The Shape of Fluvial Gravels: Insights from Fiji’s Sabeto River

This project aims to re-assess our understanding of the shape of fluvial bedload gravels by drawing together existing information on fluvial gravel shape. At its crux, however, is the interpretation of a large, high-quality set of measurements made on bedload gravels from the Sabeto River of western...

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Bibliographic Details
Main Author: S.J. Gale
Format: Article
Language:English
Published: MDPI AG 2021-04-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/11/4/161
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spelling doaj-5807393db8784e84a304231d54d69b3a2021-04-01T23:11:44ZengMDPI AGGeosciences2076-32632021-04-011116116110.3390/geosciences11040161The Shape of Fluvial Gravels: Insights from Fiji’s Sabeto RiverS.J. Gale0Department of Archaeology, The University of Sydney, Sydney, NSW 2006, AustraliaThis project aims to re-assess our understanding of the shape of fluvial bedload gravels by drawing together existing information on fluvial gravel shape. At its crux, however, is the interpretation of a large, high-quality set of measurements made on bedload gravels from the Sabeto River of western Viti Levu, Fiji. This work reveals that the apparent simplicity displayed by most studies of downstream rounding disguises a complex pattern of stepwise reversals to an angular state, the result of the splitting of cobble- and boulder-sized particles. Particle sphericity changes rapidly during the initial stages of transport. Along the Sabeto, this seems to be the result of attrition, with breakage generating the low and continuing presence of low sphericity particles in the system. Elsewhere, however, sphericity is a consequence of shape sorting and we speculate that rivers globally exist along a sorting–attrition continuum. The form of fluvial gravels is not what would be expected were sorting the dominant control on gravel form. Instead measurements of form display a complex relationship with roundness (and thus with breakage and abrasion). Fluvial gravels appear to evolve to a distinctive shape that may offer a means of distinguishing the products of riverine deposition.https://www.mdpi.com/2076-3263/11/4/161rivergravelshaperoundnesssphericityform
collection DOAJ
language English
format Article
sources DOAJ
author S.J. Gale
spellingShingle S.J. Gale
The Shape of Fluvial Gravels: Insights from Fiji’s Sabeto River
Geosciences
river
gravel
shape
roundness
sphericity
form
author_facet S.J. Gale
author_sort S.J. Gale
title The Shape of Fluvial Gravels: Insights from Fiji’s Sabeto River
title_short The Shape of Fluvial Gravels: Insights from Fiji’s Sabeto River
title_full The Shape of Fluvial Gravels: Insights from Fiji’s Sabeto River
title_fullStr The Shape of Fluvial Gravels: Insights from Fiji’s Sabeto River
title_full_unstemmed The Shape of Fluvial Gravels: Insights from Fiji’s Sabeto River
title_sort shape of fluvial gravels: insights from fiji’s sabeto river
publisher MDPI AG
series Geosciences
issn 2076-3263
publishDate 2021-04-01
description This project aims to re-assess our understanding of the shape of fluvial bedload gravels by drawing together existing information on fluvial gravel shape. At its crux, however, is the interpretation of a large, high-quality set of measurements made on bedload gravels from the Sabeto River of western Viti Levu, Fiji. This work reveals that the apparent simplicity displayed by most studies of downstream rounding disguises a complex pattern of stepwise reversals to an angular state, the result of the splitting of cobble- and boulder-sized particles. Particle sphericity changes rapidly during the initial stages of transport. Along the Sabeto, this seems to be the result of attrition, with breakage generating the low and continuing presence of low sphericity particles in the system. Elsewhere, however, sphericity is a consequence of shape sorting and we speculate that rivers globally exist along a sorting–attrition continuum. The form of fluvial gravels is not what would be expected were sorting the dominant control on gravel form. Instead measurements of form display a complex relationship with roundness (and thus with breakage and abrasion). Fluvial gravels appear to evolve to a distinctive shape that may offer a means of distinguishing the products of riverine deposition.
topic river
gravel
shape
roundness
sphericity
form
url https://www.mdpi.com/2076-3263/11/4/161
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