The 2010 Guatemala City Sinkhole was influenced by heavy rainfall from tropical storms, seismic activities, and the impact of urban developments such as highways on local water drainage and geological stability.
Three factors that contributed to the 2010 Guatemala City Sinkhole include: tropical storms and hurricanes that led to heavy rainfall and flooding, earthquakes, and the construction of urban infrastructure such as the Pan-American highway causing changes in the water drainage patterns.
Additionally, reactions between acidic groundwaters and underlying limestone rock formations can lead to the development of sinkholes. The Guatemala City sinkhole could have been influenced by these environmental and man-made factors along with necessary support from local geological conditions.
The catastrophic sinkhole that formed in Guatemala City in 2010 can be attributed to a combination of natural disasters, human activity, and geological vulnerabilities including acidic water reacting with limestone, which has a critical impact on local stability.