Бюллетень Института истории материальной культуры Российской академии наук: (охранная археология). Сборник статей. Вып. 15. Санкт-Петербург, 2024. С. 17-28., 2024
Аннотация. Статья посвящена исследованию изотопного состава останков людей с некрополя римского в... more Аннотация. Статья посвящена исследованию изотопного состава останков людей с некрополя римского времени античного города Херсонес (Севастополь, Республика Крым). Различие в изотопных отношениях углерода и азота в тканях погребенных в одних и тех же семейных склепах людей говорит о том, что, несмотря на принадлежность к одной родовой группе, тип питания ее членов мог сильно различаться по качеству и обильности. Установлено, что большинство погребенных умерли в межсезонье, в осенне-весеннее время, возможно, от простудных заболеваний.
МАТЕРИАЛЫ ПО АРХЕОЛОГИИ, ИСТОРИИ И ЭТНОГРАФИИ ТАВРИИ. Т. 28, 2023
The generalization and analysis of complex geological, geophysical, and archaeological materials ... more The generalization and analysis of complex geological, geophysical, and archaeological materials has allowed us to clarify and significantly amend the notion concerning the coastal territory of Karantinnaia Bay of Tauric Chersonese in the Hellenistic Period. The information obtained allowed the ones to draw the conclusions about the sources of the city’s water supply, the relationship of the cultural layer with the geological structure of the deluvial and proluvial deposits of the ravine, and the features of the ancient landscape and the coastline of Karantinnaia Bay. The results of engineering-geological, hydrogeological, geophysical, and archaeological works in Chersonesan Ravine and the coastal territory of Chersonese conducted from 2021 to 2023 show that the water-bearing strata of the ravine in question were one of the water supply sources of Chersonese. The main stratum belongs to the fracture-karst type. Owing to its slight mineralization, the water was good for supply. This conclusion is confirmed by the results of archaeological excavations that discovered the “water supply inlet” of ancient Chersonese, consisting of numerous wells cut in the bedrock in the thalweg zone of the ravine. In the ancient city area, the ravine can be seen as an erosional incision of a paleo-valley filled with sands, which comprise the main water-bearing stratum of the coastal territory. The stratum has a hydraulic connection with the seawater of Karantinnaia Bay. The degree of the groundwater salinity in this stratum depends on the sea level. The location of the wells and public baths in the coastal area of the town indicates that the stratum (horizon) provided stock water, for the sea level in the ancient period was significantly lower than today. The sources of water supply in Chersonesan Ravine and the coastal territory of Karantinnaia Bay could be interpreted as one of the important city-forming factors in the Hellenistic Period of Chersonese. The geological section of the deluvial and proluvial deposits of Chersonesan Ravine is represented by a layer of loams forming a cultural layer shaped from the fourth century BC to the thirteenth century AD. The relationship of the cultural layer with the geological structure points to the fact that the accumulation of deluvial and proluvial deposits in the ravine was caused by the activities of Chersonesan inhabitants in the adjacent territories of the Gerakleiskii Peninsula. The structure of the geological and archaeological section confirms the presence of a seasonal water stream in Chersonesan Ravine, which carried proluvial deposits throughout the entire period when the city existed. The significant thickness of the loamy layer behind the proteichism, in contrast to the one observed in the peribolos, may appear in result of the ancient proteichism protecting the peribolos not only from enemies, but also from the flow of proluvial deposits going down from Chersonesan Ravine. Taking the absolute marks of the cultural layer bottom certified by the wells, a detailed map of the bottom relief of Karantin Bay coastal zone, the data obtained by the method of bottom electrotomography, and the established sea level at absolute marks of minus 3–4 m into account, we have determined the contours of the coastline of the bay in the early period of Chersonese
XXI Боспорские чтения. Боспор Киммерийский и варварский мир в период античности и средневековья. Объекты искусства в археологическом контексте / Материалы международной научной конференции / Ред.-сост. В.Н. Зинько, Е.А. Зинько. – Симферополь; Керчь,, 2020
XIX Боспорские чтения. Боспор Киммериский и варварский мир в период античности и средневекоья. Традиции и инновации / Материалы международной научной конференции. Симферополь - Керчь, 2018, 2018
Статья посвящена пароходам «Генерал Коцебу» и «Веста» Русского общества пароходства и торговли, з... more Статья посвящена пароходам «Генерал Коцебу» и «Веста» Русского общества пароходства и торговли, затонувшим в конце XIX в. у западного побережья Крымского полуострова и обнаруженным в последние годы крымскими подводными археологами. Представлены наиболее яркие страницы истории пароходов, которые характеризуются как составная часть подводного культурного наследия у берегов Крыма.
