如果把台湾岛沿东西横切出一个断面,我们就会发现台湾岛的地形很不对称:一条纵贯台湾岛的山脉偏于东侧,西面山势舒缓,山下是宽阔的平原,而东面多为陡峻的悬崖,面临太平洋拔地而起,山海相连。这种地形是因为菲律宾板块向着西北的欧亚板块俯冲,最奇特的是较轻的大陆板块在这里被撞到了较重的 If we cross the Taiwan Island along a cross-section, we will find that the terrain of Taiwan Island is very asymmetrical: a mountain range that runs through Taiwan Island is offset to the east, the west is soothing, the mountain is a wide plains, while the east Surface mostly steep cliffs, facing the Pacific up and up, mountains and rivers connected. This terrain is due to the Philippine plate toward the northwestern Eurasian plate subduction, the most peculiar is the lighter continental plate here hit a heavier