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54-586: Essingen currently has about 6000 residents, and is located on the northern end of the Swabian Alb . It is mainly a dormitory community , but does have industry along the B29 federal road and Stuttgart-Aalen railway . Recreational activities include biking, hiking, and rambling. In the winter, there are opportunities for skiing. In the middle of the village lies the Schloss (castle) and Schloss Park. The castle

108-584: A Moselle Franconian dialect word used for the circular lakes of the Daun area of Germany. The word evolved from its first use in German in the modern geological sense in 1819 and is now used in English and in the geological sciences as the term for the explosion crater, even if water from rainfall might always have drained from the crater after the formation event. This extension in meaning was due to recognising that

162-551: A Swabian Alb Biosphere Reserve of 852.69 km (330 sq. mi.). The geology of the Swabian Jura is mostly limestone , which formed the seabed during the Jurassic period. The sea receded 50 million years ago. Three layers of different limestones are stacked over each other to form the range: Black Jurassic , Brown Jurassic , and White Jurassic . White Jurassic may be as pure as 99% calcium carbonate . Since limestone

216-487: A "luxury outlet town", with people from all over Europe coming to buy expensive clothes cheaper). From this, machine building and advanced engineering developed. With the invention of cars and the founding of Daimler-Benz nearby, the car industry and later also electronics and computer industries developed. The " Neckar-Alb " region is the third largest industrial zone in Germany, and the most stable. The best known company

270-401: A few kilometers apart, some of the oldest signs of human artifacts were found. Best known are: a mammoth, a horse head, a water bird, and two statues of a lion man all of surprising quality and all more than 30,000 years old. The oldest known musical instruments have been found here, too: flutes made from the bones of swans and griffon vultures, some 35,000 years old, and in 2004

324-632: A flute carved from the tusk of a mammoth dating from the Ice Age, around 37,000 years ago, and the oldest representation of the human body, the Venus of Schelklingen . This region, located south of the limes , was part of the Roman Empire from around the first to third century A.D. A Roman road ran along the Neckar river and over the plateau. In Hechingen-Stein a Roman outpost along this road

378-603: A proper noun referring more or less exclusively to the Swabian and the Franconian Jura ( German : Fränkische Alb ) areas however, and as such has no direct translation into most other languages. It is perhaps for this reason that Schwäbische Alb has sometimes been translated into English as 'Swabian Alps', thus avoiding the lesser-known name Jura . However, the area is not part of the Alps (despite its proximity), nor

432-416: A relatively shallow crater lake , which may also be called a maar. Maars range in size from 20 to 3,000  m (66 to 9,800  ft ) across and from 5 to 200 m (20 to 700 ft) deep. Most maars fill with water to form natural lakes. Most maars have low rims composed of a mixture of loose fragments of volcanic rocks and rocks torn from the walls of the diatreme . The name maar comes from

486-449: A small private museum, called Urwelt-Museum Hauff, provides visitors with the opportunity to "dig" for fossils in their shale deposits. The Urwelt-Museum Hauff houses the world's largest petrified crinoid (sea-lily) colony with a size of 18 m × 6 m (59 ft × 20 ft) and an age of about 180 million years. In a number of caves (including Vogelherd, Hohlenstein-Stadel , Geißenklösterle and Hohle Fels ), all just

540-476: A stronger Fasnet tradition. A Swabian Fasnet celebration in any case has little or nothing in common with the simultaneous celebrations along the Middle Rhein, which are well known across Germany because they are televised every year. Swabians generally are expected to go to work as normal on Rose Monday and Fat Tuesday, unlike their neighbors to the northwest. Since raising crops was not easy, raising sheep

594-523: A tectonically active region) sometimes causes mild earthquakes. The Nördlinger Ries is a large meteorite crater (15 million years old). Tertiary relicts can be found in the southern part of Swabian Jura. Famous locations are known in the Ulm area (e.g., Turritellenplatte of Ermingen). Constant rain and other weather influences are slowly dissolving the entire range. Each year, it recedes approximately 2 mm (0.08 in). Some millions of years ago,

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648-497: A tributary to the Rhine . The soil is not very fertile, the humus is often as thin as 10 cm (4 in). Many small limestone pebbles are found on the surface. Much of the Swabian Jura consists of gentle to moderate hills often covered with forest or cleared for small-scale agriculture . The traditional landscape was grass fields with juniper bushes . Today this has become a comparatively rare sight. However, in certain places it

