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冰川类型
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  glacier types
     During the last glaciation, the glacier types were wide-tail valley glacier, valley glacier and cirque glacier;
     冰川类型为宽尾山谷冰川、山谷冰川和冰斗冰川;
短句来源
  “冰川类型”译为未确定词的双语例句
     for a single glacier, the degree-day factors are subject to significant small-scale variations.
     从冰川类型来看,与极大陆型及亚大陆型冰川相比,海洋型冰川的度日因子较大。
短句来源
     The existing data indicate that the Zanda basin and its surrounding mountains are areas where the most abundant, complete and continuously occurring and best-preserved Quaternary glacial deposits are found on the Qinghai-Tibet Plateau.
     对应的冰川类型为:山谷、山麓及冰帽冰川发育阶段→大规模冰帽冰川发育阶段→冰帽、山谷及山麓冰川发育阶段。 现有资料研究表明,札达盆地及周缘高山区,是青藏高原第四纪冰川堆积发现最多、最全、分布最连续和保存最好的地区。
短句来源
  相似匹配句对
     Glacier Masterpieces
     冰川杰作
短句来源
     Types of Artificial Satellites
     人造卫星的类型
短句来源
     Glacier of the Qilian Mountain
     祁连山冰川
短句来源
     TYPE OBJECTS
     类型对象
短句来源
     During the last glaciation, the glacier types were wide-tail valley glacier, valley glacier and cirque glacier;
     冰川类型为宽尾山谷冰川、山谷冰川和冰斗冰川;
短句来源
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  glacier type
Debris flows vary in type, including glacier type and rainfall type, and have different distributions depending on their triggering factors.
      
No one method is ideal in all situations, and the best method depends on glacier type, catchment topography and climatic environment.
      
  glacier types
At present, a very wide range of glacier types exists in the tropics and Himalaya.
      
The geographic terminology is regrettable because the distribution of glacier types is not simply determined by latitude.
      


On the Tibetan Plateau, remnants of the quaternary glaciation are of general oc-curence. Cirques, U-shape valleys, glacial-scoured lakers, till plains, terminal moraines, and drift boulders are wide spread features down to 4200 m in altitude. The authors believe that there was once a fairly continuous ice cover on the Tibetan plateau in late pleistocene. Here after the snow-line was raised, and the glaciers retreated gradually to their present positions. The reasons are two-fold: (a) a general warming of the...

On the Tibetan Plateau, remnants of the quaternary glaciation are of general oc-curence. Cirques, U-shape valleys, glacial-scoured lakers, till plains, terminal moraines, and drift boulders are wide spread features down to 4200 m in altitude. The authors believe that there was once a fairly continuous ice cover on the Tibetan plateau in late pleistocene. Here after the snow-line was raised, and the glaciers retreated gradually to their present positions. The reasons are two-fold: (a) a general warming of the world climate, (b) dessication of Tibet due to further uplift. The latter is evidenced by the obvious shrinkage of many lakes on the plateau. By correlating the moraines of this glaciation with the terrace of Zi-Ling Tsangpo and Yamdrok, we reach at the conclusion that this great Ice Cover was of late pleistocene in age. Since that time the glacier retreated in three recessional stages:

王明业等同志这篇论文提供了不少西藏高原上古冰川沉积以及其他遗迹的资料。从这些遗迹的分布来看,肯定有一个时期冰川的范围远比现代为大,那时冰川会从一些山谷通过一些低的山口漫溢到另一些山谷中,会覆盖广大的山麓地区,甚至达到盆地的中心。也可以想见某些宽平的山顶上可能有平顶冰川或所谓冰帽覆盖。在这种情况下,冰川的厚度一定也比现代为大,冰川的类型也更复杂的多。但是对于西藏高原这样一个广大的地区来说,作者等的观察范围以及获得的资料究竟还是非常有限,在达到的地区内也未见到有巨厚的,延续很广的冰碛物存在,所以据此即说除雅鲁藏布江谷地和金沙江、澜沧江、怒江的峡谷外西藏高原断续出现的冰盖是相当普遍的(虽然作者等也声明说和格林兰、南极洲的冰盖不一样),结论似乎下得太早。所引waxler的关于晚更新世雪线下降随的资料仅适用于一般海洋性气候的冰川作用区,是否能用到象西藏这样大陆性很强的地区是值得怀疑的。但是无论如何,作者等的资料是很宝贵的,关于西藏高原古冰川覆盖类型的问题,目前也确实还难说孰是孰非,所以我们还是把本文发表出来,以供对西藏古冰川研究的参考。

