The City Walls of Nicaea

Antiquity ◽  
1938 ◽  
Vol 12 (48) ◽  
pp. 437-443 ◽  
Author(s):  
Alfons Maria Schneider

The village of İznik, north-east of Brussa, and far from all traderoutes, is today the mere ghost of what was once an important city. It is quite hidden within the ancient circumvallation, and occupies scarcely a third of the former area of the town. The wall itself, one of -the most impressive and best-preserved Byzantine monuments of Asia Minor, forms an irregular polygon (plan, FIG. I). The lacus Ascanius washes it on the west, while the other sides are bordered by a green, well-wooded plain, gradually giving place on the north-east to the slopes of Elmali dagh. A charming view of the village and walls can be abtained from a small knoll about 300 metres east of the city, with the lake shimmering in the distance and the fields shaded with cypresses, planes, walnut and other fruit-trees. The description of Catullus still holds good (Nicaeaeque ager uber aestuosae, 46.5): nature here is inexhaustible, and gives in abundance of the finest fruits to anyone who tills the earth. From May to October the weather is nearly always good, and in the height of summer the heat can be unbearable. Certainly the air is no longer pure and healthy as it was in Byzantine days; neglected water-courses and pools of subterranean water have brought malaria in their train. Nor is the sea alive with boats, for there is no fishing. Yet within recent years an improvement has taken place in those conditions which gave older travellers reason for feeling melancholy or annoyance, and it begins to look as if the village were slowly awakening from its long sleep.

1946 ◽  
Vol 12 (2) ◽  
pp. 80-94 ◽  
Author(s):  
Maurice Robbins

Within the town of Norton, Massachusetts, close by the boundary between it and the city of Taunton, lies the beautiful little body of water known to this day by its Indian name of Winneconnet. This lake, fed by a system of streams from the north and west and draining southward through a complicated network of ponds, swamps, and streams into the Taunton River, seems to have been the center of a large area of Indian population in ancient times. Cultivation and other disturbances of the earth surfaces have demonstrated the existence of many sites of former Indian habitation, while numerous items in local tradition point to the fact that many Indians lived and died within the township. Hardly a garden plot that has not yielded its quota of stone implements to the collections of local “relic hunters” exists in this vicinity.


Author(s):  
G. Mauro

Several studies put in evidence the relevant role of cultivated lands in the urban areas. Using GIS methodologies in order to map agricultural areas near or within the town, it is possible to analyze their relationship with the urban area. In this study, the author used several different cartography sources, like digital cartography and orthophotos, in order to locate the urban domestic gardens and the terraced landscapes accurately. The study area is a medium city of a North-East Region of Italy, Trieste. Built on a hill morphology, it had a great and fast growth in the 19th and 20th centuries. These changes deeply transformed its landform, mainly reducing its surrounding cultivated lands. At present, the residual terraced landscapes are mainly placed in the north side of the city and they represent a kind of “cultural heritage.” On the contrary, the most important garden areas are located in the terrain embankments of the south suburban areas.


