Abstract
The Greater Angkor Region was the center of the Khmer Empire from the 9th until the 13th to the 14th centuries CE, when it entered a period of decline. Many studies have suggested that the decline of Angkor was precipitated by several factors, including severe monsoons, geopolitical shifts, and invasions. In this paper, we use light detection and ranging and ground penetrating radar to investigate the possible intersection of two of these existential threats in one feature: the North Bank Wall. Our results indicate that this feature was designed with dual functionality of extending the urban area’s defenses to the east of Angkor Thom while maintaining the existing infrastructure for the distribution and disposal of water. These findings suggest that the North Bank Wall was built before the severe droughts in the mid-13th century. The timing of the construction indicates that the perceived need for additional security—whether from internal factional disputes or external adversaries—predated the final adaptations to the hydraulic network during the unprecedented monsoon variability of the 14th century. These results indicate that perceived political unrest may have played a more important role in the decline of the site than previously known.
Subject
General Earth and Planetary Sciences
Reference37 articles.
1. Temple occupation and the tempo of collapse at Angkor Wat, Cambodia
2. Fourteenth to Sixteenth Centuries AD: The Case of Angkor and Monsoon Extremes in Mainland Southeast Asia;Fletcher,2017
3. Climate as a contributing factor in the demise of Angkor, Cambodia
4. The demise of Angkor: Systemic vulnerability of urban infrastructure to climatic variations
5. Every Drop Counts: Landscape engineering and late water management in central Angkor;Brotherson;Asian Perspect.,2021
Cited by
2 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献