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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. -
Rare Birds in Iran in the Late 1960S and 1970S
Podoces, 2008, 3(1/2): 1–30 Rare Birds in Iran in the Late 1960s and 1970s DEREK A. SCOTT Castletownbere Post Office, Castletownbere, Co. Cork, Ireland. Email: [email protected] Received 26 July 2008; accepted 14 September 2008 Abstract: The 12-year period from 1967 to 1978 was a period of intense ornithological activity in Iran. The Ornithology Unit in the Department of the Environment carried out numerous surveys throughout the country; several important international ornithological expeditions visited Iran and subsequently published their findings, and a number of resident and visiting bird-watchers kept detailed records of their observations and submitted these to the Ornithology Unit. These activities added greatly to our knowledge of the status and distribution of birds in Iran, and produced many records of birds which had rarely if ever been recorded in Iran before. This paper gives details of all records known to the author of 92 species that were recorded as rarities in Iran during the 12-year period under review. These include 18 species that had not previously been recorded in Iran, a further 67 species that were recorded on fewer than 13 occasions, and seven slightly commoner species for which there were very few records prior to 1967. All records of four distinctive subspecies are also included. The 29 species that were known from Iran prior to 1967 but not recorded during the period under review are listed in an Appendix. Keywords: Rare birds, rarities, 1970s, status, distribution, Iran. INTRODUCTION Eftekhar, E. Kahrom and J. Mansoori, several of whom quickly became keen ornithologists. -
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. -
A Preliminaryfloristic Checklist of Thal Desert Punjab, Pakistan
Pak. J. Bot., 46(1): 13-18, 2014. A PRELIMINARYFLORISTIC CHECKLIST OF THAL DESERT PUNJAB, PAKISTAN HUMAIRA SHAHEEN1, RAHMATULLAH QURESHI1*, ABIDA AKRAM, M. GULFRAZ AND DANIEL POTTER2 1Department of Botany, Pir Mehr Ali Shah Arid Agriculture University, Rawalpindi, Pakistan 2Department of Plant Sciences, University of California Davis, USA. *Corresponding author e-mail: [email protected] Abstract The floristic survey of the Thal desert, Punjab, Pakistan was carried out during 2010 to 2013. So far, 248 species distributed across 166 genera and 38 families were identified during the report period. Besides, one species viz., Themeda triandra was recorded for the first time from Pakistan. Of them, one fern, 4 monocots and 33 dicots families were determined. The most dominating family was Poaceae that contributed 52 species (21.49%), followed by Fabaceae (34 spp., 13.05%) and Amaranthaceae & Asteraceae (17 spp., 7.02% each). The largest genera were Euphorbia (6 spp.), Cyperus, Eragrostis and Solanum (5 spp. each), Mollugo, Heliotropium and Cenchrus (4 spp. each), Acacia, Prosopis, Tephrosia, Corchorus, Boerhavia and Ziziphus (3 spp. each). This checklist consists of updated systematic families and plants names that will provide a useful starting point for further ecological and bioprospective research of the area under study. Introduction about the vegetation of the study area which helps further ecological investigations and conservation measures. The Thal desert is situated between 31° 10’ N and 71° 30’ E in the Punjab, province, Pakistan (Fig. 1). The area is subtropical sandy desert spread over 190 miles with its maximum breadth of 70 miles. The tract is bound by the piedmont of the Salt Range in the north, the Indus River flood plains in the west and Jhelum and Chenab River flood plains in the east. -
Bonner Zoologische Beiträge
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Bonn zoological Bulletin - früher Bonner Zoologische Beiträge. Jahr/Year: 1978 Band/Volume: 29 Autor(en)/Author(s): Desfayes M., Praz J. C. Artikel/Article: Notes on Habitat and Distribution of Montane Birds in Southern Iran 18-37 © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zoologicalbulletin.de; www.biologiezentrum.at Bonn. 18 zool. Beitr. Notes on Habitat and Distribution of Montane Birds in Southern Iran by M. DESFAYES, Washington, and J. C. PRAZ, Sempach This study was carried out in May and June 1975 to fill a gap in our knowledge of the breeding birds, their distribution and ecology, in the mountains of southern