The Vosges are a range of low mountains in eastern France, near its border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single geomorphological unit and low mountain range of around 8,000 km2 in area, it runs in a north-northeast direction from the Burgundian Gate to the Börrstadt Basin, forms the western boundary of the Upper Rhine Plain. The Grand Ballon is the highest peak at 1,424 m, followed by the Storkenkopf, the Hohneck. Geographically, the Vosges Mountains are wholly in France, far above the Col de Saverne separating them from the Palatinate Forest in Germany; the latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From 1871 to 1918 the Vosges marked for the most part the border between Germany and France, due to the Franco-Prussian War; the elongated massif is divided south to north into three sections: The Higher Vosges or High Vosges, extending in the southern part of the range from Belfort to the river valley of the Bruche.
The rounded summits of the Hautes Vosges are called ballons in French "balloons". The sandstone Vosges or Middle Vosges, between the Permian Basin of Saint-Die including the Devonian-Dinantian volcanic massif of Schirmeck-Moyenmoutier and the Col de Saverne The Lower Vosges or Low Vosges, a sandstone plateau ranging from 1,000 feet to 1,850 feet high, between the Col de Saverne and the source of the Lauter. In addition, the term "Central Vosges" is used to designate the various lines of summits those above 1,000 m in elevation; the French department of Vosges is named after the range. From a geological point of view, a graben at the beginning of the Paleogene period caused the formation of Alsace and the uplift of the plates of the Vosges, in eastern France, those in the Black Forest, in Germany. From a scientific view, the Vosges Mountains are not mountains as such, but rather the western edge of the unfinished Alsatian graben, stretching continuously as part of the larger Tertiary formations.
Erosive glacial action was the primary catalyst for development of the representative highland massif feature. The Vosges in their southern and central parts are called the Hautes Vosges; these consist of a large Carboniferous mountain eroded just before the Permian Period with gneiss, porphyritic masses or other volcanic intrusions. In the north and west, there are places less eroded by glaciers, here Vosges Triassic and Permian red sandstone remains are found in large beds; the grès vosgien are embedded sometimes up to more than 500 m in thickness. The Lower Vosges in the north are dislocated plates of various sandstones, ranging from 300 to 600 m high; the Vosges is similar to the corresponding range of the Black Forest on the other side of the Rhine: both lie within the same degrees of latitude, have similar geological formations, are characterized by forests on their lower slopes, above which are open pastures and rounded summits of a rather uniform altitude. Both areas exhibit steeper slopes towards the Rhine River and a more gradual descent on the other side.
This occurs because both the Vosges and the Black Forest were formed by isostatic uplift, in a response to the opening of the Rhine Graben. The Rhine Graben is a major extensional basin; when such basins form, the thinning of the crust causes uplift adjacent to the basin. The amount of uplift decreases with distance from the basin, causing the highest range of peaks to be adjacent to the basin, the lower mountains to stretch away from the basin; the highest points are in the Hautes Vosges: the Grand Ballon, in ancient times called Ballon de Guebwiller or Ballon de Murbach, rises to 1,424 m. The Col de Saales, between the Higher and Central Vosges, reaches nearly 579 m, both lower and narrower than the Higher Vosges, with Mont Donon at 1,008 m being the highest point of this Nordic section; the highest mountains and peaks of the Vosges are: Grand Ballon 1,424 m Storkenkopf 1,366 m Hohneck 1,363 m Kastelberg 1,350 m Klintzkopf 1,330 m Rothenbachkopf 1,316 m Lauchenkopf 1,314 m Batteriekopf 1,311 m Haut de Falimont 1,306 m Gazon du Faing 1,306 m Rainkopf 1,305 m Gazon du Faîte 1,303 m Ringbuhl 1,302 m Soultzereneck 1,302 m Le Tanet 1,292 m Petit Ballon 1,272 m Ballon d'Alsace 1,247 m Brézouard 1,229 m Ballon de Servance 1,216 m Drumont 1,200 m Planche des Belles Filles 1,148 m Molkenrain 1,123 m Champ du Feu 1,099 m Baerenkopf 1,074 m Rocher de Mutzig 1,010 m Donon 1,009 m Taennchel 992 m Climont 965 m Hartmannswillerkopf 956 m Chatte Pendue 902 m Ungersberg 901 m Tête du Coq
World War I
World War I known as the First World War or the Great War, was a global war originating in Europe that lasted from 28 July 1914 to 11 November 1918. Contemporaneously described as "the war to end all wars", it led to the mobilisation of more than 70 million military personnel, including 60 million Europeans, making it one of the largest wars in history, it is one of the deadliest conflicts in history, with an estimated nine million combatants and seven million civilian deaths as a direct result of the war, while resulting genocides and the 1918 influenza pandemic caused another 50 to 100 million deaths worldwide. On 28 June 1914, Gavrilo Princip, a Bosnian Serb Yugoslav nationalist, assassinated the Austro-Hungarian heir Archduke Franz Ferdinand in Sarajevo, leading to the July Crisis. In response, on 23 July Austria-Hungary issued an ultimatum to Serbia. Serbia's reply failed to satisfy the Austrians, the two moved to a war footing. A network of interlocking alliances enlarged the crisis from a bilateral issue in the Balkans to one involving most of Europe.
