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Bam, Iran Earthquake of 26 December 2003, Mw6.5: a Study on the Strong Ground Motions
13th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 8001 BAM, IRAN EARTHQUAKE OF 26 DECEMBER 2003, MW6.5: A STUDY ON THE STRONG GROUND MOTIONS Mehdi ZARE1 SUMMARY The Bam earthquake of 26 December 2003 (Mw6.5) occurred at 01:56:56 (GMT, 05:26:56 local time) around the city of Bam in the southeast of Iran. The Bam earthquake of 26/12/2003 (Mw6.5) has demolished the city of Bam, having a population of about 100000 at the time of the earthquake. The Bam fault - which was mapped before the event on the geological maps - has been reactivated during the 26/12/2003 earthquake. It seems that a length of about 10km (at the surface) of this fault has been reactivated, where it passed exactly from the east of the city of Bam. The fault has a slop towards the west and the foci of the event was located closed to the residential area (almost beneath the city of Bam). This caused a great damage in the macroseismic epicentral zone; however the strong motions have been attenuated very rapidly, specially towards the east-and west (fault normal) direction. The vertical directivity effects caused the amplification of the low frequency motions in the fault-normal direction as well as the greater amplitude of the motion on the vertical direction. INTRODUCTION The Bam earthquake of 26/12/2003 (Mw6.5) demolished the city of Bam in the southeast of Iran (Figure- 1). The earthquake happened at 5:26 am local time when most of the inhabitants were slept, that can be one of the causes of the great life losses. -
Review and Updated Checklist of Freshwater Fishes of Iran: Taxonomy, Distribution and Conservation Status
Iran. J. Ichthyol. (March 2017), 4(Suppl. 1): 1–114 Received: October 18, 2016 © 2017 Iranian Society of Ichthyology Accepted: February 30, 2017 P-ISSN: 2383-1561; E-ISSN: 2383-0964 doi: 10.7508/iji.2017 http://www.ijichthyol.org Review and updated checklist of freshwater fishes of Iran: Taxonomy, distribution and conservation status Hamid Reza ESMAEILI1*, Hamidreza MEHRABAN1, Keivan ABBASI2, Yazdan KEIVANY3, Brian W. COAD4 1Ichthyology and Molecular Systematics Research Laboratory, Zoology Section, Department of Biology, College of Sciences, Shiraz University, Shiraz, Iran 2Inland Waters Aquaculture Research Center. Iranian Fisheries Sciences Research Institute. Agricultural Research, Education and Extension Organization, Bandar Anzali, Iran 3Department of Natural Resources (Fisheries Division), Isfahan University of Technology, Isfahan 84156-83111, Iran 4Canadian Museum of Nature, Ottawa, Ontario, K1P 6P4 Canada *Email: [email protected] Abstract: This checklist aims to reviews and summarize the results of the systematic and zoogeographical research on the Iranian inland ichthyofauna that has been carried out for more than 200 years. Since the work of J.J. Heckel (1846-1849), the number of valid species has increased significantly and the systematic status of many of the species has changed, and reorganization and updating of the published information has become essential. Here we take the opportunity to provide a new and updated checklist of freshwater fishes of Iran based on literature and taxon occurrence data obtained from natural history and new fish collections. This article lists 288 species in 107 genera, 28 families, 22 orders and 3 classes reported from different Iranian basins. However, presence of 23 reported species in Iranian waters needs confirmation by specimens. -
