DOCSLIB.ORG

41. Carboniferous Granodiorite

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

41. Carboniferous granodiorite Location. 34 T 641581 E, 4809904 N. It is located 6.7 km south of Gorni Lom village. Category. Geosite of scientific value: outcrop of Carboniferous granodiorites. Geological setting. The outcrop is located in the Late Carboniferous St. Nikola Pluton, belonging to the Balkan granite-granodiorite complex. It is intruded between the rocks of the Chernivrah metamorphic complex and Berkovitsa low-grade metamorphic complex, parts of Berkovitsa tectonic unit. Description. The rocks of the St. Nikola Pluton crop out as prolonged in East-West direction body with width 3-3,5 km and length 16-17 km, continuing on Serbian territory. The pluton is composed of massive leucocratic to mesocratic coarse-grained rocks of granodiorite-granite composition, feldspar and quartz porphyry in places. The main rock-forming minerals are plagioclase, potassium feldspar, quartz and hornblende. Granite texture is plagioclase porphyry, and granodiorites are uneven-granular. In the rocks of the pluton is observed planar parallelism with equatorial orientation and inclination to the south from 40 to 85°. In places they show schistosity due to local tectonic events. In tectonically reworked areas granodiorites have undergone imposed metasomatic processes. Recent geochronological dating upon zircon (Carrigan et al., 2005) for St. Nikola Pluton indicate absolute age 311,9 ± 4,1 Ma, which refers to the Upper Carboniferous. Surrounding landscape. The area is surrounded by beautiful forests on the northern slopes of the highest part of the Western Balkan with peak Midzhur and outcrops of igneous and metamorphic rocks. Sensitivity and protection measures. Location of the geosite should be marked by dashboard with data about the Carboniferous magmatism and geology of the area in the center of Gorni Lom village. Access. Access to the site is on the road from Gorni Lom village to the Powder factory 4 km south of the village, and then 2,7 km on the dirt road to Martinovo village. 42. Devonian siltstones Location. 34 T 630971 E, 4832365N . It is located in the south part of Dabravka village. Category. Geosite of scientific value: outcrop of Devonian siltstones. Geological setting. The outcrop is among the Shashka siltstones of the Babin nos siltstone- diabase complex, exposed in the north-west part of the Belogradchik tectonic unit. This complex, including also the Struindol diabases, unites the only Devonian rocks in Geopark area. The unit is established during the last geological mapping of the area (Angelov et al., 2006a). Description. Shashka siltstones are established as separate unit on the map sheet Rakovitsa (Angelov et al., 2006). They are named after Shashka river west of Kireevo village, out of Geopark area. The unit is composed mainly of siltstones with transitions into sandstones, sandy shaleс and less limestones. The unit is exposed near Dabravka village where silicites and quartzites are also established. It is visited by students of the Moscow State University “Lomonosov” (Pl. 42 a,b). Surrounding landscape. Geosite is situated on the northern slope of the ridge between Dabravka and Sbegovete surrounded by beautiful landscape and impressive rock cliff on the ridge, part of the most western outcrops of the Belogradchik Formation (Pl. 42 c,d). Sensitivity and protection measures. Location of the geosite should be marked by dashboard with data about geology of the area in Dabravka village. Access. Access to the site is from the end of the main street to the flow east of Dabravka village. a b c d Plate 42: a,b – The outcrop of the Shashka siltstone near Dabravka village is visited by students and professors of the Moscow State University “M. I. Lomonosov”; c,d – outcrops of the Shashka siltstones against the most western outcrops of the Belogradchik Formation, surrounded by low forest vegetation 43. Devonian diabase Location. 34 T 627256 E, 4836718 N. It is located in Struindol village. Category. Geosite of scientific value: outcrop of Devonian diabases. Geological setting. The outcrop is among the Struindol diabases of the Babin nos siltstone- diabase complex, exposed in the north-west part of Belogradchik tectonic unit. This complex, including also the Shashka siltstones, unites the only Devonian rocks in Geopark area. The unit is established during the last geological mapping of the area (Angelov et al., 2006). Description. Struindol diabases are established as separate unit on the map sheet Rakovitsa (Angelov et al., 2006a), named after Struindol village, NW of Belogradchik town. The unit is composed of diabases, diabase tuffs and phyllitoid schists. These rocks are poorly exposed, so the outcrop in Struindol village is one of the scarce outcrops, chosen for the purposes of Geopark (Pl. 43 