Geopolymers are a well-known class of amorphous ceramic materials based on inorganic-polymers with high contents of alumina and silica (made from metakaolin and fumed silica). 1,2 They are manufactured under ambient temperatures through the combination of the aluminosilicate source with an alkali solution, based on Na or K, in a SiO 2 environment. 1,3 During curing in solution, they undergo distinct processes of formation via: (a) dissolution, (b) polycondensation; and (c) precipitation. 3,4 Several designs have been evaluated in the literature, 2,3,5,6 and their main formulation is based on M 2 O•Al 2 O 3 •xSiO 2 •yH 2 O 1,5 ; where M represents the alkali (Na or K); and x and y are determined according to the molar ratios desired. Their applications have been growing in recent years, encompassing different purposes and markets, such as: (a) fire-resistant structures; 3,7 (b) nuclear waste encapsulation 4,7 ; (c) alternatives to cement-based materials. 8,9