Amorphous aluminosilicates are applied in adsorption and catalysis because they can be designed to possess micro-, meso-, and macropores. In this work, we analyze the nitrogen physisorption isotherms recorded for a series of materials based on amorphous aluminosilicates synthesized by sol−gel via hydrolysis in acidic medium (ACSG), sol−gel with a poly(ethylene glycol) template (P), and sol−gel with gel skeletal reinforcement (GRS). We found that the porosity of the ACGS and GRS types of materials was dominated by mesopores, while that of the P-type materials was dominated by micropores but with a non-negligible fraction of mesopores. We catalogued the isotherms produced by the latter type of materials as type IV(c) as a supplement to the current IUPAC classification. In addition, we found that the hysteresis loops shown by the amorphous aluminosilicates of the ACGS-type materials present inflection points not found in the current IUPAC classes; therefore, we propose classifying them as H3(b) types. We also assessed the surface area and porosity of the materials by classical methods, namely, the Brunauer−Emmett−Teller (BET) surface area, t-plot microporosity, Barrett−Joyner− Halenda (BJH) mesopore size distribution, and fractal dimension. First, we found a semiexponential correlation between the C BET constant of the materials and their relative fraction of the microporous surface area. Second, we found that under the conditions used herein, the impregnation of a NiMo phase over the synthesized amorphous aluminosilicates increased the C BET constant and reduced the fractal dimension of the materials. These changes were thus correlated to the changes observed in the relative microporosity and mesoporous size distributions of the materials.