DOCSLIB.ORG

1 Formularul Pentru Prezentarea Soluţiilor De Rezolvare A

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
1 Formularul Pentru Prezentarea Soluţiilor De Rezolvare A Formularul pentru prezentarea soluţiilor de rezolvare a problemelor semnalate de publicul interesat Tismana II Asociaţia Bankwatch România 1.Nu au fost evaluate efectele cumulative ale tuturor carierelor şi instalaţiilor industriale din zonă Perimetrul minier Tismana II face parte din Bazinul Minier Oltenia impreuna cu perimetrele, Tismana I, Rosia, Pinoasa, Pesteana Nord, Pesteana Sud, Jilt Nord, Jilt Sud, Rosiuta si Lupoaia, perimetre pentru care s-a acordat licenta de exploatare: NR. LICENTEI DE *ANUL NR. DENUMIRE SUPRAFATA CONCESIUNE PENTRU INCETARII CTR. PERIMETRUL MINIER (KMP) EXPOATARE ACTIVITATII 1 Tismana I 2717/2001 9.716 2025 2 Tismana II 2718/2001 7.405 2025 3 Pinoasa 3499/2002 15.814 2020 4 Rosia 3496/2002 17.388 2019 5 Pesteana Nord 1457/2000 11.726 2021 6 Pesteana Nord 1458/2000 6.283 2026 7 Jilt Sud 2603/2001 9.716 2028 8 Jilt Nord 2602/2001 7.405 2027 9 Lupoaia 3498/2002 15.814 2027 10 Rosiuta 3497/2002 17.388 2027 Din punct de vedere geomorfologic perimetrul celor zece perimetre miniere sunt grupate in trei Bazine miniere: - Bazinul Rovinari, format din carierele Tismana I, Rosia, Tismana II, Pinoasa, Pesteana Nord si Pesteana Sud, este cuprins intre limita conventionala de la cca. 4 km sud de valea Tismanei. Bazinul este divizat in patru zone distincte ca forme de relief: zona de lunca a paraului Jiu, zona de lunca a paraului Tismana, zona colinara de est si zona colinara de vest. Partea centrala este reprezentata de sesul aluvial al Jiului, cu altitudini ce variaza intr +168m si +135m spre sud. Amplasarea Bazinului Rovinari este prevazuta in extravilanul/intravilanul comunelor Calnic, Negomir, Farcasesti, Balteni, Urdari si Plopsoru. - Bazinul Minier Jilt, format din carierele Jilt Nord si Jilt Sud, este încadrata in sectorul dintre valea Motrului si valea Jiltului, mai precis intre dealurile Piscul Tilvei, Culmea Runcurel, Dealul Grigorescu si paraul Jilt. Amplasarea Bazinului Minier Jilt este prevazuta in extravilanul/intravilanul comunelor Matasari, Negomir, Farcasesti, Dragotesti si Slivilesti. - Bazinul mimier Motru, format din carierele Rosiuta si Lupoaia, ce se „suprapune” peste Piemontul Motrului, astfel încât, Valea Motrului este orientată central în cadrul Bazinului minier. Amplasarea Bazinului Motru este prevazuta in extravilanul/intravilanul comunelor Matasari, Slivilesti, Ciuperceni, Catunele si orasul Motru. Suprafete necesare a se ocupa in perioada analizata pe natura de teren, perimetru minier si suprafetele ecologizate sunt redate in tabelele urmatoare. 1 SUPRAFETE NECESARE A SE OCUPA PE NATURA DE TEREN- PERIMETRELE MINIERE COMPLEXUL ENERGETIC OLTENIA NECESAR DE TERENURI A SE OCUPA PE PERIOADA LICENTEI DE EXPLOATARE PERIMETRELE MINIERE COMPLEXUL ENERGETIC OLTENIA IN PERIMETRUL MINIER IN EXTINDEREA PERIMETRULUI MINIER TOTAL SUPRAFATA OCUPATA Suprafata necesara desfasurare flux de TOTAL Suprafata necesara desfasurare flux de LA INCETARE ACTIV- excavare si haldare/ Natura de teren NECESAR excavare si haldare/ Natura de teren Suprafata ITATE SUPRAFATA Perioada Perimetrul UM ocupata de % Suprafata TOTAL PERIMETRU analizata minier TOTAL % flux de raportat neocupata NECESAR LUI MINIER raportat la exploatare A Ps Fn Lv Vie Cc Np Pd Ha la total A Ps Vie Np Pd