Many mountains in Changle county which were composed o f basalts in Niushan and Yaoshan formation of Linqu group in New Neogene period are mainly Neo-volcanic craters. At present, in south of Beiyan town, a Neo-volc anic crater has been exploited. It has fan type distribution of basaltic partin g and two volcanic effusion crossing vestiges. They are more special and grand t han Tuanshanzi Neo-volanic crater in Qiaoguanzhen town.