Showing posts with label Amazing Pics. Show all posts
Showing posts with label Amazing Pics. Show all posts
DAL RIVER IN DALARNA, SWEDEN
The Dal River (or Dalälven in Swedish) is a river in central Sweden that flows from the north of Dalarna and runs into the sea in northern Uppland; it is commonly considered to be the southern border of Norrland. The northern part is split into two rivers: Österdalälven and Västerdalälven. The two connect in Djurås. It is over 520 km long — the second longest river in Sweden, and has a hydropower potential of 1420 megawatts, of which 2/3 is utilized. The largest power plant is located at the Trängslet dam. Dalälven has been significant historically as a raft transport route.
DALLOL SULFUR SPRINGS IN DANAKIL DESERT, ETHIOPIA
Dallol is a volcanic explosion crater (or maar) in the Danakil Depression, northeast of the Erta Ale Range in Ethiopia. It has been formed by the intrusion of basaltic magma in Miocene salt deposits and subsequent hydrothermal activity.Phreatic eruptions took place here in 1926, forming Dallol Volcano, numerous other eruption craters dot the salt flats nearby. These craters are the lowest known subaerial volcanic vents in the world, at over 45 m (150 ft) below sea level.
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THE MEDIEVAL CASTLE OF PAPHOS, CYPRUS
Paphos Castle is located on the edge of Paphos harbour. It was originally built as a Byzantine fort to protect the harbour. It was then rebuilt by the Lusignans in the thirteenth century after being destroyed in the earthquake of 1222. In 1570 it was dismantled by the Venetians. After capturing the island, the Ottomans restored and strengthened it. Throughout the ages it has seen many uses. It has served as a fortress, a prison and even a warehouse for salt during the British occupation of the island. More recently the castle serves as a backdrop to the annual open air Paphos cultural festival which takes place in September.
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EXPLORATION IN PEST, HUNGRY
Pest /ˈpɛst/; Hungarian pronunciation: [ˈpɛʃt]) is the eastern, mostly flat part of Budapest, Hungary, comprising about two thirds of the city's territory. It is separated from Buda, the other part of Budapest, by the Danube River. Among its most notable parts are the Inner City, including theHungarian Parliament, Heroes' Square and Andrássy Avenue. In colloquial Hungarian, "Pest" is often used for the whole capital of Budapest.
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BEAUTIFUL ISLANDS, SEYCHELLES
Seychelles (i/seɪˈʃɛlz/ say-shelz; French: [sɛʃɛl]), officially the Republic of Seychelles (French: République des Seychelles; Creole: Repiblik Sesel), is an island country spanning an archipelago of 115 islands in the Indian Ocean, some 1,500 kilometres (932 mi) east of mainland Africa, northeast of the island of Madagascar.
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Alberta, Canada
Alberta /ælˈbɜrtə/ is a province of Canada. With a population of 3,645,257 in 2011, it is Canada's fourth-most populous province and most populous of Canada's three prairie provinces. Alberta and its neighbour, Saskatchewan, were established as provinces on September 1, 1905. Alberta is located in western Canada, bounded by the provinces of British Columbia to the west and Saskatchewan to the east, the Northwest Territories to the north, and the U.S. state of Montana to the south. Alberta is one of three Canadian provinces and territories to border only a single U.S. state and is also one of only two provinces that are landlocked. Edmonton, the capital city of Alberta, is located near the geographic centre of the province and is the primary supply and service hub for Canada's crude oil and also oil sands (Athabasca Oil Sands) and other northern resource industries. Approximately 290 km (180 mi) south of the capital is Calgary, Alberta's largest city. Calgary and Edmonton centre Alberta's two census metropolitan areas, both of which have populations exceeding one million, while the province has 16 census agglomerations.Notable tourist destinations in the province include Banff, Canmore, Drumheller, Jasper and Sylvan Lake.
