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Original scientific paper

MORPHOGRAPHIC-MORPHOSTRUCTURAL INVESTIGATIONS OF VELEBIT ON THE BASIS OF ORBITAL COLOURED PHOTOGRAPH M 1:200.000 WITH SPECIAL REGARD TO THE RUTS OF PALEOSTREAMS

VILKO KLEIN

Fulltext: croatian, pdf (2 MB) pages 1-17 downloads: 639* cite
APA 6th Edition
KLEIN, V. (1996). MORFOGRAFSKO-MORFOSTRUKTURNO PROUČAVANJE VELEBITA NA OSNOVI ORBITALNE SNIMKE U BOJI M 1:200.000 S POSEBNIM OSVRTOM NA TRAGOVE PALEOTEKUĆICA. Senjski zbornik, 23 (1), 1-17. Retrieved from https://hrcak.srce.hr/43568
MLA 8th Edition
KLEIN, VILKO. "MORFOGRAFSKO-MORFOSTRUKTURNO PROUČAVANJE VELEBITA NA OSNOVI ORBITALNE SNIMKE U BOJI M 1:200.000 S POSEBNIM OSVRTOM NA TRAGOVE PALEOTEKUĆICA." Senjski zbornik, vol. 23, no. 1, 1996, pp. 1-17. https://hrcak.srce.hr/43568. Accessed 1 Apr. 2020.
Chicago 17th Edition
KLEIN, VILKO. "MORFOGRAFSKO-MORFOSTRUKTURNO PROUČAVANJE VELEBITA NA OSNOVI ORBITALNE SNIMKE U BOJI M 1:200.000 S POSEBNIM OSVRTOM NA TRAGOVE PALEOTEKUĆICA." Senjski zbornik 23, no. 1 (1996): 1-17. https://hrcak.srce.hr/43568
Harvard
KLEIN, V. (1996). 'MORFOGRAFSKO-MORFOSTRUKTURNO PROUČAVANJE VELEBITA NA OSNOVI ORBITALNE SNIMKE U BOJI M 1:200.000 S POSEBNIM OSVRTOM NA TRAGOVE PALEOTEKUĆICA', Senjski zbornik, 23(1), pp. 1-17. Available at: https://hrcak.srce.hr/43568 (Accessed 01 April 2020)
Vancouver
KLEIN V. MORFOGRAFSKO-MORFOSTRUKTURNO PROUČAVANJE VELEBITA NA OSNOVI ORBITALNE SNIMKE U BOJI M 1:200.000 S POSEBNIM OSVRTOM NA TRAGOVE PALEOTEKUĆICA. Senjski zbornik [Internet]. 1996 [cited 2020 April 01];23(1):1-17. Available from: https://hrcak.srce.hr/43568
IEEE
V. KLEIN, "MORFOGRAFSKO-MORFOSTRUKTURNO PROUČAVANJE VELEBITA NA OSNOVI ORBITALNE SNIMKE U BOJI M 1:200.000 S POSEBNIM OSVRTOM NA TRAGOVE PALEOTEKUĆICA", Senjski zbornik, vol.23, no. 1, pp. 1-17, 1996. [Online]. Available: https://hrcak.srce.hr/43568. [Accessed: 01 April 2020]

Abstracts
In this work the autor deals with morphographic-morphostructural division of the mountain of Velebit by means of the coloured orbital photograph M 1:200.000. The most important seems to be bipartite rcsp. quadripartite transversal division of the mountain and the
phenomenon of its cuneiform morphographic structure. A lot of ruts of the arch-bent elements of an old valley-net rcsp. of paleostream beds can be noted there. It all suggests that a great number
of streams was running through the present-day high mountain residual plateau of Velebit some time in its geological past. It was the time when mountain was a part of its and that of Lika's
lower laid and more extensive plateau. The separated arch characteristics of the relief reconfirm the presence of annular structures outlined spherically or ovaly. They so seem to be further particularity of the morphostructural pattern of Velebit. Likewise, the possibility of fractal analysis of the chaotically arranged relief
elements of Velebit has been pointed out.

Keywords
morphographic-morphostructural investigations; Velebit; orbital coloured photograph; paleostreams

Hrčak ID: 43568

URI
https://hrcak.srce.hr/43568

[croatian] [german]

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