{"id":4170,"date":"2021-03-26T17:13:41","date_gmt":"2021-03-26T14:13:41","guid":{"rendered":"http:\/\/journal.phaselis.org\/?p=4170"},"modified":"2021-04-19T15:40:08","modified_gmt":"2021-04-19T12:40:08","slug":"pha-0135","status":"publish","type":"post","link":"https:\/\/journal.phaselis.org\/en\/2021-en\/pha-0135","title":{"rendered":"Phaselis Teritoryumu, \u00dc\u00e7oluk K\u00f6y\u00fc Ekizce Yaylas\u0131\u2019nda Tespit Edilen K\u00fclt Alan\u0131 Yap\u0131ta\u015flar\u0131 ve \u00c7evresinin Jeolojik \u00d6zellikleri"},"content":{"rendered":"

The Cut-Stones of Cult Area of Ekizce Plateau, \u00dc\u00e7oluk Village in Phaselis Territorium and Geological Features of Environment<\/span><\/strong><\/em><\/p>\n

Ferda \u00d6NER
\n\"\"<\/sub><\/strong>\u00a0https:\/\/orcid.org\/0000-0002-9278-6164<\/p>\n

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PHASELIS<\/em> VII (2021) 47-54
\n<\/strong>DOI<\/strong>: 10.18367\/Pha.21005
\nReceived Date<\/strong>: 14.01.2021 | Acceptance Date<\/strong>: 18.03.2021
\nOnline Publication Date<\/strong>: 26.03.2021<\/p>\n

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\u00d6z:\u00a0<\/strong>Phaselis Antik kenti teritoryumunda yer alan k\u00fclt alan\u0131 Phaselis\u2019in 48 km kuzeybat\u0131s\u0131nda \u00dc\u00e7oluk k\u00f6y\u00fc Ekizce yaylas\u0131 Tahtac\u0131 Mezarl\u0131\u011f\u0131\u2019nda bulunmaktad\u0131r. K\u00fclt alan\u0131nda g\u00f6r\u00fclen yap\u0131ta\u015flar\u0131 adak ta\u015f\u0131, yaz\u0131t ve k\u00fclt alan\u0131ndaki teraslamalarda kullan\u0131lm\u0131\u015ft\u0131r. Ekizce yaylas\u0131 ve \u00e7evresinde birbirini \u00fczerleyen naplar g\u00f6r\u00fclmektedir. Tektonik dilimler kuzey g\u00fcney do\u011frultuda, do\u011fudan bat\u0131ya do\u011fru bindirmi\u015flerdir. K\u00fclt alan\u0131 Alak\u0131r\u00e7ay nap\u0131n\u0131n Tahtal\u0131 Da\u011f\u0131 nap\u0131na bindirdi\u011fi alanda yer almaktad\u0131r. Alak\u0131r\u00e7ay nap\u0131na ait birimler Triyas ya\u015fl\u0131 kilta\u015f\u0131 kumta\u015f\u0131 ardalan masive radyolarit \u00e7amurta\u015f\u0131 ardalanmalar\u0131 olarak g\u00f6r\u00fclmektedir. Bunlar\u0131n \u00fczerine Tahtal\u0131da\u011f nap\u0131n\u0131n Tekelida\u011f formas\u00adyonu olarak isimlendirilen neritik kire\u00e7ta\u015flar\u0131 tektonik olarak yerle\u015fmi\u015flerdir. Tekelida\u011f neritik kire\u00e7ta\u015flar\u0131 sahada en \u00fcst kotlar\u0131 olu\u015fturmaktad\u0131r. Yaz\u0131tlar ve teras duvarlar\u0131nda kullan\u0131lan kire\u00e7ta\u015flar\u0131 Tekelida\u011f neritik kire\u00e7ta\u015flar\u0131\u00adna, kumta\u015flar\u0131 ise Alak\u0131r\u00e7ay grubuna ait kumta\u015flar\u0131d\u0131r. K\u00fclt alan\u0131n kullan\u0131lan ta\u015flar as\u0131l olarak neritik kire\u00e7ta\u015flar\u0131\u00add\u0131r. Bu kire\u00e7ta\u015flar\u0131n\u0131n k\u00fclt alan\u0131n\u0131n do\u011fusunda yer alan kuzey-g\u00fcney y\u00f6nl\u00fc bir s\u0131rt olu\u015fturan Anlak ve Anl\u0131ca tepelerin yama\u00e7lar\u0131ndan al\u0131nm\u0131\u015f oldu\u011fu tahmin edilmektedir. Bu s\u0131rt olduk\u00e7a dik bir yar olu\u015fturmaktad\u0131r. Bu yar\u0131n alt kesimlerinde do\u011fal olmas\u0131 m\u00fcmk\u00fcn olmayan \u00e7ok say\u0131da d\u00fcz kesilmi\u015f bloklara rastlanm\u0131\u015ft\u0131r. Neritik kire\u00e7\u00adta\u015flar\u0131, k\u0131r\u0131kl\u0131 yap\u0131lar\u0131 ve dik konumda olmalar\u0131 nedeniyle zamanla y\u0131k\u0131lm\u0131\u015ft\u0131r. G\u00fcn\u00fcm\u00fczde bu aynalardan \u00fcretilen bir\u00e7ok blok ta\u015f\u0131 yama\u00e7 molozlar\u0131n\u0131n aras\u0131nda bulmaktay\u0131z. Zaman\u0131ndaki ta\u015f oca\u011f\u0131n\u0131n Anlak tepeden (kuzey ocak) Anl\u0131ca tepeye (g\u00fcney ocak) kadar uzayan yakla\u015f\u0131k 1 km uzunlu\u011funda aynas\u0131 oldu\u011fu tahmin edilmektedir.<\/p>\n

