plateau top 中文意思是什麼

plateau top 解釋
高原頂面
  • plateau : n (pl x s )1 高原,臺地,高地;【心理學】學習高原〈指學習上無進步也無退步的一段〉;〈美喻〉平穩...
  • top : n (opp bottom foot)1 頂,頂部,頂端。2 頭,頭頂;尖端;樹梢,樹頂;(事物的)上層部分。3 最高位...
  1. Now when we arrive at their village for a research trip, they round up three camels to carry our camping equipment, food and water, and we all walk to the top of the plateau and set up camp

    現在我們每次為了研究而拜訪他們村落時,他們都會張羅好三隻駱駝,來馱運我們扎營所需的裝備、食物和水,接著我們會徒步走上高原,然後扎營。
  2. The top of the plateau was dotted thickly with pine trees of varying height

    高矮不一的松樹星羅棋布地點綴在高地上。
  3. But they base on the different cosmos dimensions : the first representation bases on the dualism between the upward and the downward ; the second one on the concept of personhood that ohen is inside gvmu, and ohen ' s door is on the top of head ; and the third one is related to the concept of sa, the implying meaning - of offering flowers is offering the blooming sa of flowers, which is without stable shape, even though there appears no - sa symbols such as flowers made of babboo and paper, and fir boughs taken from high plateau in ritual representations

    跪拜、脫帽和獻花都表示景仰,但它們各自生發意義的根抵並不相同:跪拜基於上與下二元對立認知模式;脫帽的意義來自魂靈內在於身體,以身體天靈蓋部位為出入之門的人觀理念;獻花的實質是獻花兒綻放出的花之「薩」 ,雖然儀式中己出現單純表達性的象徵替代品一一竹紙花圈和冷杉枝。
  4. 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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