Characteristics of 2017 Hojedk Earthquake Sequence in Kerman Province, Southeast Iran
Revista Geoaraguaia ISSN:2236-9716 Barra do Garças – MT v.10, n. esp. Geologia e Pedologia p.187-201. Dez-2020 CHARACTERISTICS OF 2017 HOJEDK EARTHQUAKE SEQUENCE IN KERMAN PROVINCE, SOUTHEAST IRAN CARACTERÍSTICAS DA SEQUÊNCIA DE TERREMOTO HOJEDK 2017 NA PROVÍNCIA DE KERMAN, SUDESTE DO IRÃ Nassim Mahdavi-Omran1 Mohammad-Reza Gheitanchi2 ABSTRACT Kerman province in southeast Iran, has experienced historical and instrumentally recorded earthquakes. In December 2017, three destructive earthquakes have occurred around Hojedk, in Kerman within 11 days. In this study, first the regional seismotectonics and seismicity is presented. Then, the source mechanisms of main shocks are modeled and the results are compared with the active faults and seismicity pattern is discussed. Moment tensor inversion in time domain is used to obtain the source mechanism of earthquakes. The results indicate that the mechanisms of main shocks and aftershocks are mainly reverse and are in agreement with the trend of tectonic forces as well as the mechanisms of other earthquakes. The epicentral distribution of aftershocks indicates two clusters. The spatial distributions of clusters are in agreement with the epicentral distribution of main shocks. The cluster around the first earthquake in EW cross section has a length 15-20 Km, while the cluster around the second and third has a length about 20-25 Km. The Hojedk earthquakes occurred along the northern extension of previous earthquakes where a kind of seismic gap could be observed and still exists. In 1972, within five days four earthquakes with magnitudes 5.5 to 6.2 occurred in Sefidabeh region in eastern edge of Lut block. -
Interseismic Slip-Rate of the Kuhbanan-Lakar Kuh Faults System: Using Insar Technique
EH-09260582 INTERSEISMIC SLIP-RATE OF THE KUHBANAN-LAKAR KUH FAULTS SYSTEM: USING INSAR TECHNIQUE Sajjad MOLAVI VARDANJANI M.Sc. Student, Graduate University of Advanced Technology, Kerman, Iran [email protected] Majid SHAHPASANDZADEH Associate Professor, Graduate University of Advanced Technology, Kerman, Iran [email protected] Ali ESMAEILY Assistant Professor, Dept. of Surveying Eng., Graduate University of Advanced Technology, Kerman, Iran [email protected] Mohammad Reza SEPAHVAND Assistant Professor, Graduate University of Advanced Technology, Kerman, Iran [email protected] Saeede KESHAVARZ Assistant Professor, Graduate University of Advanced Technology, Kerman, Iran [email protected] Keywords: Interseismic deformation, Geodetic fault slip-rate, InSAR, Kerman, Kuhbanan-Lakar Kuh fault system The Kuhbanan fault with ~ 300 km length, one of the largest seismogenic faults in the southeast of Iran, has caused st st several catastrophic earthquakes with Ms 5-6.2 in 20 -21 centuries (Table 1). Moreover, the corresponding cross-thrusts were also associated with at least five clusters of medium-magnitude earthquakes. The Lakar Kuh fault with ~160 km length run parallel to the Nayband fault (Figure 1). The slip-rate of faults and also the spatio-temporal distribution of large-magnitude shallow-depth earthquakes on the Kuhbanan-Lakar Kuh fault system, attain broad concern for seismic hazard assessment (Figure 1). The horizontal slip-rate of the Kuhbanan fault is estimated ~1–2 mm/yr (Walker et al., 2012). Furthermore, the total horizontal displacement of the fault is reported ~5–7 km, as determined by the offset geological markers (Table 2). Table 1. -