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Cappadocia, Turkey
Cappadocia (/kæpəˈdoʊʃə/; also Capadocia; Turkish Kapadokya, from Greek: Καππαδοκία / Kappadokía, Persian: کاپادوکیه Kāpādōkiyeh) is a historical region in Central Anatolia, largely in Nevşehir Province, in Turkey. In the time of Herodotus, the Cappadocians were reported as occupying the whole region from Mount Taurus to the vicinity of the Euxine (Black Sea). Cappadocia, in this sense, was bounded in the south by the chain of the Taurus Mountains that separate it from Cilicia, to the east by the upper Euphrates and the Armenian Highland, to the north by Pontus, and to the west by Lycaonia and eastern Galatia. The name was traditionally used in Christian sources throughout history and is still widely used as an international tourism concept to define a region of exceptional natural wonders, in particular characterized by fairy chimneys and a unique historical and cultural heritage.
The area is a popular tourist destination, as it has many areas with unique geological, historic, and cultural features.
The region is located southwest of the major city Kayseri, which has airline and railway service to Ankara and Istanbul.
The most important towns and destinations in Cappadocia are Urgup, Goreme, Ihlara Valley, Selime, Guzelyurt, Uchisar, Avanos and Zelve. Among the underground cities worth seeing are Derinkuyu, Kaymakli, Gaziemir and Ozkanak. The best historic mansions and cave houses for tourist stays are in Urgup, Goreme, Guzelyurt and Uchisar.
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Kilchurn Castle, Scotland
Kilchurn Castle is a ruined 15th and 17th century structure on a rocky peninsula at the northeastern end of Loch Awe, in Argyll and Bute, Scotland. Access to the Castle is sometimes restricted by higher-than-usual levels of water in the Loch, at which times the site effectively becomes a temporary island. It was the ancestral home of the Campbells of Glen Orchy, who later became the Earls of Breadalbane also known as the Breadalbane family branch, of the Clan Campbell. The earliest construction on the castle was the towerhouse and Laich Hall (looks onto Loch Awe).
Histroy
Kilchurn Castle was built in about 1450 by Sir Colin Campbell, first Lord of Glenorchy, as a five storey tower house with a courtyard defended by an outer wall. By about 1500 an additional range and a hall had been added to the south side of the castle. Further buildings went up during the 16th and 17th centuries. Kilchurn was on a small island in Loch Awe scarcely larger than the castle itself, although it is now connected to the mainland as the water level was altered in 1817. The castle would have been accessed via an underwater or low lying causeway. At the turn of the 16th century Kilchurn Castle was extended by Sir Duncan Campbell with the addition of a single storey dining hall built along the inside of the south curtain. During the second half of the century, another Sir Colin Campbell, the 6th Laird, continued to improve the castle's accommodation by adding some chambers to the north of the tower house, and remodelling the parapet. This included the introduction of the circular corner turrets adorned by corbels, most of which have survived remarkably well.
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Rotenburg, Germany

Rothenburg ob der Tauber (German pronunciation: [ˈʁoːtənbʊɐ̯k ɔp deːɐ̯ ˈtaʊbɐ] ( listen)) is a town in the district of Ansbach of Mittelfranken (Middle Franconia), the Franconia region of Bavaria, Germany, well known for its well-preserved medieval old town, a destination for tourists from around the world. Rothenburg was a Free Imperial City from the late Middle Ages to 1803.The name "Rothenburg ob der Tauber" means, in German, "Red fortress above the Tauber". This is so because the town is located on a plateau overlooking the Tauber River. As to the name "Rothenburg", some say it comes from the German words Rot (Red) and Burg (burgh, medieval fortified settlement), referring to the red colour of the roofs of the houses which overlook the river. The name may also refer to the process of retting ("rotten" in German) flax for linen production.
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Nuuk, Greenland

Nuuk (Danish: Godthåb) is the capital and largest city of Greenland. It is the seat of government, as well as the country's largest cultural and economic center. The major cities closest to the capital are Iqaluit and St. John's in Canada, and Reykjavík in Iceland. Nuuk is the seat of government for the Sermersooq municipality. In January 2013, it had a population of 16,454, making it one of the smallest capital cities in the world by population. Nuuk is the Kalaallisut word for "cape". It is so named because of its position at the end of the Nuup Kangerlua fjord on the eastern shore of the Labrador Sea.The site has a long history of habitation. The area around Nuuk was first occupied by the ancient pre-Inuit, Paleo-Eskimo people of the Saqqaq culture as far back as 2200 BC when they lived in the area around the now abandoned settlement of Qoornoq.For a long time it was occupied by the Dorset culture around the former settlement of Kangeq but they disappeared from the Nuuk district before AD 1000. The Nuuk area was later inhabited by Viking explorers in the 10th century, and shortly thereafter by Inuit peoples. Inuit and Norsemen both lived with little interaction in this area from about 1000 until the disappearance of the Norse settlement for uncertain reasons during the 15th century.
