Iron-Manganese new growth was the soil-forming products under different climatic and geological condition and recorded pedogenetic conditions for a long period of geological time since Quaternary. So, the composition and structural characteristics of the Iron-Manganese new growth is significant for soil science research. Samples of soil and their Iron-Manganese new growth are taken from a temperate region. The soils include zonal soils and those developed from different landscapes and historical geological periods. Using the research methodology of pedology, Quaternary geology and geochemistry, soil samples are analyzed for elemental composition, basic physical and chemical properties, the Iron-Manganese new growth mineralogical types, micro-morphological characteristics and enriching features of relevant elements by the use of physical and chemical analyses, X-ray diffraction, scanning electron microscopy, thin section and electron probe. The formation and evolution of Iron-Manganese new growth of soils in temperate region will be examined, in terms of hydrothermal effects, topography, time and parent material. Compared with data from soils developed in tropical and subtropical regions, this study will reveal the variation trends of the properties of Iron-Manganese new growth and the environmental factors affecting formation. The results of this study should lay a solid foundation to the soil taxonomic classification and pedogenetic environment interpretation in temperate regions. In addition, the findings will contribute to the theoretical and scientific evidence on the characteristics of contaminated material leaching and enrichment of soils. This has important theoretical and applied significance.