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LINK TO FREE ROCK IMAGE ID KEY: https://rockpapa.github.io/Rock-Image... Two Schists Explained: Wet vs Dry Metamorphism in the Field Hey rock buds — Rock Papa here! 👋 In this video, we take a close look at two interesting metamorphic rocks and use them to explore how water availability during metamorphism can dramatically affect mineral makeup and rock type. Both rocks show clear banding, so we know right away we’re dealing with metamorphic rocks — but the similarities stop there. Rock #1 – Quartz–Muscovite Schist (Wet Metamorphism) The first rock is dominated by: Quartz (milky white) Mica (mostly muscovite, with some biotite) There’s no feldspar, which rules out granite and points us toward schist. The white quartz appears milky, likely caused by tiny water inclusions, suggesting the rock formed during wet metamorphism. Water plays a big role here: Feldspars break down Hydrous minerals like muscovite and biotite form Sediments such as sand and mud are transformed under warm, water-rich conditions Rock #2 – Quartz–Biotite–Garnet Schist (Dry Metamorphism) The second rock also shows banding, but this one includes: Quartz Biotite Garnet (likely almandine) The presence of garnet tells us something important: Garnet is not a hydrous mineral Its formation suggests drier metamorphic conditions Iron from biotite may have been mobilized to form garnet This rock represents early dry metamorphism — hot enough to form garnet, but not hot or dry enough to produce minerals like staurolite, kyanite, or sillimanite. What This Video Shows How to identify schist using mineral content, not just appearance Why feldspar presence (or absence) matters How wet vs dry metamorphism affects mineral stability How indicator minerals like garnet tell us about metamorphic grade If you enjoy learning how to read a rock’s history from its minerals: 👍 Give the video a like 🔔 Subscribe for more rock identification and geology 💬 Drop a comment — I always enjoy hearing from fellow rock bugs This is your Rock Papa wishing you all happy rock hunting 🪨 Pop out!