Anahtar s\u00f6zc\u00fckler:<\/strong> Phaselis, K\u00fclt Alan\u0131, Yap\u0131 Ta\u015flar\u0131, Ocak Yeri<\/p>\n

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Abstract:\u00a0<\/strong>The cult area, located in the territory of the ancient city of Phaselis, is located in \u00dc\u00e7oluk village Ekizce plateau, Tahtac\u0131 Cemetery (Karabal\u00e7\u0131k Cemetery), 48 km northwest of Phaselis. The votive stone of the building stones seen in the cult area was used in the inscriptions and terraces in the cult area. The Ekizce pedestrian and surrounding nappes are observed overlapping each other. Tectonic slices thrust from east to west in the north-south direction. Cult Area is located in the area where the Alak\u0131r\u00e7ay nappe thrusts the Tahtal\u0131 Mountainnappe. The units belonging to the Alak\u0131r\u00e7ay nappe are seen as Triassicaged claystones and stone alternation and radiolarite mudstone alternations. The neritic limestones, which are named as Tekelida\u011f formation of the Tahtal\u0131da\u011f nappe, are tectonically overlaid over these. Tekelida\u011f neritic limestones constitute the highest elevations in the field. The limestones used in the inscriptions and terrace walls belong to Tekelida\u011f neritic limestones, and the sandstones belong to the Alak\u0131r\u00e7ay group. The stones used in the cult area are mainly neritic limestones. It is estimated that the limestones were taken from the slopes of Anlak and Anl\u0131ca hills that form a north-south ridge located in the east of the cult area. This ridge creates a very steep slope. In the lower parts of this period, many straight cut blocks, which cannot be natural, were found. Neritic limestones collapsed over time due to the irfractured structure and the irvertical position. Today, we find many block stones produced from the semirrors among the slope rubble. It is estimated that the quarry of its time was a mirror of approximately 1 km long extending from Anlak Tepe (northern hearth) to Anl\u0131ca hill (southern hearth).<\/p>\n

Keywords: <\/strong>Phaselis, Cult Area, Building Stones, Quarry Location<\/p>\n

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