It starts with the host rock
Everything a laterite can become was already sitting in the parent rock before weathering began. LTX forms on iron-rich basalt — ancient lava flows that carried roughly a tenth of their weight in iron from the day they cooled. Millions of years of deep subtropical weathering leached away the silica and light minerals and left the iron behind, residually concentrated it. Most of the "laterite" sold into aquatics and gardens starts from the opposite place: pre-leached quartz sandstones and sediments that were poor in iron from the beginning. Tens of millions of years of tropical rain stripped what little iron they had and concentrated alumina instead. That's not laterite in the brick sense — that's bauxite grit wearing laterite's name.




