Kırcaali Habergazetesine
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Fossil Sea Lilies of the Genus Isselicrinus Rovereto, 1914 from the Lower Oligocene, Eastern Rhodopes (Bulgaria)
GEOLOGICA BALCANICA, 47 (1), Sofia, May 2018, pp. 37–41. Fossil sea lilies of the genus Isselicrinus Rovereto, 1914 from the lower Oligocene, Eastern Rhodopes (Bulgaria) Lidiya Kirilova1, Vladimir Georgiev2 1 Regional Museum of History Kardzhali, 4 Republikanska Str., 6600 Kardzhali, Bulgaria; e-mail: [email protected] 2 Geological Institute, Bulgarian Academy of Sciences, Acad. G. Bonchev Str., Bl. 24, 1113 Sofia, Bulgaria; e-mail: [email protected] (Accepted in revised form: March 2018) Abstract. Fossil sea lilies of the genus Isselicrinus Rovereto, 1914 were found near the village of Raven, Momchilgrad Municipality, in the Eastern Rhodopes in 1978. They were recovered from the rocks of the Raven complex. The latter is composed of rhyolite pyroclastics with layers of reef limestones. With the Ar/Ar method, the pyroclastics of thе Raven complex have been dated as 31.19–30.97 Ma (early Oligocene). The presence of reef limestones suggests shallow coastal waters with normal salinity and a warm climate, in which Isselicrinus lived. These were the outskirts of a tropical basin, inhabited by faunas, which today have their descendants in the tropical areas. Kirilova, L., Georgiev, V. 2018. Fossil sea lilies of the genus Isselicrinus Rovereto, 1914 from the lower Oligocene, Eastern Rhodopes (Bulgaria). Geologica Balcanica 47 (1), 37–41. Keywords: Isselicrinus sp., family Isselicrinidae, taxonomy, lower Oligocene, Eastern Rhodopes, Bulgaria. INTRODUCTION nected by ligaments in the pits (Hess and Messing, 2011). Crinoids are marine animals that belong to the class Compared to their Mesozoic counterparts, fossil Crinoidea, phylum Echinodermata. The name of the records of Palaeogene and Miocene crinoids are quite class comes from the Greek words krinon, “a lily”, and poor. -
T.C. Sofya Büyükelçiliği 2. Uluslararası Çocuk Şenliği Düzenledi
“К-КЪРДЖЪ” ЕООД П р о д а ж б а н а а п а р т а м е н т и , гаражи и търговски обекти Кърджали, ул. “Ст.Стамболов” № 7, www.kirciinsaat.com www.koch-imot.eu GSM:+359(877) 257-777 KIRCAALİ HABER 08 Mayıs 2019 (Çarşamba) Yıl: XIII Haftalık Siyasi ve Aktüel Gazete Sayı: 470 Fiyatı 1 Lv. Kırcaali’de Coşkulu 23 Nisan Konseri Kültür Derneği’ne çok şey borç- geldiği kadar çocuklarımıza da lu olduğunu söyleyen Ayhan müziği öğretmeye çalışacağız” Şakir, ”Bu dernek olmasaydı, dedi. şimdi belki de karşınızda olma- Programın sonunda organiza- yacaktım. Bir de bir başka tarafı törlere ve tüm amatör sanatçıla- var bu olayın, müzikle, kültürle, ra çiçekler sunuldu. sanatla uğraşan çocuklar, kötü Çocuk Bayramı kutlaması tüm yollardan uzak durur. Bunu ken- çocukların sahnede hep bera- dimden biliyorum. Ben böyle ber Hayat Bayram Olsa şarkısı- büyüdüm, inşallah, elimizden na eşlik etmeleriyle son buldu. T.C. Sofya Büyükelçiliği 2. Uluslararası Çocuk Şenliği Düzenledi Türkiye Cumhuriyeti’nin kurucusu Mustafa Kemal Atatürk’ün geleceğin mimarları çocuklara armağan ettiği “23 Nisan Ulusal Egemenlik ve Çocuk Bayramı” kapsamında T.C. Sofya Büyükel- çiliği ilki 2018 yılında gerçekleştirilmiş olan Uluslararası Çocuk Şenliği’nin ikincisini bu yıl 20 Nisan Cumartesi günü 14.00-17.00 Resmiye MÜMÜN izleyicilerin de olması gözden neye çıkan Çocuk Folklor Ekibi, saatleri arasında Ramada Otel’de düzenledi. kaçmadı. Kırcaali Türk Halkoyunları ve Onursal Başkanlığını Büyükelçinin eşi Didem Ulusoy’un yaptığı Kırcaali Ömer Lütfi Kültür Der- Konsere teşrif eden konuklar Türküleri Ekibi, Sürpriz Modern Türk-Bulgar Kadınları Dostluk Derneği’nin (TUBUKADD) işbirliğiy- neği ile Türk Kültür ve Sanat arasında Türkiye Cumhuriyeti Dans Grubu ve yetenekli çocuk le düzenlenen Şenliğe çoğu çocuk olmak üzere 500’ü aşkın kişi Derneği’nin (TÜRKSAD) ortak Filibe Başkonsolosluğu Muavin ve gençler, büyük beğeni topla- katıldı. -
Annexes to Rural Development Programme
