{"id":1579,"date":"2024-02-17T21:06:44","date_gmt":"2024-02-17T20:06:44","guid":{"rendered":"https:\/\/bestfreetour.com\/?page_id=1579"},"modified":"2024-02-17T21:06:46","modified_gmt":"2024-02-17T20:06:46","slug":"slovenia","status":"publish","type":"page","link":"https:\/\/bestfreetour.com\/zh\/slovenia\/","title":{"rendered":"Slovenia"},"content":{"rendered":"\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"576\" src=\"https:\/\/bestfreetour.com\/wp-content\/uploads\/2024\/02\/Slovenia-johnny-africa-z5xyqSYE8pE-unsplash-1024x576.jpg\" alt=\"\" class=\"wp-image-1580\" srcset=\"https:\/\/bestfreetour.com\/wp-content\/uploads\/2024\/02\/Slovenia-johnny-africa-z5xyqSYE8pE-unsplash-1024x576.jpg 1024w, https:\/\/bestfreetour.com\/wp-content\/uploads\/2024\/02\/Slovenia-johnny-africa-z5xyqSYE8pE-unsplash-300x169.jpg 300w, https:\/\/bestfreetour.com\/wp-content\/uploads\/2024\/02\/Slovenia-johnny-africa-z5xyqSYE8pE-unsplash-768x432.jpg 768w, https:\/\/bestfreetour.com\/wp-content\/uploads\/2024\/02\/Slovenia-johnny-africa-z5xyqSYE8pE-unsplash-1536x864.jpg 1536w, https:\/\/bestfreetour.com\/wp-content\/uploads\/2024\/02\/Slovenia-johnny-africa-z5xyqSYE8pE-unsplash-2048x1152.jpg 2048w, https:\/\/bestfreetour.com\/wp-content\/uploads\/2024\/02\/Slovenia-johnny-africa-z5xyqSYE8pE-unsplash-107x60.jpg 107w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>\n\n\n\n<p class=\"has-pale-pink-color has-text-color has-link-color wp-elements-11c2d44ac52a5379e3fa9a1e6b48a786 wp-block-paragraph\"><strong>Slovenia Free Tour<\/strong><\/p>\n\n\n\n<p class=\"has-pale-pink-color has-text-color has-link-color wp-elements-21d56cc581a88e1d75934ff74cbf4385 wp-block-paragraph\"><strong>Ajdovscina Free Tour<\/strong><\/p>\n\n\n\n<p class=\"has-pale-pink-color has-text-color has-link-color wp-elements-c5e919295fc90fdd456545453dce273e wp-block-paragraph\"><strong>Ljubljana Free Tour<\/strong><\/p>\n\n\n\n<p class=\"has-pale-pink-color has-text-color has-link-color wp-elements-aadc5b21e81367b10ac29ed25a378ce9 wp-block-paragraph\"><strong>Bled Free Tour<\/strong><\/p>\n\n\n\n<p class=\"has-pale-pink-color has-text-color has-link-color wp-elements-811c4e70355d027095c9aa3b3b8f375c wp-block-paragraph\"><strong>Portoroz Free Tour<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Information:<\/strong><\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Slovenia<\/strong>, <a href=\"https:\/\/www.britannica.com\/topic\/nation-state\">country<\/a> in central <a href=\"https:\/\/www.britannica.com\/place\/Europe\">Europe<\/a> that was part of <a href=\"https:\/\/www.britannica.com\/place\/Yugoslavia-former-federated-nation-1929-2003\">Yugoslavia<\/a> for most of the 20th century. Slovenia is a small but topographically <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/diverse\">diverse<\/a> country made up of portions of four major European geographic landscapes\u2014the <a href=\"https:\/\/www.britannica.com\/place\/Alps\">European Alps<\/a>, the karstic <a href=\"https:\/\/www.britannica.com\/place\/Dinaric-Alps\">Dinaric Alps<\/a>, the Pannonian and Danubian lowlands and hills, and the Mediterranean coast. Easily accessible mountain passes (now superseded by tunnels) through Slovenia\u2019s present-day territory have long served as routes for those crossing the Mediterranean and transalpine regions of Europe.<\/p>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/cdn.britannica.com\/57\/183757-050-85F5A0EE\/World-Data-Locator-Map-Slovenia.jpg\"><img decoding=\"async\" src=\"https:\/\/cdn.britannica.com\/57\/183757-050-85F5A0EE\/World-Data-Locator-Map-Slovenia.jpg\" alt=\"Slovenia\"\/><\/a><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/cdn.britannica.com\/57\/183757-050-85F5A0EE\/World-Data-Locator-Map-Slovenia.jpg\">Slovenia<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The Slovenes are a South Slavic people with a unique <a href=\"https:\/\/www.britannica.com\/topic\/Slovene-language\">language<\/a>. For most of its history, Slovenia was largely controlled by the <a href=\"https:\/\/www.britannica.com\/topic\/House-of-Habsburg\">Habsburgs<\/a> of <a href=\"https:\/\/www.britannica.com\/place\/Austria\">Austria<\/a>, who ruled the <a href=\"https:\/\/www.britannica.com\/place\/Holy-Roman-Empire\">Holy Roman Empire<\/a> and its