Traditional Culture Encyclopedia - Travel guide - English introduction of tourist attractions in Northern Ireland English version of Irish attractions introduction

English introduction of tourist attractions in Northern Ireland English version of Irish attractions introduction

Kneel and beg to introduce Irish customs, festivals and so on in English. First grade level, not too difficult, very urgent, very urgent, give me points.

Irish English tour guide words

Introduction to Irish English Republic of Ireland

Introduce Ireland in English

As far as tourist attraction is concerned, the influence of this small island of Ireland far exceeds its own weight. This country is so full of joy that tourists can often only describe its charm with exaggerated cliches: it is the greenest country, full of the friendliest people, and if they are not distracted by the temptation of bars, they will all become geniuses.

Ireland is really a green country-so much rain must have its benefits-and people are famous for their friendliness. As for the geniuses, the Irish will proudly point out their four Nobel Prize in Literature laureates, claim that their success rate is unparalleled in any other country of the same size, and ensure strict compliance with the sacred "round" system (everyone takes turns buying a drink for others).

However, the charm of Ireland is far more profound than the legend of a bar or the achievements of a group of (mostly) dead writers. It has an extraordinary history, and almost everything is involved, from the prehistoric stone tablets in the Boyne Valley to the memorial to its fallen patriots, who dare to challenge the arbitrary power of their long-term occupier and contemporary friend Britain.

It has a vibrant capital, Dublin, which has led an amazing period of economic growth and turned the country from a backward rural area into the envy of Europe. As a result, the Irish have become more sophisticated, which continues to push them to achieve higher achievements. Even the most intractable problem in Northern Ireland has some kind of solution, and Ireland looks forward to the future with confidence.

Located in the south of Ireland Island in Western Europe. It is bordered by the Atlantic Ocean in the west, Northern Ireland in the northeast and Britain across the Irish Sea in the east. The longest river is river shannon, and the largest lake is Lake Korib. It has a mild maritime climate. Ireland is called "Emerald Island".

Ancient Ireland has a history of more than 6000 years. The peaks and valleys witnessed the scene of farmers farming in the fields in the Neolithic age, and the principle of peace witnessed the scene of many troops preparing for war. There are also some remote islands, such as Skillings Island and Brasket Island, which are located off the coast of Kaili. Some people who turned Ireland into an "island of saints and scholars" once lived here, which was once the Christian center of Europe. In addition, three scenic spots in Ireland are listed on the United Nations World Heritage List.

Ireland is divided into Northern Ireland, which is still under British jurisdiction, and the Republic of Ireland, which has been independently controlled.

The former often sees religious and political conflicts in the media, explosions everywhere, and masked members of terrorist organizations (the situation seems to have changed now). The latter has long been independent. What I want to introduce here is Ireland, where the political situation is peaceful and there are few hot scenes.

Ireland is located in the midwest of the British Isles, only three hours' drive from beautiful Wales, and borders Northern Ireland in the northeast, with a total area of about 72,282 square kilometers. The green, white and orange flags are the national flags, representing Irish Catholicism, Protestantism and hope respectively.

The main religion in Ireland is Catholicism, the main language is Irish, English is the second language, and many street signs are bilingual. It also has its own monetary unit, the Irish currency, which is slightly lower than the pound. This phenomenon is somewhat national pride.

Blanie Castle, located in the suburb of Cork, the second largest city, is quaint and quiet.

Ireland has rolling hills, but there are many intermittent mountains along the coast. The central region is a lowland crisscrossed by rivers and lakes. The climate belongs to maritime humid climate. The west coast near the Atlantic Ocean is charming. On the way from one town to another, endless green hills, amazing lakes and beautiful coastlines can be seen everywhere.

These mountains, lakes and bays have become a good place for urbanites to relieve pressure. There are also many ruins of ancient castles here. SF, who came early, said that her trip was to see one castle after another. Kissing the Stone Wall: Kissing makes eloquence

Ireland not only has the simplicity and freshness of the Middle Ages, but also does not forget to show the modern metropolis color. If you are tired of the noisy urban culture, why not list Ireland as your next travel goal and feel the fresh holiday mood?

Introduction to Northern Ireland, English.

Hello, the English introduction about Giant Causeway is as follows, I hope it will help you:

Giant's Road is an area with about 40,000 interlocking basalt columns, which is the result of ancient volcanic eruption. It is located in Ann Triem County on the northeast coast of Northern Ireland, 3 miles (4.8 kilometers) northeast of Bushmills Town. It was declared a World Heritage Site by UNESCO in 1986 and a National Nature Reserve by Northern Ireland's Ministry of Environment in 1987. In the 2005 Radio Times readers' vote, Giant's Road was rated as the fourth natural wonder in Britain. The top of the column forms a stepping stone extending from the foot of the cliff to the seabed. Most columns are hexagonal, although some are four-sided, five-sided, seven-sided and octagonal. The highest is about 12 meters (39 feet) high, and the solidified lava on the cliff is 28 meters thick in some places.

