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Mont Aiguille
Mont Aiguille () is a mountain in the Vercors Massif of the French Prealps, located south of Grenoble, in the commune of Chichilianne, and the département of Isère. The mountain, known as one of the Seven Wonders of Dauphiné, is a relatively flat limestone mesa surrounded by steep cliffs. The mountain lies within an area designated in 1970 as the Vercors Regional Natural Park. Mont Aiguille's limestone cliffs, especially on the northwest side, are popular with climbers. Its first climb in 1492 was said to mark the birth of mountaineering. Topography and geography Mont Aiguille is a mesa eroded from the Vercors Plateau in the drainage basin of the Rhône. It is surrounded by steep cliffs and has a height of and a clean prominence of . The surrounding terrain is difficult enough to warrant a technical climb as the easiest method of ascent. The mountain is capped with meadows botanically similar to those on the Vercors High Plateau, but beneath the cliffs there are ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Vercors Massif
The Vercors massif (; ) is a mountain range in eastern France consisting of rugged plateaus and mountains straddling the ''département in France, départements'' of Isère and Drôme in the French Prealps. It lies west of the Dauphiné Alps, from which it is separated by the rivers Drac (river), Drac and Isère (river), Isère. The cliffs at the massif's eastern limit face the city of Grenoble. Background Over time, various features of the complex geography have been recognised including, the Quatre Montagnes (four mountains), the Coulmes (gorges), the Vercors Drômois (Drome Vercors), the Hauts-Plateaux (high plateaus) and, in the foothills, Royans, Gervanne, Diois, and Trièves. The massif is sometimes called the "fortress". The movement of people tends to be between the massif and the surrounding plains rather than between the various parts of the massif itself. Until the mid twentieth century, the name ''Vercors'' was used to describe only the township of La Chapelle-en ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Mont Aiguille
Mont Aiguille () is a mountain in the Vercors Massif of the French Prealps, located south of Grenoble, in the commune of Chichilianne, and the département of Isère. The mountain, known as one of the Seven Wonders of Dauphiné, is a relatively flat limestone mesa surrounded by steep cliffs. The mountain lies within an area designated in 1970 as the Vercors Regional Natural Park. Mont Aiguille's limestone cliffs, especially on the northwest side, are popular with climbers. Its first climb in 1492 was said to mark the birth of mountaineering. Topography and geography Mont Aiguille is a mesa eroded from the Vercors Plateau in the drainage basin of the Rhône. It is surrounded by steep cliffs and has a height of and a clean prominence of . The surrounding terrain is difficult enough to warrant a technical climb as the easiest method of ascent. The mountain is capped with meadows botanically similar to those on the Vercors High Plateau, but beneath the cliffs there are ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Rock Climbing
Rock climbing is a climbing sports discipline that involves ascending climbing routes, routes consisting of natural rock in an outdoor environment, or on artificial resin climbing walls in a mostly indoor environment. Routes are documented in climbing guidebook, guidebooks, and on online databases, detailing how to climb the route (called the beta (climbing), beta), and who made the first ascent (or FA) and the coveted First ascent#In rock climbing, first free ascent (or FFA). Climbers will try to ascend a route onsight, however, a climber can spend years projecting (climbing), projecting a route before they make a redpoint (climbing), redpoint ascent. Routes range from a few metres to over a in height, and traverse (climbing), traverses can reach in length. They include slab climbing, slabs, face climbing, faces, crack climbing, cracks and overhang (climbing), overhangs/roofs. Popular rock types are granite (e.g. El Capitan), limestone (e.g. Verdon Gorge), and sandstone (e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Quart Livre
''Le Quart Livre'' (''The Fourth Book'' in English) is a novel by François Rabelais and published in its final version in 1552 in literature, 1552. The author was confronted with significant challenges in the context of this sequel to the adventures of ''Gargantua and Pantagruel, Pantagruel'', particularly in the wake of the publication of ''Gargantua and Pantagruel#The Third Book, The Third Book'' and the subsequent opposition from theologians at the Sorbonne University, Sorbonne. Nevertheless, he obtained the support of Cardinal Odet de Coligny, and despite another attempt at censorship, the work achieved rapid success. The Prologue, prologues serve to illustrate this polemical context. The novel, written with the comic flair typical of François Rabelais, is a sea voyage narrative in which the protagonists encounter fantastical creatures and places that resonate with the author's Humanism, humanist concerns. Following their decision at the end of ''The Third Book'', Pantagrue ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
François Rabelais
