1.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
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Topographic prominence
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It is a measure of the independence of a summit. A peaks key col is a point on this contour line. By convention, the prominence of Mount Everest, the Earths highest mountain, is taken to equal the elevation of its summit above sea level, if the peaks prominence is P metres, to get from the summit to any higher terrain one must descend at least P metres. Together with the convention for Mount Everest, this implies that the prominence of any island or continental highpoint is equal to its elevation above sea level, for every ridge connecting the peak to higher terrain, find the lowest point on the ridge. The key col is defined as the highest of these cols, the prominence is the difference between the elevation of the peak and the elevation of the key col. The following mental exercise may illustrate the meaning of topographic prominence, imagine you are standing at the top of a peak and imagine that an imaginary sea level rises to your feet. Now slowly lower the sea level and an imaginary island appears beneath your feet. Your island will grow and will merge with other islands that emerge, the parent peak may be either close or far from the subject peak. The summit of Mount Everest is the parent peak of Aconcagua at a distance of 17,755 km, the key col may also be close or far from the subject peak. The key col for Aconcagua is the Bering Strait at a distance of 13,655 km, the key col for the South Summit of Mount Everest is about 100 m distant. Prominence is interesting to many mountaineers because it is a measurement that is strongly correlated with the subjective significance of a summit. Peaks with low prominences are either subsidiary tops of some higher summit or relatively insignificant independent summits, peaks with high prominences tend to be the highest points around and are likely to have extraordinary views. Only summits with a sufficient degree of prominence are regarded as independent mountains, for example, the worlds second-highest mountain is K2. While Mount Everests South Summit is taller than K2, it is not considered an independent mountain because it is a subsummit of the main summit, many lists of mountains take topographic prominence as a criterion for inclusion, or cutoff. John and Anne Nuttalls The Mountains of England and Wales uses a cutoff of 15 m, in the contiguous United States, the famous list of fourteeners uses a cutoff of 300 ft /91 m. Also in the U. S.2000 feet of prominence has become a threshold that signifies that a peak has major stature. This generates lists of peaks ranked by prominence, which are different from lists ranked by elevation. Such lists tend to emphasize isolated high peaks, such as range or island high points, one advantage of a prominence-ranked list is that it needs no cutoff, since a peak with high prominence is automatically an independent peak
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Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
4.
Haute-Savoie
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Haute-Savoie is a department in the Auvergne-Rhône-Alpes region of south-eastern France, bordering both Switzerland and Italy. To the north is Lake Geneva and Switzerland, to the south and southeast are the Mont Blanc, the French entrance to the Mont Blanc Tunnel to Italy is in Haute-Savoie. It is noted for winter sports, the first Winter Olympic Games were held at Chamonix in 1924, before 1860, the territory occupied by modern Haute-Savoie and the adjoining department of Savoie had been part of the Kingdom of Sardinia since the Treaty of Utrecht in 1713. Annexation of the region by France was formalized in the Treaty of Turin on March 24,1860, from November 1942 to September 1943, Haute-Savoie was subjected to military occupation by Fascist Italy. The Maquis des Glières operated from Haute-Savoie, Haute-Savoie comprises four arrondissements, divided into 294 communes and 17 cantons. Haute-Savoie has the largest range of elevations of all the departments in France, the lowest point is 250 metres in the Rhône River Valley, some of the worlds best-known ski resorts are in Haute-Savoie. Its mountainous terrain makes mountain passes important to trade and economic life, some of the most important are the Col de la Forclaz and the Mont Blanc Tunnel, linking Chamonix to Courmayeur in the Aosta Valley. As of 1996,178,624 hectares of Haute-Savoie is forested, compared to 34.4 percent for the Rhone-Alpes region and 27.1 percent for France as a whole. Of the forested area 141,063 hectares is managed for timber and other forest products, national nature reserves are designated by the French government as areas where an outstanding natural heritage is present in both rare and typical areas in terms of species and geology. Management is charged to local organizations, with direction and evaluation focusing on protection for future generations. Lake Annecy is an attraction, along with the town of Évian-les-Bains, perhaps the best-known town on the French shore of Lake Geneva. Haute-Savoie is entirely within the watershed of the Rhone, there were 4,450 farmers in 1999,4,800 farmers and over 1,700 full-time farm employees at the end of 2006. In 1999, crop production was valued at €71.5 million, dairy production is a large part of the Haute-Savoie economy, earning €117.2 million in 2006 and representing 74 percent of the net animal-product worth. The average expenditure per capita in 2006 was €21,706, with the 2004–2007 rise of the euro, Swiss customer traffic decreased five or six percent. At the end of 2006, traditional small businesses represented 84 percent of businesses and 40 percent of retail space,4,301 companies were established in 2004 in Haute-Savoie, nearly 80 percent in the service sector, with a high percentage offering service to individuals. This accounted for 21.6 percent of new businesses, the most active sectors were real estate, construction, business services and the food industry. In 1999, Haute-Savoie had 2,779 industrial companies producing 13.60 percent of all business income. T, firms engaged in screw-cutting are major employers in the department. While the automotive industry is the client, firms also service the electronics, household-appliance
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France
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France, officially the French Republic, is a country with territory in western Europe and several overseas regions and territories. The European, or metropolitan, area of France extends from the Mediterranean Sea to the English Channel and the North Sea, Overseas France include French Guiana on the South American continent and several island territories in the Atlantic, Pacific and Indian oceans. France spans 643,801 square kilometres and had a population of almost 67 million people as of January 2017. It is a unitary republic with the capital in Paris. Other major urban centres include Marseille, Lyon, Lille, Nice, Toulouse, during the Iron Age, what is now metropolitan France was inhabited by the Gauls, a Celtic people. The area was annexed in 51 BC by Rome, which held Gaul until 486, France emerged as a major European power in the Late Middle Ages, with its victory in the Hundred Years War strengthening state-building and political centralisation. During the Renaissance, French culture flourished and a colonial empire was established. The 16th century was dominated by civil wars between Catholics and Protestants. France became Europes dominant cultural, political, and military power under Louis XIV, in the 19th century Napoleon took power and established the First French Empire, whose subsequent Napoleonic Wars shaped the course of continental Europe. Following the collapse of the Empire, France endured a succession of governments culminating with the establishment of the French Third Republic in 1870. Following liberation in 1944, a Fourth Republic was established and later dissolved in the course of the Algerian War, the Fifth Republic, led by Charles de Gaulle, was formed in 1958 and remains to this day. Algeria and nearly all the colonies became independent in the 1960s with minimal controversy and typically retained close economic. France has long been a centre of art, science. It hosts Europes fourth-largest number of cultural UNESCO World Heritage Sites and receives around 83 million foreign tourists annually, France is a developed country with the worlds sixth-largest economy by nominal GDP and ninth-largest by purchasing power parity. In terms of household wealth, it ranks fourth in the world. France performs well in international rankings of education, health care, life expectancy, France remains a great power in the world, 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 member state of the European Union and the Eurozone. It is also a member of the Group of 7, North Atlantic Treaty Organization, Organisation for Economic Co-operation and Development, the World Trade Organization, originally applied to the whole Frankish Empire, the name France comes from the Latin Francia, or country of the Franks
6.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily 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, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often 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, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
7.
French Prealps
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The French Prealps are a group of subalpine mountain ranges of medium elevation located immediately west of the French Alps. In the southern regions, the ranges are generally disorganized and lack the wide. Three non-contiguous ranges traditionally comprise the southern French Prealps, the Alpilles, Mont Sainte-Victoire, roger Frison-Roche, Les montagnes de la terre
8.
Geologic time scale
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The table of geologic time spans, presented here, agrees with the nomenclature, dates and standard color codes set forth by the International Commission on Stratigraphy. Evidence from radiometric dating indicates that Earth is about 4.54 billion years old, the geology or deep time of Earth’s past has been organized into various units according to events which took place in each period. Older time spans, which predate the reliable record, are defined by their absolute age. Some other planets and moons within the Solar System have sufficiently rigid structures to have preserved records of their own histories, for example, Venus, Mars, dominantly fluid planets, such as the gas giants, do not preserve their history in a comparable manner. Apart from the Late Heavy Bombardment, events on other planets probably had little influence on the Earth. Construction of a scale that links the planets is, therefore, of only limited relevance to the Earths time scale. The existence, timing, and terrestrial effects of the Late Heavy Bombardment is still debated, the largest defined unit of time is the supereon, composed of eons. Eons are divided into eras, which are in turn divided into periods, epochs, the terms eonothem, erathem, system, series, and stage are used to refer to the layers of rock that correspond to these periods of geologic time in Earths history. Geologists qualify these units as early, mid, and late when referring to time, and lower, middle, for example, the lower Jurassic Series in chronostratigraphy corresponds to the early Jurassic Epoch in geochronology. The adjectives are capitalized when the subdivision is formally recognized, and lower case when not, thus early Miocene but Early Jurassic. Geologic units from the time but different parts of the world often look different and contain different fossils. For example, in North America the Lower Cambrian is called the Waucoban series that is subdivided into zones based on succession of trilobites. In East Asia and Siberia, the unit is split into Alexian, Atdabanian. A key aspect of the work of the International Commission on Stratigraphy is to reconcile this conflicting terminology, the term Anthropocene is used informally by popular culture and a growing number of scientists to describe the current epoch in which we are living. The term was coined by Paul Crutzen and Eugene Stoermer in 2000 to describe the current time, others say that humans have not even started to leave their biggest impact on Earth, and therefore the Anthropocene hasnt even started yet. Whatever the case, the ICS has not officially approved the term, leonardo da Vinci concurred with Aristotles interpretation that fossils represented the remains of ancient life. The 11th-century Persian geologist Avicenna and the 13th-century Dominican bishop Albertus Magnus extended Aristotles explanation into a theory of a petrifying fluid. Avicenna also first proposed one of the principles underlying geologic time scales, the Chinese naturalist Shen Kuo also recognized the concept of deep time
9.