Coleoptera: Meloidae) in Kerman Province, Iran
J Insect Biodivers Syst 07(1): 1–13 ISSN: 2423-8112 JOURNAL OF INSECT BIODIVERSITY AND SYSTEMATICS Research Article https://jibs.modares.ac.ir http://zoobank.org/References/216741FF-63FB-4DF7-85EB-37F33B1182F2 List of species of blister beetles (Coleoptera: Meloidae) in Kerman province, Iran Sara Sadat Nezhad-Ghaderi1 , Jamasb Nozari1* , Arastoo Badoei Dalfard2 & Vahdi Hosseini Naveh1 1 Department of Plant Protection, Faculty of Agriculture and Natural Resources, University of Tehran, Karaj, Iran. [email protected]; [email protected]; [email protected] 2 Department of Biology, Faculty of Sciences, Shahid Bahonar University of Kerman, Kerman, Iran. [email protected] ABSTRACT. The family Meloidae Gyllenhaal, 1810 (Coleoptera), commonly known as blister beetles, exist in warm, dry, and vast habitats. This family was studied in Kerman province of Iran during 2018–2019. The specimens were Received: collected using sweeping net and via hand-catch. They were identified by the 23 December, 2019 morphological characters, genitalia, and acceptable identification keys. To improve the knowledge of the Meloidae species of southeastern Iran, faunistic Accepted: 11 September, 2020 investigations on blister beetles of this region were carried out. Totally, 30 species belonging to 10 genera from two subfamilies (Meloinae and Published: Nemognathinae) were identified. Among the identified specimens, 22 species 14 September, 2020 were new for fauna of Kerman province. Subject Editor: Sayeh Serri Key words: Meloidae, Southeastern Iran, Meloinae, Nemognathinae, Fauna Citation: Nezhad-Ghaderi, S.S., Nozari, J., Badoei Dalfard, A. & Hosseini Naveh, V. (2021) List of species of blister beetles (Coleoptera: Meloidae) in Kerman province, Iran. Journal of Insect Biodiversity and Systematics, 7 (1), 1–13. -
Numerical Investigation of Groundwater Balance and Artificial Recharge in the Kerman-Baghin Aquifer
Journal of Hydraulic Structures J. Hydraul. Struct., 2021; 7(2):1-21 DOI: 10.22055/jhs.2021.36940.1166 Numerical investigation of groundwater balance and artificial recharge in the Kerman-Baghin Aquifer Sina Pakmanesh 1 Mahnaz Ghaeini-Hessaroeyeh 2 Ehsan Fadaei-Kermani 3 Abstract In the present paper, the behavior of Kerman-Baghin aquifer has been investigated using the MODFLOW program and GMS 10.3 software. The piezometer data during October 2011 are applied for steady state condition of groundwater modeling. Then, the model is calibrated for 66 months for unsteady condition using observational information, and it is validated for 24 months. Finally, the results are compared with the available observed data and show acceptable accuracy in calibration and validation steps. After validating the model, the status of the aquifer is estimated for a period of 5 years. Management scenarios including 10, 20 and 30 percent reduction in groundwater abstraction as well as artificial recharge at eight selected aquifer sites have been investigated. The location of artificial recharge sites is selected based on seven parameters of land slope, distance from waterways, distance from faults, electrical conductivity, hydraulic conductivity, geology of the area and groundwater depth (thickness of unsaturated area). These parameters are combined with the index overlay method by Arc GIS 10.3 software. The results show that by continuing the current situation, the Kerman-Baghin aquifer could face an average annual deficit of more than 52 million cubic meters. It may cause various problems in the near future including abstraction water from groundwater sources and reducing water quality. The results of implementing different scenarios show that, the best scenario can be obtained by 10% reducing water withdrawal with artificial recharge in four zones 1, 2, 10 and 12. -
