Settlements in the Bronze Age

Total Page:16

File Type:pdf, Size:1020Kb

Settlements in the Bronze Age The Gentral Black Sea Region and the Kelkit River basin settlements in the Bronze Age By $evket Dönmez i. Keywords: Northern Anatolia, Samsun, Black Sea Region, survey, settlement pattern, Bronze Age The geographical area under discussion in this zone. Settlements of the earlv 2nd paper covers the region from Samsun in the west mill. B.C. have been identified there at (Map1) to Bayburl in the east (Map2). I have Kelebeg Tepe, Azay Tepe, Tepe Tarla. chosen this area that we may call the East Black Tepe,' Elmacrk Tepe, Tepecik, Karageyh Sea Region hinterland in order to collect the ex- Omer Usta Tepesi, Evren Uga[r, Pagagel isting archaeological evidence and thus make an si, Katrrdamr-Tepecik, Aqa$r Tepe, Krzkayasr assessment. (Gelinkayasr), Kolay-Tepecik, Hacrbaba Tepesr The Kelkit River (ancient Lykos) is the most im- and Kirmancik-Tepecik. However, in some settle- podant river in this area. Because of its geogra- ments on the Bafra Plain, only Early Bronze Age phical advantages this river basin must have housings were revealed. These are Bakrrdere been used as a trade route between the Central Tepesi and Kocakaya. But at Yigitler Tepesi in Black Sea Region, Caucasia and Western lran. the eastern parl of the Bafra Plain was no Early Kelkit River rises from Gümüghane Province, Bronze Age settlement following the Chalcolithic passes through the south of Giresun Province as Period, the next settlement occuring during the well as the Regadiye, Niksar and Erbaa districts Middle Bronze Age. Bengü village in the vicinity of of Tokat Province until it finally joins the Yegilrr- Kolay Town, the majority of which now lies under mak River near Tagova Dlstrict in the Amasya the Altrnkaya Dam, was locatecj on the last ter- Province. The west side of the Kelkit Basin that races overlooking the Krzrllrmak (ancient Halys). begins in Koyulhisar has been thoroughly investi- The field surveys carried out there by J. A. Den- gated and few settlements have been located gate before the beginning of U. B. Alkrm's re- there (Maps 1; 2). Although the east side which search revealed a few Bronze axes and a pair of consists of the Sugehri, $ebinkarahisar, $iran Bronze castanets dating back to the Late Bronze and Kelkit districts has not undergone any ser- Age by him2. Apart from these, there are no fino- ious resarch yet, we still get information regarding ings or settlements known from the second half this area from the neighbouring Bayburt province. of 2nd mill. B.C. in Bafra Province. Between Bafra and Alacam, most of the settle- ments such as Sivritepe, Gökgebogaz Tepesi (Ali Samsun Province Osman Tepesi), Dede Tepe and girlek Tepe (Cir- lek Tepe/Kuggular Höyü!ü/Hogkadem Tepesi) re- Samsun Provincel, which has the highest popu- vealed several pieces of pots and pans dating Iation density, is in the Alacam-Bafra-19 Mayrs from the Early and Middle Bronze Age. Alkrm car- ried out researches on site and C. Burney's field 1 survey in I955 introduced Gökgebo$az Tepesi For researches in Samsun Province, comp. Alktm 1g72a, 422-426; Alkrm 1972b, 56; Alkrm 1973a, 435-438; Alkrm and $irlek Tepesi to the archeology world3. Bur- 1973b, 62-65; Alkrm 1973c, 5-16; Alkrm 1974a, 23-28i ney pointed out that several potsherds from the .1974c, Alkrm 1974b, 553-556; Alkrm 50-53; Alkrm 1975, Early and Middle Bronze Age were found at Gök- 5-12; Alkrm 1976a,717-719; Alkrm 1976b, 42-44i Atkm nohnöaz Tonoci 1978a, 542-547; Alkrm 1978b, 23-27', Alkm 1982, 3-9; Alkrm etal. 1988; Alkrm etal. 2003; Bilgi 1990a, 211-220i The settlements revealed in the city center, Bilgi 1990b, 25-28; Bilgi 2000, 109-127; Bilgi 2001a, Bilgi namely Dündadepe (Fig.1), Ba! Tepesi, De- 2001b, 1-35; Bilgi etal. 2002, 279-296; Bilgi etal. 2003, deüstü 41-50; Bilgi elal. 2004, 87-96; Burney 1956, 179*203; Din- Tepesi, Göktepe, Akalan, Diklim Tepe gol/Yakar 1974,563-582; Dönmez 1999, 513-536; Dönmez and Kaleyeri Tepesi, were shown to have been 2000a,229-244; Dönmez 2000b, 330 334; Dönmez 2001, occupied during the Early and Mlddle Bronze 302-307; Dönmez 2002a, 873-903; Dönmez 2002b, 243- Age. Only Büyük Oyumca Tepesi revealed 293; Gökoglu 1952; Inan 1947, 119-132: Krztltan 1992, no 213*241i Kökten 1941, 121-124i Kökten 1944, 659-689; settlement following the Early Bronze Age. Kökten/Özgüg 1940a, 413-419; KökteniÖzgüg 1940b, 25- 28; Kökten/Ozgüq 1940c, 13-16; Kökten etal. 1945, 361- 400; Özgü9.'1941, 637: Özgü9 1948, 393-419; Özsait 1988, 239-256; Ozsait 1990b, 124-130: Ozsait 1999b, 89-107; 2 Ozsait 2O0Ob, 335-341; Özsait 2001. 307-312; Özsait 2003, Dengate 1971, 199; Dengate 1978,25g. 127-1401 Ozsait 2004, 273-284; Yakar/Dincol 1974, 85-99 " Burney 1956, 182. 102 $evket Dönmez ,,'-..--.'.-.r-S' / ,S' { E{ I #l l,-o] r'Ll. f rf't \r ;" '1-'ro" *t,l __Tokat.,, -=-]$;1{, | 'l'i .-._.___ ' t\lt r.{*;'),f_;=,t'-/ J {- ,r .'---- Map 1 r-----.*-'d-T- t_ *"tir. ,r./ Samsun. Western pafl -:,r__._,,.\ of survey area. MaP 2 Bayburt. Eastern part ur rutvuy drvd. In and near the Yegilrrmak (ancient lris) Valley both in the Early and Middle Bronze Age, in the east of Samsun Province no dense setile- whereas Tepecik, Kilise Tepesi and Tünbü Tepe ment has been witnessed up to the present day. are understood to have been settled durino the However, in Tekkeköy (Fig. 2) and in the south of Early Bronze Age. the Qarqamba District, Tepecik and Kilise Tepesi, Vezirköprü District, in the south-west of Sam- Ayvacrk-Tünbü Tepesi and Asarcrk-Koyuncuo$lu sun Province, was discovered to have been den- Höyü$ü settlements were discovered. Except for sely settled not only in the 3rd but also in the 2nd Tekkeköy all othör settlements were located on mill. B.C. The earliest Bronze Age seülements hills. Tekkeköy is known to have been occupied found in this area are Keltepe, Dolan Tepe, and the Kelkit River basin settlements in the Bronze Aqe Fig. 1 Samsun-Dündartepe from South. Fig.2 Tekkeköy from South Kurudere, Ya$rnözü-Qakmak, Qörlen Tepe, Kügük- proven to have been Middle Bronze Age settle- kale, Oymaagaq Höyük (Höyük Tepe), Yeltepesi ments. Oymaagaq Höyügü takes an impodant and Sivri Tepe. Among these, only Oymaaöaq place among Vezirköprü settlements. Dengate Höyük, Keltepe, Küqükkale and Sivri Tepe were dated a spear-head and blade which he found 104 $evket Dönmez Fig.3 Köyiqi Tepesil/urtyeri Tepesi from North-West. there to the second half of the 3'd mill. B.C. On Only a few of the mounds located in Ladik Drs- top of Oymaagag Höyügü, located 7 km nortn- trict were deserted after the Early Bronze Age east of Vezirköprü city centre and about 500 m ro and not resettled. These are Agcrtepe, Aqa(r Be- the west of Oymaa$aq Village, some remains re- lenaca Tepesi, inkaya, Kurban Tepe, öolma sembling city walls and an underground construc- Tepe, Kireglik, Qakrr Höyük, Agrkh Egme Höyür<, tion resembling a postern have been uncovereo Inboynu Höyük, Dökme Tepe, Kahpe Tepe, Des- during illegal excavations. The above mentioned timen Tepe, lbi, Alabag Tepe, Dogankag and construction was built by use of the shouldereo Kemalyeri. Other mounds in this area were conti- vault techniquea. These finds as well as the pot- nually inhabited from the Early to the Middle sherds indicate that Oymaagag Höyügü was a Bronze Age. These are Dedealtr Tepesi, Tombul big and imporlant settlement surrounded by city- Tepe, Kale Tepe, Kümbet Tepe, Kilise Tepe, walls in the 2nd mill. 8.C., that is the