successor states, the Austrian Empire and Austria-Hungary; in addition, coastal portions were held for a time by <a href=\"https:\/\/www.britannica.com\/place\/Venice\">Venice<\/a>. As part of Yugoslavia, Slovenia came under communist rule for the bulk of the post-<a href=\"https:\/\/www.britannica.com\/event\/World-War-II\">World War II<\/a> period. With the dissolution of the Yugoslav federation in 1991, a multiparty democratic <a href=\"https:\/\/www.britannica.com\/topic\/political-system\">political system<\/a> emerged. Slovenia\u2019s economic prosperity in the late 20th century attracted hundreds of thousands of migrants from elsewhere in the <a href=\"https:\/\/www.britannica.com\/place\/Balkans\">Balkans<\/a>. In the early 21st century, Slovenia <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/integrated\">integrated<\/a> economically and politically with western Europe, joining the <a href=\"https:\/\/www.britannica.com\/topic\/North-Atlantic-Treaty-Organization\">North Atlantic Treaty Organization<\/a> as well as the <a href=\"https:\/\/www.britannica.com\/topic\/European-Union\">European Union<\/a> in 2004. Slovenia\u2019s capital and most important city is <a href=\"https:\/\/www.britannica.com\/place\/Ljubljana\">Ljubljana<\/a>.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Land<\/h2>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"https:\/\/cdn.britannica.com\/36\/6236-050-4D66A23E\/Slovenia-map-features-locator.jpg\"><img decoding=\"async\" src=\"https:\/\/cdn.britannica.com\/36\/6236-050-4D66A23E\/Slovenia-map-features-locator.jpg\" alt=\"Slovenia. Physical features map. Includes locator.\"\/><\/a><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">Slovenia is bordered by <a href=\"https:\/\/www.britannica.com\/place\/Austria\">Austria<\/a> to the north and <a href=\"https:\/\/www.britannica.com\/place\/Hungary\">Hungary<\/a> to the far northeast. To the east, southeast, and south, Slovenia shares a 416-mile- (670-km-) long border with <a href=\"https:\/\/www.britannica.com\/place\/Croatia\">Croatia<\/a>. To the southwest Slovenia is <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/adjacent\">adjacent<\/a> to the Italian port city of <a href=\"https:\/\/www.britannica.com\/technology\/Trieste-bathyscaphe\">Trieste<\/a> and occupies a portion of the Istrian Peninsula, where it has an important coastline along the <a href=\"https:\/\/www.britannica.com\/place\/Gulf-of-Venice\">Gulf of Venice<\/a>. <a href=\"https:\/\/www.britannica.com\/place\/Italy\">Italy\u2019s<\/a> <a href=\"https:\/\/www.britannica.com\/place\/Friuli-Venezia-Giulia\">Friuli-Venezia Giulia<\/a> region is situated to the west.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Britannica Quiz<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Passport to Europe<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Relief<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/cdn.britannica.com\/65\/114565-050-134DC1B3\/Julian-Alps-Slovenia.jpg\">Julian Alps<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The Julian Alps, Slovenia.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">In Slovenia four main physiographic regions can be distinguished. The first is the Alpine region, which takes up about two-fifths of Slovenia\u2019s surface area. In the north and northwest, along the borders with Italy and Austria, are the High Alps, <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/comprising\">comprising<\/a> the Kamnik and Savinja, the Karavanke (<a href=\"https:\/\/www.britannica.com\/place\/Karawanken\">Karawanken<\/a>), and the <a href=\"https:\/\/www.britannica.com\/place\/Julian-Alps\">Julian Alps<\/a>; the latter includes Slovenia\u2019s highest peak, Mount <a href=\"https:\/\/www.britannica.com\/place\/Triglav\">Triglav<\/a>, at 9,396 feet (2,864 metres). In a vale beneath Triglav lie <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/idyllic\">idyllic<\/a> Lake Bohinj and <a href=\"https:\/\/www.britannica.com\/place\/Lake-Bled\">Lake Bled<\/a>. Slightly lower than the High Alps is the subalpine \u201cridge-and-valley\u201d terrain. The main subalpine range is the Pohorje, located south of the <a href=\"https:\/\/www.britannica.com\/place\/Drava-River\">Drava River<\/a>. The historical name for the central Alpine lands is Gorenjska (Upper <a href=\"https:\/\/www.britannica.com\/place\/Carniola\">Carniola<\/a>), a name that Slovenes still use. Slovenes refer to the Mea and Mislinja river valleys as Koro\u0161ka (Carinthia). On Gorenjska\u2019s southern edge is the spacious Ljubljana basin, which contains the capital as well as the industrial city of Kranj.