scholarly journals An Iron Sword from Southern Siberia in the Collection of the Minusinsk Museum of Local History

2019 ◽  
Vol 18 (5) ◽  
pp. 99-105
Author(s):  
Yu. S. Khudyakov ◽  
A. Yu. Borisenko ◽  
K. T. Akmatov

Purpose. We studied a rare finding of an iron sword, that was coincidentally discovered at the beginning of the 20th Century in the outskirts of Kuragino Village on the territory of Minusinsk Hollow. At present, the finding is stored in the collection of long blade weapon objects in the Minusinsk Museum of Local History. Results. The authors traced the most significant events and results achieved in the course of previous studying of archaeological findings of ancient and medieval swords on the territory of Southern Siberia and Central Asia. Definite formal signs, considerable for identification of typological affiliation, of the sword finding from the Kuragino Village are singled out. According to the formal signs, this finding is related to a particular individual type of iron swords. The item has a long, right double-edged blade and a removable guard, which is smoothly curved to sideways of the blade, and a right handle’s haft. Conclusion. Our analysis allows us to conclude that the iron sword was likely to be used by the Yenisei Kyrgyz warriors in the course of hostilities with their adversaries among the nomads, against the Old Turks and Uyghurs people, on the territory of Southern Siberia and contiguous territories of the Central Asian region during a certain historical period, including the Early Middle Ages, in particular the third quarter of the 1st millennium A. D. That historical period included inception of the Yenisei Kyrgyz state on the territory of the steppe regions of Minusinsk Hollow, which is located to the north of the West-Sayan Mountains.

2021 ◽  
Vol 02 (09) ◽  
pp. 62-68
Author(s):  
Fazilat Kholmuminovna Kasimova ◽  

Runic writing became widespread among the Turkic-speaking tribes of Southern Siberia, Central and Central Asia during the historical period when these tribes were part of the largest Central Asian state of the early Middle Ages — the Turkic Khaganate. The first information about the Turk tribe is contained in Chinese sources — the dynastic histories as "Zhou Shu", "Bei Qi Shu", "Sui Shu" and "Bei Shi". The Chinese spelling of the ethnonym-tujue is reconstructed as turkut; this latter form of the ethnonym is unknown in other (non-Chinese) literary monuments of the VI-X centuries. According to historical sources, the design of the name Turk by the plural affix - (y)/, characteristic of the Mongolian languages — is a consequence of the perception of the ethnonym by the Chinese through the medium of the Mongolian-speaking Zhuan-zhuans.


1964 ◽  
Vol 44 (1) ◽  
pp. 1-8

Early in 1963 much of the land occupied by the Roman building at Fishbourne was purchased by Mr. I. D. Margary, M.A., F.S.A., and was given to the Sussex Archaeological Trust. The Fishbourne Committee of the trust was set up to administer the future of the site. The third season's excavation, carried out at the desire of this committee, was again organized by the Chichester Civic Society.1 About fifty volunteers a day were employed from 24th July to 3rd September. Excavation concentrated upon three main areas; the orchard south of the east wing excavated in 1962, the west end of the north wing, and the west wing. In addition, trial trenches were dug at the north-east and north-west extremities of the building and in the area to the north of the north wing. The work of supervision was carried out by Miss F. Pierce, M.A., Mr. B. Morley, Mr. A. B. Norton, B.A., and Mr. J. P. Wild, B.A. Photography was organized by Mr. D. B. Baker and Mrs. F. A. Cunliffe took charge of the pottery and finds.


Author(s):  
Arkady I. Korolev ◽  
◽  
Vladimir N. Myshkin ◽  
Anton A. Shalapinin

Introduction. This is a report on the results of archaeological excavations at Maksimovka I, the subterranean burial ground located in the forest-steppe Volga region. The site is unique because it contains burial complexes of different epochs. The purpose of the paper is to introduce the materials found during the 2018 excavations for the attention of the academic community. In particular, the paper focuses on the description and characterization of the archaeological complexes under investigation, and, also, on their cultural-chronological attribution. Data. The cultural layer was not particularly rich but contained fragments of Neolithic, Eneolithic, and Bronze Age ceramics, stone tools, and waste left after stone processing. Three burials were examined in the excavation area. The first burial comprised the skeleton of a deceased person in a supine position; the head oriented to the north-northeast; the grave goods included iron items (a fragment of a boiler and of a bit, rod-shaped items, and a firesteel), grindstones, and flints. The second buried person was found in the seated position, leg bones bent at the knee joint, head oriented to northeast; the finds included a nonferrous metal ring, a bone pendant, a silicon wafer, and tubular beads. The third buried person was also in a seated position, head oriented to the northeast; no grave goods were found in the third burial. Also, two other burial constructions recovered on the site were partially examined. Results. The first burial was attributed to the Golden Horde period in the Middle Ages (the second half of the 13th or the 14th c.). The second burial has a number of parallels to burial complexes of mid-late Eneolithic era of the forest-steppe Volga region. The third burial was left unidentified in terms of its cultural-chronological attribution, granted the non-standard position of the skeletal remains in the grave and the absence of goods. Conclusions. The examination of the subterranean burial ground Maksimovka I has allowed to introduce the archaeological material of different periods, such as Neolithic, Eneolithic, Bronze, and Middle Ages.


