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IN THE NAME OF GOD IRAN NAMA RAILWAY TOURISM GUIDE OF IRAN List of Content Preamble ....................................................................... 6 History ............................................................................. 7 Tehran Station ................................................................ 8 Tehran - Mashhad Route .............................................. 12 IRAN NRAILWAYAMA TOURISM GUIDE OF IRAN Tehran - Jolfa Route ..................................................... 32 Collection and Edition: Public Relations (RAI) Tourism Content Collection: Abdollah Abbaszadeh Design and Graphics: Reza Hozzar Moghaddam Photos: Siamak Iman Pour, Benyamin Tehran - Bandarabbas Route 48 Khodadadi, Hatef Homaei, Saeed Mahmoodi Aznaveh, javad Najaf ...................................... Alizadeh, Caspian Makak, Ocean Zakarian, Davood Vakilzadeh, Arash Simaei, Abbas Jafari, Mohammadreza Baharnaz, Homayoun Amir yeganeh, Kianush Jafari Producer: Public Relations (RAI) Tehran - Goragn Route 64 Translation: Seyed Ebrahim Fazli Zenooz - ................................................ International Affairs Bureau (RAI) Address: Public Relations, Central Building of Railways, Africa Blvd., Argentina Sq., Tehran- Iran. www.rai.ir Tehran - Shiraz Route................................................... 80 First Edition January 2016 All rights reserved. Tehran - Khorramshahr Route .................................... 96 Tehran - Kerman Route .............................................114 Islamic Republic of Iran The Railways -
Novel Hydraulic Structures and Water Management in Iran: a Historical Perspective
Novel hydraulic structures and water management in Iran: A historical perspective Shahram Khora Sanizadeh Department of Water Resources Research, Water Research Institute������, Iran Summary. Iran is located in an arid, semi-arid region. Due to the unfavorable distribution of surface water, to fulfill water demands and fluctuation of yearly seasonal streams, Iranian people have tried to provide a better condition for utilization of water as a vital matter. This paper intends to acquaint the readers with some of the famous Iranian historical water monuments. Keywords. Historic – Water – Monuments – Iran – Qanat – Ab anbar – Dam. Structures hydrauliques et gestion de l’eau en Iran : une perspective historique Résumé. L’Iran est situé dans une région aride, semi-aride. La répartition défavorable des eaux de surface a conduit la population iranienne à créer de meilleures conditions d’utilisation d’une ressource aussi vitale que l’eau pour faire face à la demande et aux fluctuations des débits saisonniers annuels. Ce travail vise à faire connaître certains des monuments hydrauliques historiques parmi les plus fameux de l’Iran. Mots-clés. Historique – Eau – Monuments – Iran – Qanat – Ab anbar – Barrage. I - Introduction Iran is located in an arid, semi-arid region. Due to the unfavorable distribution of surface water, to fulfill water demands and fluctuation of yearly seasonal streams, Iranian people have tried to provide a better condition for utilization of water as a vital matter. Iran is located in the south of Asia between 44º 02´ and 63º 20´ eastern longitude and 25º 03´ to 39º 46´ northern latitude. The country covers an area of about 1.648 million km2. -
HAMIDIYEH, V1 Hamidiyeh - IRAN 0 0 0 0
254500 255000 255500 256000 256500 257000 257500 258000 48°24'40"E 48°25'0"E 48°25'20"E 48°25'40"E 48°26'0"E 48°26'20"E 48°26'40"E 48°27'0"E GLIDE number: FL-2019-000022-IRN Activation ID: EMSR352 Int. Charter call ID: 601 Product N.: 06HAMIDIYEH, v1 Hamidiyeh - IRAN 0 0 0 0 5 5 Flood - Situation as of 08/04/2019 7 7 8 8 4 4 3 3 Grading - Ready-to-print Map 01 N " 0 h 4 e ' h 9 rk 2 a ° K 1 3 Azerbaijan Turkmenistan Caspian N " 0 Sea 4 ' 9 2 ° 1 Tehran 3 ^ Dasht-e-Azadegan Hamidiyeh (! Khuzestan Iran Iraq RTP01 06 Kuwait Saudi Persian 0 0 Arabia Qatar 0 0 Gulf Gulf of Oman 0 0 7 7 8 8 4 4 3 3 6 km Cartographic Information 1:6000 Full color A1, 200 dpi resolution N " 0 2 ' 0 0,125 0,25 0,5 9 2 ° km 1 3 Grid: WGS 1984 UTM Zone 39N map coordinate system