a). Surrounding landscape. Geosite is disposed in flat terrain with rare woods and predominant field vegetation. The closest geosites are the outcrops of Carboniferous volcanic rocks (38, 39), Carboniferous granites (40), Magura Cave (53) and Antique road stop Anishte (65). Sensitivity and protection measures. Location of the geosite should be marked by signboard on the cross road in Veshtitsa village, and by information board with data about geology of the area in Struindol village. Access. Access to the site is directly from the road in Struindol village (Pl. 43 b). a б Plate 43: a,b – Outcrop of the Struindol diabase near the road in Struindol village is one of the scarce outcrops chosen for the purposes of Geopark 44. Disconformity between Sredogriv metamorphites and Bov Formation Location. 34 T 0634406 E, 4823352 N, into the riverbed of Varbovska river on the road to Belogradchik town 1 km north of Varbovo village. Category. Geosite of scientific value: disconformity. Geological setting. The outcrop is in the southern limb of the Belogradchik anticline in Montana tectonic unit where sandy marl of the Bov Formation (Middle Jurassic) lies transgressively with a long hiatus on metasandstones of the Sredogriv metamorphites (Ordovician). Description. Geosite represents disconformity surface - a type of unconformity when younger sedimentary rocks cover unconformably older highly deformed crystalline (igneous or metamorphic) rocks. It is characterized by distinct erosional surface and a clear difference in composition and appearance of the overlying sedimentary rocks and underlying metamorphic or igneous rocks due to significant hiatus - hundreds of millions and even billions of years. In this case metasandstones of the Sredogriv metamorphites are covered transgressively by sandy marls of the Bov Formation (Pl. 44 a,b). Sredogriv metamorphites have undergone low-temperature regional metamorphism and are represented by intensively deformed greenschist rocks. These are characterized by the alternation of parametamorphic rocks - metapelites (sericite, sericite-chlorite schists and black schists) meta-sandstones, meta-siltstones, polygenic meta-conglomerates and calcoschists. Mappable bodies of meta-conglomerates and olistoplakes of metagabbro, metadiabase, metavolcanites and metagranitoids are available among them. They crop out along Varbovska and Protopopinska rivers right tributaries of Stakevska river and also along Lom river in the area of Sredogriv village. Haydoutov et al. (1995) accepted Ordovician age of these rocks. Bov Formation consists mainly of sandy marls and argillaceous limestones of Middle Jurassic age. Ultimately, these rocks are enriched in fossils of ammonites, belemnites, brachiopods, bivalves and plant remains that gives the geosite status of fossil field too. Jurassic petrified wood of this outcrop (Pl. 44 c,d) is one of the most impressive paleontological specimens in the collection of the new visitor center in Belogradchik town. Disconformity with hiatus of about 350 million years is an excellent example of long interruption of sedimentation, exposed only a few kilometers south of the outcrops of Devonian, Carboniferous, Permian and Triassic rocks in the northern limb of the anticline, missing in this geosite. Outcrops of such disconformities are rare, so this geosite is a great place to demonstrate the geological history of the region. The surrounding landscape. The outcrop is located in the picturesque valley of Varbovska river that crosses southern rock cliff formed by the limestone of the West Balkan Carbonate Group, which define the inverse relief in Belogradchik anticline. Sensitivity and protection measures. Geosite needs signposting of fork for Varbovo village on the road to Belogradchik and information board at the fountain near the outcrop. Although unmarked, it is subject of students practice for the students of Sofia University "St. Kliment Ohridski”, UMG "St. Ivan Rilski" and the Moscow State University "Lomonossov" (Pl. 44 e,f). Access. Access is directly from the road to Belogradchik town, from the fountain after the bridge over Varbovska river. а b c d e f Plate 44: а, b – Unconformity of the type „disconformity‟ between Ordovician metasandstones of the Sredogrive metamorphites (below) and Jurassic sandy marls of the Bov Formation (layers above); c, d – petrified Jurassic tree from the base of the Bov Formation above the disconformity surface; e, f – the outcrop is subject of students practices (on the photos: students of the Moscow State University “Lomonosov”) 45. Plastic sharing zone Location. 34 T 0633687 E; 4828706 N. Located in the riverbed of Stakevska River east of Chiflitsi village. Category. Geosite of scientific value: plastic shearig zone. Geological setting. The site is among the
Recommended publications
  • Late Precambrian Balkan-Carpathian Ophiolite