702-469: A volcanic crater, is a maar. The carbon dioxide -saturated Lake Nyos in northwestern Cameroon is another example, as is Zuñi Salt Lake in New Mexico , a shallow saline lake that occupies a flat-floored crater about 6,500 ft (2,000 m) across and 400 ft (120 m) deep. Its low rim is composed of loose pieces of basaltic lava and wall rocks ( sandstone , shale , limestone ) of

756-486: Is soluble in water, rain seeps through cracks everywhere, forming a karst landscape, featuring subterranean rivers which flow through a large system of caves before they emerge. As a result there are hardly any rivers, lakes or other forms of surface water on the plateau. In some places, former volcanic activity has left traces, such as maars and hills. In the west, the Zollerngraben (a geological depression in

810-642: Is Kagamiike Pond as well as many on the volcanic island of Miyake-jima , Izu Islands (Furumio, Mi'ike, Mizutamari, Shinmio). Koranga Maar and Numundo Maar are in Papua New Guinea . Kawah Masemo maar is on Mount Sempu volcano in Indonesia. The San Pablo Volcanic Field in the Province of Laguna on the island of Luzon in the Philippines contains maars. The Newer Volcanics Province in

864-586: Is a mountain range in Baden-Württemberg , Germany , extending 220 km (140 mi) from southwest to northeast and 40 to 70 km (25 to 43 mi) in width. It is named after the region of Swabia . It is part of the Table Jura ( Tafeljura ). The Swabian Jura occupies the region bounded by the Danube in the southeast and the upper Neckar in the northwest. In the southwest it rises to

918-481: Is it ever referred to as such in German, the Alps being die Alpen in German (plural). 48°18′N 9°21′E  /  48.3°N 9.35°E  / 48.3; 9.35 Maar A maar is a broad, low- relief volcanic crater caused by a phreatomagmatic eruption (an explosion which occurs when groundwater comes into contact with hot lava or magma ). A maar characteristically fills with water to form

972-672: Is protected by the government of Baden-Württemberg. The highest elevations reach just over 1,000 metres (3,300 ft). They are all in the southwestern part of the Jura, in the region of the Großer Heuberg . There are many other peaks in the Alb, such as the Hornau , Ochsenberg , and Achalm . Fossils can be found everywhere in the Swabian Jura. Many large and important fossils were found here. At Holzmaden, outside of Weilheim unter Teck,

1026-498: Is still Daimler-Benz, today known simply as Daimler AG , followed by Robert Bosch . The region has one of the highest patents-to-population ratios in the world. Many products fall into the high-tech category. The small and medium enterprise sector (100-5,000 employees) predominates. Perhaps as a result, the unemployment rate is low. In general, products are expensive but compete through high quality. Several districts are recognised as especially attractive to business, e.g. Reutlingen as

1080-1123: The Butajiri - Silti -Volcanic Field, Ethiopia, the Bayuda Volcanic Field in the Sudan and Lake Nyos in the Oku Volcanic Field in Cameroon). In Saudi Arabia the Al Wahbah crater formed as a result of a maar eruption. In Japan there are maars in the Kirishima - Yaku volcanic field in the Kirishima-Yaku National Park on Kyushu . These include the several maars of the Ibusuki volcanic field such as Lake Unagi . On Honshu in Myōkō-Togakushi Renzan National Park there

1134-651: The Eifel region of Germany (where they were originally described), and in other geologically young volcanic regions of Earth. Elsewhere in Europe, La Vestide du Pal, a maar in the Ardèche department of France, is easily visible from the ground or air. Kilbourne Hole and Hunt's Hole, in southern New Mexico near El Paso, Texas , are maars. The Crocodile Lake in Los Baños in the Philippines, though originally thought to be

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1188-632: The Jura mountains , of which the Swabian and Franconian plateaux are geographically part. In German, at least outside geological circles, the word Alb is used almost universally in place of Jura . The origin of the word is uncertain. One theory is that it derives form the Latin albus ("white"). Another is that it is from a pre-Indo-European word albhros ("hill"). It is related to the German words Alpe , Alm or Alp (from Old High German alpâ ), meaning an " upland pasture ". The word Alb functions as