Jurassic
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The Jurassic is a geologic period and system that spans 56.3 million years from the end of the Triassic Period 201.3 million years ago to the beginning of the Cretaceous Period 145 Mya. The Jurassic constitutes the middle period of the Mesozoic Era, also known as the Age of Reptiles, the start of the period is marked by the major Triassic–Jurassic extinction event. The Jurassic is named after the Jura Mountains within the European Alps, by the beginning of the Jurassic, the supercontinent Pangaea had begun rifting into two landmasses, Laurasia to the north and Gondwana to the south. This created more coastlines and shifted the continental climate from dry to humid, on land, the fauna transitioned from the Triassic fauna, dominated by both dinosauromorph and crocodylomorph archosaurs, to one dominated by dinosaurs alone. The first birds also appeared during the Jurassic, having evolved from a branch of theropod dinosaurs, other major events include the appearance of the earliest lizards, and the evolution of therian mammals, including primitive placentals. Crocodilians made the transition from a terrestrial to a mode of life. The oceans were inhabited by marine reptiles such as ichthyosaurs and plesiosaurs, the chronostratigraphic term Jurassic is directly linked to the Jura Mountains. The name Jura is derived from the Celtic root jor, which was Latinised into juria, the Jurassic period is divided into the Early Jurassic, Middle, and Late Jurassic epochs. The Jurassic System, in stratigraphy, is divided into the Lower Jurassic, Middle, the separation of the term Jurassic into three sections goes back to Leopold von Buch. The Jurassic North Atlantic Ocean was relatively narrow, while the South Atlantic did not open until the following Cretaceous period, the Tethys Sea closed, and the Neotethys basin appeared. Climates were warm, with no evidence of glaciation, as in the Triassic, there was apparently no land over either pole, and no extensive ice caps existed. In contrast, the North American Jurassic record is the poorest of the Mesozoic, the Jurassic was a time of calcite sea geochemistry in which low-magnesium calcite was the primary inorganic marine precipitate of calcium carbonate. Carbonate hardgrounds were thus very common, along with calcitic ooids, calcitic cements, the first of several massive batholiths were emplaced in the northern American cordillera beginning in the mid-Jurassic, marking the Nevadan orogeny. Important Jurassic exposures are found in Russia, India, South America, Japan, Australasia. As the Jurassic proceeded, larger and more groups of dinosaurs like sauropods and ornithopods proliferated in Africa. Middle Jurassic strata are well represented nor well studied in Africa. Late Jurassic strata are also poorly represented apart from the spectacular Tendaguru fauna in Tanzania, the Late Jurassic life of Tendaguru is very similar to that found in western North Americas Morrison Formation. During the Jurassic period, the primary living in the sea were fish
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Cretaceous
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The Cretaceous is a geologic period and system that spans 79 million years from the end of the Jurassic Period 145 million years ago to the beginning of the Paleogene Period 66 Mya. It is the last period of the Mesozoic Era, the Cretaceous Period is usually abbreviated K, for its German translation Kreide. The Cretaceous was a period with a warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites and rudists, during this time, new groups of mammals and birds, as well as flowering plants, appeared. The Cretaceous ended with a mass extinction, the Cretaceous–Paleogene extinction event, in which many groups, including non-avian dinosaurs, pterosaurs. The end of the Cretaceous is defined by the abrupt Cretaceous–Paleogene boundary, the name Cretaceous was derived from Latin creta, meaning chalk. The Cretaceous is divided into Early and Late Cretaceous epochs, or Lower and Upper Cretaceous series, in older literature the Cretaceous is sometimes divided into three series, Neocomian, Gallic and Senonian. A subdivision in eleven stages, all originating from European stratigraphy, is now used worldwide, in many parts of the world, alternative local subdivisions are still in use. As with other geologic periods, the rock beds of the Cretaceous are well identified. No great extinction or burst of diversity separates the Cretaceous from the Jurassic and this layer has been dated at 66.043 Ma. A140 Ma age for the Jurassic-Cretaceous boundary instead of the usually accepted 145 Ma was proposed in 2014 based on a study of Vaca Muerta Formation in Neuquén Basin. Víctor Ramos, one of the authors of the study proposing the 140 Ma boundary age sees the study as a first step toward formally changing the age in the International Union of Geological Sciences, due to the high sea level there was extensive space for such sedimentation. Because of the young age and great thickness of the system. Chalk is a type characteristic for the Cretaceous. It consists of coccoliths, microscopically small calcite skeletons of coccolithophores, the group is found in England, northern France, the low countries, northern Germany, Denmark and in the subsurface of the southern part of the North Sea. Chalk is not easily consolidated and the Chalk Group still consists of sediments in many places. The group also has other limestones and arenites, among the fossils it contains are sea urchins, belemnites, ammonites and sea reptiles such as Mosasaurus. In southern Europe, the Cretaceous is usually a marine system consisting of competent limestone beds or incompetent marls
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Mountain
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A mountain is a large landform that stretches above the surrounding land in a limited area, usually in the form of a peak. A mountain is steeper than a hill. Mountains are formed through tectonic forces or volcanism and these forces can locally raise the surface of the earth. Mountains erode slowly through the action of rivers, weather conditions, a few mountains are isolated summits, but most occur in huge mountain ranges. High elevations on mountains produce colder climates than at sea level and these colder climates strongly affect the ecosystems of mountains, different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains tend to be used less for agriculture and more for resource extraction and recreation, the highest mountain on Earth is Mount Everest in the Himalayas of Asia, whose summit is 8,850 m above mean sea level. The highest known mountain on any planet in the Solar System is Olympus Mons on Mars at 21,171 m, there is no universally accepted definition of a mountain. Elevation, volume, relief, steepness, spacing and continuity have been used as criteria for defining a mountain, whether a landform is called a mountain may depend on local usage. The highest point in San Francisco, California, is called Mount Davidson, notwithstanding its height of 300 m, similarly, Mount Scott outside Lawton, Oklahoma is only 251 m from its base to its highest point. Whittows Dictionary of Physical Geography states Some authorities regard eminences above 600 metres as mountains, in addition, some definitions also include a topographical prominence requirement, typically 100 or 500 feet. For a while, the US defined a mountain as being 1,000 feet or taller, any similar landform lower than this height was considered a hill. However, today, the United States Geological Survey concludes that these terms do not have technical definitions in the US, using these definitions, mountains cover 33% of Eurasia, 19% of South America, 24% of North America, and 14% of Africa. As a whole, 24% of the Earths land mass is mountainous, there are three main types of mountains, volcanic, fold, and block. All three types are formed from plate tectonics, when portions of the Earths crust move, crumple, compressional forces, isostatic uplift and intrusion of igneous matter forces surface rock upward, creating a landform higher than the surrounding features. The height of the feature makes it either a hill or, if higher and steeper, major mountains tend to occur in long linear arcs, indicating tectonic plate boundaries and activity. Volcanoes are formed when a plate is pushed below another plate, at a depth of around 100 km, melting occurs in rock above the slab, and forms magma that reaches the surface. When the magma reaches the surface, it builds a volcanic mountain. Examples of volcanoes include Mount Fuji in Japan and Mount Pinatubo in the Philippines, the magma does not have to reach the surface in order to create a mountain, magma that solidifies below ground can still form dome mountains, such as Navajo Mountain in the US
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Geneva
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Geneva is the second most populous city in Switzerland and is the most populous city of Romandy, the French-speaking part of Switzerland. Situated where the Rhône exits Lake Geneva, it is the capital of the Republic, the municipality has a population of 198,072, and the canton has 484,736 residents. In 2014, the compact agglomération du Grand Genève had 946,000 inhabitants in 212 communities in both Switzerland and France, within Swiss territory, the commuter area named Métropole lémanique contains a population of 1.25 million. This area is essentially spread east from Geneva towards the Riviera area and north-east towards Yverdon-les-Bains, Geneva is the city that hosts the highest number of international organizations in the world. It is also the place where the Geneva Conventions were signed, Geneva was ranked as the worlds ninth most important financial centre for competitiveness by the Global Financial Centres Index, ahead of Frankfurt, and third in Europe behind London and Zürich. A2009 survey by Mercer found that Geneva has the third-highest quality of life of any city in the world, the city has been referred to as the worlds most compact metropolis and the Peace Capital. In 2009 and 2011, Geneva was ranked as, respectively, the city was mentioned in Latin texts, by Caesar, with the spelling Genava, probably from a Celtic toponym *genawa- from the stem *genu-, in the sense of a bending river or estuary. The medieval county of Geneva in Middle Latin was known as pagus major Genevensis or Comitatus Genevensis, the name takes various forms in modern languages, Geneva /dʒᵻˈniːvə/ in English, French, Genève, German, Genf, Italian, Ginevra, and Romansh, Genevra. The city in origin shares its name, *genawa estuary, with the Italian port city of Genoa, Geneva was an Allobrogian border town, fortified against the Helvetii tribe, when the Romans took it in 121 BC. It became Christian under the Late Roman Empire, and acquired its first bishop in the 5th century, having been connected to the bishopric of Vienne in the 4th. In the Middle Ages, Geneva was ruled by a count under the Holy Roman Empire until the late 14th century, around this time the House of Savoy came to dominate the city. In the 15th century, a republican government emerged with the creation of the Grand Council. In 1541, with Protestantism in the ascendancy, John Calvin, by the 18th century, however, Geneva had come under the influence of Catholic France, which cultivated the city as its own. France also tended to be at odds with the ordinary townsfolk, in 1798, revolutionary France under the Directory annexed Geneva. At the end of the Napoleonic Wars, on 1 June 1814, in 1907, the separation of Church and State was adopted. Geneva flourished in the 19th and 20th centuries, becoming the seat of international organizations. Geneva is located at 46°12 North, 6°09 East, at the end of Lake Geneva. It is surrounded by two chains, the Alps and the Jura
13.
Jura Mountains
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The Jura Mountains French, Massif du Jura, are a sub-alpine mountain range located north of the Western Alps, mainly following the course of the France–Switzerland border. The Jura separates the Rhine and Rhône basins, forming part of the watershed of each, the name Jura is derived from juria, a Latinized form of a Celtic stem jor- forest. The mountain range gives its name to the French department of Jura, the Swiss Canton of Jura, the Jurassic period of the timescale. The Jura Mountains are a province of the larger Central European uplands. In France, the Jura covers most of the Franche-Comté region, the range reaches its highest point at Le Crêt de la Neige in the department of Ain and finds its southern terminus in the northwestern part of the department of Savoie. The north end of the Jura extends into the tip of the Alsace region. Roughly 1,600 square kilometres of the range in France is protected by the Jura Mountains Regional Natural Park. The Swiss Jura is one of the three geographical regions of Switzerland, the other being the Swiss plateau and the Swiss Alps. In Switzerland, the covers the western border with France in the cantons of Basel-Landschaft, Solothurn, Jura, Bern, Neuchâtel. Much of the Swiss Jura region has no association with Early Modern Switzerland and was incorporated as part of the Swiss Confederacy only in the 19th century. In the 20th century, a movement of Jurassic separatism developed which resulted in the creation of the canton of Jura in 1979, the Swiss Jura has been industrialized since the 18th century and became a major centre of the watchmaking industry. The area has several cities at very high altitudes, such as La Chaux-de-Fonds, Le Locle, the Jura range proper is continued as the Table Jura in the cantons of Basel-Landschaft and Aargau, and further to Schaffhausen and into southern Germany towards the Swabian and Franconian plateaus. The range is built up vertically while decreasing in size laterally and this deformation accommodates the compression from alpine folding as the main Alpine orogenic front moves roughly northwards. The deformation becomes less pervasive away from the younger, more active Alpine mountain building, the geologic folds comprise three major bands of building that date from three epochs, the Lias, the Dogger and the Malm geologic periods. Each era of folding reveals effects of shallow marine environments as evidenced by beds with carbonate sequences, containing abundant bioclasts. Structurally, the Jura consists of a sequence of geologic folds, the highest peak in the Jura range is Le Crêt de la Neige at 1,720 metres. Vosges and Jura coal mining basins The Jura range offer a variety of tourist activities including hiking, cycling, downhill skiing, there are many signposted trails including the Jura ridgeway, a 310 km hiking route. Tourist attractions include natural features such as the Creux du Van, lookout peaks such as the Chasseral, caves such as the Grottes de lOrbe, and gorges such as Taubenloch
14.