Author(s):  
Emin Vagif Mammadov

The article is dedicated to the analysis of archeological excavation as a result of researches discovered in the Mingachevir conducted in the middle of the 20th century of the different type of underground burials of the ancient period. These burials are covered the significant historical period from the second half of the 1st millenium and the first century AD and are the important source of the scientific information on many issues of material and spiritual culture of the population of Caucasus Albania. Underground burials of the ancient period in the Mingachevir zone by the method of placing the deceased in them are divided into three types: 1) burials with a backbone stretched out on the back; 2) burials with a weakly crouched skeleton on the left or right side; 3) burials with a heavily crouched skeleton on the left or right side. The article gives a detailed analysis of all these three types of burials. The author of the article, along with a number of other researchers come to the conclusion that the first type of underground burial is considered to be innovation for the whole of the South Caucasus and its emergence is associated with the penetration of mobile tribes from the North Caucasus in particular the Scythian. Part of these Scythians finally settled in the Mingachevir zone and subsequently merged with the local population, which eventually leads to the appearance of a second type of underground burial in the form of underground graves with poorly crouched skeleton. The third type of underground burial of Mingachevir (Samunis) of the ancient period, namely burials with a heavily crouched skeleton belong to local autochthonous tribes, consolidation of which became the basis for the formation of the state of Caucasian Albania in the 4th – 3rd centuries BC. This type of underground burial has deep local roots and is based on centuries-old local funerary rituals.


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).


1968 ◽  
Vol 31 (3) ◽  
pp. 534-554 ◽  
Author(s):  
C. E. Bosworth

It is not too much to describe the Ṣaffārids of S‚stān as an archetypal military dynasty. In the later years of the third/ninth century, their empire covered the greater part of the non-Arab eastern Islamic world. In the west, Ya'qūb. al-Laith's army was only halted at Dair al-'Āqūl, 50 miles from Baghdad; in the north, Ya'qūb and his brother 'Arm campaigned in the Caspian coastlands against the local 'Alids, and 'Amr made serious attempts to extend his power into Khwārazm and Transoxania; in the east, the two brothers pushed forward the frontiers of the Dār al-Islām into the pagan borderlands of what are now eastern Afghanistan and the North-West Frontier region of West Pakistan; and in the south, Ṣaffārid authority was acknowledged even across the persion Gulf in ‘Umān. This impressive achievement was the work of two soldiers of genius, Ya'qūub and 'Amr, and lasted for little more than a quarter of a century. It began to crumble when in 287/900 the Sāmānid Amīr Ismā'īl b. Aḥmad defeated arid captured ‘Amr b. al-Laith, and 11 years later, the core of the empire, Sīstān itself, was in Sāmānid hands. Yet such was the effect in Sīstān of the Ṣaffārid brothers’ achievement, and the stimulus to local pride and feeling which resulted from it, that the Ṣaffārids returned to power there in a very short time. For several more centuries they endured and survived successive waves of invaders of Sīstān—the Ghaznavids, the Seljūqs, the Mongols—and persisted down to the establishment of the Ṣafavid state in Persia.


Author(s):  
Rinaldi Mirsa ◽  
Muhammad Muhammad ◽  
Eri Saputra ◽  
Izzati Farhana

Samudera Pasai is one of the Islamic Sultanates in Indonesia which appeared in the Middle Ages or around 1267 AD. Evidence of the existence of the Sultanate of Samuedra Pasai in Indonesia is listed in the book Rihlah ilal-Masyriq (Wanderings to the East) written by Abu Abdullah Ibnu Batutha (1304 - 1368 AD), a Muslim adventurer who traveled to Samudera Pasai in 1345 AD. The spatial pattern of the Samudera Pasai Sultanate is no longer visible because there are no traces of archaeological remains in the form of any remaining buildings, except for the tombs of Sultanate figures and historical records of foreign adventurers who have explored the Samudera Pasai Sultanate. This record strengthens the evidence of the existence of the Samudera Pasai Sultanate. The methodology used in this case is a phenomenological approach and a historical approach, which are expected to approach optimal results in uncovering spatial patterns in the development of Islam. The spatial arrangement of the sultanate generally used the concept of catur gatra tungga, which was arranged in the form of: alun-alun (the square) as the center of space, markets to the north of the square, palaces to the south of the square, and mosques to the west of the square. The spatial arrangement then formed a spatial pattern that became the center of the Samudera Pasai Sultanate.