Ha total UMC - UMC - uri* uri* 2015-2021 Pesteana Nord 710,00 136,32 1,02 0,00 0,00 0,00 0,00 24,76 0,00 162,10 4,06 304,10 1.176,20 0,00 0,00 0,00 0,00 0,00 0,00 1.176,20 8,35 1.176,20 2015-2026 Pesteana Sud 378,35 57,16 43,66 0,00 0,00 0,00 0,00 2,55 0,00 103,37 2,59 146,59 628,31 0,00 0,00 0,00 0,00 0,00 0,00 628,31 4,46 628,31 2015-2019 Rosia 1.457,91 0,35 44,10 0,00 0,75 0,00 0,00 0,00 235,69 280,89 7,03 0,00 1.738,80 0,00 0,00 0,00 0,00 0,00 0,00 1.738,80 12,34 1.738,80 2013-2020 Pinoasa 930,56 51,04 198,61 0,00 6,86 10,32 4,85 11,65 217,63 500,96 12,54 149,88 1.581,40 0,00 0,00 0,00 0,00 0,00 0,00 1.581,40 11,22 1.581,40 2013-2025 Tismana I 839,33 3,06 23,50 0,03 1,75 1,19 0,97 0,00 101,86 132,37 3,31 0,00 971,70 0,00 0,00 0,00 0,00 0,00 0,00 971,70 6,89 971,70 Ha 2013-2025 Tismana II 593,29 3,84 20,14 0,00 0,46 0,57 1,93 0,87 119,42 147,21 3,68 0,00 740,50 0,00 0,00 0,00 0,00 0,00 0,00 740,50 5,25 740,50 2015-2027 Jilt Nord 579,20 91,00 106,40 4,40 6,80 1,90 4,50 0,00 113,00 328,00 8,21 0,00 907,20 0,00 0,00 0,00 0,00 0,00 0,00 907,20 6,44 907,20 2015-2028 Jilt Sud 1.348,41 104,18 226,07 47,14 20,00 15,98 6,50 10,50 94,20 524,57 13,13 50,14 1.923,12 0,00 0,00 0,00 0,00 0,00 0,00 1.923,12 13,65 1.923,12 2015-2027 Rosiuta 1.078,80 115,63 220,94 71,48 22,12 8,23 97,28 70,20 181,82 787,70 19,72 0,00 1.866,50 18,47 68,75 1,02 33,77 70,30 192,31 2.058,81 14,61 1.866,50 2015-2027 Lupoaia 1.248,51 58,97 298,17 28,00 0,00 0,00 5,95 71,84 565,07 1.028,00 25,73 91,39 2.367,90 0,00 0,00 0,00 0,00 0,00 0,00 2.367,90 16,80 2.367,90 TOTAL 9.164,36 621,55 1.182,61 151,05 58,74 38,19 121,98 192,37 1.628,69 3.995,17 100,00 742,10 13.901,63 18,47 68,75 1,02 33,77 70,30 192,31 14.093,94 100,00 13.901,63 SUPRAFETE NECESARE A SE OCUPA PE NATURA DE TEREN- PERIMETRELE MINIERE COMPLEXUL ENERGETIC OLTENIA Raportat la repartitia terenurilor pe folosinte in judetul Gorj Suprafata necesara desfasurare flux de excavare si haldare/ Natura de teren Perimetrul minier UM TOTAL A Ps Fn Lv Vie Cc Np Pd Pesteana Nord 136,32 1,02 0,00 0,00 0,00 0,00 24,76 0,00 162,10 Pesteana Sud 57,16 43,66 0,00 0,00 0,00 0,00 2,55 0,00 103,37 Rosia 0,35 44,10 0,00 0,75 0,00 0,00 0,00 235,69 280,89 Pinoasa 51,04 198,61 0,00 6,86 10,32 4,85 11,65 217,63 500,96 Tismana I 3,06 23,50 0,03 1,75 1,19 0,97 0,00 101,86 132,37 Tismana II 3,84 20,14 0,00 0,46 0,57 1,93 0,87 119,42 147,21 Ha Jilt Nord 91,00 106,40 4,40 6,80 1,90 4,50 0,00 113,00 328,00 Jilt Sud 104,18 226,07 47,14 20,00 15,98 6,50 10,50 94,20 524,57 Rosiuta 134,10 289,69 71,48 22,12 9,25 97,28 103,97 252,12 980,01 Lupoaia 58,97 298,17 28,00 0,00 0,00 5,95 71,84 565,07 1.028,00 TOTAL NECESAR 640,02 1.251,36 151,05 58,74 39,21 121,98 226,14 1.698,99 4.187,48 Repartitia terenurilor pe folosinte in judetul Gorj* 99.149,00 88.654,00 42.542,00 8.961,00 4.434,00 12.027,00 9.833,00 278.717,00 544.317,00 TOTAL NECESAR raportat la suprafata judetului Gorj % 0,65 1,41 0,36 0,66 0,88 1,01 2,30 0,61 0,77 * Conform ACTUALIZARE PLAN DE AMENAJAREA TERITORIULUI – JUDETUL GORJ AMPLASAMENTUL SILVIC AL TERENURILOR SOLICITATE PENTRU SCOATERE DIN FONDUL FORESTIER O.S. Pesteana O.S. Motru U.M. U.P. Valea cu O.S. Targu Jiu U.P. III U.P. IV Sliv- U.P. II Mo- U.P. I Perimetrul Minier Apa U.P. I Stramba Dragotesti ilesti tru Iormanesti TOTAL Tismana I 101,86 101,86 Tismana II 119,42 119,42 Pinoasa 186,33 31,3 217,63 Rosia 201,29 34,40 235,69 Jilt Nord 113 113,00 Ha Jilt Sud 76,3 17,9 