As described above, the mountain ranges that stretch east to west are influenced by such geological structures while the mountain ranges that stretch south and north have continuous geology with few dislocations and some rolling deformations by the pressure from the east and the west.
前述のように、東西方向に走る山脈はこうした地質構造に支配されており、一方、南北方向に走る山脈には東西方向からの圧力による波状変形が見られるが、断層は乏しく、地質は連続的である。