By July 1914, the great powers of Europe were divided into two coalitions: the Triple Entente—consisting of France and Britain—and the Triple Alliance of Germany, Austria-Hungary and Italy. Russia felt it necessary to back Serbia and, after Austria-Hungary shelled the Serbian capital of Belgrade on the 28th, partial mobilisation was approved. General Russian mobilisation was announced on the evening of 30 July; when Russia failed to comply, Germany declared war on 1 August in support of Austria-Hungary, with Austria-Hungary following suit on 6th. German strategy for a war on two fronts against France and Russia was to concentrate the bulk of its army in the West to defeat France within four weeks shift forces to the East before Russia could mobilise. On 2 August, Germany demanded free passage through Belgium, an essential element in achieving a quick victory over France; when this was refused, German forces invaded Belgium on 3 August and declared war on France the same day. On 12 August and France declared war on Austria-Hungary.
In November 1914, the Ottoman Empire entered the war on the side of the Alliance, opening fronts in the Caucasus and the Sinai Peninsula. The war was fought in and drew upon each power's colonial empire as well, spreading the conflict to Africa and across the globe; the Entente and its allies would become known as the Allied Powers, while the grouping of Austria-Hungary and their allies would become known as the Central Powers. The German advance into France was halted at the Battle of the Marne and by the end of 1914, the Western Front settled into a battle of attrition, marked by a long series of trench lines that changed little until 1917. In 1915, Italy opened a front in the Alps. Bulgaria joined the Central Powers in 1915 and Greece joined the Allies in 1917, expanding the war in the Balkans; the United States remained neutral, although by doing nothing to prevent the Allies from procuring American supplies whilst the Allied blockade prevented the Germans from doing the same the U. S. became an important supplier of war material to the Allies.
After the sinking of American merchant ships by German submarines, the revelation that the Germans were trying to incite Mexico to make war on the United States, the U. S. declared war on Germany on 6 April 1917. Trained American forces would not begin arriving at the front in large numbers until mid-1918, but the American Expeditionary Force would reach some two million troops. Though Serbia was defeated in 1915, Romania joined the Allied Powers in 1916 only to be defeated in 1917, none of the great powers were knocked out of the war until 1918; the 1917 February Revolution in Russia replaced the Tsarist autocracy with the Provisional Government, but continuing discontent at the cost of the war led to the October Revolution, the creation of the Soviet Socialist Republic, the signing of the Treaty of Brest-Litovsk by the new government in March 1918, ending Russia's involvement in the war. This allowed the transfer of large numbers of German troops from the East to the Western Front, resulting in the German March 1918 Offensive.
This offensive was successful, but the Allies rallied and drove the Germans back in their Hundred Days Offensive. Bulgaria was the first Central Power to sign an armistice—the Armistice of Salonica on 29 September 1918. On 30 October, the Ottoman Empire capitulated. On 4 November, the Austro-Hungarian empire agreed to the Armistice of Villa Giusti after being decisively defeated by Italy in the Battle of Vittorio Veneto. With its allies defeated, revolution at home, the military no longer willing to fight, Kaiser Wilhelm abdicated on 9 November and Germany signed an armistice on 11 November 1918. World War I was a significant turning point in the political, cultural and social climate of the world; the war and its immediate aftermath sparked numerous uprisings. The Big Four (Britain, the United States, It
A summit is a point on a surface, higher in elevation than all points adjacent to it. The topographic terms acme, apex and zenith are synonymous; the term top is used only for a mountain peak, located at some distance from the nearest point of higher elevation. For example, a big massive rock next to the main summit of a mountain is not considered a summit. Summits near a higher peak, with some prominence or isolation, but not reaching a certain cutoff value for the quantities, are considered subsummits of the higher peak, are considered part of the same mountain. A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top. Summit may refer to the highest point along a line, trail, or route; the highest summit in the world is Everest with height of 8844.43 m above sea level. The first official ascent was made by Sir Edmund Hillary, they reached the mountain`s peak in 1953. Whether a highest point is classified as a summit, a sub peak or a separate mountain is subjective; the UIAA definition of a peak is.