94,20 Rosiuta 110,03 12,74 129,35 252,12 Lupoaia 214 351,07 565,07 TOTAL suprafata solicitata pentru scoatere din fondul forestier 201,29 442,01 330,63 30,64 343,35 351,07 1698,99 TOTAL suprafata U.P. 1509,00 2906,80 1801,64 1012,88 889,21 2309,30 10428,83 TOTAL NECESAR raportat la suprafata U.P. 13,34 15,21 18,35 3,03 38,61 15,20 16,29 % TOTAL NECESAR raportat la suprafata judetului Gorj 0,07 0,16 0,12 0,01 0,12 0,13 0,61 2 EVIDENTA TERENURILOR NECESAR A SE OCUPA PE ANI SI NATURA DE TEREN CORELATA CU SUPRAFETELE ECOLOGIZATE SI PROPUSE SPRE ECOLOGIZARE SUPRAFETE Suprafata necesara desfasurare flux de SUPRAFETE PROPUSE Perimetrul Perioada TOTAL UM excavare si haldare/ Natura de teren ECOLOGIZATE SPRE minier analizata GENERAL ECOLOGIZARE A Ps Fn Lv Vie Cc Np Pd Silvic Agricol Silvic Agricol 2015 25,4 1,02 0 0 0 0 0,89 0 27,31 0,00 0,00 2016 25,14 0 0 0 0 0 0,78 0 25,92 0,00 0,00 Pesteana Nord 2016-2021 85,78 0 0 0 0 0 23,09 0 108,87 31,23 0,00 144,77 272,11 Total 2015-2021 136,32 1,02 0,00 0,00 0,00 0,00 24,76 0,00 162,10 144,77 272,11 POST-INCHIDERE 83,92 105,13 2015 13,58 12,08 0 0 0 0 0,25 0 25,91 66,36 40,35 2016 9,41 12,16 0 0 0 0 0,45 0 22,02 0,00 0,00 2016-2021 31,29 16,52 0 0 0 0 0,91 0 48,72 102,23 110,00 Pesteana Sud 116,06 118,35 2021-2026 2,88 2,9 0 0 0 0 0,94 0 6,72 27,06 18,00 Total 2015-2026 57,16 43,66 0,00 0,00 0,00 0,00 2,55 0,00 103,37 195,65 168,35 POST-INCHIDERE 32,45 0,00 2013-2015 0,35 4,98 0 0,27 0 0 0 56,07 61,67 0,00 0,00 2016 0 9,78 0 0,12 0 0 0 44,9 54,80 45,68 91,92 2017 0 9,78 0 0,12 0 0 0 44,9 54,80 24,07 37,98 Rosia 2018 0 9,78 0 0,12 0 0 0 44,91 54,81 202,88 506,41 0,00 0,00 2019 0 9,78 0 0,12 0 0 0 44,91 54,81 0,00 0,00 Total 2015-2019 0,35 44,10 0,00 0,75 0,00 0,00 0,00 235,69 280,89 69,75 129,90 POST-INCHIDERE 597,56 171,30 2013-2015 0,00 6,09 0,00 0,00 0,37 0,00 0,00 13,02 19,48 0,00 0,00 2016 20,03 56,19 0,00 2,66 3,71 0,89 2,99 64,65 151,12 17,80 0,00 2017 9,83 31,24 0,00 2,47 1,13 1,06 1,08 43,52 90,33 19,35 0,00 2018 5,56 39,04 0,00 0,64 2,06 0,35 1,05 37,68 86,38 10,90 0,00 Pinoasa 20,50 21,24 2019 6,63 29,41 0,00 0,54 2,14 0,36 1,47 34,64 75,19 24,32 0,00 2020-2028 8,99 36,64 0,00 0,55 0,91 2,19 5,06 24,12 78,46 554,27 993,75 Total 2015-2028 51,04 198,61 0,00 6,86 10,32 4,85 11,65 217,63 500,96 626,64 993,75 POST-INCHIDERE 254,60 108,00 2013-2015 0,54 8,88 0,03 1,59 0,63 0,11 0 36,33 48,11 0,00 0,00 2016 1,2 9,6 0 0,16 0,49 0,87 0 38,27 50,59 34,85 0,00 2017 1,32 4,73 0 0 0 0 0 15,73 21,78 18,50 0,00 Tismana I 96,88 66,67 2018-2025 0 0,29 0 0 0,07 0 0 11,53 11,89 195,00 0,00 Total 2015-2025 3,06 23,50 0,03 1,75 1,19 0,97 0,00 101,86 132,37 248,35 0,00 POST-INCHIDERE 144,50 33,50 Ha 2013-2015 1,19 14,81 0 0,46 0,57 0,68 0,87 58,67 77,25 0,00 0,00 2016 2,65 5,33 0 0 0 0,42 0 39,56 47,96 0,00 0,00 2017 0 0 0 0 0 0,42 0 14,91 15,33 12,10 0,00 Tismana II 6,80 110,57 2018-2025 0 0 0 0 0 0,41 0 6,28 6,69 238,00 0,00 Total 2015-2025 3,84
Load more

Recommended publications
  • Volcaniclastic Turbidites of the Coşuştea Nappe: a Record of Late Cretaceous Arc Volcanism in the South Carpathians (Romania)
