英文介绍贵州主要旅游景点(英文介绍贵州的景点)

导读:英文介绍贵州主要旅游景点(英文介绍贵州的景点) 用英文介绍黄果树瀑布 谁能用英语介绍下贵州,包括location 特产,景点 历史等等 急求贵州特别著名的几个旅游景点介绍,需要中英文互译,谢谢!

用英文介绍黄果树瀑布

Huangguoshu Waterfall is Huangguoshu Waterfall. Baishuihe Waterfall, also known as "Huanggeshu" waterfall or "Huanggeshu" waterfall, is named because of the widespread distribution of "Huanggebanyan" in this area.

黄果树瀑布,即黄果树大瀑布。古称白水河瀑布,亦名“黄葛墅”瀑布或“黄桷树”瀑布,因本地广泛分布着“黄葛榕”而得名。

Located in Zhenning Buyi and Miao Autonomous County, Anshun City, Guizhou Province, China, it belongs to the Baishui Reach of the lower reaches of the Kebu River, a tributary of the Dabang River, a branch of the Nanpan River, the main stream of the Xijiang River.

It is the largest first-class waterfall in the Huangguoshu Waterfall Group and one of the world's famous waterfalls.

位于中国贵州安顺镇宁布依族苗族自治县,属珠江水系西江干南盘江支流北盘江支流打帮河的支流可布河下游白水河段水系,为黄果树瀑布群中规模最大的一级瀑布,是世界著名大瀑布之一。

扩展资料:

黄果树大瀑布的成因:

黄果树大瀑布的成因要上溯至2亿多年前的中三叠纪,那时黄果树一带沉积了一套巨厚的碳酸盐岩。黄果树瀑布发育在一套“中三叠世中统关岭二段中厚层夹少量薄层状云灰岩”中,位置在翁寨小背斜东翼。

黄果树瀑布形成时期的白水河,是一条发育于距今10万—50万年之间,第四纪中、晚更新世时期由“宽谷期”向“峡谷期”演化中的地上河流,后因“喜马拉雅运动”时期地壳多次间歇抬升,引起河流侵蚀基准面下降,导致河流的侵蚀、溶蚀等下切作用加强;

在该处形成“裂点”(河床因地壳抬升、侵蚀基准面下降及构造、岩性等因素的影响而发生较大转折处),这个裂点处的裂隙、溶洞暗河非常发育。

谁能用英语介绍下贵州,包括location 特产,景点 历史等等

Guizhou Province, referred to as "Qian" and "expensive" is a beautiful mountains and rivers, climate, resource rich nation a large number of inland mountainous province.

Its name comes from the mountain with your name.

Tang Guizhou Road; Song is Interpreting Road; yuan is Huguang province; next home Guizhou toast,

Is named for the start of Guizhou, Guizhou, administrative commissioner's office after the home; clear change in Guizhou Province, the provincial name has not changed. 贵州省简称“黔”和“贵”,是一个山川秀丽、气候宜人、资源富集、民族众多的内陆山区省。

其名称来源于以贵山得名。

唐为黔中道;宋属夔州路;元属湖广行省;明置贵州土司

是为贵州得名的开始,后置贵州布政使司;清改贵州省,省名至今未变。Guizhou is located in Yunnan-Guizhou Plateau, between east longitude 103 ° 36 '~ 109 ° 35', latitude 24 ° 37 '~ 29 ° 13' between the east by Hunan, Guangxi, south, west adjoin Yunnan, north Sichuan and Chongqing, something about 595 km north-south distance of about 509 km. The province's total land area of 176,167 square kilometers, accounting for 1.8% of the total area.

Guizhou Plateau in western China landforms are mountains, in the terrain from west to east, from the central north, east, south and tilted on three sides, with an average altitude of 1100 meters. Mostly mountainous Guizhou Plateau, known as "Eight mountains of water a sub-field" theory. The province's landscape can be broadly divided into: Plateau mountains, hills and basins are three basic types, of which 92.5% of the area is mountains and hills. Mountains in large, heavy mountain ranges overlapping peaks, rolling horizon, a high mountain a deep valley. Big Lou northern mountains, from west to northeast slope consistent throughout the north, Sichuan-Guizhou strategic pass Loushanguan 1444 meters high; south-central Miaoling span, 2178 meters high mountain peak leigong; northeastern border with Wuling Mountain by the winds into the Hunan Guizhou, the main peak Fanjingshan 2572 meters high; the western high-rise wumeng shan, belong to this mountain village Hezhang County Pearl City, 2900.6 meters above sea level chives ping, the highest point in Guizhou. The Qiandongnan of Liping County Tsubosato River outlet at a provincial boundary, elevation of 147.8 meters, the lowest point for the territory. Guizhou karst landforms are very typical. Karst (exposed) area of 109,084 square kilometers, accounting for 61.9% of the province's total land area, the distribution of karst in a wide range of morphological types is complete, the geographical distribution of clearly constitutes a special kind of karst ecosystem. 贵州地处云贵高原,介于东经103°36′~109°35′、北纬24°37′~29°13′之间,东靠湖南,南邻广西,西毗云南,北连四川重庆,东西长约595千米,南北相距约509千米。全省土地总面积176167平方千米,占全国总面积的1.8%。

