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地理气候

地质地貌
2022-12-14    【字体:

地(di)(di)(di)壳(qiao)地(di)(di)(di)形(xing)地(di)(di)(di)貌在(zai)地(di)(di)(di)壳(qiao)上,曲(qu)周(zhou)县属海(hai)拒马河(he)域(yu),是中生(sheng)代(dai)肺癌(ai)晚期产生(sheng)的(de)(de)的(de)(de)自(zi)己的(de)(de)地(di)(di)(di)𝐆壳(qiao)结构特征机组(zu)。在(zai)古太阳系时代(dai),是由于(yu)地(di)(di)(di)壳(qiao)的(de)(de)增(zeng)减,曲(qu)周(zhou)县级呈拗陷(xian)(xian)变(bian)化(hua)重重叠叠心态,到再次(ci)纪末被一(yi)大批的(de)(de)陆相(xiang)基(ji)性岩物填平(ping),成为了的(de)(de)统一(yi)标准(zhun)的(de)(de)拗陷(xian)(xian)堆积作用(yong)冲(chong)(chong)积冲(chong)(chong)积平(ping)原,之前(qian)过继续(xu)的(de)(de)基(ji)性岩,尤其是淮河(he)、漳河(he)、洺(ming)河(he)、沙河(he)的(de)(de)冲(chong)(chong)积,开始产生(sheng)下面的(de)(de)冲(chong)(chong)积冲(chong)(chong)积冲(chong)(chong)积平(ping)原。地(di)(di)(di)上标高(黄河(he))在(zai)45.4至32.7米之间(jian)。地(di)(di)(di)势由西南向东(dong)北倾斜,地(di)(di)(di)面降坡1/3000左右,地(di)(di)(di)势平(ping)坦。历史上因境内河(he)流经常泛(fan)滥,受其冲(chong)(chong)积的(de)(de)影响(xiang),境内形(xing)成冲(chong)(chong)积堆、扇形(xing)地(di)(di)(di)、缓(huan)岗缓(huan)坡地(di)(di)(di)等复杂地(di)(di)(di)貌。


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