ANNEXES TO RURAL DEVELOPMENT PROGRAMME (2007-2013) TABLE OF CONTENTS Annex 1 ...........................................................................................................................................4 Information on the Consultation Process ........................................................................................4 Annex 2 .........................................................................................................................................13 Organisations and Institutions Invited to the Monitoring Committee of the Implementation of the Rural Development Programme 2007-2013 .................................................................................13 Annex 3 .........................................................................................................................................16 Baseline, Output, Result and Impact Indicators............................................................................16 Annex 4 .........................................................................................................................................29 Annexes to the Axis 1 Measures...................................................................................................29 Attachment 1 (Measure 121 Modernisation of Agricultural Holding) .........................................30 List of Newly Introduced Community Standards .........................................................................30 Attachment 1.A. (Measure 121 Modernisation of Agricultural Holding -
Magmatic Complexes in the Momchilgrad Depression (Eastern Rhodopes)
Georgiev Vl.et al. MAGMATIC COMPLEXES IN THE MOMCHILGRAD… 50 years University of Mining and Geology “St. Ivan Rilski” Annual, vol. 46, part І, Geology and Geophysics, Sofia, 2003, рр.37-42 MAGMATIC COMPLEXES IN THE MOMCHILGRAD DEPRESSION (EASTERN RHODOPES) Vladimir Georgiev, Petar Milovanov Geological Institute, BAS, 1113, Sofia ABSTRACT The products of the Paleogene magmatic activity in the Momchilgrad depression have been divided into several magmatic complexes. The Kalabak andesite, Rabovo latite-andesite, Zvezdel basaltic-andesite, Sveti Ilia trachyrhyodacite, Momchilgrad trachydacite and Raven rhyolite complexes, formed into Dambalak group, have the same area of distribution and similar geochemical and isotope features. They might have resulted from the evolution on a intermediate magma reservoir as their composition evolved from intermediate to acid. Extrusive bodies of the Perperek trachyrhyolite and Ustren rhyolite complexes are located apart from the main volcanic edifices and have specific geochemical features, and probably resulted from evolution of separate acid magma reservoirs. INTRODUCTION They had similar but not identical and concurrent evolution. Therefore, the correlation and integration of the rocks Two general papers concerning Paleogene deposits and generated by different magma chambers in an uniform scheme magmatic activity were published in one issue in 1960 is not correct. Independent subdivision of the separate areas (Goranov, 1960; Ivanov, 1960). They have many similarities - produced by different reservoirs is more advisable. both authors used the lithostratigraphic approach in the subdivision of magmatic products and they both recognized The term “complex” is used in the reported subdivision of the three intermediate and three acid vocanic horizons. According magmatic rocks in the sense of the Stratigraphic code of to Goranov these horizons are Pr4, Ol2, Ol5 (intermediate) and Bulgaria (Nikolov, Sapunov, 2002) as an official Ol1, Ol3, Ol5 (acid). -
Marinova, I., P. Nenova. 2008. Petrography and Geological Setting
Geoarchaeology and Archaeomineralogy (Eds R. I. Kostov, B. Gaydarska, M. Gurova). 2008 Proceedings of the International Conference, 29-30 October 2008 Sofia, Publishing House “St. Ivan Rilski”, Sofia, 193-200. PETROGRAPHY AND GEOLOGICAL SETTING OF A THRACIAN ROCK-HEWN SANCTUARY TO THE SOUTH OF THE VILLAGE OF RAVEN, MOMCHILGRAD DISTRICT, EASTERN RHODOPES Irina Marinova, Petya Nenova Central Laboratory of Mineralogy and Crystallography „Acad. I. Kostov”, Bulgarian Academy of Sciences, 1113 Sofia, Acad. G. Bonchev Str.,Bl. 107, e-mail: [email protected] ABSTRACT. Vaulted niches, rock graves, and rock discs hewn into the base of a vertical rock wall were discovered in 1997 at 550 m to the South of the village of Raven, Momchilgrad District, Eastern Rhodopes. These rock-hewn features in shape and manner of working are identical to such structures from other suggested as Thracian rock-hewn sanctuaries in the Momchilgrad District. The petrography of the rocks, into which the sanctuary is hewn, are described – they are tough, lightweight, soft and porous massive red-brown vitric-crystal lapilli rhyolitic tuffs of the Third Felsic Volcanism manifested in the Momchilgrad Depression (Sixth Oligocene Horizon, Raven Volcanic Complex) of Middle Oligocene age. The tuffs are composed of crystal clasts (around 30 vol. %), vitric clasts (around 20-30 vol. %), lithic clasts (below 1 vol. %) and a matrix (around 40-50 vol. %). The crystal clasts are represented by quartz, oligoclase, potassium feldspar, biotite, adularia, zircon, and ore minerals. The vitric clasts consist of pumiceous and compact volcanic glass. They are not flattened and being pale coloured lend a variegated outlook of the rhyolitic tuffs. -
Volcanic and Metallogenic Evolution of the Momchilgrad Depression (Eastern Rhodopes)
Georgiev Vl. VOLCANIC AND METALLOGENIC… 50 years University of Mining and Geology “St. Ivan Rilski” Annual, vol. 46, part І, Geology and Geophysics, Sofia, 2003, рр.31-36 VOLCANIC AND METALLOGENIC EVOLUTION OF THE MOMCHILGRAD DEPRESSION (EASTERN RHODOPES) Vladimir Georgiev Geological Institute, BAS, 1113, Sofia, E-mail: [email protected] ABSTRACT Preceding volcanic activity epithermal low-sulfidation quartz-gold-adularia ore mineralizations are localized within the various Paleocene and Late Eocene sedimentary rocks in the Momchilgrad depression. Hydrothermal-metasomatic deposits of montmorillonite bentonite are formed within tuffs of the Beli Plast rhyodacite and Rabovo latite-andesite complexes. Agate occurrences associate with the latite-andesites of the Rabovo complex. Volcanogenic-sedimentary clinoptilolite zeolite deposits are formed within the tuffs of the Perperek complex. Perlite deposits are localized within the extrusive bodies of the Perperek trachyrhyolite and Ustren rhyolite complex. The formation of the quartz-Au-polymetallic Zvezdel-Pcheloyad ore field spatially and genetically is related to the Zvezdel volcano (built by basaltic- andesites of the Zvezdel complex). The Momchilgrad depression is situated in the area between Locally, the tuffs and epiclastics are interbedded by reef the Central and Southeastern Rhodopes blocks of the limestones indicating that volcanoes grew up in a shallow Rhodopes Massif. Various breccias, conglomerates, marine basin. The tuffs are cut or covered by Amph-Py sandstones, marlstones and limestones deposited within the andesites. Agate occurrences associate with the andesite depression during the Paleocene and Late Eocene. lavas of this complex. PRIABONIAN RUPELIAN The metallogenic processes preceded intense volcanic The Momchilgrad depression extended to the east of the activity in the depression. -
Full Page Photo
GEOLOGICA BALCANICA, 31. 3-4, Sofia, Decemb. 2001, p. 3-36 Late Alpine (Palaeogene) superimposed depressions in parts of Southeast Bulgaria Ivan Boyanov, Alexandar Goranov Geologica/Institute, Bulgarian Academy ofSciences, 1113 Sofia (Submitted: 6. 11.1995; accepted.for publication: 3. 04.1996; .final version received: 4. 06.200 I) 11. EoRII06, A. FopaHoa - llo3iJHeOJI&nuucKue (nOJieozeHo- Abstract. The Late Alpine superimposed depressions in the 8ble) naROJICei/Hble iJenpeccuu 6 'lacmu !Ozo-Bocmo•IHOU south-eastern part of the Balkan peninsula are structures of Eoll?apuu. TioJ.uHeanbnHikKHe HaJJO>KeHHbte .uenpeccHH 8 collisional-collapse type. They play a role of neoautochton 10f0-80CTO'IHOH '!aCTH baJJ.KaHCKOfO nonyoCTp08a .ll8nJUOTC.ll which overlays a highly disintegrated Middle and Late Al cTpyKT)'paMH KonnHJHOHHO-Konnanco8oro THna. 0HH Hrpa pine orogen ofcollage-accretional character. It is represented IOT pOnb HeOaBTOXTOHa, pa3nonmKeHHOfO Ha.ll rny60KO pac by the Sredna Gora and Rhodope superunits. The superim '!neHeHHblM KOnna>KHO-aKKpeUHOHHblM cpe.UHe-8epXHe posed depressions are of Palaeogene-Neogene age and are aJlbOHHCKHM oporeHOM, KOTOpblH npe.UCTaBeH .ll8YM.ll Ha.Ube elements of a separate tectonic entity (Maritsa superimposed .llHHHUaMH: Cpe.uHeropcKOH H Po.uoncKOH. BoJpaCT .uenpec graben system) within the boundaries of the Balkanides CHH - naneoreH-HeoreH08biH. CaMH OHH .ll8n.liiOTC.ll :meMeH Anatolian segment of the Alpine mobile belt. The following TaMH MapHUCKOH Hano>KeHHOH rpa6eH080H CHCTeMbl, T.e. three wide depressions on South Bulgarian territory are char caMOCTO.liTeJibHOH TeKTOHH'IeCKOH e.UHHHUbl, npHHa.une>Ka acterized in this paper: Upper Thrace Depression (UTD), LUeH K baJJKaHH.UHO-AHaTOnHHCKOMY cerMeHT)' AnbnHHCKO East Rhodope Depression (ERD) and the East Thrace De fO no.u8H>KHoro no.11ca. -
