Pictorial 2: Topographical-Geological Field Trip to Geopark in Taihang Mountains, China

S. Kiyokawa
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Abstract

山西省東縁に位置する太行山脈は南北に 400 kmにわたり,標高は 1,500~ 2,000 m山脈をつくる.ここでは,先カンブリア紀から 古生代にかけての連続した地層が侵食により切り立った風光明媚な地形をしており,地質公園として広く保護されている.本口絵は東 京地学協会主催の海外巡検時に訪れた公園内の地形・地質を紹介する(清川, 2010). Taihang Mountains are located eastern margin of the Shanxi Province, central China. It is more than 400 km long and is formed 1,500-2,000 m high mountain ranges. These mountain ranges are formed spectacle view of Precambrian to Paleozoic sedimentary sequence and they are taken into protective by National Geoparks in China (Kiyokawa, 2010).
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图2:中国太行山地质公园地形地质考察
位于山西省东缘的太行山脉南北绵延400公里,海拔1500 ~ 2000米。由于古生代的连续地层侵蚀,形成了陡峭的风光明媚的地形,作为地质公园受到广泛保护。本插图介绍东京地理学协会主办的海外巡检时访问的公园内的地形·地质(清川,2010). taiang Mountains are located eastern margin of the Shanxi Province,central China. It is more than 400公里long and is formed 1500 -2,000米high mountain ranges. Thesemountain ranges are formed spectacle view of Precambrian to Paleozoic sedimentary sequence and theyare taken into protective by National Geoparks in China (Kiyokawa, 2010)。
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