scholarly journals THE POPULATION OF CHERNYAKHIV CULTURE, WHICH IS BURIED IN THE CEMETERY NEAR THE VILLAGE OF VELYKA BUGAIVKA, ACCORDING TO CRANIOLOGY

2021 ◽  
Vol 40 (3) ◽  
pp. 293-303
Author(s):  
T. O. Rudych

Cemetery of Chernyakhiv culture near the Velyka Buhaivka village was excavated in 1995—2005 by an expedition of O. V. Petrauskas and R. G. Shishkin. During the excavations the anthropological material was obtained. The male series is characterized by a medium-long, narrow, medium-high, dolichocranial cranium. The face is short, narrow, mesognathic. Horizontal face profiling is sharp. Orbits are medium high, the nose is medium wide. The angle of the nasal bones is on the border of medium and large values. The nose is of medium height. According to the results of statistical analysis, the group from Velyka Buhaivka is close to the series from the cemeteries of Romashki, Kurnyky, Ranzheve. The group is closer to the series of Welbark culture Maslomench, Grudek, a bit closer to the Welbark mixed series of the Lower Vistula, than to individual series of Chernyakhiv culture from the territory of Ukraine. The female group is characterized by a long, medium-wide on the border with a wide, medium-high, dolichokranny cranium. The face is medium-wide and medium-high, orthognathic. The orbits were medium high, the nose was medium wide. Horizontal profiling of the face at the upper level is on the border of sharp and moderate, its profiling at the zygomaxillary level is sharp. The angle of the nasal bones is medium, the epiglottis is medium high. According to the results of the analysis, the women’s series from Velyka Buhaivka is closest to the women from Chernyakhiv, Zhuravka, Popivka. From the groups of Polish Welbark culture the mixed group of Slovinsko-Drawska is close to the women from Velyka Buhaivka. The dolichocranium narrow-faced type was dominant in people buried by inhumation. It is recorded in the people buried in the graves accompanied by the grave goods of the phase C2, C2—C3, D1. This type is present both in burials directed with the head to the North, and to the West.

1876 ◽  
Vol 9 (1) ◽  
pp. 147-154
Author(s):  
A. H. Schindler

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.


Antiquity ◽  
1955 ◽  
Vol 29 (114) ◽  
pp. 77-88 ◽  
Author(s):  
Kenneth Jackson

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.


2021 ◽  
Vol 40 (3) ◽  
pp. 282-292
Author(s):  
S. I. Kruts ◽  
T. O. Rudych

The anthropological composition of the population buried at the cemetery of the Scythian Age near Svitlovodsk city (Kirovograd region) is analyzed in the paper. The burial ground is located on the border of the Forest-Steppe and Steppe Zones of the Right Bank of the Dnieper. The anthropological material under study comes from cemetery without mounds. Archaeologists date the main massif of burials to the 4th century BC. The anthropological composition of the population that was buried at this burial ground was not homogenous. The male series of skulls is characterized by a long, medium-wide, high, dolichocranic skull. The face is of medium size, it is mesognathic. The horizontal profile of the face at the upper level is medium, but with a tendency to the sharp; at the middle level, the face is strongly profiled. The orbital and nasal indexes are medium. The bones of the nose are moderately protruding. The average characteristics of the male population fit into the range of variations of the Scythian series. The male series belongs morphologically and statistically to the circle of the steppe Scythian groups. The male group from the burial ground near the city of Svitlovodsk is close to the series from the Nikolaevka burial ground on the Dnister River, the group of skulls from the burial mounds near the village of Shirokoe (Left Bank of the Dnieper River), the group of skulls from the burial mounds near the village of Vyshchetarassivka, a series of skulls from the Mykhailivka burial ground. Of the forest-steppe series, only the combined group of skulls from the Trypillya region is somewhat close to it. All these statistically and morphologically similar groups originate from different territories. This illustrates the specifics of the settlement and demonstrates the mobility of the Scythian groups. The female series from the burial ground is characterized by a long, narrow, medium-high skull, mesocranic in shape. The size of the face is small, it is mesognathic. The horizontal profile of the face at the upper level is moderate, at the zygomaxilar level it belongs to the category of sharp, but with a tendency to moderate. The orbital index is medium, the nasal index belongs to the large category. The bones of the nose are medium protruding. The female series from Svitlovodsk burial ground turns out to be the most gracile among the Scythian series in Ukraine. For this reason, it differs significantly from the entire massif of the steppe Scythian series. The closest to the Svitlovodsk series is a group from mounds near Nikopol.