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Slovenia\u2019s second major physiographic region, the <a href=\"https:\/\/www.britannica.com\/place\/Karst-region-Europe\">Kras<\/a> (Karst), a spur of the lengthy <a href=\"https:\/\/www.britannica.com\/place\/Dinaric-Alps\">Dinaric Alps<\/a> in the southwestern part of the country, is dotted with caves and underground rivers, the characteristic features of <a href=\"https:\/\/www.britannica.com\/science\/karst-geology\">karst<\/a> <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/topography\">topography<\/a> (whose term is derived from the name of the region). Although it <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/constitutes\">constitutes<\/a> one-fourth of Slovenia\u2019s area, the Kras region has only a fraction of the country\u2019s population, which is concentrated between the wooded limestone ridges in dry and blind valleys, hollows, and poljes. Water is scarce in this region. The Suha Krajina is a karstified plateau; the Bela Krajina is a transitional belt that contains plains and points toward the Subpannonia (Pannonian Plain). Most of the region is known to Slovenes by its historical names: Dolenjska (Lower Carniola) and Notranjska (Inner Carniola). Scientific study of karst terrain is a Slovene specialty, research having begun during the 18th century in Habsburg Carniola.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/premium.britannica.com\/student-subscription\/?utm_source=inline&amp;utm_medium=mendel&amp;utm_campaign=student-subscription-a\"><\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Students save 67%! Learn more about our special academic rate today.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The next largest physiographic region (occupying one-fifth of the country) is the fertile Subpannonia; it is located in eastern and northeastern Slovenia and includes the valleys of the <a href=\"https:\/\/www.britannica.com\/place\/Sava-River\">Sava<\/a>, <a href=\"https:\/\/www.britannica.com\/place\/Drava-River\">Drava<\/a>, and <a href=\"https:\/\/www.britannica.com\/topic\/Mura\">Mura<\/a> rivers. Its <a href=\"https:\/\/www.britannica.com\/dictionary\/basins\">basins<\/a> contain the cities of <a href=\"https:\/\/www.britannica.com\/place\/Maribor\">Maribor<\/a> (on the Drava) and <a href=\"https:\/\/www.britannica.com\/place\/Celje\">Celje<\/a> (on the Savinja River, a tributary of the Sava). Subpannonia corresponds in part to the lower part of the old Austrian duchy of Styria; Slovenes call their portion \u0160tajerska and share some traits with their Austrian neighbours. Beyond a saddle of hills known as the Slovenske Gorice is <a href=\"https:\/\/www.britannica.com\/place\/Prekmurje\">Prekmurje<\/a>, a wheat-growing region drained by the Mura River in the extreme northeast of the country. It was ruled by Hungary until 1918; its main town is Murska Sobota.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The fourth principal region (occupying barely one-twelfth of Slovenia\u2019s surface) is Primorska, or the Slovene Littoral. It overlaps what were the Habsburg regions of <a href=\"https:\/\/www.britannica.com\/place\/Trieste-Italy\">Trieste<\/a> and <a href=\"https:\/\/www.britannica.com\/place\/Gorizia\">Gorizia<\/a> and is made up of Slovenia\u2019s portion of the <a href=\"https:\/\/www.britannica.com\/place\/Istria\">Istrian<\/a> Peninsula, the Adriatic <a href=\"https:\/\/www.britannica.com\/dictionary\/hinterland\">hinterland<\/a>, and the So\u010da and Vipava river valleys. The 29-mile (47-km) strip of coast makes up Slovenia\u2019s riviera. The city of <a href=\"https:\/\/www.britannica.com\/place\/Koper\">Koper<\/a> (just south of Trieste) is Slovenia\u2019s major port.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Drainage<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\"><a href=\"https:\/\/cdn.britannica.com\/79\/114579-050-758502AD\/Drava-River-Maribor-Slovenia.jpg\">Drava River<\/a><\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The Drava River at Maribor, Slovenia.