Aerial tramway
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An aerial tramway, sky tram, cable car, ropeway or aerial tram is a type of aerial lift which uses one or two stationary ropes for support while a third moving rope provides propulsion. With this form of lift, the grip of an aerial tramway cabin is fixed onto the propulsion rope, as such, careful phrasing is necessary to prevent confusion. It is also called a ropeway or even incorrectly referred to as a gondola lift. A gondola lift has cabins suspended from a continuously circulating cable whereas aerial trams simply shuttle back, in Japan, the two are considered as the same category of vehicle and called ropeway, while the term cable car means Cable car and funicular. An aerial railway where the vehicles are suspended from a track is known as a suspension railway. An aerial tramway consists of one or two fixed cables, one loop of cable, and a number of passenger cabins, the fixed cables provide support for the cabins while the haulage rope, by means of a grip, is solidly connected to the truck. An electric motor drives the haulage rope which provides propulsion, Aerial tramways differ from gondola lifts in that gondola lifts are considered continuous systems. A similar system of cables is used in a funicular railway, the two passenger cabins, which carry from 4 to over 150 people, are situated at opposite ends of the loops of cable. Thus, while one is coming up, the other is going down the mountain, some aerial trams have only one cabin, which lends itself better for systems with small elevation changes along the cable run. The first operational aerial tram was built in 1644 by Adam Wiebe in Gdańsk and it was moved by horses and used to move soil over the river to build defences. It is called the first known cable lift in European history and it is not known how long this lift was used. In any case, it would be another 230 years before Germany would get the cable lift. Other mining systems were developed in the 1860s by Hodgson, Hallidie went on to perfect a line of mining and people tramways after 1867 in California and Nevada. Tramways are sometimes used in regions to carry ore from a mine located high on the mountain to an ore mill located at a lower elevation. Ore tramways were common in the early 20th century at the mines in North and South America, one can still be seen in the San Juan Mountains of the US state of Colorado. Over one thousand mining tramways were built around the world—Spitsbergen, Russia, Alaska, Argentina, New Zealand and this experience was replicated with the use of tramways in the First World War particularly on the Isonzo Front in Italy. The German firm of Bleichert built hundreds of freight and military tramways, strangely, Bleichert even built the first tourist tramway at Bolzano/Bozen, in then Tyrolian Austria in 1913. Other firms entered the mining tramway business- Otto, Leschen, Breco Ropeways Ltd, ceretti and Tanfani, and Riblet for instance
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Suspension bridge
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A suspension bridge is a type of bridge in which the deck is hung below suspension cables on vertical suspenders. The first modern examples of type of bridge were built in the early 19th century. Simple suspension bridges, which lack vertical suspenders, have a history in many mountainous parts of the world. This type of bridge has cables suspended between towers, plus vertical suspender cables carry the weight of the deck below, upon which traffic crosses. This arrangement allows the deck to be level or to arc upward for additional clearance, like other suspension bridge types, this type often is constructed without falsework. The suspension cables must be anchored at each end of the bridge, the main cables continue beyond the pillars to deck-level supports, and further continue to connections with anchors in the ground. The roadway is supported by vertical suspender cables or rods, called hangers, in the latter case there will be very little arc in the outboard main cables. The earliest suspension bridges were ropes slung across a chasm, with a deck possibly at the level or hung below the ropes such that the rope had a catenary shape. The Tibetan saint and bridge-builder Thangtong Gyalpo originated the use of chains in his version of simple suspension bridges. In 1433, Gyalpo built eight bridges in eastern Bhutan, the last surviving chain-linked bridge of Gyalpos was the Thangtong Gyalpo Bridge in Duksum en route to Trashi Yangtse, which was finally washed away in 2004. Gyalpos iron chain bridges did not include a deck bridge which is the standard on all modern suspension bridges today. Instead, both the railing and the layer of Gyalpos bridges used wires. The stress points that carried the screed were reinforced by the iron chains, before the use of iron chains it is thought that Gyalpo used ropes from twisted willows or yak skins. He may have also used tightly bound cloth, the first American iron chain suspension bridge was the Jacobs Creek Bridge in Westmoreland County, Pennsylvania, designed by inventor James Finley. Finleys bridge was the first to all of the necessary components of a modern suspension bridge. Finley patented his design in 1808, and published it in the Philadelphia journal, The Port Folio, in 1810. Early British chain bridges included the Dryburgh Abbey Bridge and 137 m Union Bridge, with rapidly increasing to 176 m with the Menai Bridge. The first chain bridge on the European continent was the Chain Bridge in Nuremberg, the Clifton Suspension Bridge is one of the longest of the parabolic arc chain type
16.
Molasse
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The term molasse refers to sandstones, shales and conglomerates that form as terrestrial or shallow marine deposits in front of rising mountain chains. The molasse deposits accumulate in a basin, especially on top of flysch—like, for example. These deposits are typically the non-marine alluvial and fluvial sediments of lowlands, sedimentation stops when the orogeny stops, or when the mountains have eroded flat. The molasse can sometimes fill an foreland basin, creating a nearly flat depositional surface. Molasse can be very thick near the front, but usually thins out towards the interior of a craton, such massive
17.
Bornes Massif
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The Bornes Massif is a mountainous massif in the north French Prealps in the département of Haute-Savoie. It has 20 peaks higher than 2000 m and is a destination for winter sports. The Massif is the source of the celebrated cheese Reblochon, the name Aravis Massif is also used to refer to the whole massif, possibly an effect of tourist marketing. As with all the prealpine massifs, the Aravis chain is formed of limestone. The massif benefits from exceptional snow considering its moderate altitude, the stations are first and foremost mountain villages where there remains significant farming activity. The Glières Plateau is likewise a well-known site for cross-country skiing, the massif is the source of reblochon, the famous cheese. Reblochon was first made in Le Grand-Bornand, and is now produced in large quantities using traditional methods in the massifs valleys, two important markets are held weekly at Thônes and at Le Grand-Bornand. There is also a wood industry. Geography of the Alps Geology of the Bornes Massif Mount Saxonnex The ancient glaciers of the Bornes Massif Bornes Massif on Google map
18.
Erosion
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In earth science, erosion is the action of surface processes that remove soil, rock, or dissolved material from one location on the Earths crust, then transport it away to another location. Eroded sediment or solutes may be transported just a few millimetres, the rates at which such processes act control how fast a surface is eroded. Feedbacks are also possible between rates of erosion and the amount of eroded material that is carried by, for example. Processes of erosion that produce sediment or solutes from a place contrast with those of deposition, while erosion is a natural process, human activities have increased by 10-40 times the rate at which erosion is occurring globally. At well-known agriculture sites such as the Appalachian Mountains, intensive farming practices have caused erosion up to 100x the speed of the rate of erosion in the region. Excessive erosion causes both on-site and off-site problems, on-site impacts include decreases in agricultural productivity and ecological collapse, both because of loss of the nutrient-rich upper soil layers. In some cases, the end result is desertification. Off-site effects include sedimentation of waterways and eutrophication of bodies, as well as sediment-related damage to roads. Intensive agriculture, deforestation, roads, anthropogenic climate change and urban sprawl are amongst the most significant human activities in regard to their effect on stimulating erosion, however, there are many prevention and remediation practices that can curtail or limit erosion of vulnerable soils. Rainfall, and the surface runoff which may result from rainfall, produces four types of soil erosion, splash erosion, sheet erosion, rill erosion. Splash erosion is generally seen as the first and least severe stage in the erosion process. In splash erosion, the impact of a falling raindrop creates a crater in the soil. The distance these soil particles travel can be as much as 0.6 m vertically and 1.5 m horizontally on level ground. If the soil is saturated, or if the rate is greater than the rate at which water can infiltrate into the soil. If the runoff has sufficient flow energy, it will transport loosened soil particles down the slope, sheet erosion is the transport of loosened soil particles by overland flow. Rill erosion refers to the development of small, ephemeral concentrated flow paths which function as both sediment source and sediment delivery systems for erosion on hillslopes, generally, where water erosion rates on disturbed upland areas are greatest, rills are active. Flow depths in rills are typically of the order of a few centimetres or less and this means that rills exhibit hydraulic physics very different from water flowing through the deeper, wider channels of streams and rivers. Gully erosion occurs when water accumulates and rapidly flows in narrow channels during or immediately after heavy rains or melting snow
19.
Limestone
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Limestone is a sedimentary rock, composed mainly of skeletal fragments of marine organisms such as coral, forams and molluscs. Its major materials are the minerals calcite and aragonite, which are different crystal forms of calcium carbonate, about 10% of sedimentary rocks are limestones. The solubility of limestone in water and weak acid solutions leads to karst landscapes, most cave systems are through limestone bedrock. The first geologist to distinguish limestone from dolomite was Belsazar Hacquet in 1778, like most other sedimentary rocks, most limestone is composed of grains. Most grains in limestone are skeletal fragments of organisms such as coral or foraminifera. Other carbonate grains comprising limestones are ooids, peloids, intraclasts and these organisms secrete shells made of aragonite or calcite, and leave these shells behind when they die. Limestone often contains variable amounts of silica in the form of chert or siliceous skeletal fragment, some limestones do not consist of grains at all, and are formed completely by the chemical precipitation of calcite or aragonite, i. e. travertine. Secondary calcite may be deposited by supersaturated meteoric waters and this produces speleothems, such as stalagmites and stalactites. Another form taken by calcite is oolitic limestone, which can be recognized by its granular appearance, the primary source of the calcite in limestone is most commonly marine organisms. Some of these organisms can construct mounds of rock known as reefs, below about 3,000 meters, water pressure and temperature conditions cause the dissolution of calcite to increase nonlinearly, so limestone typically does not form in deeper waters. Limestones may also form in lacustrine and evaporite depositional environments, calcite can be dissolved or precipitated by groundwater, depending on several factors, including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits a characteristic called retrograde solubility, in which it becomes less soluble in water as the temperature increases. Impurities will cause limestones to exhibit different colors, especially with weathered surfaces, Limestone may be crystalline, clastic, granular, or massive, depending on the method of formation. Crystals of calcite, quartz, dolomite or barite may line small cavities in the rock, when conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together, or it can fill fractures. Travertine is a banded, compact variety of limestone formed along streams, particularly there are waterfalls. Calcium carbonate is deposited where evaporation of the leaves a solution supersaturated with the chemical constituents of calcite. Tufa, a porous or cellular variety of travertine, is found near waterfalls, coquina is a poorly consolidated limestone composed of pieces of coral or shells. During regional metamorphism that occurs during the building process, limestone recrystallizes into marble
20.
