Serbia can be divided into two major geographical units: the Vojvodina Plain and the southern hills and mountains. In the plain fluvial and aeolian processes and landforms on loess are typical, while south of the Sava and Danube rivers, sheet and gully erosion, mass movements, fluvial, karstic, and fluvio-karstic landform evolution are most influential in shaping the present topography. Among the now inactive geomorphic processes tectonic movements, volcanic activity, coastal, glacial, and aeolian evolution have left behind traces still detectable in modern topography. Some examples of rapid topographic change resulting in the most spectacular landforms (landslides, rockfalls, natural bridges, and rock pinnacles) are presented and described in detail from various regions of Serbia.
Keywords:
Deluvial-proluvial processes / Fluvial processes / Glacial features / Karst / Landslides / Natural bridges / Rock pinnacles / Rockfall
Source:
Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region, 2012, 345-375
TY - CHAP
AU - Pavlović, R.
AU - Ćalić, Jelena
AU - Đurović, Predrag
AU - Trivić, B.
AU - Jemcov, I.
PY - 2012
UR - https://gery.gef.bg.ac.rs/handle/123456789/458
AB - Serbia can be divided into two major geographical units: the Vojvodina Plain and the southern hills and mountains. In the plain fluvial and aeolian processes and landforms on loess are typical, while south of the Sava and Danube rivers, sheet and gully erosion, mass movements, fluvial, karstic, and fluvio-karstic landform evolution are most influential in shaping the present topography. Among the now inactive geomorphic processes tectonic movements, volcanic activity, coastal, glacial, and aeolian evolution have left behind traces still detectable in modern topography. Some examples of rapid topographic change resulting in the most spectacular landforms (landslides, rockfalls, natural bridges, and rock pinnacles) are presented and described in detail from various regions of Serbia.
PB - Springer Netherlands
T2 - Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region
T1 - Recent landform evolution in Serbia
SP - 345
EP - 375
DO - 10.1007/978-94-007-2448-8_13
UR - https://hdl.handle.net/21.15107/rcub_gery_458
ER -
@inbook{
author = "Pavlović, R. and Ćalić, Jelena and Đurović, Predrag and Trivić, B. and Jemcov, I.",
year = "2012",
abstract = "Serbia can be divided into two major geographical units: the Vojvodina Plain and the southern hills and mountains. In the plain fluvial and aeolian processes and landforms on loess are typical, while south of the Sava and Danube rivers, sheet and gully erosion, mass movements, fluvial, karstic, and fluvio-karstic landform evolution are most influential in shaping the present topography. Among the now inactive geomorphic processes tectonic movements, volcanic activity, coastal, glacial, and aeolian evolution have left behind traces still detectable in modern topography. Some examples of rapid topographic change resulting in the most spectacular landforms (landslides, rockfalls, natural bridges, and rock pinnacles) are presented and described in detail from various regions of Serbia.",
publisher = "Springer Netherlands",
journal = "Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region",
booktitle = "Recent landform evolution in Serbia",
pages = "345-375",
doi = "10.1007/978-94-007-2448-8_13",
url = "https://hdl.handle.net/21.15107/rcub_gery_458"
}
Pavlović, R., Ćalić, J., Đurović, P., Trivić, B.,& Jemcov, I.. (2012). Recent landform evolution in Serbia. in Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region
Springer Netherlands., 345-375.
https://doi.org/10.1007/978-94-007-2448-8_13
https://hdl.handle.net/21.15107/rcub_gery_458
Pavlović R, Ćalić J, Đurović P, Trivić B, Jemcov I. Recent landform evolution in Serbia. in Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region. 2012;:345-375.
doi:10.1007/978-94-007-2448-8_13
https://hdl.handle.net/21.15107/rcub_gery_458 .
Pavlović, R., Ćalić, Jelena, Đurović, Predrag, Trivić, B., Jemcov, I., "Recent landform evolution in Serbia" in Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region (2012):345-375,
https://doi.org/10.1007/978-94-007-2448-8_13 .,
https://hdl.handle.net/21.15107/rcub_gery_458 .