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Spotted Lake, Canada
Spotted Lake is very highly concentrated with numerous different minerals. It contains some of the highest quantities (in the world) of magnesium sulfate, calcium and sodium sulphates. It also contains extremely high concentrations of eight other minerals as well as some small doses of four others such as silver and titanium. Most of the water in the lake evaporates over the summer, leaving behind all the minerals. Large “spots” on the lake appear and depending on the mineral composition at the time, the spots will be different colors. The spots are made mainly of magnesium sulfate, which crystallizes in the summer. In the summer only the minerals in the lake remain, and they harden to form natural “walkways” around and between the spots...
Originally known to the First Nations of the Okanagan Valley as Khiluk, which was- and remains today revered as a sacred site producing therapeutic waters. During World War I the minerals of Spotted Lake were used in manufacturing ammunition. Later the area came under the control of the Ernest Smith Family, for a term of about 40 years. In 1979 Smith attempted to create interest in a spa at the lake. The First Nations responded with an effort to buy the lake; in October 2001 they finally struck a deal. First Nations arranged the purchase of 22 hectares of land for a total of $720,000, and contributed about 20% of the cost. The Indian Affairs Department paid the remainder.
Originally known to the First Nations of the Okanagan Valley as Khiluk, which was- and remains today revered as a sacred site producing therapeutic waters. During World War I the minerals of Spotted Lake were used in manufacturing ammunition. Later the area came under the control of the Ernest Smith Family, for a term of about 40 years. In 1979 Smith attempted to create interest in a spa at the lake. The First Nations responded with an effort to buy the lake; in October 2001 they finally struck a deal. First Nations arranged the purchase of 22 hectares of land for a total of $720,000, and contributed about 20% of the cost. The Indian Affairs Department paid the remainder.
Today there is a small sign nearby telling visitors about the lake’s healing powers. However a fence protects the lake-shore from liabilities of public access. Nevertheless the lake can be easily seen from nearby roads, and many do stop to admire.
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Rio de Janeiro, Brazil
Rio de Janeiro (/ˈriːoʊ dɪ ʒəˈnɛəroʊ/, /deɪ ʒəˈnɛəroʊ/, /deɪ dʒəˈnɛəroʊ/; Portuguese pronunciation: [ˈʁi.u dʒi ʒɐˈnejɾu], January River), commonly referred to simply as Rio,[2] is the capital city of the State of Rio de Janeiro, the second largest city of Brazil, and the third largest metropolitan area and agglomeration in South America, boasting approximately 6.3 million people within the city proper, making it the 6th largest in the Americas, and 26th in the world. Part of the city has been designated as a World Heritage Site, named "Rio de Janeiro: Carioca Landscapes between the Mountain and the Sea", identified by UNESCO on 1 July 2012 in the category Cultural Landscape. The city was the capital of Brazil for nearly two centuries, from 1763 to 1815 during the Portuguese colonial era, 1815 to 1821 as the capital of the United Kingdom of Portugal, Brazil and Algarves, and 1822 to 1960 of Brazil as an independent nation. Rio is nicknamed the Cidade Maravilhosa or "Marvelous City". Rio de Janeiro represents the second largest GDP in the country (and 30th largest in the world in 2008), estimated at about R$343 billion (IBGE/2008) (nearly US$201 billion), and is headquarters to two of Brazil's major companies—Petrobras and Vale, and major oil companies and telephony in Brazil, besides the largest conglomerate of media and communications companies in Latin America, the Globo Organizations. The home of many universities and institutes, it is the second largest center of research and development in Brazil, accounting for 17% of national scientific production—according to 2005 data. Rio de Janeiro is one of the most visited cities in the southern hemisphere and is known for its natural settings, carnival celebrations, samba, Bossa Nova, balneario beaches[10] such