1913 ◽  
Vol 19 ◽  
pp. 133-173 ◽  
Author(s):  
C. A. Scutt

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.


2010 ◽  
Vol 138 (9) ◽  
pp. 3540-3555 ◽  
Author(s):  
Zachary O. Finch ◽  
Richard H. Johnson

Abstract Upper-level inverted troughs (IVs) associated with midlatitude breaking Rossby waves or tropical upper-troposphere troughs (TUTTs) have been identified as important contributors to the variability of rainfall in the North American monsoon (NAM) region. However, little attention has been given to the dynamics of these systems owing to the sparse observational network over the NAM region. High temporal and spatial observations taken during the 2004 North American Monsoon Experiment (NAME) are utilized to analyze a significant IV that passed over northwestern Mexico from 10 to 13 July 2004. The Colorado State University gridded dataset, which is independent of model analysis over land, is the primary data source used in this study. Results show that the 10–13 July IV disturbance was characterized by a warm anomaly around 100 hPa and a cold anomaly that extended from 200 to 700 hPa. The strongest cyclonic circulation was in the upper levels around 200 hPa. Quasigeostrophic (QG) diagnostics indicate that the upper-level low forced weak subsidence (weak rising motion) to the west (east) of its center. Net downward motion to the west was a result of the Laplacian of thermal advection (forcing subsidence) outweighing differential vorticity advection (forcing weak upward motion). Despite the QG forcing of downward motion west of the upper-level IV, enhanced convection occurred west of the IV center along the western slopes of the Sierra Madre Occidental (SMO). This seemingly contradictory behavior can be explained by noting that the upper-level IV induced a midlevel cyclonic circulation, with northeasterly (southeasterly) midlevel flow to the west (east) of its center. Increased mesoscale organization of convection along the SMO foothills was found to be collocated with IV-enhanced northeasterly midlevel flow and anomalous northeasterly shear on the western (leading) flank of the system. It is proposed that the upper-level IV increased the SMO-perpendicular midlevel flow as well as the wind shear, thereby creating an environment favorable for convective storms to grow upscale as they moved off the high terrain.


1978 ◽  
Vol 44 ◽  
pp. 309-433 ◽  
Author(s):  
Patricia M. L. Christie ◽  
S. M. Elsdon ◽  
G. W. Dimbleby ◽  
A. Saville ◽  
S. Rees ◽  
...  

The ancient village of Carn Euny, formerly known as Chapel Euny, lies on a south-west slope just above the 500 foot contour in the parish of Sancreed in West Cornwall (fig. 1). The granite uplands of the region are rich in antiquities, as a glance at a recent survey shows (Russell 1971), not least those of the prehistoric period. The hill on which the site is situated is crowned by the circular Iron Age Fort of Caer Brane (pl. 27). Across the dry valley to the north-west rises the mass of Bartinny Down, with its barrows, while in the valley below the site near the hamlet of Brane is a small, well preserved entrance grave and other evidence of prehistoric activity. To the south-east about one mile away is the recently excavated village of Goldherring dating from the first few centuries of our era (Guthrie 1969). From later times, the holy well of St Uny and the former chapel which gave its name to the site, lie nearby to the west. The village contains a fine souterrain, locally known as a fogou, after a Cornish word meaning a cave (Thomas 1966, 79).Nothing appears to have been known of the settlement or Fogou before the first half of the 19th century when the existence of an unexplored fogou at Chapel Uny is first mentioned by the Reverend John Buller (1842), shortly followed by Edmonds (1849) who described to the Penzance Natural History and Antiquarian Society an ‘Ancient Cave’ which had been discovered by miners prospecting for tin.


