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第一篇：黃果樹(shù)瀑布導(dǎo)游詞英語(yǔ)作文

女士們、先生們：

大家好!今天我們將要游覽的風(fēng)景點(diǎn)是黃果樹(shù)瀑布。

黃果樹(shù)瀑布是中國(guó)第一在瀑布，也是世界上慕名的大瀑布之一。1982年11月，經(jīng)中華人民共和國(guó)國(guó)務(wù)院審定，黃果樹(shù)瀑布已被列為國(guó)家重點(diǎn)風(fēng)景名勝區(qū)。

黃果樹(shù)瀑布距省城貴陽(yáng)市137公里，位于貴州省西部鎮(zhèn)寧縣和關(guān)嶺縣接壤處的打邦河支流的白水河上。從貴陽(yáng)乘車(chē)到黃果樹(shù)，約需一個(gè)半小時(shí)左右時(shí)間。

現(xiàn)在我們進(jìn)入黃果樹(shù)瀑布景區(qū)大門(mén)，沿著石階我們可以來(lái)到景區(qū)的第一個(gè)景點(diǎn)——盆景園，黃果樹(shù)盆景園是貴州黃果樹(shù)瀑布景區(qū)里新近開(kāi)發(fā)的，又一處景觀。它距離黃果樹(shù)賓館僅只500米，占地40畝，園內(nèi)展示著各種姿態(tài)各異的珍奇盆景一共3000多盆，在園中各處爭(zhēng)奇斗艷，競(jìng)吐芬芳。盆景園地處貴州西部低洼地帶，海拔較低，終年無(wú)霜，極適宜亞熱帶植物生長(zhǎng)。這里隨處可見(jiàn)仙人掌、黃桷蘭、白玉蘭等多肉植物及其它喜溫灌木喬木。除此之外，在南方植物園里常見(jiàn)的欒樹(shù)、米蘭等，也已在此安家。盆景園里一年四季枝繁葉茂、花團(tuán)繁簇。當(dāng)游人嘆服于大瀑充的雄姿，領(lǐng)略了天星景區(qū)奇山秀水巧連天的旖旎神韻后，沿著綠蔭步入盆景園，猶如大餐后的一杯香茗、一道果品、一曲輕柔的慢板，可以使意象信息的載的心靈陡然松弛下來(lái)，園中花木為你帶來(lái)的了淡雅的情趣和格調(diào)迥異的美感享受。

黃果樹(shù)大瀑布已經(jīng)到了，你們看，這就是早已聞名遐邇的中國(guó)第一大瀑布。 黃果樹(shù)瀑布高68米，加上瀑上瀑6米，總高74米，寬81米，夏秋洪水暴漲，瀑布如黃河倒傾，峭壁震顫，谷底轟雷，十里開(kāi)外，也能聽(tīng)到它的咆哮;由于水流的強(qiáng)大沖擊力，濺起的水霧可彌漫數(shù)百米以上，使坐落在瀑布左側(cè)崖頂上的寨子和街市常常被濺起的水霧所籠罩。游人謂之“銀雨灑金街”。冬春水小，瀑布便分成三五綹從岸頂上掛下來(lái)，遠(yuǎn)遠(yuǎn)望去，那潔白的水簾飄然而下，揚(yáng)揚(yáng)灑灑，如綢緞飄舞，如仙袂飄舉，如淑女浣紗黃果樹(shù)瀑布景區(qū)導(dǎo)游詞黃果樹(shù)瀑布景區(qū)導(dǎo)游詞。

數(shù)百年來(lái)，黃果樹(shù)瀑布的雄姿一直為許多文人學(xué)者所驚嘆。清代貴州著名書(shū)法家、“頤和園”三字的題額者嚴(yán)寅亮在“望水亭”題寫(xiě)的對(duì)聯(lián)：“白水如棉，不用弓彈花自散。紅霞似錦，何需梭織天生成”，更是形象而生動(dòng)地概括了黃果樹(shù)瀑布的壯麗景色。

