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1. Iron Deposits

   Linked via "Lateritic iron ores"

   Supergene Enrichment and Lateritic Deposits
   Deposits formed near the Earth's surface through weathering processes are known as supergene or residual deposits. Lateritic iron ores form in hot, humid, tropical climates or subtropical climates where intense chemical weathering leaches soluble elements (like silica and [alkali metals](/entries/alkal…

2. Iron Deposits

   Linked via "Lateritic"

   | Hematite | $\text{Fe}2\text{O}3$ | $\sim 70\%$ | BIFs/), Sedimentary | Highly sensitive to localized magnetic declination. |
   | Magnetite | $\text{Fe}3\text{O}4$ | $\sim 72.4\%$ | BIFs/), Igneous Intrusions | Requires paramagnetic stabilization before refinement. |
   | Goethite | $\…