1.
Uluru
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It lies 335 km south west of the nearest large town, Alice Springs,450 km by road. Uluru is sacred to the Pitjantjatjara Anangu, the Aboriginal people of the area, the area around the formation is home to an abundance of springs, waterholes, rock caves and ancient paintings. Uluru is listed as a UNESCO World Heritage Site, Uluru and Kata Tjuta, also known as the Olgas, are the two major features of the Uluṟu-Kata Tjuṯa National Park. The local Anangu, the Pitjantjatjara people, call the landmark Uluṟu and this word is a proper noun, with no further particular meaning in the Pitjantjatjara dialect, although it is used as a local family name by the senior Traditional Owners of Uluru. On 19 July 1873, the surveyor William Gosse sighted the landmark and named it Ayers Rock in honour of the then Chief Secretary of South Australia, since then, both names have been used. In 1993, a dual naming policy was adopted that allowed official names that consist of both the traditional Aboriginal name and the English name, on 15 December 1993, it was renamed Ayers Rock / Uluru and became the first official dual-named feature in the Northern Territory. The order of the names was officially reversed to Uluru / Ayers Rock on 6 November 2002 following a request from the Regional Tourism Association in Alice Springs. Uluru is one of Australias most recognisable natural landmarks, the sandstone formation stands 348 m high, rising 863 m above sea level with most of its bulk lying underground, and has a total circumference of 9.4 km. Uluru is notable for appearing to change colour at different times of the day and year, most notably when it glows red at dawn, Kata Tjuta, also called Mount Olga or the Olgas, lies 25 km west of Uluru. Special viewing areas with access and parking have been constructed to give tourists the best views of both sites at dawn and dusk. Uluru is an inselberg, literally island mountain, an inselberg is a prominent isolated residual knob or hill that rises abruptly from and is surrounded by extensive and relatively flat erosion lowlands in a hot, dry region. Uluru is also referred to as a monolith, although this is a somewhat ambiguous term that is generally avoided by geologists. The remarkable feature of Uluru is its homogeneity and lack of jointing and parting at bedding surfaces, leading to the lack of development of scree slopes and these characteristics led to its survival, while the surrounding rocks were eroded. Uluru is dominantly composed of coarse-grained arkose and some conglomerate, the grains are typically 2–4 millimetres in diameter, and are angular to subangular, the finer sandstone is well sorted, with sorting decreasing with increasing grain size. The rock fragments include subrounded basalt, invariably replaced to various degrees by chlorite and epidote, the minerals present suggest derivation from a predominantly granite source, similar to the Musgrave Block exposed to the south. When relatively fresh, the rock has a colour. The strata at Uluru are nearly vertical, dipping to the south west at 85°, the strata dip below the surrounding plain and no doubt extend well beyond Uluru in the subsurface, but the extent is not known. The similar mineral composition of the Mutitjulu Arkose and the ranges to the south is now explained
2.
Northern Territory
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The Northern Territory is a federal Australian territory in the central and central northern regions of Australia. It shares borders with Western Australia to the west, South Australia to the south, to the north, the territory is bordered by the Timor Sea, the Arafura Sea and the Gulf of Carpentaria. Despite its large area—over 1,349,129 square kilometres, the Northern Territorys population of 244,000 makes it the least populous of Australias eight major states and territories, having fewer than half as many people as Tasmania. The archaeological history of the Northern Territory begins over 40,000 years ago when Indigenous Australians settled the region, makassan traders began trading with the indigenous people of the Northern Territory for trepang from at least the 18th century onwards. The coast of the territory was first seen by Europeans in the 17th century, the British were the first Europeans to attempt to settle the coastal regions. After three failed attempts to establish a settlement, success was achieved in 1869 with the establishment of a settlement at Port Darwin. Today the economy is based on tourism, especially Kakadu National Park in the Top End and the Uluru-Kata Tjuta National Park in central Australia, the capital and largest city is Darwin. The population is not concentrated in regions but rather along the Stuart Highway. The other major settlements are Palmerston, Alice Springs, Katherine, Nhulunbuy, residents of the Northern Territory are often known simply as Territorians and fully as Northern Territorians, or more informally as Top Enders and Centralians. With the coming of the British, there were four attempts to settle the harsh environment of the northern coast. The Northern Territory was part of colonial New South Wales from 1825 to 1863, except for a time from February to December 1846. It was part of South Australia from 1863 to 1911, under the administration of colonial South Australia, the overland telegraph was constructed between 1870 and 1872. A railway was built between Palmerston and Pine Creek between 1883 and 1889. The economic pattern of raising and mining was established so that by 1911 there were 513,000 cattle. Victoria River Downs was at one time the largest cattle station in the world, gold was found at Grove Hill in 1872 and at Pine Creek, Brocks Creek, Burrundi, and copper was found at Daly River. On 1 January 1911, a decade after federation, the Northern Territory was separated from South Australia, alfred Deakin opined at this time To me the question has been not so much commercial as national, first, second, third and last. Either we must accomplish the peopling of the territory or submit to its transfer to some other nation. In late 1912 there was growing sentiment that the name Northern Territory was unsatisfactory, the names Kingsland, Centralia and Territoria were proposed with Kingsland becoming the preferred choice in 1913
3.
Australia
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Australia, officially the Commonwealth of Australia, is a country comprising the mainland of the Australian continent, the island of Tasmania and numerous smaller islands. It is the worlds sixth-largest country by total area, the neighbouring countries are Papua New Guinea, Indonesia and East Timor to the north, the Solomon Islands and Vanuatu to the north-east, and New Zealand to the south-east. Australias capital is Canberra, and its largest urban area is Sydney, for about 50,000 years before the first British settlement in the late 18th century, Australia was inhabited by indigenous Australians, who spoke languages classifiable into roughly 250 groups. The population grew steadily in subsequent decades, and by the 1850s most of the continent had been explored, on 1 January 1901, the six colonies federated, forming the Commonwealth of Australia. Australia has since maintained a liberal democratic political system that functions as a federal parliamentary constitutional monarchy comprising six states. The population of 24 million is highly urbanised and heavily concentrated on the eastern seaboard, Australia has the worlds 13th-largest economy and ninth-highest per capita income. With the second-highest human development index globally, the country highly in quality of life, health, education, economic freedom. The name Australia is derived from the Latin Terra Australis a name used for putative lands in the southern hemisphere since ancient times, the Dutch adjectival form Australische was used in a Dutch book in Batavia in 1638, to refer to the newly discovered lands to the south. On 12 December 1817, Macquarie recommended to the Colonial Office that it be formally adopted, in 1824, the Admiralty agreed that the continent should be known officially as Australia. The first official published use of the term Australia came with the 1830 publication of The Australia Directory and these first inhabitants may have been ancestors of modern Indigenous Australians. The Torres Strait Islanders, ethnically Melanesian, were originally horticulturists, the northern coasts and waters of Australia were visited sporadically by fishermen from Maritime Southeast Asia. The first recorded European sighting of the Australian mainland, and the first recorded European landfall on the Australian continent, are attributed to the Dutch. The first ship and crew to chart the Australian coast and meet with Aboriginal people was the Duyfken captained by Dutch navigator, Willem Janszoon. He sighted the coast of Cape York Peninsula in early 1606, the Dutch charted the whole of the western and northern coastlines and named the island continent New Holland during the 17th century, but made no attempt at settlement. William Dampier, an English explorer and privateer, landed on the north-west coast of New Holland in 1688, in 1770, James Cook sailed along and mapped the east coast, which he named New South Wales and claimed for Great Britain. The first settlement led to the foundation of Sydney, and the exploration, a British settlement was established in Van Diemens Land, now known as Tasmania, in 1803, and it became a separate colony in 1825. The United Kingdom formally claimed the part of Western Australia in 1828. Separate colonies were carved from parts of New South Wales, South Australia in 1836, Victoria in 1851, the Northern Territory was founded in 1911 when it was excised from South Australia
4.
Stratum
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In geology and related fields, a stratum is a layer of sedimentary rock or soil with internally consistent characteristics that distinguish it from other layers. The stratum is the unit in a stratigraphic column and forms the basis of the study of stratigraphy. Each layer is one of a number of parallel layers that lie one upon another. They may extend over hundreds of thousands of kilometers of the Earths surface. Strata are typically seen as bands of different colored or differently structured material exposed in cliffs, road cuts, quarries, individual bands may vary in thickness from a few millimeters to a kilometer or more. Each band represents a mode of deposition, river silt, beach sand, coal swamp, sand dune, lava bed. Geologists study rock strata and categorize them by the material of beds, each distinct layer is typically assigned to the name of sheet, usually based on a town, river, mountain, or region where the formation is exposed and available for study. For example, the Burgess Shale is an exposure of dark, occasionally fossiliferous. Slight distinctions in material in a formation may be described as members, formations are collected into groups while groups may be collected into supergroups. Archaeological horizon Geologic formation Geologic map Geologic unit Law of superposition Bed GeoWhen Database
5.
Monolithos, Greece
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Monolithos is a Greek village on the island of Rhodes, South Aegean region, belonging to the municipal unit of Attavyros. It is located 10 km south-east of Apolakkia and 30 km from Prasonisi, outside the village is the medieval Castle, built on top of a 100m rock. This castle was built in 1480 by the Knights of Saint John to protect the island from attacks, in fact, this castle was never conquered. The Castle of Monolithos is widely ruined today but it offers views of the sea. Inside the Castle, there is a working chapel dedicated to Agios Panteleimon. Access to the castle is by a cut into the rock. The steps, whilst not particularly steep, are quite slippery due to the numbers of visitors wearing them away. On the climb up to the top, you are likely to see hundreds, if not thousands and these piles are left there by the visitors as a form of a memento. Media related to Monolithos at Wikimedia Commons Rhodes Monolithos, Information and pictures of Monolithos Castle on Rhodes Rhodes Island at Greeka. com Images of Monolithos at Flickr
6.
Rhodes
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Rhodes is the largest of the Dodecanese islands in terms of land area and also the island groups historical capital. Administratively the island forms a municipality within the Rhodes regional unit. The principal town of the island and seat of the municipality is Rhodes, the city of Rhodes had 50,636 inhabitants in 2011. It is located northeast of Crete, southeast of Athens and just off the Anatolian coast of Turkey, Rhodes nickname is The island of the Knights, named after the Knights of Saint John of Jerusalem, who once conquered the land. Historically, Rhodes was famous worldwide for the Colossus of Rhodes, the Medieval Old Town of the City of Rhodes has been declared a World Heritage Site. Today, it is one of the most popular tourist destinations in Europe, the island has been known as Ρόδος in Greek throughout its history. In addition, the island has been called Rodi in Italian, Rodos in Turkish, and Rodi or Rodes in Ladino. The island of Rhodes is shaped like a spearhead,79.7 km long and 38 km wide, with an area of approximately 1,400 square kilometres. The city of Rhodes is located at the tip of the island, as well as the site of the ancient. The main air gateway is located 14 km to the southwest of the city in Paradisi, the road network radiates from the city along the east and west coasts. There are mineral-rich spring water used to give medicinal baths and the spa resorts offer various health treatments, Rhodes is situated 363 km east-south-east from the Greek mainland, and 18 km from the southern shore of Turkey. The interior of the island is mountainous, sparsely inhabited and covered with forests of pine, while the shores are rocky, the island has arable strips of land where citrus fruit, wine grapes, vegetables, olives and other crops are grown. The Rhodian population of deer was found to be genetically distinct in 2005. In Petaloudes Valley, large numbers of tiger moths gather during the summer months, mount Attavyros, at 1,216 metres, is the islands highest point of elevation. Earthquakes include the 226 BC earthquake that destroyed the Colossus of Rhodes, one on 3 May 1481 which destroyed much of the city of Rhodes, and one on 26 June 1926. On 15 July 2008, Rhodes was struck by a 6.3 magnitude earthquake causing minor damage to a few old buildings, Rhodes has a hot-summer Mediterranean climate. The island was inhabited in the Neolithic period, although remains of this culture. In the 16th century BC, the Minoans came to Rhodes, later Greek mythology recalled a Rhodian race called the Telchines and associated the island of Rhodes with Danaus, it was sometimes nicknamed Telchinis
7.
