Plant Communities Growing on Marble Slopes Or North Pirin Mts (SW
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The Pirin Mountains, Bulgaria) in the Last Ten Years
STUDIA GEOMORPHOLOGICA CARPATHO-BALCANICA VOL. XLV, 2011: 47–68 PL ISSN 0081-6434 EMIL GACHEV (BLAGOEVGRAD) INTER-ANNUAL SIZE VARIATIONS OF SNEZHNIKA GLACIERET (THE PIRIN MOUNTAINS, BULGARIA) IN THE LAST TEN YEARS Abstract: Glacierets, which are in fact embryonic forms of recent glaciation, can serve as important indicators of contemporary climate dynamics in areas where classical glaciers do not exist, such as the high mountains in Southeastern Europe. Two glacierets are located in Bulgaria’s Pirin Mountains: Snezhnika and Banski Suhodol. Snezhnika has been relatively well studied for the last 50 years, and in particular since 1994, when annual size measurements on a regular basis started. The present study focuses on the recent variations in the size of Snezhnika i.e. in the last ten years. Data about the area of the glacieret at the end of the ablation season (in autumn), which was obtained for each year by field measurements and analytical calculations, show that temperature can be considered as a major factor that drives glacieret fluctuations. At the current stage precipitation factor can not be evaluated properly due to the deficit of accurate climate information. Key words: the Pirin Mountains, glacierets, size variation, climate change, climatic factors INTRODUCTION Although small in size and volume, in many mountain areas glacierets are natu- ral features of sufficient value for studies of the dynamics of environmental proc- esses, climatic variations and change. Glacierets are small bodies of perennial ice, which are smaller than glaciers but bigger and more persistent than snow patches. Glacierets are typified by a density of close-to-bottom ice of about 0.6 to 0.8 g cm–3, presence of annual layers in the vertical cross-section, and long- term persistence — decades to centuries (G r u n e w a l d et al. -
Bulgaria's Pirin Mountains
The Pirin Mountains, Bulgaria ABODE OF THE THUNDER GOD 13th - 27th June Introduction The YRC meet to Bulgaria came about after a chance communication from Lizzie Alderson, who runs Pirin Adventures, a company which provides mountaineering, trekking and walking holidays in the Pirin Mountains of Bulgaria. Further conversations with Lizzie in Leeds and some research on the internet confirmed that it would be a novel and extremely interesting location for an overseas meet, with plenty of scope for a fortnight’s hut-to-hut trekking, taking in ridges and summits as we pleased. Named after Perun, the Thracian god of thunder and lightning, the Pirin Mountains are crystalline and located in southwest Bulgaria within the western part of the Rila-Rhodope massif. The Pirin massif slopes southwards and has a width of 30-35km. The main axis is oriented NW-SE with an approximate length of 70km. The northern part of the range comprises the Pirin National Park of 232 square kilometres, which has UNESCO status. The geology is complex but the mountain ridges are mostly granite. The Koncheto ridge and its continuation over Kutelo and Vihren summits are different and comprise marbleised karst with remains of the granite intrusion and some limestone. Limestone is also present around Mt Orelyak to the east. There are over 180 glacial tarns and lakes in Pirin. The Alpine zone scree and rocks are replaced by sub-alpine meadow-bush areas around 2300m and mountain forest between 1000-2000m. This ecological diversity was enhanced by the rapidly ablating snowfields present in June, providing us with an amazing display of flora and fauna. -
VIHREN - Mermerni Tron Boga Peruna