as Barra da Tijuca, Copacabana, Ipanema, and Leblon. Some of the most famous landmarks in addition to the beaches include the giant statue of Christ the Redeemer ("Cristo Redentor") atop Corcovado mountain, named one of the New Seven Wonders of the World; Sugarloaf mountain (Pão de Açúcar) with its cable car; the Sambódromo, a permanent grandstand-lined parade avenue which is used during Carnival; and Maracanã Stadium, one of the world's largest football stadiums. The 2016 Summer Olympics and the Paralympics will take place in Rio de Janeiro, which will mark the first time a South American or a Portuguese-speaking nation hosts the event. It will be the third time the Olympics will be held in a Southern Hemisphere city. On 12 August 2012, at the 2012 Summer Olympics closing ceremony, Mayor Eduardo Paes received the Olympic Flag, via Jacques Rogge, from London Mayor Boris Johnson. Rio's Maracanã Stadium, which held the final of the 1950 FIFA World Cup, will host the final match of the 2014 FIFA World Cup. Rio de Janeiro also hosted the World Youth Day in 2013..
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Rotorua, New Zealand
Rotorua (/ˌroʊtəˈruːə/, from Māori: Te Rotorua-nui-a-Kahumatamomoe, "The second great lake of Kahumatamomoe") is a city on the southern shores of the lake of the same name, in the Bay of Plenty area of the North Island of New Zealand. The city is the seat of the Rotorua District, a territorial authority encompassing the city and several other nearby towns. The majority of the Rotorua District, including the city, is in the Bay of Plenty local government region; a sizable southern section and a small western section are in the Waikato local government region. Rotorua city has an estimated permanent population of 56,100; the Rotorua District has a total estimated population of 68,700[3], of which 3,600 live in the Waikato section The city is in the heart of the North Island, just 60 kilometres (37 mi) south of Tauranga, 80 kilometres (50 mi) north of Taupo, 105 kilometres (65 mi) east of Hamilton, and 230 kilometres (140 mi) southeast of the nation's most populous city, Auckland. Rotorua is a major destination for both domestic and international tourists; the tourism industry is by far the largest industry in the district. The city is known for its geothermal activity, and features geysers – notably the Pohutu Geyser at Whakarewarewa – and hot mud pools. This thermal activity is sourced to the Rotorua caldera, on which the city lies. Rotorua is home to the Waiariki Institute of Technology. The Lakes of Rotorua are a collection of many lakes surrounding the city of Rotorua.
The name Rotorua comes from Māori, the full name being Te Rotorua-nui-a-Kahumatamomoe; roto means lake and rua two – Rotorua thus meaning 'Second lake'. Kahumatamomoe was the uncle of the Māori chief Ihenga, the ancestral explorer of the Te Arawa. It was the second major lake the chief discovered, and he dedicated it to his uncle. It is the largest of a multitude found to the northeast of the city, all connected with the Rotorua Caldera and nearby Mount Tarawera. The name can also mean the equally appropriate 'crater lake'. The area was initially settled by Māori of the Te Arawa iwi. The first European in the area was probably Phillip Tapsell who was trading from the Bay of Plenty coast at Maketu from 1828. He later married into Te Arawa and became highly regarded by them. Missionaries Henry Williams and Thomas Chapman visited in 1831 and Chapman and his wife established a mission at Te Koutu in 1835. This was abandoned within a year but Chapman returned in 1838 and established a second mission at Mokoia Island. The lakeshore was a prominent site of skirmishes during the New Zealand Wars of the 1860s. A "special town district" was created in the 1883, in order to promote Rotorua's potential as a spa destination. The town was connected to Auckland with the opening of the Rotorua Branch railway and commencement of the Rotorua Express train in 1894, resulting in the rapid growth of the town and tourism from this time forward. Rotorua was established as a borough in 1922, elected its first mayor in 1923, and declared a city in 1962 before becoming a District in 1979. Since 2004, the current mayor has been Kevin Winters.
