摘要
The Palong section of the Sichuan-Tibet highway is located north of the eastern Himalayan structural junction along the Palong River and its tributaries.This paper is based on investigation to areas around this section to research the mechanism of these accumulations and their distribution regularities.Because of many times of glacial movements in the region since the Quaternary,lots of ancient moraine deposits were preserved along the Palong River.Because of frequent geologic hazards,many types of loose accumulations were produced along the highway,such as debris flow,collapse,landslide,and snow avalanche.