VIHREN - mermerni tron boga Peruna Nacionalni park Pirin - Vihren 2.914 mnv, Todorka 2.746 mnv, Banski Suhodol 2.884 mnv, Kutelo 2.908 mnv 01.10. (četvrtak ) Polazak na akciju u večernjim satima, biće naknadno određeno. Okvirno: 20:30 Novi Sad - kod lokomotive na železničkoj stanici 22:00 Beograd - autobusko stajalište na autoputu preko puta Sava centra u pravcu Niša 02.10. (petak) - Todorka (srednje teška tura) Dolazak u ranim jutranjim satima u mesto Bansko. Odlazak prevozom do doma Vihren odakle kreće uspon. Ispred doma je moguće natočiti vodu. Obilazak Banderiskih jezera, jednih od najlepših jezera na Pirinu, a zatim se penjemo do Todorkine porte, Male Todorke i na kraju do vrha Velika Todorka (2.746m). Sledi zatim hodanje kružnom stazom do jezera Todorine oči i povratak na istu stazu kojom smo došli do vozila. Napravićemo pauzu za ručak u planinarskom domu Vihren ili u obližnjem planinarskom domu Banderica. Čeka nas staza dužine 11 km i savladavanje visinske razlike od oko 950 metara. Posle završetka ture, odlazak u smeštaj u Banskom u privatnom smeštaju u sobama od 2 do 4 kreveta. Svaka soba ima svoje kupatilo. 03.10. (subota) - Vihren, Kutelo, Banski Suhodol (grupa I - naporna tura, grupa II - srednje teška tura) Polazak iz Banskog ka planinarskom domu Vihren. Uspon na vrh Vihren (2.914.mnv), treći vrh na Balkanu po visini. Ako vremenske prilike budu stabilne, delimo se u dve grupe. Grupa I Grupa I nastavlja pešačenje, silazi sa vrha Vihren i ide ka grebenu Končeto. Zatim sledi uspon na vrh Banski Suhodol (2.884 mnv), preko sajlama osiguranog veoma atraktivnog grebena Končeto, a zatim na vrhove Kutelo (2.908 mnv) i Kutelo 2. -
The Unknown Southernmost Glaciers of Europe the Unknown Southernmost Glaciers of Europe
DOI: 10.5772/intechopen.68899 Provisional chapter Chapter 4 The Unknown Southernmost Glaciers of Europe The Unknown Southernmost Glaciers of Europe Emil Gachev Emil Gachev Additional information is available at the end of the chapter Additional information is available at the end of the chapter http://dx.doi.org/10.5772/intechopen.68899 Abstract This chapter presents the perennial firn/ice patches in the mountains of the Balkan Peninsula. The detailed study of these features in the last decades has proved that many of them are, in fact, small glaciers. They have survived without complete melting since the end of the Little Ice Age, and thus the time of their formation must have not later than in 14–15th century AD. At present, the existence of 16 small glaciers is suggested (and proved for some of them) in three mountains throughout the peninsula: Prokletije (mainly in Albania), Durmitor (in Montenegro) and Pirin (in Bulgaria), the biggest num- ber being found in Prokletije. The two small glaciers (glacierets) in Pirin mountain are at present the southernmost glacial masses in Europe (the only located south of 42°N). Despite the registered warming of high mountain climate, small glaciers on the Balkan Peninsula have shown no trends towards shrinkage for the last 23 years. Keywords: small glaciers, snow patches, Pirin, Durmitor, Prokletije 1. Introduction Few mountains in Europe host classical glaciers at present: The Alps, the Great Caucasus range, the Scandinavian mountains, Polar Ural and the Pyrenees [1]. Apart from them, there are numerous small bodies of firn and ice in other mountain ranges across Europe which are still of a permanent character, with their mass moving down by gravity. -
The Unknown Southernmost Glaciers of Europe
Chapter 4 The Unknown Southernmost Glaciers of Europe Emil Gachev Emil Gachev Additional information is available at the end of the chapter Additional information is available at the end of the chapter http://dx.doi.org/10.5772/intechopen.68899 Abstract This chapter presents the perennial firn/ice patches in the mountains of the Balkan Peninsula. The detailed study of these features in the last decades has proved that many of them are, in fact, small glaciers. They have survived without complete melting since the end of the Little Ice Age, and thus the time of their formation must have not later than in 14–15th century AD. At present, the existence of 16 small glaciers is suggested (and proved for some of them) in three mountains throughout the peninsula: Prokletije (mainly in Albania), Durmitor (in Montenegro) and Pirin (in Bulgaria), the biggest num- ber being found in Prokletije. The two small glaciers (glacierets) in Pirin mountain are at present the southernmost glacial masses in Europe (the only located south of 42°N). Despite the registered warming of high mountain climate, small glaciers on the Balkan Peninsula have shown no trends towards shrinkage for the last 23 years. Keywords: small glaciers, snow patches, Pirin, Durmitor, Prokletije 1. Introduction Few mountains in Europe host classical glaciers at present: The Alps, the Great Caucasus range, the Scandinavian mountains, Polar Ural and the Pyrenees [1]. Apart from them, there are numerous small bodies of firn and ice in other mountain ranges across Europe which are still of a permanent character, with their mass moving down by gravity. -