Greece
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Greece, officially the Hellenic Republic, historically also known as Hellas, is a country in southeastern Europe, with a population of approximately 11 million as of 2015. Athens is the capital and largest city, followed by Thessaloniki. Greece is strategically located at the crossroads of Europe, Asia, situated on the southern tip of the Balkan peninsula, it shares land borders with Albania to the northwest, the Republic of Macedonia and Bulgaria to the north, and Turkey to the northeast. Greece consists of nine regions, Macedonia, Central Greece, the Peloponnese, Thessaly, Epirus, the Aegean Islands, Thrace, Crete. The Aegean Sea lies to the east of the mainland, the Ionian Sea to the west, the Cretan Sea and the Mediterranean Sea to the south. Greece has the longest coastline on the Mediterranean Basin and the 11th longest coastline in the world at 13,676 km in length, featuring a vast number of islands, eighty percent of Greece is mountainous, with Mount Olympus being the highest peak at 2,918 metres. From the eighth century BC, the Greeks were organised into various independent city-states, known as polis, which spanned the entire Mediterranean region and the Black Sea. Greece was annexed by Rome in the second century BC, becoming a part of the Roman Empire and its successor. The Greek Orthodox Church also shaped modern Greek identity and transmitted Greek traditions to the wider Orthodox World, falling under Ottoman dominion in the mid-15th century, the modern nation state of Greece emerged in 1830 following a war of independence. Greeces rich historical legacy is reflected by its 18 UNESCO World Heritage Sites, among the most in Europe, Greece is a democratic and developed country with an advanced high-income economy, a high quality of life, and a very high standard of living. A founding member of the United Nations, Greece was the member to join the European Communities and has been part of the Eurozone since 2001. Greeces unique cultural heritage, large industry, prominent shipping sector. It is the largest economy in the Balkans, where it is an important regional investor, the names for the nation of Greece and the Greek people differ from the names used in other languages, locations and cultures. The earliest evidence of the presence of human ancestors in the southern Balkans, dated to 270,000 BC, is to be found in the Petralona cave, all three stages of the stone age are represented in Greece, for example in the Franchthi Cave. Neolithic settlements in Greece, dating from the 7th millennium BC, are the oldest in Europe by several centuries and these civilizations possessed writing, the Minoans writing in an undeciphered script known as Linear A, and the Mycenaeans in Linear B, an early form of Greek. The Mycenaeans gradually absorbed the Minoans, but collapsed violently around 1200 BC and this ushered in a period known as the Greek Dark Ages, from which written records are absent. The end of the Dark Ages is traditionally dated to 776 BC, the Iliad and the Odyssey, the foundational texts of Western literature, are believed to have been composed by Homer in the 7th or 8th centuries BC. With the end of the Dark Ages, there emerged various kingdoms and city-states across the Greek peninsula, in 508 BC, Cleisthenes instituted the worlds first democratic system of government in Athens
8.
Landsat 7
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Landsat 7 is the seventh satellite of the Landsat program. Launched on April 15,1999, Landsat 7s primary goal is to refresh the global archive of photos, providing up-to-date. The Landsat Program is managed and operated by the USGS, the NASA World Wind project allows 3D images from Landsat 7 and other sources to be freely navigated and viewed from any angle. The satellites companion, Earth Observing-1, trails by one minute, Landsat 7 was built by Lockheed Martin Space Systems Company. Landsat 7 was designed to last for five years, and has the capacity to collect and it is in a polar, sun-synchronous orbit, meaning it scans across the entire earths surface. With an altitude of 705 kilometers +/-5 kilometers, it takes 232 orbits, or 16 days, the satellite weighs 1973 kg, is 4.04 m long, and 2.74 m in diameter. Unlike its predecessors, Landsat 7 has a solid state memory of 378 gigabits, the main instrument on board Landsat 7 is the Enhanced Thematic Mapper Plus. The SLC consists of a pair of mirrors that rotate about an axis in tandem with the motion of the main ETM+ scan mirror. The purpose of the SLC is to compensate for the motion of the spacecraft so that the resulting scans are aligned parallel to each other. Without the effects of the SLC, the instrument images the Earth in a fashion, resulting in some areas that are imaged twice. The net effect is that approximately 22% of the data in a Landsat 7 scene is missing when acquired without a functional SLC, following the SLC failure, an Anomaly Response Team was assembled, consisting of representatives from the USGS, NASA, and Hughes Santa Barbara Remote Sensing. The team assembled a list of possible scenarios, most of which pointed at a mechanical problem with the SLC itself. Since there is no backup SLC, a failure would indicate that the problem was permanent. However, the team was unable to rule out the possibility of an electrical failure, though such a possibility was deemed remote. This operation was successful, and on September 5,2003 and it was immediately apparent that the migration to the Side-B electrical harness had not fixed the problem with the SLC. Following this, the instrument was reconfigured again to use its primary electrical harness, the subsequent conclusion of the ART was that the SLC problem was mechanical and permanent in nature. Landsat 7 continues to acquire data in this mode, Data products are available with the missing data optionally filled in using other Landsat 7 data selected by the user. In 2013, Landsat 7 was joined by Landsat 8, the contract was part of the NASA Scientific Data Purchase which was administrated through NASAs John C. Stennis Space Center
9.
Brandberg Mountain
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The Brandberg, is Namibias highest mountain. Brandberg Mountain is located in former Damaraland, now Erongo, in the northwestern Namib Desert, near the coast, and covers an area of approximately 650 km². With its highest point, the Königstein, standing at 2,573 m above sea level and located on the flat Namib gravel plains, on a clear day The Brandberg can be seen from a great distance. There are various routes to the summit, the easiest being up the Gaaseb river valley, the nearest settlement is Uis, roughly 30 km from the mountain. The name Brandberg is Afrikaans, Dutch and German for Fire Mountain, the Damara name for the mountain is Dâures, which means burning mountain, while the Herero name, Omukuruvaro means mountain of the Gods. The Brandberg Massif or Brandberg Intrusion is an intrusion, which forms a dome-shaped massif. It originated during Early Cretaceous rifting that led to the opening of the South Atlantic Ocean, argon–argon dating yielded intrusive ages of 132 to 130 Ma. The dominant plutonic rock is a medium grained biotite-hornblende granite. In the western interior of the massif, a 2 km in diameter body of pyroxene-bearing monzonite is exposed, the youngest intrusive rocks based on cross-cutting relations are arfvedsonite granite dikes and sills in the southwestern periphery of the Brandberg massif which crop out in the Amis valley. The arfvedsonite granites contain minerals rich in rare earth element minerals such as pyrochlore, remnants of Cretaceous volcanic rocks are preserved in a collar along the western and southern margins of the massif. Their angle of dip increases towards the contact where clasts of country-rock occur within the forming a magmatic breccia. Erosion subsequently removed the overburden rock, apatite fission track dating indicates approximately 5 km denudation between 80 and 60 Ma. An associated feature is the Doros Complex, the Brandberg is a spiritual site of great significance to the San tribes. The main tourist attraction is The White Lady rock painting, located on a face with other art work, under a small rock overhang. The ravine contains more than 1000 rock shelters, as well as more than 45000 rock paintings, to reach The White Lady it is necessary to hike for about 40 minutes over rough terrain, along the ancient watercourses threading through the mountain. The higher elevations of the mountain contain hundreds of rock paintings, most of which have been painstakingly documented by Harald Pager. Pagers work was published by the Heinrich Bart Institute, in the six volume series Rock Paintings of the Upper Brandberg edited by Tilman Lenssen-Erz. The Brandberg is also home to some interesting desert flora, Damaraland is well known for its grotesque aloes and euphorbias and the region around the mountain is no exception
10.
Namibia
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Namibia, officially the Republic of Namibia, is a country in southern Africa whose western border is the Atlantic Ocean. It shares land borders with Zambia and Angola to the north, Botswana to the east and South Africa to the south, although it does not border Zimbabwe, a part of less than 200 metres of the Zambezi River separates the two countries. Namibia gained independence from South Africa on 21 March 1990, following the Namibian War of Independence. Its capital and largest city is Windhoek, and it is a state of the United Nations, the Southern African Development Community, the African Union. The dry lands of Namibia were inhabited since early times by the San, Damara, since about the 14th century, immigrating Bantu peoples arrived as part of the Bantu expansion. Since then the Bantu groups in total, known as the Ovambo people, have dominated the population of the country, in the late 19th century during European colonization, the German Empire established rule over most of the territory as a protectorate in 1884. It began to develop infrastructure and farming, and maintained this German colony until 1915, after the end of World War I, in 1920 the League of Nations mandated the country to the United Kingdom, under administration by South Africa. It imposed its laws, including racial classifications and rules, from 1948, with the National Party elected to power, South Africa applied apartheid also to what was known as South West Africa. In 1878 the Cape of Good Hope had annexed the port of Walvis Bay and the offshore Penguin Islands, following continued guerrilla warfare, South Africa installed an interim administration in Namibia in 1985. Namibia obtained full independence from South Africa in 1990, but Walvis Bay and the Penguin Islands remained under South African control until 1994. Namibia has a population of 2.1 million people and a stable multi-party parliamentary democracy, Agriculture, herding, tourism and the mining industry – including mining for gem diamonds, uranium, gold, silver, and base metals – form the basis of its economy. The large, arid Namib Desert has resulted in Namibia being overall one of the least densely populated countries in the world, Namibia enjoys high political, economic and social stability. The name of the country is derived from the Namib Desert, before its independence in 1990, the area was known first as German South-West Africa, then as South-West Africa, reflecting the colonial occupation by the Germans and the South Africans. The dry lands of Namibia were inhabited since early times by San, Damara, from about the 14th century, immigrating Bantu peoples arrived during the Bantu expansion from central Africa. From the late 18th century onwards, Oorlam people from Cape Colony crossed the Orange River and their encounters with the nomadic Nama tribes were largely peaceful. The missionaries accompanying the Oorlam were well received by them, the right to use waterholes, on their way further northwards, however, the Oorlam encountered clans of the Herero at Windhoek, Gobabis, and Okahandja, who resisted their encroachment. The Nama-Herero War broke out in 1880, with hostilities ebbing only after the German Empire deployed troops to the places and cemented the status quo among the Nama, Oorlam. The first Europeans to disembark and explore the region were the Portuguese navigators Diogo Cão in 1485 and Bartolomeu Dias in 1486, like most of interior Sub-Saharan Africa, Namibia was not extensively explored by Europeans until the 19th century
11.