Canyon
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A canyon or gorge is a deep cleft between escarpments or cliffs resulting from the erosive activity of a river over geologic timescales. A canyon may also refer to a rift between two peaks, such as those in ranges including the Rocky Mountains, the Alps. Usually a river or stream and erosion carve out such splits between mountains, examples of mountain-type canyons are Provo Canyon in Utah or Yosemite National Park in Californias Sierra Nevada. Canyons within mountains, or gorges that have an opening on one side are called box canyons. Slot canyons are very narrow canyons, often with smooth walls, steep-sided valleys in the seabed of the continental slope underwater are referred to as submarine canyons. Unlike canyons on land, submarine canyons are thought to be formed by turbidity currents, the word canyon is Spanish in origin, with the same meaning. The word canyon is used in North America while the words gorge and ravine are used in Europe and Oceania, though gorge. In the United States, place names generally use canyon in the southwest and gorge in the northeast, in Canada, a gorge is usually narrow while a ravine is more open and often wooded. The military-derived word defile is occasionally used in the United Kingdom, most canyons were formed by a process of long-time erosion from a plateau or table-land level. The cliffs form because harder rock strata that are resistant to erosion, Canyons are much more common in arid than in wet areas because physical weathering has a more localized effect in arid zones. The wind and water from the combine to erode and cut away less resistant materials such as shales. The freezing and expansion of water also serves to help form canyons, water seeps into cracks between the rocks and freezes, pushing the rocks apart and eventually causing large chunks to break off the canyon walls, in a process known as frost wedging. Canyon walls are formed of resistant sandstones or granite. Sometimes large rivers run through canyons as the result of geological uplift. These are called entrenched rivers, because they are unable to alter their course. In the United States, the Colorado River in the Southwest, Canyons often form in areas of limestone rock. As limestone is soluble to an extent, cave systems form in the rock. When these collapse, a canyon is left, as in the Mendip Hills in Somerset and Yorkshire Dales in Yorkshire, England
21.
Climbing
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Climbing is the activity of using ones hands, feet, or any other part of the body to ascend a steep object. It is done recreationally, competitively, in trades that rely on it and it is done indoors and out, on natural and manmade structures. Climbing activities include, Bouldering, Ascending boulders or small outcrops, often with climbing shoes, canyoneering, Climbing along canyons for sport or recreation. Chalk climbing, Ascending chalk cliffs uses some of the techniques as ice climbing. Competition Climbing, A formal, competitive sport of recent origins, competition Climbing has three major disciplines, Lead, Bouldering and Speed. Ice climbing, Ascending ice or hard snow formations using special equipment, usually ice axes, techniques of protecting the climber are similar to those of rock climbing, with protective devices adapted to frozen conditions. Indoor climbing, Top roping, lead climbing, and bouldering artificial walls with bolted holds in a climbing gym, mountaineering, Ascending mountains for sport or recreation. It often involves rock and/or ice climbing, pole climbing, Climbing poles and masts without equipment. Lumberjack tree-trimming and competitive tree-trunk or pole climbing for speed using spikes, rock climbing, Ascending rock formations, often using climbing shoes and a chalk bag. Equipment such as ropes, bolts, nuts, hexes and camming devices are normally employed, rope access, Industrial climbing, usually abseiling, as an alternative to scaffolding for short works on exposed structures. Rope climbing, Climbing a short, thick rope for speed, not to be confused with roped climbing, as in rock or ice climbing. Scrambling which includes rock climbing, and is considered part of hillwalking. Sport climbing is a form of climbing that relies on permanent anchors fixed to the rock. Top roping, Ascending a rock climbing route protected by a rope anchored at the top and protected by a belayer below Traditional climbing is a form of climbing without fixed anchors and bolts. Climbers place removable protection such as camming devices, nuts, free solo climbing, Climbing without ropes or protection. Tree climbing, Recreationally ascending trees using ropes and other protective equipment, a tower climber is a professional who climbs broadcasting or telecommunication towers or masts for maintenance or repair. Rock, ice and tree climbing all usually use ropes for safety or aid, pole climbing and rope climbing were among the first exercises to be included in the origins of modern gymnastics in the late 18th century and early 19th century
22.
Magdalenian
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The Magdalenian refers to one of the later cultures of the Upper Paleolithic in western Europe, dating from around 17,000 to 12,000 years ago. It is named after the site of La Madeleine, a rock shelter located in the Vézère valley, commune of Tursac. The culture was geographically widespread, and later Magdalenian sites have found from Portugal in the west to Poland in the east. It is the epoch of Gabriel de Mortillets cave chronology system. The Magdalenian epoch was a one, represented by numerous stations, whose contents show progress in the arts. It was characterized by a cold and dry climate, the existence of humans in association with the reindeer, the use of bone and ivory for various implements, already begun in the preceding Solutrian epoch, was much increased, and the period is essentially a Bone age. The bone instruments are varied, spear-points, harpoon-heads, borers, hooks. Most remarkable is the evidence La Madeleine affords of prehistoric art, numbers of bones, reindeer antlers and animal teeth were found, with rude pictures, carved or etched on them, of seals, fishes, reindeer, mammoths and other creatures. The man is naked which, together with the snake, suggests a warm climate, the fauna of the Madelenian epoch seems, indeed, to have included tigers and other tropical species side by side with reindeer, blue foxes, Arctic hares and other polar creatures. Madelenian humans appears to have been of low stature, dolichocephalic, with low retreating forehead, the culture spans approximatively from 17,000 to 12,000 BP, toward the end of the last ice age. The Magdalenian tool culture is characterised by regular blade industries struck from carinated cores, typologically, the Magdalenian is divided into six phases which are generally agreed to have chronological significance. Similarly, finds from the forest of Beauregard near Paris often have been suggested as belonging to the earliest Magdalenian, the earliest Magdalenian sites are all found in France. The Epigravettian is a similar culture appearing at the time in Italy, the Balkans, Moldavia, Romania. The later phases of the Magdalenian are also synonymous with the human re-settlement of north-western Europe after the Last Glacial Maximum during the Late Glacial Maximum, research in Switzerland, southern Germany, and Belgium has provided AMS radiocarbon dating to support this. Being hunter gatherers, Magdalenians did not simply re-settle permanently in north-west Europe, however, as they often followed herds, by the end of the Magdalenian, the lithic technology shows a pronounced trend toward increased microlithisation. The bone harpoons and points have the most distinctive chronological markers within the typological sequence, as well as flint tools, the Magdalenians are best known for their elaborate worked bone, antler, and ivory that served both functional and aesthetic purposes, including perforated batons. Cave sites such as the world famous Lascaux contain the best known examples of Magdalenian cave art, in northern Spain and south west France this tool culture was superseded by the Azilian culture. In northern Europe a slightly different situation exists, with different variants of the Tjongerian techno-complex following it
23.
Veyrier
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Veyrier is a municipality of the Canton of Geneva, Switzerland. Veyrier has an area, as of 2009, of 6.5 square kilometers, of this area,2.17 km2 or 33. 4% is used for agricultural purposes, while 0.9 km2 or 13. 8% is forested. Of the rest of the land,3.29 km2 or 50. 6% is settled,0.17 km2 or 2. 6% is either rivers or lakes. Of the built up area, housing and buildings made up 34. 6%, while parks, green belts and sports fields made up 6. 3%. Out of the land,12. 6% of the total land area is heavily forested and 1. 2% is covered with orchards or small clusters of trees. Of the agricultural land,26. 9% is used for growing crops and 3. 4% is pastures, all the water in the municipality is flowing water. The municipality includes the localities of Pinchat, Vessy and Sierne and it is bordered by Chêne-Bougeries, Thônex, Troinex, Plan-les-Ouates, Carouge, Geneva, and the French municipality of Étrembières in Haute-Savoie. Veyrier has a population of 11,273, as of 2008,24. 0% of the population are resident foreign nationals. Over the last 10 years the population has changed at a rate of 10. 1% and it has changed at a rate of 12. 8% due to migration and at a rate of -3. 1% due to births and deaths. Most of the population speaks French, with German being second most common, There are 158 people who speak Italian and 1 person who speaks Romansh. As of 2008, the distribution of the population was 49. 0% male and 51. 0% female. The population was made up of 3,600 Swiss men and 1,307 non-Swiss men, There were 3,878 Swiss women and 1,233 non-Swiss women. Of the population in the municipality 1,488 or about 16. 7% were born in Veyrier and lived there in 2000. There were 2,931 or 33. 0% who were born in the canton, while 1,470 or 16. 5% were born somewhere else in Switzerland. In 2008 there were 54 live births to Swiss citizens and 31 births to non-Swiss citizens, ignoring immigration and emigration, the population of Swiss citizens decreased by 48 while the foreign population increased by 12. There were 24 Swiss men and 32 Swiss women who emigrated from Switzerland, at the same time, there were 41 non-Swiss men and 45 non-Swiss women who immigrated from another country to Switzerland. The total Swiss population change in 2008 was an increase of 2 and this represents a population growth rate of 1. 3%. The age distribution of the population is children and teenagers make up 27% of the population, while adults make up 58. 6%, as of 2000, there were 3,605 people who were single and never married in the municipality
24.
Partridge
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Partridges are medium-sized non-migratory gamebirds, with a wide native distribution throughout the Old World, including Europe, Asia, and parts of Africa. They are sometimes grouped in the Perdicinae subfamily of the Phasianidae and these are medium-sized birds, intermediate between the larger pheasants and the smaller quails. Partridges are native to the steppes of Europe, Asia, Africa. Nowadays they are found nesting on agricultural land. They nest on the ground and have a diet consisting of seeds, species such as the grey partridge and the red-legged partridge are popular as game birds, and are often reared in captivity and released for the purpose of hunting. For the same reason, they have been introduced into areas of North America. According to Greek legend, the first partridge appeared when Daedalus threw his nephew, Perdix, supposedly mindful of his fall, the bird does not build its nest in the trees, nor take lofty flights and avoids high places. The most famous reference to the partridge is in the Christmas carol, the first gift listed is a partridge in a pear tree, and these words end each verse. Since partridges are unlikely to be seen in pear-trees it has suggested that the text in a pear tree is a corruption of the French une perdrix. The partridge has also used as a symbol that represents Kurdish nationalism. Sherko Kurmanj discusses the paradox of symbols in Iraq as an attempt to make a distinction between the Kurds and the Arabs. He says that while Iraqis generally regards the palm tree, falcon, and sword as their symbols, the Kurds consider the Oak, Partridge
25.
