Chonqking: Taking A Look Into China's Cyberpunk City

<div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhpldjp2tqONeQ75SeE04MGMJyVMwJN5cvUf87OIrZrTMcTducm34YIKiWTAl-r7O2FTYhiLhdKxRrVtnGN-mXDz_6Of_C61TqY1QuFp26tY0eaegptYQHWWfZmNzr4SBYugTz-JF6Red56m_VuY3LKqQgojDDjs1WDDZo1zEjy-OkW_wxrWnMXufKoXkqc/s1920/chonqking%202.png" imageanchor="1" style=""><img alt="Chonqking: Taking A Look Into China's Cyberpunk City" border="0" data-original-height="1080" data-original-width="1920" height="157" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhpldjp2tqONeQ75SeE04MGMJyVMwJN5cvUf87OIrZrTMcTducm34YIKiWTAl-r7O2FTYhiLhdKxRrVtnGN-mXDz_6Of_C61TqY1QuFp26tY0eaegptYQHWWfZmNzr4SBYugTz-JF6Red56m_VuY3LKqQgojDDjs1WDDZo1zEjy-OkW_wxrWnMXufKoXkqc/w320-h180/chonqking%202.png" width="280" /></a></div><div class="separator" style="clear: both; text-align: center;"></div><b>articlemostwanted</b> - Imagine this. Recently, IShowSpeed, that wild YouTube streamer everyone’s talking about, took his chaos to the streets of Chongqing, China. His live stream showed a city that looked straight out of a sci-fi movie, with towering skyscrapers, neon lights everywhere, and a vibe that had viewers going, “Wait, where even is this place?” If you caught that stream and wondered how a city could feel so unreal, buckle up. This article is your ticket to exploring Chongqing, a megacity that’s equal parts mind-blowing and unforgettable.<p>Let’s rewind a bit. Chongqing wasn’t always this futuristic beast. Back in the day, think pre-1990s, it was more like a big village hugging the banks of the Yangtze and Jialing rivers. People got around by boat, and bangbangs, those tough porters with bamboo poles, hauled goods up the steep hills. Life was simple, slow, and tied to the rivers. Then came the boom. In the last 30 years, China’s government decided to mash several cities together into one giant economic zone. High-rises shot up practically overnight, turning a sleepy riverside spot into a concrete jungle. Jili, a local guide, says it went from village vibes to megacity madness in just seven or eight years. Now, Chongqing sprawls across 82,000 square kilometers, about the size of Austria, and houses 32 million people. It’s perched in southwest China, a mountain city stacked with levels upon levels, where elevators take you from one street to another. Crazy, right?</p><p>Here’s where it gets wild. People slap the “cyberpunk” label on Chongqing, and it fits like a glove. Picture this: a skyline that could rival Blade Runner, with the Raffles complex, eight sail-shaped towers, dominating the night. At 250 meters, its Skywalk gives you a view that screams futuristic dystopia. Then there’s the nightlife. When the sun dips, the city flips a switch. Neon signs buzz, hotpot joints steam up the streets, and folks party until dawn. It’s not just the lights, though. The whole place feels layered and chaotic, with gas stations on different floors and stairs weaving through a 3D maze. Young locals like Xiao Xian, a rocker with big dreams, thrive in this after-dark energy. It’s a city that never sleeps, glowing with that sci-fi edge.</p><p>Chongqing’s got a pull for travelers, and it’s no surprise why. Hongyadong is a must-see, a rebuilt “new old city” packed with souvenir shops and restaurants, lit up like a postcard at night. Then there’s the train-through-a-skyscraper spot, where a rail line cuts through the eighth floor of a building. Tourists flock there, phones out, snapping pics for Douyin, China’s version of TikTok. It’s so popular the government built a special platform just for photos. And don’t skip the cable cars, running since 1987, offering a ride over the rivers with views that’ll stick with you. Paipai, a local trip seller, says folks come for the mountain city charm and leave with memories they can’t shake. With 3,000 to 4,000 visitors daily, it’s a paradise for anyone chasing epic shots.</p><p>Look, if you ever get the chance to hit up China, make Chongqing a priority. This isn’t just another city. It’s a full-on experience, from spicy hotpot that’ll test your limits to a nightlife that keeps rolling till the bars shut down. Sure, it’s not for everyone, the faint-hearted might struggle with the heights and the heat, but if you’re up for adventure, this place delivers. Martin, a German guy slinging sausages there, calls it a city of opportunity, and he’s not wrong. Whether you’re climbing stairs for a workout or staring out from a skyscraper, Chongqing’s got a pulse you won’t find anywhere else. So, pack your bags, grab your camera, and see what the hype’s about. You won’t forget it.</p>

Chonqking: Taking A Look Into China's Cyberpunk City

articlemostwanted - Imagine this. Recently, IShowSpeed, that wild YouTube streamer everyone’s talking about, took his chaos to the streets ...

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Bali Is More Recognized Than Indonesia: Is It A Bad Thing?

<div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjLXEuuDTiB8oYV3dzjsoFyHMybUpbwZDD4XOQ9Wc3wDhoQlV5aePWB1m1Pv5Bhd9lcIYtNziQ1E4SLRRoYgaHDcwwVr9SihcfHiTAZNFk_zayahrZ3BN0rfoqm2bomb8Xme1itiUrcZ4bCQExBxI_gq801ZyHal-Yhz1bIQqgPB-_AaPz7M7P7rw8Jwz46/s1920/bali%20island%20indo%201920%201080.png" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1080" data-original-width="1920" height="157" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjLXEuuDTiB8oYV3dzjsoFyHMybUpbwZDD4XOQ9Wc3wDhoQlV5aePWB1m1Pv5Bhd9lcIYtNziQ1E4SLRRoYgaHDcwwVr9SihcfHiTAZNFk_zayahrZ3BN0rfoqm2bomb8Xme1itiUrcZ4bCQExBxI_gq801ZyHal-Yhz1bIQqgPB-_AaPz7M7P7rw8Jwz46/s280/bali%20island%20indo%201920%201080.png" width="280" /></a></div><b style="text-align: left;">articlemostwanted - </b>If you ask people in the West about Bali, many will light up with recognition. They might mention its stunning beaches, vibrant culture, or reputation as a tropical paradise. Now, try asking them about Indonesia, the country that Bali belongs to. More often than not, you’ll get a blank stare or a vague nod. It’s a curious thing: the island of Bali often overshadows the nation it’s part of. People know the destination, but the country itself? Not so much. How did this happen? If you’re wondering about the reasons behind this odd twist of fame, stick around. This article will dive into why Bali outshines Indonesia on the global stage, and we’ll explore whether this is a good thing or a bad thing.</p><p>So, why does Bali steal the spotlight from Indonesia? The answer lies in a mix of history, marketing, and global perception. Bali’s rise to fame began decades ago when it caught the eye of Western travelers. In the 1920s and 1930s, artists, writers, and anthropologists flocked to the island, drawn by its unique Hindu culture amid a predominantly Muslim nation. This fascination grew over time, fueled by books, films, and eventually tourism campaigns. By the 1970s, Bali was a must-visit spot, while Indonesia as a whole remained a blur in the background.</p><p>Tourism data backs this up. According to Indonesia’s Ministry of Tourism and Creative Economy, Bali welcomed over 6 million foreign visitors in 2019, before the pandemic hit. That’s a huge chunk of the 16 million total visitors to Indonesia that year, as reported by Statistics Indonesia (BPS). Bali, a single island among Indonesia’s 17,000, accounts for nearly 40% of the country’s tourism traffic. The world sees Bali as a standalone gem, often unaware it’s part of a sprawling archipelago nation.</p><p>Then there’s the branding factor. Bali has a clear identity: temples, rice fields, yoga retreats. Indonesia? It’s harder to pin down. With over 300 ethnic groups and a vast landscape stretching across thousands of miles, the country struggles to present a unified image. Western media doesn’t help. A 2023 study by the Pew Research Center found that Indonesia rarely makes headlines in the U.S. or Europe unless it’s tied to natural disasters or economic stats, while Bali pops up in travel blogs and Instagram feeds nonstop. Over time, this gap widened. Bali became the star, and Indonesia faded into the shadows.</p><p>This imbalance, where Bali outshines Indonesia, isn’t something to celebrate. It’s a problem, and here’s why. First, Indonesia is massive. It’s the fourth most populous country in the world, home to over 270 million people, according to the World Bank’s 2023 data. It spans an area larger than many European nations combined. Yet, its global presence feels small. Countries with far fewer people, like Singapore or South Korea, command more attention in trade, culture, and politics. When Bali hogs the spotlight, Indonesia’s potential as a major player gets ignored. The world sees a tiny island, not the giant nation behind it.</p><p>Second, the government’s weakness makes this worse. Indonesia’s leadership lacks clout on the international stage, and it shows in painful ways. Take the passport, for example. Henley & Partners’ 2024 Passport Index ranks Indonesia’s passport at 65th globally, granting visa-free access to just 73 destinations. Compare that to Malaysia, ranked 12th with access to 181, or even Thailand at 60th with 82. A weak passport reflects a deeper issue: the government struggles to build influence or trust abroad. Domestically, corruption and inefficiency plague progress, as noted in Transparency International’s 2023 Corruption Perceptions Index, where Indonesia scores a modest 34 out of 100. Bali’s fame might dazzle tourists, but it masks a country that’s barely holding its own. These two realities, a big nation with little sway and a government failing to lead, prove Indonesia deserves more notice than it gets. Instead, Bali takes the credit, and that’s a bad thing.</p><p>In the end, Bali’s fame overshadowing Indonesia isn’t just a quirk of perception. It’s a signal of something broken. If Indonesia wants to step out of Bali’s shadow and claim the recognition it deserves, the government needs to act. Stronger policies, both at home and abroad, could lift the country’s profile. Cleaning up corruption, boosting the economy, and asserting a bolder voice in global forums would help. A stronger passport, one that opens more doors for its people, would be a clear sign of progress. Better recognition starts there. But if the government doesn’t see this, or worse, if it’s deliberately letting Indonesia coast on Bali’s coattails, the country is in trouble. Doom might be a strong word, but it fits a nation that lets an island define it. Indonesia has the size, the people, and the potential to be more than a backdrop. It’s time to prove it.</p>

Bali Is More Recognized Than Indonesia: Is It A Bad Thing?

articlemostwanted -  If you ask people in the West about Bali, many will light up with recognition. They might mention its stunning beaches,...

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Andorra La Vella, What's That?!

<div class="separator" style="clear: both; text-align: center;"> </div> <div class="separator" style="clear: both; text-align: center;"> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhcoD-3CNssCRfzfYCsjwdAfdV2EpsDculgm5zmtMGS83BkhUV6XWBXHh375_34n-bqG8y1XkntBQgBrWC7Ve_LjP4O2iHN42A5rjUWKaPempW2fgONS2eF5pi2SJlY3piCbK631KQYUjM/s1600/andorra-la-vella.jpg" imageanchor="1" style=""><img alt="Andorra La Vella" border="0" data-original-height="562" data-original-width="796" height="196" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhcoD-3CNssCRfzfYCsjwdAfdV2EpsDculgm5zmtMGS83BkhUV6XWBXHh375_34n-bqG8y1XkntBQgBrWC7Ve_LjP4O2iHN42A5rjUWKaPempW2fgONS2eF5pi2SJlY3piCbK631KQYUjM/s280/andorra-la-vella.jpg" title="Andorra La Vella" width="280" /></a></div> amw - ONE OF THE WORLD'Sauthentic curiosities, the autonomous coprincipality of all Andorra retains independent standing that, based on history, was awarded inthe 9th century by Charlemagne for its public's valiant solutions to him contrary to the Moors.<br /><br />Due to the upper valleys of the lake Valira, this small nation is nestled among the high mountain passes of this Pyrénées involving FRANCE and SPAIN. Just 2.5 occasions thesize of Washington, D.C., it's among the smallest nations on earth.<br /><br />Why is Andorra really curious, however, is it is unusual status as a coprincipality, although with no local prince; rather, it's regulated jointly by the republic of FRANCE and from the Bishop of Urgell, a little town several miles to the south in Spain. The French president and the bishop behave as coprinces only nominally, nevertheless, and since 1993 the nation has been completely autonomous and self-ruling.<br /><br /> <h3> PEAKS AND VALLEYS</h3> Andorra is situated between the French division of Ariège, at the region of Midi Pyrénées, as well as the Spanish state of Lérida (or even Lleida) at the region of Catalonia. The climate is quite severe, restricting plant to nominal mountain escape: One hint of the source of this title Andorra, is the fact that it comes in a local expression for"tree coated."<br /><br />However, this climate offers exceptional high mountain pastures for sheep and cows and is also a fantastic attraction for skiers from all around Europe. The market runs largely on tourism, together with numerous winter and summer resorts, and as a duty-free shopping centre. The majority of its people reside in one of six chief villages, increase their herds of cows or cows, and handle tiny farms, increasing rye, wheat, bar-ley, oats, and vegetables. Additionally, there are some fruit or-chards and wineries.<br /><br />The majority of the populace resides in and around the capital, Andorra la Vella, in which there's some mild manufacture, especially cigarettes, vases, along with anisette liqueur. The co principality was collectively dominated because a treaty at 1278 between the Count of Foix and the Bishop of Urgell. At that moment, there were many tiny countries between France and Spain; the most odd thing is that one burst to the 21st century. The move of Port d'Envalita (7,943 feet or 2,407 m) has functioned as a significant route between Toulouse, France, and northern Spain since early times. While the condition of the bishop remained exactly the same, the Counts of Foix finally expired and the name was consumed by the king of France from the 17th century.<br /><br />Following the French Revolution, the article fell to the president of this re-public. Back in 1993, Andorrans voted in favour of a new constitution which, while keeping the honorific position of the co princes, provides Andorra complete sovereignty and control over its own affairs, both external and internal.<br /> <i><br /></i> <i>source: <a href="https://www.britannica.com/place/Andorra" rel="nofollow">click here</a></i>

Andorra La Vella, What's That?!

amw - ONE OF THE WORLD'Sauthentic curiosities, the autonomous coprincipality of all Andorra retains independent standing that, based...

