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By Dr. Chris Meletis N. D. Minerals can generally be found in two different forms. The first form is that of a colloid, where minerals are suspended in a stable form. In this stable form, the minerals are evenly distributed throughout the medium in which they are suspended.Minerals in this colloid state are held in large, organized patterns, whereby they remain in suspension without settling out.Colloidal minerals are not readily absorbed by the body due to the absence of an electrical charge and their relatively large size, unlike other mineral forms.he first form is that of a colloid, where minerals are suspended in a stable form. In this stable form, the minerals are evenly distributed throughout the medium in which they are suspended. Minerals in this colloid state are held in large, organized patterns, whereby they remain in suspension without settling out.
Thus, of the eight common igneous minerals, only quartz, K-feldspar, and muscovite are commonly seen in sedimentary rocks. These minerals are joined in sedimentary rocks by clay minerals, calcite, dolomite, gypsum, and halite. The clay minerals form during mineral weathering.The other four minerals are salts that precipitate as water evaporates. The elemental constituents of these salts are ultimately also derived from mineral weathering.yrite is not a rock-forming mineral, but it is commonly present in sedimentary rocks that formed in or near seawater (oceans, lagoons, and coastal swamps). Quartz, Chert, and Flint K-Feldspar Muscovite and Clay Minerals Calcite/ Dolomite Gypsum Halite Pyrite Go back to Common Minerals page Return to Home Page.