| Some 50 million years ago India collided with Tibet thrusting up these immense peaks, which are still rising. This vast barrier of rock and ice is so colossal it shapes the world's climate. Warm winds from India, full of moisture, are forced upwards by the Himalayas. As the air rises so it cools, causing clouds to form and the monsoon is born. At high altitudes the monsoon rains fall as snow. Here, at the far eastern end of the range in China, one inhabitant endures the bitter winters out in the open. Most other bears would be sleeping underground by now, but the giant panda can't fatten up enough to hibernate. | |
| 5000万年前，印度板块和西藏板块相互碰撞，形成了这些高大的山峰，而且它们还在上升。这些岩石和雪域如此巨大，它们甚至左右着世界的气候。从印度方向吹来的风，温暖湿润，喜马拉雅山迫使它上升，上升过程中，它变冷，形成云，于是就产生了季风。在高海拔地区，季风雨以降雪的形式出现。这里是喜马拉雅山脉最东端，中国境内。有一种动物正在野外忍受着严寒的冬天。此时其它大多数熊类正在冬眠，但是大熊猫没有足够的体膘让自己冬眠。 |
| Some 50 million years ago India collided with Tibet thrusting up these immense peaks, which are still rising. This vast barrier of rock and ice is so colossal it shapes the world' s climate. Warm winds from India, full of moisture, are forced upwards by the Himalayas. As the air rises so it cools, causing clouds to form and the monsoon is born. At high altitudes the monsoon rains fall as snow. Here, at the far eastern end of the range in China, one inhabitant endures the bitter winters out in the open. Most other bears would be sleeping underground by now, but the giant panda can' t fatten up enough to hibernate. | |
| 5000 wan nian qian, yin du ban kuai he xi zang ban kuai xiang hu peng zhuang, xing cheng le zhei xie gao da de shan feng, er qie ta men hai zai shang sheng. zhei xie yan shi he xue yu ru ci ju da, ta men shen zhi zuo you zhe shi jie de qi hou. cong yin du fang xiang chui lai de feng, wen nuan shi run, xi ma la ya shan po shi ta shang sheng, shang sheng guo cheng zhong, ta bian leng, xing cheng yun, yu shi jiu chan sheng le ji feng. zai gao hai ba di qu, ji feng yu yi jiang xue de xing shi chu xian. zhe li shi xi ma la ya shan mai zui dong duan, zhong guo jing nei. you yi zhong dong wu zheng zai ye wai ren shou zhe yan han de dong tian. ci shi qi ta da duo shu xiong lei zheng zai dong mian, dan shi da xiong mao mei you zu gou de ti biao rang zi ji dong mian. |
| Some 50 million years ago India collided with Tibet thrusting up these immense peaks, which are still rising. This vast barrier of rock and ice is so colossal it shapes the world' s climate. Warm winds from India, full of moisture, are forced upwards by the Himalayas. As the air rises so it cools, causing clouds to form and the monsoon is born. At high altitudes the monsoon rains fall as snow. Here, at the far eastern end of the range in China, one inhabitant endures the bitter winters out in the open. Most other bears would be sleeping underground by now, but the giant panda can' t fatten up enough to hibernate. | |
| 5000 wàn nián qián, yìn dù bǎn kuài hé xī zàng bǎn kuài xiāng hù pèng zhuàng, xíng chéng le zhèi xiē gāo dà de shān fēng, ér qiě tā men hái zài shàng shēng. zhèi xiē yán shí hé xuě yù rú cǐ jù dà, tā men shèn zhì zuǒ yòu zhe shì jiè de qì hòu. cóng yìn dù fāng xiàng chuī lái de fēng, wēn nuǎn shī rùn, xǐ mǎ lā yǎ shān pò shǐ tā shàng shēng, shàng shēng guò chéng zhōng, tā biàn lěng, xíng chéng yún, yú shì jiù chǎn shēng le jì fēng. zài gāo hǎi bá dì qū, jì fēng yǔ yǐ jiàng xuě de xíng shì chū xiàn. zhè lǐ shì xǐ mǎ lā yǎ shān mài zuì dōng duān, zhōng guó jìng nèi. yǒu yī zhǒng dòng wù zhèng zài yě wài rěn shòu zhe yán hán de dōng tiān. cǐ shí qí tā dà duō shù xióng lèi zhèng zài dōng mián, dàn shì dà xióng māo méi yǒu zú gòu de tǐ biāo ràng zì jǐ dōng mián. |
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