現(xiàn)在，我們來(lái)到了瀑布跌落處---犀牛潭。此潭乃因傳說(shuō)有神犀潛藏水底而得名。有沒(méi)有神犀，誰(shuí)也沒(méi)有見(jiàn)過(guò)，但潭水的神秘幽深，至今依然，任何人駐足潭邊，都會(huì)浮想聯(lián)篇。若是晴天的上午10時(shí)或下午4時(shí)左右，由于陽(yáng)光的折射，你還可以透過(guò)瀑布沖擊時(shí)濺起的雨霧，看到從深潭中升起的七色彩虹，使你頓生雄姿蓋世，艷麗昭天之感。 這個(gè)瀑布為什么起名叫黃果樹(shù)瀑布，而不叫其他別的什么瀑布呢?據(jù)民間傳說(shuō)，是因?yàn)槠俨歼吷嫌锌酶叽蟮狞S桷樹(shù)，按當(dāng)?shù)氐目谝?，“桷”與“果”讀音相同，所以人們就習(xí)慣稱(chēng)之為黃果樹(shù)，這是一種說(shuō)法。還有一種說(shuō)法，傳說(shuō)很久以前瀑布附近的農(nóng)民都喜歡種黃果，瀑布邊上就有一大片黃果園，因此就把這個(gè)瀑布稱(chēng)之為黃果樹(shù)瀑布了。 與世界上其他著名的大瀑布相比，黃果樹(shù)大瀑布雖然沒(méi)有非洲維多利亞大瀑布、北美洲尼亞加拉大瀑布、委內(nèi)瑞拉安赫爾大瀑布那般寬闊、高深和雄偉，但是，黃果樹(shù)大瀑布自有它奇特之處，它是世界上處在喀斯特地區(qū)最在瀑布，也是最壯觀的瀑布黃果樹(shù)瀑布景區(qū)。這個(gè)大瀑布就像是一塊奇異的磁 石，在它的地面、地下、水上、水中還吸附著一連串豐姿綽約的景致。其中最神奇的一處，就是隱藏在大瀑布半腰的崖廊洞穴，由于洞外藤蘿攀附，水掛珠簾，故曰“水簾洞”。這是世界上其它大瀑布所沒(méi)有的奇特景觀。 女士們、先生們，“水簾洞”已經(jīng)到了，這個(gè)水簾洞全長(zhǎng)134米，它由6個(gè)洞窗、3個(gè)股洞泉和6個(gè)通道所組成。根據(jù)中國(guó)神話故事改編的大型電視連續(xù)劇《西游記》中水簾洞一場(chǎng)戲，就是這里拍攝。 這是第一洞窗，它的位置最低，離犀牛潭水面僅40米，但洞窗則最寬大，有十幾米寬，位置在第一、二個(gè)瀑布中間，大水時(shí)兩個(gè)瀑布就連成水簾，將洞窗全部封住;水小時(shí)則次第拉開(kāi)，從幾米到十幾米不等，閔像可以隨意開(kāi)合的窗簾。 這是第二洞窗，它離第一洞窗僅4米左右。這是一個(gè)靜謐的世界，號(hào)稱(chēng)水晶宮。它是水簾洞的心臟部分，長(zhǎng)11米，高9米，寬3米。路旁有一股泉水，清澈明凈，水長(zhǎng)年保持在一個(gè)水位。洞頂懸掛著許多鐘乳石，在麥稈狀鐘乳石上還有名貴的卷曲石。洞壁上還懸著數(shù)不清的石幔、石簾。 這是第三洞窗，它向外突出，很像陽(yáng)臺(tái)。這個(gè)洞窗有1米高，3米長(zhǎng)，外面圍有護(hù)欄，游人站在護(hù)欄后面可以伸手摸到瀑布，所以人們把這里稱(chēng)之為“摸瀑臺(tái)”。

