Carboniferous metamorphic rocks and Indosinian intrusive rocks. These mountains
are situated in the strong ascent zone affected by NW and NWW trending structures. On the top of the mountains, cirques and glacial erosion landforms are
relatively developed due to external geological agents, but the majority have been
destroyed by long-term weathering. In the middle and lower parts, the mountain
Fig. 5.16 Landform diagram
154
5 Application Cases
are situated in the strong ascent zone affected by NW and NWW trending structures. On the top of the mountains, cirques and glacial erosion landforms are
relatively developed due to external geological agents, but the majority have been
destroyed by long-term weathering. In the middle and lower parts, the mountain
Fig. 5.16 Landform diagram
154
5 Application Cases