    Late Precambrian Balkan-Carpathian Ophiolite

    University of South Florida Masthead Logo Scholar Commons Geology Faculty Publications Geology 10-2001 Late Precambrian Balkan-Carpathian Ophiolite - A Slice of the Pan-African Ocean Crust?: Geochemical and Tectonic Insights from the Tcherni Vrah and Deli Jovan Massifs, Bulgaria and Serbia Ivan P. Savov University of South Florida, [email protected] Jeffrey G. Ryan University of South Florida, [email protected] Ivan Haydoutov Bulgarian Academy of Sciences, Geological Institute Johan Schijf University of South Florida Follow this and additional works at: https://scholarcommons.usf.edu/gly_facpub Part of the Geology Commons Scholar Commons Citation Savov, Ivan P.; Ryan, Jeffrey G.; Haydoutov, Ivan; and Schijf, Johan, "Late Precambrian Balkan-Carpathian Ophiolite - A Slice of the Pan-African Ocean Crust?: Geochemical and Tectonic Insights from the Tcherni Vrah and Deli Jovan Massifs, Bulgaria and Serbia" (2001). Geology Faculty Publications. 139. https://scholarcommons.usf.edu/gly_facpub/139 This Article is brought to you for free and open access by the Geology at Scholar Commons. It has been accepted for inclusion in Geology Faculty Publications by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Journal of Volcanology and Geothermal Research 110 *2001) 299±318 www.elsevier.com/locate/jvolgeores Late Precambrian Balkan-Carpathian ophiolite Ð a slice of the Pan-African ocean crust?: geochemical and tectonic insights from the Tcherni Vrah and Deli Jovan massifs, Bulgaria and Serbia Ivan Savova,*, Jeff Ryana, Ivan Haydoutovb, Johan Schijfc aDepartment of Geology, University of South Florida, 4202 E. Fowler Ave., SCA 520, Tampa, FL 33620-5201, USA bBulgarian Academy of Sciences, Geological Institute, So®a 1113, Bulgaria cDepartment of Marine Science, University of South Florida, 140 7th Ave S, St.
  • Annex REPORT for 2019 UNDER the “HEALTH CARE” PRIORITY of the NATIONAL ROMA INTEGRATION STRATEGY of the REPUBLIC of BULGAR

    Annex REPORT for 2019 UNDER the “HEALTH CARE” PRIORITY of the NATIONAL ROMA INTEGRATION STRATEGY of the REPUBLIC of BULGAR

    Annex REPORT FOR 2019 UNDER THE “HEALTH CARE” PRIORITY of the NATIONAL ROMA INTEGRATION STRATEGY OF THE REPUBLIC OF BULGARIA 2012 - 2020 Operational objective: A national monitoring progress report has been prepared for implementation of Measure 1.1.2. “Performing obstetric and gynaecological examinations with mobile offices in settlements with compact Roma population”. During the period 01.07—20.11.2019, a total of 2,261 prophylactic medical examinations were carried out with the four mobile gynaecological offices to uninsured persons of Roma origin and to persons with difficult access to medical facilities, as 951 women were diagnosed with diseases. The implementation of the activity for each Regional Health Inspectorate is in accordance with an order of the Minister of Health to carry out not less than 500 examinations with each mobile gynaecological office. Financial resources of BGN 12,500 were allocated for each mobile unit, totalling BGN 50,000 for the four units. During the reporting period, the mobile gynecological offices were divided into four areas: Varna (the city of Varna, the village of Kamenar, the town of Ignatievo, the village of Staro Oryahovo, the village of Sindel, the village of Dubravino, the town of Provadia, the town of Devnya, the town of Suvorovo, the village of Chernevo, the town of Valchi Dol); Silistra (Tutrakan Municipality– the town of Tutrakan, the village of Tsar Samuel, the village of Nova Cherna, the village of Staro Selo, the village of Belitsa, the village of Preslavtsi, the village of Tarnovtsi,
  • 1 I. ANNEXES 1 Annex 6. Map and List of Rural Municipalities in Bulgaria

