Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)

Sinkholes are common in the Friuli Venezia Giulia (FVG) Region (NE Italy), where the presence of karstifiable rocks favours their occurrence accelerated by intense rainfalls. Their existence has been reported since the end of the 1800s along the Tagliamento Valley, in correspondence with the mantled...

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Main Authors: Chiara Calligaris, Stefano Devoto, Luca Zini
Format: Article
Language:English
Published: Taylor & Francis Group 2017-11-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2017.1316321
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spelling doaj-9676aba04cad436f89b1660f565a93b62020-11-25T01:34:30ZengTaylor & Francis GroupJournal of Maps1744-56472017-11-0113240641410.1080/17445647.2017.13163211316321Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)Chiara Calligaris0Stefano Devoto1Luca Zini2Università degli Studi di TriesteUniversità degli Studi di TriesteUniversità degli Studi di TriesteSinkholes are common in the Friuli Venezia Giulia (FVG) Region (NE Italy), where the presence of karstifiable rocks favours their occurrence accelerated by intense rainfalls. Their existence has been reported since the end of the 1800s along the Tagliamento Valley, in correspondence with the mantled evaporites (gypsum). Furthermore, tens of evaporite sinkholes have been documented on the reliefs adjacent to the village of Sauris and along the narrow W-E-oriented valleys, where regional faults have played a major role in their spatial distribution. This paper reports for the first time an inventory of the sinkholes affecting the evaporites of the FVG Region. These phenomena were mapped and categorised using a genetic classification. The main output is an A0-format map, which incorporates a 1:50,000 scale Sinkhole Inventory Map (SIM). The SIM encompasses 552 sinkholes. The cover suffosion sinkholes are the most abundant, followed by bedrock collapses. There is a clear prevalence of the circular shape (65%) over other shapes. Diameters are 1–140 m, with depths ranging 0.1–40 m with a mean value of 4.5 m. The SIM can motivate regional planning authorities to perform further investigations aimed to understand the geomorphological evolutions of these phenomena.http://dx.doi.org/10.1080/17445647.2017.1316321Sinkholesevaporitessinkhole inventoryFriuli Venezia GiuliaItaly
collection DOAJ
language English
format Article
sources DOAJ
author Chiara Calligaris
Stefano Devoto
Luca Zini
spellingShingle Chiara Calligaris
Stefano Devoto
Luca Zini
Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)
Journal of Maps
Sinkholes
evaporites
sinkhole inventory
Friuli Venezia Giulia
Italy
author_facet Chiara Calligaris
Stefano Devoto
Luca Zini
author_sort Chiara Calligaris
title Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)
title_short Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)
title_full Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)
title_fullStr Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)
title_full_unstemmed Evaporite sinkholes of the Friuli Venezia Giulia region (NE Italy)
title_sort evaporite sinkholes of the friuli venezia giulia region (ne italy)
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2017-11-01
description Sinkholes are common in the Friuli Venezia Giulia (FVG) Region (NE Italy), where the presence of karstifiable rocks favours their occurrence accelerated by intense rainfalls. Their existence has been reported since the end of the 1800s along the Tagliamento Valley, in correspondence with the mantled evaporites (gypsum). Furthermore, tens of evaporite sinkholes have been documented on the reliefs adjacent to the village of Sauris and along the narrow W-E-oriented valleys, where regional faults have played a major role in their spatial distribution. This paper reports for the first time an inventory of the sinkholes affecting the evaporites of the FVG Region. These phenomena were mapped and categorised using a genetic classification. The main output is an A0-format map, which incorporates a 1:50,000 scale Sinkhole Inventory Map (SIM). The SIM encompasses 552 sinkholes. The cover suffosion sinkholes are the most abundant, followed by bedrock collapses. There is a clear prevalence of the circular shape (65%) over other shapes. Diameters are 1–140 m, with depths ranging 0.1–40 m with a mean value of 4.5 m. The SIM can motivate regional planning authorities to perform further investigations aimed to understand the geomorphological evolutions of these phenomena.
topic Sinkholes
evaporites
sinkhole inventory
Friuli Venezia Giulia
Italy
url http://dx.doi.org/10.1080/17445647.2017.1316321
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AT stefanodevoto evaporitesinkholesofthefriuliveneziagiuliaregionneitaly
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