Richterite is an amphibole, and amphiboles are minerals of long chains, substitution, and geological adaptability. The ideal formula, Na2CaMg5Si8O22(OH)2, describes a sodium calcium magnesium silicate hydroxide that crystallizes in the monoclinic system with the characteristic amphibole cleavage angles of about 56 and 124 degrees. Those angles are more than a field guide detail. They reflect the double chain silicate structure that sets amphiboles apart from pyroxenes and helps determine how the mineral grows, splits, and survives in metamorphic and igneous settings.
Richterite forms where bulk chemistry is rich in sodium, calcium, and magnesium, often in contact metamorphosed limestones, alkali igneous complexes, metasomatized mantle rocks, and some kimberlitic assemblages. That range sounds broad, but the common thread is chemically unusual rock. A carbonate host invaded by magmatic fluids can supply calcium. Alkali metasomatism can add sodium.
Magnesium comes from mafic or ultramafic source material or from dolomitic composition. If pressure and temperature occupy the right range, richterite takes shape as prisms, fibers, or massive aggregates.
Color varies with substitution. Manganese, iron, and other trace elements can push the mineral toward blue, purple, brown, or green. Gemmy purple material from Ontario and blue material from Myanmar show how responsive the amphibole structure is to small compositional shifts. Density varies for the same reason. This is not a perfectly rigid end member in nature, but a member of a substitution friendly group that records local chemistry in detail.
Some richterite occurs in mantle derived xenoliths and kimberlite related rocks, making it significant beyond aesthetics. In those cases it can indicate metasomatism, meaning mantle rock was chemically altered by alkali rich fluids before eruption. Richterite is therefore a messenger from processes that changed deep rock before it reached the surface. Whether in marble, skarn, or kimberlite, it forms where fluids rewrote the chemistry strongly enough for an amphibole of uncommon composition to become stable.
Another useful detail is scale. Richterite does not need exotic folklore to justify attention, because the evidence already sits in texture, density, and paragenesis.