Venice, Italy

 Venice alternative obsolete form: Vinegia; Venetian: Venesia Latin: Venetiae; Slovene:  is a city in northeastern Italy sited on a group of 118 small islands separated by canals and linked by bridges. It is located in the marshy Venetian Lagoon which stretches along the shoreline, between the mouths of the Po and the Piave Rivers. Venice is renowned for the beauty of its setting, its architecture, and its artwork. The city in its entirety is listed as a World Heritage Site, along with its lagoon.

 Venice is the capital of the Veneto region. In 2009, there were 270,098 people residing in Venice's comune (the population estimate of 272,000 inhabitants includes the population of the whole Comune of Venezia; of whom around 60,000[3] live in the historic city of Venice ; 176,000 in Terraferma , mostly in the large frazioni (roughly equivalent to "parishes" or "wards" in other countries) of Mestre and Marghera; and 31,000 on other islands in the lagoon). Together with Padua and Treviso, the city is included in the Padua-Treviso-Venice Metropolitan Area (PATREVE), with a total population of 2,600,000. PATREVE is only a statistical metropolitan area without any degree of autonomy.

 

 The name is derived from the ancient Veneti people who inhabited the region by the 10th century BC. The city was historically the capital of the Republic of Venice. Venice has been known as the "La Dominante", "Serenissima", "Queen of the Adriatic", "City of Water", "City of Masks", "City of Bridges", "The Floating City", and "City of Canals". Luigi Barzini described it in The New York Times as "undoubtedly the most beautiful city built by man". Venice has also been described by the Times Online as one of Europe's most romantic cities

The Republic of Venice was a major maritime power during the Middle Ages and Renaissance, and a staging area for the Crusades and the Battle of Lepanto, as well as a very important center of commerce (especially silk, grain, and spice) and art in the 13th century up to the end of the 17th century. This made Venice a wealthy city throughout most of its history. It is also known for its several important artistic movements, especially the Renaissance period. Venice has played an important role in the history of symphonic and operatic music, and it is the birthplace of Antonio Vivaldi.

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St. Lucia

St. Lucia

 

 Saint Lucia is a sovereign island country in the eastern Caribbean Sea on the boundary with the Atlantic Ocean. Part of the Lesser Antilles, it is located north/northeast of the island of Saint Vincent, northwest of Barbados and south of Martinique. It covers a land area of 617 km² (238.23 sq mi) and has a population of 174,000 (2010). Its capital is Castries.

 

 The French were the island's first European settlers. They signed a treaty with the native Carib Indians in 1660. England took control of the island from 1663 to 1667. In ensuing years, it was at war with France 14 times, and rule of the island changed frequently (it was seven times each ruled by the French and British). In 1814, the British took definitive control of the island. Because it switched so often between British and French control, Saint Lucia was also known as the "Helen of the West Indies".

 

 Representative government came about in 1840 (with universal suffrage from 1953). From 1958 to 1962, the island was a member of the Federation of the West Indies. On 22 February 1979, Saint Lucia became an independent state of the Commonwealth of Nations associated with the United Kingdom. Saint Lucia is a mixed jurisdiction, meaning that it has a legal system based in part on both the civil law and English common law. The Civil Code of St. Lucia of 1867 was based on the Quebec Civil Code of 1866, as supplemented by English common law-style legislation. It is also a member of La Francophonie.

 

 The island nation celebrates its independence every year with a public holiday. The financial sector has weathered the global financial crisis, but the recession has hurt tourism.

 

 

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Fingal’s Cave, Scotland

 

  Fingal's Cave is a sea cave on the uninhabited island of Staffa, in the Inner Hebrides of Scotland, known for its natural acoustics. The National Trust for Scotland owns the cave as part of a National Nature Reserve. It became known as Fingal's Cave after the eponymous hero of an epic poem by 18th-century Scots poet-historian James Macpherson.

 

 

 

Formation

Fingal's Cave is formed entirely from hexagonally jointed basalt columns within a Paleocene lava flow, similar in structure to the Giant's Causeway in Northern Ireland and those of nearby Ulva.

In all these cases, cooling on the upper and lower surfaces of the solidified lava resulted in contraction and fracturing, starting in a blocky tetragonal pattern and transitioning to a regular hexagonal fracture pattern with fractures perpendicular to the cooling surfaces. As cooling continued these cracks gradually extended toward the centre of the flow, forming the long hexagonal columns we see in the wave-eroded cross-section today. Similar hexagonal fracture patterns are found in desiccation cracks in mud where contraction is due to loss of water instead of cooling.