François Rabelais ( , ; ; born between 1483 and 1494; died 1553) was a French writer who has been called the first great French prose author. A Renaissance humanism, humanist of the French Renaissance and Greek scholars in the Renaissance, Greek scholar, he attracted opposition from both Protestant theologian John Calvin and from the hierarchy of the Catholic Church. Though in his day he was best known as a physician, scholar, diplomat, and Catholic priest, later he became better known as a satirist for his depictions of the grotesque, and for his larger-than-life characters. Living in the religious and political turmoil of the Reformation, Rabelais treated the great questions of his time in his novels. Rabelais admired Erasmus and like him is considered a Christian humanism, Christian humanist. He was critical of medieval scholasticism and lampooned the abuses of powerful princes and popes. Rabelais is widely known for the first two volumes relating the childhoods of the gia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Bivouac Shelter
A bivouac shelter or bivvy (alternately ''bivy'', ''bivi'', ''bivvi'') is any of a variety of improvised camp site or shelter that is usually of a temporary nature, used especially by soldiers or people engaged in backpacking, bikepacking, scouting or mountain climbing. It may often refer to sleeping in the open with a bivouac sack, but it may also refer to a shelter constructed of natural materials like a structure of branches to form a frame, which is then covered with leaves, ferns and similar material for waterproofing and duff (leaf litter) for insulation. Modern bivouacs often involve the use of one- or two-person tents but may also be without tents or full cover. In modern mountaineering the nature of the bivouac shelter will depend on the level of preparedness, in particular whether existing camping and outdoor gear may be incorporated into the shelter. Etymology The word ''bivouac'' is French and ultimately derives from an 18th-century Swiss German usage of ''Beiwacht ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Charles VIII Of France
Charles VIII, called the Affable (; 30 June 1470 – 7 April 1498), was King of France from 1483 to his death in 1498. He succeeded his father Louis XI at the age of 13. His elder sister Anne acted as regent jointly with her husband Peter II, Duke of Bourbon until 1491, when the young king turned 21 years of age. During Anne's regency, the great lords rebelled against royal centralisation efforts in a conflict known as the Mad War (1485–1488), which resulted in a victory for the royal government. In a remarkable stroke of audacity, Charles married Anne of Brittany in 1491 after she had already been married by proxy to the Habsburg Holy Roman Emperor Maximilian I in a ceremony of questionable validity. Preoccupied by the problematic succession in the Kingdom of Hungary, Maximilian failed to press his claim. Upon his marriage, Charles became administrator of Brittany and established a personal union that enabled France to avoid total encirclement by Habsburg territories. To se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Hauterivian
The Hauterivian is, in the geologic timescale, an age in the Early Cretaceous Epoch or a stage in the Lower Cretaceous Series. It spans the time between 132.6 ± 2 Ma and 125.77 (million years ago). The Hauterivian is preceded by the Valanginian and succeeded by the Barremian. Stratigraphic definitions The Hauterivian was introduced in scientific literature by Swiss geologist Eugène Renevier in 1873. It is named after the Swiss town of Hauterive at the shore of Lake Neuchâtel. The base of the Hauterivian is defined as the place in the stratigraphic column where the ammonite genus '' Acanthodiscus'' first appears. A reference profile for the base (a GSSP) was officially ratified by the International Union of Geological Sciences in December of 2019, and is placed in La Charce, France. The top of the Hauterivian (the base of the Barremian) is at the first appearance of ammonite species '' Spitidiscus hugii''. In the ammonite biostratigraphy of the Tethys domain, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Barremian
The Barremian is an age in the geologic timescale (or a chronostratigraphic stage) between 125.77 Ma (million years ago) and 121.4 ± 1.0 Ma (Historically, this stage was placed at 129.4 million to approximately 125 million years ago) It is a subdivision of the Early Cretaceous Epoch (or Lower Cretaceous Series). It is preceded by the Hauterivian and followed by the Aptian Stage.See Gradstein ''et al.'' (2004) or the online geowhen database (link below) Stratigraphic definitions The original type locality for the Barremian Stage is in the vicinity of the village of Barrême, Alpes-de-Haute-Provence, France. Henri Coquand defined the stage and named it in 1873. The base of the Barremian is determined by the first appearance of the ammonites '' Spitidiscus hugii'' and ''Spitidiscus vandeckii''. The end of the Barremian is determined by the geomagnetic reversal at the start of the M0r chronozone, which is biologically near the first appearance of the ammonite '' Paradesh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Plateau
In geology and physical geography, a plateau (; ; : plateaus or plateaux), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wider ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, plate tectonics movements, and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. They may be formed by upwelling of volcanic magma or extrusion of lava. The underlining mechanism in forming p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
