To study the tombstones of the Islamic period of Aqalar Museum of Maragheh (northwest of Iran)

2021 ◽  
Vol 25 (2) ◽  
pp. 561-576
Author(s):  
Saeid Starnezhad ◽  
Karim Hajizadeh Bastani ◽  
Behrooz Afkhami ◽  
Habib Shahbazi Shiran
2018 ◽  
Vol 2 (3) ◽  
pp. 133-148
Author(s):  
Karim Haji Zadeh Bastani ◽  
Esmaeel Maroufi Aghdam ◽  
Said Satar Nezhad ◽  
Fariborz Tahmasebi ◽  
◽  
...  

2017 ◽  
Vol 12 (2) ◽  
pp. 258-269
Author(s):  
Ahad Ebrahimi ◽  
Bagher Asl

Ahar is name of a historical city located in northwest of Iran. The existing documents and historical writings along with some inscriptions, architectural and archeological monuments within the city and its suburbs all indicate the historic antiquity of this city. From the pre-Islamic period, little information is available about Ahar. Some sites such as the Jame mosque of Seljuk period and Sheik Shahab Aldin Ahary’s complex indicate that it was a developed city in the Islamic period. The aim of this investigation is the identification of the factors affecting on the urban evolution process in different historical periods. The spatial organization of Ahar has been developed within the Islamic period, but the hypothesis of research is the indications of pre-Islamic period are in the present-day location of it. The question of research is: what were the components affecting the formation and development of the spatial-urban organization of Ahar? This investigation is a basic research which utilizes the descriptive-analytic method based on the analysis of historical documents’ contents. The necessary information has been obtained through library and field studies. The research results show the following: the formation of Ahar dates back to the pre-Islamic period. Based on some historical documents and narratives, the location of the initial core of the city is considered to have been in the vicinity of the historical graveyard of the city; and since the reign of Islam, the city has developed around the core, yet at some periods of time in the course of history, the city has undergone locational changes and has developed toward the northern and western grounds.


This volume deals with the possibility of glimpsing pre-modern and early modern Egyptian scribes, the people who actually produced ancient documents, through the ways in which they organized and wrote those documents. Breaking with the traditional conception of variation in scribal texts as ‘free’ or indicative of ‘corruption’, this volume reconceptualizes scribal variation in pre-modern Egypt from the point of view of contemporary historical sociolinguistics, seeing scribes as agents embedded in particular geographical, temporal, and sociocultural environments. This volume comprises a set of studies of scribal variation, beginning from the well-established domain of scribal variation in pre-modern English as a methodological point of departure, and proceeding to studies of scribal variation spanning thousands of years, from Pharaonic to Late Antique and Islamic Egypt. This volume introduces to Egyptology concepts such as scribal communities, networks, and repertoires, and applies them to a variety of phenomena, including features of lexicon, grammar, orthography, palaeography, layout, and format.


2021 ◽  
Vol 193 (9) ◽  
Author(s):  
Naser Miran ◽  
Mir Hassan Rasouli Sadaghiani ◽  
Vali Feiziasl ◽  
Ebrahim Sepehr ◽  
Mehdi Rahmati ◽  
...  

2021 ◽  
Vol 37 ◽  
pp. 102903
Author(s):  
Eyal Natan ◽  
Yael Gorin-Rosen ◽  
Agnese Benzonelli ◽  
Deborah Cvikel

2021 ◽  
Vol 3 (3) ◽  
Author(s):  
Akram Alizadeh

AbstractThe Urmia Lake Basin is located between the West and East Azerbaijan provinces in the northwest of Iran. Lake Urmia is the twentieth largest lake and second largest hypersaline lake in the world. Stratigraphic columns have been constructed, using published information, to compare the sedimentary units deposited from the Permian to the Neogene on the east and west sides of the lake, and to use these to quantity subsidence and uplift. East of the lake, the sedimentary section is more complete and has been the subject of detailed stratigraphic studies, including the compilation of measured sections for some units. West of the lake, the section is incomplete and less work has been done; three columns illustrate variations in the preserved stratigraphy for the time interval. In all cases, the columns are capped by the Oligocene–Miocene Qom Formation, which was deposited during a post-orogenic marine transgression and unconformably overlies units ranging from Precambrian to Cretaceous. Permian to Cretaceous stratigraphy is used to measure subsidence in the Lake Urmia basin up to the end of the Cretaceous, and then, the subsequent orogenic uplift, which was followed by further subsidence recorded by the deposition of the Qom Formation in the Oligocene–Miocene.


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