 

 

Acoustics

The cave's size and naturally arched roof, and the eerie sounds produced by the echoes of waves, give it the atmosphere of a natural cathedral. The cave's Gaelic name, An Uaimh Bhinn, means "the melodious cave."

History

Little is known of the early history of Staffa, although the Swiss town of Stäfa on Lake Zurich was named after the island by a monk from nearby Iona. Part of the Ulva estate of the Clan MacQuarrie from an early date until 1777, the cave was brought to the attention of the English-speaking world by 18th-century naturalist Sir Joseph Banks in 1772.
It became known as Fingal's Cave after the eponymous hero of an epic poem by 18th century Scots poet-historian James Macpherson. It formed part of his Ossian cycle of poems claimed to have been based on old Scottish Gaelic poems. In Irish mythology, the hero Fingal is known as Fionn mac Cumhaill, and it is suggested that Macpherson rendered the name as Fingal through a misapprehension of the name which in old Gaelic would appear as Finn. The legend of the Giant's Causeway has Fionn or Finn building the causeway between Ireland and Scotland.

Sightseeing

The cave has a large arched entrance and is filled by the sea. Several sightseeing cruises organised from April to September by local companies pass the entrance to the cave. It is also possible to land elsewhere on the island (as some of these cruises permit) and walk overland to the cave, where a row of fractured columns forms a walkway just above high-water level permitting exploration on foot. From the inside, the entrance seems to frame the island of Iona across the water.

 

 

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Ha Long Bay, Vietnam

 Hạ Long Bay  is a UNESCO World Heritage Site, and a popular travel destination, in Quảng Ninh Province, Vietnam. Administratively, the bay belongs to Hạ Long City, Cẩm Phả town, and the part of Vân Đồn District. The bay features thousands of limestone karsts and isles in various sizes and shapes. Hạ Long Bay is a center of a larger zone which includes Bái Tử Long bay to the northeast, and Cát Bà islands to the southwest. These larger zones share similar geological, geographical, geomorphological, climate, and cultural characters.

Hạ Long Bay has an area of around 1,553 km², including 1,960–2,000 islets, most of which are limestone. The core of the bay has an area of 334 km² with a high density of 775 islets. The limestone in this bay has gone through 500 million years of formation in different conditions and environments. The evolution of the karst in this bay has taken 20 million years under the impact of the tropical wet climate. The geo-diversity of the environment in the area has created biodiversity, including a tropical evergreen biosystem, oceanic and sea shore biosystem. Hạ Long Bay is home to 14 endemic floral species and 60 endemic faunal species.

 Historical research surveys have shown the presence of prehistorical human beings in this area tens of thousands years ago. The successive ancient cultures are the Soi Nhụ culture around 18,000–7000 BC, the Cái Bèo culture 7000–5000 BC and the Hạ Long culture 5,000–3,500 years ago. Hạ Long Bay also marked important events in the history of Vietnam with many artifacts found in Bài Thơ Mount, Đầu Gỗ Cave, Bãi Cháy.

500 years ago, Nguyễn Trãi praised the beauty of Hạ Long Bay in his verse Lộ nhập Vân Đồn, in which he called it "rock wonder in the sky". In 1962, the Ministry of Culture, Sports and Tourism of North Vietnam listed Hạ Long Bay in the National Relics and Landscapes publication. In 1994, the core zone of Hạ Long Bay was listed by UNESCO as a World Heritage Site according to criterion vii, and listed for a second time according to criterion viii.

 Location

Hạ Long Bay is located in northeastern Vietnam, from E106°56' to E107°37' and from N20°43' to N21°09'. The bay stretches from Yên Hưng district, past Hạ Long city, Cẩm Phả town to Vân Đồn District, bordered on the south and southeast by the Gulf of Tonkin, on the north by China, and on the west and southwest by Cát Bà Island. The bay has a 120 km long coastline and is approximately 1,553 km² in size with about 2,000 islets. The area designated by UNESCO as the World Natural Heritage Site incorporates 434 km² with 775 islets, of which the core zone is delimited by 69 points: Đầu Gỗ island on the west, Ba Hầm lake on the south and Cống Tây island on the east. The protected area is from the Cái Dăm petrol store to Quang Hanh commune, Cẩm Phả town and the surrounding zone.

