelen de evoluties van dit Belgische aandeel algemene verschuivingen in het academisch bedrijf. Uitbreiding van de onderzoeksfinanciering zorgde voor een aangroei en voor een verjonging en vervrouwelijking van het auteursbestand en van de redactie. Ook andere ontwikkelingen in het historisch bedrijf van de voorbije halve eeuw, zoals het verschijnen van nieuwe tijdschriften en de internationalisering van het onderzoek, hadden een impact op de plaats van het tijdschrift en bijgevolg ook op Vlaamse bijdragen en hun auteurs.Bijdragen en Mededelingen betreffende de Geschiedenis der Nederlanden was and is a Dutch-Belgian project. Belgian, though in fact only Flemish, historians have edited and authored contributions. The share from the South has always been smaller than that from the North. Via a generally balanced composition of the editorial board and initiatives, such as comparatively structured special issues and forums, the journal aimed to restore the balance. Since the journal, especially in the South, was closely affiliated with university history departments, those of the universities of Ghent and Leuven in particular, the evolutions of this Belgian share therefore reflect general shifts in academia. Expansion of research financing brought about accretion, rejuvenation and feminisation of the stock of authors and editors alike. Other developments in historical scholarship from the past half century, such as the appearance of new journals and internationalisation of research, had an impact on the positioning of the journal and consequently on Flemish contributions and their authors as well.

scholarly journals IV.—On the Denudation of Western Brittany

1869 ◽  
Vol 6 (64) ◽  
pp. 442-446
Author(s):  
G. A. Lebour
Keyword(s):  
Sedimentary Rocks ◽  
The South ◽  
Upper Carboniferous ◽  
The North ◽  
Upper Silurian ◽  
East And West

Geology.—Stated roughly, the geology of the Department of Finistère may be said to consist of two masses of granite, one to the north and one to the south, enclosing between them nearly the whole of the sedimentary rocks of the district. These consist of Cambrian slates and gneiss, Lower, Middle, and Upper Silurian slates and grits, and very small and unimportant patches of Upper Carboniferous shales. The entire mass of these deposits has an east and west direction, and occupies the central part of the Department.

scholarly journals II.—Excavations at Sparta, 1906: § 12.—The Roman Stoa and the later Fortifications

1906 ◽  
Vol 12 ◽  
pp. 415-430
Author(s):  
Ramsay Traquair
Keyword(s):  
Plate Viii ◽  
The South ◽  
South Side ◽  
South Eastern ◽  
The North ◽  
Complete Part ◽  
North Side ◽  
Imperial Period ◽  
East And West ◽  
Barrel Vaults

In plan the walls surrounding the Acropolis of Sparta form an irregular oblong, terminated to the east and west by two small hills which formed citadels or outlook points. Though no single complete part remains, and in many places the walls are levelled to the ground, the lines can still be traced fairly completely. (Plate VIII. 3.)At the south eastern corner are the ruins of a Roman Stoa of the Imperial period (A). They shew a series of small compartments (Fig. 1), covered with barrel vaults, ten on either side of three larger central rooms, which are roofed with crossgroined vaults and large semicircular niches at the back. The ground on the north side is as high as the vaults and originally must have formed a terrace overlooking the street on to which the Stoa opened on its south side.

Middle Bronze Age Long Distance Exchange through Europe and Beyond

2020 ◽  
Vol 26 (2) ◽  
pp. 266-274
Author(s):  
Flemming Kaul
Keyword(s):  
Chemical Composition ◽  
Bronze Age ◽  
Glass Beads ◽  
The South ◽  
Long Distance ◽  
Blue Glass ◽  
The North ◽  
Southern Scandinavia ◽  
Middle Bronze Age ◽  
The Mediterranean

Abstract The introduction of the folding stool and the single-edged razor into Southern Scandinavia, as well as the testimony of chariot use during the Nordic Bronze Age Period II (1500-1300 BC), give evidence of the transfer of ideas from the Mediterranean to the North. Recent analyses of the chemical composition of blue glass beads from well-dated Danish Bronze Age burials have revealed evidence for the opening of long distance exchange routes around 1400 BC between Egypt, Mesopotamia and South Scandinavia. When including comparative material from glass workshops in Egypt and finds of glass from Mesopotamia, it becomes clear that glass from those distant lands reached Scandinavia. The routes of exchange can be traced through Europe based on finds of amber from the North and glass from the South.

scholarly journals The Literary Evidence for the Topography of Thebes

1911 ◽  
Vol 17 ◽  
pp. 29-53
Author(s):  
A. W. Gomme
Keyword(s):  
Small Group ◽  
Long Range ◽  
The South ◽  
Archaeological Evidence ◽  
The North ◽  
East And West ◽  
East End ◽  
The Town