Бюллетень Института истории материальной культуры Российской академии наук: (охранная археология). Сборник статей. Вып. 15. Санкт-Петербург, 2024. С. 17-28., 2024
Аннотация. Статья посвящена исследованию изотопного состава останков людей с некрополя римского в... more Аннотация. Статья посвящена исследованию изотопного состава останков людей с некрополя римского времени античного города Херсонес (Севастополь, Республика Крым). Различие в изотопных отношениях углерода и азота в тканях погребенных в одних и тех же семейных склепах людей говорит о том, что, несмотря на принадлежность к одной родовой группе, тип питания ее членов мог сильно различаться по качеству и обильности. Установлено, что большинство погребенных умерли в межсезонье, в осенне-весеннее время, возможно, от простудных заболеваний.
МАТЕРИАЛЫ ПО АРХЕОЛОГИИ, ИСТОРИИ И ЭТНОГРАФИИ ТАВРИИ. Т. 28, 2023
The generalization and analysis of complex geological, geophysical, and archaeological materials ... more The generalization and analysis of complex geological, geophysical, and archaeological materials has allowed us to clarify and significantly amend the notion concerning the coastal territory of Karantinnaia Bay of Tauric Chersonese in the Hellenistic Period. The information obtained allowed the ones to draw the conclusions about the sources of the city’s water supply, the relationship of the cultural layer with the geological structure of the deluvial and proluvial deposits of the ravine, and the features of the ancient landscape and the coastline of Karantinnaia Bay. The results of engineering-geological, hydrogeological, geophysical, and archaeological works in Chersonesan Ravine and the coastal territory of Chersonese conducted from 2021 to 2023 show that the water-bearing strata of the ravine in question were one of the water supply sources of Chersonese. The main stratum belongs to the fracture-karst type. Owing to its slight mineralization, the water was good for supply. This conclusion is confirmed by the results of archaeological excavations that discovered the “water supply inlet” of ancient Chersonese, consisting of numerous wells cut in the bedrock in the thalweg zone of the ravine. In the ancient city area, the ravine can be seen as an erosional incision of a paleo-valley filled with sands, which comprise the main water-bearing stratum of the coastal territory. The stratum has a hydraulic connection with the seawater of Karantinnaia Bay. The degree of the groundwater salinity in this stratum depends on the sea level. The location of the wells and public baths in the coastal area of the town indicates that the stratum (horizon) provided stock water, for the sea level in the ancient period was significantly lower than today. The sources of water supply in Chersonesan Ravine and the coastal territory of Karantinnaia Bay could be interpreted as one of the important city-forming factors in the Hellenistic Period of Chersonese. The geological section of the deluvial and proluvial deposits of Chersonesan Ravine is represented by a layer of loams forming a cultural layer shaped from the fourth century BC to the thirteenth century AD. The relationship of the cultural layer with the geological structure points to the fact that the accumulation of deluvial and proluvial deposits in the ravine was caused by the activities of Chersonesan inhabitants in the adjacent territories of the Gerakleiskii Peninsula. The structure of the geological and archaeological section confirms the presence of a seasonal water stream in Chersonesan Ravine, which carried proluvial deposits throughout the entire period when the city existed. The significant thickness of the loamy layer behind the proteichism, in contrast to the one observed in the peribolos, may appear in result of the ancient proteichism protecting the peribolos not only from enemies, but also from the flow of proluvial deposits going down from Chersonesan Ravine. Taking the absolute marks of the cultural layer bottom certified by the wells, a detailed map of the bottom relief of Karantin Bay coastal zone, the data obtained by the method of bottom electrotomography, and the established sea level at absolute marks of minus 3–4 m into account, we have determined the contours of the coastline of the bay in the early period of Chersonese
XXI Боспорские чтения. Боспор Киммерийский и варварский мир в период античности и средневековья. Объекты искусства в археологическом контексте / Материалы международной научной конференции / Ред.-сост. В.Н. Зинько, Е.А. Зинько. – Симферополь; Керчь,, 2020
XIX Боспорские чтения. Боспор Киммериский и варварский мир в период античности и средневекоья. Традиции и инновации / Материалы международной научной конференции. Симферополь - Керчь, 2018, 2018
Статья посвящена пароходам «Генерал Коцебу» и «Веста» Русского общества пароходства и торговли, з... more Статья посвящена пароходам «Генерал Коцебу» и «Веста» Русского общества пароходства и торговли, затонувшим в конце XIX в. у западного побережья Крымского полуострова и обнаруженным в последние годы крымскими подводными археологами. Представлены наиболее яркие страницы истории пароходов, которые характеризуются как составная часть подводного культурного наследия у берегов Крыма.