Middle ano Devgerkaya Tepesi, Sarrgazel, Köyiqi Tepesil/ur- Late Bronze Age. tyeri Tepesi (Fig. 3), Salur-Yüktepe, Budakdere- The seven mounds in the Havza District were Köyyeri Höyük and Mrhlr Tepe. Besides, it is as- inhabited from the Early Bronze Age onwards sumed that Salur Höyük (Mound), which was sur- and in the Middle Bronze Age. These setilements rounded by city walls in the 2nd mill. 8.C., was in- are Tepecik, Qegtepe, Patlangrg Tepe, Dökme habited during the Late Bronze Age, that is the Tepe l, Hakim Tepe l, Tagkaracaören Tepe and Hittite lmoerial Periods. Cin Tepe l. Other mounds are found to have ln the Kavak District however, three settle- been deserted after the Early Bronze Age. They ments, namely Güney Tepesi, Tepesidelik Tepe were either given up or resettled during the Middle and Kaletepe, were abandoned at the end of the Bronze Age. Such settlements on plains are Early Bronze Age and not resettled. The remain- found at Manevra Tepe, Cin Tepe ll, Hakim Tepe ing settlements at Kaledoru$u, Dingilkalecik Tepe, ll (BekdiQin Tepe), Cevizbagr Tepesi, Cam Tepe, Danabasan Tepe, Hacrbaba Tepe and Aytepe Bacas Tepe, Kayah Tepe, Garco Tepe, ören are considered to have been inhabited during Tepe, $eyh SafiTepesi, Kömürlük Höyügü, Muhtis both the Early and Mlddle Bronze Age. These Tepe and Boyalr. settlements which lie either on or near the Sam- 4 5 Ark,m 1973a.437 Yakar/Dinqol 1974, 92 The Central Black Sea Region and the Kelkit River basin settlements in the Bronze Age 105 ."-; T. {rl.'l lliirrrl:'" w:.iE Fig.4 Paralr Tepe ll from West. sun-Kavak highway, most probably held control form the Yegilrrmak proper; this covers the cen- over this impodant route. tral district of Amasya Province as well as Gü- müghacrköy, Hamamözü, Merzifon and Göy- nücek. The most imoortant settlements in these Amasya Province distrlcts are considered to have existed only dur- ing the Early Bronze Age. They are Hacrprnarr The number of 3'd and 2nd mill.
Recommended publications
  • Polyporus Squamosus (Huds.) Fr
    Turkish Journal of Agriculture - Food Science and Technology, 6(2): 183-188, 2018 Turkish Journal of Agriculture - Food Science and Technology Available online, ISSN: 2148-127X www.agrifoodscience.com, Turkish Science and Technology Polyporus squamosus (Huds.) Fr. in the Black Sea Region Sanem Bulam1*, Nebahat Şule Üstün2, Aysun Pekşen3 1Department of Food Engineering, Faculty of Engineering, Giresun University, 28200 Giresun, Turkey 2Department of Food Engineering, Faculty of Engineering, Ondokuz Mayıs University, 55139 Atakum/Samsun, Turkey 3Department of Horticulture, Faculty of Agriculture, Ondokuz Mayıs University, 55139 Atakum/Samsun, Turkey A R T I C L E I N F O A B S T R A C T Polyporus squamosus (Huds.) Fr., also named as Aladana, Peri Semeri, Pullu Mantar in Review Articles varying by localities of Turkey, is an edible wild mushroom species widely existed in the mycobiota of the Black Sea Region. It has not been sold in the local markets. The public Received 18 September 2017 recognition of this mushroom may change locally in the Black Sea Region. It is widely Accepted 29 January 2018 consumed by the people in some parts of the region. It is usually appeared in the nature during May-September on the logs, dead and living trunks of the deciduous trees. Keywords: Following the rainy period, it grows so fast and can produce a few kilograms fruit body Polyporus squamosus Black Sea Region within a short period. It is delicious and precious as much as meat for the nutritional Morphological value, especially during early growth stage. In this review, general knowledge on the Mushroom morphological and ecological characteristics, nutritional value and medicinal properties Nutritional of P.