Iran. In these two months, most species occupy their breeding territories. Records from April or July are not always reliable as an indication of breeding, even if the bird is observed singing. While the avifauna of the northern parts of the country is relatively well-known, that of the southern highlands (above 2,000 meters) is poorly known. Blanford (1876) collected at Rayen (Rayun) 2100 m, and Hanaka, 2400 m, south-east of Kerman, just east of the Kuh-e Hazar, from 30 April to 2 May, and also at Khan-e Sorkh Pass 2550 m, 115 km south-west of Kerman on 23 May. Species collected in these areas by Blanford are: Columba palum- bus, Cuculus canorus, Melanocorypha bimaculata, Motacilla alba, Lanius collurio, Oenanthe picata, Oe. lugens, Oe. xanthoprymna, Montícola saxa- tilis, Sylvia curruca, Serinus pusillus, Acanthis cannabina, Emberiza bucha- nani, and E. -
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. -
Turanian Vegetation
Plant Formations in the Turanian BioProvince Peter Martin Rhind Turanian Gypsophilic (gypsum-loving) Sagebrush Gypsum, which is composed of calcium sulphate, occurs in abundance in the weathered products of local mountains. Altogether it is estimated that there are some 400 gypsophilic species in the area and including many of the endemic genera. Most are dwarf shrubs of various species of sagebursh such as the endemic Artemisia terrae-albae and A. turanica (Asteraceae), and usually bloom and fruit in autumn after summer dormancy. The former is the dominant over much of central Kazakhstan. There are also many thorny or spiny species like Acanthophyllum pungens, Atraphaxis spinosa, Noaea spinosissima and Sisymbrium subspinescens, and an unusual large number of tall Apiaceae often growing to heights of over 2 m. Most are perennial species and include Ferula assa-foetida, F. ferulaeoides, Hyalolena turcomanica, Munetia oeroilanica and endemic or near endemic Oedibasis apiculata (Apiaceae). Other significant species include Caragana grandiflora, Convolvulus frutescens, Ephedra distachya and Sophora griffithii. Another type of gypsophilic sagebrush is characterized by Artemisia kemrudica (kemrud). This occupies large parts of northwest Turkmenistan on the Beltau, Krasnovodsk and Ustyurt plateaus and also occurs in the delta of the Amudarya River. It is fairly uniform with an upper layer reaching heights of 100 cm. These larger shrubs include various Calligonum species, such as the endemic Calligonum alatum (Polygonaceae) and Haloxylon aphyllum (Chenopodiaceae). However, most of the species occur in the second tier with heights of between 20-40 cm. Here the dominant shrubs is Artemisia kemrudica, while other common species include Salsola arbuscula, S. -
Report Kyrgyzstan 2017-4
ISU-Botanical trip to Kyrgyzstan. 17th of June - 28th of June 2017 picture 1 picture 2 picture 3 picture 4 Kyrgyzstan, Switzerland of the Orient, is located on the West Side of China, South of Kazakhstan, North of Tajikistan and East of Uzbekistan. It has the surface of one third of Germany but is home to only 6 million inhabitants. In the past, it often was occupied by different nations like Mongolia, Russia and China. Never ISU-enthousiasts went so far for stilling their botanical hunger. Brian Kabbes met his wife Meerim Kozhoshova here in her beautiful homeland. Both guided this trip already for the fifteenth time. Meerim is the organiser, speaks Dutch, English and Kirgiz. Brian is the speaking dictionnary of the Kirgiz flora. Most of Kyrgyz people are Muslim, what we even in the middle of the night could hear when the imam asked for the pray.... One third of the population lives in the capital Bishkek. This busy metropolis has a much higher standard than the countryside where we found the standard of living like two or even three generations ago in Europe. Here in Bishkek, we underwent the typical Asiatic busy atmosphere flavored with a sauce of past sovietunion relicts. The neighbour China is entering slowly in the life and structure of this poor country by building perfect highways that are as good or of even better quality then our European ones. The Kyrgyz people are very friendly and have a high amount of humor that shows their intelligence. They served us healthy, well spiced, not too hot food with little meat (sheep - no lamb) and plentiful use of vegetables. -
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
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