N " 0 2 ' Tick marks: WGS 84 geographical coordinate system 9 2 ± ° 1 3 Legend 0 0 0 0 5 5 6 6 8 8 Crisis Information Administrative boundaries 4 4 3 3 Flooded Area (08/04/2019 07:38 UTC) Province Flood trace Placenames ! Built Up Grading Placename Destroyed Hydrography Stream Damaged Reservoir Possibly damaged Transportation Grading River Road, Destroyed Stream Road, Damaged Transportation Bridge and elevated highway Road, Possibly damaged N " Primary Road 0 ' General Information 9 2 ° 1 3 Area of Interest Local Road 0 0 0 0 0 0 Cart Track N 6 6 " 8 8 0 ' 4 4 Ahvaz 9 2 3 3 ° 1 3 Map Information Hamidiyeh ! Severe flooding in several provinces of Iran since mid-March, has left 70 people dead. -
BASRA : ITS HISTORY, CULTURE and HERITAGE Basra Its History, Culture and Heritage
BASRA : ITS HISTORY, CULTURE AND HERITAGE CULTURE : ITS HISTORY, BASRA ITS HISTORY, CULTURE AND HERITAGE PROCEEDINGS OF THE CONFERENCE CELEBRATING THE OPENING OF THE BASRAH MUSEUM, SEPTEMBER 28–29, 2016 Edited by Paul Collins Edited by Paul Collins BASRA ITS HISTORY, CULTURE AND HERITAGE PROCEEDINGS OF THE CONFERENCE CELEBRATING THE OPENING OF THE BASRAH MUSEUM, SEPTEMBER 28–29, 2016 Edited by Paul Collins © BRITISH INSTITUTE FOR THE STUDY OF IRAQ 2019 ISBN 978-0-903472-36-4 Typeset and printed in the United Kingdom by Henry Ling Limited, at the Dorset Press, Dorchester, DT1 1HD CONTENTS Figures...................................................................................................................................v Contributors ........................................................................................................................vii Introduction ELEANOR ROBSON .......................................................................................................1 The Mesopotamian Marshlands (Al-Ahwār) in the Past and Today FRANCO D’AGOSTINO AND LICIA ROMANO ...................................................................7 From Basra to Cambridge and Back NAWRAST SABAH AND KELCY DAVENPORT ..................................................................13 A Reserve of Freedom: Remarks on the Time Visualisation for the Historical Maps ALEXEI JANKOWSKI ...................................................................................................19 The Pallakottas Canal, the Sealand, and Alexander STEPHANIE -
The Anahita Temple at Kangavar
THE ANAHITA TEMPLE AT KANGAVAR The modern town of Kangavar, the site of the Anahita Temple, is situated midway between Hamadan and Kermanshah, on the main historical Hegmataneh-Ctesphon highway. The Temple has an area of 4.6 hectare and is located on a huge schist outcropping that overlooks the Kangavar plain. Like a number of other monumental buildings, the Anahita Temple is constructed on a platform, a technique common on the IRanian plateau in historical periods. The town of Kangavar is the principal population center in the vast plain of Kangavar. This fertile plain is surrounded from the north and northwest by the central Zagros ranges. The Chelmaran heights, the main stone quarry of the region, is located on the west, not far from the Temple. High annual precipitation provides the plain with ample irrigation water supplied by natural springs and the Gamasab river, the confluence of the Khurram-rud, the Asadabad, and te Kangavar rivers. As in many regions in Iran, these rivers and the natural springs have played an important role in the cultural development of the Kangavar plain from prehistoric to the present time. The flourishing prehistoric cultures of Seh-Gabi and Godin, whose type sites are located northeast of Kangavar, and the latter's economic and cultural contact with Susa are indicative of the importance of the region from the early Neolithic to the late Chalcolithic period. Southern view of Anahita Temple The strategic geographical location of the plain also played an important role as the commercial highway and locus of contact between the cultural centers on the west and east streching as far as Khorasan and China. -
New Evidence on the Chronology of the “Anahita Temple”