    1 I. ANNEXES 1 Annex 6. Map and List of Rural Municipalities in Bulgaria

    I. ANNEXES 1 Annex 6. Map and list of rural municipalities in Bulgaria (according to statistical definition). 1 List of rural municipalities in Bulgaria District District District District District District /Municipality /Municipality /Municipality /Municipality /Municipality /Municipality Blagoevgrad Vidin Lovech Plovdiv Smolyan Targovishte Bansko Belogradchik Apriltsi Brezovo Banite Antonovo Belitsa Boynitsa Letnitsa Kaloyanovo Borino Omurtag Gotse Delchev Bregovo Lukovit Karlovo Devin Opaka Garmen Gramada Teteven Krichim Dospat Popovo Kresna Dimovo Troyan Kuklen Zlatograd Haskovo Petrich Kula Ugarchin Laki Madan Ivaylovgrad Razlog Makresh Yablanitsa Maritsa Nedelino Lyubimets Sandanski Novo Selo Montana Perushtitsa Rudozem Madzharovo Satovcha Ruzhintsi Berkovitsa Parvomay Chepelare Mineralni bani Simitli Chuprene Boychinovtsi Rakovski Sofia - district Svilengrad Strumyani Vratsa Brusartsi Rodopi Anton Simeonovgrad Hadzhidimovo Borovan Varshets Sadovo Bozhurishte Stambolovo Yakoruda Byala Slatina Valchedram Sopot Botevgrad Topolovgrad Burgas Knezha Georgi Damyanovo Stamboliyski Godech Harmanli Aitos Kozloduy Lom Saedinenie Gorna Malina Shumen Kameno Krivodol Medkovets Hisarya Dolna banya Veliki Preslav Karnobat Mezdra Chiprovtsi Razgrad Dragoman Venets Malko Tarnovo Mizia Yakimovo Zavet Elin Pelin Varbitsa Nesebar Oryahovo Pazardzhik Isperih Etropole Kaolinovo Pomorie Roman Batak Kubrat Zlatitsa Kaspichan Primorsko Hayredin Belovo Loznitsa Ihtiman Nikola Kozlevo Ruen Gabrovo Bratsigovo Samuil Koprivshtitsa Novi Pazar Sozopol Dryanovo
  • Manual on Border Controls Along the Danube and Its Navigable Tributaries

    Manual on Border Controls Along the Danube and Its Navigable Tributaries

    EU Strategy for the Danube Region Priority Area 1a – To improve mobility and multimodality: Inland waterways Practical manual on border controls along the Danube and its navigable tributaries Author(s): Milica Gvozdic (viadonau) Simon Hartl (viadonau) Katja Rosner (viadonau) Version (date): 31.08.2015 1 General information .................................................................................................................. 4 2 How to use this manual? .......................................................................................................... 5 3 Geographic scope .................................................................................................................... 5 4 Hungary ................................................................................................................................... 7 4.1 General information on border controls ................................................................................... 7 4.1.1 Control process ................................................................................................................... 8 4.1.2 Control forms ..................................................................................................................... 10 4.1.3 Additional information ....................................................................................................... 21 4.2 Information on specific border control points ......................................................................... 22 4.2.1 Mohács .............................................................................................................................
  • Dear Colleagues, Geopark Belogradchik Rocks (Bulgaria) Is Pleased to Announce the International Scientific Conference “20 Year

    Dear Colleagues, Geopark Belogradchik Rocks (Bulgaria) Is Pleased to Announce the International Scientific Conference “20 Year

