Zobrazeno 1 - 10
of 66
pro vyhledávání: '"ANDRIJA BOGNAR"'
Autor:
Andrija Bognar, Ivančica Prugovečki
Publikováno v:
Geologia Croatica, Vol 50, Iss 2, Pp 269-278 (2010)
The area of the Risnjak mountain massif is a submorphologicalregion - part of the mesomorphological region of the south-westernGorski Kotar. This area exceeds 1,500 metres in height. In the reliefstructure of the massif, the system of ranges and eros
Externí odkaz:
https://doaj.org/article/8d82dda1a6ed4f8f9bce8cd06bd45d6c
Autor:
Helena Ilona Bognar, Andrija Bognar
Publikováno v:
Geoadria, Vol 15, Iss 1, Pp 187-224 (2010)
Although natural basis cannot be a decisive criterion in defining borders, historical and politico-geographic development of the researched area reveals that natural bounds have been considerably used in the boundary demarcation between the Republic
Externí odkaz:
https://doaj.org/article/63568edf972945988478e493b91bcc10
Autor:
Helena Ilona Bognar, Andrija Bognar
Publikováno v:
Geoadria, Vol 15, Iss 1, Pp 187-224 (2010)
Iako prirodna osnova ne može biti odlučujući kriterij pri povlačenju granica, povijesni i političko-geografski razvoj istraživanog područja ukazuje da su pri razgraničenju Republike Hrvatske i Republike Slovenije u znatnoj mjeri korištene pr
Externí odkaz:
https://doaj.org/article/5c3a8af57fad42ddb0555839f5d60f6c
Autor:
Andrija Bognar
Publikováno v:
Dela, Iss 20, Pp 61-64 (2003)
V prispevku je predstavljena pomembna vloga, ki jo je imel akademik Ivan Gams pri preusmeritvi in posodobitvi hrvaške geomorfologije v 70. in 80. letih 20. stoletja. Predstavljeni so vzroki, zakaj je hrvaška geomorfologija v preteklosti izgubila st
Externí odkaz:
https://doaj.org/article/497dcc0c123247fc9f327962f964d844
Autor:
Andrija Bognar
Publikováno v:
Dela, Iss 16, Pp 61-72 (2001)
Stoletja stara slovensko-hrvaška meja je v glavnem naravna, poteka po rekah in gorskih slemenih. To opredeljuje tudi organizacijo življenja v obmejnih območjih. Nova meja to tudi potrjuje, je odraz trenutnih odnosov, moči in interesov, kar ustvar
Externí odkaz:
https://doaj.org/article/90ddaa3952fa4e508f705241b43f40d9
Publikováno v:
Geoadria, Vol 7, Iss 2, Pp 23-34 (2002)
The Baške Oštarije karst polje is stretching out at the direction E - W at lenght of 3,75 km, while the width is varying from 0,25 to 2,0 km. It divides central from the south part of the Velebit mountain and it is formed at the contact of two orog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4d8979a41fea0824246550f830f63783
https://doi.org/10.15291/geoadria.87
https://doi.org/10.15291/geoadria.87
Geomorphological Traces of the Younger Pleistocene Glaciation in the Central Part of the Velebit Mt.
Autor:
Andrija, Bognar1 abognar@geog.pmf.hr, Sanja, Faivre2 sfaivre@geog.pmf.hr
Publikováno v:
Croatian Geographical / Hrvatski Geografski Glasnik. 2006, Vol. 68 Issue 2, p19-30. 12p.
Autor:
Andrija Bognar, Helena Ilona Bognar
Publikováno v:
Geoadria, Vol 15, Iss 1, Pp 187-224 (2010)
Although natural basis cannot be a decisive criterion in defining borders, historical and politico-geographic development of the researched area reveals that natural bounds have been considerably used in the boundary demarcation between the Republic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::45a91a03bc8963d94596f1475d669c3f
http://hrcak.srce.hr/file/84077
http://hrcak.srce.hr/file/84077
Autor:
Andrija Bognar
Publikováno v:
Hrvatski geografski glasnik/Croatian Geographical Bulletin. 70:49-71
Geomorphologic characteristics and development of the Drava River bed (108-115 km from the mouth) and its floodplain will be analyzed. The emphasis will be put on the river bed and floodplain morphogenesis in the last two centuries, when the most sig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a5b4d117fc87ffc169318820207e510
https://doi.org/10.21861/hgg.2008.70.02.03
https://doi.org/10.21861/hgg.2008.70.02.03
Autor:
Sanja Faivre, Andrija Bognar
Publikováno v:
Hrvatski geografski glasnik
Volume 68.
Issue 2.
Volume 68.
Issue 2.
On the central part of the Velebit Mountain the traces of the Pleistocene glaciation have been found. The domination of the dissected relief, characterized by numerous elevations and depressions, in the conditions of low temperatures and richness of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ab100c45fd20dd7e700433f4f56d930b
https://doi.org/10.21861/hgg.2006.68.02.02
https://doi.org/10.21861/hgg.2006.68.02.02