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hanging valley
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  悬谷
     In spring 1982, Comrade Zhou Mo Lin went to Huangshan to make an investigation. He divided the vestiges of ancient glacier in Huangshan into,such as, angular crest, ice hopper, snow basic, U-valley, hanging valley, ice mortar, glacier streak rock, laxeral moraine, year round laxeral ridge, exc . This divition sinks unavoidably into a strained interprexation, so it causes an objection of the same trade.
     1982年春,周慕林同志来到黄山考察,对黄山古冰川遗迹配套式划分,如角峰、冰斗、积雪盆、U谷、悬谷、冰臼、冰川条痕石、侧碛、终碛垄等,这种划分不免陷于牵强附会,引起同行的异议。
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  “hanging valley”译为未确定词的双语例句
     When the draining type valley formed a karst reservoir, it can be divided into seepage hypotypes:such as weak karst with microseepage, strong karst, hanging valley, buried karst…etc.
     排泄型河谷岩溶水库划分为弱岩溶微渗漏、强岩溶渗漏、悬托型河谷渗漏、隐伏岩溶渗漏等亚型。
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  相似匹配句对
     The Hanging Man
     晃来晃去的人
短句来源
     VALLEY BULGING
     河谷外鼓
短句来源
     Death Valley
     死亡山谷
短句来源
     The Hanging Gardens of Babylon
     巴比伦空中花园
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  hanging valley
A small Holocene fan is forming where Queen Inlet, a hanging valley, enters West Arm fjord, Glacier Bay, Alaska.
      


The lower reaches of the Huangho river changed its way several times in the historic period. There were many reasons. One important reason among them is the influence of human activity. The paper discussed it in the following four sections.1) The course diverted due to the artificial burst of the banks in the war;2) The course diverted due to the artificial blocking, in order to make the Huangho return to its original course or to lead it to a new one;3) The influence of building banks artificially. For instance,after...

The lower reaches of the Huangho river changed its way several times in the historic period. There were many reasons. One important reason among them is the influence of human activity. The paper discussed it in the following four sections.1) The course diverted due to the artificial burst of the banks in the war;2) The course diverted due to the artificial blocking, in order to make the Huangho return to its original course or to lead it to a new one;3) The influence of building banks artificially. For instance,after banking up the river, the sediment deposition increased. It caused the bed level to be elevated over the adjacent area, making Huangho a "hanging valley".Another example is, the river pattern changed from branching to single way due to banking. Some lakes disappeard from this region caused by banking. 4) Agriculture and livestock husbandry developed alternately in the middle reaches of Huangho in the history.The condition of the forest vegetation and soil erosion, the relationship between burst in the lower reaches and the phenomena mentioned above in the middle reaches, is discussed briefly. The author concludes finally that the influence of the human activity mentioned above and the experiences from it should be remenbered not only in studying the history of Huangho diversion, but also in harnessing Huangho in the future. The author suggests that we should pay attention to the task in the middle reaches of Huangho while working in the lower reaches. Only by the conservation of soiland water and eliminating the sediment input from erosion in the middle reaches of Huangho, can there appear a new situation securely for a long time.

历史时期黄河下游发生过多次变迁,人类活动是影响变迁的重要因素。本文就此对战争中的人为决堤,治河中的人工挽堵、筑堤以及中游地区的农垦等方面的影响作了探讨。

In the past 60 years or so, many geologists and geomorphologists have advanced various views on the origin and evolution of the three gorges of the Changjiang(Yangtze)River. In the paper, which is mainly based on the field survey carried out during the last few years, the author advances the following idea. (1) The three gorges on the section of the Changjiang River from Fengjie to Yichang have sovaral features in common, For example, they are all charactericed by incisedelbows and ancient broad-valleys,...