Rio de Janeiro
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Rio de Janeiro, or simply Rio, is the second-most populous municipality in Brazil and the sixth-most populous in the Americas. The metropolis is anchor to the Rio de Janeiro metropolitan area, Rio de Janeiro is the capital of the state of Rio de Janeiro, Brazils third-most populous state. Part of the city has designated as a World Heritage Site, named Rio de Janeiro. Founded in 1565 by the Portuguese, the city was initially the seat of the Captaincy of Rio de Janeiro, later, in 1763, it became the capital of the State of Brazil, a state of the Portuguese Empire. Rio stayed the capital of the pluricontinental Lusitanian monarchy until 1822 and this is one of the few instances in history that the capital of a colonising country officially shifted to a city in one of its colonies. Rio de Janeiro has the second largest municipal GDP in the country, 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 output according to 2005 data. The Maracanã Stadium held the finals of the 1950 and 2014 FIFA World Cups, the 2013 FIFA Confederations Cup, the city is divided into 33 administrative regions. Europeans first encountered Guanabara Bay on 1 January 1502, by a Portuguese expedition under explorer Gaspar de Lemos captain of a ship in Pedro Álvares Cabrals fleet, allegedly the Florentine explorer Amerigo Vespucci participated as observer at the invitation of King Manuel I in the same expedition. The region of Rio was inhabited by the Tupi, Puri, Botocudo, in 1555, one of the islands of Guanabara Bay, now called Villegagnon Island, was occupied by 500 French colonists under the French admiral Nicolas Durand de Villegaignon. Consequently, Villegagnon built Fort Coligny on the island when attempting to establish the France Antarctique colony, Rio de Janeiro was the name of Guanabara Bay. Until early in the 18th century, the city was threatened or invaded by several, mostly French, pirates and buccaneers, such as Jean-François Duclerc, on 27 January 1763, the colonial administration in Portuguese America was moved from Salvador to Rio de Janeiro. The kingdoms capital was transferred to the city, which, thus, as there was no physical space or urban structure to accommodate hundreds of noblemen who arrived suddenly, many inhabitants were simply evicted from their homes. The first printed newspaper in Brazil, the Gazeta do Rio de Janeiro, from the colonial period until the first independent decades, Rio de Janeiro was a city of slaves. There was an influx of African slaves to Rio de Janeiro, in 1819. In 1840, the number of slaves reached 220,000 people, the Port of Rio de Janeiro was the largest port of slaves in America. As a political center of the country, Rio concentrated the political-partisan life of the Empire and it was the main stage of the abolitionist and republican movements in the last half of the 19th century. Rio continued as the capital of Brazil after 1889, when the monarchy was replaced by a republic, until the early years of the 20th century, the city was largely limited to the neighbourhood now known as the historic city centre, on the mouth of Guanabara Bay. Expansion of the city to the north and south was facilitated by the consolidation and electrification of Rios streetcar transit system after 1905, though many thought that it was just campaign rhetoric, Kubitschek managed to have Brasília built, at great cost, by 1960
12.
Brazil
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Brazil, officially the Federative Republic of Brazil, is the largest country in both South America and Latin America. As the worlds fifth-largest country by area and population, it is the largest country to have Portuguese as an official language. Its Amazon River basin includes a vast tropical forest, home to wildlife, a variety of ecological systems. This unique environmental heritage makes Brazil one of 17 megadiverse countries, Brazil was inhabited by numerous tribal nations prior to the landing in 1500 of explorer Pedro Álvares Cabral, who claimed the area for the Portuguese Empire. Brazil remained a Portuguese colony until 1808, when the capital of the empire was transferred from Lisbon to Rio de Janeiro, in 1815, the colony was elevated to the rank of kingdom upon the formation of the United Kingdom of Portugal, Brazil and the Algarves. Independence was achieved in 1822 with the creation of the Empire of Brazil, a state governed under a constitutional monarchy. The ratification of the first constitution in 1824 led to the formation of a bicameral legislature, the country became a presidential republic in 1889 following a military coup détat. An authoritarian military junta came to power in 1964 and ruled until 1985, Brazils current constitution, formulated in 1988, defines it as a democratic federal republic. The federation is composed of the union of the Federal District, the 26 states, Brazils economy is the worlds ninth-largest by nominal GDP and seventh-largest by GDP as of 2015. A member of the BRICS group, Brazil until 2010 had one of the worlds fastest growing economies, with its economic reforms giving the country new international recognition. Brazils national development bank plays an important role for the economic growth. Brazil is a member of the United Nations, the G20, BRICS, Unasul, Mercosul, Organization of American States, Organization of Ibero-American States, CPLP. Brazil is a power in Latin America and a middle power in international affairs. One of the worlds major breadbaskets, Brazil has been the largest producer of coffee for the last 150 years and it is likely that the word Brazil comes from the Portuguese word for brazilwood, a tree that once grew plentifully along the Brazilian coast. In Portuguese, brazilwood is called pau-brasil, with the word brasil commonly given the etymology red like an ember, formed from Latin brasa and the suffix -il. As brazilwood produces a red dye, it was highly valued by the European cloth industry and was the earliest commercially exploited product from Brazil. The popular appellation eclipsed and eventually supplanted the official Portuguese name, early sailors sometimes also called it the Land of Parrots. In the Guarani language, a language of Paraguay, Brazil is called Pindorama
13.
Rock (geology)
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Rock or stone is a natural substance, a solid aggregate of one or more minerals or mineraloids. For example, granite, a rock, is a combination of the minerals quartz, feldspar. The Earths outer solid layer, the lithosphere, is made of rock, rock has been used by mankind throughout history. The minerals and metals found in rocks have been essential to human civilization, three major groups of rocks are defined, igneous, sedimentary, and metamorphic. The scientific study of rocks is called petrology, which is a component of geology. At a granular level, rocks are composed of grains of minerals, the aggregate minerals forming the rock are held together by chemical bonds. The types and abundance of minerals in a rock are determined by the manner in which the rock was formed, many rocks contain silica, a compound of silicon and oxygen that forms 74. 3% of the Earths crust. This material forms crystals with other compounds in the rock, the proportion of silica in rocks and minerals is a major factor in determining their name and properties. Rocks are geologically classified according to such as mineral and chemical composition, permeability, the texture of the constituent particles. These physical properties are the end result of the processes that formed the rocks, over the course of time, rocks can transform from one type into another, as described by the geological model called the rock cycle. These events produce three general classes of rock, igneous, sedimentary, and metamorphic, the three classes of rocks are subdivided into many groups. However, there are no hard and fast boundaries between allied rocks, hence the definitions adopted in establishing rock nomenclature merely correspond to more or less arbitrary selected points in a continuously graduated series. Igneous rock forms through the cooling and solidification of magma or lava and this magma can be derived from partial melts of pre-existing rocks in either a planets mantle or crust. Typically, the melting of rocks is caused by one or more of three processes, an increase in temperature, a decrease in pressure, or a change in composition, igneous rocks are divided into two main categories, plutonic rock and volcanic. Plutonic or intrusive rocks result when magma cools and crystallizes slowly within the Earths crust, a common example of this type is granite. Volcanic or extrusive rocks result from magma reaching the surface either as lava or fragmental ejecta, the chemical abundance and the rate of cooling of magma typically forms a sequence known as Bowens reaction series. Most major igneous rocks are found along this scale, about 64. 7% of the Earths crust by volume consists of igneous rocks, making it the most plentiful category. Of these, 66% are basalts and gabbros, 16% are granite, only 0. 6% are syenites and 0. 3% peridotites and dunites
14.
Mountain
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A mountain is a large landform that stretches above the surrounding land in a limited area, usually in the form of a peak. A mountain is steeper than a hill. Mountains are formed through tectonic forces or volcanism and these forces can locally raise the surface of the earth. Mountains erode slowly through the action of rivers, weather conditions, a few mountains are isolated summits, but most occur in huge mountain ranges. High elevations on mountains produce colder climates than at sea level and these colder climates strongly affect the ecosystems of mountains, different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains tend to be used less for agriculture and more for resource extraction and recreation, the highest mountain on Earth is Mount Everest in the Himalayas of Asia, whose summit is 8,850 m above mean sea level. The highest known mountain on any planet in the Solar System is Olympus Mons on Mars at 21,171 m, there is no universally accepted definition of a mountain. Elevation, volume, relief, steepness, spacing and continuity have been used as criteria for defining a mountain, whether a landform is called a mountain may depend on local usage. The highest point in San Francisco, California, is called Mount Davidson, notwithstanding its height of 300 m, similarly, Mount Scott outside Lawton, Oklahoma is only 251 m from its base to its highest point. Whittows Dictionary of Physical Geography states Some authorities regard eminences above 600 metres as mountains, in addition, some definitions also include a topographical prominence requirement, typically 100 or 500 feet. For a while, the US defined a mountain as being 1,000 feet or taller, any similar landform lower than this height was considered a hill. However, today, the United States Geological Survey concludes that these terms do not have technical definitions in the US, using these definitions, mountains cover 33% of Eurasia, 19% of South America, 24% of North America, and 14% of Africa. As a whole, 24% of the Earths land mass is mountainous, there are three main types of mountains, volcanic, fold, and block. All three types are formed from plate tectonics, when portions of the Earths crust move, crumple, compressional forces, isostatic uplift and intrusion of igneous matter forces surface rock upward, creating a landform higher than the surrounding features. The height of the feature makes it either a hill or, if higher and steeper, major mountains tend to occur in long linear arcs, indicating tectonic plate boundaries and activity. Volcanoes are formed when a plate is pushed below another plate, at a depth of around 100 km, melting occurs in rock above the slab, and forms magma that reaches the surface. When the magma reaches the surface, it builds a volcanic mountain. Examples of volcanoes include Mount Fuji in Japan and Mount Pinatubo in the Philippines, the magma does not have to reach the surface in order to create a mountain, magma that solidifies below ground can still form dome mountains, such as Navajo Mountain in the US
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Erosion
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In earth science, erosion is the action of surface processes that remove soil, rock, or dissolved material from one location on the Earths crust, then transport it away to another location. Eroded sediment or solutes may be transported just a few millimetres, the rates at which such processes act control how fast a surface is eroded. Feedbacks are also possible between rates of erosion and the amount of eroded material that is carried by, for example. Processes of erosion that produce sediment or solutes from a place contrast with those of deposition, while erosion is a natural process, human activities have increased by 10-40 times the rate at which erosion is occurring globally. At well-known agriculture sites such as the Appalachian Mountains, intensive farming practices have caused erosion up to 100x the speed of the rate of erosion in the region. Excessive erosion causes both on-site and off-site problems, on-site impacts include decreases in agricultural productivity and ecological collapse, both because of loss of the nutrient-rich upper soil layers. In some cases, the end result is desertification. Off-site effects include sedimentation of waterways and eutrophication of bodies, as well as sediment-related damage to roads. Intensive agriculture, deforestation, roads, anthropogenic climate change and urban sprawl are amongst the most significant human activities in regard to their effect on stimulating erosion, however, there are many prevention and remediation practices that can curtail or limit erosion of vulnerable soils. Rainfall, and the surface runoff which may result from rainfall, produces four types of soil erosion, splash erosion, sheet erosion, rill erosion. Splash erosion is generally seen as the first and least severe stage in the erosion process. In splash erosion, the impact of a falling raindrop creates a crater in the soil. The distance these soil particles travel can be as much as 0.6 m vertically and 1.5 m horizontally on level ground. If the soil is saturated, or if the rate is greater than the rate at which water can infiltrate into the soil. If the runoff has sufficient flow energy, it will transport loosened soil particles down the slope, sheet erosion is the transport of loosened soil particles by overland flow. Rill erosion refers to the development of small, ephemeral concentrated flow paths which function as both sediment source and sediment delivery systems for erosion on hillslopes, generally, where water erosion rates on disturbed upland areas are greatest, rills are active. Flow depths in rills are typically of the order of a few centimetres or less and this means that rills exhibit hydraulic physics very different from water flowing through the deeper, wider channels of streams and rivers. Gully erosion occurs when water accumulates and rapidly flows in narrow channels during or immediately after heavy rains or melting snow
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Igneous rock