Сборник «Материалы научной археологической конференции «Подводная археология в России: основные н... more Сборник «Материалы научной археологической конференции «Подводная археология в России: основные направления исследований», прошедшей в городе Феодосии с 21 по 23 марта 2018 г. , предназначен для историков, археологов, преподавателей и краеведов. А также для всех, кто интересуется актуальными вопросами современной подводной археологии.
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mineralization, the water was good for supply. This conclusion is confirmed by the results of archaeological excavations that discovered the “water supply inlet” of ancient Chersonese, consisting of numerous wells
cut in the bedrock in the thalweg zone of the ravine. In the ancient city area, the ravine can be seen as an erosional incision of a paleo-valley filled with sands, which comprise the main water-bearing stratum of the coastal territory. The stratum has a hydraulic connection with the seawater of Karantinnaia Bay. The degree of the groundwater salinity in this stratum depends on the sea level. The location of the wells and public baths in the coastal area of the town indicates that the stratum (horizon) provided stock water, for the sea level in the ancient period was significantly lower than today. The sources of water supply in Chersonesan
Ravine and the coastal territory of Karantinnaia Bay could be interpreted as one of the important city-forming factors in the Hellenistic Period of Chersonese. The geological section of the deluvial and proluvial
deposits of Chersonesan Ravine is represented by a layer of loams forming a cultural layer shaped from the fourth century BC to the thirteenth century AD. The relationship of the cultural layer with the geological structure points to the fact that the accumulation of deluvial and proluvial deposits in the ravine was caused by the activities of Chersonesan inhabitants in the adjacent territories of the Gerakleiskii Peninsula. The structure of the geological and archaeological section confirms the presence of a seasonal water stream in Chersonesan Ravine, which carried proluvial deposits throughout the entire period when the city existed.
The significant thickness of the loamy layer behind the proteichism, in contrast to the one observed in the peribolos, may appear in result of the ancient proteichism protecting the peribolos not only from enemies, but also from the flow of proluvial deposits going down from Chersonesan Ravine. Taking the absolute marks of the cultural layer bottom certified by the wells, a detailed map of the bottom relief of Karantin Bay coastal zone, the data obtained by the method of bottom electrotomography, and the established sea level at absolute marks of minus 3–4 m into account, we have determined the contours of the coastline of the bay in the early period of Chersonese
mineralization, the water was good for supply. This conclusion is confirmed by the results of archaeological excavations that discovered the “water supply inlet” of ancient Chersonese, consisting of numerous wells
cut in the bedrock in the thalweg zone of the ravine. In the ancient city area, the ravine can be seen as an erosional incision of a paleo-valley filled with sands, which comprise the main water-bearing stratum of the coastal territory. The stratum has a hydraulic connection with the seawater of Karantinnaia Bay. The degree of the groundwater salinity in this stratum depends on the sea level. The location of the wells and public baths in the coastal area of the town indicates that the stratum (horizon) provided stock water, for the sea level in the ancient period was significantly lower than today. The sources of water supply in Chersonesan
Ravine and the coastal territory of Karantinnaia Bay could be interpreted as one of the important city-forming factors in the Hellenistic Period of Chersonese. The geological section of the deluvial and proluvial
deposits of Chersonesan Ravine is represented by a layer of loams forming a cultural layer shaped from the fourth century BC to the thirteenth century AD. The relationship of the cultural layer with the geological structure points to the fact that the accumulation of deluvial and proluvial deposits in the ravine was caused by the activities of Chersonesan inhabitants in the adjacent territories of the Gerakleiskii Peninsula. The structure of the geological and archaeological section confirms the presence of a seasonal water stream in Chersonesan Ravine, which carried proluvial deposits throughout the entire period when the city existed.
The significant thickness of the loamy layer behind the proteichism, in contrast to the one observed in the peribolos, may appear in result of the ancient proteichism protecting the peribolos not only from enemies, but also from the flow of proluvial deposits going down from Chersonesan Ravine. Taking the absolute marks of the cultural layer bottom certified by the wells, a detailed map of the bottom relief of Karantin Bay coastal zone, the data obtained by the method of bottom electrotomography, and the established sea level at absolute marks of minus 3–4 m into account, we have determined the contours of the coastline of the bay in the early period of Chersonese