    ASSOCIATION FOR DEVELOPMENT OF THE NORTH-WEST 3900 Belogradchik, 6, Knyaz Boris I Str. Vidin District http://www.belogradchik.bg e-mail: [email protected] phone: +359 87 8398939 Dear colleagues, Geopark Belogradchik Rocks (Bulgaria) is pleased to announce the International Scientific Conference “20 Years Global Geoparks” dedicated to the 20th anniversary of the UNESCO GEOPARKS Initiative announced in 1998 at the ProGEO Meeting in Belogradchik. The main theme of the Conference is “Geoparks and Modern Society – 20 years protection, promotion and sustainable use of Earth Heritage in park environment”. Tentative list of the conference topics: 1. Geodiversity identification, assessment and protection in geopark environment. 2. Geopark agenda – link between geological heritage and all aspect of natural and cultural heritage: interpretation, education and networking. 3. Integrated Geopark Management. 4. Geoparks towards sustainable tourism development – new approaches and trends. Presented articles will be submitted for reviewing and publishing in international thematic journals, referred in international database such as Scopus, Web of Science, Crossref. The event will be held at Belogradchik in the beginning of October, 2018. Belogradchik town is a beautiful place with remarkable geological heritage situated in NW Bulgaria. The concept of Geopark Belogradchik Rocks is based on the famous natural monument “Belogradchik rocks”, and remarkable geodiversity including sedimentary, igneous, volcanic and metamorphic rocks from Precambrian to Recent. There are dozens of caves in which artifacts of earliest settlements in Europe are preserved. The Magura Cave, which is in the tentative list of UNESCO, is known with its primitive prehistoric wall paintings and natural sparking vine. For more information you can visit websites dedicated to Belogradchik rocks, for example: http://www.belogradchik.biz/belogradchik/attractions/rocks.en.html http://severozapazenabg.com/en/ More detailed information about the Conference will be provided in the beginning of February 2018.
  • Determination of Water Resources in Rivers in the Bulgarian Basins of the Lower Danube

    Determination of Water Resources in Rivers in the Bulgarian Basins of the Lower Danube

    www.ebscohost.com www.gi.sanu.ac.rs, www.doiserbia.nb.rs, J. Geogr. Inst. Cvijic. 67(1) (11–25) Original scientific paper UDC: 911.2:556.53 (497.2) DOI: https://doi.org/10.2298/IJGI1701011I DETERMINATION OF WATER RESOURCES IN RIVERS IN THE BULGARIAN BASINS OF THE LOWER DANUBE Plamen Iliev Ninov*, Tzviatka Ivanova Karagiozova*, Maya Yordanova 1 Rankova* * National Institute of Meteorology and Hydrology — BAS, Sofia, Bulgaria Received: December 29, 2016; Reviewed: March 10, 2017; Accepted: March 31, 2017 Abstract: Object of the study is surface water bodies from category “rivers” according to Water Framework Directive 2000/60/ЕС. Surface water assessment is important for number of activities such as: water management in the country, making reports to international agencies, determining the change of the resources in the light of upcoming climate changes. The determination of water resources is based on information of hydrometric stations from the monitoring network system in the National Institute of Meteorology and Hydrology — Bulgarian Academy of Sciences (NIMH- BAS) in which real ongoing and available water flows that are subject of management are registered. In the study a technology for surface water bodies in the Bulgarian basins of the lower Danube is applied which has been developed in the frame of cooperative project together with the Ministry of Environment and Water. This is absolutely true for the Bulgarian section of the Danube River basin which is expressed in big number and variety of hydrological homogeneous sections. The river flow is characterized with annual and inter-annual variability determined by climatic factors and anthropogenic influences.
  • Deteriogenic Effect of Microbial Colonization of Prehistoric Paintings in Magoura Cave, Bulgaria

    Deteriogenic Effect of Microbial Colonization of Prehistoric Paintings in Magoura Cave, Bulgaria

