Excavations at Can Hasan: First Preliminary Report, 1961

1962 ◽  
Vol 12 ◽  
pp. 27-40 ◽  
Author(s):  
D. H. French
Keyword(s):  
Sea Level ◽  
Preliminary Report ◽  
River Valley ◽  
Unique Position ◽  
North East ◽  
The Village ◽  
The Town

The village of Can Hasan is situated in the Kaza of Karaman, in the Vilayet of Konya, about 13 km. north-east of the town of Karaman. Can Hasan is a small village of about three hundred people, lying in a wide and fertile plain, not too far from the first low foothills of the Taurus. The approximate height of the village above sea level is 1,000 m.Geographically the importance of Karaman and its surrounding villages lies in its unique position at the end of the route (Fig. 1) through the Taurus which begins at Silifke and follows the Gök Su (Calycadnus) as far as Mut, from where there is little difficulty in crossing the watershed between the river valley and the Karaman plain. This is one of the great routes through the Taurus and one of the easiest: there are others. All of them are used even to-day, when nomads with pack animals travel up to 300 km. through the Taurus from summer to winter pastures.

Woodeaton

1917 ◽  
Vol 7 ◽  
pp. 98-119 ◽  
Author(s):  
M. V. Taylor
Keyword(s):  
Sea Level ◽  
The South ◽  
North East ◽  
The North ◽  
Dry Seasons ◽  
The Village

Woodeaton is a small Oxfordshire parish, four miles north-east of the centre of Oxford city and a little west of the wide marshy level of the ‘Plain of Otmoor.’ It stands on a low, detached and rounded hill, 315 feet above sea level, and 120 feet above Otmoor. In old days it must have been difficult of access, for Otmoor spreads away to the east of it; low pastures along the river Cherwell close it in on the north and west, while south-westwards, too, the land is low-lying and marshy. Even to the south-east a marshy hollow separates it from the wooded slopes of Beckley and Elsfield, once part of Shotover Forest. However, the well-known Roman road which connects Dorchester (Oxon.) with Alchester, and which passes along the foot of Shotover, and traverses the village of Beckley and the plain of Otmoor, runs within two miles of Woodeaton; in dry seasons it may have helped those who wished to get to the spot.

Excavation and Survey at Tuscania, 1972: A Preliminary Report

1972 ◽  
Vol 40 ◽  
pp. 196-238
Author(s):  
John Ward-Perkins ◽  
Bryan Ward-Perkins ◽  
David Andrews ◽  
Sheila Gibson ◽  
David Whitehouse
Keyword(s):  
Preliminary Report ◽  
Small Town ◽  
Compact Mass ◽  
North East ◽  
Modern Development ◽  
Almost All ◽  
The Hill ◽  
The Town ◽  
Santa Maria

On 6 February 1971 the small town of Tuscania, twenty miles west of Viterbo and the same distance north-east of Tarquinia, was the scene of a local but very violent earthquake, which killed a number of people and rendered much of the old town totally uninhabitable.Tuscania (until 1911 Toscanella) is best known to most visitors to Italy for its two magnificent medieval churches, that of San Pietro on the ancient acropolis and that of Santa Maria Maggiore, both of them fine romanesque buildings on the site of earlier churches. San Pietro has been thought by some writers to incorporate parts of the earlier structure, and both churches contain a number of earlier fittings. The town itself is less familiar, although it is still enclosed within the circuit of its medieval walls, and inside these walls it has retained a large number of medieval and later buildings in a setting largely unspoilt by modern development. Almost all the growth of the last forty years has taken place northwards and westwards, outside the medieval walls, so that the visitor still has very much the impression of the old walled city, dominated in the foreground by the hill of San Pietro itself, with its picturesque group of towers and other buildings, and spreading up the ridge beyond it the compact mass of the old town.

A Trial Excavation at Monte d'Irsi, Basilicata

1971 ◽  
Vol 39 ◽  
pp. 138-170 ◽  
Author(s):  
D. B Whitehouse ◽  
M. Aylwin Cotton ◽  
John F. Cherry
Keyword(s):  
Sea Level ◽  
Archaeological Site ◽  
North West ◽  
Stream Beds ◽  
The Hill ◽  
The Village ◽  
The Town ◽  
Santa Maria

Monte d'Irsi is located approximately 6·5 km. east-southeast of the town of Irsina and 4 km. due west of the village of Santa Maria d'Irsi in the region of Basilicata. The archaeological site sits on the crown of an irregularly shaped plateau at around 480 m. above sea level; the land drops away steeply in all directions and the hill-sides are heavily eroded by stream beds which feed into the two major rivers in the area, the Bradano and the Basentello (Figs. 1 and 2 and Pl. XXVII, a). M. d'Irsi lies about 7·5 km. north-west of the confluence of the two, and since it is the highest point for 6 or 7 km. round about, forms an imposing feature of the landscape. No doubt it is this fact, connected with the proximity of M. d'Irsi to the very important Bradano valley (3 km. distant) that made the M. d'Irsi plateau a prime candidate for settlement even in prehistoric times and presumably in times of stress.

