Tour Option 1: 1 Night 2 Days Pamukkale& Ephesus Day 1

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Tour Option 1: 1 Night 2 Days Pamukkale& Ephesus Day 1 - Istanbul & Pamukkale Meet at Denizli airport and transfer to Pamukkale. Pamukkale, as soon as we arrive we will continue onto guided tour of Pamukkale and Hierapolis. Pamukkale means cotton castle in Turkish. It is the result of limestone formations built over thousands of years. Warm calcium rich mineral water flowed over the cliffs and as it cooled it deposited the calcium into the formations that are seen today. Pamukkale is now a world heritage site. Hierapolis was founded as a healing care center in 190 BC, taking advantage of the mineral waters in the area. It was one of the most important intellectual, artistic, religious and commercial centers of the Roman Empire. Overnight Kusadasi. DAY 2: Ephesus The tour begins by visiting the remains of the the Temple of Artemis, one of the seven wonders of the ancient world. Afterwards, it proceeds to the spectacular main site of Ephesus, undoubtedly the most superbly preserved Greco-Roman city. Unmistakable highlights surviving among the ruins are the Celsius Library, Agora, Theater, Odeon, Trajan Fountain, Domitianus Temple and Roman Latrines. Following a lunch break, visit the House of Virgin Mary; reputed to be where she spent her final days. Evening flight to Antalya Timing: 1 Night 2 Days Tour rates include: - Enterence fees -Transportation during the tours by air-conditioned coach -Professional English-speaking tour guide -1 day accomodation at Hotel including breakfast -1 Lunch Tour rates exclude: -Personal Expenses -Drinks at Lunch -Flight tickets .

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Decreasing Hydrothermalism at Pamukkale- Hierapolis (Anatolia) Since the 7Th Century
EGU2020-20182 https://doi.org/10.5194/egusphere-egu2020-20182 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Decreasing hydrothermalism at Pamukkale- Hierapolis (Anatolia) since the 7th century Bassam Ghaleb1, Claude Hillaire-Marcel1, Mehmet Ozkul2, and Feride Kulali3 1Université du Québec à Montréal, GEOTOP, Montreal, Canada ([email protected]) 2Pamukkale University, Denizli, Turkey 3Uskudar University, Istanbul,Turkey The dating of travertine deposition and groundwater / hydrothermal seepages in relation to late Holocene climatic changes can be achieved using short-lived isotopes of the 238U decay series, as illustrated by the present study of the Pamukkale travertine system, at the northern edge of the Denizli and Baklan graben merging area (see Özkul et al., 2013; https://doi.org/10.1016/j.sedgeo.2013.05.018. The strongly lithified self-built channels and modern pools where analysed for their 238U,234U,230Th, 226Ra, 210Pb and 210Po contents, whereas 238U,234U and 226Ra were measured in modern hydrothermal waters. When corrected for detrital contamination, 230Th-ages of travertine samples range from 1215±80 years, in the oldest self-built hydrothermal channels, to the Present (modern pool carbonate deposits) thus pointing to the inception of the existing huge travertine depositional systems during the very late Holocene, probably following the major Laodikeia earthquate of the early 7th century (cf. Kumsar et al., 2016; DOI 10.1007/s10064-015-0791-0). So far, the available data suggest three major growth phases of the travertine system: an early phase (7th to 8th centuries CE), an intermediate phase (~ 14th century CE) and a modern one, less than one century old.
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