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Andes Mountains in South America

<div class="separator" style="clear: both; text-align: center;"> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiDtmp8WxEAc6cqt1o-2aAAqbqMGTCB0V39xMlOtK2Ub-goKZ6y5bR8GP86VkjLMz2rlY9u-Brd5nZf7-aO9JAts4DCF6NsfYAkXwahgHqIyEuxkNVIvuk-Szh-KPMg22MYdz8RDyTds60/s1600/30-andes-mountains-south-america-amw.jpg" imageanchor="1" style=""><img alt="Andes Mountains in South America" border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiDtmp8WxEAc6cqt1o-2aAAqbqMGTCB0V39xMlOtK2Ub-goKZ6y5bR8GP86VkjLMz2rlY9u-Brd5nZf7-aO9JAts4DCF6NsfYAkXwahgHqIyEuxkNVIvuk-Szh-KPMg22MYdz8RDyTds60/s1600/30-andes-mountains-south-america-amw.jpg" title="Andes Mountains in South America" /></a></div> <b>amw </b>- Andes Mountains called one of the fantastic natural attributes of the Planet Earth and the Andes, Spanish Cordillera de los Andes or Los Andes, pile technique of South America.<br /> <br /> They separate a narrow western coastal place from the continent's rest, affecting significantly life's circumstances in areas as well as inside the runs themselves. The Andes retain the highest highs while in the Western Hemisphere. The highest of them is Mount Aconcagua (22,831 toes [6,959 metres]) about the border of Argentina and Chile.<br /> <br /> The Andes are not one distinct formidable highs but instead a sequence of transverse and parallel mountain stages, or cordilleras, and of intervening plateaus. Specific asian and european ranges—respectively named the Cordillera Oriental as well as most of the system's Cordillera Occidental—are trait.<br /> <br /> Some historians feel the name Andes comes from the Quechuan term anti (“east”); others propose it is derived from the Quechuan anta (“copper”). It possibly is more modest to ascribe it to the anta of the mature Aymara language, which connotes copper shade usually.<br /> <iframe allowfullscreen="" frameborder="0" height="210" src="https://www.youtube.com/embed/rhpGzPierAY" width="280"></iframe> <br /> <h1> Real characteristics of Andes</h1> There's no common deal in regards to the main north-south subdivisions of the Andes program. For the reasons with this dialogue, the machine is divided in to three broad groups. From south to northern these are the Southern Andes, comprising Patagonian cordilleras, and the Chilean, Fuegian; the Key Andes, like the cordilleras; as well as the Upper Andes, surrounding the Ecuadorian, Colombian, and Venezuelan (or Caribbean) cordilleras.<br /> <br /> <h3> Geology</h3> The Andean mountain program could be the consequence of international menu-tectonic forces through the Cenozoic Time (about the past 65 million years) that created upon earlier geologic activity. About 250 million years were joined together to the supercontinent Pangaea. The next breakup of Gondwana, its part and of Pangaea, dispersed these dishes outward, where they begun to consider the current-day continents' form and location. The accident (or convergence) of two of these plates—the continental Southamerican Platter and also the oceanic Nazca Plate—gave climb to the orogenic (pile-building) task that made the Andes.<br /> <br /> Many of the rocks containing the current-morning cordilleras are of era that is good. They began as sediments eroded from your Amazonia craton (or shield)—the old granitic fragment that comprises a lot of Brazil—and deposited between about 450 and 250 thousand years back on the craton’s western flank. The weight of those remains forced a subsidence (downwarping) of the crust, along with the ensuing force and warmth metamorphosed the deposits into more tolerant stones; hence, sandstone, siltstone, and limestone were altered, respectively, into quartzite, shale, and marble.<br /> <br /> Roughly 170 thousand years back this complicated geologic matrix started to be uplifted whilst the western fringe of the Nazca Dish was compelled underneath the western fringe of the Southamerican Dish (i.e., the Nazca Dish was subducted), caused by the latter plate’s westward motion in reaction to the starting of the Atlantic Sea towards the east. This subduction-uplift procedure was followed closely by the invasion of substantial levels of magma in the layer, first within the type of a volcanic arc across the western fringe of the Southamerican Dish and later from the shot of warm options into surrounding continental stones; the latter procedure produced numerous dikes and veins containing levels of financially useful nutrients that later were to perform a vital part within the individual profession of the Andes.<br /> <br /> This activity's strength elevated throughout the Cenozoic Period, and also the cordilleras' existing form surfaced. The approved period of time due to their increase have been from about 15-million to 6million years back. Nevertheless, through the usage of methods that are more complex, scientists within the early 21st-century could decide the uplift started about 25 thousand years back. The resulting hill method displays an exceptional straight differential greater than 40,000 legs between your base of the Peru-Chile (Atacama) Trench off the Pacific coastline of the region and also the highs of the large hills inside a horizontal length of significantly less than 200 miles. The tectonic processes that produced the Andes have extended to the time that is present. The system—part of the circum that is bigger - Pacific string that frequently is known as Fire—remains' Band volcanically active and it is susceptible to disastrous earthquakes.<br /> <br /> The Fuegian Andes start about the mountainous Estados (Staten) Area, the Tierra del Fuego archipelago's easternmost point, achieving a height of 3,700 feet. They operate through Grande Area towards the northwest, where the greatest ridges—including Brackets Darwin and significantly less than 7,900 feet high. the existence of the impartial Sierra de la Costa complicates the physiography of the southernmost neighborhood of the Andes program.<br /> <br /> The Patagonian Andes increase north of Magellan of the Strait. Depressions and several transverse and breaches reduce this tough and crazy part of the Andes totally; several amounts are filled by fjords, glaciers, streams, ponds, or snow areas. The crests of the hills exceed 10,000 feet (Attach Fitzroy achieving 11,073 feet) north to permission 46° S but typical only 6,500–8,400 feet from permission 46° to 41° S, aside from Mount Tronador (11,453 feet). This area represents one of the most generally acknowledged upper degree of the Patagonian Andes; there's some difference, nevertheless, about that restriction, some putting it further south, in the Beach of Penas, (47° S) yet others considering it to become towards the north, around 30° S.<br /> <br /> Other functions that are significant would be the over 50 lakes. These depressions which are free from water type rich valleys named nevada, that are quickly attained by low moves. Wonderful and impenetrable woods develop on both sides of those cordilleras, particularly about the western hills; these woods protect the hills as large whilst the snow-line, though in the greater altitudes toward the north as well as in Tierra del Fuego the vegetation is gloomier and less thick. Both Argentina have produced national areas to protect the natural splendor that was area’s.<br /> <br /> <h3> Physiography of the Central Andes</h3> The Key Andes begin at latitude 35° S, at a position where the cordillera undergoes a pointed change of character. Its breadth increases to about 50 kilometers, and it becomes dry and higher; the passes, too, are not secondary and much more difficult to corner. Glaciers are uncommon and located just at elevations. The main assortment also will be the discharge split between streams flowing to the Pacific as well as the Atlantic and serves since the boundary between Chile and Argentina. The last of the southern series of volcanoes, Mount Tupungato (21,555 feet) is simply east of Santiago, Chile. A line of high, snowcapped mountains rise between Tupungato and the grand Mount Aconcagua. For the north of Aconcagua lies Mount Mercedario (22,211 feet), and between them will be the large travels of Support Espinacito (16,000 feet) and Support Patos (12,825 feet). Farther north the moves are far higher although numerous. Ojos del Salado, Mounts Bonete, and Pissis' mountains surpass 20,000 feet.<br /> <br /> The peak of Tres Cruces (22,156 feet) at 27° S latitude marks the culmination of this part of the cordillera. Towards the north is available a transverse depression and the southern limit of the large plateau region named the Atacama Level in Argentina and Chile as well as the Altiplano in Bolivia. Where the fantastic plateau is surrounded by two amounts: the Oriental as well as the Occidental greater because it innovations grow into Bolivia and Peru.<br /> <br /> Northward, to latitude 18° S, El Cóndor, Sierra Nevada's mountains, Llullaillaco, Galán, and Antofalla all surpass 19,000 feet. Due to the remains of salts they contain the 2 major stages and many volcanic extra stores enclose depressions called salars; in northwestern Argentina, the Sierra de Calalaste involves the large Antofalla Salt Flat. Volcanoes of the region occur mostly on the northerly line along the Cordillera Occidental so far as Misti Volcano (permission 16° S) in Peru.<br /> <br /> The Cordillera Occidental's slopes descend steadily for the Atacama Desert over the coastline. At about 18° S the trend of the Cordillera Occidental improvements into a northwesterly direction. The Cordillera Oriental to the east, lower and created on the wide sleep of lava, is cut and denuded by rivers with large gradients, provided by heavy rainfall. It has two pieces. The southern piece is 150 miles extensive and—with the exception of Chorolque Peak in Bolivia (18,414 feet)—of fairly low elevation. The upper section in Bolivia, named Cordillera True, is slender, with bigger peaks and snow; 000 legs, the most crucial highs, at over 21, are Mounts Illimani and Illampu.<br /> <br /> Into Bolivia the Cordillera Oriental penetrates at about latitude 22° S and identifies a wide semicircle to the north and then towards the northwest; for the west the Altiplano reaches its broadest extent. The Altiplano—500 miles 80 miles and long wide—is one of many largest interior basins of the entire world. Different in elevation from 11,200 to 12,800 legs, it has no discharge store to the sea. Approximately in the centre of the plateau is a superb depression between the two cordilleras.<br /> <br /> The three amounts are products of erosive action of streams that have cut at deep canyons between them. West of the Cordillera Vilcabamba, the Apurímac River runs in another of the biggest canyons of the Western Hemisphere. The city of Cuzco lies in the valley west of the Cordillera de Vilcanota at an elevation of nearly 11,000 feet.<br /> <br /> The Andes typically have now been referred to as three cordilleras, that can come together in the Vilcanota and Loja (Ecuador) troubles. The Pasco Knot is just a big, high level. Towards the northwest it's surrounded from the Cordillera Huarochirí, about the northwest mountain which the Rímac River increases in a bunch of ponds given by glaciers and descends quickly towards the sea (15,700 ft in 60 miles). 800 legs, Ticlio Pass an elevation of some 15, can be used with a train. Several small ponds and wetlands are observed about the troubles, with Sea Junín (about 20 kilometers long) being the biggest.<br /> <br /> North three distinct amounts operate across the level, of the Pasco Knot: the Cordilleras Occidental, Main, and Asian. At permission 10° S, within the Cordillera Occidental, the heavy, Huaylas Valley that is slim divides Cordillera Negra towards the west and two amounts; the Santa Water reduces Cordillera Negra to strain in to the Pacific and runs between them. Sometimes, earthquakes that increase there break off the glaciers and hurry down the hills, destroying vegetation and negotiations within their pathways. Cordillera Negra, since it isn't coated with ideal so-named, is gloomier.<br /> <br /> Latitude 9° S is joined at by both amounts. The Marañón Water, which goes northward between your Cordilleras Occidental and Main at about 6° S, changes its path of circulation towards the northeast, penetrating right into an area of thin transverse water spaces (pongos) that slice the cordillera to achieve the Amazon basin. These contain Rentema (about one-and-one-next kilometers long and 200 ft wide), Mayo, Mayasito, and Huarcaya spaces and—the many important—Manseriche Space, that will be eight miles long.<br /> <br /> Between your Cordilleras Central and Asian, the Huallaga River operates in a deep stuff with several little valleys; it reduces the western cordillera at Aguirre Space (permission 6° S). The Cordillera Oriental ends at 5° S in the Amazon container.