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Igneous rock, or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava, the magma can be derived from partial melts of existing rocks in either a planets mantle or crust. Typically, the melting is caused by one or more of three processes, an increase in temperature, a decrease in pressure, or a change in composition, solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, Igneous and metamorphic rocks make up 90–95% of the top 16 km of the Earths crust by volume. Igneous rocks form about 15% of the Earths current land surface, most of the Earths oceanic crust is made of igneous rock. In terms of modes of occurrence, igneous rocks can be either intrusive or extrusive, the mineral grains in such rocks can generally be identified with the naked eye. Intrusive rocks can also be classified according to the shape and size of the intrusive body, typical intrusive formations are batholiths, stocks, laccoliths, sills and dikes. When the magma solidifies within the earths crust, it cools slowly forming coarse textured rocks, such as granite, gabbro, the central cores of major mountain ranges consist of intrusive igneous rocks, usually granite. When exposed by erosion, these cores may occupy huge areas of the Earths surface, intrusive igneous rocks that form at depth within the crust are termed plutonic rocks and are usually coarse-grained. Intrusive igneous rocks that form near the surface are termed subvolcanic or hypabyssal rocks, hypabyssal rocks are less common than plutonic or volcanic rocks and often form dikes, sills, laccoliths, lopoliths, or phacoliths. Extrusive igneous rocks, also known as rocks, are formed at the crusts surface as a result of the partial melting of rocks within the mantle. Extrusive igneous rocks cool and solidify quicker than intrusive igneous rocks and they are formed by the cooling of molten magma on the earths surface. The magma, which is brought to the surface through fissures or volcanic eruptions, hence such rocks are smooth, crystalline and fine-grained. Basalt is an extrusive igneous rock and forms lava flows, lava sheets. Some kinds of basalt solidify to form long polygonal columns, the Giants Causeway in Antrim, Northern Ireland is an example. The molten rock, with or without suspended crystals and gas bubbles, is called magma and it rises because it is less dense than the rock from which it was created. When magma reaches the surface from beneath water or air, it is called lava, eruptions of volcanoes into air are termed subaerial, whereas those occurring underneath the ocean are termed submarine. Black smokers and mid-ocean ridge basalt are examples of volcanic activity
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Metamorphic rock
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Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means change in form. The original rock is subjected to heat and pressure, causing profound physical and/or chemical change, the protolith may be a sedimentary, an igneous, or even an existing type of metamorphic rock. Metamorphic rocks make up a part of the Earths crust. They are classified by texture and by chemical and mineral assemblage and they may be formed simply by being deep beneath the Earths surface, subjected to high temperatures and the great pressure of the rock layers above it. They can form from tectonic processes such as continental collisions, which cause horizontal pressure and they are also formed when rock is heated up by the intrusion of hot molten rock called magma from the Earths interior. The study of rocks provides information about the temperatures and pressures that occur at great depths within the Earths crust. Some examples of rocks are gneiss, slate, marble, schist. Metamorphic minerals are those that only at the high temperatures and pressures associated with the process of metamorphism. These minerals, known as index minerals, include sillimanite, kyanite, staurolite, andalusite, and some garnet. Other minerals, such as olivines, pyroxenes, amphiboles, micas, feldspars, and quartz, may be found in metamorphic rocks and these minerals formed during the crystallization of igneous rocks. They are stable at temperatures and pressures and may remain chemically unchanged during the metamorphic process. However, all minerals are only within certain limits. The change in the size of the rock during the process of metamorphism is called recrystallization. Both high temperatures and pressures contribute to recrystallization, high temperatures allow the atoms and ions in solid crystals to migrate, thus reorganizing the crystals, while high pressures cause solution of the crystals within the rock at their point of contact. The layering within metamorphic rocks is called foliation, and it occurs when a rock is being shortened along one axis during recrystallization. This causes the platy or elongated crystals of minerals, such as mica and chlorite and this results in a banded, or foliated rock, with the bands showing the colors of the minerals that formed them. Textures are separated into foliated and non-foliated categories, foliated rock is a product of differential stress that deforms the rock in one plane, sometimes creating a plane of cleavage. For example, slate is a metamorphic rock, originating from shale
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Megalith
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A megalith is a large stone that has been used to construct a structure or monument, either alone or together with other stones. The word megalithic describes structures made of large stones without the use of mortar or concrete. For later periods, the monolith, with an overlapping meaning, is more likely to be used. The word megalith comes from the Ancient Greek μέγας and λίθος, megalith also denotes an item consisting of rock hewn in definite shapes for special purposes. It has been used to describe buildings built by people from parts of the world living in many different periods. A variety of stones are seen as megaliths, with the most widely known megaliths not being sepulchral. The construction of these took place mainly in the Neolithic and continued into the Chalcolithic. At a number of sites in eastern Turkey, large ceremonial complexes from the 9th millennium BC have been discovered and they belong to the incipient phases of agriculture and animal husbandry. Large circular structures involving carved megalithic orthostats are a feature, e. g. at Nevalı Çori. Although these structures are the most ancient megalithic structures known so far, at Göbekli Tepe, four stone circles have been excavated from an estimated 20. Some measure up to 30 metres across, as well as human figures, the stones carry a variety of carved reliefs depicting boars, foxes, lions, birds, snakes and scorpions. Dolmens and standing stones have been found in areas of the Middle East starting at the Turkish border in the north of Syria close to Aleppo. They can be encountered in Lebanon, Syria, Iran, Israel, Jordan, the largest concentration can be found in southern Syria and along the Jordan Rift Valley, however they are being threatened with destruction. They date from the late Chalcolithic/Early Bronze Age, megaliths have also been found on Kharg Island and pirazmian in Iran, at Barda Balka in Iraq, and at Jaintapur in Bangladesh. A semicircular arrangement of megaliths was found in Israel at Atlit Yam and it is a very early example, dating from the 7th millennium BC. The most concentrated occurrence of dolmens in particular is in an area on both sides of the Jordan Rift Valley, with greater predominance on the eastern side. They occur first and foremost on the Golan Heights, the Hauran, and in Jordan, in Saudi Arabia, only very few dolmen have been identified so far in the Hejaz. They seem, however, to re-emerge in Yemen in small numbers, the standing stone has a very ancient tradition in the Middle East, dating back from Mesopotamian times
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Prehistory
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Prehistory means literally before history, from the Latin word for before, præ, and Greek ιστορία. Neighbouring civilisations were the first to follow, most other civilisations reached the end of prehistory during the Iron Age. The period when a culture is written about by others, but has not developed its own writing is known as the protohistory of the culture. By definition, there are no records from human prehistory. Clear techniques for dating were not well-developed until the 19th century and this article is concerned with human prehistory as defined here above. There are separate articles for the history of the Earth. However, for the race as a whole, prehistory ends when recorded history begins with the accounts of the ancient world around the 4th millennium BC. For example, in Egypt it is accepted that prehistory ended around 3200 BC, whereas in New Guinea the end of the prehistoric era is set much more recently. The three-age system is the periodization of prehistory into three consecutive time periods, named for their respective predominant tool-making technologies, Stone Age Bronze Age Iron Age. The notion of prehistory began to surface during the Enlightenment in the work of antiquarians who used the word primitive to describe societies that existed before written records, the first use of the word prehistory in English, however, occurred in the Foreign Quarterly Review in 1836. The main source for prehistory is archaeology, but some scholars are beginning to more use of evidence from the natural and social sciences. This view has been articulated by advocates of deep history, human population geneticists and historical linguists are also providing valuable insight for these questions. Human prehistory differs from history not only in terms of its chronology, restricted to material processes, remains and artifacts rather than written records, prehistory is anonymous. Because of this, reference terms that use, such as Neanderthal or Iron Age are modern labels with definitions sometimes subject to debate. Palaeolithic means Old Stone Age, and begins with the first use of stone tools, the Paleolithic is the earliest period of the Stone Age. The early part of the Palaeolithic is called the Lower Palaeolithic, evidence of control of fire by early humans during the Lower Palaeolithic Era is uncertain and has at best limited scholarly support. The most widely accepted claim is that H. erectus or H. ergaster made fires between 790,000 and 690,000 BP in a site at Bnot Yaakov Bridge, Israel. The use of fire enabled early humans to cook food, provide warmth, Early Homo sapiens originated some 200,000 years ago, ushering in the Middle Palaeolithic
20.
Rock-cut architecture
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Rock-cut architecture is the creation of structures, buildings, and sculptures, by excavating solid rock where it naturally occurs. Rock-cut architecture is designed and made by man from the start to finish, in India and China, the terms cave and cavern are often applied to this form of man-made architecture. However, caves and caverns, that began in natural form, are not considered to be rock-cut architecture even if extensively modified, although rock-cut structures differ from traditionally built structures in many ways, many rock-cut structures are made to replicate the facade or interior of traditional architectural forms. Interiors were usually carved out by starting at the roof of the planned space and this technique prevents stones falling on workers below. The three main uses of rock-cut architecture were temples, tombs and cave dwellings, some rock-cut architecture, mostly for tombs, is excavated entirely in chambers under the surface of relatively level rock. If the excavation is made into the side of a cliff or steep slope, there can be an impressive facade, as found in Lycian tombs, Petra, Ajanta. Ellora in India and Lalibela in Ethiopia provide the most spectacular, rock-cut architecture is also said to be cut, hewn, etc. from the living rock. Another term sometimes associated with architecture is monolithic architecture, which is rather applied to free-standing structures made of a single piece of material. Monolithic architecture is often rock-cut architecture but monolithic structures might be also cast of artificial material, gomateshwara, the largest monolithic statue in the world is situated at Shravanabelagola, Karnataka, India. It was built in 983 A. D and was carved out from a single block of granite. In many parts of the world there are rock reliefs, relief sculptures carved into rock faces. Ancient monuments of architecture are widespread in several regions of world. It dates from about 1280 BCE, and consists of a monumentally scaled facade carved out of the cliff, in the 5th century BCE, the Lycians, who inhabited southern Anatolia built hundreds of rock-cut tombs of a similar type, but smaller in scale. Excellent examples are to be found near Dalyan, a town in Muğla Province, since these served as tombs rather than as religious sites, the interiors were usually small and unassuming. The ancient Etruscans of central Italy also left an important legacy of architecture, mostly tombs, as those near the cities of Tarquinia. The creation of rock-cut tombs in ancient Israel began in the 8th-century BCE, the Nabataeans in their city of Petra, now in Jordan, extended this tradition, carving their temples and tombs into the yellowish-orange rock that defines the canyons and gullies of the region. These structures, dating from 1st century BCE to about 2nd century CE, are important in the history of architecture given their experimental forms. Here too, because the structures served as tombs, the interiors were rather perfunctory, in Petra one even finds a theater where the seats are cut out of the rock
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Monolithic church
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A monolithic church or rock-hewn church is a church made from a single block of stone. Because freestanding rocks of sufficient size are rare, such churches are usually hewn into the ground or into the side of a hill or mountain and they can be of comparable architectural complexity to constructed buildings. The term monolithic church is most often used to refer to the complex of 11 churches in Lalibela, Ethiopia, the most famous of the edifices is the cross-shaped Church of St. George. Tradition credits its construction to King Lalibela, who was a devout Christian, the medieval monolithic churches of this 12th-century New Jerusalem are situated in a mountainous region in the heart of Ethiopia near a traditional village. Lalibela is an important center of Ethiopian Christianity, and even today is a place of pilgrimage, Lalibela is one of the worlds precious heritages registered by UNESCO. Many other churches were hewn from rock in Ethiopia, outside of Lalibela, despite Dr. Josiefs death soon after his presentation, research over the next few years raised the total number of these rock-hewn churches to 153. There are a number of monolithic churches elsewhere in the world, however, none have the free-standing external walls of the Lalibela churches. They instead more closely resemble cave monasteries in that they consist of tunnels converging into a single rock, examples include, The Geghard monastery, Armenia The Rock-hewn Churches of Ivanovo, Bulgaria near Ruse The subterranean St
22.
