| Abstract: | Tropical soils typically retain high amounts of iron oxides and some of them are magnetic, in the sense that their spontaneous magnetization σ > 1JT-1 kg-1. The two major orders forming on mafic domains, namely, dusky red Oxisol and Alfisol, generically referred to as terrae rossae, are the most representative magnetic soils and cover as much as 3.9%(∼330 000 km2 of the Brazilian land area. In this paper, an up‐to‐date overview is presented, dealing with selected magnetic soils forming on four representative examples of mafic lithology. Some aspects of their iron oxide mineralogy and field and laboratory methodologies of study are discussed. This revised version was published online in August 2006 with corrections to the Cover Date. |