Otherwise, it's a subpeak. In many parts of the western United States, the term summit refers to the highest point along a road, highway, or railroad. For example, the highest point along Interstate 80 in California is referred to as Donner Summit and the highest point on Interstate 5 is Siskiyou Mountain Summit. A summit climbing differs from the common mountaineering. Summit expedition requires: 1+ year of training, a good physical shape, a special gear. Although a huge part of climber’s stuff can be left and taken at the base camps or given to porters, there is a long list of personal equipment. In addition to common mountaineers’ gear, Summit climbers need to take Diamox and bottles of oxygen. There are special requirements for crampons, ice axe, rappel device, etc. Geoid Hill – Landform that extends above the surrounding terrain Nadir Summit accordance Peak finder Summit Climbing Gear List
A mountain range or hill range is a series of mountains or hills ranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form and alignment that have arisen from the same cause an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are found on many planetary mass objects in the Solar System and are a feature of most terrestrial planets. Mountain ranges are segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not have the same geologic structure or petrology, they may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, volcanic landforms resulting in a variety of rock types. Most geologically young mountain ranges on the Earth's land surface are associated with either the Pacific Ring of Fire or the Alpide Belt.
The Pacific Ring of Fire includes the Andes of South America, extends through the North American Cordillera along the Pacific Coast, the Aleutian Range, on through Kamchatka, Taiwan, the Philippines, Papua New Guinea, to New Zealand. The Andes is 7,000 kilometres long and is considered the world's longest mountain system; the Alpide belt includes Indonesia and Southeast Asia, through the Himalaya, Caucasus Mountains, Balkan Mountains fold mountain range, the Alps, ends in the Spanish mountains and the Atlas Mountains. The belt includes other European and Asian mountain ranges; the Himalayas contain the highest mountains in the world, including Mount Everest, 8,848 metres high and traverses the border between China and Nepal. Mountain ranges outside these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Great Dividing Range, the Altai Mountains and the Hijaz Mountains. If the definition of a mountain range is stretched to include underwater mountains the Ocean Ridges form the longest continuous mountain system on Earth, with a length of 65,000 kilometres.
The mountain systems of the earth are characterized by a tree structure, where mountain ranges can contain sub-ranges. The sub-range relationship is expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains. Equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, the White Mountains and the Blue Ridge Mountains are children of the Appalachians; the parent-child expression extends to the sub-ranges themselves: the Sandwich Range and the Presidential Range are children of the White Mountains, while the Presidential Range is parent to the Northern Presidential Range and Southern Presidential Range. The position of mountains influences climate, such as snow; when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the leeward side, it warms again and is drier, having been stripped of much of its moisture.
A rain shadow will affect the leeward side of a range. Mountain ranges are subjected to erosional forces which work to tear them down; the basins adjacent to an eroding mountain range are filled with sediments which are buried and turned into sedimentary rock. Erosion is at work while the mountains are being uplifted until the mountains are reduced to low hills and plains; the early Cenozoic uplift of the Rocky Mountains of Colorado provides an example. As the uplift was occurring some 10,000 feet of Mesozoic sedimentary strata were removed by erosion over the core of the mountain range and spread as sand and clays across the Great Plains to the east; this mass of rock was removed as the range was undergoing uplift. The removal of such a mass from the core of the range most caused further uplift as the region adjusted isostatically in response to the removed weight. Rivers are traditionally believed to be the principal cause of mountain range erosion, by cutting into bedrock and transporting sediment.
