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Tschaggunser Mittagspitze
The Tschaggunser Mittagsspitze is a high mountain in the Rätikon mountain range of the Central Eastern Alps. It is located in the Austrian state Vorarlberg, south of the village Tschagguns in the Montafon valley. Etymology The name of Tschaggunser Mittagsspitze may be traced to "peak ("-spitze") above which the sun culminates at noon Noon (or midday) is 12 o'clock in the daytime. It is written as 12 noon, 12:00 m. (for meridiem, literally 12:00 noon), 12 p.m. (for post meridiem, literally "after noon"), 12 pm, or 12:00 (using a 24-hour clock) or 1200 ( military time). Sola ... ("Mittag-") as seen from Tschagguns". Further reading * Mountains of Vorarlberg Mountains of the Alps {{Austria-geo-stub ...
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Vorarlberg
Vorarlberg ( , ; gsw, label=Vorarlbergisch, Vorarlbearg, , or ) is the westernmost States of Austria, state () of Austria. It has the second-smallest geographical area after Vienna and, although it also has the second-smallest population, it is the state with the second-highest population density (also after Vienna). It borders three countries: Germany (Bavaria and Baden-Württemberg via Lake Constance), Switzerland (Grisons and Canton of St. Gallen, St. Gallen), and Liechtenstein. The only Austrian state that shares a border with Vorarlberg is Tyrol (state), Tyrol, to the east. The capital of Vorarlberg is Bregenz (29,698 inhabitants), although Dornbirn (49,845 inhabitants) and Feldkirch, Vorarlberg, Feldkirch (34,192 inhabitants) have List of cities and towns in Austria, larger populations. Vorarlberg is also the only state in Austria in which the local dialect is not Austro-Bavarian dialects, Austro-Bavarian, but rather an Alemannic dialects, Alemannic dialect; it therefore ha ...
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Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ...
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Rätikon
The Rätikon is a mountain range of the Central Eastern Alps, located at the border between Vorarlberg, Liechtenstein and Graubünden. It is the geological border between the Eastern and Western Alps and stretches from the Montafon as far as the Rhine. In the south, the Prättigau is its limit, and in the north, it is the Walgau. In the east, it borders the Silvretta groups. The Rätikon mountain range derives its name from Raetia, a province of the Roman Empire, named after the Rhaetian (''Raeti'' or ''Rhaeti'') people. Topography and geology The classification of the Rätikon to the central Eastern Alps is based solely on geographic-geological traditions. Large parts of the Rätikon consist of sedimentary rocks (limestone). From a geological point of view, the north-west Rätikon is assigned to the Northern Limestone Alps, while the South-West Rätikon belongs to the Bündner Schist/Bündner slate of the Western Alps. Peaks Its chief peaks are: *Schesaplana 2964  ...
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Central Eastern Alps
The Central Eastern Alps (german: Zentralalpen or Zentrale Ostalpen), also referred to as Austrian Central Alps (german: Österreichische Zentralalpen) or just Central Alps, comprise the main chain of the Eastern Alps in Austria and the adjacent regions of Switzerland, Liechtenstein, Italy and Slovenia. South them is the Southern Limestone Alps. The term "Central Alps" is very common in the Geography of Austria as one of the seven major landscape regions of the country. "Central Eastern Alps" is usually used in connection with the Alpine Club classification of the Eastern Alps (''Alpenvereinseinteilung'', AVE). The Central Alps form the eastern part of the Alpine divide, its central chain of mountains, as well as those ranges that extend or accompany it to the north and south. The highest mountain in the Austrian Central Alps is Grossglockner at . Location The Central Alps have the highest peaks of the Eastern Alps, and are located between the Northern Limestone Alps and the ...