Reindeer
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This includes both sedentary and migratory populations. While overall widespread and numerous, some of its subspecies are rare, for this reason, it is considered to be vulnerable by the IUCN. Reindeer vary considerably in colour and size, both sexes can grow antlers annually, although the proportion of females that grow antlers varies greatly between population and season. Antlers are typically larger on males, hunting of wild reindeer and herding of semi-domesticated reindeer are important to several Arctic and Subarctic peoples. In traditional festive legend, Santa Clauss reindeer pull a sleigh through the sky to help Santa Claus deliver gifts to children on Christmas Eve. The name Rangifer, which Carl Linnaeus chose for the genus, was used by Albertus Magnus in his De animalibus. This word may go back to a Saami word raingo, for the origin of the word tarandus, which Linnaeus chose as the specific epithet, he made reference to Ulisse Aldrovandis Quadrupedum omnium bisulcorum historia fol. However, Aldrovandi – and before him Konrad Gesner – thought that rangifer, in any case, the tarandos name goes back to Aristotle and Theophrastus – see In history below. Because of its importance to many cultures, Rangifer tarandus and some of its subspecies have names in many languages, the name rein is of Norse origin. The Finnish name poro may also stem from the same, the word deer was originally broader in meaning, but became more specific over time. In Middle English, der meant a wild animal of any kind. Cognates of Old English dēor in other dead Germanic languages have the sense of animal, such as Old High German tior, Old Norse djúr or dýr, Gothic dius, Old Saxon dier. The name caribou comes, through French, from Mikmaq qalipu, meaning snow shoveler, in Inuktitut, spoken in eastern Arctic North America, the caribou is known by the name tuktu. In the western North American Arctic, the used by the Iñupiat is tuttu. Across the range of a species, individuals may display considerable morphological, genetic, COSEWIC developed Designated Unit attribution to add to classifications already in use. The species taxonomic name Rangifer tarandus was defined by Carl Linnaeus in 1758, the subspecies taxonomic name, Rangifer tarandus caribou was defined by Gmelin in 1788. Based on Banfields often-cited A Revision of the Reindeer and Caribou, Genus Rangifer, R. t. caboti, R. t. osborni and R. t. terraenovae were considered invalid and included in R. t. caribou. Some recent authorities have considered them all valid, even suggesting that they are quite distinct and he affirms that true woodland caribou is very rare, in very great difficulties and requires the most urgent of attention
26.
Horse
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The horse is one of two extant subspecies of Equus ferus. It is an ungulate mammal belonging to the taxonomic family Equidae. The horse has evolved over the past 45 to 55 million years from a small multi-toed creature, Eohippus, into the large, humans began to domesticate horses around 4000 BC, and their domestication is believed to have been widespread by 3000 BC. Horses in the subspecies caballus are domesticated, although some domesticated populations live in the wild as feral horses. There is an extensive, specialized vocabulary used to describe equine-related concepts, covering everything from anatomy to life stages, size, colors, markings, breeds, locomotion, and behavior. Horses anatomy enables them to use of speed to escape predators and they have a well-developed sense of balance. Related to this need to flee from predators in the wild is an unusual trait, female horses, called mares, carry their young for approximately 11 months, and a young horse, called a foal, can stand and run shortly following birth. Most domesticated horses begin training under saddle or in harness between the ages of two and four and they reach full adult development by age five, and have an average lifespan of between 25 and 30 years. There are more than 300 breeds of horse in the world today, horses were historically used in warfare, from which a wide variety of riding and driving techniques developed, using many different styles of equipment and methods of control. Many products are derived from horses, including meat, milk, hide, hair, bone, humans provide domesticated horses with food, water and shelter, as well as attention from specialists such as veterinarians and farriers. Specific terms and specialized language are used to describe equine anatomy, different life stages, colors, depending on breed, management and environment, the modern domestic horse has a life expectancy of 25 to 30 years. Uncommonly, a few animals live into their 40s and, occasionally, the oldest verifiable record was Old Billy, a 19th-century horse that lived to the age of 62. In modern times, Sugar Puff, who had listed in Guinness World Records as the worlds oldest living pony. The exception is in endurance riding, where the age to compete is based on the animals actual calendar age. The following terminology is used to describe horses of various ages, Colt, a common terminology error is to call any young horse a colt, when the term actually only refers to young male horses. Filly, A female horse under the age of four, foal, A horse of either sex less than one year old. A nursing foal is sometimes called a suckling and a foal that has been weaned is called a weanling, most domesticated foals are weaned at five to seven months of age, although foals can be weaned at four months with no adverse physical effects. Gelding, A castrated male horse of any age, mare, A female horse four years old and older
27.
Marmot
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Marmots are large squirrels in the genus Marmota, of which there are 15 species. Other species prefer rough grassland and can be found widely across North America, the similarly-sized but more social prairie dog is not classified in the genus Marmota but in the related genus Cynomys. Marmots typically live in burrows, and hibernate there through the winter, most marmots are highly social and use loud whistles to communicate with one another, especially when alarmed. Marmots mainly eat greens and many types of grasses, berries, lichens, mosses, roots, the following is a list of all Marmota species recognized by Thorington and Hoffman plus the recently defined M. kastschenkoi. They divide marmots into two subgenera, the etymology of the term marmot is uncertain. It may have arisen from the Gallo-Romance prefix marm-, meaning to mumble or murmur, another possible origin is post-classical Latin, mus montanus, meaning mountain mouse. Beginning in 2010, Alaska celebrates February 2 as Marmot Day, the Marmot Burrow International Marmot Network
28.
Flint
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Flint is a hard, sedimentary cryptocrystalline form of the mineral quartz, categorized as a variety of chert. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks, inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white, from a petrological point of view, flint refers specifically to the form of chert which occurs in chalk or marly limestone. Similarly, common chert occurs in limestone, the exact mode of formation of flint is not yet clear but it is thought that it occurs as a result of chemical changes in compressed sedimentary rock formations, during the process of diagenesis. One hypothesis is that a gelatinous material fills cavities in the sediment, such as bored by crustaceans or molluscs. This hypothesis certainly explains the shapes of flint nodules that are found. The source of dissolved silica in the media could be the spicules of silicious sponges. Certain types of flint, such as that from the south coast of England, pieces of coral and vegetation have been found preserved like amber inside the flint. Thin slices of the stone often reveal this effect, puzzling giant flint formations known as paramoudra and flint circles are found around Europe but especially in Norfolk, England on the beaches at Beeston Bump and West Runton. Flint sometimes occurs in large flint fields in Jurassic or Cretaceous beds, flint was used in the manufacture of tools during the Stone Age as it splits into thin, sharp splinters called flakes or blades when struck by another hard object. This process is referred to as knapping, flint mining is attested since the Palaeolithic, but became more common since the Neolithic. When struck against steel, a flint edge will produce sparks, the hard flint edge shaves off a particle of the steel that exposes iron which reacts with oxygen from the atmosphere and can ignite the proper tinder. Prior to the availability of steel, rocks of pyrite would be used along with the flint. These methods are popular in woodcraft, bushcraft, and among those who wish to use traditional skills, a later, major use of flint and steel was in the flintlock mechanism, used primarily in flintlock firearms, but also used on dedicated fire-starting tools. The sparks ignite the powder and that flame, in turn, ignites the main charge, propelling the ball, bullet. While the military use of the flintlock declined after the adoption of the cap from the 1840s onward, flintlock rifles. Flint and steel used to strike sparks were superseded by ferrocerium and this man-made material, when scraped with any hard, sharp edge, produces sparks that are much hotter than obtained with natural flint and steel, allowing use of a wider range of tinders. Because it can produce sparks when wet and can start fires when used correctly, ferrocerium is used in many cigarette lighters, where it is referred to as flint
29.
Dolmen
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A dolmen is a type of single-chamber megalithic tomb, usually consisting of two or more vertical megaliths supporting a large flat horizontal capstone, although there are also more complex variants. Most date from the early Neolithic, Dolmens were typically covered with earth or smaller stones to form a tumulus. In many instances, that covering has weathered away, leaving only the skeleton of the burial mound intact. It remains unclear when, why, and by whom the earliest dolmens were made, the oldest known dolmens are in Western Europe, where they were set in place around 7,000 years ago. Archaeologists still do not know who erected these dolmens, which makes it difficult to know why they did it and they are generally all regarded as tombs or burial chambers, despite the absence of clear evidence for this. Human remains, sometimes accompanied by artefacts, have found in or close to the dolmens which could be scientifically dated using radiocarbon dating. However, it has been impossible to prove that these date from the time when the stones were originally set in place. The word dolmen has a confused history, the word entered archaeology when Théophile Corret de la Tour dAuvergne used it to describe megalithic tombs in his Origines gauloises using the spelling dolmin. The name was derived from a Breton language term meaning stone table but doubt has been cast on this. Nonetheless it has now replaced cromlech as the usual English term in archaeology, granja is used in Portugal, Galicia, and Spain. The rarer forms anta and ganda also appear, in the Basque Country, they are attributed to the jentilak, a race of giants. The etymology of the German, Hünenbett, Hünengrab and Dutch, of other Celtic languages, Welsh, cromlech was borrowed into English and quoit is commonly used in English in Cornwall. Great dolmen Passage grave Polygonal dolmen Rectangular, enlarged or extended dolmen Simple dolmen Korean dolmens exhibit a distinct from the Atlantic European dolmen. The largest concentration of dolmens in the world is found on the Korean Peninsula, with an estimated 35,000 dolmens, Korea alone accounts for nearly 40% of the world’s total. Three specific UNESCO World Heritage sites at Gochang, Hwasun and Ganghwa by themselves account for over 1,000 dolmens, the Korean word for dolmen is goindol supported stone. Serious studies of the Korean megalithic monuments were not undertaken until relatively recently, after 1945, new research is being conducted by Korean scholars. In 1981 a curator of National Museum of Korea, Gongil Ji, the boundary between them falls at the Bukhan River although examples of both types are found on either side. Korean dolmens can also be divided into three types, the table type, the go-table type and the unsupported capstone type
30.
Neolithic
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It ended when metal tools became widespread. The Neolithic is a progression of behavioral and cultural characteristics and changes, including the use of wild and domestic crops, the beginning of the Neolithic culture is considered to be in the Levant about 10, 200–8800 BC. It developed directly from the Epipaleolithic Natufian culture in the region, whose people pioneered the use of wild cereals, which then evolved into true farming. The Natufian period was between 12,000 and 10,200 BC, and the so-called proto-Neolithic is now included in the Pre-Pottery Neolithic between 10,200 and 8800 BC. By 10, 200–8800 BC, farming communities arose in the Levant and spread to Asia Minor, North Africa, Mesopotamia is the site of the earliest developments of the Neolithic Revolution from around 10,000 BC. Early Neolithic farming was limited to a range of plants, both wild and domesticated, which included einkorn wheat, millet and spelt, and the keeping of dogs, sheep. By about 6900–6400 BC, it included domesticated cattle and pigs, the establishment of permanently or seasonally inhabited settlements, not all of these cultural elements characteristic of the Neolithic appeared everywhere in the same order, the earliest farming societies in the Near East did not use pottery. Early Japanese societies and other East Asian cultures used pottery before developing agriculture, unlike the Paleolithic, when more than one human species existed, only one human species reached the Neolithic. The term Neolithic derives from the Greek νέος néos, new and λίθος líthos, stone, the term was invented by Sir John Lubbock in 1865 as a refinement of the three-age system. In the Middle East, cultures identified as Neolithic began appearing in the 10th millennium BC, early development occurred in the Levant and from there spread eastwards and westwards. Neolithic cultures are attested in southeastern Anatolia and northern Mesopotamia by around 8000 BC. The total excavated area is more than 1,200 square yards, the Neolithic 1 period began roughly 10,000 years ago in the Levant. A temple area in southeastern Turkey at Göbekli Tepe dated around 9500 BC may be regarded as the beginning of the period. This site was developed by nomadic tribes, evidenced by the lack of permanent housing in the vicinity. At least seven stone circles, covering 25 acres, contain limestone pillars carved with animals, insects, Stone tools were used by perhaps as many as hundreds of people to create the pillars, which might have supported roofs. Other early PPNA sites dating to around 9500–9000 BC have been found in Jericho, Israel, Gilgal in the Jordan Valley, the start of Neolithic 1 overlaps the Tahunian and Heavy Neolithic periods to some degree. The major advance of Neolithic 1 was true farming, in the proto-Neolithic Natufian cultures, wild cereals were harvested, and perhaps early seed selection and re-seeding occurred. The grain was ground into flour, emmer wheat was domesticated, and animals were herded and domesticated
31.