MIT SUMMIT from Skiing, Snowboarding and Mountaineering Experiences
Bulgaria boasts the full range of terrains, landscapes and opportunities for adventure any outdoor enthusiast may dream of. Mountains rising over 2,900 m, more FROM SUMMIT than 200 mountain lodges and over 300 alpine lakes, clearwater rivers and canyons, tens of thousands of kilometres of marked hiking trails, a well-developed system of TO SEA protected areas, and more than 300 km of coastline. ADVENTURE TRAVEL ADVENTURE TRAVEL ADVENTURE Every time of the year brings new adventure. In spring we open the rafting, kayaking and FOUR canyoning season along high-water rivers, we climb old and new routes, we marvel at the sheer scale of bird migration, and we pitch camp for a long, nine-month season that’s also great for SEASONS cycling throughout. In summer we hike through cool ancient forests, we balance on challenging rocky arêtes, we fly, we surf, we dive and enjoy plunging in water. In autumn we are still high up in the mountains, hiking and trekking, and we continue camping. Winter rewards us with great skiing, snowboarding and mountaineering experiences. bulgariatravel.org ADVENTURE TRAVEL bulgariatravel.org 360mag.bg hiking-bulgaria.com stenata.com 2021 ADVENTURE TRAVEL IN BULGARIA - AIR - CONTENTS 74 PARA-/ HANG GLIDING Sopot 75 SKYDIVING Montana - HIGHLIGHTS - 76 BUNGEE 6 FROM SEA TO SUMMIT 77 HOT-AIR BALLOONS FOUR SEASONS 8 - MOUNTAINS - - CYCLING - 32 NATURAL DIVERSITY 58 MARKED/TRACKED ROAD AND MOUNTAIN BIKE ROUTES 34 MOUNTAIN LODGES AND SPORTS CENTRES Rudopia Belmeken High-Altitude Sports Complex Trans- Rhodope Bike Trail Malyovitsa -
Second Circular 10 IAG/AIG SEDIBUD (Sediment Budgets in Cold
Second Circular 10th I.A.G./A.I.G. SEDIBUD (Sediment Budgets in Cold Environments) Workshop MONITORING OF GEOMORPHOLOGICAL PROCESSES IN COLD ENVIRONMENTS UNDER CLIMATE CHANGE – Bansko, Bulgaria, 7-10 September 2016 Global climate change concerns particularly the territories within the cryosphere margins - high-latitude and high-altitude regions from high arctic/antarctic and subarctic/subantarctic to alpine and upland sites. Especially in such cold areas the geomorphic responses are extremely fast and the climate oscillations intensify hazardous processes. Vihren and Kutelo peaks (view from Todorka peak) The 10th I.A.G./A.I.G. SEDIBUD (Sediment Budgets in Cold Environments) Workshop will take place in Bansko ski resort (925 m a.s.l.) at the foot of the Pirin Mountains, Bulgaria. In order to introduce you to the work of the Bulgarian team and to the characteristics of this region, we propose a one-day field trip. The field trip will take place in the area of Vihren peak (2914 m) with the Banderitsa valley and the double cirque Kazanite – crossing the subalpine and the alpine belt of Pirin and observing fossil glacial, nival, slope, fluvial and karst processes. In the Balkans high mountain area remnants from the Pleistocene glaciations can be observed and the related landforms are modified by the contemporary warmer conditions (and by the climate oscillations during the Holocene period). Frost and nival activity have a high importance in the contemporarily unglacierized alpine area. Studies on sedimentary fluxes and budgets must consider the influences of the past glacial and the paraglacial processes. This kind of geomorphological investigations has never before been conducted in this area and the results (from 2011-2012 and ongoing) that will be presented are the first for the country. -
High Mountain Relief in Marble in Pirin Mountains, Bulgaria: Structure, Specifics and Evolution
