Knowledge (XXG)

Hohentwiel

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continued to erode the landscape. The Würm glaciation saw the Rhine glacier advance northward. The Lake Constance foreland glacier, part of the Rhine glacier, eroded the molasse and tuff layers around the Hohentwiel plug, causing the mountain summit to become exposed as the ice receded. Tuff is only
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no longer reached the surface land area, but solidified in ascending passages through the molasse. The composition of the magma likely had a higher silica content, causing the mass to have increased viscosity and durability. This resulted in the formation of a vent plug under the tuff layer,
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are situated 4-6 km north-northwest of the mountain. Hohentwiel's headwaters slope steeply downward and are completely forested while its foot has flatter slopes to the west. The mountain rises approximately 260 metres out of the Aachtal Valley to the east.
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Active volcanoes were present for a duration of 6-7 million years. The time span can be divided into two sections. In the first three million years, eruptions of volcanoes such as Ur-Hohentwiel reached the earth's surface, creating a
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Hohentwiel is located in a geological unit that encompasses Hegau and the western portion of Lake Constance. Its multiple geological layers were formed through sedimentation and volcanism, as evidenced by the Rhine Rift Valley, where
114:, is a useful starting point for translations, but translators must revise errors as necessary and confirm that the translation is accurate, rather than simply copy-pasting machine-translated text into the English Knowledge (XXG). 829:. The castle served as a Württemberg prison in the 18th century and was destroyed in 1801 after being peacefully handed over to the French. Today the former fortress Hohentwiel is the biggest castle ruin in Germany. 580:
Hohentwiel is an isolated extinct volcanic mountain located in the south of Baden-Württemberg, Germany, in the Hegau region. It is part of the administrative district of Freiburg and the district of Constance. The
547:(Old German Name Book) of 1859 in favour of a Celtic conjecture. As Hermann Jellinghaus noted upon revisiting the naming work of Förstemann in 1916, the latter suggestion was found to be "hardly Celtic", and as 720:, characterised by four major glacial periods: Günz (400,000 - 300,000 years ago), Mindel (300,000 - 200,000 years ago), Riß 200,000 - 130,000 years ago) and Würm (20,000 years ago). During these periods, 504:
The first written accounts of Hohentwiel Castle are held within the St. Gallen monastery chronicle of Ekkehard IV (circa A.D. 980-1060) as "castellum tuiel", which was reportedly besieged in 915. In the
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During the Miocene period (c. 23-5.3 million years ago), after the flood waters receded, the deep fractures and stresses caused from the uplift of the Alps and Swabian Alb resulted in
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region. This erosive processes of the subsidance caused much of the surrounding dry surface area to wear away. The material was deposited in the still-flooded depression, forming a
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In the later Middle Ages the noble families von Singen-Twiel (12th–13th centuries), von Klingen (to 1300) and von Klingenberg (to 1521) resided here. In 1521, it was passed on to
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runs at the base the eastern slope of Hohentwiel, while Lake Constance is located some kilometres south-east, and the town of Hilzingen 3 km west. The extinct volcanoes
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were formed. A remnant of this activity is the Ur-Hohentwiel vent, which is filled with depositing tuff, as well as phonolite that rises out of the eastern terrain.
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on the sea floor (marine molasse). With a thickness of roughly 5000 metres, the resulting molasse blanket filled the space between the two continents.
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mountain which towered over its surroundings by 100-200 metres. In the course of time and with a decrease in eruptions, the thickness of the covering
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Do not translate text that appears unreliable or low-quality. If possible, verify the text with references provided in the foreign-language article.
2089: 125: 2817: 2420: 2742: 2185: 806:, who developed Hohentwiel into one of the strongest fortresses of his duchy. During this time, it began to be used as a prison, and in 1526, 2797: 963: 938: 3033: 2877: 2757: 2029: 2269: 2777: 2612: 2451: 2140: 2712: 2582: 1020: 757:
sands, and Jurassic nape. These sedimentary layers range in thickness from 100 to 150 metres, with an additional 70 metres of basic
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reduced due to erosion. During the Tortonian period of the late Miocene, the second phase of volcanic activity took place. Rising
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Content in this edit is translated from the existing German Knowledge (XXG) article at ]; see its history for attribution.
2662: 2195: 845: 238: 2952: 2927: 2747: 2682: 2677: 2155: 2034: 1939: 1682: 1081: 838: 749:, Lower Freshwater Molasse, Brackish Molasse, Upper Seawater Molasse, Jurassic Gelfluh of the Upper Freshwater Molasse, 325: 2647: 509:, the name of the castle evolved from "Tuiel" to "Twiel" and eventually moved to its current spelling of "Hohentwiel" ( 210: 2707: 2672: 2657: 2597: 2180: 1971: 1712: 788: 455: 191: 42: 2782: 2667: 2220: 1415: 3048: 2882: 2857: 2632: 1375: 217: 184: 2957: 2942: 2902: 2862: 2847: 2837: 2592: 2587: 2069: 1946: 787:
Hohentwiel Castle, whose ruins are on top of Hohentwiel, was built in 914 using stone taken from the mountain by
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present in the western portion, due to the neutralising effect of the ice masses in their direction of advance.
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Stratification of the Hohentwiel landscape is characterised by layers of sedimentary rocks - including
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continents. To compensate for the elevation of land, the area inbetween the newly formed Alps and
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Miller, Douglas. Armies of the German Peasants' War 1524–1526. Oxford: Osprey Publishing, 2003.