Twejer ◽  
2021 ◽  
Vol 4 (1) ◽  
pp. 589-628
Author(s):  
Dilshad Aziz Marif ◽  

This paper deals with the ancient settlements in the plain where the city of Sulaimani found in 1874 A.D. In his book (Babylonian Problems) Lane (1923) proposes that modern Sulaimani built on the long-lost city of Celonae that was mentioned by the Roman historian Quintus Curtius Rufus (1st century A.D.) in his book "Histories of Alexander the Great.” Also, the Kurdish historian Amin Zeki in his book (The History of Sulaimani)1951, agrees with Lane, and he suggests that the name of modern Sulaimani’s name perhaps derived from the same name of Celonae. Many other historians and archaeologists repeat the same identification. In this paper, we investigated this identification, and we found that the city of Celonae was mentioned only once by the Roman historian Quintus Curtius Rufus (1st century A.D.) in his book "Histories of Alexander the Great,” he refers to the journey of Alexander the Great from Susa to Ekbatana, according to Rufus, on his way, Alexander camped in Celonae. We suggest a new identification for the Celonae Town in the northern edges of Garmian district at the foot or on the top of one of the mountains of the modern Qaradagh ranges, because, Alexander took the road from Susa to the north then east crossing the city of Sittake on the Tigris near Celucia/al-Madain, then moving to other cities along the road to the direction of the north-east, camped in Celonae, then moved to the east and reached Bagastana (Behistun) and after wards to Ecbatana, the capital of the Median Empire in (modern Hamadan). We found also, that the Assyrian royal inscriptions refer to a mountain called Siluna, the Assyrian king Adad-Narari III (811-783 B.C.) in his campaign on Namri and Media, after crossing the Lower Zab toward the east, first he mentions the mountain Siluna, where the sun rises, then he occupied Namri and crossed the other lands in the east to reach Media, and since Namri was the land of the Kassites (in the post-Kassite period) located in the area of Sangaw-Garmian-Qaradagh-Bamo ranges, we can conclude that the mountain Siluna and the city Celonae were located in the same place somewhere in Qaradagh ranges. In the base of the above-mentioned evidence, we can reject the previous identification of Celonai with modern Sulaimani. On the other hand, in this paper we discussed other identifications of modern Sulaimani with ancient cities and towns mentioned in the cuneiform records, for instance, Radner (2017), suggests that the Zamuan capital city of Arrakdi of the Lullubu people located under modern Sulaimani, but this is not a proper identification, because the city of Arrakdi was mentioned in the cuneiform records three times, and in all records they refer to the point that the city located beyond a roughed mountain, the Annals of Ashurnasirpal II refers that the city located at the foot of the roughed mountain Lara, and this mountain should be modern Lare mountain in the east of Shabazher district far east from modern Sulaimani. Also, the cuneiform tablet that was discovered in Sitak in Sharbazher district and that tablet also refers to Arrakdi. Also, we found that Spiser linked the village of Uluba (Ulubulagh) now it is a district in the southern east of Sulaimani, with the Lullubian City of Lagalaga, this identification only based on the similarities between the two toponyms. On the other hand, Abdulraqeeb Yusuf, suggests that the old village of Daragha, which is now a district in the eastern part of Sulaimani derived from the Zamuan city Dagara of the Lullubies, this identification also not appropriate one, because the village and district named after the name of a nobleman called Mr. Dara Agha, and there is no archaeological ruin in this district as well. The city of Sulaimani was built on an area where a huge archaeological Gird/Tell existed, the Babanian princes built their palace on this artificial hill and the administrative buildings to the east of it, when they dug for the foundations, they discovered coins, a stone with unknown script, and many jars, some of them big jars contained human skulls. In 2005, when the modern building Kaso Mall constructed on the northwest of the hill, we found two seals date back to Jamdet-Naser = Nineveh V period, and Ubaid potsherds, and some bull skulls, their horns cut with a sharp instrument. This evidence indicate that the city was built on a settlement date back to the 5th-4th millennium B.C. Other archaeological discoveries in Girdi Kunara and Girdi De Kon in the western part of the city at the bank of Qiliasan and Tanjero rivers, in Kunara many cuneiform tablets discovered there, we can link these sites also with the Lullubies in the third & second millennium B.C.


1901 ◽  
Vol 33 (3) ◽  
pp. 537-552
Author(s):  
J. F. Fleet

For more than a century, Indian archæologists have been greatly puzzled about the identity of an ancient city named Tagara. The city is referred to in some of the Indian epigraphic records. Thus, a record of a.d. 997 describes the Śilāhāra prince Aparājita, of the Northern Koṅkaṇ, as Tagara-pura-paramēśvara, or “ supreme lord of the town of Tagara,” giving to him a hereditary title commemorative of the place which his family claimed as its original home. Another Śilāhāra record, of a.d. 1058, similarly applies to Mārasiṁha, of the Karhāḍ branch of the family, the title of Tagara-puravar-ādhīśvara, or “ supreme lord Tagara, a best of towns, an excellent town, a chief town;” and it further describes his grandfather Jatiga II. more specifically, but less accurately, as Tagara-nagara-bhūpālaka, or “ king of the city of Tagara.” And a Western Chalukya record of a.d. 612 specifies Tagara as the residence of the person to whom the grant of a village, registered in that charter, was made. The city is further mentioned, as Tagara, by the Greek geographer Ptolemy, who, writing about the middle of the second century a.d., assigned to it a certain latitude and longitude which have the effect of placing it about eighty-seven miles towards the north-east from another place, mentioned by him as Baithana, which his details would locate about 270 miles on the east-north-east of Barygaza.


Antiquity ◽  
1976 ◽  
Vol 50 (200) ◽  
pp. 216-222
Author(s):  
Beatrice De Cardi

Ras a1 Khaimah is the most northerly of the seven states comprising the United Arab Emirates and its Ruler, H. H. Sheikh Saqr bin Mohammad al-Qasimi, is keenly interested in the history of the state and its people. Survey carried out there jointly with Dr D. B. Doe in 1968 had focused attention on the site of JuIfar which lies just north of the present town of Ras a1 Khaimah (de Cardi, 1971, 230-2). Julfar was in existence in Abbasid times and its importance as an entrep6t during the sixteenth and seventeenth centuries-the Portuguese Period-is reflected by the quantity and variety of imported wares to be found among the ruins of the city. Most of the sites discovered during the survey dated from that period but a group of cairns near Ghalilah and some long gabled graves in the Shimal area to the north-east of the date-groves behind Ras a1 Khaimah (map, FIG. I) clearly represented a more distant past.


Author(s):  
Sergey B. Kuklev ◽  
Vladimir A. Silkin ◽  
Valeriy K. Chasovnikov ◽  
Andrey G. Zatsepin ◽  
Larisa A. Pautova ◽  
...  