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The name Rotorua comes from Māori, the full name being Te Rotorua-nui-a-Kahumatamomoe; roto means lake and rua two – Rotorua thus meaning 'Second lake'. Kahumatamomoe was the uncle of the Māori chief Ihenga, the ancestral explorer of the Te Arawa. It was the second major lake the chief discovered, and he dedicated it to his uncle. It is the largest of a multitude found to the northeast of the city, all connected with the Rotorua Caldera and nearby Mount Tarawera. The name can also mean the equally appropriate 'crater lake'. The area was initially settled by Māori of the Te Arawa iwi. The first European in the area was probably Phillip Tapsell who was trading from the Bay of Plenty coast at Maketu from 1828. He later married into Te Arawa and became highly regarded by them. Missionaries Henry Williams and Thomas Chapman visited in 1831 and Chapman and his wife established a mission at Te Koutu in 1835. This was abandoned within a year but Chapman returned in 1838 and established a second mission at Mokoia Island. The lakeshore was a prominent site of skirmishes during the New Zealand Wars of the 1860s. A "special town district" was created in the 1883, in order to promote Rotorua's potential as a spa destination. The town was connected to Auckland with the opening of the Rotorua Branch railway and commencement of the Rotorua Express train in 1894, resulting in the rapid growth of the town and tourism from this time forward. Rotorua was established as a borough in 1922, elected its first mayor in 1923, and declared a city in 1962 before becoming a District in 1979. Since 2004, the current mayor has been Kevin Winters.
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Fairy Pools, Isle of Skye, Scotland
Glen Brittle (Gleann Breadail in Scots Gaelic) is a large glen in the south of the Isle of Skye, in Scotland. It runs roughly south to north, along the River Brittle, which has its mouth at Loch Brittle (a sea loch). The glen is also overlooked from the east by the formidable Cuillin, the largest mountains on Skye. Many tributaries of the Brittle run down from these mountains into the glen, including a stream with waterfalls known as the Fairy Pools, a popular place to go for a walk. Because of its location by the peaks, the area is popular with hikers and mountain bikers. A single road and power line run through the glen on the east side of the river. On the slopes on the west side there are large sections of forest maintained by the Forestry Commission. In terms of settlement there are two scattered hamlets in the south of the glen - Glenbrittle and Bualintur. The most popular choice of accommodation is the SYHA's 1930s youth hostel by the Allt a' Choire Ghreadaidh (a Brittle tributary) just north of Glenbrittle hamlet. This is an ideal starting point for walks up to the Cuillin hills. The sandy beach at the southernmost point of the glen is the most popular attraction. It is adjacent to the campsite, where there is also a grocery shop, and campers often visit the beach and swim in the loch. Wildlife enthusiasts also enjoy the glen, as it is home to many interesting animals and plants. In the northern woods and fields red deer can be seen. Sheep and meadow pipits graze pretty much everywhere, whilst there are also large flocks of herring gulls and hooded crows about, as well as a pair of ravens by the hostel. Rabbits and swallows tend to be restricted to the farmland in the south. Again, the beach is the star attraction for wildlife. Turnstones, ringed plovers, grey herons, dunlins, curlews and most of all oystercatchers all hang around probing in the mud for food. One of the less pleasant species to populate the beach at dusk is the common midge.
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Giant Crystal Cave, Mexico
Cave of the Crystals or Giant Crystal Cave (Spanish: Cueva de los Cristales) is a cave connected to the Naica Mine 300 metres (980 ft) below the surface in Naica, Chihuahua, Mexico. The main chamber contains giant selenite crystals (gypsum, CaSO4·2 H2O), some of the largest natural crystals ever found.The cave's largest crystal found to date is 12 m (39 ft) in length, 4 m (13 ft) in diameter and 55 tons in weight. The cave is extremely hot with air temperatures reaching up to 58 °C (136 °F) with 90 to 99 percent humidity. The cave is relatively unexplored due to these factors. Without proper protection people can only endure approximately ten minutes of exposure at a time. A group of scientists known as the Naica Project have been heavily involved in researching these caverns.