Author(s):  
Tanieva Guldona Mamanovna ◽  

In the Middle Ages, Central Asian pilgrims traveled to Mecca in three directions: the North direction ‒ through the Russian Empire, the central direction‒ through the territory of Persia, and the south direction ‒ along roads through India and the Arabian Sea. Therefore, the question of the directions of the Hajj was reflected in the diplomatic correspondence of the Central Asian khanates with Persia, India, the Russian and Ottoman empires тоо. Depending on the political, economic and ideological interests of these states, sometimes pilgrims were given permits to be sent to Mecca through their territories, and sometimes not. The degree of intensity of pilgrimage movements, in most cases, depended on the activities of interstate ambassadors. On the issue of eliminating various prohibitions and obstacles in the movements of pilgrimage roads, the Central Asian ambassadors were active and historical documents reveal these data to us. In this period the Central Asian ambassadors, who were sent to the reception of the governors those neighbor states on other issues, in most cases negotiated precisely on the direction of the Hajj of the Central Asian pilgrims also. One of such far-sighted ambassadors was a rich merchant from Bukhara, who lived in the XVIII c. Ernazar Maksud ogli officially sent several times by the Central Asian rulers to the Russian Empire. In this article analyzes the question of how the problems of the Hajj road were solved at the international diplomatic level by the example of the activities this ambassador. The history of negotiations between Ernazar and the Russian emperors on matters of the northern direction of the Hajj road and their results illuminated on base documents on this issue, which stored in the fund of the Archive of Foreign Policy of the Russian Empire (AFPRE). The scientific conclusions of this article serve for an extensive study of the issues of diplomatic and economic relations between the Central Asian khanates and the Russian Empire in the XVIII century, revealing the history of the embassy relations of the khanates and the history of the pilgrimage of the Hajj of the Central Asian people and the features of the directions of roads from Central Asia to Mecca.


1900 ◽  
Vol 32 (4) ◽  
pp. 763-768
Author(s):  
T. K. Krishṇa Menon

Malayalam is the language of the south-west of the Madras Presidency. It is the third most important language of the Presidency, the first and the second being Tamil and Telugu respectively. It is spoken in Malabar, Cochin, and Travancore. Out of a total of 5,932,207 inhabitants of these parts, 5,409,350 persons are those who speak Malayalam. These countries, taken as a whole, are bounded on the north, by South Canara, on the east by the far-famed Malaya range of mountains, on the south by the Indian Ocean, and on the west by the Arabian Sea.


2005 ◽  
Vol 84 (2) ◽  
pp. 77-85 ◽  
Author(s):  
R.J.O. Hamblin ◽  
B.S.P. Moorlock ◽  
J. Rose ◽  
J.R. Lee ◽  
J.B. Riding ◽  
...  

AbstractMapping combined with till provenance studies have resulted in a re-appraisal of the pre-Devensian glacial stratigraphy of Norfolk, England. The traditional model invoked two formations, a North Sea Drift Formation (NSDF) overlain by a Lowestoft Formation, formed by co-existing ice-sheets originating in Scandinavia and Northern Britain respectively. The NSDF included three diamictons, the First, Second and Third Cromer tills. The Briton’s Lane Sands and Gravels were considered to overlie the Lowestoft Formation. However, our work has shown this stratigraphy to be untenable, and we propose a model of several glaciations instead of co-existing ice-sheets. In our revised stratigraphy, the oldest formation, the Happisburgh Formation (including the Happisburgh or First Cromer Till) includes massive, sandy tills derived from northern Britain. The overlying Lowestoft Formation, including the Second Cromer (Walcott) Till is confirmed as derived from the west, introducing much Jurassic material as well as Chalk. The Sheringham Cliffs Formation includes both brown sandy tills (the Third Cromer Till) and ‘marly drift’, in a variety of tectonic relationships, and derived from the north and NNW. Finally the Briton’s Lane Formation is the only formation to include Scandinavian erratics. Dating of the four formations is at varying levels of confidence, with the Lowestoft Formation most confidently confirmed as MIS 12. The Happisburgh Formation is believed to represent an earlier glaciation, and MIS 16 is proposed. The Sheringham Cliffs Formation is tentatively believed to date from MIS 10, and the Briton’s Lane Formation is assigned to MIS 6.


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