<br /> <br /> The lasting snow-line reaches an elevation of 19,000 legs in Support Chanchani (about permission 16° S) and decreases to about 15,000 legs in Cordillera Blanca and also to 13,000 toes on Mount Huascarán. While vegetation modifications to bushes and heathland hills become softer and broader to look at. The elevation reduces, and moves are reduced at Porculla Pass (7,000 legs) east.<br /> <br /> <h3> Physiography of the Upper Andes</h3> An eroded and tough high-mass of hills named the Loja Knot (4° S) in Ecuador represents the move between the Ecuadorian Andes and also the cordilleras. The Ecuadorian program includes a lengthy, slim level from south to northern outlined by two mountain chains comprising numerous large volcanoes operating. The western edge may be the greater and older Cordillera Central, assigned with a type of 20 volcanoes; several of those, for example Chimborazu Volcano (20,702 legs), have lasting snowcaps.<br /> <br /> their surrounding hills as well as these basins, that are intensively grown, include approximately 50% of Ecuador’s population.<br /> <br /> A next cordillera it has been called the Cordillera Oriental and hasbeen recognized within the asian marketplace of Ecuador. The number seems to be an old alluvial development that's been split large rain and by streams right into a quantity of hill people. Forest are remote or type abnormal small stores and covers such people whilst the cordilleras of Guacamayo and Lumbaquí.<br /> <br /> Further towards the north may be the excellent massif of the Pasto Hills (permission 1°–2° D), that will be the most crucial Colombian physiographic complex and also the supply of most of the country’s streams.<br /> <br /> Three unique ranges Main, and Asian, work northward. The Cordillera Occidental, mildly large and similar towards the coastline, reaches a height of almost 13,000 legs at Support Paramillo before descending in to the lowlands of Colombia in three amounts. The Cordillera Key may be the greatest (average elevation of nearly 10,000 legs) but additionally the smallest selection of Colombian Andes, extending some 400 kilometers before its most northern spurs disappear at about permission 8° D. In to a level which Medellín can be found, the number expands at about permission 6° D.<br /> <br /> Between Occidental and the Cordilleras Central is the Patía, a superb despair -Cauca area, divided in to three plains. The southernmost may be the thin area the seas which circulation towards the Pacific, of the Patía Water. The center plain may be the greatest in height (8,200 feet) and comprises the partition of another two.<br /> <br /> The Cordillera Oriental developments somewhat towards the northeast and it is the greatest of the three and also the largest. The typical elevation is 900 feet, 7,900 to 8. North of permission 3° D following a little despair increases in to the Sumapaz Uplands, which variety in height from 10 000 feet and the cordillera expands. North of the Sumapaz Upland the number separates into two, attaching a sizable basic 200 kilometers long and 125 kilometers broad, frequently disturbed by transverse stores that are little that sabanas which contain in regards to a third of Colombia’s population was named by type many upland basins. Bogotá's city is about most and the biggest filled of those sabanas; additional essential towns on sabanas are Sogamoso and Chiquinquirá. East of Ford (5° D) the cordillera separates in to a number of sudden similar organizations operating towards the north northeast; included in this the Sierra Nevada del Cocuy (18,022 toes) is large enough to possess snowcapped mountains.<br /> <br /> Further north the main amounts of the Cordillera Main arrived at a finish, however the flanking stores proceed and diverge towards northeast and the north. Those chains' westernmost may be the Sierra, which on its part contains the Sierra; the variety extends far north as permission 11° D in La Guajira Peninsula and types some of the border between Colombia. The asian string enters Venezuela whilst the Cordillera de Mérida and bends towards the east.<br /> <br /> The Venezuelan Andes are displayed from the Cordillera de Mérida (280 kilometers long, 50 to 90 kilometers broad, and about 10,000 legs in height), which stretches in a northeasterly path towards the town of Barquisimeto, where it stops.<br /> Soils<br /> <br /> Guardian substance, topography, the complicated interchange between environment, and biology that decides soil types as well as their situation is seriously suffering from elevation within the Andes. Generally soils are fairly youthful and therefore are susceptible to excellent erosion by winds and water due to the high gradients of a lot of the property.<br /> <br /> Within Patagonian Andes and the Fuegian, the forming of soils is challenging; those things of powerful winds and of glaciers have remaining almost clean stone in several locations. Peat bogs, podzols, and field soils, all with heavy perspectives (levels) of humus, are observed; discharge is bad. Soils which are full of natural substance and therefore are well-drained happen in lakes' region. North soils, of permission 45° S are shaped directly at elevations on weathered stones, and reddish-brown soils with gravel are observed within the lower areas; erosion is large.<br /> <br /> This earth form, with several variations, stretches to north of Peru across the Cordillera Occidental.<br /> <br /> Within the embryonic soils dark with natural content are observed. At altitudes between 6, 000 000 toes, reddish, brown happen on container surfaces and on reasonable hills. In places that are drained, soils having a sandy skyline are not fairly sterile; these soils would be the many financially essential in Bolivia and Ecuador. Colombia's sabana soils are grey-brown, by having an impenetrable claypan in a few amounts, leading to inadequate drainage.<br /> <br /> At elevations soils are stony and slim. About the western cordilleras' east-side, slim, descending towards the Amazon bowl, damp soils that are badly created are susceptible to erosion that is substantial. Intrazonal soils (individuals with weakly produced perspectives) contain humic clay and solonetz (dim alkaline soils) kinds discovered near to ponds and lagoons. Additionally one of them team are soils created from Chile from ash within the Cordillera Occidental to Ecuador.<br /> <br /> In Colombia yellow brown soils on hills as well as in gorges would be the foot of the coffee farms that are big.<br /> <br /> <h3> Weather</h3> The hottest water forests and deserts generally are separated from tundralike puna with a few miles. There also is significant climatic imbalance between the external slopes (i.e., those facing the Pacific or the Amazon basin) along with the central hills of the cordilleras; the additional mountains are beneath the impact of often the ocean or even the Amazon basin. As mentioned above, the distinct lasting snow varies greatly. It improves to 20,000 feet at latitude 27° S, after which it begins descending again till it reaches 15,000 legs within the Andes,600 feet from 2.<br /> <br /> Precipitation varies widely. South of permission 38° S precipitation exceeds 20-inches, whereas to the north it diminishes significantly and becomes significantly seasonal. Farther north—on the Altiplano of Bolivia, the plateau, and in the sabanas of Colombia—rainfall as well as the valleys of Ecuador is modest, although volumes are extremely variable. It rains solely in very small portions to the west-side of the Cordillera Occidental but significantly more in Ecuador. About the east (Amazonian) side of the Cordilleras Orientales, rain usually is seasonal and major.<br /> <br /> Heat varies significantly with elevation. While in the Peruvian and Ecuadorian Andes, as an example, the climate is hawaiian up to an altitude of 4,900 feet, becoming subtropical upto 8,200 feet; hot conditions win throughout the day, and times are not slightly cool. Between 8, 200 500 feet conditions are slight, but you can find noticeable differences between all the time; this zone comprises the Andes' most welcoming area. From 11,500 to 14,800 legs it usually is cold—with good differences between morning and between shadow—and and sunshine conditions are below-freezing during the night. Between about 13,500 and 15,700 ft (the puna), the environment of the páramo is located, with continuous subfreezing conditions. Lastly, above 15,700 legs, the climate of the highs and large ridges is polar with exceptionally low temperatures and frigid winds.<br /> <br /> As in different mountainous aspects of the world, an extensive number of microclimates (extremely local climatic problems) occur due to the interaction of element, experience of winds, permission, period of morning, and other factors. Peru, specifically, has one of habitats due to its numerous microclimates' world’s most complex arrays.<br /> <br /> <h3> Place and animal life</h3> The ability of flowers and pets to reside within the Andes differs with altitude, even though the lifestyle of plant areas is also determined by weather, availability of water, and soil, while that of animal life can also be afflicted with the variety of food solutions; the permanent snow-line is the upper limit of habitation. Animals and some flowers can stay at any altitude, among others can stay merely at specified amounts. Cats seldom stay above 13,000 feet, while white-tailed rats may surpass 17 and will not remain lower than 13,000 feet. The camelids (llama, guanaco, alpaca, and vicuña) are animals largely of the Altiplano (11,200 to 12,800 feet), while they could live-well at lower altitudes. It's believed that the condor may fly-up to 26.<br /> <br /> Height amplifies quite a few climatic variables—such as temperature, wind, light, and dryness—that figure out what kinds of plants increase in various elements of the Andes, although possibly the low pressures of high altitudes are very important to vegetation. Generally, the Andes could be divided into altitudinal rings, each with regular main vegetation and fauna; but permission imposes variations between south and northern, and distance to the Pacific and also to the Amazon basin is shown in variations between your additional and internal hills of the Cordilleras Occidental and Oriental.<br /> <br /> A zone at about permission 35° S separates two distinct regions of the Andes.<br /> <br /> Faculties for the north are not same. The Cordillera Occidental is incredibly dried inside the south, slightly damp (with water and tight rainfall) in central and northern Peru, and damp with large or average rainfall in Ecuador and Colombia. The climatic structure is followed by vegetation: while in the south it is desertlike and bad, nevertheless at greater altitudes vegetation occurs. Pets are the guemul, puma, vizcacha, cuy (guinea pig), chinchilla, camelids, rats, and lizards; one of the birds will be the condor, partridge, parina, huallata, and coot. Eliminating areas where irrigation approaches are utilized , agricultural potential is bad. The east side of the Cordilleras Orientales northward from Bolivia has the majority of it, rich vegetation warm forest having a rich jungle fauna.<br /> <br /> To the level (valleys, plains, stages, and inner hills of the cordilleras), living again is closely related to altitude. Exotic arms and eternal snows lay inside a few kilometers in peaks,000 legs of each different, where elevation can vary from 1,600 ft in deep gorges to over 20. As much as an elevation 000 legs, of 8, vegetation reflects the dried warm and subtropical environment, and farming is vital: Colombia's great coffee marketplace is situated mostly in the warm valleys with this sector. Between 11 and 8,200,500 feet lies the Andes' most used area; several of the key locations of the nations is there, and also the area helps the key section of Andean agriculture. Temperatures change from comfortable in the valleys to reasonable reduced (all the way down to 50 °F [10 °C]) on the plains, sabanas, and mountains, and there is periodic rain and water from rivers. This zone is also suited to livestock and poultry farming.<br /> <br /> Between 11,500 and 13,400-feet relief is normally not smooth and burdensome for farming. In Colombia this sector is sub and páramo -páramo, with seasonal rainfall; in Ecuador water is not scarce; as well as in Peru páramo has from reasonable to rare rainfall. From 13,400 to 15,700 feet (the puna), vegetation includes plants that fight the cold temperature and evening cold; above 16,000 feet, vegetation is almost missing.<br /> <br /> Source: <a href="https://www.britannica.com/place/Andes-Mountains">Click here</a><br /> <i>Advertising - Read Also :</i><br /> <i>- <a href="http://sekertarisku.com/madu-alami-manfaat-bahaya/">Madu Alami, Manfaat dan Bahayanya</a></i><br /> <i>- <a href="http://www.dongenganakdunia.com/2016/08/sang-cahaya-biru-dongeng-jerman.html">Sang Cahaya Biru - Dongeng Jerman</a></i>

Andes Mountains in South America

amw - Andes Mountains called one of the fantastic natural attributes of the Planet Earth and the Andes, Spanish Cordillera de los Andes or...