Of SE Iranian Mountains Exemplified by the Kuh-I-Jupar, Kuh-I-Lalezar and Kuh-I-Hezar Massifs in the Zagros
Umbruch 77.2-3 09.12.2008 15:43 Uhr Seite 71 Polarforschung 77 (2-3), 71 – 88, 2007 (erschienen 2008) The Pleistocene Glaciation (LGP and pre-LGP, pre-LGM) of SE Iranian Mountains Exemplified by the Kuh-i-Jupar, Kuh-i-Lalezar and Kuh-i-Hezar Massifs in the Zagros by Matthias Kuhle1 Abstract: Evidence has been provided of two mountain glaciations in the tion the Kuh-i-Lalezar massif (4374 m, 29°23'28.01" N 4135 m high, currently non-glaciated Kuh-i-Jupar massif in the semi-arid 56°44'49.38" E) has been visited in April and May 1973. The Zagros: an older period during the pre-LGP (Riss glaciation, c. 130 Ka) and a younger one during the LGP (Würm glaciation, Marine Isotope Stage (MIS) results attained by Quaternary geological and geomorpholo- 4-2: 60-18 Ka). During the pre-LGP glaciation the glaciers reached a gical methods stand in contrast to earlier assumptions concern- maximum of 17 km in length; during the LGP glaciation they were 10-12 km ing the former glaciation of these semi-arid Iranian mountains. long. They flowed down into the mountain foreland as far as 2160 m (LGP glaciation) and 1900 m (pre-LGP glaciation). The thickness of the valley Parts – Kuh-i-Jupar massif – were already published in glaciers reached 550 (pre-LGP glaciation) and 350 m (LGP glaciation). German. They are included in this paper in a summarized During the pre-LGP a 23 km-wide continuous piedmont glacier lobe devel- form. In continuation of these results new observations from oped parallel to the mountain foot. -
Kerman Province)
Quaderni del Museo Civico di Storia Naturale di Ferrara - Vol. 7 - 2019 - pp. 27-35 ISSN 2283-6918 Contribution to the knowledge of Iranian flora: a herborization in the Dasht-e-Lut area (Kerman Province) LORENZO CECCHI Università degli Studi di Firenze, Sistema Museale di Ateneo, Museo di Storia Naturale, Collezioni di Botanica - Via Giorgio La Pira 4 - Florence (Italy); E-mail: [email protected] Abstract A joined research project named “Meteorites and plants from Lut desert” was performed in 2017 by the Botanical and Mineralogical sections of Natural History Museum of Florence with other Italian and Iranian partners. It enabled the collection of 146 plant specimens in SE Iran. It’s a small but rather rare and significant contribution to the knowledge of a very remote and poorly known region of central Asia, including both important endemics and characteristic species of steppic and desertic environments. Keywords: Iranian flora, Dasht-e-Lut area, Kerman Province. Riassunto Contributo alla conoscenza floristica dell’Iran: un’erborizzazione nell’area del deserto di Lut (Provincia di Kerman) Il progetto di ricerca congiunto “Meteorites and plants from Lut desert”, condotto dalle sezioni di Botanica e Mineralogia del Museo di Storia Naturale di Firenze in collaborazione con rappresentanti di altre istituzioni sia italiane che iraniane, ha permesso la raccolta di 146 campioni vegetali nell’Iran sud-orientale. Si tratta di un modesto ma raro e significativo contributo alla conoscenza di una regione particolarmente remota e poco conosciuta dell’Asia centrale, che comprende importanti endemismi e specie caratteristiche di ambienti steppici e desertico. Parole chiave: Flora iraniana, Area di Dasht-e-Lut, provincia di Kerman. -
