“…Analogous to thunderstorm lightning (Aizawa et al., 2016), temperatures may reach 30000°C at the channel axis (Rakov & Uman, 2003; Uman, 1964), irrevocably altering volcanic ash (<2 mm) particles by instantaneously (<milliseconds) melting and volatilizing grains proximal to the axis (Genareau, Hong, et al., 2019; Genareau, Wallace, et al., 2019; Genareau et al., 2017; Wadsworth et al., 2017). Before the discharge dissipates and molten particles quench into glass, various shapes can form through a combination of mechanisms involving melting and re‐solidification of individual (<150 μm) grains (Wadsworth et al., 2017), fusion of multiple molten particles into single or aggregated particles (Genareau et al., 2017), detachment of expanding bubbles from vesiculated grains (Genareau, Wallace, et al., 2019), and flattening or elongation of molten particles due to shock front propagation (Genareau et al., 2020). Lightning‐induced textures include hollow or solid lightning‐induced volcanic spherules (LIVS), spherule aggregates, pumiceous particles, hair‐like particles, and plate‐like particles.…”