    [Show full text]
  • Empirical Correlations of Shear Wave Velocity (Vs) and Penetration Resistance (SPT-N) for Different Soils in an Earthquake-Prone Area (Erbaa-Turkey)
    Engineering Geology 119 (2011) 1–17 Contents lists available at ScienceDirect Engineering Geology journal homepage: www.elsevier.com/locate/enggeo Empirical correlations of shear wave velocity (Vs) and penetration resistance (SPT-N) for different soils in an earthquake-prone area (Erbaa-Turkey) Muge K. Akin a,⁎, Steven L. Kramer b, Tamer Topal c a Dept. of Geological Engineering, Yuzuncu Yıl University, Van, Turkey b Dept.of Civil and Environmental Engineering, University of Washington, Seattle, USA c Dept. of Geological Engineering, Middle East Technical University, Ankara, Turkey article info abstract Article history: The seismicity of the northern part of Turkey is mainly controlled by the North Anatolian Fault zone (NAFZ). Received 17 August 2010 The NAFZ is one of the world's most active seismic zones, and has produced destructive earthquakes and Received in revised form 17 January 2011 related hazards in the northern region of Turkey. Several earthquakes and earthquake-related hazards have Accepted 24 January 2011 occurred along different segments of this fault zone in the recent past. The study area, Erbaa town, is located Available online 2 February 2011 along the eastern segment of North Anatolian Fault Zone (NAFZ) and is one of the largest towns of Tokat Province in the Middle Black Sea Region of Turkey. The center of Erbaa is located on the left embankment of Keywords: SPT-based uphole the Kelkit River. After the disastrous 1942 (Ms =7.2) and 1943 (Ms =7.6) earthquakes, the settlement was Shear wave velocity shifted southwards. SPT-N As a part of a seismic microzonation study of the Erbaa area, shear wave velocity (Vs) values of the geological Erbaa units exposed in this area were required for site response analyses.
    [Show full text]
  • Palaeoearthquakes on the Kelkit Valley Segment of the North Anatolian Fault, Turkey
    Turkish Journal of Earth Sciences (Turkish J. Earth Sci.), Vol.C. ZABCI20, 2011, ET pp. AL. 411–427. Copyright ©TÜBİTAK doi:10.3906/yer-0910-48 First published online 14 June 2010 Palaeoearthquakes on the Kelkit Valley Segment of the North Anatolian Fault, Turkey: Implications for the Surface Rupture of the Historical 17 August 1668 Anatolian Earthquake CENGİZ ZABCI1,*, HÜSNÜ SERDAR AKYÜZ1, VOLKAN KARABACAK2, TAYLAN SANÇAR3,4, ERHAN ALTUNEL2, HALİL GÜRSOY5 & ORHAN TATAR5 1 İstanbul Teknik Üniversitesi, Ayazağa Yerleşkesi, Jeoloji Mühendisliği Bölümü, Maslak, TR−34469 İstanbul, Turkey (E-mail: [email protected]) 2 Eskişehir Osmangazi Üniversitesi, Jeoloji Mühendisliği Bölümü, TR−26040 Eskişehir, Turkey 3 İstanbul Teknik Üniversitesi, Ayazağa Yerleşkesi, Avrasya Yerbilimleri Enstitüsü, Maslak, TR−34469 İstanbul, Turkey 4 Tunceli Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, TR−62000 Tunceli, Turkey 5 Cumhuriyet Üniversitesi, Jeoloji Mühendisliği Bölümü, TR−58140 Sivas, Turkey Received 02 November 2009; revised typescript receipts 20 May 2010; accepted 14 June 2010 Abstract: Th e 26 December 1939 Erzincan (Ms= 7.8) and 20 December 1942 Erbaa-Niksar (Ms= 7.1) earthquakes created a total surface rupture more than 400 km between Erzincan and Erbaa on the middle to eastern sections of the North Anatolian Fault. Th ese two faulting events are separated by a 10-km-wide releasing stepover, which acted like a seismic barrier in the 20th century. To understand the rupture behaviour in this structurally complex section of the North Anatolian Fault, we undertook palaeoseismological trench investigations on the Kelkit Valley segment where there is little or no palaeoseismic information. We found evidence for three surface faulting earthquakes predating the 1939 event during the past millennium in trenches excavated in Reşadiye and Umurca.