Excavations at Hacılar, First Preliminary Report

1958 ◽  
Vol 8 ◽  
pp. 127-156 ◽  
Author(s):  
James Mellaart
Keyword(s):  
Bronze Age ◽  
Preliminary Report ◽  
River Valley ◽  
Early Bronze Age ◽  
The South ◽  
Entire Surface ◽  
Main Road ◽  
South West ◽  
Antique Dealer ◽  
The Village

The village of Hacilar is situated in the Vilayet of Burdur in South-west Anatolia, about 25 km. west of Burdur itself on the main road to Yeşilova and Denizli. The chalcolithic site lies about 1·5 km. west of the village and just beyond the orchards, which are irrigated by a plentiful spring at the foot of a great limestone crag which overlooks the village. It is this spring which since neolithic times has been the main reason for more or less continuous occupation in this region. Apart from the neolithic and early chalcolithic site at Hacılar there is a large Early Bronze Age mound on the northern outskirts and a classical site to the south-west of the village.The prehistoric site is an inconspicuous mound, about 150 metres in diameter, rising to a height of not more than 1·50 m. above the level of the surrounding fields (Fig. 1 and Pl. XXIXa). The entire surface of the mound is under cultivation and a series of depressions show the holes made by a local antique-dealer in search of painted pots and small objects. About 1 km. west of the site runs the Koca Çay, the ancient Lysis, and on the eastern scarp of this river valley lies the cemetery of the Early Bronze Age settlement. Not a single burial has yet been found in the chalcolithic or neolithic levels of our site and it is therefore not unreasonable to suggest that its cemetery also may eventually be located there.

scholarly journals The first records of Aegopinella ressmanni (Westerlund, 1883) in the Czech Republic extends its distribution range northwards

2008 ◽  
Vol 7 ◽  
pp. 47-50
Author(s):  
Michal Horsák ◽  
Jan Myšák
Keyword(s):  
Czech Republic ◽  
River Valley ◽  
Distribution Range ◽  
The Czech Republic ◽  
Terrestrial Snail ◽  
First Time ◽  
The Village ◽  
The Town

A topsoil-dwelling Eastern Alpine terrestrial snail Aegopinella ressmanni (Westerlund, 1883) was found for the first time in the Czech Republic at nine sites in E Bohemia. Abundant populations of the species occurred in wet habitats of the Tichá Orlice River valley between the village of Hnátnice and the town of Brandýs nad Orlicí. These Czech populations were found 250 km far from the known northernmost sites in Germany and Austria.

scholarly journals Notes and Inscriptions from Pamphylia

1911 ◽  
Vol 17 ◽  
pp. 215-249
Author(s):  
H. A. Ormerod ◽  
E. S. G. Robinson
Keyword(s):  
Sea Level ◽  
The South ◽  
The West ◽  
The North ◽  
Great Rivers ◽  
Short Time ◽  
The Village ◽  
The Town

The following notes were made by us on a short journey in Pamphylia during March 1911.It had been our intention on reaching Adalia about the middle of the month to go at once into Lycia, but the lateness of the season made the higher ground impossible, and it seemed better to spend a short time in examining the country in the immediate neighbourhood of Adalia, much of which was still imperfectly known (Fig. 1).The best description of the Pamphylian plain is that given by Lanckoronski. From the Kestros to the Melas stretches a low-lying, swampy plain, traversed by three great rivers which come down from the Pisidian highlands, feverish in summer, and during the winter months impossible for wheeled traffic. To the west of the Kestros rises a rocky plateau of travertine some hundred feet above sea-level, on which stands the town of Adalia (Attaleia) on cliffs above the sea, which diminish towards the west. To the north of Adalia rises a third level, which viewed from the south, resembles a high raised beach, running roughly parallel with the present coast as far as the village of Barsak. To the east of that point the hills turn in a north-easterly direction and sink gradually down towards the Kestros. The western part of the plateau is crossed by two main roads, leading respectively to Istanoz and Buldur.

scholarly journals The rediscovery of the Madagascar Red Owl Tyto soumagnei (Grandidier 1878) in north-eastern Madagascar

1994 ◽  
Vol 4 (4) ◽  
pp. 305-311 ◽  
Author(s):  
Dominique Halleux ◽  
Steven M. Goodman
Keyword(s):  
Twentieth Century ◽  
Sea Level ◽  
Geographic Range ◽  
Adult Bird ◽  
South West ◽  
North Eastern ◽  
In Captivity ◽  
One Year ◽  
The Village ◽  
The Town