REVISTA DE GEOMORFOLOGIE (2017) 19: 118–135 DOI 10.21094/rg.2017.012 www.geomorfologie.ro, http://revistadegeomorfologie.ro High mountain relief in marble in Pirin Mountains, Bulgaria: structure, specifics and evolution Emil GACHEV1* 1South-West University “Neofit Rilski”, Blagoevgrad, Bulgaria Received 25 October 2017; Revised 15 November 2017; Accepted 1 December 2017 *Correspondence to: Emil GACHEV, e-mail: [email protected] ABSTRACT The present article is focused on high mountain relief in marble, which combines glacial, periglacial and karstic morphology. High mountain karst is found in Northern Pirin (Vihren and Sinanitsa area) and central Pirin (Orelek area), the latter lacking traces of glaciation due to its low altitude. In the most representative area, Vihren part, several vast and deep cirques-uvalas were formed, which comprise a large diversity of landforms. Main factor for the specifics of relief in marble is the structure of the rock, which combines carbonate mineral content and crystalline properties; they favour both the occurrence of karstification and frost weathering. The high elevation of Northern Pirin (up to 2914 m a.s.l.), and the resulting extensive former glaciation enhanced the karst processes by weathering of the morphological surface. At present, surface karst is most developed on elevated sections of cirque bottoms, which were ice free before the beginning of the Holocene and are away from rockfall creep accumulation. A special element of glaciokarstic relief in Pirin are the summer lasting snow/ice features (glacierets and snow patches), two of which are considered centuries old, and still survive despite the temperature warming. In general, karst processes in the high mountain areas of Pirin are less developed than in the western part of the Balkan Peninsula (the Dinarides), due to the greater susceptibility of marble to physical weathering compared to limestone, which leads to a more intensive formation of regolith on the surface, and in result of the generally colder and dryer climate. -
Pirin National Park
WHC Nomination Documentation File name: 225.pdf UNESCO Region EUROPE SITE NAME ("TITLE") Pirin National Park DATE OF INSCRIPTION ("SUBJECT") 9/12/1983 STATE PARTY ("AUTHOR") BULGARIA CRITERIA ("KEY WORDS") N (i)(ii)(iii) DECISION OF THE WORLD HERITAGE COMMITTEE: The Committee mad no statement. BRIEF DESCRIPTION: The park has a limestone Balkan landscape, with its lakes, waterfalls, caves and pine forests, and a rich flora containing many endemic plant species. The rugged mountains, with around seventy glacial lakes scattered throughout them, are a relic of the ancient glacial days of Europe. 1.b. State, province or region: County of Blagoevgrad 1.d Exact location: South West Bulgaria, Pirin Mountain Pirin National Park Republic of Bulgaria Nomination for changes in the boundaries of Pirin National Park as Natural World Heritage Property 2009 Ministry of Environment and Water Pirin National Park Directorate Table of content EXECUTIVE SUMMARY 4 1. IDENTIFICATION OF THE PROPERTY 10 2. DESCRIPTION 16 3. JUSTIFICATION FOR INSCRIPTION 27 Criterion VII 27 Criterion IX 28 Criterion X 30 4. STATE OF CONSERVATION AND FACTORS AFFECTING THE PROPERTY 35 5. PROTECTION AND MANAGEMENT OF THE PROPERTY 43 6. MONITORING 58 7. DOCUMENTATION 61 8. CONTACT INFORMATION 64 9. SIGNATURE ON BEHALF OF THE STATE PARTY 66 Pirin WHS Nomination 2009 2 Acronyms CC Consultative Council EEA Environmental Executive Agency GIS Geographic Information System IBA Important Bird Area IPA Important Plant Area MAB UNESCO Man and Biosphere Programme MoEW Ministry of Environment -
Abbreviations
Abbreviations AD (Anno Domini) AMS (Accelerator Mass Spectrometry) a.s.l. (above sea level) BAN (Bulgarian Academy of Sciences) BC (Before Christ) BP (Before Present) CRU (Climate Research Unit, University of East Anglia) DBH (Diameter at Breast Hight) ELA (Equilibrium Line Altitude) ENSO (El Niño and the Southern Oscillation) EPS (Expressed Population Signal) GCM (General Circulation Model) GIS (Geographical Information System) GPR (Ground Penetrating Radar) GPS (Global Positioning System) IPCC (Intergovernmental Panel on Climate Change) ITCZ (Intertropical Convergence Zone) IUCN (International Union for Conservation of Nature) LGM (Last Glacier Maximum) LIA (Little Ice Age) MDI (Multivariate Dating Index) NAO (North Atlantic Oscillation) NIMH (National Institute of Meteorology and Hydrology) NP (National Park) PDSI (Palmer Drought Severity Index) Rbar (Interseries Correlation) SD (Standard Deviation) SOM (Soil Organic Matter) SPI (Standardized Precipitation Index) TRA (Tree-Ring Analyser) TRW (Tree-Ring-Width) WGMS (World Glacier Monitoring Service) 149 Geographical Features A G Albanian Alps (Mts.), 78 Glazne (river), 19 Golemya Kazan (cirque), 23, 34–37, 39, 44, 46, 65–67, 77, 80 B Golyamo and Malko Spano Pole (meadow), 15 Banderica (river, cirque), 15, 17, 19–21, 34, Gotse Delchev (town), 50, 51, 53–56 35, 37, 40, 47, 97 Banderizhka Polyana (meadow), 15 Banderizhki Suhodol (cirque, dry-valley), 15 H Banderizhko (lake), 37 Hadzhidimovo (town), 56 Banski Suhodol (cirque, dry-valley), 39, 76, 77 Bansko (town), 15, 19, 23, 27, 28, 50, -