Obelisk
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An obelisk is a tall, four-sided, narrow tapering monument which ends in a pyramid-like shape or pyramidion at the top. These were originally called tekhenu by their builders, the Ancient Egyptians, the Greeks who saw them used the Greek obeliskos to describe them, and this word passed into Latin and ultimately English. Ancient obelisks are monolithic, that is, they consist of a single stone, though this technological capacity exists today, most modern obelisks are made of several stones, some, like the Washington Monument, are buildings. The term stele is used for other monumental, upright. Obelisks were prominent in the architecture of the ancient Egyptians, who placed them in pairs at the entrance of temples. The word obelisk as used in English today is of Greek rather than Egyptian origin because Herodotus, a number of ancient Egyptian obelisks are known to have survived, plus the Unfinished Obelisk found partly hewn from its quarry at Aswan. These obelisks are now dispersed around the world, and fewer than half of them remain in Egypt, the earliest temple obelisk still in its original position is the 68-foot 120-metric-ton red granite Obelisk of Senusret I of the XIIth Dynasty at Al-Matariyyah in modern Heliopolis. The obelisk symbolized the sun god Ra, and during the religious reformation of Akhenaten was said to be a petrified ray of the Aten. It was also thought that the god existed within the structure, Benben was the mound that arose from the primordial waters Nu upon which the creator god Atum settled in the creation story of the Heliopolitan creation myth form of Ancient Egyptian religion. The Benben stone is the top stone of the Egyptian pyramid and it is also related to the Obelisk. The pyramid and obelisk might have inspired by previously overlooked astronomical phenomena connected with sunrise and sunset. The Ancient Romans were strongly influenced by the form, to the extent that there are now more than twice as many obelisks standing in Rome as remain in Egypt. All fell after the Roman period except for the Vatican obelisk and were re-erected in different locations. The largest standing and tallest Egyptian obelisk is the Lateran Obelisk in the square at the west side of the Lateran Basilica in Rome at 105.6 feet tall, not all the Egyptian obelisks in the Roman Empire were set up at Rome. Herod the Great imitated his Roman patrons and set up a red granite Egyptian obelisk in the hippodrome of his new city Caesarea in northern Judea and this one is about 40 feet tall and weighs about 100 metric tons. It was discovered by archaeologists and has been re-erected at its former site and this one stood 95 feet tall and weighing 380 metric tons. Its lower half reputedly also once stood in Istanbul but is now lost, the Istanbul obelisk is 65 feet tall. Rome is the capital of the world
23.
Architrave
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An architrave is the lintel or beam that rests on the capitals of the columns. It is an element in Classical architecture. The term can also be applied to all sides, including the vertical members, in an entablature in classical architecture, it is the lowest part, below the frieze and cornice. The word is derived from the Greek and Latin words arche, the architrave is different in the different orders. In the Tuscan, it consists of a plain face, crowned with a fillet. In the Doric and composite, it has two faces, or fasciae, and three in the Ionic and Corinthian, in which it is 10/12 of a high, though. It means the part of something. The part on which the idea, the reasoning, the thought or the philosophy are based, examples, 1). the Mature Hegel- the Hegel of the Philosophy of Right- who becomes the architrave on which he constructs his social philosophy. Ref. Page, XIV, The Ethics of Democracy, A Contemporary Reading of Hegels Philosophy of Right LINK 2) to become the architrave of his theoretic construction Ref. Pag and it is placed above the bracket of a pillar, which gives it extra support. Dravidian architecture recognizes several distinct types of Architraves, rounded, wavy, flower shaped, bevel and tenon type, voluted, figural
24.
Glacial erratic
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A glacial erratic is a piece of rock that differs from the size and type of rock native to the area in which it rests. Erratics take their name from the Latin word errare, and are carried by glacial ice, Erratics can range in size from pebbles to large boulders such as Big Rock in Alberta. Geologists identify erratics by studying the surrounding the position of the erratic. Erratics are significant because, They can be transported by glaciers and their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. They can be transported by ice rafting and this allows quantification of the extent of glacial flooding resulting from ice dam failure which release the waters stored in proglacial lakes such as Lake Missoula. Erratics released by ice-rafts that were stranded and subsequently melt, dropping their load, Erratics dropped by icebergs melting in the ocean can be used to track Antarctic and Arctic-region glacial movements for periods prior to record retention. Also known as dropstones, these can be correlated with ocean temperatures and levels to better understand, and examination of their mineralogical character leads the identification of their sources…. In geology, an erratic is material moved by forces from one location to another. Erratics are formed by ice erosion resulting from the movement of ice. Glaciers erode by multiple processes, abrasion/scouring, plucking, ice thrusting, glaciers crack pieces of bedrock off in the process of plucking, producing the larger erratics. In an abrasion process, debris in the basal ice scrapes along the bed, polishing and gouging the underlying rocks, similar to sandpaper on wood, producing smaller glacial till. In ice thrusting, the glacier freezes to its bed, then as it surges forward, evidence supports another option for creation of erratics as well, rock avalanches onto the upper surface of the glacier. Rock avalanche–supraglacial transport occurs when the glacier undercuts a rock face, the characteristics of rock avalanche–supraglacial transport includes, Monolithologic composition - a cluster of boulders of similar composition are frequently found in close proximity. Commingling of the multiple lithologies normally present throughout the basin, has not occurred. Angularity - the supraglacially transported rocks tend to be rough and irregular, the sides of boulders are roughly planar, suggesting that some surfaces may be original fracture planes. Great size - the size distribution of the boulders tends to be skewed toward larger boulders than those produced subglacially, surficial positioning of the boulders - the boulders are positioned on the surface of glacial deposits, as opposed to partially or totally buried. Orientations - the boulders may be enough that original fracture planes can be matched. Locations of the boulder trains - the boulders appear in rows, Erratic materials may be transported by multiple glacier flows prior to their deposition, which can complicate the reconstruction of the glacial flow
25.
Latin
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Latin is a classical language belonging to the Italic branch of the Indo-European languages. The Latin alphabet is derived from the Etruscan and Greek alphabets, Latin was originally spoken in Latium, in the Italian Peninsula. Through the power of the Roman Republic, it became the dominant language, Vulgar Latin developed into the Romance languages, such as Italian, Portuguese, Spanish, French, and Romanian. Latin, Italian and French have contributed many words to the English language, Latin and Ancient Greek roots are used in theology, biology, and medicine. By the late Roman Republic, Old Latin had been standardised into Classical Latin, Vulgar Latin was the colloquial form spoken during the same time and attested in inscriptions and the works of comic playwrights like Plautus and Terence. Late Latin is the language from the 3rd century. Later, Early Modern Latin and Modern Latin evolved, Latin was used as the language of international communication, scholarship, and science until well into the 18th century, when it began to be supplanted by vernaculars. Ecclesiastical Latin remains the language of the Holy See and the Roman Rite of the Catholic Church. Today, many students, scholars and members of the Catholic clergy speak Latin fluently and it is taught in primary, secondary and postsecondary educational institutions around the world. The language has been passed down through various forms, some inscriptions have been published in an internationally agreed, monumental, multivolume series, the Corpus Inscriptionum Latinarum. Authors and publishers vary, but the format is about the same, volumes detailing inscriptions with a critical apparatus stating the provenance, the reading and interpretation of these inscriptions is the subject matter of the field of epigraphy. The works of several hundred ancient authors who wrote in Latin have survived in whole or in part and they are in part the subject matter of the field of classics. The Cat in the Hat, and a book of fairy tales, additional resources include phrasebooks and resources for rendering everyday phrases and concepts into Latin, such as Meissners Latin Phrasebook. The Latin influence in English has been significant at all stages of its insular development. From the 16th to the 18th centuries, English writers cobbled together huge numbers of new words from Latin and Greek words, dubbed inkhorn terms, as if they had spilled from a pot of ink. Many of these words were used once by the author and then forgotten, many of the most common polysyllabic English words are of Latin origin through the medium of Old French. Romance words make respectively 59%, 20% and 14% of English, German and those figures can rise dramatically when only non-compound and non-derived words are included. Accordingly, Romance words make roughly 35% of the vocabulary of Dutch, Roman engineering had the same effect on scientific terminology as a whole
26.
Ancient Greek
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Ancient Greek includes the forms of Greek used in ancient Greece and the ancient world from around the 9th century BC to the 6th century AD. It is often divided into the Archaic period, Classical period. It is antedated in the second millennium BC by Mycenaean Greek, the language of the Hellenistic phase is known as Koine. Koine is regarded as a historical stage of its own, although in its earliest form it closely resembled Attic Greek. Prior to the Koine period, Greek of the classic and earlier periods included several regional dialects, Ancient Greek was the language of Homer and of fifth-century Athenian historians, playwrights, and philosophers. It has contributed many words to English vocabulary and has been a subject of study in educational institutions of the Western world since the Renaissance. This article primarily contains information about the Epic and Classical phases of the language, Ancient Greek was a pluricentric language, divided into many dialects. The main dialect groups are Attic and Ionic, Aeolic, Arcadocypriot, some dialects are found in standardized literary forms used in literature, while others are attested only in inscriptions. There are also several historical forms, homeric Greek is a literary form of Archaic Greek used in the epic poems, the Iliad and Odyssey, and in later poems by other authors. Homeric Greek had significant differences in grammar and pronunciation from Classical Attic, the origins, early form and development of the Hellenic language family are not well understood because of a lack of contemporaneous evidence. Several theories exist about what Hellenic dialect groups may have existed between the divergence of early Greek-like speech from the common Proto-Indo-European language and the Classical period and they have the same general outline, but differ in some of the detail. The invasion would not be Dorian unless the invaders had some relationship to the historical Dorians. The invasion is known to have displaced population to the later Attic-Ionic regions, the Greeks of this period believed there were three major divisions of all Greek people—Dorians, Aeolians, and Ionians, each with their own defining and distinctive dialects. Often non-west is called East Greek, Arcadocypriot apparently descended more closely from the Mycenaean Greek of the Bronze Age. Boeotian had come under a strong Northwest Greek influence, and can in some respects be considered a transitional dialect, thessalian likewise had come under Northwest Greek influence, though to a lesser degree. Most of the dialect sub-groups listed above had further subdivisions, generally equivalent to a city-state and its surrounding territory, Doric notably had several intermediate divisions as well, into Island Doric, Southern Peloponnesus Doric, and Northern Peloponnesus Doric. The Lesbian dialect was Aeolic Greek and this dialect slowly replaced most of the older dialects, although Doric dialect has survived in the Tsakonian language, which is spoken in the region of modern Sparta. Doric has also passed down its aorist terminations into most verbs of Demotic Greek, by about the 6th century AD, the Koine had slowly metamorphosized into Medieval Greek
27.
Aso Rock
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Aso Rock is a large outcrop that is on the outskirts of Abuja, the capital of Nigeria. The Aso Rock is a 400-metre monolith and is the citys most noticeable feature, the Nigerian Presidential Complex, Nigerian National Assembly, and Nigerian Supreme Court are located around it. Much of the town extends to the south of the rock, Aso means victorious in the native language of the Asokoro. Aso Rock was the site of the 2003 Aso Rock Declaration and it reaffirmed the Commonwealths principles as detailed under the Harare Declaration, but set the promotion of democracy and development as the organisations priorities
28.
Sibebe
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Sibebe is a granite mountain in Swaziland, located 10 km from the capital city Mbabane. It is the second-largest monolith in the world and the largest exposed granite pluton and it is also known as Bald Rock. The Mbabane-Mbuluzi Rotary Club organises an annual fund-raising walk up Sibebe Rock, several thousand people take part each year. Sibebe also gives its name to a lager produced by Swaziland Beverages, called Sibebe Premium Lager
29.
