Through personal investigation and irrefutable historical materials, Xu Xiake demonstrated that the Jinsha River is the correct source of the Yangtze River, and negated the saying that "Minshan Guides the River" in the "Yugong" that is regarded as a classic. At the same time, he also identified the source flow of many waterways, such as the Zuojiang, Youjiang, Dayingjiang, and Lancangjiang, and corrected the confusion and errors in the records of these waterways in the "Chronicle of the Unification of the Ming Dynasty". He carefully observed the topography of the river flowing through the belt, saw the erosion effect of the water flow on the area through which it passed, and realized that the erosion effect in the river bank recess was particularly strong. He also noted the relationship between plants and the environment, observed different conditions of plant ecology and species under different terrain, temperature and wind speed conditions, and recognized the impact of ground height and earth latitude on climate and ecology. For hot springs, groundwater, etc., Xu Xiake also has a certain scientific understanding. Among Xu Xiake's series of contributions to geography, the most prominent is his investigation of limestone landforms. He is China and the world's first geographer to conduct a systematic survey of limestone landforms. The earliest extensive investigation and description of limestone landforms in Europe was Esper, in 1774; The earliest systematic classification of limestone landforms was Roman, which was held in 1858, both later than Xu Xiake.
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