Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Emil Gachev"'
Publikováno v:
Journal of the Bulgarian Geographical Society, Vol 50, Iss , Pp 75-94 (2024)
Several perennial snow and ice bodies have been recently studied and monitored in three mountain massifs across the Balkan Peninsula: Prokletije (Northern Albania), Durmitor (Montenegro) and Pirin (Bulgaria), the two glacierets in the Pirin Mountains
Externí odkaz:
https://doaj.org/article/87033f3f8d994111b8da71d2da101383
Autor:
Emil Gachev
Publikováno v:
Journal of the Bulgarian Geographical Society, Vol 44, Iss , Pp 39-47 (2021)
Periglacial landforms are typical features of the high mountain environment on the Balkan Peninsula. Their formation and diversity is determined by climatic, topographic and geological factors. Presently active periglacial processes occur above 1700-
Externí odkaz:
https://doaj.org/article/e34525dc504e46279269ec97bc4416b9
Autor:
Emil GACHEV
Publikováno v:
Revista de Geomorfologie, Vol 19, Iss 1 (2017)
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 lacki
Externí odkaz:
https://doaj.org/article/9e655a6e7dfe4c0d879011436c2de5fe
Autor:
Emil Gachev
Publikováno v:
Acta geographica Slovenica. 60:191-211
This study presents results from regular observation of permanent and summer-persisting firn-ice bodies in the highest parts of the Dinaric Alps. The sizes of six small glaciers and two snow patches on the Prokletije Massif (in Albania) and the Durmi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::878957bb5666cea27997e90151b316bf
https://doi.org/10.3986/ags.8092
https://doi.org/10.3986/ags.8092
Autor:
Emil Gachev
Publikováno v:
Mediterranean Geoscience Reviews. 2:103-117
This study presents a review on Holocene glacial traces in Bulgaria. Pleistocene glaciation in this territory was spread over a number of mountains above 2000 m a. s. l., while in the later time, it was restricted only to the highest areas of the two
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::712e4226efde65a70973b0b7e8f5909e
https://doi.org/10.1007/s42990-020-00028-3
https://doi.org/10.1007/s42990-020-00028-3
Autor:
Emil Gachev
Publikováno v:
Revista de Geomorfologie, Vol 22, Iss 1 (2020)
Rock glaciers are lobate or tongue-shaped assemblages of poorly sorted, angular-rock debris and ice, commonly found in high mountain environments, which move as a consequence of the deformation of internal ice (Giardino and Vitek, 1988; Barsch, 1996)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1b837051f4cf9ffb03d3967a79d3cfdc
Publikováno v:
Quaternary International. 415:33-54
Mountain glaciers are among the best environmental indicators of short-term climatic variations. Although presently there are no classical glaciers on the Balkan Peninsula, mountains in this part of Europe comprise a number of small but permanent fir
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a0d1823568fe8510b1a7249a8c48f63a
https://doi.org/10.1016/j.quaint.2015.10.042
https://doi.org/10.1016/j.quaint.2015.10.042
Autor:
Mircea Voiculescu, Emil Gachev, Flavius Sîrbu, Florina Ardelean, Alexandru Onaca, Brigitte Magori, Adrian C. Ardelean
Publikováno v:
CATENA. 185:104288
The proposed research addresses the problem of permafrost occurrence for the first time in the highest mountains of the Balkan Peninsula. The likely/unlikely presence of ice-rich permafrost in 13 rock glaciers in the Rila and Pirin Mountains was inve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9d34b23fd949c3453852323deb933e0
https://doi.org/10.1016/j.catena.2019.104288
https://doi.org/10.1016/j.catena.2019.104288
Autor:
Emil Gachev
Publikováno v:
Glaciers Evolution in a Changing World
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ca7db69e5a67112840d2f6be26a509fe
https://doi.org/10.5772/intechopen.68899
https://doi.org/10.5772/intechopen.68899
Autor:
Emil Gachev, Ilia Mitkov
Publikováno v:
Proceedings of the 33rd Romanian Geomorphology Symposium.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74d34123b26db0d309f359b886d5aee9
https://doi.org/10.15551/prgs.2017.50
https://doi.org/10.15551/prgs.2017.50