In 1910 miners discovered a cavern beneath the Naica mine workings, the Cave of Swords (Spanish: Cueva de las Espadas). It is located at a depth of 120 m, above the Cave of Crystals, and contains spectacular, smaller (1 m long) crystals. It is speculated that at this level, transition temperatures may have fallen much more rapidly, leading to an end in the growth of the crystals. The Giant Crystal cave was discovered in 2000 by miners excavating a new tunnel for the Industrias Peñoles mining company located in Naica, Mexicowhile drilling through the Naica fault, which they were concerned would flood the mine. The mining complex in Naica contains substantial deposits of silver, zinc and lead. The Cave of Crystals is a horseshoe-shaped cavity in limestone. Its floor is covered with perfectly-faceted crystalline blocks. Huge crystal beams jut out from both the blocks and the floor. The caves are accessible today because the mining company's pumping operations keep them clear of water. If the pumping were stopped, the caves would again be submerged. The crystals deteriorate in air, so the Naica Project is attempting to visually document the crystals before they deteriorate further. Two other smaller caverns were also discovered in 2000, the Queen’s Eye Cave and the Candles’ Cave, and a further chamber was found in a drilling project in 2009. The new cave, named the Ice Palace, is 150 m deep and is not flooded, but its crystal formations are much smaller, with small 'cauliflower' formations and fine, threadlike crystals.
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In 1910 miners discovered a cavern beneath the Naica mine workings, the Cave of Swords (Spanish: Cueva de las Espadas). It is located at a depth of 120 m, above the Cave of Crystals, and contains spectacular, smaller (1 m long) crystals. It is speculated that at this level, transition temperatures may have fallen much more rapidly, leading to an end in the growth of the crystals. The Giant Crystal cave was discovered in 2000 by miners excavating a new tunnel for the Industrias Peñoles mining company located in Naica, Mexicowhile drilling through the Naica fault, which they were concerned would flood the mine. The mining complex in Naica contains substantial deposits of silver, zinc and lead. The Cave of Crystals is a horseshoe-shaped cavity in limestone. Its floor is covered with perfectly-faceted crystalline blocks. Huge crystal beams jut out from both the blocks and the floor. The caves are accessible today because the mining company's pumping operations keep them clear of water. If the pumping were stopped, the caves would again be submerged. The crystals deteriorate in air, so the Naica Project is attempting to visually document the crystals before they deteriorate further. Two other smaller caverns were also discovered in 2000, the Queen’s Eye Cave and the Candles’ Cave, and a further chamber was found in a drilling project in 2009. The new cave, named the Ice Palace, is 150 m deep and is not flooded, but its crystal formations are much smaller, with small 'cauliflower' formations and fine, threadlike crystals.
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Meteora, Greece
The Metéora (Greek: Μετέωρα, pronounced [mɛˈtɛoɾɐ], lit. "middle of the sky", "suspended in the air" or "in the heavens above" — etymologically related to "Meteorite") is one of the largest and most important complexes of Eastern Orthodox monasteries in Greece, second only to Mount Athos. The six monasteries are built on natural sandstone rock pillars, at the northwestern edge of the Plain of Thessaly near the Pineios river and Pindus Mountains, in central Greece. The nearest town is Kalambaka. The Metéora is included on the UNESCO World Heritage List under criteria[ I, II, IV, V and VII.