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Most of Slovenia\u2019s intricate fluvial network is directed toward the <a href=\"https:\/\/www.britannica.com\/place\/Danube-River\">Danube River<\/a>. The <a href=\"https:\/\/www.britannica.com\/place\/Sava-River\">Sava<\/a> originates in the <a href=\"https:\/\/www.britannica.com\/place\/Julian-Alps\">Julian Alps<\/a> and flows past Ljubljana toward Croatia; its narrow valley serves as a rail <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/conduit\">conduit<\/a> to <a href=\"https:\/\/www.britannica.com\/place\/Zagreb\">Zagreb<\/a>, Croatia\u2019s capital, and farther to <a href=\"https:\/\/www.britannica.com\/place\/Belgrade\">Belgrade<\/a>, <a href=\"https:\/\/www.britannica.com\/place\/Serbia\">Serbia\u2019s<\/a> capital. The <a href=\"https:\/\/www.britannica.com\/place\/Drava-River\">Drava<\/a> enters Slovenia from the Austrian state of <a href=\"https:\/\/www.britannica.com\/place\/Karnten\">K\u00e4rnten<\/a>, and the Mura emerges from the Austrian state of <a href=\"https:\/\/www.britannica.com\/place\/Steiermark\">Steiermark<\/a>; they meet in Croatia and, like the Sava, ultimately reach the Danube. In the west the <a href=\"https:\/\/www.britannica.com\/place\/Soca-river-Europe\">So\u010da<\/a> originates beneath Mount Triglav and, after a precipitous course, reaches the Gulf of Venice in Italian territory.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">The relatively steep gradients of Slovenia\u2019s topography create fast runoff, which in turn ensures most of Slovenia <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/copious\">copious<\/a> water and hydroelectric resources. On the other hand, it also washes away valuable soil nutrients. Pollution of the rivers remains a problem.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Soils<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Slovenia\u2019s complex geology has created a pedological mosaic. The small, thick Pleistocene cover is acidic and viscid. Permeable thin brown podzols\u2014cambisols and fluvisols\u2014are productive if fertilized, but they cover only about one-tenth of its surface, chiefly to the northeast. The carbonate bedrock underlying much of the country produces thin lithosols suited to forest growth. There are many good alluvial soils (particularly in Subpannonia) as well as bog varieties. Karstic sinkholes and poljes are famous for having <a href=\"https:\/\/www.britannica.com\/science\/terra-rossa\">terra rossa<\/a>, a <a href=\"https:\/\/www.britannica.com\/science\/red-soil\">red soil<\/a> produced by the <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/degradation\">degradation<\/a> of the underlying limestone.<\/p>\n\n\n\n<h1 class=\"wp-block-heading\">Climate of Slovenia<\/h1>\n\n\n\n<p class=\"wp-block-paragraph\">Slovenia may be divided into three climatic zones. Conditions in <a href=\"https:\/\/www.britannica.com\/place\/Istria\">Istria<\/a> indicate a transition from the <a href=\"https:\/\/www.britannica.com\/science\/Mediterranean-climate\">Mediterranean climate<\/a> of the Dalmatian coast to a moderate continental climate. In the moderate zone the highest monthly precipitation (up to 15 inches [381 mm]) occurs in spring and autumn, and the highest temperatures (often rising above 80 \u00b0F [27 \u00b0C]) occur in June and July. Winter temperatures rarely drop below 50 \u00b0F (10 \u00b0C), but this mildness is sometimes interrupted by the strong <a href=\"https:\/\/www.britannica.com\/science\/bora\">bora<\/a>, a cold northerly wind.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Central and northern Slovenia have a continental \u201ccool summer\u201d climate; the eastern third of the <a href=\"https:\/\/www.britannica.com\/topic\/nation-state\">country<\/a> also falls into the continental category but has warm summers. Monthly summer rainfall in the cool belt is more than 3 inches (80 mm), and high temperatures average in the upper 60s F (about 20 \u00b0C), although there are uncomfortable hot spells. The east and northeast have much less overall precipitation, and midsummer highs reach well past 70 \u00b0F (21 \u00b0C). From November to February, temperature readings below freezing occur frequently, but snow cover has become less frequent and usually melts rapidly.