    GEOLOGICA BALCANICA, 43.1 – 3, Sofia, Dec. 2014, 77-98. Volcaniclastic turbidites of the Coşuştea Nappe: a record of Late Cretaceous arc volcanism in the South Carpathians (Romania) Antoneta Seghedi, Gheorghe Oaie National Institute of Marine Geology and Geoecology, 23-25 Dimitrie Onciul St., sector 2, Bucharest, Romania; e-mails: [email protected]; [email protected] (Accepted in revised form: November 2014) Abstract. Sedimentological and mineralogical composition of Upper Cretaceous terrigenous and volcaniclastic sandstones are presented for the Coşuştea Nappe of the South Carpathians, Romania, in order to constrain the provenance and tectonic setting of deposition. Existing geochemical data on volcaniclastic rocks were interpreted using discrimination diagrams in order to get additional information. The Coşuştea Nappe includes terrigenous turbidites, overlain by upward coarsening sequences of volcaniclastic turbidites, both associated with a strongly dismembered mélange complex. Facies association and vertical facies distribution suggest that terrigenous successions are midfan turbidites, dominated by deposition in suprafan channels. Their sandstone mineralogy indicates that a major sediment source, located on the upper plate, provided detritus of Getic type metamorphic basement and withinplate volcanic rocks, with minor input from the accretionary wedge. Volcaniclastic sedimentation took place as dominantly sandstone deposition in supracone lobes, followed by coarse sedimentation as channelized debris flows. Vertical facies distribution suggests evolution in time from midfan to proximal fan turbidites. Mineralogical composition of volcaniclastic sandstones indicates provenance from a major volcanic source, with minor contributions from the accretionary wedge and from an upper continental plate supplying terrigenous siliciclastic detritus, and suggests that volcaniclastic turbidites accumulated in a trench or a slope forearc basin.
    [Show full text]
  • The Rosaceae Family from the Lower Basin of the Motru River
    Muzeul Olteniei Craiova. Oltenia. Studii i comunicri. tiinele Naturii, Tom XXIII/2007 ISSN 1454-6914 THE ROSACEAE FAMILY FROM THE LOWER BASIN OF THE MOTRU RIVER IULIAN COSTACHE, MARINELA ELENA COSTACHE Abstract. The paper presents the species from Rosaceae Family, which were identified in the Lower Basin of the Motru River. Their identification was performed short before the defence of the Ph.D. thesis. Key words: Basin, flora, Motru, Rosaceae Rezumat Rosaceele din Bazinului inferior al Motrului. Lucrarea prezint speciile din familia Rosaceae identificate în Bazinul inferior al râului Motru. Identificarea a fost realizat înainte de susinerea tezei de doctorat. Cuvinte cheie: Bazin, flora, Motru, Rosaceae INTRODUCTION From the geographical point of view, the Lower Basin of the Motru River lies in the western part of the Getic Piedmont, with the coordinates: 440 55' north latitude and 230 45' east longitudes. The studied area is 691 Km2. From the administrative-territorial point of view, the territory under research is located at the borderline between the counties of Gorj and Mehedini – the borderline starts in the eastern part of the Negoieti Hills (Comneti-Mehedini, altitude 388 m) and reaches Valea Jiului near Gura Motrului (altitude 110 m). Being situated in the south-western part of the country and of the Getic Piedmont, the studied area has a Central-European climate with sub-Mediterranean influences. In the territory under research, there have been made floristic and phytosociological studies between 1997 and 2005, within the PhD thesis (COSTACHE I., 2005). Besides the scientific side of the research, it had been wanted the applicant approach too, instructive- ecological.