Zuma Rock
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Zuma Rock is a large monolith, an igneous intrusion composed of gabbro and granodiorite that is located in Niger State, Nigeria. It rises spectacularly immediately north of Nigerias capital Abuja, along the road from Abuja to Kaduna off Madala. Zuma Rock rises 725 metres above its surroundings, zuma is depicted on the 100 naira note. It was used for a retreat by the Gbagyi people against invading neighbouring tribes during intertribal warring
30.
Great Sphinx of Giza
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Facing directly from West to East, it stands on the Giza Plateau on the west bank of the Nile in Giza, Egypt. The face of the Sphinx is generally believed to represent the Pharaoh Khafre, cut from the bedrock, the original shape of the Sphinx has been restored with layers of blocks. It measures 238 feet long from paw to tail,66.3 ft high from the base to the top of the head and 62.6 feet wide at its rear haunches. It is the oldest known sculpture in Egypt and is commonly believed to have been built by ancient Egyptians of the Old Kingdom during the reign of the Pharaoh Khafre. The Sphinx is a monolith carved into the bedrock of the plateau, the nummulitic limestone of the area consists of layers which offer differing resistance to erosion, leading to the uneven degradation apparent in the Sphinxs body. The lowest part of the body, including the legs, is solid rock, the body of the lion up to its neck is fashioned from softer layers that have suffered considerable disintegration. The layer in which the head was sculpted is much harder, the Great Sphinx is one of the worlds largest and oldest statues, but basic facts about it are still subject to debate, such as when it was built, by whom and for what purpose. These questions have resulted in the idea of the Riddle of the Sphinx. In the New Kingdom, the Sphinx was called Hor-em-akhet, the English word sphinx comes from the ancient Greek Σφίγξ apparently from the verb σφίγγω, after the Greek sphinx who strangled anyone who failed to answer her riddle. The name may alternatively be a corruption of the phonetically different ancient Egyptian word Ssp-anx. This name is given to royal statues of the Fourth dynasty of ancient Egypt, medieval Arab writers, including al-Maqrīzī, call the Sphinx balhib and bilhaw, which suggest a Coptic influence. The modern Egyptian Arabic name is أبو الهول, the circumstantial evidence mentioned by Hassan includes the Sphinxs location in the context of the funerary complex surrounding the Second Pyramid, which is traditionally connected with Khafra. A diorite statue of Khafre, which was discovered buried upside down along with other debris in the Valley Temple, is claimed as support for the Khafra theory, the Dream Stele, erected much later by the pharaoh Thutmose IV, associates the Sphinx with Khafra. When the stele was discovered, its lines of text were already damaged and incomplete, an extract was translated, which we bring for him, oxen. and all the young vegetables, and we shall give praise to Wenofer. Khaf. the statue made for Atum-Hor-em-Akhet, the Egyptologist Thomas Young, finding the Khaf hieroglyphs in a damaged cartouche used to surround a royal name, inserted the glyph ra to complete Khafras name. When the Stele was re-excavated in 1925, the lines of text referring to Khaf flaked off and were destroyed. In 1857, Auguste Mariette, founder of the Egyptian Museum in Cairo, unearthed the much later Inventory Stela, such an act became common when religious institutions such as temples, shrines and priests domains were fighting for political attention and for financial and economic donations. Gaston Maspero, the French Egyptologist and second director of the Egyptian Museum in Cairo and he supports this by suggesting that Khafras Causeway was built to conform to a pre-existing structure, which, he concludes, given its location, could only have been the Sphinx
31.
Savandurga
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Savandurga is a hill 60 km west of Bangalore off the Magadi road 12. 919654°N77. 292881°E /12.919654,77.292881, in India. The hill is considered to be among the largest monolith hills in Asia, the hill rises to 1226 m above mean sea level and forms a part of the Deccan plateau. It consists of gneiss, granites, basic dykes and laterites. The Arkavathi river passes nearby through the Thippagondanahalli reservoir and on towards Manchanabele dam, Savandurga is formed by two hills known locally as Karigudda and Biligudda. The earliest record of the name of the hill is from 1340 AD by Hoysala Ballala III from Madabalu where it is called Savandi. Another view is that the name is originated from Samantadurga attributed to a Samantharaya and this was the secondary capital of the Magadi rulers such as Kempegowda. From 1638 to 1728, Mysore took over place and Dalavayi Devaraja occupied this place with the palace at Nelapattana. In 1791 Lord Cornwallis captured it from Tipu Sultans forces during the Third Anglo-Mysore War, robert Home in his Select views in Mysore shows distant views of the hill from Bangalore. He called it Savinadurga or the fort of death, there were no steps to reach the hill top and it was covered by bamboos and other trees forming a barricade. Megalithic burial urns have been found in the area, saavana in Sanskrit also means three time rituals. The main deity of the place is Sri Savandi Veerabhadraswamy Virabhadra, the temple is situated in the foot of the Savandurga hill. The lord Veerabhadraswamy has followers across the south karnataka districts like Bangalore, Ramanagara, Tumkur, there is a Temple of Sri Lakshmi Narasimha Swamy, where there is an Idol of Lord Narasimha has been worshiped for many generations. The Savandurga hills are frequented by pilgrims who come to visit the Savandi Veerabhadreshwara Swamy, picnickers come to spend time among the serene environs of the hill. Rock climbers, cave explorers and adventurers are among others who frequent the locale, Manchanabele Dam is a great place for watersports. It is worth visiting this dam if you are visiting savandurga, Bus route, Take a bus to Magadi Road from Majestic Bus Stand, Bangalore. Total travelling time 2hrs 15 mins from Bangalore. Along with Ramanagara, this was also a location for the making of David Leans movie A Passage to India, adventure, Many Bangalore Based private adventure tourism companies organise activities here. Please do a research about the safety record of each organization before signing up for any activity. Savandurga provides for some top class serious slab climbing routes in the world, there are a dozen routes, bolted or otherwise on the south face of the monolith
32.
Sangla Hill
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Sangla Hill, is a tehsil in the Nankana Sahib District of the Punjab Province of Pakistan. It lies 103 km from the provincial capital of Lahore. The area has a population of more than 2,00,000 Muslims, with around 10,000 of the population being Christian, the city still has very old building such as a temple which is visible when coming into the city from Faisalabad Road. Sangla Hill city is surrounded by many villages whose residents are mostly Aarein, Jutt, Malik, Butt, Mughal, Ansari, Awaan etc. and a little more minorities. These all people belong to any cast and religion are grace of Sangla city to enhance the brotherhood, most of these are the farmers from Sialkot. They migrated from district Sialkot in 1865 and after migration they took initiatives in eradication of jungles, the city is surrounded by almost 109 villages. The city is the market and economic hub of the area. The city of Sangla Hill is 20 km south-west of Shahkot and 35 km north-west of Sheikhupura, on the east side is Safdarabad Road, and on the north side the road to Hafizabad. To the west, the Main Faisalabad Road links to Faisalabad, Sangla Hill has some very old buildings which belonged to Hindu people, who left them in place during the partition of 1947. A Hindu temple is visible at the side of the Salarwala–Sangla Hill road. Another such Hindu Temple is at the side of hussain trust hospital. Land of temple is encroached. One more Hindu temple is in the building behind the bank at Sangla Faisalabad road. Land of this temple is encroached as well and it is visible nowadays. Presence of these show how much religious tolerance once Sangla Hill enjoyed. These temples are a sign of richness and diversity of the culture of ancient town. Restoration of these temples can give Sangla Hill its lost historical significance, the main feature of the town is the hill, whose peak is visible from five miles away. There are two stations, Sadr and City. The town also has two colleges, one for males and one for females, there are two English-language schools, St. Anthony High School, an international school, and Fauji Foundation Higher Secondary school. The schools have been operating for the past 22 years, a new middle/primary school, Evergreen Grammar School, opened in 2011
33.
Bellary
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Bellary is a historic city in Ballari district in Karnataka state, India. It is 306 kilometres from Bangalore, the state capital, There are several legends explaining how Ballari got its name. The first is that a few devout travelling merchants halting in Ballari and they then installed a balla upside down as a Shiva Linga and worshiped it. Eventually, that place was turned into a dedicated to Balleshwara or Shiva, which became distorted to Malleshwara. The second legend is that the city is named after Indra, the king of Gods, the third legend derives the citys name from the old Kannada word Vallari and Vallapuri. The Union Ministry of Home Affairs of the Government of India approved a proposal to rename the city in October 2014, numerous neolithic archaeological sites have been discovered around Ballari, such as the ash mounds at Sanganakallu, Budhihal, Kudithini, Tekkalakote, Hiregudda and Kupgal. The Sanganakallu settlement, spread over an area of 1,000 acres, is one of the largest neolithic complexes known around Ballari. After the Sevuna Yadavas and the Hoysalas were defeated by the Islamic sultanates of Delhi, the Vijayanagara Empire arose under Harihara I and Bukka I, Ballari itself was ruled by the family of Hande Hanumappa Nayaka, a Palayagara of the Vijayanagara rulers. The Hande Nayakas ceased to be rulers of Ballari after Major Thomas Munro disposed of the palayagars of the ceded districts, in 1808 AD, the ceded districts were split into the Ballari and Kadapa districts, and in 1867 AD the Ballari Municipal Council was created. Further, in 1882 AD, Anantapuram district was carved out of the Ballari District, the Maratha princely state of Sandur was surrounded by Ballari district. The industries in the town included a distillery and two steam cotton presses. The steam cotton-spinning mill established in 1894 had 17,800 spindles, on 1 October 1953 AD, the Ballari district of Madras Presidency was divided on a linguistic basis. Areas with a significant Kannada speaking population were transferred to Mysore state, the Ballari city municipal council was upgraded to a city corporation in 2004. Granite rocks and hills form a prominent feature of Bellary, the city is spread mainly around two hills of granite composition, the Ballari Gudda and the Kumbara Gudda. These two hills are dominant features and visible from every part of the city. Ballari Gudda has a circumference of nearly 2 miles and a height of 480 feet, the length of this rock from north-east to south-west is about 1,150 ft. To the east and south lies an irregular heap of boulders, to the west there is a monolith. When viewed from the south-east it looks like the profile of a face and is therefore also known as Face Hill. Bellary is located at 15. 15°N76. 93°E /15.15,76.93 and it has an average elevation of 495 meters
34.
India
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India, officially the Republic of India, is a country in South Asia. It is the seventh-largest country by area, the second-most populous country, and it is bounded by the Indian Ocean on the south, the Arabian Sea on the southwest, and the Bay of Bengal on the southeast. It shares land borders with Pakistan to the west, China, Nepal, and Bhutan to the northeast, in the Indian Ocean, India is in the vicinity of Sri Lanka and the Maldives. Indias Andaman and Nicobar Islands share a border with Thailand. The Indian subcontinent was home to the urban Indus Valley Civilisation of the 3rd millennium BCE, in the following millennium, the oldest scriptures associated with Hinduism began to be composed. Social stratification, based on caste, emerged in the first millennium BCE, early political consolidations took place under the Maurya and Gupta empires, the later peninsular Middle Kingdoms influenced cultures as far as southeast Asia. In the medieval era, Judaism, Zoroastrianism, Christianity, and Islam arrived, much of the north fell to the Delhi sultanate, the south was united under the Vijayanagara Empire. The economy expanded in the 17th century in the Mughal empire, in the mid-18th century, the subcontinent came under British East India Company rule, and in the mid-19th under British crown rule. A nationalist movement emerged in the late 19th century, which later, under Mahatma Gandhi, was noted for nonviolent resistance, in 2015, the Indian economy was the worlds seventh largest by nominal GDP and third largest by purchasing power parity. Following market-based economic reforms in 1991, India became one of the major economies and is considered a newly industrialised country. However, it continues to face the challenges of poverty, corruption, malnutrition, a nuclear weapons state and regional power, it has the third largest standing army in the world and ranks sixth in military expenditure among nations. India is a constitutional republic governed under a parliamentary system. It is a pluralistic, multilingual and multi-ethnic society and is home to a diversity of wildlife in a variety of protected habitats. The name India is derived from Indus, which originates from the Old Persian word Hindu, the latter term stems from the Sanskrit word Sindhu, which was the historical local appellation for the Indus River. The ancient Greeks referred to the Indians as Indoi, which translates as The people of the Indus, the geographical term Bharat, which is recognised by the Constitution of India as an official name for the country, is used by many Indian languages in its variations. Scholars believe it to be named after the Vedic tribe of Bharatas in the second millennium B. C. E and it is also traditionally associated with the rule of the legendary emperor Bharata. Gaṇarājya is the Sanskrit/Hindi term for republic dating back to the ancient times, hindustan is a Persian name for India dating back to the 3rd century B. C. E. It was introduced into India by the Mughals and widely used since then and its meaning varied, referring to a region that encompassed northern India and Pakistan or India in its entirety
35.
