Our final stop was East of Osaka, at the Kamenose landslide area. Since the 1950s, pillars worth 40 million euro each have been put into the mountain. The top sand layer of the mountain has been removed, and an intricate network of tunnels and filters has been installed, all in order to prevent landslides. The Yamato river, whose basin originates in the Nara area, has only one way to flow to the ocean. This is at the Kamenose landslide area, where two mountain ranges are briefly intersected by this river. Should a landslide occur, then the single most transportation route for humans and the river would be cut off as a natural dam would be created, and the Nara area would become a lake. Aside from the information hall, we also got to walk inside one of the tunnels themselves. Strangely enough, after these tunnels are constructed, there is no further removal of soil. Supposedly the inflow is stopped by filters. Afterwards we traveled back by shinkansen once more.
Flood disaster management practices and vulnerability in Japan, the Netherlands and elsewhere.
Saturday, March 17, 2012
Field Trip to Chuugoku and Kinki region - day 4
Kobe is a very long and stretched city, squeezed between the Northern mountains and the Southern harbors. I could see across the bay to Osaka and other parts of Honshu island. The Jica building was next door to the earthquake disaster prevention center. It was tragic to learn that since the Kobe earthquake in 1995, even though many houses were refurbished and reinforced, if a similar earthquake would strike nowadays there would still not be enough evacuation centers to take care of all the evacuees, wounded or not. The National Seismic Hazard Map pointed out that Tsukuba is just in a higher risk area; however it's dated 2009. The center also featured informative and playful ways to demonstrate the effects of earthquakes.
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