    Annuaire de l’Université de Sofia“ St. Kliment Ohridski” Faculte de Biologie 2015, volume 100, livre 4, pp. 253-259 First National Conference of Biotechnology, Sofia 2014 DETERIOGENIC EFFECT OF MICROBIAL COLONIZATION OF PREHISTORIC PAINTINGS IN MAGOURA CAVE, BULGARIA MILENA MITOVA*, MICHAIL ILIEV, RALITSA ANGELOVA, VENETA GROUDEVA Department of General and Industrial Microbiology, Faculty of Biology, Sofia University “St. Kliment Ohridski”, Sofia, Bulgaria *Corresponding author: [email protected] Keywords: Biodeterioration effect, microbial colonization, paintings, Magoura cave Abstract: The Magoura Cave is located in North-Western Bulgaria. The cave contained an impressive display of prehistoric paintings, made by the guano faeces of cave dwelling bats. Many different types of microorganisms may grow on such substrates under favourable environmental conditions and have a biodeterioration effect on the paintings. The aim of the present study is focused on complete characterization of the microbial communities inhabiting the Magoura cave and determination of the most active biodeteriogens. The comparative analysis of the microbial colonization clearly demonstrates that each sample possesses unique microbial population structure and specific ratios between different target groups. The monitoring studies reveal that in the cave present continuously stable microbial population with steady qualitative and quantitative composition. In some samples high levels of sulphate-reducing bacteria, denitrifying and ammonifying bacteria as well as silicate bacteria were found. Some of these bacteria are typical biodeteriogens and it is possible they take part in the destruction of the paintings. Based on the results obtained, special treatments must be developed for the restriction of the microbial colonization and the conservation of the unique rock paintings.
  • Water Utilization and Water Management Balances of the Lom River Basin in Bulgaria

    Water Utilization and Water Management Balances of the Lom River Basin in Bulgaria

    WATER UTILIZATION AND WATER MANAGEMENT BALANCES OF THE LOM RIVER BASIN IN BULGARIA StIiliana Yancheva, Maria Temelkova Institute of Water Problems, Bulgarian Academy of Sciences Sofia , Bulgaria [email protected], [email protected] Abstract The paper present the received results from water management balance (WMB) for existing multi - purpose water resources system (WRS) in the Lom river basin – one important feeder of Danube river in North-West Bulgaria. It is done a short description and are marked the specific features of present water resources use in the river valley. For certain points from the river network are determined the main statistical characteristics of natural river flow (for the period 1961 - 2004 year). Based on the developed scheme for water use and different variants of the individual users needs are made water management balances (WMB). Experimental simulations researches for WMB are carried out with prepared input information for the inflow and water demand. Sequences for the inflow and irrigation demand in the relevant points are 44 years long by months. The results for different variants of WMB are analyzed and it is made assessment of water availability of different users. The Lom river basin problems in result of the economical, political and climate changes are discussed. Keywords: river basin, water management balance, water supply availability, water resources management, operation, management, computer model, simulation, climate change. 1 INTRODUCTION The implementation of the European directive for water (Directive 2000/60/EU) and the Law for water in Bulgaria makes necessary the developing of Plans for water management of river basins (PMRB). That is why it needs to be done an assessment for the condition of the water resources and to develop water management balances (WMB) in the river basins.
  • New Data on the Butterflies of Western Stara Planina Mts (Bulgaria & Serbia) (Lepidoptera, Papilionoidea)

    New Data on the Butterflies of Western Stara Planina Mts (Bulgaria & Serbia) (Lepidoptera, Papilionoidea)

    Ecologica Montenegrina 20: 119-162 (2019) This journal is available online at: www.biotaxa.org/em New data on the butterflies of Western Stara Planina Mts (Bulgaria & Serbia) (Lepidoptera, Papilionoidea) MARIO LANGOUROV National Museum of Natural History, Bulgarian Academy of Sciences, 1 Tsar Osvoboditel Blvd, 1000 Sofia, Bulgaria. E-mail: [email protected] Received 9 January 2019 │ Accepted by V. Pešić: 7 March 2019 │ Published online 9 March 2019. Abstract The paper represents results of surveys carried out in the Western Stara Planina Mts within the last four years in order to improve the knowledge of the butterfly fauna, especially in the Bulgarian part of the mountain. A total of 150 species of Lepidoptera (Papilionoidea) was recorded with comments on their distribution in the Bulgarian part of the studied region. Nineteen species were recorded for the first time in the Bulgarian part of the mountain and one species (Apatura metis) – for the Serbian part. It has been found that the highest butterfly diversity is linked to the largest limestone area in the mountain near Komshtitsa Village where 101 species were observed. Interesting records for some rare or endangered species (Muschampia cribrellum, M. tessellum, Lycaena helle, Kirinia climene, Apatura metis, Nymphalis vaualbum, Melitaea didyma, M. arduinna, M. diamina and Brenthis ino) are discussed in detail. The high conservation value of the studied region proves by the species considered as threatened at the European level, of which seven species are included in the Annexes II and IV of the Habitats Directive, 12 species are listed in the Red Data Book of European butterflies and 26 in the European Red List of Butterflies.
  • 5. TURISMUL Zona Transfrontalieră, Este Caracterizată Printr-Un Potenţial Turistic Foarte Ridicat, Insuficient Exploatat Şi Insuficient Promovat

