Karstic uvala revisited: Toward a redefinition of the term
Abstract
Uvalas are a particular type of karst closed depression. While other types of closed depression – dolines and
poljes – are regularly listed and relatively well defined in overviews of karst surface morphology, uvalas are
either excluded or their vague identification is stressed. The leading idea of this paper is to obtain a clearer
meaning of the term uvala and prevent its abandonment from karstology and general geomorphology. Within
the study, 43 examples of uvalas have been selected. The studied uvalas are located in the Dinaric karst and
karst of the Carpatho–Balkanides. All the case examples have been digitally processed in the same way.
Creation of high-resolution digital elevation models enabled quantification of morphometric parameters,
generation of inclination maps and cross-sections, as well as application of statistical analyses. Formation of
the geographical information system of the studied uvalas was done using raster-based and vector-based GIS
software packages.... In 12 studied uvalas, detailed structural–geological mapping has been carried out, which
revealed dominant development of uvalas along regional scale tectonically broken zones. A revised definition
of the term uvala is suggested, leaving the opportunity for further discussion.
Keywords:
Karst surface morphology / Karst depression / Uvala / Dinaric karst / Carpatho-BalkanidesSource:
Geomorphology, 2011, 134, 32-42Publisher:
- Elsevier
Funding / projects:
- Geography of Serbia (RS-47007)
DOI: 10.1016/j.geomorph.2011.06.029
ISSN: 0169-555X
WoS: 000295655900004
Scopus: 2-s2.0-80052907983
Institution/Community
Географски институт „Јован Цвијић“ САНУ / Geographical Institute Jovan Cvijić SASATY - JOUR AU - Ćalić, Jelena PY - 2011 UR - https://dais.sanu.ac.rs/123456789/2272 AB - Uvalas are a particular type of karst closed depression. While other types of closed depression – dolines and poljes – are regularly listed and relatively well defined in overviews of karst surface morphology, uvalas are either excluded or their vague identification is stressed. The leading idea of this paper is to obtain a clearer meaning of the term uvala and prevent its abandonment from karstology and general geomorphology. Within the study, 43 examples of uvalas have been selected. The studied uvalas are located in the Dinaric karst and karst of the Carpatho–Balkanides. All the case examples have been digitally processed in the same way. Creation of high-resolution digital elevation models enabled quantification of morphometric parameters, generation of inclination maps and cross-sections, as well as application of statistical analyses. Formation of the geographical information system of the studied uvalas was done using raster-based and vector-based GIS software packages. In 12 studied uvalas, detailed structural–geological mapping has been carried out, which revealed dominant development of uvalas along regional scale tectonically broken zones. A revised definition of the term uvala is suggested, leaving the opportunity for further discussion. PB - Elsevier T2 - Geomorphology T1 - Karstic uvala revisited: Toward a redefinition of the term SP - 32 EP - 42 IS - 134 IS - 1-2 DO - 10.1016/j.geomorph.2011.06.029 UR - https://hdl.handle.net/21.15107/rcub_dais_2272 ER -
@article{ author = "Ćalić, Jelena", year = "2011", abstract = "Uvalas are a particular type of karst closed depression. While other types of closed depression – dolines and poljes – are regularly listed and relatively well defined in overviews of karst surface morphology, uvalas are either excluded or their vague identification is stressed. The leading idea of this paper is to obtain a clearer meaning of the term uvala and prevent its abandonment from karstology and general geomorphology. Within the study, 43 examples of uvalas have been selected. The studied uvalas are located in the Dinaric karst and karst of the Carpatho–Balkanides. All the case examples have been digitally processed in the same way. Creation of high-resolution digital elevation models enabled quantification of morphometric parameters, generation of inclination maps and cross-sections, as well as application of statistical analyses. Formation of the geographical information system of the studied uvalas was done using raster-based and vector-based GIS software packages. In 12 studied uvalas, detailed structural–geological mapping has been carried out, which revealed dominant development of uvalas along regional scale tectonically broken zones. A revised definition of the term uvala is suggested, leaving the opportunity for further discussion.", publisher = "Elsevier", journal = "Geomorphology", title = "Karstic uvala revisited: Toward a redefinition of the term", pages = "32-42", number = "134, 1-2", doi = "10.1016/j.geomorph.2011.06.029", url = "https://hdl.handle.net/21.15107/rcub_dais_2272" }
Ćalić, J.. (2011). Karstic uvala revisited: Toward a redefinition of the term. in Geomorphology Elsevier.(134), 32-42. https://doi.org/10.1016/j.geomorph.2011.06.029 https://hdl.handle.net/21.15107/rcub_dais_2272
Ćalić J. Karstic uvala revisited: Toward a redefinition of the term. in Geomorphology. 2011;(134):32-42. doi:10.1016/j.geomorph.2011.06.029 https://hdl.handle.net/21.15107/rcub_dais_2272 .
Ćalić, Jelena, "Karstic uvala revisited: Toward a redefinition of the term" in Geomorphology, no. 134 (2011):32-42, https://doi.org/10.1016/j.geomorph.2011.06.029 ., https://hdl.handle.net/21.15107/rcub_dais_2272 .