| British Columbia is the third largest Canadian provinces, both in area and population. It is nearly 1.5 times as large as Texas, and extends 800 miles(1,280km) north from the United States border. It includes Canada’s entire west coast and the islands just off the coast. Most of British Columbia is mountainous, with long rugged ranges running north and south. Even the coastal islands are the remains of a mountain range that existed thousands of years ago. During the last Ice Age, this range was scoured by glaciers until most of it was beneath the sea. Its peaks now show as islands scattered along the coast. The southwestern coastal region has a humid mild marine climate. Sea winds that blow inland from the west are warmed by a current of warm water that flows through the Pacific Ocean. As a result, winter temperatures average above freezing and summers are mild. These warm western winds also carry moisture from the ocean. Inland from the coast, the winds from the Pacific meet the mountain barriers of the coastal ranges and the Rocky Mountains. As they rise to cross the mountains, the winds are cooled, and their moisture begins to fall as rain. On some of the western slopes almost 200 inches (500cm) of rain fall each year. More than half of British Columbia is heavily forested. On mountain slopes that receive plentiful rainfall, huge Douglas firs rise in towering columns. These forest giants often grow to be as much as 300 feet(90m) tall, with diameters up to 10 feet(3m). More lumber is produced from these trees than from any other kind of tree in North America. Hemlock, red cedar, and balsam fir are among the other trees found in British Columbia. | |
| 英属哥伦比亚是加拿大的第三大省，无论是面积还是人口都是如此。它几乎是德克萨斯的1.5倍，从美国边境一直向北延伸了800英里(1，280 公里)。它包括了加拿大整个西海岸及附近岛屿。 大部分英属哥伦比亚多山峦。绵长而粗犷的山脉贯通南北。甚至那些沿海的岛屿都是那些存在于千万年前的山脉的遗迹。在上一个冰河时期，这些山脉被冰河冲刷侵蚀，直到大部分山脉被淹没在海中。它们的峰顶显现为沿着海岸散布的岛屿。 西南海岸地区有着潮湿温和的海洋性气候。从太平洋来的温暖的洋流使得从西吹过内陆的海风变得温暖。因此这儿冬天平均气温在零上而且夏天也不会酷热。这些温暖的西风同样也从海洋带来了湿气。 来自太平洋的、从海岸向内陆的风遇到海岸山脉和落基山脉这些山脉屏障。当气流升高跨越这些山脉时，风的温度就降低了，风中的水分形成降雨。在一些朝西 山坡区域每年大约有200英寸(500厘米)的降水。 大部分英属哥伦比亚密布着森林。在有充足降水的斜坡，巨大的道格拉斯枞树高耸入云。这些森林巨人常常长到高达300英尺(90米)，直径粗达10英尺(3米)。这些树产出了比北美其他任何树都多的木材。铁杉、红香椿、香脂冷杉枞都是发现于英属哥伦比亚的其它树种。 |
| British Columbia is the third largest Canadian provinces, both in area and population. It is nearly 1. 5 times as large as Texas, and extends 800 miles 1, 280km north from the United States border. It includes Canada' s entire west coast and the islands just off the coast. Most of British Columbia is mountainous, with long rugged ranges running north and south. Even the coastal islands are the remains of a mountain range that existed thousands of years ago. During the last Ice Age, this range was scoured by glaciers until most of it was beneath the sea. Its peaks now show as islands scattered along the coast. The southwestern coastal region has a humid mild marine climate. Sea winds that blow inland from the west are warmed by a current of warm water that flows through the Pacific Ocean. As a result, winter temperatures average above freezing and summers are mild. These warm western winds also carry moisture from the ocean. Inland from the coast, the winds from the Pacific meet the mountain barriers of the coastal ranges and the Rocky Mountains. As they rise to cross the mountains, the winds are cooled, and their moisture begins to fall as rain. On some of the western slopes almost 200 inches 500cm of rain fall each year. More than half of British Columbia is heavily forested. On mountain slopes that receive plentiful rainfall, huge Douglas firs rise in towering columns. These forest giants often grow to be as much as 300 feet 90m tall, with diameters up to 10 feet 3m. More lumber is produced from these trees than from any other kind of tree in North America. Hemlock, red cedar, and balsam fir are among the other trees found in British Columbia. | |
| ying shu ge lun bi ya shi jia na da de di san da sheng, wu lun shi mian ji hai shi ren kou dou shi ru ci. ta ji hu shi de ke sa si de 1. 