Thufur morphology within the Ponor depression (Stara Planina, Serbia)

Author:

Milosevic Marko1ORCID,Calic Jelena2ORCID,Kovacevic-Majkic Jelena2ORCID,Milivojevic Milovan2

Affiliation:

1. m.milosevic@gi.sanu.ac.rs

2. Geographical Institute “Jovan Cvijić” SASA, Belgrade, Serbia

Abstract

Thufur (earth hummocks) are small periglacial landforms typical for subpolar latitudes, as well as for the high alpine areas at lower latitudes. Their presence in the mountains of the Balkan Peninsula was spotted during the mid-20th century. In this paper we analyze morphometry and morphology of thufur in the context of physio-geographical conditions for their formation. The main aims are to inventorize the thufur in the study area and to determine the physio-geographical factors which enabled their formation at non-zonal elevations. Statistical analysis was performed on the sample of 305 thufur mapped in the field, measuring their circumference, height, and delineating their areas. Classification of the results revealed morphological varieties in terms of horizontal and vertical development. The elevation of the sampling location Ponor is 1,410 m a.s.l., which is considerably lower than the zonal periglaciation in Serbia, at approx. 1,900 m. Therefore, the role of relief as a climate modifier is analyzed in the context of conditions for the azonal development of periglaciation process. Topographical conditions for thufur formation were analyzed through slope inclinations and vertical dissection, determined using the Digital Elevation Model over Europe with 25 m resolution.

Funder

Ministry of Education, Science and Technological Development of the Republic of Serbia

Publisher

National Library of Serbia

Subject

Geology,Geography, Planning and Development,Earth-Surface Processes,Demography,Tourism, Leisure and Hospitality Management

Reference46 articles.

1. Anđelković, J., Krstić, B., Ćirić, A., Martinović, D., & Bogdanović, P. (1975). Osnovna geološka karta SFRJ 1:100000: List K 34-34, Pirot [Basic Geological Map SFRY 1:100000: Sheet K 34-34, Pirot]. Savezni geološki zavod, Beograd.

2. Belij, S. (1990). Tufuri na Maja Rusoliji [Thufur on Mt. Maja Rusolija]. In K. Natek (Ed.), Geomorfologija in geoekologija: Zbornik referatov 5. znanstvenega posvetovanja geomorfologov Jugoslavije, Krško, 18. do 23. junij 1990 [Geomorphology and Geoecology: Proceedings of the 5th Scientific Meeting of Yugoslav geomorphologists, Krško, 1990, Jun 18-23] (pp. 149-163). Znanstvenoraziskovalni center SAZU.

3. Belij, S. (1992). Savremeni geomorfološki procesi u kriosferi severoistočne Šar-planine [Recent geomorphological processes on the cryosphere of the north-east Šara-mountain]. Bulletin of the Serbian Geographical Society, 62(1), 13-24. http://www.digitalna.nb.rs/view/URN:NB:RS:SD_009D9B E9B60FF0ED17AA71C7413495B7-1992-B072

4. Belij, S. (1994). Savremeni periglacijalni procesi i oblici reljefa severozapadne Šar planine [Contemporary periglacial processes and relief forms on the SW part of Šara Mountain]. In R. Lazarević (Ed.), Šarplaninske župe Gora, Opolje i Sredska: Odlike prirodne sredine (Posebna izdanja, Knjiga 41/1) [Šara mountain Župas Gora, Opolje and Sredska: Trait of Natural Environment (Special editions, Book 47/1)] (pp. 41-63). Geografski institut „Jovan Cvijić” SANU.

5. Belij, S., Ducić, V., Milovanović, B., Luković, J., & Miščević, I. (2004). Mrazne travne humke - tufuri na obodu Pešterskog polja [Frosted grass mounds - thufurs on the Pešter peripheral area]. Protection of Nature, 55(1-2), 17-26. http://www.zzps.rs/wp/casopisi_pdf/006/casopis.pdf?script=lat

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3