Iranica Antiqua, vol. XLIV, 2009 doi: 10.2143/IA.44.0.2034383 NEW EVIDENCE ON THE CHRONOLOGY OF THE “ANAHITA TEMPLE” BY Massoud AZARNOUSH (Iranian Center for Archaeological Research, Tehran) Abstract: Partly standing-partly excavated remains of a monument in Kangavar, a town in western Iran between Hamadan and Kermanshah, have been dated to the Seleucid and/or Parthian periods. In an article published in 1981, nevertheless, M. Azarnoush argues in favour of a late Sasanian date for this site. The discovery of a brick under the massive masonry of the western platform of the monument in the course of later excavations provided the possibility for thermoluminescence dating of this sample. The TL reading of the brick confi rms the Sasanian date of the monument. The present article intends to assess this and some other new information about the site. Keywords: W-Iran, Kangavar, Anahita Temple, Sasanian, chronology I- Introduction In an article published in 1981, I argued in favour of a late Sasanian date for the monument of Kangavar, frequently labelled the “Anahita Temple” (Azarnoush 1981: 69-94, Pl. 12-19). By that time I had completed two seasons of excavations on this site, following fi ve seasons of work headed by Seyfollâh-e Kâmbakhsh-e Fard, another Iranian archaeologist of whose expeditions I am certainly honoured to have been a member. Reasons backing the new chronology may be outlined in the following: – Isidor of Charax is the oldest author who mentions the presence of an Artemis Temple in Concobar, most probably the Greek pronunciation for the Iranian Kangavar. -
The Political Economy of the IRGC's Involvement in the Iranian Oil and Gas Industry
The Political Economy of the IRGC’s involvement in the Iranian Oil and Gas Industry: A Critical Analysis MSc Political Science (Political Economy) Thesis Research Project: The Political Economy of Energy University of Amsterdam, Graduate School of Social Sciences 5th June 2020 Author: Hamed Saidi Supervisor: Dr. M. P. (Mehdi) Amineh (1806679) Second reader: Dr. S. (Said) Rezaeiejan [This page is intentionally left blank] 2 Table of Contents Table of Contents ................................................................................................................................ 3 Abstract ............................................................................................................................................... 6 Acknowledgments ............................................................................................................................... 7 Maps ................................................................................................................................................ 8 List of Figures and Tables ................................................................................................................. 10 List of Abbreviations ........................................................................................................................ 11 I: RESEARCH DESIGN .................................................................................................................................... 13 1.1. Introduction ........................................................................................................................ -
Effect of the Kharkhe Storage Dam on Vulnerability of Downstream Land and the Kharkhe Bondary
American-Eurasian J. Agric. & Environ. Sci., 3 (6): 917-921, 2008 ISSN 1818-6769 © IDOSI Publications, 2008 Effect of the Kharkhe Storage Dam on Vulnerability of Downstream Land and the Kharkhe Bondary 1M. Mohammadpour, 2A. Behnia, 2A. M. Akhoond-Ali and 3A. Telvari 1Department of Hydrology, Shahid Chamran University, Ahvaz, Iran 2Shahid Chamran University, Ahvaz, Iran 3Institude of Watershed Manaagement, Tehran, Iran Abstract: River boundaries, as defined by the state law, comprise the land along and surrounding riverbanks expected to be inundated or flooded during flood events of a 25-year return-period. Construction of large water structures such as dams across rivers may lead to considerable decrease in the flood discharge proportionate to structure size which will in turn result in lower flood probability. Assessment of the vulnerability of