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Anatolian Plateau

<div class="separator" style="clear: both; text-align: center;"> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjxV4eF-WBLx98Q2P1UVgEbMHJhBguOuNlLympw-lajczlcY757VMneXYbKg6XzO0nbMfU7mnGLk4mskO_PfT8NWHGBXV0vi-T3fcuynParSToI0Hr4p1uF2jOyWGKgwUAv9HKT8HhjKA0/s1600/4-Anatolian+Plateau.jpg" imageanchor="1" style=""><img alt="Anatolian Plateau" border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjxV4eF-WBLx98Q2P1UVgEbMHJhBguOuNlLympw-lajczlcY757VMneXYbKg6XzO0nbMfU7mnGLk4mskO_PfT8NWHGBXV0vi-T3fcuynParSToI0Hr4p1uF2jOyWGKgwUAv9HKT8HhjKA0/s1600/4-Anatolian+Plateau.jpg" title="Anatolian Plateau" /></a></div> <b>articlemostwanted </b>- THE ANATOLIAN PLATEAU is the main upland region of the ancient area of Anatolia, today's TURKEY. The plateau is hemmed in by two parallel mountain ranges, the Taurus to the south, along the Mediterranean coast, and the Pontic Mountains to the north, along the coast of the BLACK SEA.<br /> <br /> <h3> History of Anatolian Plateau</h3> <span style="background-color: #cccccc;"><a href="http://forticeoffice.com/services/" rel="nofollow">virtual office di jakarta</a> .adv</span> - Anatolia has worked as a bridge between the civilizations of Europe and Asia for thousands of years, with waves of various cultures making the most of this main position and developing cities and empires on the plateau. The place of the very first big empire of the Western world, the Hittite, dating from the 15th century B.C.E., the Anatolian Plateau was later on given its modern-day name Anatolia, or "increasing sun" by the Greeks looking eastward.<br /> <br /> <h3> Geography of the Plateau</h3> Most of the Anatolian Plateau lies at elevations above 1,640 feet (500 m).This mountainous region lies at the center of the Arabian, African, Eurasian, Aegean and Turkish tectonic plates: the resulting landscape is dotted with volcanoes (today extinct) and routine earthquakes. The main plateau is composed of uplifted blocks and downfolded troughs filled by shallow salt lakes. Elevations on the plateau itself range from 1,980 to 3,960 feet (600 to 1,200 m). This increases to the east, where the two range of mountains, the Taurus and Pontic, sign up with to form the eastern highlands (consisting of the greatest mountain peaks in Turkey such as Mount Ararat).<br /> <br /> The two biggest basins on the plateau are the Konya Ovasi and the basin occupied by Tuz Golu (Salt Lake)-both drain large inland locations and have no external outlet. Other parts of the Anatolian Plateau are drained either by short rivers that stream south into the Mediterranean, or by numerous larger rivers (notably the Halys and the Sakarya) that drain pipes northward into the Black Sea.<br /> <br /> Two extinct VOLCANOES, Erciyes and Hasan, left lava flows that have worn down over time to form amazing landscapes of rock cones and topped pinnacles in Goreme, near Nevsehir. The earth in these locations is colored a range of grays and reds. The Anatolian plateau is primarily dry with a mixture of dark and desert soils. Summers here are hotter and drier than in the rest of Anatolia, however also colder and wetter in the winter season, with temperature levels balancing freezing and frequent heavy snows.<br /> <br /> The Anatolian plateau is primarily covered in STEPPE, with brief yards, bushes and stunted willow trees. Wooded areas are restricted to the northwest and northeast, and growing (wheat and barley) is restricted to narrow river valleys. IRRIGATION is practiced where water is readily available, but a deeply established river course makes it difficult for engineers to raise the water to the surrounding farming land.<br /> <br /> Summertime dust storms, locusts, extreme heat, and periodic droughts restrict agricultural output. Some locations are cultivated with orchards and vineyards, but for one of the most part the land is used for grazing. Some larger animals reside in the highlands (wolf, fox, bear), but the ubiquitous domesticated Angora goat is all over. Stock raising is necessary and overgrazing has also triggered some erosion issues.<br /> <br /> <h3> Current state</h3> The capital of the republic of Turkey was transferred to the Anatolian Plateau in 1923. The city of Ankara was picked as the capital of the brand-new state to remove it from undertones of the royal capital at Istanbul and to put it in the geographic center of the nation. The area is likewise the home of ancient ruins of the Hittite civilization at Catal Huyuk and to the underground cities of Kaymakli and Derinkuyu, ancient refuges for early Christians.<br /> Konya (Roman Iconium) is the area's significant cultural center, understood for its mosques and "whirling dervishes.".<br /> <br /> <i>source: <a href="http://edugeography.com/content/anatolian-plateau.html">click here</a></i>

Anatolian Plateau

articlemostwanted - THE ANATOLIAN PLATEAU is the main upland region of the ancient area of Anatolia, today's TURKEY. The plateau is he...

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Amur River

<table align="center" cellpadding="0" cellspacing="0" class="tr-caption-container" style="margin-left: auto; margin-right: auto; text-align: center;"><tbody> <tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgyM9vpmsNTwNL-T2qgX_aMgrkbzfqyb78Wz7t5J0Cymc6hhYsNDHeKCH_Nh-t0s-F2MI9gwmoSFbVUKwiuDmJYnmjxeEERwfswwejsYWOQ3hzoDh8emO0YHqv9ZxwbbGhIdnI52TFAEf4/s1600/18-amur-river.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgyM9vpmsNTwNL-T2qgX_aMgrkbzfqyb78Wz7t5J0Cymc6hhYsNDHeKCH_Nh-t0s-F2MI9gwmoSFbVUKwiuDmJYnmjxeEERwfswwejsYWOQ3hzoDh8emO0YHqv9ZxwbbGhIdnI52TFAEf4/s1600/18-amur-river.jpg" /></a></td></tr> <tr><td class="tr-caption" style="text-align: center;">credit: edugeography.com</td></tr> </tbody></table> <b>articlemostwanted </b>- There is a river that located in Siberia that streams more then 1,800 mi (2,897 km) towards the Tatar Straits location, the passage in between Sakhalin and the Russian Pacific Ocean. It flows from the junction of the Shilka and the rivers that located at east region of Lake BAIKAL called Argun rivers. This river called Amur river.<br /> <br /> With all tributaries, the Amur basin covers nearly 750,000 square mi (1,942,491 square km) of location.<br /> The Russian push into the river valley in the mid-17th century led to a border clash with the Chinese Empire.<br /> The Treaty of Nerchinsk (1689) admitted the territorial sovereignty of the Manchu dynasty over the Amur river area for 150 years.<br /> The Chinese know the river as the Heilongjiang.<br /> <br /> In the mid-19th century, the Amur river, as the lone river in Siberia that flows eastward to the PACIFIC OCEAN, got geopolitical significance for the Russian Empire.<br /> After the unequal treaties concluded with CHINA in 1850 and 1860, RUSSIA annexed the Amur area. Russian 19th-century geographers mentioned the Amur as Russia's gateway to the Pacific.<br /> <br /> Not only is the river is plentiful with fish, however also the mild environment is appropriate for farming (grain, veggies, fruits).<br /> <br /> <span style="background-color: #cccccc;"><a href="http://robust-chemical.com/lemari-asam-fume-hood-based-on-wooden-structure/" rel="nofollow">lemari asam pdf</a> .adv</span> - A methodical geographical exploration of the river by the Russians started in 1824 with Grigorii Spasskii's research "Historical and Statistical Notes about Places along the Amur River." In 1846, navigator Alexander Gavrilov cruised to the mouth of the Amur and reported that the river was too shallow for even little ships.<br /> <br /> This was modified by Gennadii Nevel'skoi's expedition in 1849 that found that the mouth of the Amur river was navigable by ships of any size.<br /> The Russian government feared a British profession of the river mouth and the east Siberian general governor, Nikolai Murav'ev-Amurskii, coined the Russian geopolitical logic that whoever will control the mouth shall manage Siberia to Lake Baikal.<br /> <br /> In 1856, the tzarist federal government declared the Amur region an open market zone. After the emancipation of the serfs (1861), the federal government supported the complimentary colonization with tax exemptions. Though some countless peasants settled along the Amur, the region continued to be underpopulated up until the modern age.<br /> <br /> In view of the prohibited migration in between 1860 and World War I, the tzarist government established the socalled Amur Cossack Division, which monitored the border line along the river.<br /> In the Russian Civil War (1917-22) Japanese soldiers occupied the Amur river region. Again in the 1930s and in the late 1960s, the Amur ended up being a military trouble spot in between the Soviet Union and its East Asian next-door neighbors, JAPAN and China.<br /> <br /> In the period of Sino-Soviet fight, the Soviet federal government developed a frontier ethos that was, at least, reflected by the construction of the BAM (Baikal-Amur- Magistrale).<br /> <br /> After the breakdown of the Soviet Union in 1989, the Amur region experienced a population outflow to European Russia that led to a decreasing commercial production. Nonetheless, the Amur river area seeks economic cooperation with close-by China and facilitates border trade in between the cities Blagoveshchensk and Heihe.<br /> <br /> <i>source: <a href="http://edugeography.com/content/amur-river.html">click here</a></i>

Amur River

credit: edugeography.com articlemostwanted - There is a river that located in Siberia that streams more then 1,800 mi (2,897 km) towards...

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Amu Darya - One the Longest River Of Central Asia