Mount Taibai is the highest peak, in the Chinling range, its main peaknamed Baxiantai reaches 3767 meters above sea level. After analysis of the traces of glaciation on Mount Taibai are foundwiththe following characteristics: 1.Hanging cirque glaciers and little velley glaciers. 2.The paternaster lakes and rock steps, slightly advanceing and retreating. 3.The dual nature of continental glacier and maritime glacier, accord withthe geographical position of Mount Taibai. 4.According to the height of snow line (3,600M),...

Mount Taibai is the highest peak, in the Chinling range, its main peaknamed Baxiantai reaches 3767 meters above sea level. After analysis of the traces of glaciation on Mount Taibai are foundwiththe following characteristics: 1.Hanging cirque glaciers and little velley glaciers. 2.The paternaster lakes and rock steps, slightly advanceing and retreating. 3.The dual nature of continental glacier and maritime glacier, accord withthe geographical position of Mount Taibai. 4.According to the height of snow line (3,600M), the scope of glacia-tion, weathering of moraine, and distribution of this area of old block fi-eld and old block stream, indicate the glaciation corresponds to the ice ageof late pleistoncene's late phase.

太白山是秦岭山脉的最高地带,主峰八仙台海拔3767米。根据冰川遗迹的分析有以下几点特点: 1、属冰斗悬冰川和小型谷地冰川; 2、串珠状冰湖和冰坎发育,表明冰川虽属小型,但很活跃,有小的进退; 3、一方面具有大陆型低平衡冰川类型的特点,另一方面又表现为具有海洋性冰川的性格。这种具有双重性的特点与太白山所处的地理位置是统一的,即具过渡性性质; 4、从雪线的高度(海拔3600米)、冰川的规模(小型)、冰碛物的风化状况,以及较老石海、石河的分布,表明这一冰川作用可能与晚更新世晚期的冰期相当。

There are 8900 glaciers in the Tianshan Mts., with a total area of 9192.43 km2 and a total ice volume of 1010.5 km~3.These glaciers are mainly distributed in big and high mountains above 5000m a.s.l. in the western part of the mountains. Eastwards from here, the number of glaciers decrease, and the size of glaciers become smaller. Valley glaciers are mainly developed on very high peaks or the "mountain knot" of the Tianshan Mts, and their vertical elevation differences are commonly3600-4600m,which has resulted...

There are 8900 glaciers in the Tianshan Mts., with a total area of 9192.43 km2 and a total ice volume of 1010.5 km~3.These glaciers are mainly distributed in big and high mountains above 5000m a.s.l. in the western part of the mountains. Eastwards from here, the number of glaciers decrease, and the size of glaciers become smaller. Valley glaciers are mainly developed on very high peaks or the "mountain knot" of the Tianshan Mts, and their vertical elevation differences are commonly3600-4600m,which has resulted in the special complex glacier type in China. The glaciation grades in most of the rivers in the Tianshan Mountains are smaller than 0.20 and depend on the number of the valley glaciers and their sizes.

据最新编目资料,中国天山有冰川8900条,面积9192.43km~2,冰储量1010.5km~3,主要分布在西部5000m以上的高大山地,由此向东数量减少,规模变小。山谷冰川主要发育在高度巨大的山峰或山汇,垂直高差一般在3600—4600m,形成特有的复合冰川类型。大部河流的冰川作用等级在0.20以下,其大小取决于山谷型冰川的数量和个体规模。

 
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