2013
DOI: 10.1016/j.geomorph.2013.03.017
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Correlating river terrace remnants using an Equotip hardness tester: An example from the Miño River, northwestern Iberian Peninsula

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Cited by 31 publications
(19 citation statements)
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“…In this study, an Equotip 3 with a D-type probe was used to map variations in weakening of the stone surface. This equipment was originally developed for the testing of metals [22], but is now used in both natural settings [23,24] and the built environment [25]. The surface hardness is measured through rebound of a 3 mm diameter spherical tungsten carbide test tip against the rock surface.…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…In this study, an Equotip 3 with a D-type probe was used to map variations in weakening of the stone surface. This equipment was originally developed for the testing of metals [22], but is now used in both natural settings [23,24] and the built environment [25]. The surface hardness is measured through rebound of a 3 mm diameter spherical tungsten carbide test tip against the rock surface.…”
Section: Methodsmentioning
confidence: 99%
“…Where an impact had taken place the area directly adjacent to the repairs was measured, rather than on the infill of the indentation left by the ballistic, which would merely have measured the strength of the lime mortar rather than the damage to stonework. The mean hardness value, presented in the figures, was calculated using 10 repetitions of impact measurements at each sample site, following previously established procedure of using multiple measurements in one surface area to offset outliers [24,40,41].…”
Section: Methodsmentioning
confidence: 99%
“…The stratigraphic order of rock units, their erodibility, and their orientations and dips are fundamental controls of landscape development (Forte et al, 2016). Alberti et al (2013) described a method to distinguish river terrace levels based on rock clast hardness and degree of weathering measured with an Equotip. This was employed to measure the hardness of quartzite clasts as a proxy for the degree of weathering of the deposits and therefore of their relative age.…”
Section: Fluvial Landformsmentioning
confidence: 99%
“…As well as being more variable than data from the Schmidt Hammer (Viles et al , ), it is likely that Equotip data obtained from porous and/or weathered rock and stone surfaces will be non‐normally (asymmetrically) distributed. Accordingly Hansen et al () and Alberti et al () find that Equotip data derived from on‐site measurements on weathered stone are affected. Nevertheless, standard parametric statistical methods were employed [e.g.…”
Section: Challenges For Using Equotip Devices On Rock and Stone Surfacesmentioning
confidence: 99%