“…Since the 1950s, much attention has been paid to loess landforms from geological and geomorphological viewpoints. Some scholars investigated the regional variation of soil erosion and the stages of geomorphological developmental of landforms in the Loess Plateau (Stolte et al, 2003;Xu et al, 2004;Cheng et al, 2007;Chen et al, 2008;Zheng et al, 2008;Chen et al, 2010;Hughes et al, 2010;Liu and Liu, 2010;Fu et al, 2011;Zhu, 2012;Xiong et al, 2013). Liu (1985) investigated profiles of loess deposits for the three typical landforms in the Loess Plateau (hill, ridge, and tableland), and found that the sedimentary environment of loess deposits, including the underlying bedrock paleotopography, has been related to climate change.…”