The Theopetra caves 5 kilometres (3.1 mi) south of Meteora had inhabitants fifty millennia ago
The oldest known example of a man-made structure was found within a prehistoric cave in central Greece, according to the Greek culture ministry. The structure is a stone wall that blocked two-thirds of the entrance to the Theopetra cave near Kalambaka on the north edge of the Thessalian plain. It was constructed 23,000 years ago, probably as a barrier to cold winds. “An optical dating test, known as Optically Stimulated Luminescence, was applied on quartz grains nested within the stones. We dated four different samples from the sediment and soil materials, and all provided identical dates,” Nikolaos Zacharias, director of the laboratory of archaeometry at the University of Peloponnese, told Discovery News. According to a statement by the ministry of culture, “the dating matches the coldest period of the most recent ice age, indicating that the cavern’s inhabitants built the stone wall to protect themselves from the cold.” Excavated since 1987, the Theopetra cave is well known to palaeontologists as it was used and inhabited continuously from the Palaeolithic period onwards (50,000 to 5,000 years ago).[5] In the 9th century, an ascetic group of hermit monks moved up to the ancient pinnacles. They were the first people to inhabit Metéora. They lived in hollows and fissures in the rock towers, some of which reach 1800 ft (550m) above the plain. This great height, combined with the sheerness of the cliff walls, kept away all but the most determined visitors. Initially the hermits led a life of solitude, meeting only on Sundays and special days to worship and pray in a chapel built at the foot of a rock known as Dhoupiani. As early as the 11th century AD hermit monks were believed to be living among the caves and cutouts in the rocks. The exact date of the establishment of the monasteries is unknown. By the late 11th and early 12th centuries, a rudimentary monastic state had formed called the Skete of Stagoi and was centered around the still-standing church of Theotokos (mother of God). By the end of the 12th century, an ascetic community had flocked to Metéora.
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The Theopetra caves 5 kilometres (3.1 mi) south of Meteora had inhabitants fifty millennia ago
The oldest known example of a man-made structure was found within a prehistoric cave in central Greece, according to the Greek culture ministry. The structure is a stone wall that blocked two-thirds of the entrance to the Theopetra cave near Kalambaka on the north edge of the Thessalian plain. It was constructed 23,000 years ago, probably as a barrier to cold winds. “An optical dating test, known as Optically Stimulated Luminescence, was applied on quartz grains nested within the stones. We dated four different samples from the sediment and soil materials, and all provided identical dates,” Nikolaos Zacharias, director of the laboratory of archaeometry at the University of Peloponnese, told Discovery News. According to a statement by the ministry of culture, “the dating matches the coldest period of the most recent ice age, indicating that the cavern’s inhabitants built the stone wall to protect themselves from the cold.” Excavated since 1987, the Theopetra cave is well known to palaeontologists as it was used and inhabited continuously from the Palaeolithic period onwards (50,000 to 5,000 years ago).[5] In the 9th century, an ascetic group of hermit monks moved up to the ancient pinnacles. They were the first people to inhabit Metéora. They lived in hollows and fissures in the rock towers, some of which reach 1800 ft (550m) above the plain. This great height, combined with the sheerness of the cliff walls, kept away all but the most determined visitors. Initially the hermits led a life of solitude, meeting only on Sundays and special days to worship and pray in a chapel built at the foot of a rock known as Dhoupiani. As early as the 11th century AD hermit monks were believed to be living among the caves and cutouts in the rocks. The exact date of the establishment of the monasteries is unknown. By the late 11th and early 12th centuries, a rudimentary monastic state had formed called the Skete of Stagoi and was centered around the still-standing church of Theotokos (mother of God). By the end of the 12th century, an ascetic community had flocked to Metéora.
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Luxor, Egypt
Luxor (/ˈlʌk.sɔr/ or /ˈlʊk.sɔr/;[3] Arabic: الأقصر al-Uqṣur ; Egyptian Arabic: Loʔṣor IPA: [ˈloʔsˤoɾ]; Saidi Arabic: Logṣor [ˈloɡsˤor]) is a city in Upper (southern) Egypt and the capital of Luxor Governorate. The population numbers 487,896 (2010 estimate), with an area of approximately 416 square kilometres (161 sq mi) As the site of the Ancient Egyptian city of Thebes, Luxor has frequently been characterized as the "world's greatest open air museum", as the ruins of the temple complexes at Karnak and Luxor stand within the modern city. Immediately opposite, across the River Nile, lie the monuments, temples and tombs on the West Bank Necropolis, which include the Valley of the Kings and Valley of the Queens. Thousands of tourists from all around the world arrive annually to visit these monuments, contributing a large part towards the economy for the modern city.