Kerman Province
In TheGod Name of Kerman Ganjali khan water reservoir / Contents: Subject page Kerman Province/11 Mount Hezar / 11 Mount joopar/11 Kerman city / 11 Ganjalikhan square / 11 Ganjalikhan bazaar/11 Ganjalikhan public bath /12 Ganjalikhan Mint house/12 Ganjalikhan School/12 Ganjalikhan Mosque /13 Ganjalikhan Cross market place /13 Alimardan Khan water reservoir /13 Ibrahimkhan complex/ 13 Ibrahimkhan Bazaar/14 Ibrahimkhan School /14 Ibrahimkhan bath/14 Vakil Complex/14 Vakil public bath / 14 Vakil Bazaar / 16 Vakil Caravansary / 16 Hajagha Ali complex / 16 Hajagha Ali mosque / 17 Hajagha Ali bazaar / 17 Hajagha Ali reservoir / 17 Bazaar Complex / 17 Arg- Square bazaar / 18 Kerman Throughout bazaar / 18 North Copper Smithing bazaar / 18 Arg bazaar / 18 West coppersmithing bazaar / 18 Ekhteyari bazaar / 18 Mozaffari bazaar / 19 Indian Caravansary / 19 Golshan house / 19 Mozaffari grand mosque / 19 Imam mosque / 20 Moshtaghieh / 20 Green Dome / 20 Jebalieh Dome / 21 Shah Namatollah threshold / 21 Khaje Etabak tomb / 23 Imam zadeh shahzadeh Hossien tomb / 23 Imam zadeh shahzadeh Mohammad / 23 Qaleh Dokhtar / 23 Kerman fire temple / 24 Moaidi Ice house / 24 Kerman national library / 25 Gholibig throne palace / 25 Fathabad Garden / 25 Shotor Galoo / 25 Shah zadeh garden / 26 Harandi garden / 26 Arg-e Rayen / 26 Ganjalikhan anthropology museum / 27 Coin museum / 27 Harandi museum garden / 27 Sanatti museum / 28 Zoroasterian museum / 28 Shahid Bahonar museum / 28 Holy defense museum / 28 Jebalieh museum / 29 Shah Namatollah dome museum / 29 Ghaem wooden -
Mayors for Peace Member Cities 2021/10/01 平和首長会議 加盟都市リスト
Mayors for Peace Member Cities 2021/10/01 平和首長会議 加盟都市リスト ● Asia 4 Bangladesh 7 China アジア バングラデシュ 中国 1 Afghanistan 9 Khulna 6 Hangzhou アフガニスタン クルナ 杭州(ハンチォウ) 1 Herat 10 Kotwalipara 7 Wuhan ヘラート コタリパラ 武漢(ウハン) 2 Kabul 11 Meherpur 8 Cyprus カブール メヘルプール キプロス 3 Nili 12 Moulvibazar 1 Aglantzia ニリ モウロビバザール アグランツィア 2 Armenia 13 Narayanganj 2 Ammochostos (Famagusta) アルメニア ナラヤンガンジ アモコストス(ファマグスタ) 1 Yerevan 14 Narsingdi 3 Kyrenia エレバン ナールシンジ キレニア 3 Azerbaijan 15 Noapara 4 Kythrea アゼルバイジャン ノアパラ キシレア 1 Agdam 16 Patuakhali 5 Morphou アグダム(県) パトゥアカリ モルフー 2 Fuzuli 17 Rajshahi 9 Georgia フュズリ(県) ラージシャヒ ジョージア 3 Gubadli 18 Rangpur 1 Kutaisi クバドリ(県) ラングプール クタイシ 4 Jabrail Region 19 Swarupkati 2 Tbilisi ジャブライル(県) サルプカティ トビリシ 5 Kalbajar 20 Sylhet 10 India カルバジャル(県) シルヘット インド 6 Khocali 21 Tangail 1 Ahmedabad ホジャリ(県) タンガイル アーメダバード 7 Khojavend 22 Tongi 2 Bhopal ホジャヴェンド(県) トンギ ボパール 8 Lachin 5 Bhutan 3 Chandernagore ラチン(県) ブータン チャンダルナゴール 9 Shusha Region 1 Thimphu 4 Chandigarh シュシャ(県) ティンプー チャンディーガル 10 Zangilan Region 6 Cambodia 5 Chennai ザンギラン(県) カンボジア チェンナイ 4 Bangladesh 1 Ba Phnom 6 Cochin バングラデシュ バプノム コーチ(コーチン) 1 Bera 2 Phnom Penh 7 Delhi ベラ プノンペン デリー 2 Chapai Nawabganj 3 Siem Reap Province 8 Imphal チャパイ・ナワブガンジ シェムリアップ州 インパール 3 Chittagong 7 China 9 Kolkata チッタゴン 中国 コルカタ 4 Comilla 1 Beijing 10 Lucknow コミラ 北京(ペイチン) ラクノウ 5 Cox's Bazar 2 Chengdu 11 Mallappuzhassery コックスバザール 成都(チォントゥ) マラパザーサリー 6 Dhaka 3 Chongqing 12 Meerut ダッカ 重慶(チョンチン) メーラト 7 Gazipur 4 Dalian 13 Mumbai (Bombay) ガジプール 大連(タァリィェン) ムンバイ(旧ボンベイ) 8 Gopalpur 5 Fuzhou 14 Nagpur ゴパルプール 福州(フゥチォウ) ナーグプル 1/108 Pages -