Climate

The climate of the bay is tropical, wet, sea islands, with two seasons: hot and moist summer, and dry and cold winter. The average temperature is from 15 °C- 25 °C, and annual rainfall is between 2 meters and 2.2 meters. Hạ Long Bay has the typical diurnal tide system (tide amplitude ranges from 3.5-4m). The salinity is from 31 to 34.5MT in the dry season and lower in the rainy season.

 

Tourism

 

 

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Neuschwanstein Castle, Germany

 
Neuschwanstein Castle (German: Schloss Neuschwanstein, pronounced , English: "New Swanstone Castle) is a nineteenth-century Romanesque Revival palace on a rugged hill above the village of Hohenschwangau near Füssen in southwest Bavaria, Germany. The palace was commissioned by Ludwig II of Bavaria as a retreat and as an homage to Richard Wagner. Ludwig paid for the palace out of his personal fortune and by means of extensive borrowing, rather than Bavarian public funds.

 

 The palace was intended as a personal refuge for the reclusive king, but it was opened to the paying public immediately after his death in 1886. Since then more than 61 million people have visited Neuschwanstein Castle. More than 1.3 million people visit annually, with as many as 6,000 per day in the summer. The palace has appeared prominently in several movies and was the inspiration for Disneyland's Sleeping Beauty Castle and later, similar structures.

 

Location

 

The municipality of Schwangau lies at an elevation of 800 m (2,620 ft) at the south west border of the German state of Bavaria. Its surroundings are characterized by the transition between the Alpine foothills in the south (toward the nearby Austrian border) and a hilly landscape in the north that appears flat by comparison.

In the Middle Ages, three castles overlooked the villages. One was called Schwanstein Castle. In 1832, Ludwig's father King Maximilian II of Bavaria bought its ruins to replace them with the comfortable neo-Gothic palace known as Hohenschwangau Castle. Finished in 1837, the palace became his family's summer residence, and his elder son Ludwig (born 1845) spent a large part of his childhood here.

Vorderhohenschwangau Castle and Hinterhohenschwangau Castle sat on a rugged hill overlooking Schwanstein Castle, two nearby lakes (Alpsee and Schwansee), and the village. Separated only by a moat, they jointly consisted of a hall, a keep, and a fortified tower house. In the nineteenth century only ruins remained of the twin medieval castles, but those of Hinterhohenschwangau served as a lookout place known as Sylphenturm.

 

 

 

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Santorini, Greece

Santorini, Greece

 

 
Santorini , classically Thera , and officially Thira , is an island in the southern Aegean Sea, about 200 km (120 mi) southeast of Greece's mainland. It is the largest island of a small, circular archipelago which bears the same name and is the remnant of a volcanic caldera. It forms the southernmost member of the Cyclades group of islands, with an area of approximately 73 km² (28 sq mi) and a 2011 census population of 15,550. The municipality of Santorini includes the inhabited islands of Santorini and Therasia and the uninhabited islands of Nea Kameni, Palaia Kameni, Aspronisi, and Christiana. The total land area is 90.623 km² (34.990 sq mi). Santorini is part of the Thira regional unit.

 

 Santorini is essentially what remains after an enormous volcanic eruption that destroyed the earliest settlements on a formerly single island, and created the current geological caldera. A giant central, rectangular lagoon, which measures about 12 by 7 km (7.5 by 4.3 mi), is surrounded by 300 m (980 ft) high, steep cliffs on three sides. The main island slopes downward to the Aegean Sea. On the fourth side, the lagoon is separated from the sea by another much smaller island called Therasia; the lagoon is connected to the sea in two places, in the northwest and southwest. The depth of the caldera, at 400m, makes it possible for all but the largest ships to anchor anywhere in the protected bay; there is also a fisherman harbour at Vlychada, on the southwestern coast. The island's principal port is Athinias. The capital, Fira, clings to the top of the cliff looking down on the lagoon. The volcanic rocks present from the prior eruptions feature olivine and have a small presence of hornblende.

 

 

It is the most active volcanic centre in the South Aegean Volcanic Arc, though what remains today is chiefly a water-filled caldera. The volcanic arc is approximately 500 km (310 mi) long and 20 to 40 km (12 to 25 mi) wide. The region first became volcanically active around 3–4 million years ago, though volcanism on Thera began around 2 million years ago with the extrusion of dacitic lavas from vents around the Akrotiri.

