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地理气候

地质地貌
2022-12-14    【字体:

工(gong)(gong)(gong)程(cheng)(cheng)工(gong)(gong)(gong)程(cheng)(cheng)工(gong)(gong)(gong)程(cheng)(cheng)地(di)(di)(di)(di)质(zhi)(zhi)土壤(rang)类型在(zai)工(gong)(gong)(gong)程(cheng)(cheng)工(gong)(gong)(gong)程(cheng)(cheng)工(go🏅ng)(gong)(gong)程(cheng)(cheng)地(di)(di)(di)(di)质(zhi)(zhi)上,曲周(zhou)(zhou)县(xian)属海拒马河(he)(he)(he)域,是(shi)中生(sheng)代到晚期进行(xing)的(de)的(de)自主的(de)工(gong)(gong)(gong)程(cheng)(cheng)工(gong)(gong)(gong)程(cheng)(cheng)工(gong)(gong)(gong)程(cheng)(cheng)地(di)(di)(di)(di)质(zhi)(zhi)空间结构机(ji)组(zu)。在(zai)古地(di)(di)(di)(di)球表面(mian)时候,犹豫地(di)(di)(di)(di)壳的(de)搬家,曲周(zhou)(zhou)县(xian)区呈拗陷崎岖交叠睡眠(mian)状(zhuang)态,到3、纪(ji)末被大批的(de)陆相堆(dui)积(ji)(ji)(ji)(ji)作用(yong)物填(tian)平(ping),变成 的(de)統一的(de)拗陷堆(dui)积(ji)(ji)(ji)(ji)作用(yong)冲(chong)积(ji)(ji)(ji)(ji)丘陵(ling)(ling),已后(hou)进行(xing)长(zhang)久的(de)堆(dui)积(ji)(ji)(ji)(ji)作用(yong),特(te)点是(shi)大河(he)(he)(he)、漳(zhang)河(he)(he)(he)、洺河(he)(he)(he)、沙(sha)河(he)(he)(he)的(de)冲(chong)积(ji)(ji)(ji)(ji),日渐进行(xing)昨天的(de)冲(chong)积(ji)(ji)(ji)(ji)冲(chong)积(ji)(ji)(ji)(ji)丘陵(ling)(ling)。地(di)(di)(di)(di)标高(黄河(he)(he)(he))在(zai)45.4至(zhi)32.7米(mi)之间。地(di)(di)(di)(di)势由西南向东北倾(qing)斜,地(di)(di)(di)(di)面(mian)降(jiang)坡(po)1/3000左右,地(di)(di)(di)(di)势平(ping)坦。历史上因(yin)境(jing)内河(he)(he)(he)流经常(chang)泛滥,受其冲(chong)积(ji)(ji)(ji)(ji)的(de)影响,境(jing)内形成冲(chong)积(ji)(ji)(ji)(ji)堆(dui)、扇形地(di)(di)(di)(di)、缓(huan)岗缓(huan)坡(po)地(di)(di)(di)(di)等复杂地(di)(di)(di)(di)貌(mao)。


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