Bronze Age
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The Bronze Age is a historical period characterized by the use of bronze, proto-writing, and other early features of urban civilization. The Bronze Age is the principal period of the three-age Stone-Bronze-Iron system, as proposed in modern times by Christian Jürgensen Thomsen. An ancient civilization is defined to be in the Bronze Age either by smelting its own copper and alloying with tin, arsenic, or other metals, or by trading for bronze from production areas elsewhere. Copper-tin ores are rare, as reflected in the fact there were no tin bronzes in Western Asia before trading in bronze began in the third millennium BC. Worldwide, the Bronze Age generally followed the Neolithic period, with the Chalcolithic serving as a transition, although the Iron Age generally followed the Bronze Age, in some areas, the Iron Age intruded directly on the Neolithic. Bronze Age cultures differed in their development of the first writing, according to archaeological evidence, cultures in Mesopotamia and Egypt developed the earliest viable writing systems. The overall period is characterized by use of bronze, though the place and time of the introduction. Human-made tin bronze technology requires set production techniques, tin must be mined and smelted separately, then added to molten copper to make bronze alloy. The Bronze Age was a time of use of metals. The dating of the foil has been disputed, the Bronze Age in the ancient Near East began with the rise of Sumer in the 4th millennium BC. Societies in the region laid the foundations for astronomy and mathematics, the usual tripartite division into an Early, Middle and Late Bronze Age is not used. Instead, a division based on art-historical and historical characteristics is more common. The cities of the Ancient Near East housed several tens of thousands of people, ur in the Middle Bronze Age and Babylon in the Late Bronze Age similarly had large populations. The earliest mention of Babylonia appears on a tablet from the reign of Sargon of Akkad in the 23rd century BC, the Amorite dynasty established the city-state of Babylon in the 19th century BC. Over 100 years later, it took over the other city-states. Babylonia adopted the written Semitic Akkadian language for official use, by that time, the Sumerian language was no longer spoken, but was still in religious use. Elam was an ancient civilization located to the east of Mesopotamia, in the Old Elamite period, Elam consisted of kingdoms on the Iranian plateau, centered in Anshan, and from the mid-2nd millennium BC, it was centered in Susa in the Khuzestan lowlands. Its culture played a role in the Gutian Empire and especially during the Achaemenid dynasty that succeeded it
32.
Oppidum
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An oppidum is a large fortified Iron Age settlement. They continued in use until the Romans began conquering Europe, north of the River Danube, where the population remained independent from Rome, oppida continued to be used into the 1st century AD. Oppidum is a Latin word meaning the settlement in any administrative area of ancient Rome. The word is derived from the earlier Latin ob-pedum, enclosed space, possibly from the Proto-Indo-European *pedóm-, in his Commentarii de Bello Gallico, Julius Caesar described the larger Celtic Iron Age settlements he encountered in Gaul during the Gallic Wars in 58 to 52 BC as oppida. Although he did not explicitly define what features qualified a settlement to be called an oppidum and they were important economic sites, places where goods were produced, stored and traded, and sometimes Roman merchants had settled and the Roman legions could obtain supplies. They were also political centres, the seat of authorities taking decisions that affected large numbers of people, Most of the places that Caesar called oppida were city-sized fortified settlements. However, Geneva, for example, was referred to as an oppidum, Caesar also refers to 20 oppida of the Bituriges and 12 of the Helvetii, twice the number of fortified settlements of these groups known today. That implies that Caesar likely counted some unfortified settlements as oppida, a similar ambiguity is in evidence in writing by the Roman historian Livy, who also used the word for both fortified and unfortified settlements. In his work Geographia, Ptolemy listed the coordinates of many Celtic settlements, however, research has shown many of the localisations of Ptolemy to be erroneous, making the identification of any modern location with the names he listed highly uncertain and speculative. An exception to that is the oppidum of Brenodurum at Bern, in particular, Dehn suggested defining an oppidum by four criteria, Size, The settlement has to have a minimum size, defined by Dehn as 30 hectares. Topography, Most oppida are situated on heights, but some are located on areas of land. Fortification, The settlement is surrounded by a wall, usually consisting of three elements, a facade of stone, a construction and an earthen rampart at the back. Chronology, The settlement dates from the late Iron Age, the last two centuries BC and they could be referred to as the first cities north of the Alps. The period of 2nd and 1st centuries BC places them in the known as La Tène. A notional minimum size of 15 to 25 hectares has often been suggested, however, the term is not always rigorously used, and it has been used to refer to any hill fort or circular rampart dating from the La Tène period. One of the effects of the inconsistency in definitions is that it is uncertain how many oppida were built, in European archaeology, the term oppida is also used more widely to characterize any fortified prehistoric settlement. For example, significantly older hill-top structures like the one at Glauberg have been called oppida, the Spanish word castro, also used in English, means a walled settlement or hill fort, and this word is often used interchangeably with oppidum by archaeologists. According to prehistorian John Collis oppida extend as far east as the Hungarian plain where other settlement types take over, central Spain has sites similar to oppida, but while they share features such as size and defensive ramparts the interior was arranged differently
33.
Lake Geneva
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Lake Geneva is a lake on the north side of the Alps, shared between Switzerland and France. It is one of the largest lakes in Western Europe and the largest on the course of the Rhône,59. 53% of it comes under the jurisdiction of Switzerland, and 40. 47% under France. Lake Geneva has been explored by four submarines, the Auguste Piccard, forel, both built by Jacques Piccard, and the two Mir submersibles. Following the rise of Geneva it became Lac de Genève, in the 18th century, Lac Léman was revived in French and is the customary name in that language. In contemporary English, the name Lake Geneva is predominant, a note on pronunciation, English, Lake Geneva /ˌleɪk dʒᵻˈniːvə/ French, le lac Léman, le Léman or le lac de Genève German, Genfersee or Genfer See Italian, Lago Lemano, Lago di Ginevra. The Chablais Alps border is its southern shore, the western Bernese Alps lie over its eastern side, the high summits of Grand Combin and Mont Blanc are visible from some places. Compagnie Générale de Navigation sur le lac Léman operates boats on the lake, the lake lies on the course of the Rhône. Other tributaries are La Dranse, LAubonne, La Morges, La Venoge, La Vuachère, Lake Geneva is the largest body of water in Switzerland, and greatly exceeds in size all others that are connected with the main valleys of the Alps. It is in the shape of a crescent, with the horns pointing south, the northern shore being 95 km, the crescent form was more regular in a recent geological period, when the lake extended to Bex, about 18 km south of Villeneuve. The lakes surface is the lowest point of the cantons of Valais, the culminating point of the lakes drainage basin is Monte Rosa at 4,634 metres above sea level. The beauty of the shores of the lake and of the sites of many of the places near its banks has long been celebrated, however, it is only from the eastern end of the lake, between Vevey and Villeneuve, that the scenery assumes an Alpine character. The shore between Nyon and Lausanne is called La Côte because it is flatter, between Lausanne and Vevey it is called Lavaux and is famous for its hilly vineyards. The average surface elevation of 372 m above sea level is controlled by the Seujet Dam in Geneva, simulations indicate that the Tauredunum event was most likely caused by a massive landslide near the Rhône delta, which caused a wave eight meters high to reach Geneva within 70 minutes. In 888 the town was part of the new Kingdom of Burgundy, in the late 1960s, pollution made it dangerous to swim at some beaches of the lake, indeed, visibility under water was near zero. By the 1980s, intense environmental pollution had almost wiped out all the fish, today, pollution levels have been dramatically cut back, and it is again considered safe to swim in the lake. Major leisure activities practiced include sailing, wind surfing, boating, rowing, on a scientific footnote, in 1827, Lake Geneva was the site for the first measurement of the speed of sound in water. The loud airborne sound coupled into the lake, establishing an underwater sound that could be measured at a distance. The flash of the exploding gunpowder provided the starting cue for the timepiece
34.
Swiss Plateau
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The Swiss Plateau or Central Plateau constitutes one of the three major landscapes in Switzerland alongside the Jura Mountains and the Swiss Alps. It covers about 30% of the Swiss surface and it comprises the regions between the Jura and the Alps, partly flat but mostly hilly, and lies at an average height between 400 and 700 m AMSL. It is by far the most densely populated region of Switzerland, in the north and northwest, the Swiss Plateau is sharply delimited geographically and geologically by the Jura Mountains. In the south, there is no border with the Alps. Usually, the rising of the terrain to altitudes above 1500 metres AMSL, however, if a division into the three main regions Jura Mountains, Swiss Plateau and Alps is considered, the Alpine foreland belongs clearly to the Swiss Plateau. In the southwest, the Swiss Plateau is confined by Lake Geneva, in the northeast, by Lake Constance, geologically, the Swiss Plateau is part of a larger basin that extends beyond the border of Switzerland. At its southwestern end, in France, the plateau, in the Genevois, ends at Chambéry where Jura, at the other side of the Lake Constance, the plateau continues in the German and Austrian Pre-Alps. Many cantons of Switzerland include a part in the Swiss Plateau, the geological layers of the Swiss Plateau are relatively well known. Around 2500 –3000 metres below the surface, but considerably deeper near the Alps and it is covered by unfolded strata of Mesozoic sediments, which are part of the Helvetic nappes. Its depth gradually decreases from about 2.5 km in the west to 0.8 km in the east and these layers, like the ones of the Jura Mountains, were deposited in a relatively shallow sea, the Tethys Ocean. Above the Mesozoic layers, is the Molasse, consisting of conglomerate, sandstone, marl, the uppermost layer consists of gravel and glacial sediments that have been transported by the glaciers of the ice ages. Geologically the most important layer of the Swiss Plateau is the thick molasse sequence that accumulated at the border of the Alps due to the erosion of the concurrently uplifted mountains. The thickness of the molasse increases from west to east, the former alpine rivers built huge fans of sediment at the foot of the mountains. The eroded material has been sorted by grain size, the coarse material was predominantly deposited near the Alps. In the middle of the plateau, there are sandstones and near the Jura, clays. During the Tertiary orogenic uplift, around 60 –40 millions years ago, through processes of rising and lowering that were brought by the folding of the Alps, the area was twice flooded by a sea. The corresponding sediments are distinguished as sea molasse and freshwater molasse, even though the latter consists rather of fluvial, lower sea molasse, The limestone plateau subsided gradually, and a shallow sea invaded, spreading east to the Carpathian Mountains. The sediments consisted of fine-grained sands, clay and marl, there were no conglomerate fans since the proper Alpine folding began only at the end of that period
35.