<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Plant and animal life<\/h2>\n\n\n\n<p class=\"wp-block-paragraph\">Slovenia\u2019s flora reflects the country\u2019s physiographic <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/diversity\">diversity<\/a>, especially its varying elevations. At the highest elevations below the tree line, junipers alternate with high meadowland. Lower is a central belt of coniferous and deciduous trees (birch and beech) mixed with pasturage and arable lands, and, still lower, deciduous growth including karstic heath and maquis (good for rough grazing) is found. At <a href=\"https:\/\/www.britannica.com\/science\/sea-level\">sea level<\/a> along the Slovene Littoral is a typically Mediterranean cover of brushwood, including maquis. Fruit and vegetable areas are scattered about the country, and forests, which are noted for their mushrooms, cover about three-fifths of the terrain.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Several animal species have been given protected status. Along with others of direct economic importance, they include the reintroduced (though still rare) ibex, the European <a href=\"https:\/\/www.britannica.com\/animal\/brown-bear\">brown bear<\/a>, the chamois, the wild boar, and red, fallow, and <a href=\"https:\/\/www.britannica.com\/animal\/roe-deer\">roe deer<\/a> as well as standard varieties of small game. The lynx has reappeared. The Subpannonian habitat suits migratory fowl and upland birds, and the <a href=\"https:\/\/www.britannica.com\/animal\/trout\">trout<\/a> and grayling found in the So\u010da River are renowned among sport anglers. The Adriatic waters off Slovenia\u2019s coast are not an especially favourable <a href=\"https:\/\/www.merriam-webster.com\/dictionary\/environment\">environment<\/a> for fish.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">All information come from <a href=\"http:\/\/Netherlands, country located in northwestern Europe, also known as Holland. \u201cNetherlands\u201d means low-lying country; the name Holland (from Houtland, or \u201cWooded Land\u201d) was originally given to one of the medieval cores of what later became the modern state and is still used for 2 of its 12 provinces (Noord-Holland and Zuid-Holland). A parliamentary democracy under a constitutional monarch, the kingdom includes its former colonies in the Lesser Antilles: Aruba, Bonaire, Cura\u00e7ao, Saba, Sint Eustatius, and Sint Maarten. The capital is Amsterdam and the seat of government The Hague. Netherlands Netherlands Explore Holland's population, waterways, and vast tulip cross-breeding and cultivation program Explore Holland's population, waterways, and vast tulip cross-breeding and cultivation program Learn about the geography, agriculture, and commerce of The Netherlands. See all videos for this article  The country is indeed low-lying and remarkably flat, with large expanses of lakes, rivers, and canals. Some 2,500 square miles (6,500 square km) of the Netherlands consist of reclaimed land, the result of a process of careful water management dating back to medieval times. Along the coasts, land was reclaimed from the sea, and, in the interior, lakes and marshes were drained, especially alongside the many rivers. All this new land was turned into polders, usually surrounded by dikes. Initially, man power and horsepower were used to drain the land, but they were later replaced by windmills, such as the mill network at Kinderdijk-Elshout, now a UNESCO World Heritage site. The largest water-control schemes were carried out in the second half of the 19th century and in the 20th century, when steam pumps and, later, electric or diesel pumps came into use. Exploring Amsterdam: Canals, design, and museums Exploring Amsterdam: Canals, design, and museums Overview of Amsterdam. See all videos for this article  Despite government-encouraged emigration after World War II, which prompted some 500,000 persons to leave the country, the Netherlands is today one of the world\u2019s most densely populated countries. Although the population as a whole is \u201cgraying\u201d rapidly, with a high percentage over age 65, Amsterdam has remained one of the liveliest centres of international youth culture. There, perhaps more than anywhere else in the country, the Dutch tradition of social tolerance is readily encountered. Prostitution, \u201csoft-drug\u201d (marijuana and hashish) use, and euthanasia are all legal but carefully regulated in the Netherlands, which was also the first country to legalize same-sex marriage.  