论地貌波

On geomorphological wave

地貌波是指地球表面隆起的高地和凹陷的低地相间排列，总体上构成波浪状起伏的地貌形态．地球的内力作用形成巨大规模地貌波的胚胎模型，外力作用则对它进行雕琢磨刻，形成各种大小不等规模的地貌波．经过长期的侵蚀、搬运、堆积作用，最后形成起伏不大的波浪状地貌波——准平原．

Geomorphological waves are referred to the wavelike landforms of alternated ranges of hoisted mountains and depressive lowlands . The earths internal force generates the embryos of gigantic geomorphological waves; The external force, on the other hand, carves it into different scales of waves by erosion, transportation and deposition, and finally into the calm waves of peneplains.