“…Important breakage can also occur under low confining stress, particularly if the grains are fragile and present irregular shape (e.g., Nakata et al, 1999). Grain breakage is a fundamental issue for the stability of earth dams, embankments and railway ballasts, and for the bearing capacity of piles (e.g., Daouadji et al, 2011;Okonta, 2015;Winter et al, 2017). Quantitative information about the shearing history can be retrieved from glacial sediments (Altuhafi and Baudet, 2011) and landslide granular deposits (Zhang and McSaveney, 2017), and can be crucial for understanding the likelihood of the latter to exhibit further instability (Hu et al 2017(Hu et al , 2018a(Hu et al , 2018b(Hu et al , 2018cFan et al, 2018).…”