<table align="center" cellpadding="0" cellspacing="0" class="tr-caption-container" style="margin-left: auto; margin-right: auto; text-align: center;"><tbody> <tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhBudqeLFLwz4SRtnz8aFiPEw9kj_fJiqK8Ltzp-wf43npGJNhL9KQMOuT2KGVI8giYhvZeZuoc1j6UK-57_pLjnpgdO8zzq8jBIlJfcdAl8qm3PyE8uQgw3ML0EnlLN3bVy17Y34a8Un4/s1600/30-amu-darya-articlemostwanted.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhBudqeLFLwz4SRtnz8aFiPEw9kj_fJiqK8Ltzp-wf43npGJNhL9KQMOuT2KGVI8giYhvZeZuoc1j6UK-57_pLjnpgdO8zzq8jBIlJfcdAl8qm3PyE8uQgw3ML0EnlLN3bVy17Y34a8Un4/s1600/30-amu-darya-articlemostwanted.jpg" /></a></td></tr> <tr><td class="tr-caption" style="text-align: center;">Courtesy of Britannia</td></tr> </tbody></table> <b>articlemostwaanted </b>- Amu Darya, in English called Amu River, Tajik Daryoi Amu, Turkmen Amyderya, Uzbek Amudaryo, ancient name Oxus River, one of the longest rivers of Central Asia. The Amu Darya was traditionally known to the Western world from Greek and Roman times as the Oxus and was called the Jay'un by the Arabs. It allegedly derives its present name from the city of Amul, which is said to have occupied the site of modern Türkmenabat (formerly Chärjew) in Turkmenistan. As well known as it was in antiquity, the river nevertheless received but little attention in Europe until the reign of Peter I the Great, tsar of Russia. Though the first relatively authentic map of the river was made in 1734, systematic research in the region began only at the end of the 19th century. At the end of the 1920s, a map of the entire Amu Darya basin was published in Tashkent.<br /> <br /> <h3> AMU DARYA RIVER COURSE AND BASIN</h3> The river is formed by the confluence of the Vakhsh and Panj (Pyandzh) rivers (at which point it becomes known as the Amu Darya) and flows west-northwest. In its upper course the Amu Darya forms part of Afghanistan’s northern border with Tajikistan, Uzbekistan, and Turkmenistan. It then flows across the desert of eastern Turkmenistan and in its lower course forms part of the boundary between Uzbekistan to the northeast and Turkmenistan to the southwest. The Amu Darya is 879 miles (1,415 km) long, but its length is 1,578 miles (2,540 km) if measured from the sources of its headstream, the Panj River, in the Pamirs. In the past the Amu Darya discharged into the Aral Sea, but the diversion of river water for agriculture in the 20th and 21st centuries has contributed to the shrinking of the Aral Sea and ensured that the river no longer reaches its historic terminus.<br /> <br /> Not far below the junction of the Panj with the Vakhsh, the Amu Darya is joined by three additional tributaries: from the left (south) by the Qonduz River and from the right (north) by the Kofarnihon (Kafirnigan) and Surkhan rivers. After leaving the highland zone, the river veers to the northwest to cross the arid Turan Plain, where it forms the boundary between the Karakum Desert to the southwest and the Kyzylkum Desert to the northeast. The Amu Darya loses much of its water in this region to irrigation, evaporation, and seepage.<br /> <br /> The Amu Darya’s basin extends for 600 miles (950 km) from north to south and for more than 900 miles (1,450 km) from east to west. It borders the Syr Darya basin to the north, the Tarim Basin to the east, and the Indus and Helmand river basins to the south. Of the basin’s total area of 179,700 square miles (465,500 square km), only half lies within its source region, the mountain ranges of the Pamirs and the Hindu Kush to the east.<br /> <br /> <h3> CLIMATE AND HYDROLOGY</h3> Rainfall and temperature in the Amu Darya basin vary mainly according to topography. Mid-latitude westerlies are the main source of precipitation in the river basin. The precipitation falls mainly as snow during the winter and helps feed the glaciers in the source areas of the Amu Darya, at the highest elevations in the Pamirs and the Hindu Kush, where temperatures average below freezing in winter and annual precipitation may exceed 40 inches (1,015 mm). Mean monthly temperatures increase and precipitation decreases at lower elevations. In the lower reaches of the Amu Darya, mean annual precipitation is less than 4 inches (100 mm), with mean July temperatures above 77 °F (25 °C) and mean January temperatures ranging between 32 °F and 50 °F (0 °C and 10 °C).<br /> <br /> Hydrologically, therefore, the Amu Darya basin consists of two units: a mountainous zone of nourishment and a lowland zone of depletion. The Amu Darya’s headwaters rise in the mountains of Tajikistan and Afghanistan, among the permanent snows and glaciers of the Pamirs, the Trans-Alay Range to the northwest, and the Hindu Kush, where elevations range from 16,400 to 23,000 feet (5,000 to 7,000 metres). The river’s two principal sources, the Vakhsh River and the Panj River, whose tributaries include the Pamir, follow a westerly course.<br /> <br /> <span style="background-color: #cccccc;"><a href="http://robust-chemical.com/lemari-asam-fume-hood-based-on-wooden-structure/" rel="nofollow">lemari asam lokal berkualitas</a> .adv</span> - The Amu Darya’s flow increases from March to May, when snow melts on the plains and rainfall increases, and the flow is further augmented in summer as the ice and snow of the mountain ranges melt. The flow gradually abates from September to February. During winter, ice forms along the banks of the river’s upper reaches, and its lower sections may freeze completely for more than two months. As the ice floes begin to disperse in February and March, they jam the river downstream, forming a natural dam. These dams sometimes burst catastrophically and cause major flooding. In its upper course the river’s flow is stable; in its lower course it is much less so. The river’s sediment load is high.<br /> <br /> <h3> HUMAN IMPACT ON THE NATURAL ENVIRONMENT</h3> Before the 1970s, the Amu Darya branched into a number of tributaries that emptied into the Aral Sea through an extensive delta. However, the Soviet government began diverting massive amounts of water from the river beginning in the 1950s to irrigate cotton and other crops grown in the river’s lower basin. The main section of the Karakum Canal was completed in the 1960s to carry water from the Amu Darya at Kerki, Turkmenistan, westward to Mary and Ashgabat. The diversion of water from the Amu Darya for irrigation decreased the amount of water entering the Aral Sea, which consequently began shrinking. Increased irrigation on the hot, dry floodplains of the Amu Darya and in adjacent regions resulted in evaporation that left salt deposits that make the soil infertile. Surface runoff transported these salts into surface waters and increased the salinity of the Amu Darya. By the first decade of the 21st century, the southern shore of the Aral Sea had receded many miles from the former delta of the Amu Darya. Lakes and wetlands fed by the river in the delta area shrank to only a tiny percentage of their former size.<br /> <br /> Junipers and poplars grow down to the river’s edge in the mountain regions, where sweetbrier and blackberries also abound. Willows, buckthorn, poplars, and oleasters predominate at lower elevations. The trees along the river’s lowest reaches once formed an impenetrable tangle at the river’s reed-covered delta, but salt- and drought-resistant plants are now the predominant flora there. The depleted and polluted waters of the lower Amu Darya and its former delta, once rich with wildlife, are now nearly devoid of fish and birds.<br /> <br /> Even before its diminished lower reaches were closed to navigation, the Amu Darya carried little traffic because of its unstable riverbed and shoals. A complex system of dams was erected beginning in the mid-20th century, mainly on the lower course, to provide irrigation and to protect the cultivated fields from flood. A giant 984-foot (300-metre) dam and hydroelectric station was constructed on the Vakhsh River at Norak (Nurek), Tajikistan, in the 1970s and ’80s. Construction of another dam on the Vakhsh at Rogun, Tajikistan, was halted when floodwaters ravaged the site in 1993; some work on the project has been done since then.<br /> <br /> source: <a href="http://www.britannica.com/place/Amu-Darya">click here</a>

Amu Darya - One the Longest River Of Central Asia

Courtesy of Britannia articlemostwaanted - Amu Darya, in English called Amu River, Tajik Daryoi Amu, Turkmen Amyderya, Uzbek Amudaryo, a...

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American Samoa - Best Natural Deepwater Harbors

<div class="separator" style="clear: both; text-align: center;"> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi_fRDG8ka2lv3QAbCWqPCT0M5I4LTVfLS_KLsN_5AS8t5jZcCveQcpPChGMukSdwhHg6ANpl07LX-rXoZloXM3HwQWFnHf6q5Y3xrkMYqLOjxRBtNQFopE3h-A1I7yoDagIpR2ZROVlaA/s1600/15-american-samoa.jpg" imageanchor="1" style=""><img border="0" height="191" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi_fRDG8ka2lv3QAbCWqPCT0M5I4LTVfLS_KLsN_5AS8t5jZcCveQcpPChGMukSdwhHg6ANpl07LX-rXoZloXM3HwQWFnHf6q5Y3xrkMYqLOjxRBtNQFopE3h-A1I7yoDagIpR2ZROVlaA/s280/15-american-samoa.jpg" width="280" /></a></div> <b>articlemostwanted </b>- <b>AMERICAN SAMOA</b>, an area of the UNITED STATES in the PACIFIC OCEAN, includes the eastern half of the Samoan island chain and makes up 5 volcanic islands: the primary island of Tutuila and its smaller partner, Anu'u, plus the islands of Ofu, Olosega, and Ta'u (the Manu'a Islands) to the east.<br /> <br /> The area, with its capital at Pago Pago, is 77.6 square mi (199 square km) and has a highest point at Lata of 3,188 ft (966 m). It has a population of 70,260. The area likewise includes the more distant coral atolls, Rose and Sand, and small Swains Island, far to the north. The islands extend roughly 186 mi (300 km) from west to east and lie about two-thirds of the way from HAWAII to NEW ZEALAND.<br /> <br /> <span style="background-color: #cccccc;"><a href="http://forticeoffice.com/" rel="nofollow">virtual office surabaya</a> .adv</span> - The primary town and management center, Pago Pago, has among the very best natural deep water harbors in the South Pacific Ocean, secured from rough seas and high winds. Strategically situated at the crossroads of the South Pacific, the harbor at Pago attracted the interest of the United States Navy as early as the 1870s and stayed a primary coaling point for U.S. ships crossing the Pacific until completion of World War I, when oil changed coal in the majority of bigger vessels. Since then, <b>American Samoa</b> has actually stayed a relative backwater and has therefore retained much of its conventional lifestyle, unlike a number of its next-door neighbors.<br /> <br /> <b>American Samoa</b>'s nearest next-door neighbors are the sovereign states of [Western] SAMOA and TONGA to the west and southwest and the New Zealand dependences of Tokelau, Cook Islands and Niue to the north, east, and south. The islands lie just to the east of the INTERNATIONAL DATE LINE and at the crossway of the 3 cultural divisions of POLYNESIA, MICRONESIA, and MELANESIA, though the Samoans themselves fall within the Polynesian sphere. The islands are volcanic in origin, with rugged peaks and restricted coastal plains.<br /> <br /> <h2> American Samoa Climate </h2> The climate is tropical marine, with ample rainfall, promoting dense forests on most the islands and allowing cultivation of bananas, coconuts, taro, breadfruit, yams, copra, pineapples, and papayas. Industries are limited to several large tuna canneries, plus local handicrafts and garments. Tourist is not heavy, because there is minimal airline service. The canneries were opened in the 1950s and 1960s and made up 90 percent of all exports in 1995. But few locals wish to work there, so half the labor force are aliens, mostly from Western Samoa and tonga. Young people originally <b>American Samoa</b> are increasingly leaving for the mainland United States for higher education and employment possibility. The population therefore differs commonly (for instance, in 1984 it was provided as just 36,000). About 90 percent survive Tutuila, mainly near Pago Pago.<br /> <br /> <h2> American Samoa Culture </h2> The islands were settled long before European contact in the 18th century. Native chiefs looked to the United States in the late 19th century for defense versus the squabbles of European colonial powers. The first treaty with a local chief permitting U.S. boats to anchor in Pago Harbor was checked in 1872, and negotiations in between Great Britain, Germany, and the United States caused a partition in 1899 (at 171 degrees west longitude), though the ranking Samoan chiefs did not formally cede their areas till 1904 (after the United States had actually currently established its administration).<br /> <br /> The bigger islands in the group, Upolu and Savai'i, went to GERMANY and from 1962 formed the independent country of Samoa. The population of the eastern islands in 1900 was less than 6,000. After World War I, the Samoans were primarily delegated themselves, and their standard system of federal government and family based common landownership was preserved. Subsistence economy was successful and local traditions were strong, so many Western impacts were either turned down or, like Christianity, molded to fit the Samoan way.<br /> <br /> Because 1951 the islands have actually fallen under the jurisdiction of the United States Department of the Interior, and a new constitution was adopted in 1966, but, unlike America's other territories in the Pacific, there is little desire to change the status quo, either toward independence or towards closer affiliation with the United States. The islands count on heavy subsidies and welfare programs but are also cautious of losing their traditional lifestyle by submitting entirely to U.S. law (for instance, the continuation of government management by semi-hereditary chiefs, the matai, and the system of communal landholding, under which about 92 percent of the land remains to be held by standard kin groups). <b>American Samoa</b> hence remains an unorganized, unincorporated territory of the United States.<br /> <br /> Samoans are primarily independent, and rigorous restrictions of migration are planned to preserve their autonomy and traditional culture.<br /> <i><br /></i> <i>BIBLIOGRAPHY. World Factbook (CIA, 2004); Ron Crocombe, The South Pacific (University of the South Pacific, Institute of Pacific Studies, 2001); Frederica Bunge and Melinda W. Cooke, Oceania: A Regional Study (Foreign Area Studies Series, 1985); K.R. Howe, Robert C. Kiste, Brij V. Lal, eds., Tides of History: The Pacific Islands in the Twentieth Century (University of Hawaii Press, 1994).</i>

American Samoa - Best Natural Deepwater Harbors

articlemostwanted - AMERICAN SAMOA , an area of the UNITED STATES in the PACIFIC OCEAN, includes the eastern half of the Samoan island cha...