933:. Sammlung geologischer Führer (3., berichtigte Aufl ed.). Berlin Stuttgart: Borntraeger. 2549: 2544: 2509: 2500: 2478: 2460: 2044: 2024: 2014: 1966: 1838: 1768: 1662: 1517: 1162: 1016: 959: 934: 814: 791:. Originally, the Monastery of St. Georg was within the fortress, but in 1005 it was moved to 774: 628: 582: 467: 408: 129: 1763: 2717: 2064: 2049: 1929: 1707: 1702: 1599: 1542: 1124: 883: 871: 684: 556: 532: 506: 539:
derivation of duellum meaning 'place where fighting ' but this attribution was rejected by
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origin has been advanced, on the basis of its initial sound being suggestive of an
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Hohentwiel. Die Geschichte einer Burg zwischen Festungsalltag und großer Politik
822: 796: 680: 552: 480:, along with several other volcanoes in the Hegau region. It mostly consists of 173: 866: 1999: 1859: 1790: 1748: 1614: 1567: 1547: 1502: 1475: 1400: 1390: 1380: 1308: 1288: 1119: 713: 958:. Hegau-Bibliothek (1. Aufl ed.). Singen (Hohentwiel) Bonn: Markorplan. 567:' - meaning 'swell'. Nevertheless, this interpretation remains inconclusive. 347: 334: 82: 2322: 1951: 1628: 1577: 1370: 1298: 1066: 750: 746: 481: 2115: 1961: 1807: 1795: 1758: 1562: 1323: 624: 464: 445: 473:
Hohentwiel was an active volcano about 7–8 million years ago during the
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to the source of your translation. A model attribution edit summary is
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Mountain of volcanic origin in Baden-Württemberg, Germany
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at the lower level. This is topped by an upper layer of
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material in the far western portion of the mountain.
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a machine-translated version of the German article.
716:was the last strongly formative period in Earth's 956:Hohentwiel-Buch. / mit Beitr. von Jörg Assmann 496:and giving the mountain its present-day shape. 132:accompanying your translation by providing an 94:Click for important translation instructions. 81:expand this article with text translated from 1082: 8: 931:Hegau und westlicher Bodensee: mit 1 Tabelle 510: 57:Learn how and when to remove these messages 2216: 2161: 1979: 1232: 1089: 1075: 1067: 954:Peters, Dirk (2002). Assmann, Jörg (ed.). 292: 16:For the maritime patrol radar system, see 276:Learn how and when to remove this message 258:Learn how and when to remove this message 3039:Mountains and hills of Baden-Württemberg 639:convering the area and formation of the 896: 850: 2191:Rheineck–Walzenhausen Mountain Railway 2186:International Rhine Regulation Railway 619:Sedmentation since the Jurassic Period 783:Aerial photo of the Hohentwiel castle 395:The location within Baden-Württemberg 7: 1002:; Silberburg Verlag, Stuttgart, 1960 924: 922: 196:adding citations to reliable sources 1000:Konrad Widerholt, Ein Mann in Hegau 382: 14: 627:(201-145 million years ago), the 38:This article has multiple issues. 3054:Mountains and hills of the Hegau 1641: 1634: 1627: 877: 865: 853: 704:approximately 100 metres thick. 381: 374: 301: 172: 68: 27: 667:Volcanism in the Miocene Period 183:needs additional citations for 46:or discuss these issues on the 484:, which represents the former 142:You may also add the template 1: 839:List of volcanoes in Germany 320:696.2 m (2,284 ft) 144:{{Translated|de|Hohentwiel}} 3034:Extinct volcanoes of Europe 2663:Friedrichshafen Landratsamt 2176:Bodensee–Toggenburg Railway 1015:. Stadler, Konstanz, 1990, 813:The fortress resisted five 804:Duke Ulrich von Württemberg 789:Burchard II, Duke of Swabia 655:subsided, and with it, the 551:recurs in several areas of 155:Knowledge (XXG):Translation 3070: 2421:Stahringen–Friedrichshafen 929:Schreiner, Albert (2008). 808:Hans Müller von Bulgenbach 772: 449:of the industrial city of 106:Machine translation, like 15: 2813:Münsterlingen-Scherzingen 2648:Friedrichshafen-Fischbach 1625: 1108: 708:The Quaternary Glaciation 368: 300: 83:the corresponding article 2658:Friedrichshafen Kluftern 2452:St. Margrethen–Lauterach 2196:Rorschach–Heiden Railway 2090:Wettingen-Mehrerau Abbey 1872:Bregenz Forest Mountains 2783:Ludwigshafen (Bodensee) 2668:Friedrichshafen-Manzell 2146:Friedrichshafen Airport 1062:virtual Hohentwiel tour 1039:(in German). 7 May 2020 907:(in German). 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It is the 439:in southern 424: 423: 290: 272: 254: 245: 235: 228: 221: 214: 207:"Hohentwiel" 202: 190:Please help 185:verification 182: 130:edit summary 121: 88: 80: 54: 47: 41: 40:Please help 37: 2753:Langenargen 2708:Kreuzlingen 2623:Enzisweiler 2598:Bottighofen 2151:Pfänderbahn 1940:Rhine Delta 1882:Hohenkrähen 1855:Allgäu Alps 1784:Alter Rhein 1683:Liebesinsel 1673:Galgeninsel 1528:