丘狀起伏的 的英文怎麼說

中文拼音 [qiūzhuàngqǐfúde]
丘狀起伏的 英文
hummocky
  • 丘 : 名詞1. （小土山; 土堆） mound; hillock 2. （墳） grave 3. （姓氏） a surname
  • 狀 : Ⅰ名詞1 （形狀） form; shape 2 （情況） state; condition; situation; circumstances 3 （陳述事件或...
  • 起 : 起Ⅰ動詞1 （站起; 坐起） rise; get up; stand up 2 （取出; 取走） draw out; remove; extract; pull 3...
  • 伏 : Ⅰ動詞1 （身體向前靠在物體上; 趴） bend over; lie prostrate 2 （低下去） subside; go down 3 （隱藏...
  • 的 : 4次方是 The fourth power of 2 is direction
  • 丘狀 : moundy
  • 起伏 : rise and fall; ups and downs; heave rolling; undulate; fluctuate
  1. Because the road line is in mountainous region and heavy hilly area and its surface relief undulates greatly, more slope wash and dilurial layer distribution, there are more harm, for example, island shaped perennially frozen soil, drift ice and so on, which effect the stability of the road foundation

    由於沿線地處山嶺重丘地區，地勢起伏較大，坡積物及洪積層分佈較多。故島狀多年凍土、涎流冰等病害較多，影響路基的穩定。
  2. Nestled deep in the green hills of west virginia, a dish-shaped telescope keeps an unceasing vigil on the sky.

    在西弗吉尼亞州綠丘起伏的深處，一個盤狀的射電望遠鏡一直毫不間斷地監視著天空。
  3. Relatively flat or undulating sandy turf - covered ground usually along a seashore

    砂丘相對平坦或有波狀起伏的覆草沙地，通常在海岸邊
  4. But the conflict between them was appeared during our research in field and the discussion with others. it is followed that the former with the rolling bedrock, the mid with mild bedrock and the latter with the stable bedrock relatively. the conflict between two conclusion above arise, what relationship between loess landforms and their bedrock exist

    但在野外調查及同其他學者交流中發現兩者並非總體對應一致，顯示出陜北黃土高原南部黃土塬基底起伏相對較大，北部黃土梁狀（為主）丘陵溝壑區及黃土峁狀（為主）丘陵溝壑區基底相對平坦的特徵。
  5. The unconformability between the loess landform of shaanbei loess plateau and its bedrock shape was pointed out first after the full demonstration. the top of loess formation of the south part in shaanbei is flat which likes " platform ", the shape of the bedrock is rolling that likes ridge, and the bedrock bended to fold. the top of loess formation of the mid - part in shaanbei is rolling, but the shape of the bedrock below begins to get flat, the top of loess formation of the north part in shaanbei, loess mao district, is much more rolling among them, however, its shape of the bedrock below is the flattest relatively likes the platform shape of loess formation in south

    具體地講，陜北高原南部的洛） 11黃土源，黃上層頂部相對平坦，地貌類型以黃土源為主格調，而其下伏基巖地層詔皺相對發育，古地勢起伏相對較大：陜北高原中部的延安一安塞黃土梁狀（為主）丘陵溝壑區，黃土層頂部起伏相對增大，地貌類型以黃土梁為主格調，而其下伏基巖地層槽皺程度趨弱，地層較平緩，古地勢起伏相對降低；陜北高原北部的綏德一子洲黃土赤狀（為主）丘陵溝壑區，黃土層頂部起伏度相對最大，地貌類型以黃上赤為主格調，而其下伏基底地層以平緩為特徵，古地勢起伏強度亦相對較低。
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