1242-803: The Province of Ciudad Real . Active maars were commonplace in Fife and Lothian , Scotland during the Carboniferous period. The location of one such maar was Elie Ness. Active maar volcanoes are mainly known outside Europe. In the US there are numerous maar areas, such as in Alaska ( Ukinrek maars , Nunivak in the Bering Sea ); in Washington ( Battle Ground Lake ); in Oregon ( Fort Rock basin with

1296-883: The Swabian Jura and the Albvorland (the Swabian Volcano) there are maar-forming volcanoes. Because the over 350 eruption points were only active in the Upper Miocene 17 to 11 million years ago, all the maars, apart from the dry maar, Randecker Maar and the Molach, are only detectable geologically. In the Ore Mountains near Hammerunterwiesenthal , the Hammerunterwiesenthal Maar formed about 30 million years ago during

1350-552: The Eifel and Volcanic Eifel there are numerous dry maars: The following volcanic features are often colloquially referred to as a "maar" or "maar lake", although they are not, strictly speaking, maars: In Germany there are also several maars outside of the Eifel. A well-known example is the Messel pit , a former maar lake near Messel in the county of Darmstadt-Dieburg and which is known for its well preserved fossils . In addition in

1404-715: The Oligocene; the maar measures 2 kilometres from east to west and 1.4 kilometres from north to south. The Chaîne des Puys in France contains numerous maars; Lake Albano in the Alban Mountains is a complex maar, and there is also a submarine maar ( Kolumbo ) near Santorini in Greece. The Campo de Calatrava Volcanic Field in Spain contains numerous maars; a typical example being the maar of Hoya del Mortero at Poblete in

1458-567: The States of South Australia and Victoria , Australia, has numerous maars, such as Mount Gambier , Mount Schank and Tower Hill , whose complex system of nested maars is enclosed by one of the largest maars in the world. Foulden Maar in Otago , New Zealand , is an important fossil site, but there are many more maars in New Zealand. As already mentioned these include Lake Pupuke , but

1512-511: The Swabian Jura includes regions just around the mountain range. It is a popular recreation area. The whole Schwäbische Alb area is a UNESCO global geopark covering 6,688 km (2582 sq mi.); it was designated as a National Geopark in Germany in 2002 and became a member of the European Geoparks Network in 2004; in 2015 it was included in the newly established scheme of UNESCO Global Geoparks. In its central area it comprises

1566-574: The discharge of the water from subterranean rivers can be spectacular, too, e.g. the Blautopf , a source for a tributary of the Danube. Also because of the porous limestone, the Danube nearly disappears near Immendingen (in 1911, 1921, 1928 and 1943 it disappeared completely), only to reappear several kilometers further down. Most of the water lost by the Danube resurfaces in the Aachtopf , a spring for

1620-690: The exact traditions vary from village to village, creating a fantastic variety of heroes, villains and good and evil creatures. It is also often the case that, while in one town a strong tradition of celebrating Fasnet has survived, the neighboring town will have almost no tradition. This is in many instances linked to the after-effects of the Protestant Reformation and the later influence of the Calvinistic Pietists, who more or less strictly opposed such frivolous - even heathen - behaviour. Catholic regions to this day tend to have

1674-765: The explosive reaction that occurs when magma comes into contact with permafrost . Hydromagmatic eruptions are increasingly explosive when the ratio of water to magma is low. Since permafrost melts slowly, it provides a steady source of water to the eruption while keeping the water to magma ratio low. This produces the prolonged, explosive eruptions that created these large maars. Examples of the Seward Peninsula maars include North Killeak Maar, South Killeak Maar, Devil Mountain Maar and Whitefish Maar. Maars occur in western North America, Patagonia in South America,

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1728-503: The foreland of the Swabian Jura officially don't belong to it. There are many castles, monasteries, churches, ruins and old towns. Here is a small selection. A good way for tourists to get to know the Swabian Jura is to travel on the Schwäbische Albstraße , a "National Scenic Byway", leading from Tuttlingen or Trossingen to Nördlingen or Aalen . The name German : Jura (related to Jurassic ) derives from