5 bei, cong mei guo bian jing yi zhi xiang bei yan shen le 800 ying li 1, 280 gong li. ta bao kuo le jia na da zheng ge xi hai an ji fu jin dao yu. da bu fen ying shu ge lun bi ya duo shan luan. mian chang er cu guang de shan mai guan tong nan bei. shen zhi nei xie yan hai de dao yu dou shi nei xie cun zai yu qian wan nian qian de shan mai de yi ji. zai shang yi ge bing he shi qi, zhei xie shan mai bei bing he chong shua qin shi, zhi dao da bu fen shan mai bei yan mo zai hai zhong. ta men de feng ding xian xian wei yan zhe hai an san bu de dao yu. xi nan hai an di qu you zhe chao shi wen he de hai yang xing qi hou. cong tai ping yang lai de wen nuan de yang liu shi de cong xi chui guo nei lu de hai feng bian de wen nuan. yin ci zhe er dong tian ping jun qi wen zai ling shang er qie xia tian ye bu hui ku re. zhei xie wen nuan de xi feng tong yang ye cong hai yang dai lai le shi qi. lai zi tai ping yang de cong hai an xiang nei lu de feng yu dao hai an shan mai he luo ji shan mai zhei xie shan mai ping zhang. dang qi liu sheng gao kua yue zhei xie shan mai shi, feng de wen du jiu jiang di le, feng zhong de shui fen xing cheng jiang yu. zai yi xie chao xi shan po qu yu mei nian da yue you 200 ying cun 500 li mi de jiang shui. da bu fen ying shu ge lun bi ya mi bu zhe sen lin. zai you chong zu jiang shui de xie po, ju da de dao ge la si cong shu gao song ru yun. zhei xie sen lin ju ren chang chang zhang dao gao da 300 ying chi 90 mi, zhi jing cu da 10 ying chi 3 mi. zhei xie shu chan chu le bi bei mei qi ta ren he shu dou duo de mu cai. tie shan hong xiang chun xiang zhi leng shan cong dou shi fa xian yu ying shu ge lun bi ya de qi ta shu zhong. |
| British Columbia is the third largest Canadian provinces, both in area and population. It is nearly 1. 5 times as large as Texas, and extends 800 miles 1, 280km north from the United States border. It includes Canada' s entire west coast and the islands just off the coast. Most of British Columbia is mountainous, with long rugged ranges running north and south. Even the coastal islands are the remains of a mountain range that existed thousands of years ago. During the last Ice Age, this range was scoured by glaciers until most of it was beneath the sea. Its peaks now show as islands scattered along the coast. The southwestern coastal region has a humid mild marine climate. Sea winds that blow inland from the west are warmed by a current of warm water that flows through the Pacific Ocean. As a result, winter temperatures average above freezing and summers are mild. These warm western winds also carry moisture from the ocean. Inland from the coast, the winds from the Pacific meet the mountain barriers of the coastal ranges and the Rocky Mountains. As they rise to cross the mountains, the winds are cooled, and their moisture begins to fall as rain. On some of the western slopes almost 200 inches 500cm of rain fall each year. More than half of British Columbia is heavily forested. On mountain slopes that receive plentiful rainfall, huge Douglas firs rise in towering columns. These forest giants often grow to be as much as 300 feet 90m tall, with diameters up to 10 feet 3m. More lumber is produced from these trees than from any other kind of tree in North America. Hemlock, red cedar, and balsam fir are among the other trees found in British Columbia. | |
| yīng shǔ gē lún bǐ yà shì jiā ná dà de dì sān dà shěng, wú lùn shì miàn jī hái shì rén kǒu dōu shì rú cǐ. tā jī hū shì dé kè sà sī de 1. 5 bèi, cóng měi guó biān jìng yī zhí xiàng běi yán shēn le 800 yīng lǐ 1, 280 gōng lǐ. tā bāo kuò le jiā ná dà zhěng gè xī hǎi àn jí fù jìn dǎo yǔ. dà bù fèn yīng shǔ gē lún bǐ yà duō shān luán. mián cháng ér cū guǎng de shān mài guàn tōng nán běi. shèn zhì nèi xiē yán hǎi de dǎo yǔ dōu shì nèi xiē cún zài yú qiān wàn nián qián de shān mài de yí jī. zài shàng yī ge bīng hé shí qī, zhèi xiē shān mài bèi bīng hé chōng shuā qīn shí, zhí dào dà bù fèn shān mài bèi yān mò zài hǎi zhōng. tā men de fēng dǐng xiǎn xiàn wèi yán zhe hǎi àn sàn bù de dǎo yǔ. xī nán hǎi àn dì qū yǒu zhe cháo shī wēn hé de hǎi yáng xìng qì hòu. cóng tài píng yáng lái de wēn nuǎn de yáng liú shǐ de cóng xī chuī guò nèi lù de hǎi fēng biàn de wēn nuǎn. yīn cǐ zhè ér dōng tiān píng jūn qì wēn zài líng shàng ér qiě xià tiān yě bú huì kù rè. zhèi xiē wēn nuǎn de xī fēng tóng yàng yě cóng hǎi yáng dài lái le shī qì. lái zì tài píng yáng de cóng hǎi àn xiàng nèi lù de fēng yù dào hǎi àn shān mài hé luò jī shān mài zhèi xiē shān mài píng zhàng. dāng qì liú shēng gāo kuà yuè zhèi xiē shān mài shí, fēng de wēn dù jiù jiàng dī le, fēng zhōng de shuǐ fèn xíng chéng jiàng yǔ. zài yī xiē cháo xī shān pō qū yù měi nián dà yuē yǒu 200 yīng cùn 500 lí mǐ de jiàng shuǐ. dà bù fèn yīng shǔ gē lún bǐ yà mì bù zhe sēn lín. zài yǒu chōng zú jiàng shuǐ de xié pō, jù dà de dào gé lā sī cōng shù gāo sǒng rù yún. zhèi xiē sēn lín jù rén cháng cháng zhǎng dào gāo dá 300 yīng chǐ 90 mǐ, zhí jìng cū dá 10 yīng chǐ 3 mǐ. zhèi xiē shù chǎn chū le bǐ běi měi qí tā rèn hé shù dōu duō de mù cái. tiě shān hóng xiāng chūn xiāng zhī lěng shān cōng dōu shì fā xiàn yú yīng shǔ gē lún bǐ yà de qí tā shù zhǒng. |
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