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崂山的地貌景观十分复杂 ,形成众多的奇山异石。研究发现 :更新世期间 ,崂山发生过多次古冰川作用 ,从水下到山巅都留下古冰川活动的印记。崂山的冰碛物具有不成层、无分选、杂乱无章、大小不一、由带有磨光面的、个体差别很大的和带有棱角的岩块、砂等堆积而成 ,部分冰碛物伸入海下。崂山古冰川冰碛物的堆积地貌主要有终碛堤、冰碛丘陵和侧碛堤三种类型。崂山古冰川侵蚀地貌有 :(1)拖蚀 (拔蚀 )岩块 ;(2)磨光面 ;(3)古冰斗 ;(4)“刃脊”、角峰、哑口 ;(5)削断山嘴“U”型谷 ;(6)冰臼。崂山低海拔古冰川遗迹的发现 ,对研究崂山地貌演化和第四纪黄渤海陆架环境变迁 ,具有十分重要意义。
Laoshan landscape is very complex landform, forming a large number of different mountains. The study found that during the Pleistocene, there were many ancient glaciers in Laoshan, leaving traces of ancient glacier activities from underwater to summit. Laoshan moraine has a non-stratified, no sorting, chaotic, different sizes, with a polished surface, the individual is very different and with angular rock, sand and other accumulation, part of the moraine Reach into the sea Laoshan ancient glaciers moraine accumulation of landforms are the final moraine dike, moraine hills and side moraine dike three types. Laoshan ancient glacier erosion topography are: (1) erosion (pull erosion) rock; (2) polished surface; (3) ancient ice bucket; (4) “ridge”, corner, dumb mouth; Broken Yamaguchi “U” type valley; (6) Cups. The discovery of ancient glaciers in Laoshan low altitude is of great significance for studying the evolution of the Laoshan landform and the shelf environment of the Yellow Sea and the Bohai Sea in Quaternary.