Computer simulation has shown that as mountain belts change from tectonically active to inactive, the rate of erosion drops because there are fewer abrasive particles in the water and fewer landslides. Mountains on other planets and natural satellites of the Solar System are isolated and formed by processes such as impacts, though there are examples of mountain ranges somewhat similar to those on Earth. Saturn's moon Titan and Pluto, in particular exhibit large mountain ranges in chains composed of ices rather than rock. Examples include the Mithrim Montes and Doom Mons on Titan, Tenzing Montes and Hillary Montes on Pluto; some terrestrial planets other than Earth exhibit rocky mountain ranges, such as Maxwell Montes on Venus taller than any on Earth and Tartarus Montes on Mars, Jupiter's moon Io has mountain ranges formed from tectonic processes including Boösaule Montes, Dorian Montes, Hi'iaka Montes and Euboea Montes. Peakbagger Ranges Home Page Bivouac.com
Bas-Rhin is a department in Alsace, a part of the Grand Est super-region of France. The name means "Lower Rhine", geographically speaking it belongs to the Upper Rhine region, it is the more populous and densely populated of the two departments of the traditional Alsace region, with 1,121,407 inhabitants in 2016. The prefecture and the General Council are based in Strasbourg; the INSEE and Post Code is 67. The inhabitants of the department are known as Bas-Rhinoises; the Rhine has always been of great historical and economic importance to the area, it forms the eastern border of Bas-Rhin. The area is home to some of the foothills of the Vosges Mountains. To the north of Bas-Rhin lies the Palatinate forest in the German State of Rhineland-Palatinate, the German State of Baden-Württemberg lies to the east. To the south lies the department of Haut-Rhin, the town of Colmar and southern Alsace, to the west the department of Moselle. On its south-western corner, Bas-Rhin joins the department of Vosges.
The Bas-Rhin has a continental-type climate, characterised by cold, dry winters and hot, stormy summers, due to the western protection provided by the Vosges. The average annual temperature is 7 °C on high ground; the annual maximum temperature is high. The average rainfall is 700 mm per year. Established according to data from the Infoclimat station at Strasbourg-Entzheim, over the period from 1961 to 1990; this is the last French department to have kept the term Bas meaning "Lower" in its name. Other departments using this prefix preferred to change their names - e.g.: Basses-Pyrenees in 1969 became Pyrénées-Atlantiques and Basses-Alpes in 1970 became the department of Alpes-de-Haute-Provence. The same phenomenon was observed for the inférieur departments such as Charente-Inférieure, Seine-Inférieure, Loire-Inférieure. Bas-Rhin is one of the original 83 departments created on 4 March 1790, during the French Revolution. On 14 January 1790 the National Constituent Assembly decreed: "- That Alsace be divided into two departments with Strasbourg and Colmar as their capitals.
In 1871 Bas-Rhin was annexed by Germany and became Bezirk Unterelsass in Reichsland Elsaß-Lothringen. Strasbourg, the chef lieu of Bas-Rhin is the official seat of the European Parliament as well as of the Council of Europe; the demography of Bas-Rhin is characterized by high density and high population growth since the 1950s. In January 2014 Bas-Rhin had 1,112,815 inhabitants and was 18th by population at the national level. In fifteen years, from 1999 to 2014, its population grew by more than 86,000 people, or about 5,800 people per year, but this variation is differentiated among the 517 communes. The population density of Bas-Rhin is 234 inhabitants per square kilometre in 2014, more than twice the average in France, 112 in 2009; the first census was conducted in 1801 and this count, renewed every five years from 1821, provides precise information on the evolution of population in the department. With 540,213 inhabitants in 1831, the department represented 1.66% of the total French population, 32,569,000 inhabitants.
From 1831 to 1866, the department gained 48,757 people, an increase of 0.26% on average per year compared to the national average of 0.48% over the same period. Demographic change between the Franco-Prussian War of 1870 and the First World War was higher than the national average. Over this period, the population increased by 100,532 inhabitants, an increase of 16.74%, compared to 10% nationally. The population increased by 9.23% between the two world wars from 1921 to 1936 compared to a national growth of 6.9%. Like other French departments, Bas-Rhin experienced a population boom after the Second World War, higher than the national level; the rate of population growth between 1946 and 2007 was 83.83%
Musée archéologique (Strasbourg)
The Musée archéologique of Strasbourg, France is the largest of the numerous Alsacian museums displaying regional archeological findings from Prehistory to the Merovingian dynasty. It is located in the basement of the Palais Rohan; the museum goes back to the legacy of the historian Johann Daniel Schöpflin, who bequeathed his collection to the city of Strasbourg. The Société pour la conservation des monuments historiques d’Alsace, founded in 1855, expanded and publicly displayed the municipal collections, of which a large number was however destroyed in 1870, during the Franco-Prussian War. During the reconstruction of the city and its museums, the musée archéologique moved to the premises that are still its own. In the 20th century, longtime directors Robert Forrer and Jean-Jacques Hatt worked on the systematic study of the Alsatian ground and the substantial enlargement of the collection. Between 1988 and 1992, the musée was renovated, its collections continue to grow due to the numerous excavations made in and around Strasbourg since the beginning of the construction of the new Tramway network.