Luxor was the ancient city of Thebes, the great capital of Egypt during the New Kingdom, and the glorious city of the god Amon-Ra. The city was regarded in the Ancient Egyptian texts as w3s.t (approximate pronunciation: "Waset"), which meant "city of the sceptre" and also as t3 ip3t (conventionally pronounced as "ta ipet" and meaning "the shrine") and then, in a later period, the Greeks called it Thebai and the Romans after them Thebae. Thebes was also known as "the city of the 100 gates", sometimes being called "southern Heliopolis" ('Iunu-shemaa' in Ancient Egyptian), to distinguish it from the city of Iunu or Heliopolis, the main place of worship for the god Re in the north. It was also often referred to as niw.t, which simply means "city", and was one of only three cities in Egypt for which this noun was used (the other two were Memphis and Heliopolis); it was also called niw.t rst, "southern city", as the southernmost of them.
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Luxor was the ancient city of Thebes, the great capital of Egypt during the New Kingdom, and the glorious city of the god Amon-Ra. The city was regarded in the Ancient Egyptian texts as w3s.t (approximate pronunciation: "Waset"), which meant "city of the sceptre" and also as t3 ip3t (conventionally pronounced as "ta ipet" and meaning "the shrine") and then, in a later period, the Greeks called it Thebai and the Romans after them Thebae. Thebes was also known as "the city of the 100 gates", sometimes being called "southern Heliopolis" ('Iunu-shemaa' in Ancient Egyptian), to distinguish it from the city of Iunu or Heliopolis, the main place of worship for the god Re in the north. It was also often referred to as niw.t, which simply means "city", and was one of only three cities in Egypt for which this noun was used (the other two were Memphis and Heliopolis); it was also called niw.t rst, "southern city", as the southernmost of them.
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Havasu Falls, Grand Canyon, Arizona, USA
Havasu Falls (Havasupai: Havasuw Hagjahgeevma) is a waterfall in the Grand Canyon located 1½ miles (2.4 km) from Supai, Arizona, USA. It is arguably the most famous and most visited of all the falls on Havasu Creek and consists of one main chute that drops over a 90-foot (27 m) to 100-foot (30 m) vertical cliff into a large pool. Due to the high mineral content of the water, the configuration of the falls is ever-changing and sometimes breaks into two separate chutes of water. The falls are known for their natural pools, created by mineralization, although the configuration of the falls and the pools are damaged or destroyed repeatedly by large floods that wash through the area. A small man-made dam was once constructed to help restore the pools and to preserve what is left. High calcium carbonate concentration in the water creates the vivid blue-green color and forms the natural travertine dams that occur in various places near the falls. There are many picnic tables on the opposite side of the creek, and it is easy to cross over by following the edges of the pools. It is possible to swim behind the falls and enter a small rock shelter behind it
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Hallgrímskirkja - Reykjavík, Iceland
Hallgrímskirkja (Icelandic pronunciation: [ˈhatlkrimsˌcʰɪrca], church of Hallgrímur) is a Lutheran (Church of Iceland) parish church in Reykjavík, Iceland. At 74.5 metres (244 ft), it is the largest church in Iceland and the sixth tallest architectural structure in Iceland after Longwave radio mast Hellissandur, the radio masts of US Navy at Grindavík, Eiðar longwave transmitter and Smáratorg tower. The church is named after the Icelandic poet and clergyman Hallgrímur Pétursson (1614 to 1674), author of the Passion Hymns.
State Architect Guðjón Samúelsson's design of the church was commissioned in 1937. He is said to have designed it to resemble the basalt lava flows of Iceland's landscape. It took 38 years to build the church. Construction work began in 1945 and ended in 1986, the landmark tower being completed long before the church's actual completion. The crypt beneath the choir was consecrated in 1948, the steeple and wings were completed in 1974, and thenave was consecrated in 1986. Situated in the centre of Reykjavík, it is one of the city's best-known landmarks and is visible throughout the city. It is similar in style to the expressionist architecture of Grundtvig's Church of Copenhagen, Denmark, completed in 1940.
The church houses a large pipe organ by the German organ builder Johannes Klais of Bonn. It has mechanical action, four manuals and pedal, 102 ranks, 72 stops and 5275 pipes. It is 15 metres tall and weighs 25 tons. Its construction was finished in December 1992. It has been recorded by Christopher Herrick in his Organ Fireworks VII CD.
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