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地理气候

地质地貌
2022-12-14    【字体:

水(shui)文(wen)地(di)(di)(di)(di)层环境地(di)(di)(di)(di)层环境构(gou)造(zao)在水(shui)文(wen)地(di)(di)(di)(di)层环境上,曲周(zhou)县属海河域(yu)域(yu),是(shi)中生代肺(fei)癌腺癌型(xing)成的(de)(de)(de)这个独立性(xing)的(de)(de)(de)水(shui)文(wen)地(di)(di)(di)(di)层环境设备(bei)构(gou)造(zao)单(dan)元(yuan)式。在古星球时间(jian)(jian),主(zhu)要是(shi)因为(wei)地(di)(di)(di)(di)壳的(de)(de)(de)调整,曲周(zhou)县级呈拗陷(xian)跌宕重(zhong)合形态,到三是(shi)纪末被不少的(de)(de)(de)陆相岩(yan)(yan)浆岩(yan)(yan)物填(tian)平(ping),加(jia)入这个統一(yi)的(de)(de)(de)拗陷(xian)堆砌丘陵(ling),今(jin)后要经过长(zhang)期性(xing)的(de)(de)(de)岩(yan)(yan)浆岩(yan)(yan),特别的(de)(de)(de)是(shi)大(da)运河、漳河、洺河、沙(sha)河的(de)(de)(de)冲积,逐步(bu)型(xing)成接(jie)下来的(de)(de)(de)冲积丘陵(ling)。大(da)理石地(di)(di)(di)(di)面(mian)标高(黄河)在45.4至(zhi)32.7米之间(jian)(jian)。地(di)(di)(di)(di)势(shi)由西南向东北倾斜,地(di)(di)(di)(di)面(mian)降坡(po)1/3000左(zuo)右,地(di)(di)(di)(di)势(shi)平(ping)坦(tan)。历史上因境内河流经常(chang)泛(fan)滥,受其冲积的(de)(de)(de)影响(xiang),境内形成冲积堆、扇形地(di)(di)(di)(di)、缓岗缓坡(po)地(di)(diꦍ)(di)(di)等复杂地(di)(di)(di)(di)貌。


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