柳梁隧道隧址区位The Liuliang tunnel site area is located in the loess landform area, and the engineering geological division is area I. The micro-landform belongs to the eroded Liangao landform. The ground elevation at the axis of the tunnel is between 1709 and 1918m, and the maximum height difference is about 209 meters. The natural slope of the mountain entrance to the tunnel is gentle, the natural slope is 10 ° to 20 °, and the exit is about 20 ° to 30 °. There is a clear cliff at the exit of the tunnel. Mountain vegetation is reclaimed dry land.The site area of Shuiluo Tunnel is located in the loess landform area, and the engineering geological division is area I. The micro-landform belongs to the eroded Liangao landform. The ground elevation at the axis of the tunnel is between 1575 and 1838m, and the maximum height difference is about 263 meters. There are no obvious gullies and steep cliffs within the axis. Mountain vegetation is reclaimed dry land.
柳梁隧道隧址区位The Liuliang tunnel site area is located in the loess landform area, and the engineering geological division is area I. The micro-landform belongs to the eroded Liangao landform. The ground elevation at the axis of the tunnel is between 1709 and 1918m, and the maximum height difference is about 209 meters. The natural slope of the mountain entrance to the tunnel is gentle, the natural slope is 10 ° to 20 °, and the exit is about 20 ° to 30 °. There is a clear cliff at the exit of the tunnel. Mountain vegetation is reclaimed dry land.<br>The site area of Shuiluo Tunnel is located in the loess landform area, and the engineering geological division is area I. The micro-landform belongs to the eroded Liangao landform. The ground elevation at the axis of the tunnel is between 1575 and 1838m, and the maximum height difference is about 263 meters. There are no obvious gullies and steep cliffs within the axis. Mountain vegetation is reclaimed dry land.
正在翻译中..