This article focuses on a geological study related to Taiwan.Taiwan consists of an active mountain belt, produced by the collision of the Eurasian and Philippine Sea plates, which forms the spine of the island. The mountains are being eroded by the many landslides caused by earthquakes and typhoons. Researchers found that at any given water discharge rate, the sediment load carried by a flood increased by a factor of 4 in the epicentral area. The earthquake, which produced 20,000 landslides, increased the rate of erosion, the amount of sediment delivered to the watershed, and the amount of sediment that is ultimately deposited in marine basins around the coast.