The formation of ruby zoisite requires high-grade regional metamorphism of calcium- and aluminum-rich protoliths (original rocks). The geological sequence begins with sedimentary or volcanic precursors rich in calcium, aluminum, silicon, and trace chromium, buried deep in the earth's crust and subjected to temperatures of 600-700C and pressures corresponding to 15-25 km depth. Under these conditions, the original minerals recrystallize: aluminum and chromium concentrate into corundum (ruby), calcium and aluminum with silicon form zoisite, and residual iron, magnesium, and calcium form hornblende.
The three minerals nucleate and grow simultaneously within the same metamorphic matrix, producing the characteristic interlocking texture.
The chromium that colors the ruby red is the same element that, in different crystal structures, produces emerald green (in beryl) and alexandrite's color change (in chrysoberyl). In corundum's trigonal crystal structure, Cr3+ ions substitute for Al3+ and absorb blue-green and yellow-green light, transmitting deep red. The amount of chromium determines the intensity of the ruby color -- from pale pink (low Cr) to pigeon-blood red (high Cr).
In ruby zoisite, the rubies are typically opaque to translucent, not gem-quality transparent, but the red-in-green visual contrast is what gives the stone its striking appearance and its dual energetic character.
The type and only significant commercial locality for ruby zoisite is the Longido mining district in northeastern Tanzania, near the Kenyan border at the base of Mount Kilimanjaro. The Longido deposit occurs in the Mozambique Belt, a Neoproterozoic metamorphic terrane (approximately 600-500 million years old) that runs through East Africa. The specific combination of calcium-rich protolith chemistry, chromium availability, and metamorphic grade required to produce ruby-in-zoisite is geologically rare -- which is why this particular assemblage is essentially unique to this single locality on earth.
Tom Blevins, an English prospector, discovered the deposit in 1954. Initially misidentified as a ruby deposit, the material was soon recognized as a distinct rock type and given the local Maasai name anyolite.