贵州地貌属于中国西部高原山地,境内地势西高东低,自中部向北、东、南三面倾斜,平均海拔在1100米左右。贵州高原山地居多,素有“八山一水一分田”之说。全省地貌可概括分为:高原山地、丘陵和盆地三种基本类型,其中92.5%的面积为山地和丘陵。境内山脉众多,重峦叠峰,绵延纵横,山高谷深。北部有大娄山,自西向东北斜贯北境,川黔要隘娄山关高 1444米;中南部苗岭横亘,主峰雷公山高2178米;东北境有武陵山,由湘蜿蜒入黔,主峰梵净山高2572米;西部高耸乌蒙山,属此山脉的赫章县珠市乡韭菜坪海拔2900.6米,为贵州境 内最高点。而黔东南州黎平县地坪乡水口河出省界处,海拔为147.8米,为境内最低点。贵州岩溶地貌发育非常典型。喀斯特(出露)面积109084平方千米,占全省国土总面积的61.9 %,境内岩溶分布范围广泛,形态类型齐全,地域分布明显,构成一种特殊的岩溶生态系统 。Guizhou's climate is warm and humid, subtropical humid monsoon climate. Temperature changes little, cool and pleasant weather. In particular, be liable to a unique climate. In 2002, the provincial capital Guiyang city, the average annual temperature is 14.8 ℃, compared with last year increased 0.3 ℃. From the provincial perspective, usually the coldest month (January) average temperature over the 3 ℃ ~ 6 ℃, higher than in other parts of the same latitude; the hottest month (July) mean temperature is generally 22 ℃ ~ 25 ℃, the typical summer cool area. Precipitation are more significant during the rainy season, cloudy much less sunshine. In 2002, nine states in the host city of cities, precipitation is at most Xingyi City, 1,480 millimeters; at least the Bijie City of 687.9 millimeters. Affected by the monsoon rainfall are more concentrated in the summer. Generally cloudy days throughout the territory of more than 150 days, annual relative humidity above 70%. Affected by the impacts of atmospheric circulation and topography, climate in Guizhou was diversity, "mountain the season, ten-mile different days." In addition, climate instability, more types of severe weather, drought, autumn, Ling cold, the frequency of large hail, etc., to cause serious harm to agricultural production. 贵州的气候温暖湿润,属亚热带湿润季风气候。气温变化小,冬暖夏凉,气候宜人。特别是气候独特的可处。2002 年,省会贵阳市年平均气温为14.8℃,比上年提高0.3℃。从全省看,通常最冷月(1月)平均 气温多在3℃~6℃,比同纬度其他地区高;最热月(7月)平均气温一般是22℃~25℃,为典型夏凉地区。降水较多,雨季明显,阴天多,日照少。2002年,9个市州地所在城市中,降水量最多是兴义市,为1480毫米;最少的是毕节市,为687.9毫米。受季风影响降水多集中于夏季。境内各地阴天日数一般超过150天,常年相对湿度在70%以上。受大气环流及地形等影响,贵州气候呈多样性,“一山分四季,十里不同天”。另外,气候不稳定,灾害性天气种类较多,干旱、秋风、凌冻、冰雹等频度大,对农业生产危害严重。Guizhou soil a total area of 159.1 thousand square kilometers, accounting for 90.4% of the province's land area, the soil is a zone of red soil in subtropical evergreen broad-leaved forest - yellow soil zone. Large areas of central and eastern part of the moist evergreen broad-leaved forest dominated by yellow; southwest of partial dry evergreen broad-leaved forest dominated by red soil; the north-west of North Asia hot ingredients with evergreen broad-leaved fores t , mostly yellow brown. In addition, there are constrained by the parent rock of the limestone soil and purple soil, and thick bone soil, paddy soil, brown soil, tidal soil, peat soil, swamp soil, coal soil, rocky soil, mountain meadow soil, red clay, the new plot soil and other soil types. For agricultural production, the amount of soil resources in Guizhou is obviously insufficient, can be used for agriculture, forestry and animal husbandry of the soil accounts for only 83.7% of the total area of the province. 贵州土壤面积共159100平方千米,占全省土地面积的90.4%,土壤的地带性属中亚热带常绿阔叶林红壤—黄壤地带。中部及东部广大地区为湿润性常绿阔叶林带,以黄壤为主;西南部为偏干性常绿阔叶林带,以红壤为主;西北部为具北亚热成分的常绿阔叶林带,多为黄棕壤 。此外,还有受母岩制约的石灰土和紫色土、粗骨土、水稻土、棕壤、潮土、泥炭土、沼泽土、石炭土、石质土、山地草甸土、红粘土、新积土等土类。对于农业生产而言,贵州土壤 资源数量明显不足,可用于农、林、牧业的土壤仅占全省总面积的83.7%。Guizhou, rich vegetation, with significant sub-tropical nature of the composition of a wide range of flora complex composition. The province of vascular plants (excluding bryophytes) a total of 269 subjects, 1655 genera and 6255 kinds (varieties). Flora of tropical and sub-tropical nature of the distinct advantage of geographical elements, such as the pan-tropical distribution of tropical Asia, the Old World tropical distribution of geographical elements account for a large proportion of the temperate nature of the geographical components also exist to varying degrees. In addition, there are more elements unique to China. Due to special geographical location, Guizhou and diverse vegetation types, both types of Chinese subtropical evergreen broad-leaved forest vegetation zone, another of the ravine near the tropical nature of the monsoon forest, mountain rain season; both cold-temperate subalpine coniferous forest , another warm coniferous forest of the same place; both a large area of secondary deciduous broad-leaved forest, there are very limited distribution of valuable deciduous forest. The spatial distribution of vegetation has shown a clear transition, so that the geographical distribution of various vegetation types overlap each other, intricate, complicated by a variety of vegetation types and diverse portfolio.