List of Appendices
Preparation of Regional Water and Wastewater Master Plans for Central Region Regional Final Master Plan for ViK OOD - Kardzhali LIST OF APPENDICES APPENDIX 1-1 PROJECTS UNDER IMPLEMENTATION ............................................................................................. 1 APPENDIX 1-2 REGULATORY FRAMEWORK IN BULGARIA...................................................................................... 3 APPENDIX 1-3 REGULATORY FRAMEWORK IN THE EUROPEAN COMMUNITY ....................................................... 9 APPENDIX 2-1 PROJECT SCOPE ............................................................................................................................. 12 APPENDIX 2-2 ADMINISTRATIVE DATA ................................................................................................................ 13 APPENDIX 2-3 MAPS OF GROUNDWATER BODIES ................................................................................................ 22 APPENDIX 2-4 DRINKING WATER MONITORING FOR THE YEAR 2012 ................................................................... 26 APPENDIX 3-1 GENERAL FEATURES OF SURFACE WATER...................................................................................... 28 APPENDIX 3-2 GROUNDWATER QUANTITY .......................................................................................................... 32 APPENDIX 3-3 WATER SUPPLY ZONES ................................................................................................................. 39 APPENDIX 3-4 GROUNDWATER -
3-1 CHAPTER 3 GIS DATABASE 3.1 Introduction the Project Objective
The Study on Integrated Water Management Final Report - Main Report in the Republic of Bulgaria Chapter 3 CHAPTER 3 GIS DATABASE 3.1 Introduction The project objective, concerning GIS as stated in the Inception and Interim Report, is the development of GIS Database (GIS-DB) for storing all basic data and information needed for the river basin management. The GIS database and the integrated basin analysis model are effective tools for the development and update of the river basin management plan. The main purpose of GIS-DB for MoEW is to create an effective geo-spatial database, using contemporary GIS principles and technologies, based on international and national standards and legislation. The GIS-DB is designed to provide MoEW and related organizations with accurate and up-to-date geographic information, related to the river basin management. The development of the GIS-DB is based on the existing technical infrastructure (software, hardware) of MoEW and related institutions, but it introduce and implement additional software products, technologies and procedures for use of geographical data. The general functions for the use of the GIS-DB for MoEW are: • Collection and integration of digital and non-digital data from variety of sources and formats to a standardized and structured model; • Storing of geographic information and other related non-spatial information on a geodatabase level; • Actualization of the geographic and other related non-spatial information; • Performing of analysis and modeling of the geographic information; • Facilitating the exchange of geographic information between the different informational databases within MoEW system; • Exchange of geographic information with external systems (other ministries, governmental institutions, European commission). -
Pagina 1 Di 17 13/10/2014
Pagina 1 di 17 Print Bluetongue, Bulgaria Close Information received on 24/09/2014 from Pr. Nikola T. Belev, OIE Delegate, OIE Regional Representation for Eastern Europe, Ministry of Agriculture and Food , SOFIA, Bulgaria Summary Report type Follow-up report No. 5 Date of start of the event 04/07/2014 Date of pre-confirmation of the 04/07/2014 event Report date 24/09/2014 Date submitted to OIE 24/09/2014 Reason for notification Reoccurrence of a listed disease Date of previous occurrence 27/03/2008 Manifestation of disease Clinical disease Causal agent Bluetongue virus Serotype 4 Nature of diagnosis Clinical, Laboratory (basic) This event pertains to the whole country Immediate notification (15/07/2014) Follow-up report No. 1 (07/08/2014) Follow-up report No. 2 (08/08/2014) Related reports Follow-up report No. 3 (01/09/2014) Follow-up report No. 4 (08/09/2014) Follow-up report No. 5 (24/09/2014) New outbreaks (119) Outbreak 1 Velika, Tsarevo, Burgas, BURGAS Date of start of the outbreak 29/07/2014 Outbreak status Continuing (or date resolved not provided) Epidemiological unit Farm Species Susceptible Cases Deaths Destroyed Slaughtered Affected animals Goats 50 0 0 0 0 Sheep 37 2 1 0 0 Outbreak 2 Kisiitsite, Tryavna, Gabrovo, GABROVO Date of start of the outbreak 30/07/2014 Outbreak status Continuing (or date resolved not provided) Epidemiological unit Farm Species Susceptible Cases Deaths Destroyed Slaughtered Affected animals Sheep 11 1 1 0 0 Outbreak 3 Belitsa, Tryavna, Gabrovo, GABROVO Date of start of the outbreak 31/07/2014 Outbreak -
Annexes to Rural Development Programme
ANNEXES TO RURAL DEVELOPMENT PROGRAMME (2007-2013) TABLE OF CONTENTS Annex 1 ...........................................................................................................................................4 Information on the Consultation Process ........................................................................................4 Annex 2 .........................................................................................................................................13 Organisations and Institutions Invited to the Monitoring Committee of the Implementation of the Rural Development Programme 2007-2013 .................................................................................13 Annex 3 .........................................................................................................................................16 Baseline, Output, Result and Impact Indicators............................................................................16 Annex 4 .........................................................................................................................................29 Annexes to the Axis 1 Measures...................................................................................................29 Attachment 1 (Measure 121 Modernisation of Agricultural Holding) .........................................30 List of Newly Introduced Community Standards .........................................................................30 Attachment 2 (Measure 123 Adding value of agricultural and forestry -
Oligocene Pyroclastic Rocks and a Petrified Forest in the Nanovitsa Depression
БЪЛГАРСКА АКАДЕМИЯ НА НАУКИТЕ • BULGARIAN ACADEMY OF SCIENCES ГЕОХИМИЯ, МИНЕРАЛОГИЯ И ПЕТРОЛОГИЯ • 42 • СОФИЯ • 2005 GEOCHEMISTRY, MINERALOGY AND PETROLOGY • 42 • SOFIA • 2005 Oligocene pyroclastic rocks and a petrified forest in the Nanovitsa depression Svetoslav Georgiev, Peter Marchev Abstract. The 31Ma-old tuffs in the Nanovitsa depression of the Eastern Rhodopes preserve evidence of a series of large eruptions of acid pyroclastic rocks and one of the largest Oligocene natural disasters in the Rhodopes region. Intra-depression acid tuffs overlie Zvezdel, Dambalak and Sveti Ilia intermediate lava flows, as well pyroclastic rocks from the Borovitsa volcanic area (second acid volcanism) dated at 31.8 Ma. The pyroclastic sequence consists of two ignimbrite units (Raven and Sapdere type) and one mixed unit comprising air-fall tuffs and epiclastic rocks. Air-fall deposits buried a forest, consisting of giant (up to 4 m in diameter) and smaller sub-vertical trees. The trees are silicified, with well-preserved wood structure. The presence of numerous sub-horizontal carbonized branches in the transitional level between the air-fall tuffs and the ignimbrites, as well as the well- developed radial cracks and gas-escape structures above the branches, suggest a quick deposition of both the air-fall tuffs and the ignimbrites from an eruption column. Careful examination of the orientation of the branches places constraints on the location of the vent that generated the eruption, which we argue to be to the NE of the Nanovitsa depression. The ignimbrites are strongly zeolitized, which hinders the correct determination of their whole-rock chemical composition. Whole-rock analyses of a pumice clast and two melt inclusions in quartz phenocrysts show a high-K high-silica rhyolite composition for the magma.