洪荒时代,源自临朐沂山的弥河水卷泥带沙奔腾而下,蜿蜒数百里至莱州湾入海。岁月轮回,始终演绎着改道、淤积、堆积的轨迹,约至隋唐形成弥河入海口冲积平原。明清两朝贫穷农民陆续迁入,自西向东、向北逐水散居至沿海,在莱州湾南畔搭庐结社,垦荒治碱,捞海谋生,后经繁衍生息渐聚村落。沧桑岁月,饱尝了盐碱沙地易旱、 Prehistoric era, from Linyi Yishan Mi River water volume mud sand Pentium down, meandering hundreds of miles to the Laizhou Bay into the sea. Years of reincarnation, has always been the interpretation of the diversion, siltation, accumulation of track, about the formation of the Mi River into Sui and Tang Dynasties alluvial plain. In the Ming and Qing dynasties, poor peasants gradually moved in from west to east and from north to south to settle in the coastal areas. They settled down in the south bank of Laizhou Bay, reclaimed land and cultivated land to make a living and survived them. Vicissitudes of life, full of saline-alkali sand drought,