    [Show full text]
  • New Species of Trichoptera ( Hydroptilidae, Philopotamidae) from Turkey and the List of the Species of Ordu and Giresun Provinces in Northeastern Anatolia1
    © Biologiezentrum Linz/Austria; download unter www.biologiezentrum.at Denisia 29 347-368 17.07.2010 New species of Trichoptera ( Hydroptilidae, Philopotamidae) from Turkey and the list of the species of Ordu and Giresun provinces 1 in northeastern Anatolia F. SİPAHİLER Abstract: In the present paper the following new species are described and illustrated: Hydroptila mardinica nov.sp. (Hydroptilidae) from southeastern Anatolia, and Wormaldia malickyi nov.sp. (Philopotamidae) and Philopotamus giresunicus nov.sp. (Philopotamidae), both from northeastern Anatolia. A faunistic list for Ordu and Giresun provinces, located in the western part of northeastern Turkey, is given. A sketch map of the localities is provided. In this region, 85 species are recorded, belonging to 19 families. Of these, 38 species (44.7 %) are known in the western part of Turkey. This area constitutes the boundary of the distribution of western species. Caucasian/Transcaucasian species are represented in this region by 25 species (29.4 %); the rate increases in the eastern provinces of northeastern Anatolia to 42.8 % (60 species). Chaetopteryx bosniaca MARINKOVIC, 1955 is a new record for the Turkish fauna. K e y w o r d s : Trichoptera, fauna, Ordu, Giresun, new species, northern Turkey. Introduction The new species Hydroptila mardinica nov.sp. (Hydroptilidae), with asymmetrical genitalia, belongs to the occulta species group. In Turkey, most of the species of this group are found in southern Turkey. H. mardinica nov.sp. is the second species of this group to occur in southeastern Anatolia. The new species of the family Philopotamidae, Wormaldia malickyi nov.sp. and Philopotamus giresunicus nov.sp., are found in the same place in Giresun province, a small spring on the rising slopes of the mountain.
    [Show full text]
  • Assessment of Avalanche Hazard Situation in Turkey During Years
    Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2018-205 Manuscript under review for journal Nat. Hazards Earth Syst. Sci. Discussion started: 7 August 2018 c Author(s) 2018. CC BY 4.0 License. 1 2 Assessment of avalanche hazard situation in Turkey during years 2010s 3 Tayfun Kurt 4 Independent researcher, Istanbul, Turkey, [email protected] 5 6 ABSTRACT 7 8 Avalanches constitute risky situations especially for mountainous areas in the eastern part of Turkey. 9 According to records of the Disaster and Emergency Management Presidency, avalanches have killed 10 30 people per year in Turkey over the last 30 years. Developing winter tourism also affects losses. For 11 example, an avalanche occurred in Torul, Köstere, in the province of Giresun, on January 25, 2009, 12 which killed 10 mountaineers and injured 7 people. 13 14 This research is focused on, known fatal avalanches and avalanche mitigation works. The obtanied 15 map provides are reliable and easy to understand information where avalanches contstitue 16 risksy sitation in regional scale as well as where new avalanche paths may develop under 17 favourable conditions. Moreover the figure of avalanche hazard situation is presented to construct a 18 picture of the potential threats. This paper provides information about avalanche fatalities and avalanche 19 mitigation works in Turkey. 20 21 Keywords: Avalanche situation, avalanche hazard in Turkey, avalanche hazard 22 management. 23 24 25 26 27 1 Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2018-205 Manuscript under review for journal Nat. Hazards Earth Syst.
