logo

Search published articles


Showing 2 results for Anani

Bahram Anani, Mostanser Gholinezhad,
year 8, Issue 28 (8-2024)
Abstract

Abstract
In recent years Archaeologist have taken a special attention at south of Khorasan, especially the Qaen region. Recent archaeological surveys have provided valuable findings for researchers. Specific geographical location and the connection as a natural corridor among central Asia, North of Khorasan, southeast of Iran, and central plateau of Iran, which was made by central desert, can be a great cause in different periods, especially in the early second millennium B.C. The expansion of “GKC” (BMAC) in the Eastern half of Iran is one of the most important developments of the second millennium B.C. New findings show that this culture has spread to parts of South of Khorasan, for example, findings of the Razeh, Gavand and Bekanda previously studied. Sartakhteh Baraz site in Qaen is one of the significant sites in Southern Khorasan in which many evidences of the BMAC have been observed, which is less studied and, in this research, we attempt to introduce this site and identify the expansion of GKC. This site located in a mountainous region in Qaen area in North of Southern Khorasan. This site is much destroyed because it is located near a rural area. The main sources of this research have been chosen from the library sources and survey of Sartakhteh Baraz of Qaen area in 2016. The research method is descriptive-analytical. Then these findings were analyzed and interpreted in theoretical studies. This paper intends to introduce and describing BMAC at the South of Khorasan of Iran Based on evidence of Sartakhteh Baraz site of Qaen; furthermore, its results can demonstrate different aspects of this culture. It seems this culture has expanded in South of Khorasan in the first half of the second millennium B.C. 
Keywords: South of Khorasan, Qaen, GKC (BMAC), Sartakhteh Baraz Site.

Introduction
South Khorasan is located in the east of Iran from a geographical point of view. This region has received less attention in terms of archaeological studies than other regions of the Iranian Plateau. Although these studies have greatly increased in the last decade and have attracted some attention, they are still far from reaching favorable point. South Khorasan, or the current South Khorasan province, geologically has two deserts and mountainous parts. Qaen region, which includes more the mountainous part of the region, is considered one of the cold and rainy regions of the province, so that the average annual rainfall in the city is 180 mm. The pattern of placement of Qaen region is in the form of sometimes continuous mountain ranges in the direction of northwest to Southeast, where Baraz, shaskouh, Ahangaran and Qaen mountains are among the main mountain ranges in the region. Qaen, together with Sarayan and Ferdows covers the northern half of the province, and archaeologically, it is one of the richest areas of Southern Khorasan. Many important settlements of South Khorasan in different periods are scattered in this areas. Strategically, this region forms a link between North Khorasan and Central Asia with the central Plateau and even the southeast. This factor has made the basic and important issues of archaeology in different periods to be tied with archaeology studies in South Khorasan. The studies of BMAC culture in this area are important in the sense that specializes studies and surveys have not been done for this area, and most of the studies include surveys with the purpose of identification. The purpose of the current research is to identify and introduce new evidences is of BMAC culture and explain the spread of this culture in parts of South Khorasan. This research, by using the descriptive-analytical method as well as using field research based on the findings obtained from the archaeological surveys of the central part of Qaen city, tried to analyze and introduce the new evidences obtained from the BMAC culture in the South of Khorasan.
Research questions and Hypotheses: The most important question raised in this research is how to analyze the spread of Great Khorasan culture in South Khorasan? It seems that by identifying new evidences in South Khorasan region, it is possible to discuss this culture more precisely in this region in such a way that it is very likely that the Great Khorasan culture spread in this region in its final stages.