SummaryThe Madagascar Red Owl, known from the eastern rainforest of central Madagascar by a few specimens collected in the nineteenth and early twentieth century and one sight record in 1973, was rediscovered in late July 1993 in north-eastern Madagascar. An adult bird, held in captivity for approximately one year, was located in the town of Andapa. According to the owner, the owl had been obtained south-west of Andapa, near the village of Antanamangotroka, in a forested area connected to the Réserve Spéciale d'Anjanaharibe-Sud, and at about 800 m above sea-level. This record expands the known geographic range of this species and provides the first documentation of its continued existence in over 20 years.La Chouette de Soumagne, connue de la forêt pluviale orientale du Domaine du Centre de Madagascar à travers quelques spécimens collectés au 19ème siècle et début du 20ème siècle et d'aprés une observation en 1973, a été redécouverte à la fin du mois de juillet 1993 au nord-est de Madagascar. Un individu adulte, qui venait de passer plus d'un an en captivité, a été découvert dans la ville d'Andapa. D'après la personne qui détenait l'animal, la chouette avait été capturee au sud-ouest d'Andapa, pres du village d'Antanamangotroka, au sein d'une zone forestière connectée avec la Réserve Spéciale d'Anjanaharibe-Sud, à une altitude d'environ 800 m au-dessus du niveau de la mer. Cette nouvelle donnée constitue une expansion significative de l'aire de distribution de cette espèce et apporte la preuve de la survie de cette espèce endémique qui n'avait pas été observee depuis plus de 20 ans.

The City Walls of Nicaea

Antiquity ◽  
1938 ◽  
Vol 12 (48) ◽  
pp. 437-443 ◽  
Author(s):  
Alfons Maria Schneider
Keyword(s):  
Fruit Trees ◽  
North East ◽  
The North ◽  
The Earth ◽  
Long Sleep ◽  
Water Courses ◽  
The Village ◽  
The City ◽  
The Town ◽  
Subterranean Water

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.

Continental Bell- or Disc-Barrows in Holland with special reference to Tumulus I at Rielsch Hoefke

1938 ◽  
Vol 4 (2) ◽  
pp. 258-271 ◽  
Author(s):  
A. E. van Giffen
Keyword(s):  
Special Reference ◽  
Sea Level ◽  
European Continent ◽  
The Past ◽  
South West ◽  
Peculiar Form ◽  
Open Side ◽  
High Terrace ◽  
The Village ◽  
The Town

There are half a dozen barrows, now restored, on the heath called ‘Rechte Heide’ belonging to the municipality of the village of Goirle in the province of North Brabant, Holland, about 5 km. south-west of the town of Tilburg (fig. 1). The barrows stand on the east bank of the brook called ‘Oude Lei’ a little north of the ‘Rielsch Hoefke’ farm. Although their popular name is ‘De Vijfberg’ (The Five Mounds) in reality they number seven; six of these form a curve with the open side looking east, the seventh one lying a little further south. The height of the surrounding heath is about 20 m. above sea-level. It consists of Rhine-Meuse diluvium, belonging to the so-called high terrace, and it is fairly level.Although more than once disturbed in the past the importance of this group was only perceived by W. J. A. and J. Willems during an excursion in 1935, when they observed that one of them (fig. 1, no. 1) was surrounded by a bank and ditch. The peculiar-form, recognisable at once from the outside (pl. XLIXa), is in my opinion that of a typical bell-barrow which made it at that time unique in Holland and, as far as I know, in the whole of the European Continent.

XIV.—The Discovery of Prehistoric Pits at Peterborough and the Development of Neolithic Pottery

Archaeologia ◽  
1910 ◽  
Vol 62 (1) ◽  
pp. 333-352 ◽  
Author(s):  
G. Wyman Abbott ◽  
Reginald A. Smith
Keyword(s):  
Sea Level ◽  
East Side ◽  
The West ◽  
West Side ◽  
North East ◽  
The North ◽  
South West ◽  
Early Settlement ◽  
Human Habitation ◽  
The Town

The series of relics exhibited to the Society come from an early settlement at Peterborough, dating from a time when flint was in general use, perhaps before the introduction of metal, at least among the poorer inhabitants of the country. The site is a promontory rising out of the Fens and lying on the north-east side of the town. The river Nene joined the Fens about half a mile to the south-west of the site, which is only a few feet above sea-level, and was almost surrounded in times of flood. So far as can be determined at present, the extent of the settlement is several acres, but the ground has not yet been moved except on the west side, where unfortunately no observations were taken. There were no surface indications of human habitation, and no burrows noticed on the promontory or in its neighbourhood. The subsoil is gravel, fine and coarse, varying in depth from 8 to 10 feet. The top 18 inches of gravel, underlying the soil, is reddish brown, mixed with a reddish loam, which sometimes occupies natural pockets 3 to 8 feet deep, cutting down through the gravel and at times reaching the cornbrash below.

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