    [Show full text]
  • Lucrări Ştiin Ifice, Seria I, Vol. Xii (3) Romanian Culas Culele Din România
    LUCRĂRI ŞTIINŢIFICE, SERIA I, VOL. XII (3) ROMANIAN CULAS CULELE DIN ROMÂNIA V. LALA1, I. PETROMAN1, CORNELIA PETROMAN1, I. TRIŞCĂU1, O. AMZULESCU1, S. PALADE1, MONICA DOBOŞ1 1Banat’s University of Agricultural Sciences and Veterinary Medicine Timişoara, Faculty of Agricultural Management, Timişoara, Romania ; [email protected] Abstract: Romanian culas are the proof of the artistic sense and craftsmen’s skills who have taken over elements from the architecture of the fortified boyars’ houses. The buildings that can be admired in certain areas in the country are a synthesis of the features of the peasants’ houses. Keywords: cula, Romania, peasant architecture INTRODUCTION As a general rule, culas (from the Turkish kula ‘tower’) are tall buildings, with walls painted in white and penetrated by small towers, looking like small fortresses built for the needs of a single family. They are the equivalent of the Transylvanian peasant fortresses and of the Moldavian fortified monasteries – all built to protect from the invaders. Culas have a high ground floor, lighted through very narrow openings and connected to the first floor by an inner staircase. It seems that they also had secret ways out (through tunnels) like medieval fortresses. Culas in Argeş have no veranda, while the ground floor is isolated. Some of them (e.g. the cula in Curtişoara harbouring nowadays the folk art section of the Museum in Târgu Jiu, or the culas in Măldăreştii de Sus, near Horezu) have two storeys. They are spread all over the Balkans, and it seems they have been built on the present territory of Romania (all over Oltenia and Western Walachia) FACULTATEA DE MANAGEMENT AGRICOL starting with the year 1650, when lower or higher boyars were trying to protect their assets from the Turks.
    [Show full text]
  • Floods in the Last Decade: Management Flood Risk Strategy in Novaci City, Romania
    Floods in the Last Decade: Management Flood Risk Strategy in Novaci City, Romania Camelia Slave To Link this Article: http://dx.doi.org/10.46886/IJAREG/v4-i1/3145 DOI: 10.46886/IJAREG/v4-i1/3145 Received: 09 Aug 2017, Revised: 23 Sep 2017, Accepted: 12 Oct 2017 Published Online: 29 Nov 2017 In-Text Citation: (Slave, 2017) To Cite this Article: Slave, C. (2017). Floods in the Last Decade: Management Flood Risk Strategy in Novaci City, Romania. International Journal of Academic Research in Enviornment & Geography, 4(1), 37–47. Copyright: © 2017 The Author(s) Published by Knowledge Words Publications (www.kwpublications.com) This article is published under the Creative Commons Attribution (CC BY 4.0) license. Anyone may reproduce, distribute, translate and create derivative works of this article (for both commercial and non-commercial purposes), subject to full attribution to the original publication and authors. The full terms of this license may be seen at: http://creativecommons.org/licences/by/4.0/legalcode Vol. 4, No. 1 (2017) Pg. 37 - 47 https://kwpublications.com/journals/journaldetail/IJAREG JOURNAL HOMEPAGE Full Terms & Conditions of access and use can be found at https://kwpublications.com/pages/detail/publication-ethics International Journal of Academic Research in Environment & Geography Vol. 4, No. 1, 2017, E-ISSN: 2313-769X © 2017 KWP Floods in the Last Decade: Management Flood Risk Strategy in Novaci City, Romania Camelia Slave University of Agronomic Sciences and Veterinary Medicine Bucharest, Romania Email: [email protected] Abstract Floods are natural phenomena and constitute a natural component of the hydrological cycle of the earth.
    [Show full text]
  • Paper Available On: CODEN: JEBIDP
    407 © 2012 Triveni Enterprises J. Environ. Biol. Vikas Nagar, Lucknow, INDIA 33, 407-415 (2012) [email protected] ISSN: 0254-8704 Full paper available on: www.jeb.co.in CODEN: JEBIDP Conditions of gully development within piedmont areas with examples from the western part of the Getic Piedmont, Romania Author Details Sandu Boengiu Geography Department, University of Craiova, Romania, Str. Al. I. Cuza, nr. 13, Craiova, Romania Alina Vladut Geography Department, University of Craiova, Romania, Str. Al. I. Cuza, nr. 13, Craiova, Romania (Corresponding author ) e-mail: [email protected] Emil Marinescu Geography Department, University of Craiova, Romania, Str. Al. I. Cuza, nr.y 13, Craiova, Romania Abstract Features of gully morphometry and associated relief characteristics emphasizep that gully develop under a Publication Data wide variety of rock conditions, rainfall regimes, geomorphic predisposition, and human influence. Consequently, many slopes within piedmont areas, in this case, the Getic Piedmont, are characterized by dense gully Paper received: systems, as there occur excessive clearing, inappropriate land use, compaction of the soil caused by 25 October 2010 grazing, on the general background of a favourable climate.o Both rainfall and runoff factors must be considered in assessing a water erosion problem. The erosional slope development within the Getic Piedmont was Revised received: evaluated based on maps and field studies in the last 15 years, which emphasized that about 20 % of the total 02 July 2011 surface of the piedmont is affected by gully erosion. The results show that the factors leading to the strong gully erosion in this area include – the widely distributed friable rocks, the unique geomorphologic configuration, the Accepted: strong and time-concentrated rainfall, the alternanCce of drought-humid periods that prepares the ground for the 30 July 2011 development of fissures in soils, the drought that influence the growth and recovery of vegetation, and the intense human activities.