Viaje a Bulgaria Senderismo Y Cultura a La Sombra De Los
VIAJE A BULGARIA VERANO 2016 SENDERISMO Y CULTURA A LA SOMBRA DE LOS BALCANES Irungo Mendizaleal 2016 IRUNGO MENDIZALEAK BULGARIA MAPA INTRODUCCIÓN En este viaje tendremos la oportunidad de conocer los lugares de interés cultural más importantes del país, así como caminar por los principales macizos (Rila, Pirin y Balcanes Centrales) y subir las montañas más representativas, incluyendo las dos cimas más altas de Bulgaria, el Vihren (2914 m) y el Musala (2925 m). Durante nuestro circuito pasaremos por varios sitios de la UNESCO, los 3 monasterios más importantes del país, ciudades cosmopolitas y pueblos perdidos en los montes. El viajero podrá disfrutar de curiosos y pintorescos sitios naturales junto con los sitios más espirituales al pie de las IRUNGO MENDIZALEAK BULGARIA montañas. Esta es una oportunidad perfecta para ver y sentir todas las caras de Bulgaria: el ambiente más moderno y los rincones más remotos, los sitios naturales mejores preservados y los pueblos auténticos, siempre acompañados por la hospitalidad de los búlgaros. ITINERARIO Día 1: Vuelo a Sofía Salida en vuelo con destino a Sofia. Llegada a Sofia, asistencia en el aeropuerto y traslado a nuestro hotel. Cena de bienvenida en taberna con productos locales. Noche en hotel céntrico 4*. Día 2. Monte Vitosha - Sofía Por la mañana traslado hasta las faldas del monte Vitosha. Visita al monasterio de Dragalevski y caminata de unas 2:30 horas recorriendo los bonitos bosques caducifolios (mayoritariamente hayedos) con vistas panorámicas a la ciudad. Llegada al pueblo de Boyana y visita a su iglesia con frescos del S.X-XIII declarados patrimonio de la UNESCO. -
Karstification in the Mountains Durmitor (Montenegro) and Pirin (Bulgaria) and Its Expression in Surface Landforms
Karstification in the mountains Durmitor (Montenegro) and Pirin (Bulgaria) and its expression in surface landforms Emil Gachev, Ilia Mitkov South-west University “Neofit Rilski” Blagoevgrad, Bulgaria Abstract— The present study makes a comparison of the development of karstic processes and their landform expression in two representative high mountain areas on the Balkan Peninsula: Durmitor (Dinaric chain, Montenegro) and Pirin (Rhodope massif, Bulgaria). Main accent is put on epikarst and its features. On the background of many similarities: strong glaciation in the Pleistocene, pronounced cirques and arêtes, preserved moraine deposits, rough present-day topography, some obvious differences are observed. These are mostly derived by the differences in carbonate bedrock (limestone in Durmitor and marble in Pirin), and climate (damp to the west and drier to the east). The tectonic setting is also important. Such a comparison has not been done so far. It would contribute to obtain a better Fig. 1. Areas with high mountain karst on the Balkan Peninsula, and regional outlook on the processes in the high mountain sites ofthe study. karstic areas in Southeastern Europe. Keywords— high mountain karst; Northern Pirin; Balkan II. STUDY SITES Peninsula A. Geographical location I. INTRODUCTION Durmitor is situated in northwest Montenegro. This is the second highest massif in the Dinaric chain (after Karst processes generate a distinct type of environment, Prokletije in northern Albania), part of the central range, which is clearly distinguishable on the field. Apart from reaching to 2522 m (Bobotovkuk peak). This mountain is their high aesthetic attractiveness, karst areas are important small, but sharply distinct: it rises abruptly over 1000 m for the formation of water resources and biodiversity.