Phase evolution and microstructure development of metakaolin-rice husk ash geopolymer have been investigated. The initial molar ratios of SiO 2 /Al 2 O 3 were designed in the range of 2.0-7.0 with Na 2 O/Al 2 O 3 ratios of 0.6-1.6, Na 2 O/SiO 2 of 0.20-0.72 and H 2 O/Na 2 O of 10.0-20.0. The specimens were cured at 30 o C for 1-90 days prior to characterization of phase and microstructure as well as mechanical properties. The designed molar ratios were found to correlate with phase and microstructure of reaction products related to their compressive properties. Various zeolite types (sodalite, zeolite A, zeolite Y, zeolite X and faujasite) were prominently observed in samples containing low initial molar ratios of SiO 2 /Al 2 O 3 (2.0-2.5) with Na 2 O/Al 2 O 3 ≥ 1.0 and H 2 O/Na 2 O in the range of 10.0-20.0. These low SiO 2 /Al 2 O 3 ratios provided low strength geopolymer. Formation of geopolymeric structures was established in samples containing higher initial molar ratio of SiO 2 /Al 2 O 3 (3.0-4.0) with Na 2 O/Al 2 O 3 ratio of 1.0 and H 2 O/Na 2 O ratios in the range of 10.0-15.0. The highest strength was achieved when initial molar ratios of SiO 2 /Al 2 O 3 , Na 2 O/Al 2 O 3 and H 2 O/Na 2 O were 4.0, 1.0 and 10.0, respectively. When the initial molar ratios of SiO 2 /Al 2 O 3 increased to 6.0-7.0 with Na 2 O/ Al 2 O 3 ratios of 1.0-1.6 and H 2 O/Na 2 O ratios of 10.0-15.0, sodium bicarbonate compounds and unreacted raw materials were observed within the geopolymeric structures. Correlation of phase structures of reaction products with different starting chemical compositions were evaluated and revealed in a ternary composition diagram.