2018 ◽  
Vol 2 (XVIII) ◽  
pp. 145-157
Author(s):  
Dariusz Rozmus

The vast destruction of the heritage sites in Syria and Iraq caused by the activities of ISIS may not only be attributed to fanatical iconoclasm with a religious background. The ideologists of the jihad movements in the so-called Islamic State intend to introduce one, unified version of Islam. In their world, there is no place for democracy, secularity, nationalism (even for patriotism) and other “abominations” of the West. Monuments which constituted elements of local traditions were destroyed with the application of huge resources. In the face of the tragedy of people, considerations in the field of broadly conceived culture may only supplement a description of unspeakable tragedies which were caused by the wars in the Near East. However, we may examine this question in such a way as not to separate the people from their heritage, for a human being is an integral part of his or her culture. “This isn’t a choice between people or stone,” said Deborah Lehr, chair of Antiquities Coalition. “Culture is part of who these people are, and this, ironically, is the cradle of civilization.”. Due to the situation which occurred, the stock-taking and digitalisation of artefacts and architectural monuments assumes huge significance. These proceedings should be also conducted with the use of the most recent methods of satellite teledetection.


1950 ◽  
Vol 45 ◽  
pp. 261-298 ◽  
Author(s):  
J. M. Cook ◽  
R. V. Nicholls

The village of Kalývia Sokhás lies against the base of one of the massive foothills in which Taygetus falls to the plain three or four miles to the south of Sparta (Plate 26, 1). It is bounded by two rivers which flow down in deep clefts from the mountain shelf. The hillside above rises steeply to a summit which is girt with cliffs on all but the west side and cannot be much less than four thousand feet above sea level; this von Prott believed to be the peak of Taleton. Its summit is crowned by the ruins of a mediaeval castle which was undoubtedly built as a stronghold to overlook the Spartan plain; the only dateable object found there, a sherd of elaborate incised ware, indicates occupation at the time when the Byzantines were in possession of Mystra. The location of the other sites mentioned by Pausanias in this region remains obscure, but fortunately that of the Spartan Eleusinion has not been in doubt since von Prott discovered a cache of inscriptions at the ruined church of H. Sophia in the village of Kalývia Sokhás. In 1910 Dawkins dug trenches at the foot of the slope immediately above the village and recovered a fragment of a stele relating to the cult of the goddesses and pieces of inscribed tiles from the sanctuary. The abundance of water in the southern ravine led von Prott to conclude that the old town of Bryseai with its cult of Dionysus also lay at Kalývia Sokhás; but no traces of urban settlement have come to light at the village, and the name rather suggests copious springs such as issue from the mountain foot at Kefalári a mile to the north where ancient blocks are to be seen in the fields.


2007 ◽  
Vol 27 (4) ◽  
pp. 555-578 ◽  
Author(s):  
MIRIAM BERNARD ◽  
BERNADETTE BARTLAM ◽  
JULIUS SIM ◽  
SIMON BIGGS

ABSTRACTRetirement communities are a relatively new long-term accommodation and care option in the United Kingdom. Policy makers and providers endorse the proposition that they are suited for the accommodation of both ‘fit’ and ‘frail’ older people, although comparatively little is known about what it is actually like to live in such communities, about whether they cater adequately for older people with a wide spectrum of needs and abilities, or if they provide acceptable solutions to older people's housing or care needs. This paper addresses these questions by reporting the findings of an independently funded three-year study of a new retirement village, Berryhill, in the north Midlands of England. The paper examines the background to this and similar developments, details how the study was carried out, and then examines what it was like to live at Berryhill. It focuses on the housing and care aspects, and explores the residents' motivations for moving to the village; their views about the accommodation; and their use of and satisfaction with the social and leisure amenities. The health and care needs of residents and the formal and informal supports are also featured. The conclusion discusses whether the village can truly be a ‘home for life’ in the face of increasing frailty, and whether or not these new models of accommodation and care can indeed cater for both ‘fit’ and ‘frail’ older people.


1951 ◽  
Vol 16 (3) ◽  
pp. 257-260 ◽  
Author(s):  
Charles C. Dipeso

The Amerind Foundation, Inc. spent the first three weeks of December, 1948, excavating a ball court at the archaeological site of Arizona:BB:15:3, which is located in Cochise County, Sec. 20, T15S, R20E. The actual village area is located on the west bank of the San Pedro River twenty-two miles north of the city of Benson at an approximate elevation of 3300 feet.The ball court was located in the north half of the village on a terrace some forty feet above the river channel. It appeared as a shallow but conspicuous oval depression which was overgrown with mesquite trees and other desert flora of the Sonoran plateau type. Fortunately the court had not been disturbed by any previous excavations nor by erosion (Fig. 86, a).


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