river boundary is of great importance due to their rich soil and easy access to irrigation water which makes such riverbank farms economically valuable especially in dry areas. The results of such assessment can be used in land use planning. For the purposes of the present study, a reach of 190 km was selected along the banks of the Karkheh River downstream the Karkheh Storage Dam in southern Iran. Estimations were then made of river flood events prior to constructing the dam with return periods of 2 to 100 years and their corresponding post-construction values for the same periods. Values of flood inundation of the river banks were determined for flood events with different return periods. Using the values thus obtained, the vulnerability curve was plotted for various flood probabilities before and after constructing the dam. -
Analyses of the Impact of Climate Change on Water Resources Components, Drought and Wheat Yield in Semiarid Regions: Karkheh River Basin in Iran
HYDROLOGICAL PROCESSES Hydrol. Process. (2013) Published online in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/hyp.9747 Analyses of the impact of climate change on water resources components, drought and wheat yield in semiarid regions: Karkheh River Basin in Iran S. Ashraf Vaghefi,1 S. J. Mousavi,1 K. C. Abbaspour,2* R. Srinivasan3 and H. Yang2 1 Department of Civil and Environmental Engineering, Amirkabir University of Technology, Tehran, Iran 2 Eawag, Swiss Federal Institute of Aquatic Science and Technology, PO Box 611, 8600, Dübendorf, Switzerland 3 Texas A&M University, Texas Agricultural Experimental Station, Spatial Science Lab, College Station, TX, 77845, USA Abstract: Water resources availability in the semiarid regions of Iran has experienced severe reduction because of increasing water use and lengthening of dry periods. To better manage this resource, we investigated the impact of climate change on water resources and wheat yield in the Karkheh River Basin (KRB) in the semiarid region of Iran. Future climate scenarios for 2020–2040 were generated from the Canadian Global Coupled Model for scenarios A1B, B1 and A2. We constructed a hydrological model of KRB using the Soil and Water Assessment Tool to project water resources availability. Blue and green water components were modeled with uncertainty ranges for both historic and future data. The Sequential Uncertainty Fitting Version 2 was used with parallel processing option to calibrate the model based on river discharge and wheat yield. Furthermore, a newly developed program called critical continuous day calculator was used to determine the frequency and length of critical periods for precipitation, maximum temperature and soil moisture. -
Water Resources Management in Karkheh Basin-Iran
PROCEEDINGS OF THE 3RD INTERNATIONAL CONFERENCE ON ENERGY AND DEVELOPMENT - ENVIRONMENT - BIOMEDICINE Water Resources Management in Karkheh Basin-Iran AMIR HAMZEH HAGHIABI1 , NIKOS E. MASTORAKIS2 1-Department of water engineering Lorestan University Khorramabad, Lorestan Province IRAN [email protected] 2- Technical University of Sofia, BULGARIA– also with the WSEAS Research Department, WSEAS, A.I.Theologou 17-23, Zografou, 15773, Athens, GREECE Abstract: - Karkheh basin is located in the semiarid and arid regions of Western Iran, an area with severe water scarcity. 70% of rainfall is directly evaporated. The potential annual evaporation of the southern and northern regions is 3,600 mm 1,800 mm, respectively. Agriculture plays an important role in the economy of the basin. In the present situation, 3.9 bm3 of water are used for irrigating 378,164 ha of irrigated agriculture (horticulture and field crops), and surface water and groundwater resources provide 63 percent and 37 percent, respectively, of this volume. Of the irrigated area, 76.5% is under cereals (wheat and barely), 23% under pulses, and 0.5% under cultivation of forage, orchards, melons and vegetables, and oil seeds. The area is particularly low in terms of yields, productivity and incomes. Irrigation efficiency in the basin is 28-36 percent and the overall Crop Water Productivity in the basin is about 0.55 kg/m3. In this paper, the specifications of the Karkheh Reservoir Dam & Hydroelectric Power Plant as the biggest dam in history of Iran with total volume of reservoir 7.3 Bm3 and Karkheh irrigation and drainage network project are illustrated. Also the situation of water availability in the basin, surface and groundwater potential and some aspects of water resources management in the basin are considered. -