The island is the site of one of the largest volcanic eruptions in recorded history: the Minoan eruption (sometimes called the Thera eruption), which occurred some 3,600 years ago at the height of the Minoan civilization. The eruption left a large caldera surrounded by volcanic ash deposits hundreds of metres deep and may have led indirectly to the collapse of the Minoan civilization on the island of Crete, 110 km (68 mi) to the south, through a gigantic tsunami. Another popular theory holds that the Thera eruption is the source of the legend of Atlantis.

 

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Pamukkale, Turkey

 

 

Pamukkale, Turkey

 

 Pamukkale, meaning "cotton castle" in Turkish, is a natural site in Denizli Province in southwestern Turkey. The city contains hot springs and travertines, terraces of carbonate minerals left by the flowing water. It is located in Turkey's Inner Aegean region, in the River Menderes valley, which has a temperate climate for most of the year.

 The ancient Greco-Roman and Byzantine city of Hierapolis was built on top of the white "castle" which is in total about 2,700 metres (8,860 ft) long, 600 m (1,970 ft) wide and 160 m (525 ft) high. It can be seen from the hills on the opposite side of the valley in the town of Denizli, 20 km away.

 Tourism is and has been a major industry. People have bathed in its pools for thousands of years. As recently as the mid-20th century, hotels were built over the ruins of Hierapolis, causing considerable damage. An approach road was built from the valley over the terraces, and motor bikes were allowed to go up and down the slopes. When the area was declared a World Heritage Site, the hotels were demolished and the road removed and replaced with artificial pools. Wearing shoes in the water is prohibited to protect the deposits.

 

 

Museum

In this museum, alongside historical artifacts from Hierapolis, there are also artifacts from Laodiceia, Colossae, Tripolis, Attuda and other towns of the Lycos (Çürüksu) valley. In addition to these, the museum has a large section devoted to artifacts found at Beycesultan Hüyük that includes some of the most beautiful examples of Bronze Age craft.
Artifacts from the Caria, Pisidia and Lydia regions are also on display in this museum. The museum’s exhibition space consists of three closed areas of the Hierapolis Bath and the open areas in the eastern side which are known to have been used as the library and gymnasium. The artifacts in open exhibition space are mostly marble and stone. Hierapolis is broken down into ruins.
 

Tourist attraction

Pamukkale is a tourist attraction. It is recognized as a World Heritage Site together with Hierapolis. Hierapolis-Pamukkale was made a World Heritage Site in 1988.
The underground volcanic activity which causes the hot springs also forced carbon dioxide into a cave, which was called the Plutonium, which here means "place of the god Pluto". This cave was used for religious purposes by priests of Cybele, who found ways to appear immune to the suffocating gas.
Tadpoles can be found in the pools.
 

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Big Island, Hawaii, USA

Big Island, Hawaii, USA

 

 

Hawaiʻi is the largest island located in the U.S. state of Hawaii. It is the largest and the southeastern-most of the Hawaiian islands, a chain of volcanic islands in the North Pacific Ocean. With an area of 4,028 square miles (10,430 km²), it is larger than all of the other islands in the archipelago combined and is the largest island in the United States. The island is often referred to as the Island of Hawaiʻi, the Big Island, or Hawaiʻi Island to distinguish between the island and the state. It is coterminous with Hawaiʻi County and includes the Hilo Micropolitan Statistical Area.

History

Hawaiʻi is said to have been named for Hawaiʻiloa, the legendary Polynesian navigator who first discovered it. Other accounts attribute the name to the legendary realm of Hawaiki, a place from which the Polynesian people are said to have originated , the place where they go in the afterlife, the realm of the gods and goddesses. Captain James Cook, the English explorer and navigator who was the captain of the first European expedition that discovered the Hawaiian Islands (obviously Polynesians had discovered them long before), called them the "Sandwich Islands" after his patron, the Earl of Sandwich. Cook was killed on the Big Island at Kealakekua Bay on February 14, 1779, in a mêlée which followed the theft of a ship's boat.
Hawaiʻi was the home island of Paiʻea Kamehameha, later known as Kamehameha the Great. Kamehameha united most of the Hawaiian islands under his rule in 1795, after several years of war, and gave the kingdom and the island chain the name of his native island.
 