    [Show full text]
  • Articles and Archives of Official Institutions
    Open Access Nat. Hazards Earth Syst. Sci., 14, 1145–1154, 2014 Natural Hazards www.nat-hazards-earth-syst-sci.net/14/1145/2014/ doi:10.5194/nhess-14-1145-2014 and Earth System © Author(s) 2014. CC Attribution 3.0 License. Sciences Avalanche situation in Turkey and back calculation of selected events A. Aydın1, Y. Bühler2, M. Christen2, and I. Gürer3 1Düzce University Faculty of Forestry, Konuralp Campus, 81620 Düzce, Turkey 2WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260 Davos Dorf, Switzerland 3Professor Emeritus, Gazi University Faculty of Engineering Civil Engineering Department, Maltepe 06570 Ankara, Turkey Correspondence to: A. Aydın ([email protected]) Received: 24 December 2013 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 21 January 2014 Revised: – – Accepted: 8 April 2014 – Published: 19 May 2014 Abstract. In Turkey, an average of 24 people die in snow one-fourth of the total land surface on earth and are home avalanches every year, mainly in the eastern part of Anato- to about 1/10 of all human beings (Ives et al., 1997; Price lia and in the eastern Black Sea region, where high-mountain and Butt, 2000). Seventy-eight percent of Turkey’s land sur- ranges are close to the sea. The proportion of people killed face consists of mountains, with 33.4 million people (about in buildings is very high (87 %), especially in comparison to 47 % of the country’s total population) living in these regions other European countries and North America. In this paper (EEA, 2010). we discuss avalanche occurrence, the climatic situation and Turkey in general is comprised of two peninsulas, Thrace historical avalanche events in Turkey; in addition, we identify and Anatolia, with a 2-D area of 769 471 km2, excluding bottlenecks and suggest solutions to tackle avalanche prob- lakes (Elibüyük and Yılmaz, 2010).
    [Show full text]
  • Table 2. Geographic Areas, and Biography
    Table 2. Geographic Areas, and Biography The following numbers are never used alone, but may be used as required (either directly when so noted or through the interposition of notation 09 from Table 1) with any number from the schedules, e.g., public libraries (027.4) in Japan (—52 in this table): 027.452; railroad transportation (385) in Brazil (—81 in this table): 385.0981. They may also be used when so noted with numbers from other tables, e.g., notation 025 from Table 1. When adding to a number from the schedules, always insert a decimal point between the third and fourth digits of the complete number SUMMARY —001–009 Standard subdivisions —1 Areas, regions, places in general; oceans and seas —2 Biography —3 Ancient world —4 Europe —5 Asia —6 Africa —7 North America —8 South America —9 Australasia, Pacific Ocean islands, Atlantic Ocean islands, Arctic islands, Antarctica, extraterrestrial worlds —001–008 Standard subdivisions —009 History If “history” or “historical” appears in the heading for the number to which notation 009 could be added, this notation is redundant and should not be used —[009 01–009 05] Historical periods Do not use; class in base number —[009 1–009 9] Geographic treatment and biography Do not use; class in —1–9 —1 Areas, regions, places in general; oceans and seas Not limited by continent, country, locality Class biography regardless of area, region, place in —2; class specific continents, countries, localities in —3–9 > —11–17 Zonal, physiographic, socioeconomic regions Unless other instructions are given, class
    [Show full text]
  • Surveying Georgia's Past on the Use of Cartographic Sources For
    Annali di Ca’ Foscari. Serie orientale [online] ISSN 2385-3042 Vol. 53 – Giugno 2017 [print] ISSN 1125-3789 Surveying Georgia’s Past On The Use Of Cartographic Sources For Caucasian History Patrizia Licini (Associazione Geografi Italiani, AGeI) Abstract This study represents the historical geographer’s approach to the History of cartography. Modern historians of the Roman Empire and archaeologists misuse geographical information from Ptolemy’s map of the Caucasus–Ptolemy’s 3rd Map of Asia in the standard set of twenty-seven maps, including a world map, all in the Ptolemaic model, with twenty-six regional maps. In fact, modern writers on ancient history think that the story of maps is linear–beginning, middle and end. But the case of Ptolemy is typical in that his work began to have a powerful influence in the fifteenth cen- tury. After Ptolemy’s death in the second half of the second century, however, his Geography had disappeared for a thousand years, and with it the idea of coordinate-based mapping according to a mathematical grid system. No original copies from Ptolemy’s own time have survived. A medieval Greek copy without maps only reappeared in fourteenth-century Florence, with maps first drawn by Florentine cosmographers in further copies in 1415. Here we have an antinomia, an apparent contradiction, which nothing but the History of cartography solves as “Ptolemy’s paradox”. Ptolemy’s maps of Roman Britain makes a striking contrast with the map showing our present state of knowl- edge about the British Isles. It has long been recognized as a puzzling fact that, in Ptolemy’s map of the British Isles, the shape of Britain is turned abruptly to the east from the latitude 55° north, cor- responding to Scotland, so as to make a right angle with the southern part of the country–England and Wales.