Discussion
The Great Khorasan culture refers to a collection of settlement sites of the late Bronze Age (simultaneous with the V and VI Bronze age) that was formed in a cultured range beyond political borders. This area includes parts of Southern Turkmenistan, Northern Afghanistan, Northeastern Iran, southwestern Tajikistan and Southern Uzbekistan. Among the prominent features of this culture are the presence of distinctive types of pottery, the abundant use of bronze metal and precious metals such as gold and silver, the presence of a variety of prestigious and everyday goods that are made of imported and local stones, including: turquoise, agate, chlorite and marble. In addition to that, collections of unique and possibly ritual objects such as scepters of power, miniature columns, stone weights, mixed stone figurines of seated women in woolen clothes, marble vessels and collections of silver and gold vessels with special reliefs, all it shows specialized industry and exchange economy in this culture (Vahdati, 2015:42-43). 
  In general, the beginning of archaeological activities in the area of GKC (BMAC) in the central east of Iran in recent years, has led to the identification of new settlements and cemeteries of this culture. The new archaeological data and documents obtained from the settlements in the northeast and east of Iran (Khorasan) show the new areas of expansion and influence of GKC. The site of Sartakhteh Baraz of Qaen is one of the most important sites in South Khorasan, where the evidences of GKC has been observed. Sartakhteh Baraz site was first identified during archaeological investigation by Gholinezhad (Gholinezhad, 2016). This area includes large mound with an area of approximately 120×300 meters, which, due to agricultural activities, cultural data are removed from the original context and placed on the slopes and lands prepared for agriculture (fig 2). Therefore, the distribution of cultural materials can be seen on a large scale. The surveys conducted show that the data and evidence obtained include pottery (fig 4), dagger (fig 5), and a wand head (fig 6) vessel of kohl with a rod (fig 7). The pottery data in the area includes samples that belong to the third to second millennium BC according to the forms and types of pottery (Anani 1400: 113). Among these, there are 6 pieces related to the BMAC culture except for the two pieces that have pea paste and cover, the other pieces have orange paste and cover (Table 1). Some of these pottery are very similar to examples of the final stages of the BMAC culture such as Bustan and Molali in the first half of the second millennium BC (Ionesov, 2002). Based on this, it can be concluded that the layers of the BMAC culture in this area belong to the final stage of this culture. In addition to these, bronze tools and artifacts have been found in abundance in the graves related to the BMAC culture with we witness in the prominent sites of this culture such as Gonur Depe (Sarianidi, 2007:90-93).

Conclusion
In recent years the expansion of archaeological activities and surveys in South Khorasan has increased the identification of settlements and sites of different periods. However we are still far from the desired point and it is necessary that many areas of South Khorasan be investigated systematically and of course specialized. During the surveys, 4 sites belonging to the Great Khorasan culture have been identified in the South of Khorasan. However, if we consider Gonabad as part of this region regardless of the current political boundaries, the number of sites will increase. The new findings obtained from the Sartakhteh Baraz site in the Qaen region show the importance of this region in the late Bronze Age. As mentioned in this research, these findings belong to a new culture that appears in this region. The Great Khorasan culture has spread over a wide area from Central Asia to the Iranian plateau. In the meantime, South Khorasan has acted as a communication route and passage. In such a way that it connects the north-east and south of Turkmenistan to the south-east and the center of the Iranian plateau. Accordingly, it is obvious that we are facing the remains of this culture in this region. But the important question raised here is why most of the areas obtained in this region are cemeteries? Although the answer to this question is not the goal of the present study, before answering this question, it should be noted that all these sites have been archaeologically investigated and none of them have been stratified. The sites that have been explored have only been speculated and demarcated. However during these speculations, it has been almost determined that some of these areas are cemeteries. In the meantime, considering the difference that Sartakhte Baraz site has with other contemporaneous sites and has evidence from earlier periods, it creates the possibility that we may be facing a settlement here. Accordingly, in order to reach a reasonable answer, it is necessary to carry out a stratigraphy excavation in this area in order to be able to answer this question and of course many questions related to this culture in South Khorasan. Another important point that was mentioned and raised as a hypothesis is that the settlements in South Khorasan probably belong to the final stages (first half of the second millennium BC) of the GKC. of course, this assumption also needs more studies in the entire eastern region of Iran. It is hoped that more ambiguities can be answered in the future.

Sanam Janani, Mehdi Razani, Hadi Ebrahimi,
year 9, Issue 32 (8-2025)
Abstract

Abstract
Damage to cultural artifacts after discovery occurs due to various factors. One of these harmful cases is moisture originating from underground water, which appears as soil moisture, and over time, due to the oxidation process and the salts and ions in the water, as well as the incompatible pH of the environment with the texture and construction of the artifacts, it aggravates the process of destruction. In line with the mission of archaeometry as a bridge between archeology and other sciences, hydrogeology is used in this study in order to protect ancient artifacts. Iron Age Museum of Tabriz is located in the central area of the city and among the young Quaternary sediments that form the free aquifer of Tabriz. Underground water is one of the main factors causing corrosion and decay in the bones in this museum site. There are various solutions for lowering the water table locally, which according to the location coordinates and technical requirements of the site, the best method is to use underground water pumping. In this study, by using the available data in the study zone which is taken from the Tabriz urban train project and the data obtained from the Regional Water Company of East Azarbaijan, by using computer methods, the appropriate amounts of water pumping have been simulated according to the optimal water level drop and We define the placement of bones in a dry position. The use of new sciences for archeometric purposes is the main goal of this study and an attempt is made to solve the problem of destruction of ancient bones by establishing this connection.
Keywords: Conservation, Groundwater, Pumping Well, Soil Moisture, Tabriz Iron Age Museum.