    5. TURISMUL Zona Transfrontalieră, Este Caracterizată Printr-Un Potenţial Turistic Foarte Ridicat, Insuficient Exploatat Şi Insuficient Promovat

    Analiza şi diagnoza situaţiei curente în cadrul ariei transfrontaliere România - Bulgaria 5. TURISMUL Zona transfrontalieră, este caracterizată printr-un potenţial turistic foarte ridicat, insuficient exploatat şi insuficient promovat. Aici pot fi practicate aproape toate formele de turism datorită patrimoniului natural şi antropic variat, valoros şi atractiv. Potenţialul turistic identificat în fiecare din unităţile administrative analizate este prezentat în continuare. Mehedinţi Pe teritoriul judeţului Mehedinţi se regăsesc toate formele de relief, împărţite în procente egale, dispuse în trepte din nord - vest spre sud - est; de la cea mai înaltă treaptă munţii Mehedinţi şi Cernei, apoi podişul Mehedinţi, dealurile Motrului şi câmpia Bălăciţei spre cea mai coborâtă câmpia Blahniţei (terasele Dunării şi văile Drincei şi Blahniţei). Variaţia reliefului duce la apariţia peisajelor cu relief carstic şi structuri geologice deosebite ce atrag numeroşi turişti. De asemenea caracteristicele climei temperat continentale cu influenţe mediteraneene fac posibile practicarea turismului pe durata întregului an. Resursele turistice naturale de pe teritoriul judeţului sunt legate în special de o zonă turistică importantă pentru ţara noastră - Porţile de Fier. Variaţia reliefului duce la apariţia de peisaje inedite ce atrag numeroşi turişti - pe abrupturile calcaroase între Sviniţa şi Greben, traseele drumurilor DN 67D de la Baia de Aramă-Obârşia Cloşani- Valea Cernei şi DN57(E70) ce însoţeşte traseul Dunării, viaductele arterei peste afluenţii Dunării, fie Sistemele Hidroenergetice şi de navigaţie Porţile de Fier I şi Porţile de Fier II sau zone fosilifere Sviniţa, Bahna sau tufărişurile mediteraneene de la Izverna şi din Defileul Dunării, viaductele peste afluenţii Dunării, porturile din municipiul Drobeta -Turnu Severin şi oraşul Orşova. Turiştii pot valorifica fondul piscicol din lacurile naturale, de acumulare, al Dunării şi al râurilor de pe teritoriul judeţului şi fondul cinegetic din pădurile judeţului.
  • “Road Map” for Revision of the Bulgarian Biosphere