    [Show full text]
  • ETİ Elektrik Üretim A.Ş
    AKINCI 13.1) Environmental Impact Assessment (EIA) regarding AKINCI HES project has been completed and enclosed approved report and details can be analyzed. ETİ Elektrik Üretim A.Ş. Sahrayıcedit. Man., Omca Sk. No 37, Golden Plaza E Blok, Kat: 1 D: 3-4 Tel. : 0 216 355 16 30 34734 Kozyatağı – İSTANBUL Fax : 0 216 355 16 39 Form No : G 604 1 T.R. Ministry of Environment and Forestry General Directorate of Environmental Impact Assessment and Planning Date of decision : 18/03/2008 Decision No: 1457 EIA Certificate In accordance with article 14 of Environmental Impact Assessment Regulation coming into force through publication on 16.12.2003 dated and 25318 numbered Official Gazette, "Akıncı HES Facilities and Material Mines" project has been approved positive in terms of Environmental Impact Assessment. Owner of the project: Eti Elektrik Üretim A.Ş. Location of the project: Tokat province, Reşadiye and Niksar districts 2 ETI ELEKTRİK ÜRETİM A.Ş. Final EIA Report Regarding AKINCI HES Facilities and Material Mines TOKAT PROVINCE NİKSAR and REŞADİYE DISTRICTS KELKİT STREAM ROGHT COAST LOCALITY DERYA MÜHENDİSLİK MÜŞAVİRLİK İNŞAAT SANAYİ VE TİCARET ANONİM ŞİRKETİ İSTANBUL-2008 3 ETİ Elektrik Üretim A.Ş. Akıncı HES Plants and Material Centres Final ÇED (Environmental Effect Assessment) Report Name of the project owner ETİ ELEKTRİK ÜRETİM A.Ş. Address SAHRAYICEDIT.OMCA SK.No:37 GOLDEN PLAZA E BLOK KAT:1 DAİRE:3 - 4 KADIKÖY/İSTANBUL Phone and Fax numbers TEL: +90(216)355 16 30 FAX: +90(216) 355 16 39 Name of the project TOKAT PROVINCE AKINCI HES FACILITIES AND MATERIAL MINES Open address of the location selected for TOKAT PROVINCE NİKSAR and the project (province, district, region, REŞADİYE DISTRICTS KELKİT locality) STREAM RIGHT COATS LOCALITY Name of the company/study group DERYA MÜHENDİSLİK arranging the report MÜŞAVİRLİK İNŞAAT SANAYİ VE TİCARET ANONİM ŞİRKETİ (Derya Engineering Consultancy Construction Industry and Trade Inc.
    [Show full text]
  • 19 Aceitação Para Publicação: 10/13/2019
    The effects of livestock supports and external input use on profitability of beef cattle farming: 368 the case of Samsun Province, Turkey Eroglu, N.A.; Bozoğlu, M. The effects of livestock supports and external input use on profitability of beef cattle farming: the case of Samsun Province, Turkey Recebimento dos originais: 03/03/2019 Aceitação para publicação: 10/13/2019 Nevra Alhas Eroglu (corresponding author) Phd in Agricultural Economics Institution: Regional Directorate of Turkish Statistical Institute Address: Canik Municipality Mevlana campus, Samsun, Turkey. E-mail: [email protected] Mehmet Bozoğlu Professor in Agricultural Economics (PhD) Institution: Ondokuz Mayis University, Department of Agricultural Economics, College of Agriculture Address: Ondokuz Mayis University campus, Samsun, Turkey. E-mail: [email protected] Abstract Though beef cattle breeding sector has been substantially supported in Turkey, domestic demand could not been sufficiently met and price of beef meat has been steadily increased. By the way, the cost of production has considerably been raised. The objective of this study is to examine the profitability of beef meat. The sample of the study was determined by stratified sampling method from the members of Red Meat Producers Association and the cross sectional data was collected from 171 beef cattle farms via farm surveys. The results of the study indicated that the production of average beef meat was 19067 kg, whereas gross profit and relative profit were USD 60435.24 and 1.34, respectively. The breeding material (40.79%), concentrate feed (34.46%) and roughage (6.49%) had the highest share in the production cost. The cattle breeding supports raised the relative profit to 1.40.