On June 7, 2018, a sub-mesoscale anticyclonic eddy induced by the wind (north-east) was registered on the shelf in the area of the city of Gelendzhik. With the help of field multidisciplinary expedition ship surveys, it was shown that this eddy exists in the layer above the seasonal thermocline. At the periphery of the eddy weak variability of hydrochemical parameters and quantitative indicators of phytoplankton were recorded. The result of the formation of such eddy structure was a shift in the structure of phytoplankton – the annual observed coccolithophores bloom was not registered.


2020 ◽  
Vol 8 (2) ◽  
pp. 13
Author(s):  
Ankita Pandey

Guwahati derives its name from the Assamese word “Guwa” means areca nut and “Haat” means market. However, the modern Guwahati had been known as the ancient Pragjyotishpura and was the capital of Assam under the Kamrupa kingdom. A beautiful city Guwahati is situated on the south bank of the river Bramhaputra. Moreover, It is known as the largest city in the Indian state of Assam and also the largest metropolis in North East India. It has also its importance as the gateway to the North- East India. Assamese and English are the spoken languages in Guwahati.  In 1667, the Mogul forces were defeated in the battle by the Ahom forces commanded by Lachut Barphukan. Thus, in a sense Guwahati became the bone of contention among the Ahoms, Kochas and the Moguls during the medieval period.  Guwahati the administrative headquarters of Lower Assam with a viceroy or Barbhukan was made by the Ahom king.  Since 1972 it has been the capital of Assam. The present paper will discuss the changes happened in Guwahati over the period of late 1970s till the present time. It will focus on the behavior of people, transformed temples, Panbazar of the city, river bank of Bramhaputra, old Fancy Bazaar, chaotic ways, festivals and seasons including a fifth man made season etc. It will also deal how over the years a city endowed with nature’s gifts and scenic views, has been changing as “a dirty city”. Furthermore, it will also present the insurgencies that have barged into the city. The occurrence of changes will be discussed through the perspective and point of view of Srutimala Duara as presented in her book Mindprints of Guwahati.


2021 ◽  
pp. 102452942110113
Author(s):  
Luke Telford

Based on 52 qualitative interviews with working-class individuals, this paper explores the social and economic decline of a coastal locale referred to as High Town in Teesside in the North East of England. First, the paper outlines how the locality expanded as a popular seaside resort under capitalism’s post-war period. It then assesses how the seaside existed together with industrial work, offering stable employment opportunities, economic security and a sense of community. Next, the article documents the shift to neoliberalism in the 1980s, specifically the decline of High Town’s seaside resort, the deindustrialization process and therefore the 2015 closure of High Town’s steelworks. It explicates how this exacerbated the locale’s economic decline through the loss of industrial work’s ‘job for life’, its diminishing popularity as a coastal area and the further deterioration of the town centre. The paper concludes by suggesting that High Town has lost its raison d’être under neoliberalism and faces difficulties in revival.


Archaeologia ◽  
1779 ◽  
Vol 5 ◽  
pp. 95-97
Author(s):  
Pegge

Rudston, a village in the East-Riding of Yorkshire, on the Wolds, near Burlington, is thus noticed in bishop Gibson's edition of Camden, col. 901. “More inward into the “land, is Ruston, where, in the church-yard, is a kind of “pyramidal stone of great height. Whether the name of the “town may not have some relation to it, can be known only “from the private history of the place; but if the stone bear “any resemblance to a cross, rod in Saxon doth imply so much.” This cross, as the bishop calls it, and I think not improperly, is a very curious monument; and, no doubt, of very remote antiquity. I am not aware that it has ever been engraved, and therefore I here present the Society with an accurate drawing* of it, which I received A. 1769, from the friendly hand of Mr. Willan, whose account I shall take the liberty to subjoin. “This stone stands about four yards from the North East “corner of Rudston church, which is situated on a high hill. “Its depth under ground equal to its height above, as appeared “from an experiment made by the late Sir William Strickland. “All the four sides are a little convex, and the whole covered “with moss. No tradition in this country of any authorrity, either concerning the time, manner, or occasion of its “erection.”


1945 ◽  
Vol 82 (6) ◽  
pp. 267-273 ◽  
Author(s):  
W. Anderson

Formerly there were several surface brine springs in the North-East Coalfield; to-day there are none. From the many accounts of their occurrence nothing has been learned of their exact position, and very little of the composition of their waters. The earliest record, made in 1684, described the Butterby spring (Todd, 1684), and then at various times during the next two centuries brine springs at Framwellgate, Lumley, Birtley, Walker, Wallsend, Hebburn, and Jarrow were noted. In particular the Birtley salt spring is often mentioned, and on the 6-in. Ordnance map, Durham No. 13, 1862 edition, it is sited to the south-east of the village. Although no record has been found there must have been either a brine spring or well at Gateshead, for the name of the present-day suburb, Saltwell, is very old, and brine springs are still active in the coal workings of that area.


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