Page 1 of 27 PODOCES, 2007, 2(2): 77-96 a Century of Breeding Bird Assessment by Western Travellers in Iran, 1876–1977 - Appendix 1 C.S
PODOCES, 2007, 2(2): 77-96 A century of breeding bird assessment by western travellers in Iran, 1876–1977 - Appendix 1 C.S. ROSELAAR and M. ALIABADIAN Referenced bird localities in Iran x°.y'N x°.y'E °N °E Literature reference province number Ab Ali 35.46 51.58 35,767 51,967 12 Tehran Abadan 30.20 48.15 30,333 48,250 33, 69 Khuzestan Abadeh 31.06 52.40 31,100 52,667 01 Fars Abasabad 36.44 51.06 36,733 51,100 18, 63 Mazandaran Abasabad (nr Emamrud) 36.33 55.07 36,550 55,117 20, 23-26, 71-78 Semnan Abaz - see Avaz Khorasan Abbasad - see Abasabad Semnan Abdolabad ('Abdul-abad') 35.04 58.47 35,067 58,783 86, 88, 96-99 Khorasan Abdullabad [NE of Sabzevar] * * * * 20, 23-26, 71-78 Khorasan Abeli - see Ab Ali Tehran Abiz 33.41 59.57 33,683 59,950 87, 89, 90, 91, 94, 96-99 Khorasan Abr ('Abar') 36.43 55.05 36,717 55,083 37, 40, 84 Semnan Abr pass 36.47 55.00 36,783 55,000 37, 40, 84 Semnan/Golestan Absellabad - see Afzalabad Sistan & Baluchestan Absh-Kushta [at c.: ] 29.35 60.50 29,583 60,833 87, 89, 91, 96-99 Sistan & Baluchestan Abu Turab 33.51 59.36 33,850 59,600 86, 88, 96-99 Khorasan Abulhassan [at c.:] 32.10 49.10 32,167 49,167 20, 23-26, 71-78 Khuzestan Adimi 31.07 61.24 31,117 61,400 90, 94, 96-99 Sistan & Baluchestan Afzalabad 30.56 61.19 30,933 61,317 86, 87, 88, 89, 90, 91, Sistan & Baluchestan 94, 96-99 Aga-baba 36.19 49.36 36,317 49,600 92, 96-99 Qazvin Agulyashker/Aguljashkar/Aghol Jaskar 31.38 49.40 31,633 49,667 92, 96-99 Khuzestan [at c.: ] Ahandar [at c.: ] 32.59 59.18 32,983 59,300 86, 88, 96-99 Khorasan Ahangar Mahalleh - see Now Mal Golestan Ahangaran 33.25 60.12 33,417 60,200 87, 89, 91, 96-99 Khorasan Ahmadabad 35.22 51.13 35,367 51,217 12, 41 Tehran Ahvaz (‘Ahwaz’) 31.20 48.41 31,333 48,683 20, 22, 23-26, 33, 49, 67, Khuzestan 69, 71-78, 80, 92, 96-99 Airabad - see Kheyrabad (nr Turkmen. -
Some 4000 Metre Peaks of Southern Iran Guy Sheridan
ALBIGNA VALL£Y-1978 tens or years as a stance, to take the rest or the pany up. The rrequent rains during the past weeks must have loosened the foundation round the slab and it suddenly crashed down, burying all 3 climbers. On hearing the details I had to think ofan incident many yeal-s ago when I saw a horizontal slab, much smaller than the one which had caused rhis accidenr, and ITied to pur my hand on it to use it as a tance. I lill remember my terror when I relt it moving downwat-ds. I tried 10 ease il back into Ihe old po ilion and succeeded bur I know now, hearing the tragic story, how lucky I had been at the time. 92 The 4000m peaks of southern Iran (This and next 8 photos and maps: G. Sheridanl 186 Some 4000 metre peaks of southern Iran Guy Sheridan In January and February 1975 I spent many hours browsing through past Alpine Joumals and other books in the Alpine Club library in an attempt to gather information about the mountains of Southern Iran. I ,vas largely unsuccessful and when my wife and I left UK in April the same year we were hardly more knowledgeable about the topography ofSouthern Iran than when we first looked at the Times Atlas. Nonetheless the 2t years that I had on loan service to the Imperial Iranian Marines provided me with plenty ofopportunities to gain knowledge at hrst hand. I hope that this short article will enable others who find themselves in Iran and want to visit the higher peaks of that vast country to do so without being con fronted with similar frustrations.