This relative independence of outlook was evident as early as the 16th and 17th centuries, when the Dutch rejected monarchical controls and took a relatively enlightened view of other cultures, especially when they brought wealth and capital to the country\u2019s trading centres. In that period Dutch merchant ships sailed the world and helped lay the foundations of a great trading country characterized by a vigorous spirit of enterprise. In later centuries, the Netherlands continued to have one of the most advanced economies in the world, despite the country\u2019s modest size. The Dutch economy is open and generally internationalist in outlook. With Belgium and Luxembourg, the Netherlands is a member of the Benelux economic union, which in the 1950s and 1960s served as a model for the larger European Economic Community (EEC; now embedded in the European Union [EU]), of which the Benelux countries are members. The Netherlands is also a member of the North Atlantic Treaty Organization (NATO) and the Organisation for Economic Co-operation and Development (OECD), and it plays host to a number of international organizations, especially in the legal sector, such as the International Court of Justice. Brown globe on antique map. Brown world on vintage map. North America. Green globe. Hompepage blog 2009, history and society, geography and travel, explore discovery Britannica Quiz Countries &amp; Their Features  The Dutch reputation for tolerance was tested in the late 20th and early 21st centuries, when an increase in immigration from non-European Union countries and a populist turn in politics resulted in growing nationalism and even xenophobia, marked by two race-related political assassinations, in 2002 and 2004, and the government\u2019s requirement that immigrants pass an expensive \u2018\u2018integration\u2019\u2019 test before they enter the country. Land Relief Netherlands Netherlands Urk, Netherlands Urk, Netherlands Urk, once an island of the former Zuiderzee, now part of the North East (Noordoost) Polder, Netherlands.  The Netherlands is bounded by the North Sea to the north and west, Germany to the east, and Belgium to the south. If the Netherlands were to lose the protection of its dunes and dikes, the most densely populated part of the country would be inundated (largely by the sea but also in part by the rivers). This highly developed part of the Netherlands, which generally does not lie higher than about three feet (one metre) above sea level, covers more than half the total area of the country. About half of this area (more than one-fourth of the total area of the country) actually lies below sea level. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now  The lower area consists mainly of polders, where the landscape not only lies at a very low elevation but is also very flat in appearance. On such land, building is possible only on \u201crafts,\u201d or after concrete piles, sometimes as long as 65 feet (20 metres), have been driven into the silt layer.  In the other, higher area, the layers of sand and gravel in the eastern part of the country were pushed sideways and upward in some places by ice tongues of the Saale Glacial Stage, forming elongated ridges that may reach a height of more than 330 feet (100 metres) and are the principal feature of the Hoge Park Veluwe National Park. The only part of the country where elevations exceed 350 feet (105 metres) is the border zone of the Ardennes. The Netherlands\u2019 highest point, the Vaalserberg, in the extreme southeastern corner, rises to 1,053 feet (321 metres). Drainage and dikes north dam across the IJsselmeer north dam across the IJsselmeer Part of the north dam (the Afsluitdijk) across the IJsselmeer, Netherlands.  