Places of interest

• Akaka Falls; one of the taller waterfalls on the island.
• Amy B. H. Greenwell Ethnobotanical Garden houses many endangered endemic plants.
• East Hawaiʻi Cultural Center
• Hawaiʻi Tropical Botanical Garden
• Hawaiʻi Volcanoes National Park; comprising the active volcanoes Kīlauea and Mauna Loa
• Huliheʻe Palace; a royal palace in Kailua-Kona
• ʻImiloa Astronomy Center of Hawaiʻi in Hilo
• Ka Lae, the southernmost point in the United States
• Laupahoehoe Train Museum
• Lyman House Memorial Museum in Hilo
• Manuka State Wayside Park
• Mauna Kea Observatory; Mauna Kea Observatories
• Nani Mau Gardens
• Onizuka Center for International Astronomy
• Onizuka Space Center; museum dedicated to the memory of Challenger astronaut Ellison Onizuka located in Kona's Keahole Airport
• Pacific Tsunami Museum overlooking Hilo Bay
• Pana'ewa Rainforest Zoo in Hilo
• Pua Mau Place Arboretum and Botanical Garden
• Puʻuhonua o Hōnaunau National Historical Park
• Pu'ukohola Heiau National Historic Site, the site of one of the most significant heiau in Hawaii.
• Rainbow Falls State Park
• Sadie Seymour Botanical Gardens
• Umauma Falls
• University of Hawaiʻi at Hilo Botanical Gardens
• World Botanical Gardens
• Waipiʻo Valley
• Wao Kele o Puna

 
 

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Glow worm cave, New Zealand

Glow worm cave, New Zealand

 

The Waitomo Glowworm Caves attraction is a cave at Waitomo on the North Island of New Zealand, known for its population of glowworms, Arachnocampa luminosa. This species is found exclusively in New Zealand. They are around the size of an average mosquito. This cave is part of the Waitomo Caves system that includes the Ruakuri Cave and the Aranui Cave.

 

 

History

The name "Waitomo" comes from the Māori words wai, water and tomo, hole or shaft. The local Māori people had known about the caves for quite some time before the local Māori Chief Tane Tinorau and an English surveyor, Fred Mace, did an extensive exploration in 1887^].Their exploration was conducted with candlelight on a raft going into the cave where the stream goes underground. This is now the exit for the cave. As they began their journey, they came across the Glowworm Grotto and were amazed by the twinkling glow coming from the ceiling. As they travelled further into the cave by poling themselves towards an embankment, they were also astounded by the limestone formations. These formations surrounded them in all shapes and sizes.

They returned many times after and Chief Tane independently discovered the upper level entrance to the cave, which is now the current entrance. Tane Tinorau and his wife Huti, by 1889, had opened the cave to visitors and were leading groups for a small fee. The administration of the cave was taken over by the government in 1906 after there was an escalation in vandalism. In 1910, the Waitomo Caves Hotel was built to house the many visitors.

In 1989, the land and cave were returned to the descendants of Chief Tane Tinorau and Huti. They now receive a percentage of the cave’s revenue and are involved in the management and development of the cave. These descendants encompass many of the employees of the caves today.

 

Biology

The most renowned animal in the cave is the glowworm Arachnocampa luminosa. There are several small underwater lakes that were created by freshwater creeks or brooks.

The walls of the caves are covered with a variety of fungi including the cave flower (a distant relation to the genus Pleurotus) that is actually a mushroom-like fungus. The most common animals in the caves are insects. This includes albino cave ants, giant crickets, and of course the glowworms.

 

Guided tours

The guided tour through the Waitomo Glowworm Caves brings the visitor through three different levels and begins at the top level of the cave and the Catacombs. The levels are linked by the Tomo, which is a 16 m vertical shaft made of limestone. The second level is called the Banquet Chamber. This level is where early visitors stopped to eat and there is evidence of this in the smoke on the ceiling of the chamber. From here it may be possible to link back to the upper level to see the largest formation called the Pipe Organ but on busy days this area is closed to the public because the build-up of carbon monoxide may be hazardous.
The third and final level goes down into the Cathedral, demonstration platform, and the jetty. The Cathedral is an enclosed area with rough surfaces, now paved, and is about 18 m high, giving it good acoustics. A number of famous singers and choirs have performed here including Dame Kiri Te Kanawa.
The tour concludes with a boat ride through the Glowworm Grotto. The boat takes the visitor onto the underground Waitomo River where the only light comes from the tiny glowworms creating a sky of living lights.

 

 

 

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