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Altai Mountains

<table align="center" cellpadding="0" cellspacing="0" class="tr-caption-container" style="margin-left: auto; margin-right: auto; text-align: center;"><tbody> <tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiUiMxk8qtsbcB1JNE_aJQ4nUCXdNKRPGBQ2hPDTngZn4usIgmibAVK8GEOZMeD6vBtAo_uQ3G72oO_EyjzDdM0jITq5d3PH0ukNhdp_OlY91Kp5vxFcMMY283i8L1WhL8VEGmfhf_bpiM/s1600/1-altai-mountains-articlemostwated.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiUiMxk8qtsbcB1JNE_aJQ4nUCXdNKRPGBQ2hPDTngZn4usIgmibAVK8GEOZMeD6vBtAo_uQ3G72oO_EyjzDdM0jITq5d3PH0ukNhdp_OlY91Kp5vxFcMMY283i8L1WhL8VEGmfhf_bpiM/s1600/1-altai-mountains-articlemostwated.jpg" /></a></td></tr> <tr><td class="tr-caption" style="text-align: center;">Courtesy of wikipedia - Altai mountains</td></tr> </tbody></table> <b>articlemostwanted </b>- THE ALTAI MOUNTAINS are a system of remote mountains in central Asia that cover an area of 326,256 square mi (845,000 square km) bounding RUSSIA, KAZAKHSTAN, MONGOLIA, and CHINA. This system is a natural marvel that has been mainly unblemished by huge markets and has a really sporadic population. Its name is originated from the Mongolian word altan, which means "golden." This region is the home of many types of wild animals and plants and is comprised of various landscapes. Most of the population in this area depends on farming and tourism.<br /> <br /> Altai mountains stretch for 1,242 mi (2,000 km) from northwest to southeast, reaching a height of about 14,783 feet (4,506 m) at Belukha. Many rivers can be discovered in the Altai Mountains and the majority of them are fed by glaciers. Some of the largest rivers are Katun, Biya, and Chuya.<br /> <br /> <span style="background-color: #cccccc;"><a href="http://robust-chemical.com/lemari-asam-fume-hood-based-on-wooden-structure/" rel="nofollow">lemari asam laboratorium</a> .adv</span> - The glaciers cover a location of about 900 square mi(2,330 square km). Together with extensive river disintegrations, they have contributed significantly to the development of the ruggedness of the region, where high waterfalls, steppes, and countless lakes can also be discovered. The deepest lake in the Altai Mountains, Telet-skoe, is 1,066 ft (325 m) deep. The Altai Mountains are the source of the Ob and Irtysh Rivers, 2 of the significant rivers in Asia. The region is rich in many natural resources like iron, gold, mercury, manganese, and marble. The United Nations Educational, Scientific and Cultural Organization (UNESCO) acknowledged the significance in protecting this eco-region and added 5 clusters of the Altai in the World Natural Heritage List.<br /> <br /> The area is defined by a continental climate with long, cold winters and short, cool summer seasons. Snow starts covering the mountains during October and November, marking the start of winter season. Temperature levels struck the lowest in January, where they can vary from 7 degrees F (-14 degrees C) in the foothills to -76 degrees F (-60 degrees C) in the STEPPEs. In northern Siberia, one can discover vast locations of completely frozen soil. Summertimes begin someplace in between May and July and end in September. Throughout this time temperature levels frequently reach 75 degrees F (24 degrees C) throughout the day. Temperature levels of 104 degrees F (40 degrees C) have likewise been recorded in the lower regions. At night, temperature levels get cooler, normally ranging from 41 degrees F (5 degrees C) to 50 degrees F (10 degrees C). Elevations of 5,000 to 65,000 ft (1,500 to 19,000 m) experience high precipitation, normally ranging from 20 in (50 cm) to 40 in (1 m) a year. One aspect of the summertime that many individuals appreciate is the absence of mosquitoes.<br /> <br /> Four vegetation zones can be found in the Altai Mountains: the mountain subdesert, steppe, forest, and the Alpine areas. The most extensively used plants and trees are cedar, badan, kuril tea, and marijuana. The subdesert has hardly any plant life; the few plants that exist are drought-resistant and salt-tolerant. Numerous sod turfs and shrubs can be discovered in the steppe. The forest is usually boggy and covers a large location in the low to medium mountain location. Here are found pines, firs, larches, and birch and aspen forests. The meadows in the Alpine region are utilized for pasture throughout the summer season.<br /> <br /> Wildlife is abundant in this region. There are 230 types of small birds, like woodpeckers, and 20 species of fish. Big mammals like bears, lynx, and musk deer are found mainly in the forest. In the Alpine area live reindeer, mountain goats, rams, as well as unusual animals like snow leopards. Some locations in the mountains are unattainable to locals and visitors since they are utilized to study uncommon types of animals and plants.<br /> <br /> The Altai Mountains are occupied by mainly Altais and Russian inhabitants, a number of whom moved there in the 19th century, primarily to leave religious persecution The native population that existed before the 19th century continues to stay in the old ways and is somewhat separated from civilization. This area deals with many difficulties, particularly with civilization knocking on its door. The big concern is ways to maintain the ecosystem and its natural charm in spite of the enhancing variety of travelers and developments.<br /> <br /> <i>source: R.W. MCCOLL, PH.D.</i>

Altai Mountains

Courtesy of wikipedia - Altai mountains articlemostwanted - THE ALTAI MOUNTAINS are a system of remote mountains in central Asia that co...

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Afghanistan Economy Fact

<table align="center" cellpadding="0" cellspacing="0" class="tr-caption-container" style="margin-left: auto; margin-right: auto; text-align: center;"><tbody> <tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjjv9aqbuJTVya21XEP8gK8CKt66H0IHWK9UDet-k0f7RBAJV__GWfc6jQc1wFbYijWrwqc_N-Ck_SjgP40PEii_fDlPHC2ZFKwXhMKVtFUxUhNTPMTrAm8ZYDFqbYoeWpv6KwsIGPoYuQ/s1600/29-afghanistan-economy-fact-articlemostwanted.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjjv9aqbuJTVya21XEP8gK8CKt66H0IHWK9UDet-k0f7RBAJV__GWfc6jQc1wFbYijWrwqc_N-Ck_SjgP40PEii_fDlPHC2ZFKwXhMKVtFUxUhNTPMTrAm8ZYDFqbYoeWpv6KwsIGPoYuQ/s1600/29-afghanistan-economy-fact-articlemostwanted.jpg" /></a></td></tr> <tr><td class="tr-caption" style="text-align: center;">Courtesy of worldtofravel.com</td></tr> </tbody></table> <b>articlemostwanted </b>- Ahmad Shah DURRANI unified the Pashtun tribes and established Afghanistan in 1747. The nation served as a buffer between the British and Russian Empires till it won self-reliance from notional British control in 1919. A short experiment in democracy ended in a 1973 coup and a 1978 communist counter-coup. The Soviet Union got into in 1979 to support the tottering Afghan communist program, touching off a long and damaging war. The USSR withdrew in 1989 under relentless pressure by internationally supported anti-communist mujahedin rebels. A series of succeeding civil wars saw Kabul lastly fall in 1996 to the Taliban, a hardline Pakistani-sponsored movement that emerged in 1994 to end the country's civil war and anarchy. Following the 11 September 2001 terrorist attacks, a United States, Allied, and anti-Taliban Northern Alliance military action fell the Taliban for sheltering Osama BIN LADIN.<br /> <br /> <span style="background-color: #cccccc;"><a href="http://robust-chemical.com/lemari-asam-fume-hood-based-on-wooden-structure/" rel="nofollow">lemari asam pdf</a> .adv</span> - A UN-sponsored Bonn Conference in 2001 established a procedure for political reconstruction that included the adoption of a brand-new constitution, a presidential election in 2004, and National Assembly elections in 2005. In December 2004, Hamid KARZAI ended up being the first democratically chosen president of Afghanistan and the National Assembly was inaugurated the following December. KARZAI was reelected in August 2009 for a second term. The 2014 governmental election was the country's very first to include a runoff, which featured the top 2 vote-getters from the preliminary, Abdullah ABDULLAH and Ashraf GHANI. Throughout the summer season of 2014, their campaigns disputed the results and traded allegations of fraud, leading to a US-led diplomatic intervention that consisted of a complete vote audit as well as political settlements in between the two camps. In September 2014, GHANI and ABDULLAH consented to form the Government of National Unity, with GHANI inaugurated as President and ABDULLAH raised to the newly-created position of Chief Executive Officer. The day after the launch, the Ghani administration signed the US-Afghan Bilateral Security Agreement and NATO Status of Forces Agreement, which supply the legal basis for the post-2014 worldwide military presence in Afghanistan.<br /> <br /> Despite gains towards building a steady central federal government, the Taliban stay a major difficulty for the Afghan Government in practically every province. The Taliban still considers itself the rightful federal government of Afghanistan and it remains a capable and confident insurgent force regardless of credit reports in 2015 that its creator and spiritual leader, Mullah Mohammad OMAR, probably passed away in 2013.<br /> <br /> Afghanistan's economy is recovering from decades of problem. The economy has actually improved considerably considering that the fall of the Taliban routine in 2001 mostly because of the infusion of international help, the healing of the agricultural sector, and service sector development. In spite of the development of the past few years, Afghanistan is extremely poor, landlocked, and extremely depending on foreign aid. Much of the population remains to struggle with scarcities of real estate, clean water, electrical energy, healthcare, and jobs. Criminality, insecurity, weak governance, absence of facilities, and the Afghan Government's difficulty in extending guideline of law to all parts of the country lead to difficulties to future financial growth. Afghanistan's living standards are amongst the most affordable on the planet.<br /> <br /> The worldwide neighborhood continues to be committed to Afghanistan's development, promising over $67 billion at 9 donors' conferences between 2003-10. In July 2012, the donors at the Tokyo conference promised an added $16 billion in civilian product through 2015. Despite this help, the Government of Afghanistan will have to overcome a variety of challenges, consisting of low income collection, anemic task production, high levels of corruption, weak government capacity, and bad public facilities.<br /> <br /> Afghanistan's development rate slowed markedly in 2014-15. The drawdown of global security forces that started in 2014 has actually negatively impacted economic growth, as a significant part of commerce, specifically in the services sector, has actually dealt with the continuous worldwide troop existence in the nation. Afghan President Ashraf GHANI is devoted to instituting economic reforms to include improving profits collection and battling corruption. However, the reforms will take some time to carry out and Afghanistan will stay dependent on worldwide donor support over the next several years.<br /> <br /> <i>source: <a href="https://www.cia.gov/library/publications/the-world-factbook/geos/af.html">CIA</a></i>

Afghanistan Economy Fact

Courtesy of worldtofravel.com articlemostwanted - Ahmad Shah DURRANI unified the Pashtun tribes and established Afghanistan in 1747. The...

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Albania - The Only European Country Where Muslim is Majority

<table align="center" cellpadding="0" cellspacing="0" class="tr-caption-container" style="margin-left: auto; margin-right: auto; text-align: center;"><tbody> <tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhkh8UZy9g3KLhQ-1EslOVTFM3wHeCbecxrqAlmdqWS0Sk2thpBzxRtYk5yyTcneMiEhHZ8vs_ra4pnZ0W-9viBtfM0LWVW-ie7SNMlbUmGVpVZFXydy1oLR_rORvIRi-8b0UGuhME5BzY/s1600/4-albania-muslim-europe-country-articlemostwanted.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhkh8UZy9g3KLhQ-1EslOVTFM3wHeCbecxrqAlmdqWS0Sk2thpBzxRtYk5yyTcneMiEhHZ8vs_ra4pnZ0W-9viBtfM0LWVW-ie7SNMlbUmGVpVZFXydy1oLR_rORvIRi-8b0UGuhME5BzY/s1600/4-albania-muslim-europe-country-articlemostwanted.jpg" /></a></td></tr> <tr><td class="tr-caption" style="text-align: center;">Courtesy of operationworld.org</td></tr> </tbody></table> <b>articlemostwanted </b>- ALBANIA IS UNIQUE in many ways. This small, mountainous country on the western side of the Balkan Peninsula has a language and also a society that vary significantly from those of its neighbors. Most notably, it is the only nation in Europe with a bulk Muslim populace. Albania has been isolated from the outside world for the majority of its record, in the beginning as a result of the physical inaccessibility of its surface and later due to 500 years of profession by the OTTOMAN EMPIRE.<br /><br /> <h3> SECLUSION</h3> Also during the duration of communist policy after The second world war, Albanian leaders pursued their own specific course in spite of stress from its larger neighbors in Yugoslavia as well as the Soviet Union, causing among one of the most isolated nations around the world-- politically, financially, and also culturally. Considering that reforms started in 1990, Albania has struggled to catch up to the remainder of Europe, delaying much behind in political and economic growth.<br /><br />Mostly all of Albania is hilly, from the southern reaches of the Dinaric Alps in the north to the numerous smaller ranges to the eastern as well as southern. These arrays form Albania's boundaries: SERBIA As Well As MONTENEGRO to the north, MACEDONIA (Former Yugoslav Republic of Macedonia) to the east, and also GREECE to the south. Numerous Albanians live across these boundaries, however, mostly in the district of Kosovo to the northeast, but also in Macedonia as well as Greece. The varieties of Albanians residing in these areas is frequently disputed and also is the cause of local stress, as Albanians seek to locate a unified voice on their own throughout the Balkans.<br /><br />The slim coastal plain along the ADRIATIC SEA is the website of Albania's limited agricultural outcome, increasing equipments ideal to a cozy Mediterranean environment: citrus, figs, grapes, olives. The plain is watered by Albania's major rivers, the Drin, Ersenn, and Semani. Higher elevations are suitable for expanding wheat and for often tending lamb and goats. The hills likewise include mineral wealth, but Albania does not have the resources to extract them beneficially. Where the hills meet this level is where the majority of Albania's bigger towns are located, consisting of the capital, Tirana, at the foot of the Dajti Mountains. The other major cities are Shkodra in the much north, Durrës on the coastline, and also Vlora in the much southern, where the hills come right down to the sea. These last three cities, long essential for trade in the Adriatic, were Venetian vendor republics for much of their record, mirrored in their historical names, Scutari, Durazzo, as well as Valona.<br /><br />Today, many Italian impacts are gone, and also these cities are repopulated with ethnic Albanians, a people whose origins are uncertain, however who are believed to be the area's earliest inhabitants, predating the neighbor-ing Slavic individuals by a number of centuries. Their language is thought to be originated from that of the ancient Illyrians, an individuals whose kingdoms once controlled the Balkan Peninsula till they were conquered by the Romans in the 1st century B.C.E., then pushed out of much of their original region by shifting Slavs in the 6th to 8th centuries. A middle ages kingdom was resurrected in the 15th century under Albania's primary nationwide hero, Skanderbeg, winning a noteworthy triumph over the Footrest Turks in 1449. Yet within 40 years, Albania had droppeded to the Ottomans and also had to wait till 1913 to recuperate its political independence.<br /><br />In the meantime, Albania came to be the only European district of the Ottoman Empire where most its residents transformed to Islam, and also Albania contributed significantly to the growth of the Footrest state-- several of its boys increased via the ranks to end up being grand vizier, chief minister of the sultan. After getting freedom, Albania veered from republic to monarchy as well as back prior to submitting completely to the stringent socialist program led for four decades by Enver Hoxha. Throughout this duration, Albania's economic situation was One Hundred Percent nationalized (also individual vehicles were owned by the state), and also diplomatic connections were reduced with all of its former allies, Yugoslavia, the Soviet Union, and also finally, even CHINA, leaving Hoxha's regimen totally separated.<br /><br />From 1992, a new routine and also a brand-new constitution have actually attempted to turn around the mistakes of the past fifty years, but Albania remains the least established country in Europe, with about half of its populace working with tiny farms as well as fifty percent of its sector turned off. Today, much of the national earnings derives from remittances sent back from Albanians functioning abroad, primarily in Greece and also ITALY.<br /><br /><i>BIBLIOGRAPHY. James Pettifer, Albania & Kosovo (A & C Black, 2001); Wayne C. Thompson, Nordic, Central and Southeastern Europe 2003, The World Today Series (Stryker-Post Publications, 2003); World Factbook (CIA,2004).</i>

