Issue 21
Issue 21
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2024-01-28
MAGNETIC INVESTIGATIONS IN THE SHAHRIZOR PLAIN, IRAQI KURDISTAN
Archaeological features, such as architecture etc. can be traced by high resolution and large-scale magnetometer prospecting. Moreover, soil magnetic data deliver additional information about the alteration of the ancient landscape. In combination with an archaeological survey, the geophysical results can provide information to reconstruct the spatial organization within these settlements as well as an epoch-spanning analysis of settlements and their role in urbanization processes and within settlement hierarchies.
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2024-01-28
Human Landscape - Site (Trans-) Formation in the Transtigris Area
he formation of Ear per rone Age centres in pesopotamia is the resut of ong term processes hich can be e pained b en ironmenta economica and socia de eopments heir phsica appearance is not on a testimon of centrai ation but aso of the socia eoution relected in its impact on andscapes Large te sites surrounded b a eb of roads for inter-regiona and inter-site communication traceabe through aeria and sate ite photograph ofer a testing ground for ne methods hie the pains of northern S ria ha e itte ariation in terrain the centra Trans‐Tigris area sho s a high diferentiated terrain afected b the ridges of the agros iedmont one
2024-03-28
PRELIMINARY REPORT OF THE CHARMO (JARMO) PREHISTORIC INVESTIGATIONS, 2022
The archaeological mission from the University of Tsukuba began to investigate the Neolithic sites in the Iraqi-Kurdistan region in 2014. The purpose of our investigations was to reconsider the issue of Neolithization in Iraqi-Kurdistan, where research began in the 1940s and 50s and was stalled by political issues starting in the 1960s. With the full support of the Directorate General of Cultural Heritage of the Ministry of Culture of the Kurdistan Regional Government and the Slemani Department of Cultural Heritage, we first began our research at the Qalat Said Ahmadan site, located in the Pshdar Plain. We were able to identify the cultural deposits of the end of the Pre-Pottery Neolithic period, those of the Hassuna, Samarra, Halaf, Ubaid, and Iron Age, and have clarified the nature of the Neolithic site located at the edge of the fan deposits [Tsuneki et al. 2015, 2016, 2019].