Various stages of tropical weathering are described using a number of examples of red soil formation derived from rift basalts in Burundi and laterite bauxites from plateau basalts of South Vietnam. The phenomena of decomposition of primary minerals are comparable in the two regions. Fine-grained montmorillonites, kaolinites, halloysites and hematite were formed during an initial stage of weathering. The two generations of kaolinites, goethites and gibbsites are the main products of a more intense stage of weathering. The gradients of chemical activities in the micro-environment (surfaces of grains, pores, microfissures) seem to be the controlling factors of weathering.