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Tschagguns
Tschagguns is a village in the Montafon valley, Bludenz district in the Austrian state of Vorarlberg. Tschagguns offers skiing with its own ski resort called Golm. Tschagguns offers hiking, mountain biking, winter sports and much more. Gauertal is a valley found in Tschagguns between Mittagspitze and Golm. It is famous for the "3 Türme" which means 3 Towers. Population Sons and daughters of the place * Werner Bleiner (born 1946), ski racer * Christian Orlainsky (born 1962), ski racer Persons with reference to the place * Georg Friedrich Haas (born 1953 in Graz), composer, has grown up in Tschagguns Honorary citizen * Arnold Durig Arnold Durig (12 November 1872 – 18 October 1961) was an Austrian physiologist remembered for his investigations involving physiological and pathophysiological aspects of individuals exposed to high altitude conditions. He very probably ... (1872-1961), physiologist References Cities and towns in Bludenz District {{Vora ...
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Montafon
Montafon ( in local dialect: "''Muntafu''") is a 39 km long valley in the westernmost Austrian federal state of Vorarlberg. It is traversed by the river Ill (Vorarlberg) and extends from the city of Bludenz and the Verwall Alps in the north, to the Silvretta and Rätikon mountain range in the south. Piz Buin, at 3,312 meters, is the highest peak within the Silvretta mountain range and the highest peak in Vorarlberg. The Montafon region has a population of 16,421(2021). Geography The Montafon is an association of ten communities ("Stand Montafon"), all of which belong to the Bludenz district. The main town is Schruns. Regional tourism is marketed by the Tourist Association Montafon, run by the municipalities, the Vorarlberger Illwerke and the regional mountain cableways. The municipalities: * Bartholomäberg (1,100 m) *Gaschurn (1,000m) *Lorüns (583 m) * St. Anton im Montafon (650 m) *Sankt Gallenkirch (900m) * Schruns (700 m) *Silbertal (890 m) * Stallehr (600 m) ...
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Pyramidal Peak
A pyramidal peak, sometimes called a glacial horn in extreme cases, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Pyramidal peaks are often examples of nunataks. Formation Glaciers, typically forming in drainages on the sides of a mountain, develop bowl-shaped basins called cirques (sometimes called ‘corries’ - from Scottish Gaelic ʰəɾə(a bowl) - or s). Cirque glaciers have rotational sliding that abrades the floor of the basin more than walls and that causes the bowl shape to form. As cirques are formed by glaciation in an alpine environment, the headwall and ridges between parallel glaciers called arêtes become more steep and defined. This occurs due to freeze/thaw and mass wasting beneath the ice surface. It is widely held that a common cause for headwall steepening and extension headward is the crevasses known as bergschrund that occur between the moving ice and the he ...
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Culmination
In observational astronomy, culmination is the passage of a celestial object (such as the Sun, the Moon, a planet, a star, constellation or a deep-sky object) across the observer's local meridian. These events were also known as meridian transits, used in timekeeping and navigation, and measured precisely using a transit telescope. During each day, every celestial object appears to move along a circular path on the celestial sphere due to the Earth's rotation creating two moments when it crosses the meridian. Except at the geographic poles, any celestial object passing through the meridian has an upper culmination, when it reaches its highest point above the horizon, and nearly twelve hours later, is followed by a lower culmination, when it reaches its lowest point. The time of ''culmination'' (when the object culminates) is often used to mean upper culmination. An object's altitude (''A'') in degrees at its upper culmination is equal to 90 minus the observer's latitude (''L'') ...
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Solar Noon
Noon (or midday) is 12 o'clock in the daytime. It is written as 12 noon, 12:00 m. (for meridiem, literally 12:00 noon), 12 p.m. (for post meridiem, literally "after noon"), 12 pm, or 12:00 (using a 24-hour clock) or 1200 (military time). Solar noon is the time when the Sun appears to contact the local celestial meridian. This is when the Sun reaches its apparent highest point in the sky, at 12 noon apparent solar time and can be observed using a sundial. The local or clock time of solar noon depends on the longitude and date, with Daylight Savings Time tending to place solar noon closer to 1:00pm. Etymology The word ''noon'' is derived from Latin ''nona hora'', the ninth canonical hour of the day, in reference to the Western Christian liturgical term none, one of the seven fixed prayer times in traditional Christian denominations. The Roman and Western European medieval monastic day began at 6:00 a.m. (06:00) at the equinox by modern timekeeping, so the ninth hour star ...
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Mountains Of Vorarlberg
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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