 贵州植被丰厚,具有明显的亚热带性质,组成种类繁多,区系成分复杂。全省维管束植物( 不含苔藓植物)共有269科、1655属、6255种(变种)。植物区系以热带及亚热带性质的地理成分占明显优势,如泛热带分布、热带亚洲分布、旧世界热带分布等地理成分占较大比重,温带性质的地理成分也不同程度存在。此外,还有较多的中国特有成分。由于特殊的地理位置,贵州植被类型多样,既有中国亚热带型的地带性植被常绿阔叶林,又有近热带性质的沟谷季雨林、山地季雨林;既有寒温性亚高山针叶林,又有暖性同地针叶林;既有大面积次生的 落叶阔叶林,又有分布极为局限的珍贵落叶林。植被在空间分布上又表现出明显的过渡性,从而使各种植被类型在地理分布上相互重叠、错综,各种植被类型组合变得复杂多样。Guizhou Province in the Yangtze and Pearl rivers, the upper reaches of the two major river systems cross zone, there are 69 county shelter to protect the Yangtze River area, the Yangtze River, Pearl River upper reaches of the region's major ecological barrier. Soon the terrain from the province's river systems in western, central north, east, south and three sides diversion. Miaoling is the Yangtze River and Pearl River 2 River watershed is north of the Yangtze River drainage area of 115,747 square kilometers, accounting for 65.7% of the province's land area, the main rivers are the Wujiang River, Red River, water Jiang, Hongzhou River, Wuyang He , Jinjiang, Songtao River, songkan River, Kraal River, Yokoe and so on. Miaoling south of the Pearl River is a watershed area of 60420 square kilometers, accounting for 34.3% of the province's land area, the main rivers Nanpanjiang, North Pan River, Red River, are Liujiang, seizing and River. 贵州河流处在长江和珠江两大水系上游交错地带,有69个县属长江防护林保护区范围,是长江、珠江上游地区的重要生态屏障。全省水系顺地势由西部、中部向北、东、南三面分流。 苗岭是长江和珠江两流域的分水岭,以北属长江流域,流域面积115747平方千米,占全省国土面积的65.7%,主要河流有乌江赤水河、清水江、洪州河、舞阳河锦江松桃河、松坎河、牛栏江、横江等。苗岭以南属珠江流域,流域面 积60420平方千米 ,占全省国土面积的34.3%,主要河流有南盘江、北盘江、红水河、都柳江、打狗河等。

