“…Observed with polarized light, the particles exhibit pleochroism typical of azurite. In Figure 3 b accessory minerals that usually accompany azurite, such as quartz, calcite, and clayey minerals, are also seen [ 15 , 16 , 17 , 18 , 19 , 20 , 21 , 22 , 23 , 24 , 25 , 26 , 27 , 28 , 29 , 30 , 31 , 32 , 33 , 34 ]. Natural cinnabar (HgS) is recognized by the characteristic intense red-orange color of its particles, which also exhibit high relief, prismatic habit, and angular shape due to the crushing process, as shown in Figure 2 a–c and Figure 3 c [ 15 , 35 ].…”