嶂
1、(形声。从山,章声。本义:高险的山,如屏障的山峰)同本义。
嶂,峰嶂。---《广韵》
嶂,山峰如屏障也。---《增韵》
千嶂里,长烟落日孤城闭。---宋·范仲淹《渔家傲》
嶂表:山外
嶂气
该公司对这嶂大厦拥有绝对产权。
The company has an absolute interest in the building.
北人堕泪南人笑,青嶂无梯闻杜鹃。
North Duolei Penan people laugh, green peaks no ladder heard the cuckoo.
鹅凰嶂,传说是神仙的故居。
The sagas tell that E Huang was the hometown of gods.
水波潋滟,山峦重嶂,但又怎比这水仙的舞步翩跹。
The waves were beside the daffodils and the mountains around them.
现在他只是拥有一个简单的身份,金毓嶂【1】先生。
Now, he's a simple mister Jin Yuzhang.
终于攀登到顶,1003米的白云嶂,我们征服了你!
Got to the top finally, 1003 meter high, Baiyunzhang, we conquered you!
金毓嶂先生:最后,他为了国家和谐和社会进步献出了自己生命。
Mr. JIN YUZHANG (Guangxu Relative): (Though Translator) In the end, he sacrificed his life for the sake of national unity and social progress.
金口大峡谷位于大渡河下游,主要支谷有8条,皆以嶂谷地貌为特色。
The Jinkou Grand Canyon is situated in the lower reaches of Dadu River with 8 chief branch gorges.
塞下秋来风景异,衡阳雁去无留意。四面边声连角起。千嶂里,长烟落日孤城闭。
Plug under the autumn scenery, Hengyang go without attention. From all sides of the sound from the angle. The thousand peaks in the sunset in the closed.
矿床赋存于白石嶂花岗岩体南东端之南西侧内外接触带及F19断裂的上下盘附近。
The deposit occurs near the internal and external contact zones at the southwest side of southeast end of Baishizhang granite as well as hanging wall and footwall of F19 fracture.
赣南—粤北地区鸡笼嶂组是一套以酸性火山岩为主的岩石组合,属晚侏罗世莲花寨群。
The Jilongzhang Formation in the South Jiangxi-North Guangdong area is a suite of volcanic rocks dominated by acid composition, Which can be attributed to the Late Jurassic Lianhuazhai Group.
西北山区最高峰为观音峰,海拔1429米,南部山区最高山峰为青嶂山,海拔917米。
Northwest mountain peak as the Goddess of Mercy Peak, elevation 1429 meters, the highest peaks of the mountains of southern blue mountain peaks, elevation 917 meters.
更新世阶段地壳迅速的抬升、外力的物理风化作用,特别是晚更新世间歇性山区洪水的冲蚀,是形成嶂谷的直接原因。
The rapid crustal uplift in the Pleistocene and physical weathering and erosion, especially the erosional process of the flood in the mountains, are the direct causes for the formation of the gorges.
更新世阶段地壳迅速的抬升、外力的物理风化作用,特别是晚更新世间歇性山区洪水的冲蚀,是形成嶂谷的直接原因。
The rapid crustal uplift in the Pleistocene and physical weathering and erosion, especially the erosional process of the flood in the mountains, are the direct causes for the formation of the gorges.