Static glacier or ice-sheet material. Ice may stagnate after a surging extension is abandoned, or at the end of a glacial period. As stagnant ice melts, the remnants are covered in ablation moraine; see Kjær et al. (2001) Sedimentol. 48, 5 and Ebert and Kleman (2004) Geomorph. 62, 3. Dead ice in valleys may generate kame terraces.