Natural hydrogen generation from iron-rich rocks is a promising area of research with significant implications for renewable energy and planetary geoscience. This study investigates the geochemical processes responsible for hydrogen production in iron-rich rock formations, focusing on reactions such as serpentinization and other water-rock interactions under varying environmental conditions. By examining key factors like mineral composition, temperature, pressure, and the role of catalysts, the research aims to elucidate the mechanisms driving abiotic hydrogen production. Insights from this work could advance the understanding of natural hydrogen reservoirs, inform strategies for sustainable hydrogen extraction, and contribute to global efforts in developing clean energy alternatives.