Albania - The Only European Country Where Muslim is Majority

Courtesy of operationworld.org articlemostwanted - ALBANIA IS UNIQUE in many ways. This small, mountainous country on the western side o...

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Greek Empire Facts

<table align="center" cellpadding="0" cellspacing="0" class="tr-caption-container" style="margin-left: auto; margin-right: auto; text-align: center;"><tbody> <tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjxRuIMlwlgGtQwd1m30NPSxpyZw5ZwboZYYxsP-VOaOuTIwz_YiUAooC_zw5ZbK-_pUd4B3aU7_PXWwGiB9A1vaXif1fqhqJEIYdAw1KWa-jEYMHMUxH_Z6T671hqmCUf6ygTqTC7V0Pw/s1600/30-greek-empire-facts-articlemostwanted.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjxRuIMlwlgGtQwd1m30NPSxpyZw5ZwboZYYxsP-VOaOuTIwz_YiUAooC_zw5ZbK-_pUd4B3aU7_PXWwGiB9A1vaXif1fqhqJEIYdAw1KWa-jEYMHMUxH_Z6T671hqmCUf6ygTqTC7V0Pw/s1600/30-greek-empire-facts-articlemostwanted.jpg" /></a></td></tr> <tr><td class="tr-caption" style="text-align: center;">Courtesy of omgfacts.com</td></tr> </tbody></table> <b>articlemostwanted </b>- Greece is an area on the south of the European landmass. It is described by mountains, enclosed on all parts except the north by the sea, and endowed with big and little islands. The Ionian and AEGEAN SEAs and several bays permitted the Greeks to flourish in maritime trade and to grow a civilization that was motivated from several sources, both external and local. The Greek realm extent far beyond Greece itself, comprising many villages around the Mediterranean and BLACK SEAs. The mountains, which functioned as natural obstacles and borders, imposed the political type of Greece.<br /><br />Starting early of times the Greeks existed in sovereign communities separated from one another by the geography. At the future these communities were formed into CITY-STATES. The mountains stopped large-scale farming and stopped the Greeks to see beyond their limits to new lands where productive soil was more plentiful. The Greeks began to sail the seas to do commerce since very old times and reached the Pillars of Hercules, but the huge movement of growth of Greek people was between the 8th and 7th centuries B.C.E., increasing geographical knowledge. <br /><br />These voyages that arranged the Greek colonization of Mediterranean part were real explorations. The outcome was essential for the knowledge of the whole Mediterranean Sea and Black Sea and the nearby area, into the core mountains of Asia and eastern Africa. <br /><br />The extension of Alexander the Great’s empire started in 336 B.C.E., when he prospered his father to the power of Macedonia. After that, Alexander starting a military expansion with the purpose of winning the Persian area in Asia Minor and make Egypt free, turn out to be the emperor of a new big realm. At its highest extent, this kingdom concealed over 3,000 mi (4,828 km) from Greece to INDIA, surrounding Egypt and Persia, up to the river Indo. The center of this territory was Alexandria in Egypt, founded about 331 B.C.E.<br /><br />Throughout army rallies, country by country, numerous teams of geographers, botanists, and other men of science gathered data and examples for Aristotle, the advisor of Alexander. As a historian saved the documentations of the journey, cartographers created maps that functioned as the foundation for the geography of Asia for decades. To manage his colony, Alexander approved a type of monarchy previously used in the Persian Empire, presenting in his court also some components like uniforms and customs from the Persian civilization. This type of government disagree with the dissimilar populations under Alexander’s power, and they rebelled. <br /><br />Alexander tried to end these turbulences by announcing and inspiring the creation of a hegemony between different persons living in his empire. This plan died with its organizer, Alexander, beginning an age of war between his heirs and marked the starting of the fall of this kingdom. After 40 years of clash, the occupied territory was shared into three regions: Egypt went to the Ptolemys, the kingdom of Syria belong to the Seleucids, and the Antigonids got Macedon. These new realms, so-called Hellenistic, brought the Greek civilization into Asia and Egypt, making times of prosperity for all cheers to a large availability of valuable metals and many kinds of goods, mainly resources from the Persian War. New commerce lines were founded and in Alexandria, the biggest library of the early world was developed. The campaigns of Alexander in Libya and in Asia touched Turkestan and India, revealing many of new huge mountains and big deserts, the great rivers of India, and the Southern Ocean (sailed for the first time by the fleet of Nearco from the Indo to the Euphrates).<br />

Greek Empire Facts

Courtesy of omgfacts.com articlemostwanted - Greece is an area on the south of the European landmass. It is described by mountains, encl...

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Tunisia Economic Outlook 2014

<table align="center" cellpadding="0" cellspacing="0" class="tr-caption-container" style="margin-left: auto; margin-right: auto; text-align: center;"><tbody> <tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgfpZTMxBNCQyN_lXVg83pzL1CXuRSHoBbulk4nzlunT5EvtocieNdxahfYXREulsom6nt14-ZaZMLd1CliGzjdfYvJyxqNP2LdRMU-mxwhugaBxruL8XjLrZNTyRunp1L149_zGEoQu8M/s1600/2-tunisa-economic-outlook-articlemostwanted.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgfpZTMxBNCQyN_lXVg83pzL1CXuRSHoBbulk4nzlunT5EvtocieNdxahfYXREulsom6nt14-ZaZMLd1CliGzjdfYvJyxqNP2LdRMU-mxwhugaBxruL8XjLrZNTyRunp1L149_zGEoQu8M/s1600/2-tunisa-economic-outlook-articlemostwanted.jpg" /></a></td></tr> <tr><td class="tr-caption" style="text-align: center;">Courtesy of www.olympicweddings-greece.com</td></tr> </tbody></table> <b>articlemostwanted </b>- In the situation of a political and security disaster, Tunisia recorded reasonable growth of 2.6% in 2013, degraded from the 2012 level (3.7%).<br />Development is expected to speed up in 2014 and 2015 in the quieter atmosphere brought about by the implementation of a new charter and the establishment of a transitional administration composed of technocrats.<br /><br />Tunisia’s reappearance to tough growth will need a justification of public spending and efficient oversight of the monetary sector, the labor market and asset.<br />Tunisia recorded growth of 2.6% in 2013, under the legitimate forecast (4.5%) and the 2012 level (3.7%). This stoppage can be clarified by political gridlock, the deteriorating of the security condition, a delicate social situation, inactivity in the euro area (the country’s chief client and chief supplier), and a 3.3% weakening in agricultural manufacture.<br /><br />Unanticipated resilience was shown by the key areas of tourism (+2% in hard-currency revenues) and export business (with growth of 6%), assisted by the devaluation of the dinar (10% against the euro, 6.7% against the US dollar). Employment also presented timid development, by the unemployment ratio decreasing to 15.7% in the third quarter of 2013 from 17 % in the similar period a year earlier. Unemployment between young alumni nevertheless remains at an intensely worrisome level (34%, or one out of three), due to a broadening gap among their skills and the needs of industries.<br /><br />The chief macroeconomic pointers deteriorated and social wasting, notably power subsidies, weighed severely on financial balances.<br />Growth is expected to restart in 2014 and 2015, carrying an end to the event of recession that happened in 2011 (-1.8%). And the present account shortfall is expected to reduce in 2014 through economic revival and the return of tourism.<br /><br />Tunisia is traditionally well united into global value chains (GVCs), particularly in three manufacturing sectors: textiles and clothing; agro-business; and the mechanical, electrical and electronics manufacture. The best development took place in the final, cheers to the growth of automotive and aeronautics machineries, by exports continuing by an average 18% per year from 2000 to 2012. Tunisia’s three key business sectors account for 75% of the country’s exporting companies, and in excess of 65% of jobs in industry. Latest activities such as information and communication technologies have established recently, however their incorporation into GVCs has been limited to subcontracting links by limited added value, and they continue focused geographically along the shore. Tunisia’s integration into GVCs is being motivated by free-trade arrangements with the European Union (EU), but it is handicapped by many problems including trade and investment rules, the business weather, logistics, transport, regional inequities, and technology handovers.<br /> <br /> <i>source: afdb</i>

Tunisia Economic Outlook 2014

Courtesy of www.olympicweddings-greece.com articlemostwanted - In the situation of a political and security disaster, Tunisia recorded r...

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Ahaggar Mountains - Montains in the Desert

<div class="separator" style="clear: both; text-align: center;"> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgUXEmdciwh6R88_u9ITR0xJ03rmkOmRHCyei4tvenwYt9yCgLbcnKFFgCvVSY-Up2jV781vTvZ8ccfdFrBRRmI66-1TzHybYMN8VCln5b5g-OREqCjQbTlxXU2zcdx7aHW4EgcURk3-Us/s1600/ahaggar-mountains.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgUXEmdciwh6R88_u9ITR0xJ03rmkOmRHCyei4tvenwYt9yCgLbcnKFFgCvVSY-Up2jV781vTvZ8ccfdFrBRRmI66-1TzHybYMN8VCln5b5g-OREqCjQbTlxXU2zcdx7aHW4EgcURk3-Us/s1600/ahaggar-mountains.jpg" /></a></div> THE AHAGGAR IS a large mountainous plateau region lying on the TROPIC OF CANCER in the north-central SAHARA DESERT. It covers an area of 210,000 square mi(543,900 square km) which is about the size of FRANCE, or of ARIZONA and NEW MEXICO combined. It is about 1,000 mi (1,609 km) east of the ATLANTIC OCEAN, 1,000 mi north of the BIGHT OF BENIN, and 1,000 mi south of the MEDITERRANEAN SEA.<br /> <br /> Most of the Ahaggar lies in southeast ALGERIA about 900 mi (1,450 km) south of Algiers. However, small areas extend into NIGER in the south and LIBYA in the northeast. The Ahaggar is a part of the Mid-Sahara Rise, which stretches 1,300 mi (2,092 km) east to west and 965 mi (1,553 km) south to north. The Mid-Sahara Rise includes the Adrar des Iforhas Mountains in MALI and the Massif de l’Air Mountains in Niger.<br /> <br /> The Sahara lies on the African shield, a thick pre-Cambrian crystalline base. Geological studies have concluded that about 300 million years ago violent earthquakes of enormous proportions pushed up this central massif or plateau region of the Sahara. This was followed by volcanic eruptions that poured enormous beds of basaltic lava over the area.<br /> <br /> The geologic activity underlying the Ahaggar plateau pushed its granite base up thousands of feet above the Sahara. The Ahaggar plateau’s height is above 3,000 ft (915 m). The geologic activity produced enormous cliffs and fissures. These were broken into strange formations. At the heart of the Ahaggar, volcanic eruptions produced pumice and lava beds in many areas, some of which are basaltic. There are also “organ pipes” or volcanic needles or spires of rock that may reach 1,000 ft (305 m) high.<br /> <br /> The Ahaggar Mountain chain, which is also called the Hoggar Mountains, is situated on top of the Ahaggar plateau. The plateau is like a platform covered with lava fields. The Tuaregs call the platform the Atakor, while the Arabs call it the Kudia. The Atakor platform averages 6,600 ft (2,012 m). At the heart of the Ahaggar chain is the Atakor range, which has extinct volcanoes in many places that rise to about 9,000 ft (2,743 m). They rise from the plateau and are the highest portion of the plateau. At the center of the Ahaggar Mountains is the highest peak, Mount Tahat (9,573 feet or 2,918 m). Other peaks include Mount Atakor and Mount Assekrem, which is where the Berber Tuaregs locate the “end of the world.”<br /> <br /> While most of the Ahaggar is waterless and totally bare of vegetation, there are occasional snows. In some places in deep ravines, there are verdant strips that can be seen on aerial photographs. There are two waterfalls in the Ahaggar. One is at Tamekrest and the other is at Imeleoulaouene. A variety of animals live in the mountains along with the nomads, mostly Tuaregs, who frequent the oases located in these rugged reaches.<br /> <br /> <i>BIBLIOGRAPHY. Jeremy Keenan, The Tuareg: People of the Ahagger (Sickle Moon Books, 2002); Louis Carl and Joseph Petit, Mountains in the Desert (Doubleday, 1954); Louis Carl and Joseph Petit, Tefedest: Journey to the Heart of the Sahara (Allen & Unwin, 1954); Claude Blanguernon and Thomas Turner, The Hoggar (Human Relations Area Files, 1970); Douglas Porch, The Conquest of the Sahara (Oxford University Press, 1986). By ANDREW J. WASKEY DALTON STATE COLLEGE</i>