Lake Annecy
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Lake Annecy is a perialpine lake in Haute-Savoie in France. It is the third largest lake in France, after the Lac du Bourget and Lac de Grand-Lieu and it is known as Europes cleanest lake because of strict environmental regulations introduced in the 1960s. It is a popular tourist destination known for its swimming and water sports, the lake was formed about 18,000 years ago, at the time the large alpine glaciers melted. It is fed by small rivers from the surrounding mountains, and from a powerful underwater source, the Boubioz. Menthon-Saint-Bernard Saint-Jorioz Sevrier Talloires Veyrier-du-Lac A cycle path goes partially around Lake Annecy past Sevrier and it has an aim to reach Albertville. The lake is around 14 km long, faverges Montmin Chevaline killings This article incorporates text from a publication now in the public domain, Chisholm, Hugh, ed. article name needed. Official website of Lake Annecy Association of the Friends of the Old Annecy Best Cycling Climbs from Lake Annecy
36.
Mont Blanc
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Mont Blanc or Monte Bianco, both meaning White Mountain, is the highest mountain in the Alps and the highest in Europe west of Russia after the Caucasus peaks. It rises 4,808 m above sea level and is ranked 11th in the world in topographic prominence, the mountain lies in a range called the Graian Alps, between the regions of Aosta Valley, Italy, and Savoie and Haute-Savoie, France. The location of the summit is on the line between the valleys of Ferret and Veny in Italy and the valleys of Montjoie, and Arve in France. The Mont Blanc massif is popular for mountaineering, hiking, skiing, the three towns and their communes which surround Mont Blanc are Courmayeur in Aosta Valley, Italy, and Saint-Gervais-les-Bains and Chamonix in Haute-Savoie, France. The latter town was the site of the first Winter Olympics, a cable car ascends and crosses the mountain range from Courmayeur to Chamonix, through the Col du Géant. The 11.6 km Mont Blanc Tunnel, constructed between 1957 and 1965, runs beneath the mountain and is a major transport route. The first recorded ascent of Mont Blanc was on 8 August 1786 by Jacques Balmat and this climb, initiated by Horace-Bénédict de Saussure, who gave a reward for the successful ascent, traditionally marks the start of modern mountaineering. The first woman to reach the summit was Marie Paradis in 1808, nowadays the summit is ascended by an average of 20,000 mountaineer-tourists each year. It could be considered an easy, yet arduous, ascent for someone who is well-trained and acclimatized to the altitude, from lAiguille du Midi, Mont Blanc seems quite close, being 1,000 m higher. Some routes require knowledge of mountaineering, a guide. All routes are long and arduous, involving delicate passages and the hazard of rock-fall or avalanche, climbers may also suffer altitude sickness, occasionally life threatening, particularly if they do not acclimatize to it. Since the French Revolution, the issue of the ownership of the summit has been debated, from 1416 to 1792, the entire mountain was within the Duchy of Savoy. In 1723 the Duke of Savoy, Victor Amadeus II, acquired the Kingdom of Sardinia, the resulting state of Sardinia was to become preeminent in the Italian unification. In September 1792, the French revolutionary Army of the Alps under Anne-Pierre de Montesquiou-Fézensac seized Savoy without much resistance, in a treaty of 15 May 1796, Victor Amadeus III of Sardinia was forced to cede Savoy and Nice to France. This act further states that the border should be visible from the town of Chamonix, however, neither the peak of the Mont Blanc is visible from Courmayeur nor the peak of the Mont Blanc de Courmayeur is visible from Chamonix because part of the mountains lower down obscure them. After the Napoleonic Wars, the Congress of Vienna restored the King of Sardinia in Savoy, Nice and Piedmont, his traditional territories, forty-five years later, after the Second Italian War of Independence, it was replaced by a new legal act. This act was signed in Turin on 24 March 1860 by Napoleon III and Victor Emmanuel II of Savoy, a demarcation agreement, signed on 7 March 1861, defined the new border. With the formation of Italy, for the first time Mont Blanc was located on the border of France, the 1860 act and attached maps are still legally valid for both the French and Italian governments
37.
Hiking
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Hiking is the preferred term, in Canada and the United States, for a long, vigorous walk, usually on trails, in the countryside, while the word walking is used for shorter, particularly urban walks. On the other hand, in the United Kingdom, and the Republic of Ireland, the word hiking is also often used in the UK, along with rambling, hillwalking, and fell walking. The term bushwalking is endemic to Australia, having been adopted by the Sydney Bush Walkers club in 1927, in New Zealand a long, vigorous walk or hike is called tramping. It is an activity with numerous hiking organizations worldwide. In the United States, Canada, the Republic of Ireland, a day hike refers to a hike that can be completed in a single day. However, in the United Kingdom, the walking is also used, as well as rambling. In Northern England, Including the Lake District and Yorkshire Dales, fellwalking describes hill or mountain walks, hiking sometimes involves bushwhacking and is sometimes referred to as such. This specifically refers to walking through dense forest, undergrowth, or bushes. In extreme cases of bushwhacking, where the vegetation is so dense that human passage is impeded, the Australian term bushwalking refers to both on and off-trail hiking. Common terms for hiking used by New Zealanders are tramping, walking or bushwalking, trekking is the preferred word used to describe multi-day hiking in the mountainous regions of India, Pakistan, Nepal, North America, South America, Iran and in the highlands of East Africa. Hiking a long-distance trail from end-to-end is also referred to as trekking, in North America, multi-day hikes, usually with camping, are referred to as backpacking. The idea of taking a walk in the countryside for pleasure developed in the 18th-century, in earlier times walking generally indicated poverty and was also associated with vagrancy. Thomas West, an English priest, popularized the idea of walking for pleasure in his guide to the Lake District of 1778. To this end he included various stations or viewpoints around the lakes, published in 1778 the book was a major success. Another famous early exponent of walking for pleasure, was the English poet William Wordsworth, in 1790 he embarked on an extended tour of France, Switzerland, and Germany, a journey subsequently recorded in his long autobiographical poem The Prelude. His famous poem Tintern Abbey was inspired by a visit to the Wye Valley made during a tour of Wales in 1798 with his sister Dorothy Wordsworth. Wordsworths friend Coleridge was another keen walker and in the autumn of 1799, he and Wordsworth undertook a three weeks tour of the Lake District. John Keats, who belonged to the generation of Romantic poets began, in June 1818, a walking tour of Scotland, Ireland
38.
Mountain bike
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A mountain bike or mountain bicycle is a bicycle designed for off-road cycling. Mountain bikes share similarities with other bikes, but incorporate features designed to enhance durability and these typically include suspension on the frame and fork, large knobby tires, more durable heavy duty wheels, more powerful brakes, and lower gear ratios needed for steep grades with poor traction. Mountain bikes are ridden on mountain trails, fire roads, logging roads, single tracks. These types of terrain commonly include rocks, washouts, ruts, loose sand, loose gravel, roots, Mountain bikes are built to handle this terrain and the obstacles that are found in it like logs, vertical drop offs, and smaller boulders. Each of these place different demands on the bike requiring different designs for optimal performance, MTB development has included an increase in suspension, typically up to 8 or 203mm, and gearing, up to 30 speeds, to facilitate both climbing and rapid descents. The original mountain bikes were modified heavy cruiser bicycles used for freewheeling down mountain trails, the sport became popular in the 1970s in Northern California, USA with riders using older single speed balloon tire bicycles to ride down rugged hillsides. Joe Breeze, a frame builder, used this idea. The 2006 documentary film, Klunkerz, A Film About Mountain Bikes, however, it was not until the late 1970s and early 1980s that road bicycle companies started to manufacture mountain bicycles using high-tech lightweight materials, such as M4 aluminium. The first production Mountain bike available was the 1979 Lawwill Pro Cruiser, one of the bikes that bridged the gap between BMX bikes and mountain bikes. The frame design was based on a frame that Don Koski fabricated from electrical conduit, mert Lawwill had Terry Knight of Oakland build the frames. The bikes sold for about $500 new and were made from 1979 though 1980. The first mass production mountain bike was the Specialized Stumpjumper, first produced in 1981. Mountain bikes can be divided into four categories based on configuration, Rigid, A bicycle with neither front nor rear suspension. Hard tail, A bicycle equipped with a fork. Soft tail, Having neither front nor rear suspension, as with a rigid and these designs are much more common in road bikes than mountain bikes. Dual or full suspension, A bicycle equipped with front and rear suspension. The front suspension is usually handled by a telescopic fork similar to that of a motorcycle, there are several different styles of mountain biking, usually defined by the terrain, and therefore bikes employed. Styles of mountain bike riding and mountain bikes have evolved rapidly in recent years leading to such as Freeride. Definitions for the most widely used terms are listed below, in the 1980s and early 1990s XC mountain bikes typically consisted of a lightweight steel hardtail frame with rigid forks
39.
Paragliding
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Paragliding is the recreational and competitive adventure sport of flying paragliders, lightweight, free-flying, foot-launched glider aircraft with no rigid primary structure. The pilot sits in a harness suspended below a fabric wing comprising a number of interconnected baffled cells. Wing shape is maintained by the lines, the pressure of air entering vents in the front of the wing. Despite not using an engine, paragliders flight can last many hours and cover many hundreds of kilometers, by skillful exploitation of sources of lift, the pilot may gain height, often climbing to altitudes of a few thousand meters. Jalbert advanced governable gliding parachutes with multi-cells and controls for lateral glide, in 1954, Walter Neumark predicted a time when a glider pilot would be able to launch himself by running over the edge of a cliff or down a slope. Whether on a holiday in Skye or ski-ing in the Alps. In 1961, the French engineer Pierre Lemoigne produced improved parachute designs that led to the Para-Commander, the PC had cutouts at the rear and sides that enabled it to be towed into the air and steered – leading to parasailing/parascending. He filed US Patent 3131894 on January 10,1963, about that same time, David Barish was developing the sail wing for recovery of NASA space capsules – slope soaring was a way of testing out. After tests on Hunter Mountain, New York, in September 1965, authors Patrick Gilligan and Bertrand Dubuis wrote the first flight manual, The Paragliding Manual in 1985, officially coining the word paragliding. These developments were combined in June 1978 by three friends, Jean-Claude Bétemps, André Bohn and Gérard Bosson, from Mieussy, Haute-Savoie, Bohn followed him and glided down to the football pitch in the valley 1000 metres below. From the 1980s, equipment has continued to improve, and the number of paragliding pilots, the first Paragliding World Championship was held in Verbier, Switzerland, in 1987, though the first officially sanctioned FAI World Championship was held in Kössen, Austria, in 1989. Europe has seen the greatest growth in paragliding, with France alone currently registering over 25,000 active pilots, the paraglider wing or canopy is usually what is known in aeronautical engineering as a ram-air airfoil. Such wings comprise two layers of fabric that are connected to supporting material in such a way as to form a row of cells. By leaving most of the open only at the leading edge, incoming air keeps the wing inflated. When inflated, the wings cross-section has the typical teardrop aerofoil shape, modern paraglider wings are made of high-performance non-porous materials such as ripstop polyester or nylon fabric. In some modern paragliders, especially wings, some of the cells of the leading edge are closed to form a cleaner aerodynamic profile. Holes in the internal ribs allow a flow of air from the open cells to these closed cells to inflate them, and also to the wingtips. The pilot is supported underneath the wing by a network of suspension lines and these start with two sets of risers made of short lengths of strong webbing
40.
