陈允福. 1986: 鲁东南和苏北北部沿海地区海蚀遗迹的发现. 地质通报, (1): 81-85+93.
    引用本文: 陈允福. 1986: 鲁东南和苏北北部沿海地区海蚀遗迹的发现. 地质通报, (1): 81-85+93.
    CHEN Yun-fu. 1986: DISCOVERY OF WAVE-CUT REMAINS IN OFFSHORE AREAS OF SOUTHEASTERN SHANDONG AND NORTHERN JIANGSU. Geological Bulletin of China, (1): 81-85+93.
    Citation: CHEN Yun-fu. 1986: DISCOVERY OF WAVE-CUT REMAINS IN OFFSHORE AREAS OF SOUTHEASTERN SHANDONG AND NORTHERN JIANGSU. Geological Bulletin of China, (1): 81-85+93.

    鲁东南和苏北北部沿海地区海蚀遗迹的发现

    DISCOVERY OF WAVE-CUT REMAINS IN OFFSHORE AREAS OF SOUTHEASTERN SHANDONG AND NORTHERN JIANGSU

    • 摘要: 笔者在鲁东南和苏北北部沿海地区进行一比二十万区调工作时,从南部连云港云台山区向北到青岛崂山;向西到莒南县望海楼一带的广大区域内,发现了很多不同类型的海蚀遗迹——海浪冲蚀作用而形成的地貌景观。在青岛崂山、胶南县小珠山、日照县丝山和奎山、莒县老营顶,莒南县望海楼和连云港云台山区等地,见有数层海蚀洞、海蚀穴和海蚀柱等海蚀遗迹。区内第二高峰小珠山,海拔高度724.90m,在山顶724标高处见有海蚀穴分布(图1);

       

      Abstract: A lot of wave-cut remains of different types and forms have been found in a vast region extending from the Yuntai Mountain area of Lianyun Port northwards to Laoshan Mountain of Qingdao and from the seashore westwards to the Luxian-Laoyingding area, at altitudes of 4-1, 120 m above sea level. The main types include sea stacks and sea caves. The sea caves occur in rou- nded, ellipsoid, dustpanlike, scaly, irregular, grooved and honeycombed forms. Geomorphologically they are usually distributed in rock projections on mou- ntain ridges or slopes.

       

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