    [Show full text]
  • Romanian Toponymy – Orientation Landmarks
    Review of Historical Geography and Toponomastics, vol. II, no.3-4, 2007, pp 35-44 ROMANIAN TOPONYMY – ORIENTATION LANDMARKS Ion NICOLAE* University of Bucharest, Department of Geography, Romania, e-mail: [email protected] Abstract: Romanian Toponymy – orientation landmarks. The Romanian Toponymy is part of a wider European corpus with some distinct characteristics that the paper will mention. The real fossiles of the Human Geography (cf. Raoul Blanchard) the places names from the Romanian space reflect – on the Romanian majority background – the ethnical diversity (80% from the toponyms are formed in the Romanian language) the ressource valorification, the lack of population processes (for instance rural colonization) and the authorities interfering. There are detailed the toponymic stratification, the natural/popular toponymic changes generated by the authorities impact (through the seven networks, very active in the communist period). It is also shown the origins of the main regionimes, of the historical provinces (from Ardeal, Transylvania and Ţara Românească). Rezumat: Toponimia românească – repere de orientare. Toponimia românească este o componentă firească a toponimiei europene, cu anumite trsăsături specifice, între care unele vor fi evidenţiate în cele ce urmează. Adevărate folise ale geografiei umane (cf.Raoul Blanchard) numele de locuri din spaţiul românesc semanlează – pe fondul majorităţii româneşti – diversitatea etnică (80% dintrte toponime sunt formate în limba română), modalităţile de valorificare a resurselor (subterane şi supraterane), procesele de impopulare (colonizarea rurală între altele) şi intervenţia autorităţilor. Sunt detaliate stratifiarea toponimică, modificările toponimiei naturale/populare generate de impactul autorităţilor (prin cele şapte grile, foarte active în perioada comunistă). Se arată, de asemenea, originea principalelor regionime, a numelor provinciilor istorice (de la Ardeal/Transilvania la Ţara Românească).
    [Show full text]
  • COLEOPTERA: CERAMBYCIDAE) from the PATRIMONY of “GRIGORE ANTIPA” NATIONAL MUSEUM of NATURAL HISTORY (BUCHAREST) (Part V)
    Travaux du Muséum National d’Histoire Naturelle © Décembre Vol. LIII pp. 235–272 «Grigore Antipa» 2010 DOI: 10.2478/v10191-010-0018-3 THE CATALOGUE OF THE PALAEARCTIC SPECIES OF LAMIINAE (COLEOPTERA: CERAMBYCIDAE) FROM THE PATRIMONY OF “GRIGORE ANTIPA” NATIONAL MUSEUM OF NATURAL HISTORY (BUCHAREST) (Part V) To Dr. Nicolae Sãvulescu’s memory RODICA SERAFIM Abstract. The catalogue presents Palaearctic Cerambycidae coleopteran species of the subfamily Lamiinae preserved in the collections of “Grigore Antipa” National Museum of Natural History of Bucharest. Résumé. Le catalogue présente les espèces de coléoptères paléartiques de Cerambycidae, sousfamille Lamiinae, gardés dans les collections du Muséum National d’Histoire Naturelle “Grigore Antipa” de Bucarest. Key words: Coleoptera, Cerambycidae, Lamiinae, catalogue, collections, “Grigore Antipa” National Museum of Natural History, Bucureºti (Bucharest). INTRODUCTION The Cerambycidae collections preserved in “Grigore Antipa” National Museum of Natural History from Bucureºti (Bucharest), consists of: - material from the old coleopteran collection from the Palaearctic area (which gather specimens from Richard Canisius, Deszö Kenderessy, Eduard Fleck, Fridrich Deubel, Arnold Lucien Montandon, Emil Varady collections, acquired between 1883 – 1923); - lots of material from Dr. Nicolae Sãvulescu’s collection acquired between 1961 – 1982 and material from the same collection, which were included in the Museum patrimony in 1992, after Dr. Nicolae Sãvulescu’s death; - specimens obtained by exchange with foreign specialists and collectors; - donations: Daniel Kubisz, Mihai ªerban Procheº, Viorel Ungureanu, Petru Istrate; - material collected in the field in Romania by the specialists of the “Grigore Antipa” Museum and by their collaborators, during 1946 – 2009. - material collected from Morocco, Turkey, Bulgaria, Tunisia, Syria (Expeditions of „Grigore Antipa” Museum in the Mediterranean countries), during 2005 – 2008.
