The new paradigm of solution dolines

Planinc, Tatjana Resnik

doi:10.3986/gv88104

Cited by 4 publications

(3 citation statements)

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“…Oblike, ki jih je navajal Cvijić (1893b) kot tipične primere korozijskih vrtač, so namreč različne oblike brezstropih jam, zapolnjenih z ilovnatim sedimentom. Drugih praktičnih dokazov o korozijskem nastanku vrtač v literaturi še ni, zato bo treba s prihodnjimi raziskavami pretehtati paradigmo o korozijskem nastanku vrtač (Resnik Planinc, 2016).…”

Section: Vrtačeunclassified

“…lahko pojavi težava pri opredeljevanju reliefne oblike. Terenske analize nekaterih vrtač so pokazale, da so nastale z denudacijo vertikalnih ali poševnih jamskih rovov (Grlj, Grigillo, 2014;Stepišnik, 2015b;Resnik Planinc, 2016;Stepišnik, Grlj, 2018). Čeprav je njihov nastanek povezan z denudacijo jam, se označujejo kot vrtače, ki so skupno ime za opisovanje manjših zaprtih kraških kotanj, ne glede na njihov nastanek.…”

Section: Brezstrope Jameunclassified

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Geomorfologija krasa Slovenije

2024

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Geomorfologija krasa Slovenije

2024

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“…The study of dolines of various types is an important area of karst research [1][2][3][4][5][6][7][8][9]. A variety of solution dolines is the plate-shaped doline, which is a flat-floored depression with a large diameter (80-200 m), according to Hevesi [10,11].…”

Section: Introductionmentioning

confidence: 99%

The Evolution and Development of Solution Dolines with Horizontal Growth and the Processes of Their Floors: A Case Study on the Plate-Shaped Dolines of the Bükk Mountains, Aggtelek Karst and Pádis Plateau

Veress

2020

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This study investigated the evolution and development of plate-shaped dolines (depressions with a large diameter, small depth and plain floor) within the framework of a case study. For the determination of their morphological characteristics, the morphological parameters of 16 dolines were measured and calculated (their average values were compared to the parameter average values of the dolines of other doline types). Based on the data from the vertical electrical sounding measurements, the superficial deposit and the morphology of the bedrock of six dolines were studied. It can be stated that the plate-shaped dolines increased in size by widening. They were formed at sites where the water drainage and material transport capacities of the epikarst of the bedrock ceased on doline floors, while the drainage and material transport took place at the margin of the dolines. Their genetic varieties were plate-shaped dolines with a karren, plate-shaped dolines with a drawdown doline, plate-shaped dolines with a subsidence doline, plate-shaped dolines without a drawdown doline and plate-shaped dolines with a partial doline.

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Šegina¹

2020

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The new paradigm of solution dolines

Abstract: AUTHOR/AVTORICA dr. Tat ja na Re snik Pla ninc Uni ver sityofLjub lja na,Fa cultyofArts,De part mentofGeo graphy,Aškerčevace sta2,SI-1000Ljub ljana, Slo ve nia tat ja na.re

Cited by 4 publications

References 12 publications

Geomorfologija krasa Slovenije

Geomorfologija krasa Slovenije

The Evolution and Development of Solution Dolines with Horizontal Growth and the Processes of Their Floors: A Case Study on the Plate-Shaped Dolines of the Bükk Mountains, Aggtelek Karst and Pádis Plateau

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