The museum presents an overview of the human habitat in the region beginning with the earliest traces of Human dwelling and settling. A special focus is put on its outposts along the Rhine like Seltz. One of the museums most famous objects is the much studied stele of the legionnary Caius Largennius; the museum displays findings from the Gallo-Roman sanctuaries on the Mont Donon and in Mackwiller, as well as Merovingian findings made around Erstein. — Media related to Musée archéologique de Strasbourg at Wikimedia Commons
France the French Republic, is a country whose territory consists of metropolitan France in Western Europe and several overseas regions and territories. The metropolitan area of France extends from the Mediterranean Sea to the English Channel and the North Sea, from the Rhine to the Atlantic Ocean, it is bordered by Belgium and Germany to the northeast and Italy to the east, Andorra and Spain to the south. The overseas territories include French Guiana in South America and several islands in the Atlantic and Indian oceans; the country's 18 integral regions span a combined area of 643,801 square kilometres and a total population of 67.3 million. France, a sovereign state, is a unitary semi-presidential republic with its capital in Paris, the country's largest city and main cultural and commercial centre. Other major urban areas include Lyon, Toulouse, Bordeaux and Nice. During the Iron Age, what is now metropolitan France was inhabited by a Celtic people. Rome annexed the area in 51 BC, holding it until the arrival of Germanic Franks in 476, who formed the Kingdom of Francia.
The Treaty of Verdun of 843 partitioned Francia into Middle Francia and West Francia. West Francia which became the Kingdom of France in 987 emerged as a major European power in the Late Middle Ages following its victory in the Hundred Years' War. During the Renaissance, French culture flourished and a global colonial empire was established, which by the 20th century would become the second largest in the world; the 16th century was dominated by religious civil wars between Protestants. France became Europe's dominant cultural and military power in the 17th century under Louis XIV. In the late 18th century, the French Revolution overthrew the absolute monarchy, established one of modern history's earliest republics, saw the drafting of the Declaration of the Rights of Man and of the Citizen, which expresses the nation's ideals to this day. In the 19th century, Napoleon established the First French Empire, his subsequent Napoleonic Wars shaped the course of continental Europe. Following the collapse of the Empire, France endured a tumultuous succession of governments culminating with the establishment of the French Third Republic in 1870.
France was a major participant in World War I, from which it emerged victorious, was one of the Allies in World War II, but came under occupation by the Axis powers in 1940. Following liberation in 1944, a Fourth Republic was established and dissolved in the course of the Algerian War; the Fifth Republic, led by Charles de Gaulle, remains today. Algeria and nearly all the other colonies became independent in the 1960s and retained close economic and military connections with France. France has long been a global centre of art and philosophy, it hosts the world's fourth-largest number of UNESCO World Heritage Sites and is the leading tourist destination, receiving around 83 million foreign visitors annually. France is a developed country with the world's sixth-largest economy by nominal GDP, tenth-largest by purchasing power parity. In terms of aggregate household wealth, it ranks fourth in the world. France performs well in international rankings of education, health care, life expectancy, human development.
France is considered a great power in global affairs, being one of the five permanent members of the United Nations Security Council with the power to veto and an official nuclear-weapon state. It is a leading member state of the European Union and the Eurozone, a member of the Group of 7, North Atlantic Treaty Organization, Organisation for Economic Co-operation and Development, the World Trade Organization, La Francophonie. Applied to the whole Frankish Empire, the name "France" comes from the Latin "Francia", or "country of the Franks". Modern France is still named today "Francia" in Italian and Spanish, "Frankreich" in German and "Frankrijk" in Dutch, all of which have more or less the same historical meaning. There are various theories as to the origin of the name Frank. Following the precedents of Edward Gibbon and Jacob Grimm, the name of the Franks has been linked with the word frank in English, it has been suggested that the meaning of "free" was adopted because, after the conquest of Gaul, only Franks were free of taxation.
Another theory is that it is derived from the Proto-Germanic word frankon, which translates as javelin or lance as the throwing axe of the Franks was known as a francisca. However, it has been determined that these weapons were named because of their use by the Franks, not the other way around; the oldest traces of human life in what is now France date from 1.8 million years ago. Over the ensuing millennia, Humans were confronted by a harsh and variable climate, marked by several glacial eras. Early hominids led a nomadic hunter-gatherer life. France has a large number of decorated caves from the upper Palaeolithic era, including one of the most famous and best preserved, Lascaux. At the end of the last glacial period, the climate became milder. After strong demographic and agricultural development between the 4th and 3rd millennia, metallurgy appeared at the end of the 3rd millennium working gold and bronze, iron. France has numerous megalithic sites from the Neolithic period, including the exceptiona