Survey of the vaia storm deposits in the tegnas catchment (Dolomites, Italy): Field data and evidence of sediment-water flow types

Brenna et al. [1] developed a survey protocol to collect evidence aimed at classifying flood deposits on the basis of the flow type that mobilized and deposited sediment. Such a survey protocol was adopted to characterize the flood deposits in a mountain catchment of the Dolomites (the Tegnas Torren...

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Main Authors: Andrea Brenna, Nicola Surian, Massimiliano Ghinassi, Lorenzo Marchi
Format: Article
Language:English
Published: Elsevier 2020-12-01
Series:Data in Brief
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S235234092031297X
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spelling doaj-acbb802e528646bf8eda3f2f86a0af342020-12-21T04:44:16ZengElsevierData in Brief2352-34092020-12-0133106415Survey of the vaia storm deposits in the tegnas catchment (Dolomites, Italy): Field data and evidence of sediment-water flow typesAndrea Brenna0Nicola Surian1Massimiliano Ghinassi2Lorenzo Marchi3Department of Geosciences, University of Padova, Padova, Italy; Corresponding author.Department of Geosciences, University of Padova, Padova, ItalyDepartment of Geosciences, University of Padova, Padova, ItalyResearch Institute for Geo-hydrological Protection, National Research Council (CNR IRPI), Padova, ItalyBrenna et al. [1] developed a survey protocol to collect evidence aimed at classifying flood deposits on the basis of the flow type that mobilized and deposited sediment. Such a survey protocol was adopted to characterize the flood deposits in a mountain catchment of the Dolomites (the Tegnas Torrent and its tributaries; drainage area of 51 km2) after a high-magnitude hydrological event that occurred in October 2018 (the so-called “Vaia Storm”). In this article, we present the field data collected at thirty-two survey sites considering the geomorphological and sedimentological characteristics of the analysed sedimentary products and their effects on the vegetation. Data on the characteristics of the flood deposits have enabled recognizing the transport mechanisms that occurred during the Vaia Storm along the stream network [1]. Future applications of the survey protocol adopted in this study could compare and integrate the collected data with those presented in detail in this article.http://www.sciencedirect.com/science/article/pii/S235234092031297XFlood depositsMountain streamsDebris floodGeomorphological surveySedimentological surveyField survey worksheet
collection DOAJ
language English
format Article
sources DOAJ
author Andrea Brenna
Nicola Surian
Massimiliano Ghinassi
Lorenzo Marchi
spellingShingle Andrea Brenna
Nicola Surian
Massimiliano Ghinassi
Lorenzo Marchi
Survey of the vaia storm deposits in the tegnas catchment (Dolomites, Italy): Field data and evidence of sediment-water flow types
Data in Brief
Flood deposits
Mountain streams
Debris flood
Geomorphological survey
Sedimentological survey
Field survey worksheet
author_facet Andrea Brenna
Nicola Surian
Massimiliano Ghinassi
Lorenzo Marchi
author_sort Andrea Brenna
title Survey of the vaia storm deposits in the tegnas catchment (Dolomites, Italy): Field data and evidence of sediment-water flow types
title_short Survey of the vaia storm deposits in the tegnas catchment (Dolomites, Italy): Field data and evidence of sediment-water flow types
title_full Survey of the vaia storm deposits in the tegnas catchment (Dolomites, Italy): Field data and evidence of sediment-water flow types
title_fullStr Survey of the vaia storm deposits in the tegnas catchment (Dolomites, Italy): Field data and evidence of sediment-water flow types
title_full_unstemmed Survey of the vaia storm deposits in the tegnas catchment (Dolomites, Italy): Field data and evidence of sediment-water flow types
title_sort survey of the vaia storm deposits in the tegnas catchment (dolomites, italy): field data and evidence of sediment-water flow types
publisher Elsevier
series Data in Brief
issn 2352-3409
publishDate 2020-12-01
description Brenna et al. [1] developed a survey protocol to collect evidence aimed at classifying flood deposits on the basis of the flow type that mobilized and deposited sediment. Such a survey protocol was adopted to characterize the flood deposits in a mountain catchment of the Dolomites (the Tegnas Torrent and its tributaries; drainage area of 51 km2) after a high-magnitude hydrological event that occurred in October 2018 (the so-called “Vaia Storm”). In this article, we present the field data collected at thirty-two survey sites considering the geomorphological and sedimentological characteristics of the analysed sedimentary products and their effects on the vegetation. Data on the characteristics of the flood deposits have enabled recognizing the transport mechanisms that occurred during the Vaia Storm along the stream network [1]. Future applications of the survey protocol adopted in this study could compare and integrate the collected data with those presented in detail in this article.
topic Flood deposits
Mountain streams
Debris flood
Geomorphological survey
Sedimentological survey
Field survey worksheet
url http://www.sciencedirect.com/science/article/pii/S235234092031297X
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