Giant Causeway, now owned and managed by the National Trust, is the most popular tourist attraction in Northern Ireland.

Is this ok?

What are the tourist attractions in Northern Ireland?

At the headland on the edge of the antrim Plain in Northern Ireland, at the foot of the cliff along the coast, there are about 37,000 Yanzkowski Corners composed of hexagonal, pentagonal and quadrilateral pillars, which extend from the cliff to the sea surface and have stood by the sea for thousands of years. Known as the "road of giants".

The coast of Giant's Road includes low tide areas, cliffs, roads leading to the top of cliffs and a highland. The average height of the cliff is 100 meter. Giant's Road is the most distinctive place on this coastline. These more than 37,000 basalt columns of the same size converge into a causeway that stretches for thousands of meters. The shape is very regular, and it looks like it was cut by hand. A large number of basalt columns are arranged together, forming a spectacular basalt column forest. Their neat and beautiful shapes and majestic momentum are breathtaking. "Giant's Road" is a natural wonder of the world. It belongs to the world natural heritage and is also a famous tourist attraction in Northern Ireland.

The cross-sectional width of the stone pillars that make up the Giant's Road is between 3 ~ 5 1 cm, with a typical width of about 0.45 m and a length of about 6000 m. The widest point of the headland is about 12 m wide, and the narrowest point is only 3 or 4 m, which is also the highest place of the stone pillars. Some stone pillars here are more than 6 meters above sea level, and the highest can reach 12 meters. Some stone pillars are submerged or as high as the sea surface.

Standing on some short stones, you can see that their sections are regular polygons. Different shapes of stone pillars have visual names, such as "chimney cap", "big wine bowl" and "lady fan"

Legend of the Giant's Road: The Giant's Road is also called the Giant's Dike or the Giant's Point. This name comes from Irish folklore. There is a saying that the "Giant's Road" was built by Irish giant Finn McMahole. He carried the pillars to the bottom of the sea one by one, so that he could go to Scotland to fight his opponent Finn Gail. When McMahole finished, he decided to have a rest. Meanwhile, his opponent, Finn Gail, decided to travel through Ireland to evaluate his opponent, but he was frightened by the huge body of the giant McMahole. Especially after McMahole's wife told him that it was actually a giant's child, Gail was worried about his life when he thought about what kind of monster the father should be. He hurried back to Scotland and destroyed the causeway behind him to stop Finn McMahole from going to Scotland. Now all the causeway remains are located on the coast of antrim.

On the other hand, the Giant's Road was specially built by the commander of the Irish King's army, the giant Finn McCul, to welcome his beloved girl. Legend has it that the commander of the Irish king's army, the giant Finn McMahole, is very powerful. Once in a fight with a Scottish giant, he picked up a stone and threw it at his fleeing opponent. The stone fell into the sea and became today's giant island. Later, he fell in love with the giant girl who lived in hebrides. In order to bring her here, he built such a causeway.

Formation of the Giant's Road: Seen from the air, the ochre stone pillar causeway of the Giant's Road is particularly eye-catching and intriguing against the blue sea. But what kind of natural forces created this world-famous spectacle?

Modern geologists have solved the mystery of "Giant's Road" by studying its structure. "Giant's Road" is actually natural basalt. At the end of Cretaceous, the embryonic North Atlantic began to split and expand, and the mid-Atlantic ridge was the center of the split and expansion and the boundary of the separation plate. The magma in the upper mantle rises from the mid-ridge rift, covering a large area and overlapping lava layers.

At that time, the dominant position of the North Atlantic was fixed, but its boundary was in the stage of formation and change. Although North America and Eurasia have been separated, the newly formed sea lanes between the separated North America and Europe are still under development. About 80 million years ago, the west coast of Greenland was separated from Canada, but the southeast coast is still closely connected with the northwest coast of the British Isles. After about 20 million years, these coasts began to separate. This series of geological changes has led to intense crustal movement and frequent volcanic eruptions on both sides of the Atlantic Ocean. There are large volcanoes on Skye, Ram, Mar and Allen, as well as Cape Mohen in Adna and Silver Gallian, Clifton and Moen in southern Ireland. These ancient volcanoes must have been spectacular in the early days, but the most important records about the situation at that time were floods, plateaus and basalts.

