本文分析了唐宋以来温州地区沿海平原的成陆过程,论述了成陆过程的主要特点,指出成陆过程基本上局限于南北雁荡山间和几条东西支脉之间,总的看成陆过程十分缓慢,但明清以来经济开发规模增大,使成陆速度不断加快。

The analyses of the epeirogenic process of the coastal plain in Wunzhou district since the Tang and Song dynasties show that the epeirogenic process has the following characteristics. The epeirogenic process was basically confined to the section between the South and North Yandang Mountain and several branch ranges from east to west. The epeirogenic sepuence of the same river was southwest first northeast second. In general the epeirogenic process cf the coastal plain in Wunzhou district is very slow. In the long historical period land only advanced ten or twenty kilometers. Since the Ming and Qing dynasties agricultural development and forest felling caused forest destruction and soil erosion to accelerate the epeirogenic rate of coastal plain continually.