The Zuiderzee was originally an estuary of the Rhine River. By natural action it then became a shallow inland sea, biting deep into the land, and eventually it was hollowed into an almost circular shape by the action of winds and tides. In 1920 work was begun on the Zuiderzee project, of which the IJsselmeer Dam (Afsluitdijk), begun in 1927, was a part. This 19-mile- (30-km-) long dam was completed in 1932 to finally seal off the Zuiderzee from the Waddenzee and the North Sea. In the IJsselmeer, or IJssel Lake, formed from the southern part of the Zuiderzee, four large polders, the IJsselmeer Polders, with a total area of about 650 square miles (1,700 square km), were constructed around a freshwater basin fed by the IJssel and other rivers and linked with the sea by sluices and locks in the barrier dam.  The first two polders created there\u2014Wieringermeer and North East (Noordoost) Polder, drained before and during World War II\u2014are used mostly for agriculture. The two polders reclaimed in the 1950s and \u201960s\u2014South Flevoland Polder (Zuidelijk) and East Flevoland Polder (Oostelijk)\u2014are used for residential, industrial, and recreational purposes. Among the cities that have developed there are Lelystad and Almere. Netherlands: Delta Works flood-control project Netherlands: Delta Works flood-control project Learn about flood control in the Netherlands. See all videos for this article  In the southwest, the disastrous gales and spring tide of February 1, 1953, which flooded some 400,000 acres (162,000 hectares) of land and killed 1,800 people, accelerated the implementation of the Delta Project, which aimed to close off most of the sea inlets of the southwestern delta. These delta works were designed to shorten the coastline by 450 miles (725 km), combat the salination of the soil, and allow the development of the area through roads that were constructed over 10 dams and 2 bridges built between 1960 and 1987. The largest of these dams, crossing the five-mile- (eight-km-) wide Eastern Schelde (Oosterschelde) estuary, has been built in the form of a storm-surge barrier incorporating dozens of openings that can be closed in the event of flood. The barrier is normally open, allowing salt water to enter the estuary and about three-fourths of the tidal movement to be maintained, limiting damage to the natural environment in the Eastern Schelde. In the interest of the commerce of the ports of Rotterdam and Antwerp, no dams were constructed in the New Waterway, which links Rotterdam to the North Sea, or the West Schelde, an approach to Antwerp, Belgium. The dikes along these waterways consequently had to be strengthened.  A region with a very specific character has been formed by the great rivers\u2014Rhine, Lek, Waal, and Maas (Meuse)\u2014that flow from east to west through the central part of the country. The landscape in this area is characterized by high dikes along wide rivers, orchards along the levees formed by the rivers, and numerous large bridges over which pass the roads and railways that connect the central Netherlands with the southern provinces. Soils Keukenhof Gardens Keukenhof Gardens Keukenhof Gardens, near Lisse, Netherlands.  In the late Pleistocene Epoch (from about 126,000 to 11,700 years ago), the Scandinavian ice sheet covered the northern half of the Netherlands. After this period, a large area in the north of what is now the Netherlands was left covered by moraine (glacial accumulation of earth and rock debris). In the centre and south, the Rhine and Maas rivers unloaded thick layers of silt and gravel transported from the European mountain chains. Later, during the Holocene Epoch (i.e., the past 11,700 years), clay was deposited in the sheltered lagoons behind the coastal dunes, and peat soil often subsequently developed in these areas. If the peat soil was washed away by the sea or dug away by humans (for the production of fuel and salt), lakes were created. Many of these were reclaimed in later centuries (as mentioned above), while others now form highly valued outdoor recreational areas. Climate  The climate of the Netherlands is temperate, with gentle winters, cool summers, and rainfall in every season. Southerly and westerly winds predominate, and the sea moderates the climate through onshore winds and the effect of the Gulf Stream. Koninck, Philips: View over a Flat Landscape Koninck, Philips: View over a Flat Landscape View over a Flat Landscape, oil on canvas by Philips Koninck, 1664; in the Museum Boymans-van Beuningen, Rotterdam, Netherlands.  