Introduction
The discovery of ancient bones belonging to the Iron Age of the first and second millennium BC in the area of Tabriz Blue Mosque in 1997 is an important event in the field of archeology and ancient anthropology in Azarbaijan. When this ancient area has been discovered, studies have been carried out in the fields of dating about these bones and studies related to the origin and the migration (Kasiri, 2019) and the conservation and restoration of the graves in the Iron Age Museum area in 2016 was carried out by Majidi and Razani. In recent years, the effect of humidity on buried organisms in the soil has been the subject of many researchers’ studies. Soil moisture can play an important role in decomposition (Swift et al, 1979). Fluctuations of groundwater in the soil is one of the most important factors affecting microbial activity in the field conditions (Lund and Goksoyr, 1980). Iron Age Museum of Tabriz is located in the central area of this city and among the young Quaternary sediments that form the unconfined groundwater aquifer of Tabriz. Tabriz aquifer has an alluvial nature, which has expanded as a result of the Mehran Rood River flowing in its ancient path and creating numerous meanders during geological time. Hydrogeology as a new branch of earth sciences and engineering studies the condition, behavior and hydrological characteristics of the layers of the earth. As a porous environment, the basement contains soil grains, and the empty space between these grains can be saturated with water and provide a path for the flow of groundwater. The voracity of water movement in the basement compared to the surface currents is very low and varies from a few centimeters per year to several meters per day. Due to passing through various minerals and rocks, groundwater often has a significant amount of different solutes and has relatively high electrical conductivity (E.C). These solutes can cause a lot of damage to cultural works by sedimentation or crystallization in case of evaporation of groundwater. The climatic conditions of each region are different in the occurrence of damaging moisture factors and their effects in different seasons of the year (Nawai, 2016). The amount of humidity in the environment, which can cause destruction due to freezing with the participation of the temperature change parameter, will cause serious damage due to the transport of new solutes and sedimentation at each stage and the recrystallization of previous sediments. In addition to the above, the penetration of moisture through underground water can change the pH of the environment, and this change causes the destruction of cultural works by increasing the acidity.

Discussion
Iron Age Museum of Tabriz, as a result of its archaeological excavations, 108 graves were identified, based on the typology of pottery and metal artefacts and the method of burial and comparing them with the collections discovered from the excavations of Hassanlou Hill and Dinkhah Tepe, dating from around 1200 to 800 BC and the period of Iron Age I and II have been estimated for them, which of course is relatively consistent with the results of carbon 14 dating of these sites (Hojbari Nubri, 1381 and 1383). Its cultural, historical, social and economic nature, along with the aesthetic quality and historical and cultural importance of that area; The type of constituent materials and the composition and method of construction of the works found in it, the value, validity and information and messages hidden in those findings and how they are used are valuable documents of its cultural heritage collection. These works, mainly from archaeological excavations, have been obtained over several years, and their preservation in relatively inappropriate conditions has led to the progress of damage caused by the burial of these objects in the ground, and after a rather long period of time, they will disappear (Bagherzadeh Kasiri, 2016, 8). Based on the studies of Tabriz Urban Railway line 1, water level data is available near the study area of Asr Ahan Museum site, and according to the principle that the groundwater level almost follows the topography, it is possible to estimate the groundwater level in The location of the museum was found. For this purpose, the water level data was collected in the study boreholes near the study area (Table 8) and the map of the ISO lines of ground water in the study area was drawn (Fig. 10). It is necessary to explain that ISO lines or equipotential lines of groundwater are curves on each of these curves, the level of ground water has the same values and the map of parallel lines shows the changes of the level of ground water in the study area. It is possible to draw this type of map both manually and by using software that allows for interpolation and drawing. Next, modeling of groundwater drawdown due to pumping from the extraction well was done using GMS software version 16.4. For archeological stratification, before installing the drilling machine, a manual well should be dug to the desired diameter and to the depth of the ground water, and after reaching the depth of the underground water, the drilling machine will continue drilling from inside this well until it hits The stone should be foamed.

Conclusion
The Iron Age Museum site of Tabriz is one of the prominent sites in the northwest of the Iran, which is facing major problems due to the groundwater infiltration. This research uses information and data of the studies of the aquifer of this region with taking account to the problem of how to intervene in the ancient sites. It has provided a solution to deal with the problem of groundwater in order to reduce its flow, and in this regard, by introducing the place of preliminary evaluations using speculation and Finally suggests a piezometric well to start working in this area and control the groundwater level. Noting that the change of seasons and amount of rainfall can affect the condition of groundwater to some extent; Therefore, by changing the flow rate and duration of pumping, other values of drawdown can be achieved. For this reason, it is suggested that if the plan is implemented, a piezometer well should be drill as close as possible to the museum site so that the condition of the groundwater as well as the amount of its draw done due to pumping from the extraction well can be under immediate control. To prevent the water used in the green space and other uses of the museum site from returning to the area of ancient graves, drainage channels should be used between the area and the main space of the museum.


Page 1 from 1