1782-420: The geological sciences such as the term tuff ring or maar-diatreme volcanoes. These last are volcanoes produced by explosive eruptions that cut deeply into the country rock with the maar being " the crater cut into the ground and surrounded by an ejecta ring ". A 2011 geological clarification of a maar is " Maar volcanoes are distinguished from other small volcanoes in having craters with their floor lying below

1836-601: The higher mountains of the Black Forest . The highest mountain in the region is the Lemberg (1,015 m (3,330 ft)). The area's profile resembles a high plateau, which slowly falls away to the southeast. The northwestern edge is a steep escarpment (called the Albtrauf or Albanstieg, rising up 400 m (1,300 ft), covered with forests), while the top is flat or gently rolling. In economic and cultural terms,

1890-467: The highest rents in Germany, while land on the plateau itself is considered cheap (by south German standards). Many town names end in -ingen . There were several military training grounds, some also used by NATO troops. On the Münsingen training ground which existed for over 100 years, a biosphere reserve is in the making. The region has several larger and many small nature reserves. The towns in

1944-473: The hills are not steep or high) and numerous small resorts can be found. It is often windy and a bit colder than the rest of Germany. Because of a special micro climate, a small weather station near the town of Stetten am kalten Markt is known as the "coldest spot in Germany". The Swabian Jura are not densely populated by German standards. Most of the larger towns are outside the region, though they are often counted as part of it. These towns often have some of

1998-536: The hollow. The largest known maars are found at Espenberg on the Seward Peninsula in northwest Alaska. These maars range in size from 4 to 8 km (2.5 to 5.0 mi) in diameter and a depth up to 300 m (980 ft). These eruptions occurred in a period of about 100,000 years, with the youngest (the Devil Mountain Maar) occurring about 17,500 years ago. Their large size is due to

2052-419: The lake may no longer exist. Since maar lakes are formed after initially ground or subsurface water interacts with a magma intrusion to create an explosion crater, the name came to be used for the crater type as well. The present definition of the term relates to both its common and scientific discourse use in language over two centuries. Depending upon context there may be other descriptors available to use in

2106-640: The latter is the Eckfelder Maar . Near Steffeln is the Eichholzmaar (also called the Gussweiher ) which has dried out during the last century and is being renaturalised into a maar. In some cases the underlying rock is so porous that maar lakes are unable to form. After winters of heavy snow and rainfall many dry maars fill partially and temporarily with water; others contain small bogs or often artificial ponds that, however, only occupy part of

2160-768: The maars of Big Hole , Hole-in-the-Ground , Table Rock ); in Death Valley National Park , California ( Ubehebe Crater ); in Nevada ( Soda Lakes ); as well as the maars of the White Rock Canyon , Mount Taylor , the Potrillo volcanic fields ( Kilbourne Hole and Hunt's Hole ), and Zuñi Salt Lake in New Mexico. In Central Mexico, the Tarascan volcanic field contains several maars in

2214-624: The mountains reached as far as Stuttgart . In some places, the limestone was more resistant to decay and thus the recession of the main range has left small mountains (called "Zeugenberge"—"witness mountains" or outliers ; e.g. the Achalm or the Hohenstaufen ) which testify to the former territory of the range. The omnipresent caves are great tourist spots, beautiful and not very crowded. Many different types can be found, from dry dripstone caves to caves that can only be entered by boat. Sometimes

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2268-411: The poor quality of the soil made it a backward region. For many villages fetching water required a long journey by horse. Since water often needed to be stored over a long time, it was often stagnant. Thus disinfection via alcohol was very popular: "Most" ( cider ) was mixed with water and even given to babies. A modern water supply system (outstanding for its time) was built in the late 1880s, which eased

2322-426: The pre-eruptive surface ". Maar lakes , also referred to simply as maars , occur when groundwater or precipitation fills the funnel-shaped and usually round hollow of the maar depression formed by volcanic explosions. Examples of these types of maar are the three maars at Daun in the Eifel mountains of Germany . A dry maar results when a maar lake dries out, becomes aggraded or silted up . An example of

2376-455: The situation. Locals in the areas speak the distinct German dialect known as Swabian German , which varies even throughout the Jura and is difficult to understand for speakers of Standard German. The dialect at the top of the plateau ( German : Albschwäbisch ) is markedly different from, and stronger than, even the broadest Swabian of the lowland areas. Across the whole Swabian region, many phrases and grammar are highly localized, even down to