Bhongir
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Bhongir is a town and District Headquarter of Yadadri Bhuvanagiri district of the Indian state of Telangana. It is a part of Hyderabad Metropolitan Region, located on National Highway 163, Bhongir Fort is one of the isolated monolithic rocks carved by the Western Chalukya ruler Tribhuvanamalla Vikramaditya VI and was thus named after him as Tribhuvanagiri. This name gradually became Bhuvanagiri and subsequently Bhongir, Bhongir is located at 17. 5108°N78. 8889°E /17.5108,78.8889. It has an elevation of 329 metres. The municipal area covers 9.63 km², as of 2011 India census, Bhongir had a population of 53,339. Males constitute 51% of the population and females 49%, Bhongir has an average literacy rate of 70%, less than the national average of 74. 04%, with male literacy of 78% and female literacy of 61%. 12% of the population is under 6 years of age, Bhongir as a Lok Sabha constituency came into existence in 2008 as per Delimitation Act of 2002. Notable persons from the town are Alimineti Madhava Reddy, Pratyusha, the are certain notable landmarks in the town. Bhongir Fort is one such structure, rock Climbing School at Bhongir Fort is the training center for rock climbing. Pailla Shekar Reddy is the present MLA, list of towns in India by population
36.
Madhugiri
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Madhugiri is a Taluk headquarters in Tumkur district in the Indian state of Karnataka. The town derives its name from a hillock, Madhu-giri which is to the north of the place, Madhugiri has been declared as Educational District by karnataka state educational department. It includes Madhugiri, Sira, Koratagere and Pavagada Taluks, at 3,930 ft elevation, Madhugiri is a single hill. It is the second largest monolith in Asia, nestled on its steep slopes is a fort. Antaralada Bagilu, Diddibagilu, and Mysuru Gate are the three gateways of the fort, a series of doorways leads to the hill. The ruined temple of Gopalakrishna is located at the top, the construction of the original mudfort was undertaken by Raja Hira Gowda in the 17th century around 1670 AD. An interesting incident prompted the Gowda family to considering building a fortress, a stray sheep went missing around the Madhugiri hillock only to return late in the night dripping with water. This was music to the ears since a spring would definitely be welcome sign for rain deficient area, a decision to construct a fortress was arrived and the task was completed. The Gowdas started ruling this region based at Madhugiri Fort, genesis of the name Madhugiri is derived from the Honeybee colonies which were prevalent in those days towards the northern parts of the Madhugiri fortress. There are two temples located in Madhugiri one is Venkatramana and other is Malleswara. There is also a Jaina temple on the precincts of the Madhugiri fort, Madhugiri, or also known as Maddagiri, is located around 43 km north of Tumkuru town, and 107 km north-west of Bengaluru city. The monolith and the greenery of Madhugiri are the main attractions. The place has old temples of Venkataramanaswami and Malleshwara built by the Vijayanagara feudatories in the Dravidian style, the highlight is the rock dome, atop which stands a fort. There are a series of leading to the top and the climb is steep. On the top is the ruined Gopalakrishna temple, asias second largest monolith is located in Madhugiri. Jayamangali Blackbuck Reserve also known as Maidana Halli Blackbuck Sanctuary is 25 km from Madhugiri and it is near Kodigenahalli, one of the prominent hobli of Madhugiri. Prior permission for overnight camping inside the reserve is needed, chennarayana Durga, located 10 km from Koratagere on the way to Madhugiri via Tumkur, is one of the nine Durga forts. Inside the fort, there is a temple and semi-ruined old structures can be explored
37.
Karnataka
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Karnataka is a state in south western region of India. It was formed on 1 November 1956, with the passage of the States Reorganisation Act, originally known as the State of Mysore, it was renamed Karnataka in 1973. The capital and largest city is Bangalore, the state covers an area of 191,976 square kilometres, or 5.83 percent of the total geographical area of India. It is the seventh largest Indian state by area, with 61,130,704 inhabitants at the 2011 census, Karnataka is the eighth largest state by population, comprising 30 districts. Kannada, one of the languages of India, is the most widely spoken. Most of these rivers flow out of Karnataka eastward into the Bay of Bengal, though several etymologies have been suggested for the name Karnataka, the generally accepted one is that Karnataka is derived from the Kannada words karu and nādu, meaning elevated land. Karu nadu may also be read as karu, meaning black, the British used the word Carnatic, sometimes Karnatak, to describe both sides of peninsular India, south of the Krishna. With an antiquity that dates to the paleolithic, Karnataka has been home to some of the most powerful empires of ancient, the philosophers and musical bards patronised by these empires launched socio-religious and literary movements which have endured to the present day. Karnataka has contributed significantly to both forms of Indian classical music, the Carnatic and Hindustani traditions, Karnatakas pre-history goes back to a paleolithic hand-axe culture evidenced by discoveries of, among other things, hand axes and cleavers in the region. Evidence of neolithic and megalithic cultures have also found in the state. Gold discovered in Harappa was found to be imported from mines in Karnataka, prior to the third century BCE, most of Karnataka formed part of the Nanda Empire before coming under the Mauryan empire of Emperor Ashoka. Four centuries of Satavahana rule followed, allowing them to large areas of Karnataka. The decline of Satavahana power led to the rise of the earliest native kingdoms, the Kadambas, the Kadamba Dynasty, founded by Mayurasharma, had its capital at Banavasi, the Western Ganga Dynasty was formed with Talakad as its capital. These were also the first kingdoms to use Kannada in administration, as evidenced by the Halmidi inscription, the Western Chalukyas patronised a unique style of architecture and Kannada literature which became a precursor to the Hoysala art of 12th century. Parts of modern-day Southern Karnataka were occupied by the Chola Empire at the turn of 11th century, the Cholas and the Hoysalas fought over the region in the early 12th century before it eventually came under Hoysala rule. At the turn of the first millennium, the Hoysalas gained power in the region, literature flourished during this time, which led to the emergence of distinctive Kannada literary metres, and the construction of temples and sculptures adhering to the Vesara style of architecture. The expansion of the Hoysala Empire brought minor parts of modern Andhra Pradesh, in the early 14th century, Harihara and Bukka Raya established the Vijayanagara empire with its capital, Hosapattana, on the banks of the Tungabhadra River in the modern Bellary district. The empire rose as a bulwark against Muslim advances into South India, in 1565, Karnataka and the rest of South India experienced a major geopolitical shift when the Vijayanagara empire fell to a confederation of Islamic sultanates in the Battle of Talikota
38.
Mount Kelam
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Mount Kelam is an exposed granitic dome in West Kalimantan, Borneo, with an elevation of 1,002 m. In 1894, German botanist Johannes Gottfried Hallier became the second European to climb Mount Kelam, Hallier ascended the summit 5 times between January 30 and February 13. He wrote the account of the mountain, Mount Klamm is a unique mountain of grand beauty. It rises singly and abruptly from a plain overgrown by young forest almost up to 1000 m above seal level. Above the upper edge of the cliff there is high mountain vegetation compiled of bushes, the mountains summit area was relatively inaccessible in Halliers time and remains so today. Hallier described it as follows, After once again climbing a slope with Gleichenia thickets. The smooth water-washed stone seamed with water channels shows no variation in structure, and it appears almost as if the whole mountain was composed of a single monstrous block of rock. On this wall has been erected the steep 45 metre high rattan ladder, it is secured only at the bottom, in the middle and in the earth at the top. Leptospermum trees form a canopy on the mountains upper slopes, while grasses. The critically endangered plant species Nepenthes clipeata is endemic to Mount Kelam. Other Nepenthes native to this mountain include N. albomarginata, N. ampullaria, N. rafflesiana, however, habitat stresses such as droughts and forest fires have destroyed much of the summit vegetation. The highly sought-after N. clipeata has additionally suffered from overcollection by plant hunters and is now close to extinction in the wild
39.
Indonesia
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Indonesia, officially the Republic of Indonesia, is a unitary sovereign state and transcontinental country located mainly in Southeast Asia with some territories in Oceania. Situated between the Indian and Pacific oceans, it is the worlds largest island country, with more than seventeen thousand islands. At 1,904,569 square kilometres, Indonesia is the worlds 14th-largest country in terms of area and worlds 7th-largest country in terms of combined sea. It has an population of over 260 million people and is the worlds fourth most populous country. The worlds most populous island, Java, contains more than half of the countrys population, Indonesias republican form of government includes an elected legislature and president. Indonesia has 34 provinces, of which five have Special Administrative status and its capital and countrys most populous city is Jakarta, which is also the most populous city in Southeast Asia and the second in Asia. The country shares land borders with Papua New Guinea, East Timor, other neighbouring countries include Singapore, Vietnam, the Philippines, Australia, Palau, and the Indian territory of the Andaman and Nicobar Islands. Despite its large population and densely populated regions, Indonesia has vast areas of wilderness that support the second highest level of biodiversity. The country has abundant natural resources like oil and natural gas, tin, copper, agriculture mainly produces rice, palm oil, tea, coffee, cacao, medicinal plants, spices and rubber. Indonesias major trading partners are Japan, United States, China, the Indonesian archipelago has been an important region for trade since at least the 7th century, when Srivijaya and then later Majapahit traded with China and India. Local rulers gradually absorbed foreign cultural, religious and political models from the early centuries CE, Indonesian history has been influenced by foreign powers drawn to its natural resources. Indonesia consists of hundreds of native ethnic and linguistic groups. The largest – and politically dominant – ethnic group are the Javanese, a shared identity has developed, defined by a national language, ethnic diversity, religious pluralism within a Muslim-majority population, and a history of colonialism and rebellion against it. Indonesias national motto, Bhinneka Tunggal Ika, articulates the diversity that shapes the country, Indonesias economy is the worlds 16th largest by nominal GDP and the 8th largest by GDP at PPP, the largest in Southeast Asia, and is considered an emerging market and newly industrialised country. Indonesia has been a member of the United Nations since 1950, Indonesia is a member of the G20 major economies and World Trade Organization. The name Indonesia derives from the Greek name of the Indós, the name dates to the 18th century, far predating the formation of independent Indonesia. In 1850, George Windsor Earl, an English ethnologist, proposed the terms Indunesians—and, his preference, in the same publication, one of his students, James Richardson Logan, used Indonesia as a synonym for Indian Archipelago. However, Dutch academics writing in East Indies publications were reluctant to use Indonesia, they preferred Malay Archipelago, the Netherlands East Indies, popularly Indië, the East, and Insulinde
40.