Fabricius' view, based on archaeological evidence, that the lower town of Thebes extended over the high hills East and West of the Kadmeia (Pl. XIX. A) has in general been accepted by subsequent scholars: it has only been modified by the theory of Kalopais and Soteriádes, which makes the town extend yet further eastwards.How weak this archaeological evidence is, was shown by the criticisms of Wilamowitz and Frazer; and the literary evidence suggests quite a different view. It is to this that I wish to draw attention. Any theory based on such evidence is of course liable to be upset at any moment by fresh archaeological discoveries. But in the present uncertainty it may be useful to see to what theory this evidence seems to lead us.Thebes is situate towards the East end of the long range of low, cultivated hills, running eastwards from Helikon as far as Mount Sorós, and dividing the Aonian plain on the North from that of Leuktra and Plataia on the South. Here is a small group of hills, none of them rising much above the general height of the range, divided by the three streams flowing from. South to North, the Plakiótissa (identified with Dirke), a small and nameless brook, and the H. Joánnes (the ancient Ismenos)

On the northern rockling Ciliata septentrionalis (Collett) in the Plymouth area

1975 ◽  
Vol 55 (4) ◽  
pp. 925-931 ◽  
Author(s):  
P. R. Dando
Keyword(s):  
Larval Development ◽  
The South ◽  
Northern Norway ◽  
The Past ◽  
The North

The known range of the northern rockling, Ciliata septentrionalis, extends from Iceland and northern Norway in the north to Plymouth in the south (Wheeler, 1965). This species has probably been confused with the five-bearded rockling, C. mustela (L.), in the past (Wheeler, 1969) and this together with the small size of the fish, enabling it to escape through the mesh of most trawls, may explain the paucity of records and knowledge of the species. Brook, (1885, 1888) described the egg and larval development of C. mustela but the egg and larva of C. septentrionalis have not been described. It is probable that the abundance of both these species can only be estimated by a combination of fecundity studies and egg and larval counts.

The West Court at Perachora

1967 ◽  
Vol 62 ◽  
pp. 353-371
Author(s):  
J. J. Coulton
Keyword(s):  
Short Distance ◽  
Sixth Century ◽  
East Side ◽  
The South ◽  
The West ◽  
Rock Face ◽  
North East ◽  
The North ◽  
South West ◽  
East And West

About 10 metres south-west of the sixth-century temple of Hera Akraia at Perachora, and nearly due west of the little harbour lies the small courtyard previously known as the ‘Agora’. Since its purpose is not known, it will here be non-committally referred to as the West Court. It was first excavated in 1932, and more fully, under the supervision of J. K. Brock, in 1933, but it was not entirely cleared until 1939, and it was at that time that the Roman house which stood in the middle of the court was demolished. The West Court is discussed briefly (under the name of ‘Agora’) in Perachora 1 and in the preliminary reports of the Perachora excavations. Short supplementary excavations were carried out in 1964 and 1966 to examine certain points of the structure.In shape the West Court is an irregular pentagon, about 24 metres from north to south and the same from east to west (Fig. 1; Plate 91 a, b). It is enclosed on the west, north, and on part, at least, of the east side by a wall of orthostates on an ashlar foundation. For a short distance on either side of the south corner, the court is bounded by a vertically dressed rock face which is extended to the north-east and west by walls of polygonal masonry. At the south-west corner the west orthostate wall butts against the polygonal wall, which continues for about 0·80 m. beyond it and then returns north for about 8 metres behind it.

scholarly journals XVII. Description of the mineral bason in the counties of Monmouth, Glamorgan, Brecon, Carmarthen, and Pembroke. By Mr. Edward Martin

1806 ◽  
Vol 96 ◽  
pp. 342-347 ◽  
Keyword(s):  
Iron Ore ◽  
The South ◽  
South Side ◽  
The North ◽  
North Side ◽  
South Wales ◽  
East And West ◽  
East End

1. The irregular oval line, delineated on the annexed map (Plate XIV.) shows nearly the inner edge of a limestone bason, in which all the strata of coal and iron ore (commonly called Iron Stone) in South Wales are deposited; the length of this bason is upwards of 100 miles, and the average breadth in the counties of Monmouth, Glamorgan, Carmarthen, and part of Brecon, is from 18 to 20 miles, and in Pembrokeshire only from 3 to 5 miles. 2. On the north side of a line, that may be drawn in an east and west direction, ranging nearly through the middle of this bason, all the strata rise gradually northward; and on the south side of this line they rise southward, till they come to the surface, except at the east end, which is in the vicinity of Pontipool, where they rise eastward.

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