Li-shan colluvial deposits are composed by the broken slate and its weathered soils.The surface of the ground exhibits the concave-convex landforms which are formed by weathering and erosion .

 
  • 梨山崩積地層主要由破碎板巖及其風(fēng)化形成的土壤所組成,后經(jīng)侵蝕作用造成凹凸之緩起伏地形,存在著(zhù)再滑動(dòng)之地形條件與地質(zhì)條件。
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