    “Road Map” for Revision of the Bulgarian Biosphere

    “ROAD MAP” FOR REVISION OF THE BULGARIAN BIOSPHERE RESERVES DESIGNATED UNDER UNESCO’S MAN AND THE BIOSPHERE PROGRAMME “ROAD MAP” FOR REVISION OF THE BULGARIAN BIOSPHERE RESERVES DESIGNATED UNDER UNESCO’S MAN AND THE BIOSPHERE PROGRAMME CURRENT STATE Bulgaria has 16 Biosphere reservesn (BR) all designated in 1977 – Alibotush, Bayuvi Dupki - Dzhindzhiritsa, Bistrishko Branishte, Boatin, Chervenata stena, Chuprene, Dzhendema, Dupkata, Kamchia, Kupena, Mantaritsa, Uzunbudzhak, Parangalitsa, Srebarna, Steneto, Tsarichina. They were selected to represent typical ecosystems with relatively untouched biotic and abiotic components and are more or less evenly distributed throughout the country. All BRs belong to the first generation of Biosphere Reserves, designated long before the adoption of the Seville Strategy and the Statutory Framework, and thus, they were established only with core zones. So, only the conservation and partly the logistic support funtions, related to research and biodiversity monitoring have been taking place. None of the 16 Bulgarian BRs coressponds to the zoning and functional requirements of the Seville Strategy and Statutory framework, adopted in 1995. Fifteen BRs are strict reserves and one (Srebarna) is a managed reserve according to the Bulgarian legislation. These categories are very strict and do not allow any human activities related to sustainable usage of natural resources. According to the Constitution of the Republic of Bulgaria (Article 18) and the Protected Areas Act - PAA (Article 8, paragraph 1), the strict and managed reserves are exclusive state property and are managed by the respective governmental institutions and their branches, i.e. the Ministry of Environment and Water (MOEW) and the Regional Inspectorates of Environment and Water (RIEW).
  • Guide to Western Stara Planina the Unknown Natural Wealth Authors: Lora Zhebril Zhivko Momchev

    Guide to Western Stara Planina the Unknown Natural Wealth Authors: Lora Zhebril Zhivko Momchev

    WORKING TOGETHER IN SUPPORT OF SUSTAINABLE SOLUTIONS GUIDE BG GUIDE TO WESTERN STARA PLANINA THE UNKNOWN NATURAL WEALTH AUTHORS: LORA ZHEBRIL ZHIVKO MOMCHEV EDITOR: VENCI GRADINAROV WWW.BGTEXT.BG GRAPHIC DESIGN: OILARIPI TREKKING ASSOCIATION WWW.OILARIPI.COM FRONT COVER: IVAN VELOV PUBLISHED BY WWF BULGARIA, SOFIA © 2017 WWF BULGARIA. ALL RIGHTS RESERVED. ALL MATERIALS IN THIS PUBLICATION ARE SUBJECT TO COPYRIGHT AND CAN BE REPRO- DUCED WITH PERMISSION. ANY REPRODUCTION IN FULL OR IN PART MUST MENTION THE TI- TLE AND CREDIT THE ABOVE-MENTIONED PUBLISHER (WWF BULGARIA) AS THE COPYRIGHT OWNER. THE DESIGNATION OF GEOGRAPHICAL ENTITIES IN THIS REPORT, AND THE PRE- SENTATION OF MATERIAL, DO NOT IMPLY THE EXPRESSION OF ANY OPINION WHATSOEVER ON THE PART OF WWF CONCERNING THE LEGAL STATUS OF ANY COUNTRY, TERRITORY, OR AREA, OR OF ITS AUTHORITIES, OR CONCERNING THE DELIMITATION OF ITS FRONTIERS OR BOUNDARIES. GUIDE TO WESTERN STARA PLANINA THE UNKNOWN NATURAL WEALTH © PLAMEN DIMITROV PLAMEN © THE GUIDEBOOK FOR WESTERN STARA PLANINA WAS DEVELOPED WITHIN THE “FOR THE BALKAN AND THE PEOPLE”PROJECT, AN INITIATIVE OF SIX BULGARIAN AND FOUR SWISS ORGANIZATIONS. IT WILL GIVE YOU A HINT ABOUT SOME REMARKABLE PLACES TO VISIT IN THE AREA AND IT WILL INTRODUCE YOU TO SOME OF THE SIGNIFICANT SUCCESSFUL RESULTS OF THE PROJECT OVER THE PAST FIVE YEARS. IT WILL TELL YOU HOW THE IMPOSSIBLE SOMETIMES BECOMES POSSIBLE AT PLACES WHERE NOBODY EXPECTED. WITH THE HELP OF THE FINANCIAL SUPPORT OF THE BULGARIAN-SWISS COOPERATION PROGRAM AND THE EFFORTS OF ALL THE EXPERTS FROM THE PARTNER ORGANIZATIONS, SEVERAL FARMERS FROM NORTH-WEST BULGARIA MANAGED TO SUCCESSFULLY COM- PLETE ALL PROCEDURES FOR REGISTRATION AS PRODUCERS , COMPLETELY OUT OF THE GREY SECTOR.