As a specific geographic location and complex topography, so that Guizhou complex and diverse climatic and ecological conditions, three-dimensional characteristics of agriculture obvious regional agricultural production, regional strong, suitable for conducting the comprehensive development of agriculture as a whole, suitable for the development of specialized Agriculture. 由于特定的地理位置和复杂的地形地貌,使贵州的气候和生态条件复杂多样,立体农业特征明显,农业生产的地域性、区域性较强,适宜于进行农业的整体综合开发,适宜于发展特色农业

急求贵州特别著名的几个旅游景点介绍,需要中英文互译,谢谢!

第一个,织金洞

金洞原名“打鸡洞”、“乾宏洞”、“织金天宫”,位于贵州织金县城东北面二十三公里织金洞公园正门官寨乡东街口。1980年4月,织金县人民政府组织的旅游资源勘察队发现此洞。织金洞囊括了当今世界溶洞中的各种沉积形态,它既是一座地下艺术宝库,又是一座岩溶博物馆,堪称“世界奇观”。 织金洞是我国著名的喀斯特风景名胜区,中国旅游胜地40佳之一。1988年国务院审定公布的第二批国家级重点风景名胜区,与红枫湖、龙宫、黄果树大瀑布三个国家级风景区共同形成旅游黄金环线。

织金洞已开发的洞厅47个,洞厅最宽处173米,一般高50—60米,最高达150米。洞内地形复杂,有迎宾厅、万寿宫等10个景点、40多种岩溶形态,有“岩溶博物馆”之称。洞外有地面岩溶、峡谷、溪流、瀑布等自然景观与布依、苗、彝族村寨。整个风景名胜区面积450平方公里,除织金洞景区外有织金古城、裸结河峡谷、洪家渡景区。织金城建于公元1382年,三面环山,一水贯城,城内有71处清泉,庵堂寺庙50余处,有结构奇特的财神庙、洞庙结合的保安寺等。

2009年织金洞风景名胜区成功升级为国家AAAA级风景名胜区

第二个,黄果树瀑布。

黄果树瀑布,位于中国贵州省安顺市镇宁布依族苗族自治县,是珠江水系打邦河的支流白水河九级瀑布群中规模最大的一级瀑布,因当地一种常见的植物“黄果树”而得名,瀑布高度为77.8米,其中主瀑高67米;瀑布宽101米,其中主瀑顶宽83.3米。黄果树瀑布属喀斯特地貌中的侵蚀裂典型瀑布。黄果树瀑布不只一个瀑布的存在,以它为核心,在它的上游和下游20千米的河段上,共形成了雄、奇、险、秀风格各异的瀑布18个。1999年被大世界吉尼斯总部评为世界上最大的瀑布群,列入世界吉尼斯记录。

第三个,青岩古镇

青岩古镇,位于贵阳市南郊,距市区约29公里。它是贵州四大古镇之一,一座建于600年前的军事古镇 。古镇内设计精巧、工艺精湛的明清古建筑交错密布,寺庙、楼阁画栋雕梁、飞角重檐相间。悠悠古韵,被誉为中国最具魅力小镇之一。

第四个,百里杜鹃

百里杜鹃风景区位于贵州省黔西大方县交界处,地理坐标为:东经105°45′~106°04′45〃,北纬27°08′30〃~27°20′00〃。百里杜鹃属贵州西北部次生地带性植被中保存最好的一部分,初步查 明景区内有马缨杜鹃、树型杜鹃、狭叶马缨杜鹃、美容杜鹃、大白花杜鹃、露珠杜鹃、团花杜鹃、迷人杜鹃、银

叶杜鹃、皱皮杜鹃、锈叶杜鹃、问客杜鹃、腺堮马银花、多花杜鹃、映山红、锦绣杜鹃、贵定杜鹃、暗绿杜鹃、映山红变种、落叶杜鹃、水红杜鹃百合杜鹃、多头杜鹃41个品种,占世界5个亚属中的4 个,花色多样,有鲜红、粉红、紫色、金黄、淡黄、雪白、淡白、淡绿等。最为难得的是一树不同花,即一棵树上开出不同颜色的花朵,最多的达7 种之多被誉为“世界上最大的天然花园”。有“世界级的国宝精品”之美称。