Hang gliding
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Hang gliding is an air sport or recreational activity in which a pilot flies a light, non-motorized foot-launched heavier-than-air aircraft called a hang glider. Most modern hang gliders are made of an aluminium alloy or composite frame covered with synthetic sailcloth to form a wing, typically the pilot is in a harness suspended from the airframe, and controls the aircraft by shifting body weight in opposition to a control frame. Early hang gliders had a low ratio, so pilots were restricted to gliding down small hills. The Fédération Aéronautique Internationale and national airspace governing organizations control some aspects of hang gliding. Obtaining the safety benefits of being instructed is highly recommended, the earliest forms of gliding had existed in China. By the end of the sixth century A. D. the Chinese had managed to build kites large and it was only a matter of time before someone decided to simply remove the kite strings and see what happened. Most early glider designs did not ensure safe flight, the problem was that early pioneers did not sufficiently understand the underlying principles that made a birds wing work. Starting in the 1880s technical and scientific advancements were made that led to the first truly practical gliders, otto Lilienthal built controllable gliders in the 1890s, with which he could ridge soar. His rigorously documented work influenced later designers, making Lilienthal one of the most influential early aviation pioneers and his aircraft was controlled by weight shift and is similar to a modern hang glider. Hang gliding saw a stiffened flexible wing hang glider in 1904, in 1910 in Breslau, the triangle control frame with hang glider pilot hung behind the triangle in a hang glider, was evident in a gliding clubs activity. In April 1909, a article by Carl S. Volmer Jensen with a biplane hang glider in 1940 called VJ-11 allowed safe three-axis control of a foot-launched hang glider. In 1960-1962 Barry Hill Palmer adapted the flexible wing concept to make foot-launched hang gliders with four different control arrangements, in 1963 Mike Burns adapted the flexible wing to build a towable kite-hang glider he called Skiplane. Since then, the Rogallo wing has been the most used airfoil of hang gliders, there are basically two types of sail materials used in hang glider sails, Woven Polyester Fabrics, and Composite Laminated Fabrics made of some combination of polyester film and polyester fibers. Woven polyester sailcloth is a tight weave of small diameter polyester fibers that has been stabilized by the hot-press impregnation of a polyester resin. The resin impregnation is required to provide resistance to distortion and stretch and this resistance is important in maintaining the aerodynamic shape of the sail. Woven polyester provides the best combination of weight and durability in a sail with the best overall handling qualities. Laminated sail materials using polyester film achieve superior performance by using a stretch material that is better at maintaining sail shape but is still relatively light in weight. In most hang gliders, the control is and has achieved using a horizontal bar held by the pilot, also known as triangle control frame
41.
Model aircraft
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A model aircraft is a small sized unmanned aircraft or, in the case of a scale model, a replica of an existing or imaginary aircraft. Model aircraft are divided into two groups, flying and non-flying. Non-flying models are also termed static, display, or shelf models, some can be very large, especially when used to research the flight properties of a proposed full scale design. Static models range from mass-produced toys in white metal or plastic to highly accurate and detailed models produced for museum display, many models are available in kit form, typically made of injection-moulded polystyrene. Aircraft manufacturers and researchers also make wind tunnel models not capable of flight, used for testing. Sometimes only part of the aircraft is modelled, static model aircraft are scale models built using plastic, wood, metal, paper, fiberglass or any other suitable material. Some static models are scaled for use in tunnels, where the data acquired is used to aid the design of full scale aircraft. Models are available that have already built and painted, models that require construction, painting and gluing. Most of the worlds airlines allow their aircraft to be modelled as a form of publicity. In the early days, airlines would order large models of their aircraft, in addition, airlines and airplane makers hand out desktop model airplanes to airport, airline and government officials as a way of promoting their airline, celebrating a new route or an achievement. Static model aircraft are available commercially in a variety of scales from as large as 1,18 scale to as small as 1,1250 scale. Plastic model kits requiring assembly and painting are primarily available in 1,144,1,72,1,50,1,48,1,32, and 1,24 scale, often depending on the size of the original subject. Die-cast metal models are available in 1,400,1,200,1,72,1,600,1,500,1,300,1,250. A variety of odd scales are available, but less common. Scales are not usually random, but are based upon simple divisions of either the Imperial system, or the Metric system. For example,1,48 scale is 1/4 to 1-foot and 1,72 is 1 to 6 feet, while scales are simpler, such as 1, 100th. 1,72 scale was first introduced in the Skybirds wood, Skybirds was followed closely by Frog which produced 1,72 scale aircraft in 1936 under the Frog Penguin name. According to Fine Scale Modeler magazine,1,72 was also popularized by the US War Department during the Second World War when it requested models of single engine aircraft at that scale, the War Department also requested models of multi-engine aircraft at a scale of 1,144
42.
Speleology
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Speleology and caving are often connected, as the physical skills required for in situ study are the same. In Romania, the term speology is used, this is derived from a Greek word for cave, speos, rather than the Latin, spelaeum. Speleology is a field that combines the knowledge of chemistry, biology, geology, physics, meteorology and cartography to develop portraits of caves as complex. In 1895 Martel founded the Société de Spéléologie, the first organization devoted to science in the world. The creation of an accurate, detailed map is one of the most common technical activities undertaken within a cave, caves provide a home for many unique biota. Cave ecologies are diverse, and not sharply distinct from surface habitats. Generally however, the deeper the cave becomes, the more rarefied the ecology, cave environments fall into three general categories, Endogean the parts of caves that are in communication with surface soils through cracks and rock seams, groundwater seepage, and root protrusion. Parahypogean the threshold regions near cave mouths that extend to the last penetration of sunlight and these can be in regular contact with the surface via wind and underground rivers, or the migration of animals, or can be almost entirely isolated. Deep hypogean environments can host autonomous ecologies whose primary source of energy is not sunlight, cave organisms fall into three basic classes, There are also so-called accidental trogloxenes which are surface organisms that enter caves for no survival reason. Some may even be troglophobes, which survive in caves for any extended period. Examples include deer which fell through a sinkhole, frogs swept into a cave by a flash flood, the two factors that limit cave ecologies are generally energy and nutrients. To some degree moisture is available in actively forming Karst caves. Cut off from the sunlight and steady deposition of plant detritus, the majority of energy in cave environments comes from the surplus of the ecosystems outside. One major source of energy and nutrients in caves is dung from trogloxenes, because of their rarity and position in the ecosystem they are threatened by a large number of human activities. Dam construction, limestone quarrying, water pollution and logging are just some of the disasters that can devastate or destroy underground biological communities. Speleologists also work with archaeologists in studying underground ruins, tunnels, sewers and aqueducts, such as the various inlets and outlets of the Cloaca Maxima in Rome
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Tibetan Buddhism
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Tibetan Buddhism is the body of Buddhist doctrine and institutions characteristic of Tibet, the regions surrounding the Himalayas and much of Central Asia. It derives from the latest stages of Indian Buddhism and preserves the Tantric status quo of eighth-century India, Tibetan Buddhism aspires to Buddhahood or rainbow body. Religious texts and commentaries comprise the Tibetan Buddhist canon, such that Tibetan is a language of these areas. Among its prominent exponents is the 14th Dalai Lama of Tibet, the number of its adherents is estimated to be between ten and twenty million. Westerners unfamiliar with Tibetan Buddhism initially turned to China for an understanding, there the term used was lamaism to distinguish it from a then traditional Chinese form. The term was taken up by scholars including Hegel, as early as 1822. Insofar as it implies a discontinuity between Indian and Tibetan Buddhism, the term has been discredited, another term, Vajrayāna is occasionally used mistakenly for Tibetan Buddhism. More accurately, it signifies a certain subset of practices included in, not only Tibetan Buddhism, the native Tibetan term for all Buddhism is doctrine of the internalists. There is an association between the religious and the secular the spiritual and the temporal in Tibet. The term for this relationship is chos srid zung brel, in the west the term Indo-Tibetan Buddhism has become current, in acknowledgement of its derivation from the latest stages of Buddhist development in northern India. Tibetan Buddhism comprises the teachings of the three vehicles of Buddhism, the Foundational Vehicle, Mahāyāna, and Vajrayāna, the Mahāyāna goal of spiritual development is to achieve the enlightenment of buddhahood in order to most efficiently help all other sentient beings attain this state. The motivation in it is the mind of enlightenment — an altruistic intention to become enlightened for the sake of all sentient beings. Bodhisattvas are revered beings who have conceived the will and vow to dedicate their lives with bodhicitta for the sake of all beings, Tibetan Buddhism teaches methods for achieving buddhahood more quickly by including the Vajrayāna path in Mahāyāna. Buddhahood is defined as a free of the obstructions to liberation as well as those to omniscience. When one is freed from all mental obscurations, one is said to attain a state of continuous bliss mixed with a simultaneous cognition of emptiness, in this state, all limitations on ones ability to help other living beings are removed. It is said there are countless beings who have attained buddhahood. Buddhas spontaneously, naturally and continuously perform activities to all sentient beings. However it is believed that ones karma could limit the ability of the Buddhas to help them, there is a long history of oral transmission of teachings in Tibetan Buddhism
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Frankenstein
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Shelley started writing the story when she was 18, and the first edition of the novel was published anonymously in London in 1818, when she was 20. Her name first appeared on the edition, published in France in 1823. Mary, Percy, Lord Byron and John Polidori decided to have a competition to see who could write the best horror story. After thinking for days, Shelley dreamt about a scientist who created life and was horrified by what he had made, Frankenstein is infused with elements of the Gothic novel and the Romantic movement. At the same time, it is an example of science fiction. It has had an influence in literature and popular culture and spawned a complete genre of horror stories, films. Since the novels publication, the name Frankenstein has often used to refer to the monster itself. This usage is considered erroneous, but usage commentators regard it as well-established. In the novel, the monster is identified by such as creature, monster, demon, wretch, abortion. Speaking to Victor Frankenstein, the wretch refers to himself as the Adam of your labours, and elsewhere as someone who would have been your Adam, Frankenstein is written in the form of a frame story that starts with Captain Robert Walton writing letters to his sister. It takes place at a time in the 18th century. The novel Frankenstein is written in form, documenting a fictional correspondence between Captain Robert Walton and his sister, Margaret Walton Saville. Walton is a writer and captain who sets out to explore the North Pole. During the voyage, the spots an dog sled driven by a gigantic figure. A few hours later, the crew rescues a nearly frozen, Frankenstein has been in pursuit of the gigantic man observed by Waltons crew. Frankenstein starts to recover from his exertion, he sees in Walton the same obsession that has destroyed him, the recounted story serves as the frame for Frankensteins narrative. Victor begins by telling of his childhood, as a young boy, Victor is obsessed with studying outdated theories that focus on simulating natural wonders. When Victor is five years old, his parents adopt Elizabeth Lavenza, weeks before he leaves for the University of Ingolstadt in Germany, his mother dies of scarlet fever, Victor buries himself in his experiments to deal with the grief