The position of the country\u2014between the area of high-pressure air masses centred on the Azores and the low-pressure region centred on Iceland\u2014makes the Netherlands an area of collision between warm and polar air masses, thus creating unsettled weather. Winds meet with little resistance over the flat country, though the hills in the south significantly diminish the velocity of the potent wind that prevails along the coast. On average, frost occurs 60 days per year. July temperatures average about 63 \u00b0F (17 \u00b0C), and those of January average 35 \u00b0F (2 \u00b0C). Annual rainfall averages about 31 inches (790 mm), with only about 25 clear days per year. The average rainfall is highest in summer (August) and autumn and lowest in springtime. The country is known\u2014not least through the magnificent landscapes of Dutch painters\u2014for its heavy clouds, and on an average day three-fifths of the sky is clouded. Plant and animal life  Most wild Dutch plant species are of the Atlantic district within the Euro-Siberian phytogeographic region. Gradients of salt and winter temperature variations cause relatively minor zonal differences in both wild and garden plants from the coast to more continental regions. The effects of elevation are negligible. Vegetation from coastal sand dunes, muddy coastal areas, slightly brackish lakes, and river deltas is especially scarce in the surrounding countries. Lakes, marshes, peatland, woods, heaths, and agricultural areas determine the general floral species. Clay, peat, and sand are important soil factors for the inland vegetation regions.  Animal life is relegated by region according to vegetation. Seabirds and other sea life, such as mollusks, are found especially in the muddy Waddenzee area and in the extreme southwest. Migrating birds pass in huge numbers through the Netherlands or remain for a summer or winter stay. Species of waterbirds and marsh and pasture birds are numerous. Larger mammals, such as roe deer, red deer, foxes, and badgers, are mostly restricted to nature reserves. Some species, such as boars, beavers, fallow deer, mouflons, and muskrats, have been introduced locally or reintroduced. Some reptiles and amphibians are endangered. Numerous species of river fish and river lobsters have become scarce because of water pollution. There is a diversity of brackish and freshwater animals inhabiting the many lakes, canals, and drainage ditches, but the vulnerable species of the nutritionally deficient waters have become rare.  Nature reserves have been formed by governmental and private organizations. Well-known reserves include the Naardermeer of Amsterdam, the Hoge Veluwe National Park, and the Oostvaardersplassen in the centre of the country. Some endangered species are protected by law.\">Encyclopedia Britannica<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Slovenia Free Tour Ajdovscina Free Tour Ljubljana Free Tour Bled Free Tour Portoroz Free Tour Information: Slovenia, country in central Europe that was part of Yugoslavia for most of the 20th century. Slovenia is a small but topographically diverse country made up of portions of four major European geographic landscapes\u2014the European Alps, the karstic Dinaric &hellip; <\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1579","page","type-page","status-publish","hentry","latest_post"],"translation":{"provider":"WPGlobus","version":"3.0.2","language":"zh","enabled_languages":["en","es","zh","it"],"languages":{"en":{"title":true,"content":true,"excerpt":false},"es":{"title":false,"content":false,"excerpt":false},"zh":{"title":false,"content":false,"excerpt":false},"it":{"title":false,"content":false,"excerpt":false}}},"yoast_head":"<!-- This site is optimized with the Yoast SEO Premium plugin v27.6 (Yoast SEO v27.7) - https:\/\/yoast.com\/product\/yoast-seo-premium-wordpress\/ -->\n<title>Slovenia - Best Free Tour<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/bestfreetour.com\/slovenia\/\" \/>\n<meta property=\"og:locale\" content=\"zh_CN\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Slovenia - 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