暮春3月下旬至4月末各种杜鹃花先后怒放,杜鹃花漫山遍野,千姿百态,铺山盖岭,五彩缤纷。真是好一幅“千峰叠起嶂,乌金地下埋,杜鹃花似海,满山留异香”的美丽画卷。其花色品种之多,分布之密集,美学价值、观赏价值之高,艺术感染力之强,实属世界罕见。公园分为金坡景区、普底景区、野营区、游乐区、休闲疗养区、后备发展区。共有五彩路、数花峰、醉九牛、漫步云台、黄家坝阻击战纪念碑、百花坪、马缨岭、锦鸡箐、对嘴岩、御赐银杏、千年古桑、杜鹃花王、移山湖、花底岩等20多个景点。此外人文资源也十分丰富:彝族的“火把节”、苗族的“跳花坡”内容丰富多彩、目不暇接。彝族的舞蹈《撮泰吉》、苗族的高架芦笙舞、无伴奏多声部合唱等别具特色。因此,百里杜鹃不百里杜鹃--戛木杜鹃仅是杜鹃花的世界、杜鹃花的海洋,也是参天古树云集、山水林洞辉映、珍禽异兽栖息、民族风情浓郁的原始森林旅游区。游客在观杜鹃花、赏民族歌舞之余,还可以饱览灵山秀水、古树、山珍、名药。每年相约春天的“中国杜鹃花节”规模盛大、丰富多彩,吸引了大量的专家和中外游人前来观光旅游,已成为国内外媒体每年关注的旅游和文化热点。

百里杜鹃——戛木景区:距大方县城72公里,有花底岩、戛木等主要景点。花底岩多岩溶,有天生桥,两边悬崖成剪状排开,像万里长城逶迤而来。下有伏流,此桥边底100多米,在桥的右下侧,伏流出口处形成戛木杜鹃--落红一个半月形的巨大岩溶景观,深落在花山花海之下。花底岩险要处有只闻其声而不见其形的地下瀑布,有"迎客松"式的千年疙瘩万年树--岩松,有走马转阁的岩长廊。戛木有保存完好的原生马樱杜鹃林带,这里杜鹃花有着花大、树大、色艳特点,每到春天来时放眼望去红艳如火,霞展满天。由于海拔较高,在雨雪、凌冻和冰霜的塑造下树干、树枝轮廓分明,线条曲折多变。造型奇美,可谓树绝花奇。

1987年3月,贵州省人民政府将百里杜鹃列为省级风景名胜区,同时落红--拼图百里杜鹃 被列为贵州省“十大风景名胜区”之一。1993年5月,原国家林业部批准建立百里杜鹃国家级森林公园。2001被列为地区级自然保护区。2007年7月贵州省委批准成立贵州省百里杜鹃风景名胜区党工委和管委会,为毕节地委行署正县级派出机构,统一管理和开发百里杜鹃,为百里杜鹃这一“地球的彩带、世界的花园”面向全国、走向世界提供了强有力的组织保障。

根据《中共贵州省委常委专题会议纪要》(九届[2006]9号)精神,省编办下发了《关于设立贵州百里杜鹃风景名胜区党的工作委员会和管理委员会的批复》(省编办发(2007)76号),批准成立贵州百里杜鹃风景名胜区(贵州百里杜鹃国家级森林公园、贵州百里杜鹃自然保护区)党的工作委员会和管理委员会,为地委、行署正县级派出机构,对百里杜鹃风景区实行统一领导和管理。受大方和黔西两县委托,管理大方县普底乡、大水乡和黔西县金坡乡、仁和乡以及大方、黔西两县部分乡镇所涉及的村(组)。百里杜鹃风景名胜区辖7个乡(镇)的54个村(居)(其中,有4个乡是整体划入),辖区面积近500平方公里,辖区内居住人口近9万人。

第五个,红枫

红枫湖是国家AAAA级风景名胜区,位于贵州清镇平坝县境内,距安顺77千米、贵阳33千米。红枫湖是岛屿最多的高原岩溶湖泊, 湖中有岛屿100多个,以岩溶地貌和湖光山色为特色,是国家级风景名胜区,被誉为贵州腹地的一颗明珠。红枫湖始建于1958年,当时挖水库修电站。湖边有座红枫岭,岭上及湖周多枫香树。深秋时节,枫叶红似火,红叶碧波,风景优美,故名“红枫湖”。

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