Philippines
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The Philippines, officially the Republic of the Philippines, is a sovereign island country in Southeast Asia situated in the western Pacific Ocean. It consists of about 7,641 islands that are categorized broadly under three main geographical divisions from north to south, Luzon, Visayas, and Mindanao, the capital city of the Philippines is Manila and the most populous city is Quezon City, both part of Metro Manila. The Philippines has an area of 300,000 square kilometers, and it is the eighth-most populated country in Asia and the 12th most populated country in the world. As of 2013, approximately 10 million additional Filipinos lived overseas, multiple ethnicities and cultures are found throughout the islands. In prehistoric times, Negritos were some of the archipelagos earliest inhabitants and they were followed by successive waves of Austronesian peoples. Exchanges with Chinese, Malay, Indian, and Islamic nations occurred, then, various competing maritime states were established under the rule of Datus, Rajahs, Sultans or Lakans. The arrival of Ferdinand Magellan in Homonhon, Eastern Samar in 1521 marked the beginning of Hispanic colonization, in 1543, Spanish explorer Ruy López de Villalobos named the archipelago Las Islas Filipinas in honor of Philip II of Spain. With the arrival of Miguel López de Legazpi from Mexico City, in 1565, the Philippines became part of the Spanish Empire for more than 300 years. This resulted in Roman Catholicism becoming the dominant religion, during this time, Manila became the western hub of the trans-Pacific trade connecting Asia with Acapulco in the Americas using Manila galleons. Aside from the period of Japanese occupation, the United States retained sovereignty over the islands until after World War II, since then, the Philippines has often had a tumultuous experience with democracy, which included the overthrow of a dictatorship by a non-violent revolution. It is a member of the United Nations, World Trade Organization, Association of Southeast Asian Nations, the Asia-Pacific Economic Cooperation forum. It also hosts the headquarters of the Asian Development Bank, the Philippines was named in honor of King Philip II of Spain. Spanish explorer Ruy López de Villalobos, during his expedition in 1542, named the islands of Leyte, eventually the name Las Islas Filipinas would be used to cover all the islands of the archipelago. Before that became commonplace, other such as Islas del Poniente. The official name of the Philippines has changed several times in the course of its history, during the Philippine Revolution, the Malolos Congress proclaimed the establishment of the República Filipina or the Philippine Republic. From the 1898 Treaty of Paris, the name Philippines began to appear, since the end of World War II, the official name of the country has been the Republic of the Philippines. The metatarsal of the Callao Man, reliably dated by uranium-series dating to 67,000 years ago is the oldest human remnant found in the archipelago to date and this distinction previously belonged to the Tabon Man of Palawan, carbon-dated to around 26,500 years ago. Negritos were also among the archipelagos earliest inhabitants, but their first settlement in the Philippines has not been reliably dated, there are several opposing theories regarding the origins of ancient Filipinos
41.
Mount Pulong Bato
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Mount Pulong Bato is a monolith located in Zamboanga City at the Zamboanga Peninsula, the western tip of the island of Mindanao in the Philippines. The mountain is situated in the Upper Abong-Abong Park within the Pasonanca Natural Park, in Barangay Pasonanca, Pulong Bato became infamous because when the Philippine Institute of Volcanology and Seismology confirmed the mountain is a volcano which is unknown to most people. What is unusual about the mountain is, unlike the other surrounding the city. According to PHIVOLCS, the volcano is an Intrusion type of volcano meaning it was formed within earths crust, magma was pushed from the beneath the earth surface but did not come out through an eruption like a typical volcano. The magma eventually solidified while it is enclosed by softer rocks, which was later exposed by erosion or weathering. The mountain is near the premises of the famous Abong-Abong Park, where both domestic and foreign Catholic devotees pilgrimage annually during Holy Week to observe the holiday and meditate
42.
Pakistan
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Pakistan, officially the Islamic Republic of Pakistan, is a federal parliamentary republic in South Asia on the crossroads of Central Asia and Western Asia. It is the sixth-most populous country with a population exceeding 200 million people, in terms of area, it is the 33rd-largest country in the world with an area covering 881,913 square kilometres. It is separated from Tajikistan by Afghanistans narrow Wakhan Corridor in the north, Pakistan is unique among Muslim countries in that it is the only country to have been created in the name of Islam. As a result of the Pakistan Movement led by Muhammad Ali Jinnah and it is an ethnically and linguistically diverse country, with a similarly diverse geography and wildlife. Initially a dominion, Pakistan adopted a constitution in 1956, becoming an Islamic republic, an ethnic civil war in 1971 resulted in the secession of East Pakistan as the new country of Bangladesh. The new constitution stipulated that all laws were to conform to the injunctions of Islam as laid down in the Quran. Pakistan has an economy with a well-integrated agriculture sector. The Pakistani economy is the 24th-largest in the world in terms of purchasing power and it is ranked among the emerging and growth-leading economies of the world, and is backed by one of the worlds largest and fastest-growing middle classes. The post-independence history of Pakistan has been characterised by periods of military rule, the country continues to face challenging problems such as illiteracy, healthcare, and corruption, but has substantially reduced poverty and terrorism and expanded per capita income. It is also a member of CERN. Pakistan is a signatory to the Kyoto Protocol, the Paris Agreement, the name Pakistan literally means land of the pure in Urdu and Persian. It is a play on the word pāk meaning pure in Persian and Pashto, the letter i was incorporated to ease pronunciation and form the linguistically correct and meaningful name. Some of the earliest ancient human civilisations in South Asia originated from areas encompassing present-day Pakistan, the earliest known inhabitants in the region were Soanian during the Lower Paleolithic, of whom stone tools have been found in the Soan Valley of Punjab. The Vedic Civilization, characterised by Indo-Aryan culture, laid the foundations of Hinduism, Multan was an important Hindu pilgrimage centre. The Vedic civilisation flourished in the ancient Gandhāran city of Takṣaśilā, the Indo-Greek Kingdom founded by Demetrius of Bactria included Gandhara and Punjab and reached its greatest extent under Menander, prospering the Greco-Buddhist culture in the region. Taxila had one of the earliest universities and centres of education in the world. At its zenith, the Rai Dynasty of Sindh ruled this region, the Pala Dynasty was the last Buddhist empire, which, under Dharampala and Devapala, stretched across South Asia from what is now Bangladesh through Northern India to Pakistan. The Arab conqueror Muhammad bin Qasim conquered the Indus valley from Sindh to Multan in southern Punjab in 711 AD, the Pakistan governments official chronology identifies this as the time when the foundation of Pakistan was laid
43.
Sigiriya
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Sigiriya or Sinhagiri is an ancient rock fortress located in the northern Matale District near the town of Dambulla in the Central Province, Sri Lanka. The name refers to a site of historical and archaeological significance that is dominated by a column of rock nearly 200 metres high. According to the ancient Sri Lankan chronicle the Culavamsa, this site was selected by King Kasyapa for his new capital and he built his palace on the top of this rock and decorated its sides with colourful frescoes. On a small plateau about halfway up the side of rock he built a gateway in the form of an enormous lion. The name of place is derived from this structure —Sīhāgiri. The capital and the palace was abandoned after the kings death. It was used as a Buddhist monastery until the 14th century, Sigiriya today is a UNESCO listed World Heritage Site. It is one of the best preserved examples of ancient urban planning, the environment around the Sigiriya may have been inhabited since prehistoric times. There is clear evidence that the rock shelters and caves in the vicinity were occupied by Buddhist monks. Buddhist monastic settlements were established during the 3rd century BCE in the western and northern slopes of the hills surrounding the Sigiriya rock. Several rock shelters or caves were created during this period and these shelters were made under large boulders, with carved drip ledges around the cave mouths. Rock inscriptions are carved near the ledges on many of the shelters. These were made in the period between the 3rd century BCE and the 1st century CE, in 477 CE, Kashyapa, the king’s son by a non-royal consort, seized the throne from King Dathusena, following a coup assisted by Migara, the King’s nephew and army commander. The rightful heir, Moggallana, fearing for his life, fled to South India, afraid of an attack by Moggallana, Kashyapa moved the capital and his residence from the traditional capital of Anuradhapura to the more secure Sigiriya. During King Kashyapa’s reign, Sigiriya was developed into a complex city, most of the elaborate constructions on the rock summit and around it, including defensive structures, palaces, and gardens, date from this period. The Culavamsa describes King Kashyapa as the son of King Dhatusena, Kashyapa murdered his father by walling him up alive and then usurping the throne which rightfully belonged to his brother Moggallana, Dhatusenas son by the true queen. Moggallana fled to India to escape being assassinated by Kashyapa, in India he raised an army with the intention of returning and retaking the throne of Sri Lanka, which he considered to be rightfully his. Expecting the inevitable return of Moggallana, Kashyapa is said to have built his palace on the summit of Sigiriya as a fortress, Moggallana finally arrived, declared war, and defeated Kashyapa in 495 CE
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Sri Lanka
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Sri Lanka, officially the Democratic Socialist Republic of Sri Lanka, is an island country in South Asia near south-east India. Sri Lanka has maritime borders with India to the northwest and the Maldives to the southwest, Sri Lankas documented history spans 3,000 years, with evidence of pre-historic human settlements dating back to at least 125,000 years. Its geographic location and deep harbours made it of strategic importance from the time of the ancient Silk Road through to World War II. Sri Lanka was known from the beginning of British colonial rule until 1972 as Ceylon, Sri Lankas recent history has been marred by a thirty-year civil war which decisively ended when the Sri Lankan military defeated the Liberation Tigers of Tamil Eelam in 2009. A diverse and multicultural country, Sri Lanka is home to many religions, ethnic groups, in addition to the majority Sinhalese, it is home to large groups of Sri Lankan and Indian Tamils, Moors, Burghers, Malays, Kaffirs and the aboriginal Vedda. Sri Lanka has a rich Buddhist heritage, and the first known Buddhist writings of Sri Lanka, Sri Lanka is a republic and a unitary state governed by a semi-presidential system. The legislative capital, Sri Jayawardenepura Kotte, is a suburb of the capital and largest city. Along with the Maldives, Sri Lanka is one of the two countries in South Asia that are rated among high human development on the Human Development Index. In antiquity, Sri Lanka was known to travellers by a variety of names, according to the Mahavamsa, the legendary Prince Vijaya named the land Tambapanni, because his followers hands were reddened by the red soil of the area. In Hindu mythology, such as the Mahabharata, the island was referred to as Lankā, in Tamil, the island is referred to as Eelam. Ancient Greek geographers called it Taprobanā or Taprobanē from the word Tambapanni, as a British crown colony, the island was known as Ceylon, it achieved independence as the Dominion of Ceylon in 1948. The country is known in Sinhalese as Śrī Laṃkā and in Tamil as Ilaṅkai, in 1972, its formal name was changed to Free, Sovereign and Independent Republic of Sri Lanka. Later in 1978 it was changed to the Democratic Socialist Republic of Sri Lanka, as the name Ceylon still appears in the names of a number of organisations, the Sri Lankan government announced in 2011 a plan to rename all those over which it has authority. The pre-history of Sri Lanka goes back 125,000 years, the era spans the Palaeolithic, Mesolithic and early Iron Ages. Among the Paleolithic human settlements discovered in Sri Lanka, Pahiyangala and it is said that Kubera was overthrown by his demon stepbrother Ravana, the powerful emperor who built a mythical flying machine named Dandu Monara. The modern city of Wariyapola is described as Ravanas airport, early inhabitants of Sri Lanka were probably ancestors of the Vedda people, an indigenous people numbering approximately 2,500 living in modern-day Sri Lanka. According to the Mahāvamsa, a written in Pāḷi, the original inhabitants of Sri Lanka are the Yakshas and Nagas. Ancient cemeteries that were used before 600BC and other signs of advanced civilization has also discovered in Sri Lanka
