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Wyszukujesz frazę "Pirin Mountains" wg kryterium: Temat


Wyświetlanie 1-3 z 3
Tytuł:
Macromycetes in the Pirin Mts (SW Bulgaria)
Autorzy:
Denchev, C.M.
Fakirova, V.I.
Gyosheva, M.M.
Petrova, R.D.
Powiązania:
https://bibliotekanauki.pl/articles/67341.pdf
Data publikacji:
2007
Wydawca:
Polskie Towarzystwo Botaniczne
Tematy:
macromycete
Pirin Mountains
Bulgaria
fungal diversity
Pirin National Park
Opis:
This paper attempts to compile available and unpublished data on the macromycetes of the Pirin Mts. The total number of currently known species is 350, including 34 ascomycetes and 316 basidiomycetes. Among them, 60 species are reported for the first time for the Pirin Mts, including Inocybe pisciodora which is a new record for Bulgaria.The species composition, ecological-trophic structure, and economically important edible fungi are briefly discussed. A list of 25 macroscopic fungi of conservation significance for the mycota of this mountain, evaluated with the recent IUCN criteria, is given, including 4 Critically Endangered, 9 Endangered, 7 Vulnerable, and 5 Near Threatened species.
Źródło:
Acta Mycologica; 2007, 42, 1
0001-625X
2353-074X
Pojawia się w:
Acta Mycologica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Present state of Bulgarian glacierets
Autorzy:
Gachev, E.
Gikov, A.
Zlatinova, C.
Blagoev, B.
Powiązania:
https://bibliotekanauki.pl/articles/294843.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
Pirin Mountains
glacierets
inter-annual dynamics
climate fluctuations
Opis:
he present article makes a revision of the recent studies related to Bulgarian glacierets, all located in the northern part of the Pirin Mountains, as well as presents some latest results from field measurements of firn size and morphology descriptions. This has been the first scientific study of Banski suhodol glacieret, which at present is the largest in Bulgaria. Data gained until now indicates differences between the Pirin and the High Tatras concerning the driving factors of glacieret inter-annual dynamics, as for Bulgarian glacierets air temperature appears to be one of the most sufficient controls.
Źródło:
Landform Analysis; 2009, 11; 16-24
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Relief transformation along footpaths in the Rila, Pirin, and Western Tatra Mountains
Autorzy:
Buchwał, A.
Fidelus, J.
Rogowski, M.
Powiązania:
https://bibliotekanauki.pl/articles/294895.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
Rila Mountains
Pirin Mountain
Western Tatras Mountains
footpaths erosion
relief transformation along
Opis:
High mountain areas are characterized by substantial geodiversity and different morphogenetic processes play a key role in shaping their relief. One of the most transformed landforms within the high mountain areas affected by such processes today are footpaths and tourist trails. For this reason, this issue needs to be closely examined for a variety of mountains ranges. The main aim of the research was to characterize effects of changes in relief experienced by footpaths and their vicinity in three different high-mountain regions: the Rila Mts., the Pirin Mts, and the Western Tatra Mts. Geomorphological mapping was used to study the erosive relief in details. The comparative analysis of geomorphological effects of relief transformation along surveyed footpaths allow for the determination of regularities in landform formation. In the Tatra Mountains, the footpaths experiencing the highest degree of physical transformation are those running along the slope gradient and across eroded rock debris zones, with little or no turf. Such paths create favourable conditions for erosion to produce deep incisions, the depth of which can reach one metre. In the case of the Rila and Pirin Mountains, the deepest incisions reach 1.8 m. Research has shown that among the different forms of human impact the great amount of pressure on relief in high mountain areas is exerted by pastoral activity and forest management practices.
Źródło:
Landform Analysis; 2009, 10; 18-25
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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