Abstract
The following paper gives a description of the landscapes formed in the Upper Kama basin in the Holocene. First of all, the authors describe the first river terraces and the most ancient floodplain generations. In the Upper Kama basin, 35 Mesolithic sites are known. During the mapping of the study area, 3 micro regions were identified with a large concentration of Mesolithic settlements and territories with early unknown Holocene sites. The first group includes: the area of the upper Kama near the village of Liokmartovo-Kazantsevo, the old-channel formation of Chashkinskoye Lake and the lower stream of the river Kosa. The second one is the Upper Kama in the Gainy and Kosinsky districts of the Perm region. The analysis of the Mesolithic sites locations showed dependence of the first terraces on the most ancient floodplains of large water arteries. At the same time, this dependence should not be exaggerated because people often settled on smaller rivers and streams.
Highlights
Hermand Jean-Pierre, professor of Acoustics & Environmental Hydroacoustics Laboratory Université libre de Bruxelles (Brussels, Kingdom of Belgium) Rasmussen Hugo, engineer Danish Nitro-Electro (Copenhagen, Kingdom of Denmark)
The following paper gives a description of the landscapes formed in the Upper Kama basin in the Holocene
3 micro regions were identified with a large concentration of Mesolithic settlements and territories
Summary
Лычагина Евгения Леонидовна, кандидат исторических наук, доцент кафедры древней и средневековой истории России. Российская Федерация) Зарецкая Наталия Евгеньевна, кандидат геолого-минералогических наук, старший научный сотрудник лаборатории геохимии изотопов и геохронологии Геологический институт РАН Демаков Денис Александрович, магистрант кафедры древней и средневековой истории России Пермский государственный гуманитарно-педагогический университет В статье дается характеристика ландшафтов, сформировавшихся в бассейне Верхней Камы в раннем голоцене. К первой группе относятся: район Верхней Камы около д. Ко второй – Верхняя Кама в пределах Гайнского и Косинского районов Пермского края. Анализ мест расположения мезолитических памятников показал наличие зависимости от сформировавшихся первых террас и наиболее древних пойм крупных водных артерий. Под Верхним Прикамьем мы понимаем бассейны рек Камы в её верхнем течении, Вишеры, Колвы и Косы в пределах северной части Пермского края и Коми-Пермяцкого округа. В бассейне Верхней Камы известно 35 мезолитических памятников [2]. Лычагина Е.Л., Зарецкая Н.Е., Чернов А.В., Демаков Д.А., Митрошин Е.Н
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