    [Show full text]
  • Sobre El Territorio De Formación De La Lengua Rumana
    SOBRE EL TERRITORIO DE FORMACIÓN DE LA LENGUA RUMANA DAN MUNTEANU Universidad de Las Palmas de Gran Canaria RESUMEN El artículo se propone reconsiderar la polémica cuestión enunciada en el título, a la luz de los más recientes resultados de las investigaciones históricas, que relaciona con los más importantes argumentos y contraargumentos lingüísticos invocados a favor de una u otra teoría acerca de la cuna del rumano. La conclusión del autor es que el pueblo rumano y su lengua se formaron en condiciones específicas; por tanto no debemos hablar de una cuna, como en el caso de las lenguas románicas occidenta­ les, sino de núcleos de rumanidad diseminados en un área muy extensa, en ambas orillas del Danubio. ABSTRACT What the author intends in this paper is to reconsider the controversial matter stated in the title, in the light of the most recent results of the historical research —the idea expressed in the tittle relates them with the most important liguistic arguments and counterarguments called on in favour of both theories about the hirthplace of the Romanian language. The author's conclusión is that both the Romanian people and their language were formed in very particular conditions. That means that we cannot talk about a single hirthplace of the language, which is the case of the western Romance languages, but about the nuclei of Romanity, disseminated in a very broad área, in both sides of the Danube. [14] DANMUNTEANU 302 1 La cuestión enunciada en el título ha sido tratada de manera directa o indirecta por muchos lingüistas e historiadores extranjeros y rumanos, desde distintas perspectivas.
    [Show full text]
  • Itor !W..] Oman 1 Lo R
    ITOR !W..]OMAN 1 LO R Impäratul Traian. Bazo-relief de pe Columna lui Traian. ' oo r .. .. 1.i.....6 ' c '''' r , °-.4' ' e, . ; , A 4 ,.,., .., .:o V X, 4t f, ii;Ske o") 'e - ,.,- =Fr o 1 Decebal se sinucide pe mormantul lard sale. Bazo-rellef de pe Columna ILA Traian. TONIA thUIIL'I EuH h A. b. XENOFOL PROFESOR LA UNIVERSITATEA DIN IAI, MEMBRU AOADEMIEI ROMANE. MEMBRU TITULAR AL INSTITUTULUI DIN FRANTIA EDITIA III-a, ingrijità de I. VLADESCU DOCTOR IN LITERE ASISTENT LA UNIVERSiTATEA DIN DUCUREVI IYu surd vremile sub càrma omulul, ci bietul om sub vreml". ti/RON COSTIN. VOLUMUL I DACIA ANTE-ROMANA SI DACIA ROMANA 513 innainte de Hr. 270 durdi Hr. BI TCUREz;l'I EL) [TURA ((CARTEA ROMÄNEA SC Ä» II STOW PIP Lttilb:10e ,_ _ XENOPOL VOL.I PREFATA LA EDITIA III-a Poate pärea indreizneald incercarea de aliza asupra-mi ingrijirea unei noui editii a Istoriei Romdpilor din Dacia Tra- iancl" a lui Xenopol. Este o muncei de ditiva ani, de multä reibdare idein- delungatä familiaritate cu materialul. Ceiteva cuvinte despre aceea ce am socolit cei trebuie fäcut. Autorul 112C6 din 1913 reveizuse toate volumele, in numeir de 14, cari duc povestirea trecutului nostru Oa la 1866, utili- zeind toate scrierile qi documentele publicate dela 1893 incoace"1. Revederea aceasta a tost socotitei ca o initiare fulgerätoare care inspirti respectur (N. Iorga) 2. Prime le 5 volume, peintila 1600, au apärut ubingrijirea sa Mai din 1913-1914 in -editura C. Sfetea". Restul n'a mai putut fi continual, din cauza boalei autorului qi apoi a eveni- mentelor, aduse de marele rtisboiu.
    [Show full text]
  • Ptolemy's Maps of Northern Europe, a Reconstruction of The
    ^^ ^A#. #^^'*i. 'v,'^ \ '^- I' " ,>. , iPc^-^: UsPiM^ ^'^m. 13 .J 6 ' Qlorncll Muiueraiti; Hibrary Jllljata. SJjm Inrk BOUGHT WITH THE INCOME OF THE SAGE ENDOWMENT FUND THE GIFT OF HENRY W. SAGE 1891 The date shows when this volume was taken. To renew this book copy the call No^snd give to the libra--"—' ^^^^ RULES -rA-fga#'"^)-A-n-8- ^ All books subject to recall All borrowers must regis- ter in the library to borrow ' books for home use. All books must be re- turned at end of college year for inspection and repairs. Limited books must be returned within the four week limit and not renewed. Students must return all books before leaving town. Officers should arrange for the return of books wanted during their absence from town. Volumes of periodicals and of pamphlets are held in the library as much as possible. For special pur- poses they are given out for a limited time. • Borrowers should not use their library privileges for ' the benefit of other persons. Books of special value and gift books, when the giver wishes it, are not allowed to circulate. Readers are asked to re- port all cases of books marked or mutilated. po not deface books by marks and writing. Cornell University Library GA213 .S38 + Ptolemy's maps of northern Europe, a rec 3 1924 029 954 868 olin Overs .''"""'^m^ PTOLEMY'S MAPS OF NORTHERN EUROPE A RECONSTRUCTION OF THE PROTOTYPES BY GUDMMD SCHOTTE PH. D. PUBLISHED BY THE ROYAL DANISH GEOGRAPHICAL SOCIETY KJ0BENHAV,N ' COPENHAGEN H. HAGERUP . PUBLISHER 'mM«mmmsiatKmiimi=:' PTOLEMY'S MAPS OF NORTHERN EUROPE PTOLEMY'S MAPS OF NORTHERN EUROPE A RECONSTRUCTION OF THE PROTOTYPES BY GUDMUND SCHUTTE PH.
