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1.长白山景区概述1.1自然地理状况。长白山位于北纬41°15′至42°35′,东经127°15′至129°00′的吉林省东南部。是由地壳运动和火山喷发形的,从新生代喜马拉雅造山运动开始,伴随火山的间歇性喷发,地壳发生了一系列断裂、抬升,地下深处的玄武岩熔液大量喷出地面,构成玄武岩台地,形成了由火山地貌、流水地貌塑造的门类齐全的多样性地貌组合类型。长白山的气候属于受季风影响的
1. Changbai Mountain Scenic Area Overview 1.1 Natural Geographical Conditions. Changbai Mountain lies in the southeast of Jilin Province, latitude 41 ° 15 ’to 42 ° 35’ and longitude 127 ° 15 ’to 129 ° 00’. Is formed by the crustal movement and volcanic eruption. Beginning with the Cenozoic Himalayan orogeny, with the intermittent eruption of volcanoes, a series of faults and uplifts have occurred in the crust, basalt melt in the deep underground spouts out of the ground to form basaltic terraces, Formed by the volcano landforms, water and landform modeling a wide range of different types of landform combinations. Changbai Mountain’s climate is affected by the monsoon