第二篇：黃果樹(shù)瀑布導(dǎo)游詞

Huangguoshu Waterfall belongs to the Baishui River system at the lower reaches of Kebu River, a tributary of Dabang River, a tributary of Beipan River, a tributary of Nanpan River, the main stream of Xijiang River in the the Pearl River water system. Kebu River is the west source (or tributary) of Dabang River, a north bank tributary at the downstream of Beipan River, a tributary of Nanpan River in the Xijiang River system of the the Pearl River Basin. Originating from Ertang in Liuzhi Special District, Guizhou Province, it flows northeast to Zhedongnan in Liuzhi Special District, passes through Biandan Mountain and reaches the mouth of Guijia River, initially known as Baishui River. The Huangguoshu Waterfall flows south here and intersects with Dongyuan Wanger River into Dabang River. The river is 48 kilometers long, with a catchment area of 731.4 square kilometers, a drop of 339 meters, and a flow rate of 14.6 cubic meters per second at the mouth.

The flow rate of Huangguoshu Waterfall is generally maintained at 8 to 12 cubic meters per second. The maximum flow during the rainy season can reach 110-150 cubic meters per second. At a flow rate of 2-3 cubic meters per second, Huangguoshu Waterfall can form a landscape. With a flow rate of about 5 cubic meters, it can showcase the beautiful side of Huangguoshu Waterfall without losing its grandeur. Due to the decrease in upstream water volume, during the dry season from early November to the end of April each year, Wangerhe Reservoir will divert water to Huangguoshu Waterfall, with a daily flow rate of no less than 5 cubic meters per second. This can ensure that the flow rate of Huangguoshu Waterfall during the dry season remains above 8 cubic meters per second. Even if facing another severe drought, the Huangguoshu Waterfall will still remain beautiful and spectacular.

Huangguoshu Waterfall has a long history as a scenic spot. After the establishment of the Peoples Republic of China, Anshun City and Zhenning County in Guizhou Province developed it. In 1982, it was included in the first batch of national key scenic spots.

The Dahuang Fruit Tree Tourism Circle includes the unique and magnificent natural landscapes and diverse ethnic customs and cultures of Anshun, covering Tianxing Bridge, Langgong, Longgong, Getu River, Guanling National Paleontological Geological Park, the Earths Great Rift - Huajiang Grand Canyon, Tianlong Tunpu, Yunfeng Tunpu, and multiple tourist ethnic villages, covering an area of over 120 square kilometers.

The origin of Huangguoshu Waterfall can be traced back to the Middle Triassic period over 200 million years ago, when a thick set of carbonate rocks was deposited in the Huangguoshu area. The Huangguoshu Waterfall developed in a set of thick layers interbedded with a small amount of thin layered limestone in the second section of the Guanling Formation of the Middle Triassic, located on the eastern wing of the Wengzhai anticline. The Baishui River during the formation of Huangguoshu Waterfall was an above ground river that developed between 100000 and 500000 years ago and evolved from the "wide valley period" to the "canyon period" during the middle and late Pleistocene periods of the Quaternary. Later, due to the intermittent uplift of the crust during the Himalayan Movement, the erosion benchmark level of the river decreased, leading to the strengthening of erosion, dissolution, and other downward cutting effects of the river. A "fissure" was formed at this point (where the riverbed underwent significant turning points due to the uplift of the crust, the decline of the erosion benchmark level, and the influence of factors such as structure and lithology). The fissures, karst caves, and underground rivers at this fissure point were very developed. The Baishui River first formed a karst erosion fissure type sinkhole waterfall. Later, under the influence of factors such as river erosion, dissolution, and lateral erosion, intermittent uplift of the crust, and increasing hydrodynamic forces in the late Pleistocene warm and humid climate, the top of the sinkhole gradually collapsed, and the Huangguoshu Waterfall finally appeared, with a history of 50000 years.