2430-405: The states of Michoacán and Guanajuato . In Nicaragua is the maar of Laguna de Xiloa, part of the Apoyeque volcano. From South America, there are known maars in Chile (e.g. Cerro Overo and Cerro Tujle in northern Chile). Jayu Khota is a maar in Bolivia . The maar of Birket Ram lies on the Golan Heights ; further south maars occur in Africa ( Bilate Volcanic Field and Haro Maja in

2484-400: The town in Germany where it is simplest to open a new business. Educational resources are at a high level. The schools and universities of the region all enjoy top rankings within Germany. The Swabian Jura and the neighbouring region have developed from one of the poorest regions of Germany to one of its richest within the past 150 years. In winter it often snows. Skiing is popular (though

2538-440: The underlying diatreme , as well as chunks of ancient crystalline rocks blasted upward from great depths. Maars in Canada are found in the Wells Gray-Clearwater volcanic field of east-central British Columbia and in kimberlite fields throughout Canada. Another field of maars is found in the Pali-Aike Volcanic Field in Patagonia , South America. and in the Sudanese Bayuda Volcanic Field . The Auckland volcanic field in

2592-590: The urban area of Auckland , New Zealand, has several maars, including the readily accessible Lake Pupuke in the North Shore suburb of Takapuna . Arizona 's Meteor Crater was for many years thought to be a maar of volcanic origin but it is now known to be an impact crater . In the Volcanic Eifel there are about 75 maars. Both lake-filled and dry maars are typical, though the latter are more common. The last eruptions took place at least 11,000 years ago, and many maars are older, as evidenced by their heavy erosion and less obvious shapes and volcanic features. In

2646-426: The village level; however, the Swabian dialect of the highland regions is characterised by a sing-song melody, and some of the verb forms are also distinct, not only from Standard German , but also from those of the rest of Swabia . In former times, Yiddish , Pleißne and Romani was also spoken. The Pleißne was spoken by hawkers selling items such as baskets, brushes, and whips, and belongs to Rotwelsch . It

2700-509: Was built circa 1550 by the Woellwarth Family. It has remained in the family until recently when it was sold at auction causing much controversy in the village. Some villagers wanted to save the castle to be used for various activities and events but the consensus was that the castle would be too expensive to maintain and run. Essingen is a larger municipality, and the nearby villages of Lauterburg, Forst, Dauerwang, Hermannsfeld, Birkenteich and Hohenroden belong to Essingen. Wolfgang Hofer (* 1963)

2754-411: Was discovered in the 1970s and has been turned into an outdoor museum. The limes actually cuts across the plateau at Aalen , which gets its name from the original Roman cavalry post, or ala , on the outskirts of the modern town. Here too, the Roman ruins are being excavated and a museum has been open to the public since the late 1980s. Life was extremely hard in the Swabian Jura. The lack of water and

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2808-433: Was elected mayor in 1997, he was reelected in 2005, 2013 and 2021. Elections in May 2014: This Ostalbkreis location article is a stub . You can help Misplaced Pages by expanding it . Swabian Alb The Swabian Jura ( German : Schwäbische Alb [ˈʃvɛːbɪʃə ˈʔalp] , more rarely Schwäbischer Jura [ˈʃvɛːbɪʃɐ ˈjuːʁa] ), sometimes also named Swabian Alps in English,

2862-408: Was popular. This yielded the development of a strong textile industry. In the 1950s, Reutlingen was the German town with the highest number of millionaires, until the decline of the German textile industry hit them as well. Still, many high quality textile companies can be found, such as Hugo Boss , Merz b. Schwanen , Trigema , Reusch, Groz-Beckert and others (the town of Metzingen is widely known as

2916-505: Was used as a code. The " Swabian – Alemannic " carnival is an important tradition in many of the villages, called variously " Fastnacht ", "Fasnacht", "Fasnet", or "Fasching". Of particular cultural importance is the Fasnet celebration in Rottweil. Typical of the Allemannic tradition are the witches and forest- or well-spirits, who typically signify Winter or the forces of nature coming to drive Winter out. The various roles are often claimed to have been defined in pre-Christian times and here

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