    [Show full text]
  • Prefectul Judeţului Mehedinţi
    PREFECTUL JUDEŢULUI MEHEDINŢI O R D I N privind numerotarea secţiilor de votare din judeţul Mehedinţi Având în vedere: - prevederile art.15 din Legea nr.33/2007 privind organizarea şi desfăşurarea alegerilor pentru Parlamentul European; - dispoziţiile art.25 alin.(2) şi (3) din Legea nr.373/2004 pentru alegerea Camerei Deputaţilor şi a Senatului; În temeiul art.32 alin.(l) din Legea nr.340/2004 privind prefectul şi instituţia prefectului, astfel cum a fost modificată şi completată prin O.U.G. nr.179/2005, aprobată prin Legea nr.181/2006; Prefectul judeţului Mehedinţi emite prezentul O R D I N: Articol unic:Secţiile de votare din judeţul Mehedinţi, pentru organizarea şi desfăşurarea alegerii membrilor din România în Parlamentul European din data de 25 noiembrie 2007, se numerotează după cum urmează : Municipiul Dr.Tr.Severin: SECŢIA DE - B- dul Aluniş în întregime (bl.VD1,VD2,VD3) VOTARE NR.1 - Al. Aluniş în întregime (bl. B1, B2, B3, B4, C1, C2, Sala Polivalentă C3, C4); B-dul Aluniş, - Str. Brâncoveanu de la nr.1 la nr.47 şi de la nr.2 nr.1A la nr.14 (bl. B1, B2, B3, B4, B5); - Str. Calomfirescu de la nr.1 la nr.9 (bl. B1, C1, C2, C3, C4, C5); - B-dul T.Vladimirescu de la nr.1 la nr.7 şi de la nr.2 la nr.28(bl.C,B1,B2,B3,B4,B5,A1,A2) SECŢIA DE - str. Adrian de la nr.1 la nr.69 şi de la nr.2 la nr. 58 VOTARE NR.2 - str. Bolintineanu de la nr.
    [Show full text]
  • 2010 DOI: 10.2478/V10191-010-0007-6
    Travaux du Muséum National d’Histoire Naturelle © Décembre Vol. LIII pp. 103–113 «Grigore Antipa» 2010 DOI: 10.2478/v10191-010-0007-6 THE DISTRIBUTION OF STONE CRAYFISH AUSTROPOTAMOBIUS TORRENTIUM (SCHRANK, 1803) (CRUSTACEA: DECAPODA: ASTACIDAE) IN THE SOUTH-WEST ROMANIAN MOUNTAIN AND SUB-MOUNTAIN AREA LUCIAN PÂRVULESCU, IORGU PETRESCU Abstract. Data is presented in relation to the geographical distribution of the endangered crayfish species Austropotamobius torrentium. One hundred and seventy-four sampling stations situated along the streams of 15 geographical units from the South-West of Romania (Anina Mountains, Almãj, Dognecea, Godeanu, Locva, Þarcu, Retezat, Semenic, Mehedinþi, Vâlcan, Parâng, ªureanu, Poiana Ruscã, Lipova Hills and Mehedinþi Plateau) have been investigated. A distribution map was compiled. The data from older publications were collated. The actual habitat of this species occupies a large area of South-West Romania in the mountain and sub-mountain area, being absent in the Poiana Ruscã Mts, Lipova and Dognecea Hills. Résumé. Données sur la distribution géographique de l’espèce menacée Austropotamobius torrentium. Un nombre de 174 endroits qui se trouvent sur les ruisseaux des 15 unités géographiques du Sud-Ouest de la Roumanie (les montagnes de Anina Almãj, Dognecea, Godeanu, Locvei, Þarcu, Retezat, Semenic, Mehedinþi, Vâlcan, Parâng, ªureanu, Poiana Ruscã, les collines de Lipova et le plateau Mehedinþi) ont été inventoriés. On a réalisé une carte détaillée de distribution. On a centralisé les données des autres publications qui étaient plus anciennes. L’habitat actuel de l’espèce occupe une grande partie du Sud – ouest de la Roumanie de la zone de montagne et sous montagne, et est absent dans les montagnes de Poiana Ruscã et les collines de Dognecea et Lipova.
    [Show full text]