    [Show full text]
  • Hydrogeological and Groundwater Investigations of Niksar Basin, Tokat, Turkey
    Journal of Himalayan Earth Sciences Volume 54, No. 1, 2021 pp. 69-89 Hydrogeological and Groundwater Investigations of Niksar Basin, Tokat, Turkey Syed Mobasher Aftab1* 1Balochistan University of Information Technology, Engineering & Management Sciences, Quetta *Corresponding author's email: [email protected] Submitted date: 03/06/2020 Accepted date: 24/02/2021 Published online: 31/03/2021 Abstract The study area comprises the Niksar Basin of Tokat district, located in the Middle Black Sea region, Turkey. The Kelkit River flows through the center of Niksar Valley. The lithological units exposed on the northern and southern parts of Kelkit River have disparate geological sequences; grouped as "Pontid" and "Anatolit" respectively. The micritic and biomicritic limestone of Upper Jurassic - Lower Cretaceous, limestone of Upper Cretaceous, and the detrital limestone of Upper Cretaceous - Lower Paleocene form characteristic karstic aquifers. In the valley, a thick sequence of loose gravel, sand, and clayey materials of Pliocene and Quaternary are deposited. The presence of clay lenses in these materials created suitable hydrodynamic conditions for the formation of confined and unconfined aquifers. The karstic aquifers recharged through precipitation and valley-fill aquifer through Kelkit River. These aquifers fulfill the water supply demands of the entire population of Niksar Town and surrounding villages. This paper summarizes hydrogeological research conducted on all basinal formations. The Karstic aquifers and the unconfined aquifer of valley-fill sediments were systematically analyzed. The physical characteristics of the aquifer formations, karstification, occurrence, and movement of groundwater, recharge, and discharge sources, and discharge hydrograph analysis were conducted. The exposed hydrogeological formations were recharged through precipitation by 0.329x109m3 and discharged by 0.317x109m3 during the study period.
    [Show full text]
  • On the Staphylinidae of Turkey VI. Thirteen New Species and Additional Records (Coleoptera: Staphylinidae)
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Koleopterologische Rundschau Jahr/Year: 2009 Band/Volume: 79_2009 Autor(en)/Author(s): Assing Volker Artikel/Article: On the Staphylinidae of Turkey VI. Thirteen new species and additional records (Coleoptera: Staphylinidae). 117-172 ©Wiener Coleopterologenverein (WCV), download unter www.biologiezentrum.at Koleopterologische Rundschau 79 117–172 Wien, Juli 2009 On the Staphylinidae of Turkey VI. Thirteen new species and additional records (Coleoptera: Staphylinidae) V. ASSING Abstract Thirteen species are described from Turkey: Aleochara (Ceranota) simplicicornis sp.n. (Ordu, Erzurum), Aploderus transversicollis sp.n. (Samsun), Atheta (Parameotica) soganlica sp.n. (Trabzon), Borboropora myrmecophila sp.n. (Antalya), Gabrius pravus sp.n. (Samsun), Gyrophaena ciliciana sp.n. (Adana), G. cultellata sp.n. (Samsun), G. spoliata sp.n. (Samsun), Ochthephilum hamatum sp.n. (Muğla), Oxypoda meybohmi sp.n. (Kahramanmaraş), O. miricornis (Kahramanmaraş), Stenus (Hemistenus) abstrusus sp.n. (Gümüşhane, Giresun, Trabzon), and S. (H.) abrasus sp.n. (Rize). The sexual characters of several additional species are illustrated. Aleochara caloderoides ASSING, 2007 is attributed to the subgenus Ceranota STEPHENS, 1839. The preoccupied name Atheta akiensis ASSING, 2006 is replaced with Atheta albomontis nom.n. A lectotype is designated for Lathrobium decipiens CZWALINA, 1888, a preoccupied senior synonym of Tetartopeus czwalinai (JAKOBSON, 1909); its habitus and aedeagus are illustrated. A total of 39 species are recorded from Turkey for the first time, one of them, also for Morocco, Kyrgyzstan, Iran, and various European countries. Numerous new province records are reported. The distributions of five species are mapped. Key words: Coleoptera, Staphylinidae, Turkey, new species, replacement name, lectotype designation, additional records, taxonomy, distribution.
    [Show full text]