Arkeolojik Verilerin Işiğinda Epi-Paleolitikten Tunç Çaği Sonuna Kadar Anadolu-Iran Ilişkileri
Hacettepe Üniversitesi Sosyal Bilimler Enstitüsü Arkeoloji Anabilim Dalı ARKEOLOJİK VERİLERİN IŞIĞINDA EPİ-PALEOLİTİKTEN TUNÇ ÇAĞI SONUNA KADAR ANADOLU-İRAN İLİŞKİLERİ Bayram Aghalari Doktora Tezi Ankara, 2017 ARKEOLOJİK VERİLERİN IŞIĞINDA EPİ-PALEOLİTİKTEN TUNÇ ÇAĞI SONUNA KADAR ANADOLU-İRAN İLİŞKİLERİ Bayram Aghalari Hacettepe Üniversitesi Sosyal Bilimler Enstitüsü Arkeoloji Anabilim Dalı Doktora Tezi Ankara, 2017 KABUL VE ONAY BİLDİRİM YAYIMLAMA VE FİKRİ MÜLKİYET HAKLARI BEYANI ETİK BEYAN v TEŞEKKÜR Hacettepeli olduğum ilk günden beri beni yönlendiren, yardımlarını esirgemeyen, tez çalışmam konusunda tecrübe ve görüşlerinden yararlandığım danışman hocam Doç. Dr. Halil TEKİN'e sonsuz teşekkürlerimi sunarım. Tez izleme komitemde yer alan Hacettepe Üniversitesi arkeoloji bölüm başkanı Prof. Dr. Sevinç GÜNEL, Prof. Dr. Halime HÜRYILMAZ, Doç. Dr. Ayşegül AYKURT, Ankara Üniversitesi bölüm başkanı Prof. Dr. Tayfun YILDIRIM ve Prof. Dr. Fikri KULAKOĞLU'NA tez çalışmam boyunca bilgilerini benimle paylaşmaları, konuya farklı bakış açılarıyla katkıda bulunmalarından ve beni desteklemelerinden dolayı çok teşekkür ederim. Ayrıca ders aşamasında bilgilerinden yararlandığım bütün Hacettepe Arkeoloji bölümü öğretim üyeleri ve görevlilerine teşekkürlerimi bildirmek isterim. Tez çalışmam boyunca yararlandığım İngiliz Arkeoloji Enstitüsü (BIAA) elemanlarına derin teşekkürlerimi bildirmek isterim. Yanı sıra araştırmanın uygulamasını gerçekleştirdiğim süre içinde teknik yardım ve desteklerini gördüğüm Türk ve İranlı arkadaşlarıma da teşekkür ederim. Maddi Manevi desteklerini esirgemeyen hayatımın her anında yanımda olan, Eğitim ve öğretim hayatım boyunca beni her yönden destekleyen, sevgili aileme derin teşekkürlerim sonsuzdur. vi ÖZET AGHALARİ, Bayram. Arkeolojik verilerin ışığında Epi-Paleolitikten Tunç Çağları sonuna kadar Anadolu-İran ilişkileri, Doktora Tezi, Ankara, 2017. Yukarıda belirtildiği başlıklı bu çalışmada Ön Asya'nın iki önemli coğrafi bölgesi olarak Anadolu-İran ilişki ve bağlantıları Epi-Paleolitik dönemden itibaren ele alınmıştır. -
The Seismicity of Iran. the Firuzabad
The seismicity of Iran. The Firuzabad (Nehavend) earthquake of 16 August 1958 N. AMBRASEYS (*) - A. MOINFAB (**) Received on October 10th, 1973 SUMMARY. — The Firuzabad (Iran) earthquake of the 16th August 1958 had a smaller magnitude (il/ = 6.6) than did the last major earthquake in the same area which occurred on the 13th December 1957, and had a 7.1 magnitude. The Firuzabad earthquake killed 132 and injured about 200 people in 170 villages. It affected an area of 1,100 square kilometres -within which 2,500 housing units were destroyed or damaged beyond repair. The earthquake had its macroseismic epicentre somewhat southeast of the 1957 earthquake and the shock was felt over an area of 80,000 square kilometres. The damage pattern from the Firuzabad earthquake did not resemble that of the 1957 shock, in that the Firuzabad earthquake affected a smaller region but was the more intense of the two. In contrast, the 1957 earthquake had a somewhat more moderate surface intensity over a much wider area. The Firuzabad earthquake was associated with a fault-zone at least 20 kilometres long. This earthquake and the seismic events of the previous year as well as the aftershocks of the 21st of September 1958, show quite clearly a progressive expansion of seismic activity along a northwest-south- west axis in the Zagros mountains. RIASSUNTO. — Il terremoto di Firuzabad (Iran) del 16 Agosto 1958 ebbe una magnitudo inferiore (6.6) di quella del 13 Dicembre 1957 (7.1), la più forte avvenuta in ordine di tempo nella stessa zona; in 170 villaggi, 132 fu- rono i morti e 200 ca.