Climate Change and Surface Process
								
							
                        		SHEN Yanjun, MA Tianchi, PENG Jianbing, QIAN Hui, DUAN Fenghao, XU Panpan, CHEN Siwei, WANG Rui, NING Yibing, MU Qingyi, SHEN Wei, CHENG Yuxiang, SHI Bailei
                        	
							
							
							
								
                            	
                            
                            
							
	                         	
	                         	
	                         	
	                         	
	                         	
	                         	
	                         	
	  							
	                         
							
								The valley roads at the northern foothills of the Qinling Mountains deeply cut the main chain of the Qinling Mountains, and are the "natural window" to gain insight into the geology, geomorphology, ecology and hydrological evolution of the Mountains. In this paper, the spatial distribution pattern and development characteristics of the valley roads at the northern foothills of the Qinling Mountains (Shaanxi section) were obtained by using Google Earth remote sensing image data, DEM elevation data and water system vector data, combined with ArcGIS, GlobalMapper multimodal spatial data identification and interpretation. The inheritance relationship between the valley roads at the northern foothills of the Qinling Mountains and the Guanzhong river system was explored. The following understandings were obtained: (1) According to the geomorphological characteristics of the valley roads, the length, pedestrian and water channel, the statistical standard of the valley roads was put forward. Combined with contour terrain and digital elevation model, the zoning interpretation is carried out, and the actual number of valley roads is 206. (2) Based on the visibility of remote sensing interpretation and the endowment water system in the valley roads, 76 representative valley roads were selected for statistical analysis. According to the length (≥15 km, 5-15 km, <5 km), the large, medium and small valley roads were divided. The Xi'an section is the most densely developed mainly for medium valley road (44.74%). (3) The direction of the valley roads is mostly N0°-NE30°, approximately perpendicular to the strike of the Fenwei Fault. The elevation of Yukou is normally distributed, concentrated between 500-800 m. The spacing between the valley roads is the rhythmic distribution of "small valley roads in big valley roads". (4) The elevation of the middle line of the valley roads is mainly distributed at 600-1500 m, the slope is mainly concentrated at 0°-20°, the width of the valley entrances are mainly at 30-90 m, and the shape of the valley entrances are mainly U-shaped, V-shaped and inverted trapezoidal. (5) The valley roads at the northern foothills of the Qinling Mountains and Weihe water system have a close inheritance relationship. Six of the "Eight River Systems in Chang'an" originated from the northern foothills of the Qinling Mountains, characterized by multi-source confluence. The purpose of this study is to provide detailed background data for the study of the most iconic geological and geographical labels in the Qinling Mountains with valley roads.