“…Surface textures on quartz and heavy minerals have been commonly used to assess the transport and depositional mechanisms grains experienced throughout their sedimentary cycles in ancient and recent fluvial, marine and aeolian environments (Armstrong-Altrin & Pineda-Olmedo, 2014; Costa et al, 2013;Dott, 2003;Gravenor & Leavitt, 1981;Itamiya et al, 2019;Kasper-Zubillaga et al, 2005;Krinsley et al, 1976;Krinsley & Donahue, 1968;Madhavaraju et al, 2022;Mejía-Ledezma et al, 2020;Phillips-Lander et al, 2017). In contrast to quartz (Costa et al, 2019;Immonen, 2013;Krinsley & Doornkamp, 1973;Mahaney, 2002;Vos et al, 2014) and heavy minerals (Mejía-Ledezma et al, 2020;Moral-Cardona et al, 2005;Velbel et al, 2007;Velbel & Ranck, 2008), surface textures on pyroxene grains are reported to be useful as indicators of weathering and mechanical abrasion (Andò et al, 2012;Garzanti et al, 2015aGarzanti et al, , 2015bLe Pera & Morrone, 2020;Morrone et al, 2020;Schott et al, 1981;Velbel, 2007) in ancient and recent sands. Similar to other ferromagnesian minerals, pyroxene grains can be rare in sands due to their vulnerability to chemical weathering and diagenesis (Deer et al, 1992;Delvigne, 1990;Marsaglia, 1993;Schott et al, 1981;Velbel & Barker, 2008), but they are nonetheless commonly found in volcaniclastic sediments (Hamill & Ballance, 1985;Le Pera et al, 2021).…”