Ahaggar Mountains - Montains in the Desert

THE AHAGGAR IS a large mountainous plateau region lying on the TROPIC OF CANCER in the north-central SAHARA DESERT. It covers an area of 2...

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Afghanistan - ANCIENT LANDS

<div class="separator" style="clear: both; text-align: center;"> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiZTiuEwV56KIV17SXCvqoN_3FOLdTcTcz2oWl-QslsO-eD4cI14itYcUl_lBvt83e9V0JAcjVyjZFrMdWGbgV3w9pEQ1_2E97nev1BFydFtW_EhBfvEFdaQdcWBnDIGHCgoc2SCIXNqxo/s554/afghanistan-ancient-land.jpg" imageanchor="1" style=""><img border="0" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiZTiuEwV56KIV17SXCvqoN_3FOLdTcTcz2oWl-QslsO-eD4cI14itYcUl_lBvt83e9V0JAcjVyjZFrMdWGbgV3w9pEQ1_2E97nev1BFydFtW_EhBfvEFdaQdcWBnDIGHCgoc2SCIXNqxo/s1600/afghanistan-ancient-land.jpg" /></a></div> THE STATE OF AFGHANISTAN is a landlocked country that borders PAKISTAN to the south, IRAN to the west, TURKMENISTAN, UZBEKISTAN, and TAJIKISTAN to the north, and CHINA to the northeast. The country is divided into 32 provinces. Since the overthrow of the Taliban in 2001, Afghanistan is in the process of reconstructing its government.<br /> <br /> Afghanistan, known since ancient times for its lapis mines, is divided by several mountain ranges. Cutting the country in half is the HINDU KUSH, from which smaller ranges project: from the Band-I-Turkestan on the west to the Suleiman Range to the east. To the southeast is the Dasht-I-Margo desert. Afghanistan has a dry climate with hot summers and cold winters. The country experiences sparse rainfall. Its chief rivers are the AMU DARYA, the Kabul, the Helmand, and the Hari Rud. Major cities include Kabul, Kandahar, Herat, Mazar e-Sharif, Jalalabad, and Konduz.<br /> <br /> <h4> ANCIENT LANDS</h4> The region in and around Afghanistan has been inhabited since the Paleolithic and Neolithic eras. Afghanistan has been the scene of migrations throughout history. Since ancient times, Afghanistan captured the interest of foreign peoples. The region of what is now Afghanistan entered into recorded history under the PERSIAN EMPIRE. By 331 B.C.E., Alexander the Great extended his empire into Afghanistan after conquering Persia. Alexander’s empire disintegrated after his death in 323 B.C.E. with Afghanistan passing to Seleucis<br /> Nikator, one of his generals. Afghanistan soon after came under the control of Chandragupta from INDIA. Around 650 C.E., ISLAM came to Afghanistan through Arabs who conquered the Sassanids in Persia. In 1219, the Mongols under Genghis Khan spread destruction throughout Afghanistan. For 500 years, Afghanistan was part of the power plays between the Mughals in India and the Safavids in Persia. In the 18th century, Afghanistan was united for the first time under Ahmed Shah Durrani, who created an empire that included modern-day Pakistan.<br /> <br /> By the 19th century, Afghanistan was caught in the middle of the imperial ambitions of Britain, which had controlling interests in India and RUSSIA. Britain fought two wars to gain control of Afghanistan, both of which ended disastrously. In the 20th century, Afghanistan entered a period of modernization through King Amanullah between 1919 and 1929. In 1933, King Mohammad Zahir Shah extended the modernization through the creation of a constitution and a parliament. However, by the 1960s, the communists had gained a foothold in Afghan politics, and by 1973, Sardar Mohammad Daoud abolished the monarchy and established a republic with financial backing from the Soviet Union.<br /> <br /> In 1979, the Soviet Union invaded Afghanistan to support a communist government under the Najibullah regime. Soviet occupation was met by fierce resistance by the Mujahideen, who were mainly supported by the United States. In 1989, the Soviets withdrew from Afghanistan, prompting civil war among the Mujahideen. By 1996, Afghanistan fell under the rule of the Taliban, a fanatical extremist Muslim sect. The Taliban imposed Sharia law as the legal system for Afghanistan and severely restricted women’s rights. Additionally, Afghanistan became a breeding ground for international terrorism, harboring Osama bin Laden, leader of the al Qaeda terrorist group that masterminded the attacks in New York City and Washington, D.C., on September 11, 2001.<br /> <br /> In November of that year, the United States led a coalition of nations to overthrow the Taliban regime, when it would not surrender bin Laden. The Taliban offered no significant resistance and retreated to the mountains. At the end of 2001, an agreement was reached in Bonn, Germany, to lay out a blueprint for Afghanistan’s reconstruction.<br /> <br /> Afghanistan has a diverse array of ethnic groups. The Pashtun are the majority ethnic group, followed by Tajiks, Uzbeks, Hazara, Aimaq, Turkmen, Baluch, and Nuristani. Pashto and Dari are the main languages spoken. Twenty years of war have left Afghanistan’s infrastructure in ruins. Agriculture makes up 60 percent of the economy. Afghanistan is one of the leading exporters of opium, which is most profitable for farmers to grow.<br /> <br /> <i>BIBLIOGRAPHY. Sir Martin Ewans, Afghanistan: A Short History of Its People and Politics (First Perennial, 2002); Cary Gladstone, Afghanistan: History, Issues, Bibliography (Novinka Books, 2001); World Factbook (CIA, 2003).</i>

Afghanistan - ANCIENT LANDS

THE STATE OF AFGHANISTAN is a landlocked country that borders PAKISTAN to the south, IRAN to the west, TURKMENISTAN, UZBEKISTAN, and TAJIK...

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Adriatic Sea

<div class="separator" style="clear: both; text-align: center;"> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhnakCAAmIlf9tX4_eaowe_sNOfFn68J1jPr0Mzbk_vAHKM8z-YTF5145JVLsQ2Dg49arMCvZUD1SmciQZv1Yau1itwudOLLvK3QY_6V5dYRATpcDzS00Kfy0Zexz1EnVfGx3qvS6dxO0I/s1600/adriatic-sea-1.jpg" imageanchor="1" style=""><img border="0" height="201" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhnakCAAmIlf9tX4_eaowe_sNOfFn68J1jPr0Mzbk_vAHKM8z-YTF5145JVLsQ2Dg49arMCvZUD1SmciQZv1Yau1itwudOLLvK3QY_6V5dYRATpcDzS00Kfy0Zexz1EnVfGx3qvS6dxO0I/s280/adriatic-sea-1.jpg" width="280" /></a></div> <div style="text-align: justify;"> <a href="http://www.articlemostwanted.com/2013/04/adriatic-sea.html"><br /></a></div> <div style="text-align: justify;"> <b><a href="http://www.articlemostwanted.com/2013/04/adriatic-sea.html">THE ADRIATIC SEA</a> (in Italian “Mar Adriatico,” inSerbian “Jadransko more”) is a northwest-to-southeast arm of the MEDITERRANEAN SEA.</b> The sea separates the Italian peninsula from the Austro-Hungarian, Montenegrin, and Albanian littorals, and the Italian Apennine Mountains from the Balkan Dinaric Alps. The western coast is Italian and the eastern comprises slovenia, croatia, bosnia and herzegovina, serbia and montenegro, and albania. The name derives from the Italian town of Adria (Hadria), designating in early historic times the sea’s upper portion. The term was later extended geographically to the south.</div> <div style="text-align: justify;"> <br /></div> <div style="text-align: justify;"> The Adriatic has a total surface area of about 60,000 square mi (160,000 square km), with a maximum  length of about 480 mi (770 km) and a width of nearly 100 mi (160 km); however, the Strait of Otranto, connecting the Adriatic and the Ionian Sea to the south, is 45 mi (72 km) in breadth. The mean depth is 133 fathoms (240 m), but the northern portion ofthe Adriatic is shallowest between the southern promontory of Istria and Rimini (about 25 fathoms or 46 m), where the low Italian littoral merges in the northwest into marshes and lagoons along the delta of the Po River. The freshwater Po and Adige are the major rivers flowing into the saline Adriatic and account for substantial silting. The Po’s sediment extended the coastline for 2 mi or 3.2 km within the last two millennia.</div> <div style="text-align: justify;"> <br /></div> <div class="separator" style="clear: both; text-align: center;"> <a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhX04aLpGUFL4FNcm32E7fj_yyNvJ900KUb61P-DfrcCPYT9GYnVKHwZfKlOyHS5l28Vo89dsOogMdqjvk25h-VsOABK5T5x8maQBtk1o_loQLz_EWVPRUajtqu6Ljhx6rP0MTzDzuVil0/s1600/adriatic-sea-2.jpg" imageanchor="1" style=""><img border="0" height="210" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhX04aLpGUFL4FNcm32E7fj_yyNvJ900KUb61P-DfrcCPYT9GYnVKHwZfKlOyHS5l28Vo89dsOogMdqjvk25h-VsOABK5T5x8maQBtk1o_loQLz_EWVPRUajtqu6Ljhx6rP0MTzDzuVil0/s280/adriatic-sea-2.jpg" width="280" /></a></div> <div style="text-align: justify;"> <br /></div> <div style="text-align: justify;"> The area between Šibenik and Ortona (Croatia and ITALY) exceeds 100 fathoms (180 m) in depth, but west of Durrës (Albania) and south of Dubrovnik (Croatia), the basin exceeds 500 fathoms (900 m). The rocky east coast has many long and narrow islands with the long axes lying parallel to the mainland coast and elevations of a few hundred feet; larger islands such as Brac have elevations of 2,552 ft (778 m). There are <a href="http://www.articlemostwanted.com/2013/04/adriatic-sea.html">more than 1,000 islands in the Adriatic Sea</a>, although only 66 are inhabited, notably near Venice (Italy), and Trieste (Italy). Due to eutrophication and minimal tidal flow, making the sea a shallow, closed system, the Adriatic has notable water and air pollution yet remains an important tourism and fishing locale.</div> <div style="text-align: justify;"> <br /></div> <div style="text-align: justify;"> <i>BIBLIOGRAPHY. Pierre Cabanes, Histoire de l’Adriatique (Seuil, 2001); Harry Hodgkinson, The Adriatic Sea (Cape, 1955); Andrew Paton, Highlands and Islands of the Adriatic (Chapman and Hall, 1849); Eugenio Turri, Adriatico mare d’Europa: La geografia e la storia (Rolo Banca, 1999).</i></div>

Adriatic Sea

THE ADRIATIC SEA (in Italian “Mar Adriatico,” inSerbian “Jadransko more”) is a northwest-to-southeast arm of the MEDITERRANEAN SEA. T...

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