About 50 million years ago (Tertiary), volcanoes in western Scotland from the hebrides Line to eastern Northern Ireland were very active, and the lava plateaus in Ireland and Scotland were formed by large-scale lava flows at that time. The ejected basalt is a particularly hot fluid lava. According to records, its downhill speed exceeds 48 kilometers per hour. Fluid lava is easy to spread in a large area, so it is called "overflow basalt". They form chunks of lava throughout the volcanic active area. The Deccan Plateau in India has a similar geological situation. 700,000 cubic kilometers of basalt lava was formed in Deccan Plateau 40-60 million years ago.

Thick basaltic magma spewed out from cracks in the earth's crust and flowed to the sea like a river. When it meets seawater, it cools rapidly and becomes solid basalt. During the solidification of magma, it shrinks, crystallizes and bursts, and the contraction force is very uniform, so it forms regular columnar patterns, generally hexagonal prisms. This process is a bit like a thick layer of mud at the bottom of a quagmire cracking in the sun. The main feature of basalt lava column is that cracks extend straight up and down, and water can flow down from top to bottom. As a result, a unique network of basalt columns was formed, and all the basalt columns were incredibly connected, with only tiny cracks between them. Because volcanic lava overflowed five or six times in different periods, the cliff formed a multi-level structure.

"Giant's Road" is the perfect expression of columnar basaltic rocks. These stone pillars form a stone road with the width of a dense stone forest. The Giant's Road and the Giant's Road Coast are not only steep natural landscapes, but also provide valuable information for the study of earth science.

During the thousands of years since its formation, due to glacial erosion and Atlantic ocean waves during the Great Ice Age, the basalt column at Jaentzkowski Point was gradually shaped into a rugged and peculiar landscape. Each basalt stone pillar is actually made up of several hexagonal stones stacked together. The waves gradually eroded the exposed part along the fault line between stones, and the stone pillars were cut off at different heights and taken away loosely, thus forming the prototype of the giant road with stepped appearance. After thousands of years of erosion and weathering, the stepped effect of basalt dike is finally formed.

Relatives of the Giant's Road are all over the world: columnar basaltic landforms similar to the Giant's Road are also distributed in other parts of the world, such as Staffa Island in hebrides, southern Iceland and Zhuzishan in Liuhe County, Jiangsu Province, China. But they are not as complete and spectacular as the Giant's Road.

For example, on Staffa Island in hebrides on the west coast of Scotland, there are also a group of basalt columns. Basalt pillars are well developed in most parts of the island, and there is a famous huge cave-fingal Cave, which has been described by poems and novels for centuries. When the composer Felix Mendelssohn visited the island in 1829, he was inspired by the beautiful scenery in front of him and composed a famous orchestral prelude, which is now called Inner hebrides.

Introduction to Northern Ireland English

Northern Ireland is a region of Britain, located in the northeast of Ireland Island, with Belfast as its capital. The terrain is low in the middle and mountainous around. The main river is the Bain River. The inner lake in the upper reaches, with an area of 396 square kilometers, is the largest lake in Britain and belongs to glacial lake. It has a mild maritime climate. 180 1 year, Ireland was assigned to Britain. 192 1 year, 26 counties in the south formed a free state, and 1937 * * * Republic was established. Six counties in the north still belong to Britain, called Northern Ireland, and become part of the United Kingdom of Great Britain and Northern Ireland.

Northern Ireland is a region of Britain, located in the northeast of Ireland Island, and is the capital of Belfast. The middle is flat and surrounded by mountains. The main river is the Bane River. The upper reaches of the Nye River, with an area of 396 square kilometers, is the largest lake in Britain. It is a temperate climate. 180 1 Orchid Island was classified as Britain in Ireland. 192 1 year, 26 counties in the south formed a free state, 1937, the Republic was founded, and six counties in the north were still owned by Britain, called Northern Ireland, which is a part of the United Kingdom of Great Britain and Northern Ireland.

Introduction to Northern Ireland English

Northern Ireland is one of the four countries in Britain. Located in the northeast of Ireland Island, it borders the Republic of Ireland in the south and west. At the time of the 200 1 British census, its population was 1 685,000, accounting for about 30% of the island's total population and 3% of the British population.

Northern Ireland consists of six counties in Ulster, Ireland. It was established as a separate branch of the United Kingdom on May 3rd by the Irish Government Act 1920[5], although its constitutional roots lie in the Joint Act 1800 between Great Britain and Ireland. For more than 50 years, it has its own decentralized government and parliament. These institutions were suspended in 1972 and abolished in 1973. Many attempts to restore autonomy eventually led to the establishment of today's Northern Ireland Administration and Northern Ireland Parliament in 1998. Parliament operates on the principle of joint democracy that requires cross-community support.