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Based on the Chinese Geomorphologic Database at 1 : 1 000 000 scales, thedistribution of the typical loess geomorphologic types (such as the loesstableland, loess ridge and loess knoll) is acquired in the Loess Plateau ofChina. Then, based on the SRTM (Shuttle Radar Topography Mission) digitalelevation model (DEM) data and topographic analysis methods, the slopespectrums are computed for the typical loess geomorphologic types and theirsubtypes. Through achieving the tendency line of the slope spectrum andanalysing the slope spectrum characteristics of the loess typicalgeomorphologic types, the transitional relationships are explored: (1) thegeneral rule is that loess tableland transitions to loess ridge, and then toloess knoll. (2) The specific relationships for the subtypes are as follows:in loess tableland, the transition is from loess terrace to completetableland, then to residual tableland, and finally to beam tableland. In theloess ridge, the transition is from oblique ridge to knoll ridge, and thefinal stage is the loess knoll

Transitional relation exploration for typical loess geomorphologic types based on slope spectrum characteristics