In the past 60 years or so, many geologists and geomorphologists have advanced various views on the origin and evolution of the three gorges of the Changjiang(Yangtze)River. In the paper, which is mainly based on the field survey carried out during the last few years, the author advances the following idea. (1) The three gorges on the section of the Changjiang River from Fengjie to Yichang have sovaral features in common, For example, they are all charactericed by incisedelbows and ancient broad-valleys, etc. These features show that they were very similar in forming process and resulted from headward erosion and river captures Caused by the uplift of the Three-Gorge region since the Tertiary period. (2) Bat the three gorges each have their own features of shape. This indicates that they wore formed in different ages and experienced different stages of development. The Qu Tang Gorge, uppermost of the three gorges, Is in the stage of youth for its wall is intact. The Xi Ling Gorge, lowest of them, has many hanging valleys and Some benchas on the walls. So it appears to consist of many massive columns. It is a rejuvenescent gorge. The We Gorge, its wall being a series of triangle surfaces, is in the stage of maturity. (3) Based on the studies of the relative deposits containing a large number of grano-dedris, the Changjiang River linked up two big basins(the Si Chuan Basin and the Jiang Han Basin)about 200±20×10~4 years ago.

关于长江三峡的起源与演变,60多年来诸多地质学家和地貌学家提出了种种不同的看法。本文主要根据近几年野外调查,提出如下见解。 1 长江上的三个峡,在地貌上有许多共同的特点,它们是在第三纪以来三峡地区构造上升的基础上通过溯源深切与河流袭夺贯通的。 2 这三个峡尚有各自的特点,表明它们的形成时代与峡谷的发展阶段是不一样的,其中瞿塘峡处青年期,巫峡处壮年期,西陵峡处回春发展时期。 3 据峡外的相关沉积的形成时代,推断长江三峡是在距今200±20万年前贯通的

In the past 60 years or so, many geologists and geomorphologists have advanced variotus views on the origin and evolution of the three gorges of the Changjiang (Yangtze) River. In the paper, which is mainly based on the field survey carried oat daring the last few years, the author advances the following idea. (1) The three gorges on the section of the Changjiang River from Fengjie to Yichang have several features in common, For example, they are all charactericed by incisedelbows and ancient broad-valleys,...

In the past 60 years or so, many geologists and geomorphologists have advanced variotus views on the origin and evolution of the three gorges of the Changjiang (Yangtze) River. In the paper, which is mainly based on the field survey carried oat daring the last few years, the author advances the following idea. (1) The three gorges on the section of the Changjiang River from Fengjie to Yichang have several features in common, For example, they are all charactericed by incisedelbows and ancient broad-valleys, etc. These features show that they were very similar in forming process and resulted from headward erosion and river captures Caused by the uplift of the Three-Gorge region since the Tertiary period, (2) But the three gorges each have their own features of shape. This indicates that they were. formed in different ages and experienced different stages of development. The Qu Tang Gorge, uppermost of the three gorges, Is in the staga of youth for its wall is intact. The Xi Ling Gorge, lowest of them, has many hanging valleys and Some benches on the walls. So it appears to consist of many massive columns. It is a rejuvenescent gorge. The We Gorge, its wall being a series of triangle surfaces, is in the stage of maturity. (3) Based on the studies of the relative deposits containing a large number of grano-dedris, the Changjiang River linked up two big baslns(the Si Chuan Basin and the Jiang Hen Basin) about 200±20×10~4 years ago.

关于长江三峡的起源与演变,60多年来许多地质学家和地貌学家提出了种种不同的看法。本文主要根据近几年野外调查,提出如下见解。 1 长江上的三个峡,在地貌上有许多共同的特点,它们是在第三纪以来三峡地区构造上升的基础上通过溯源深切与河流袭夺贯通的。 2 这三个峡尚有各自的特点,表明它们的形成时代与峡谷的发展阶段是不一样的,其中瞿塘峡处青年期,巫峡处壮年期,西陵峡处回春发展时期。 3 据峡外的相关沉积的形成时代,推断长江三峡是在距今200±20万年前贯通的

 
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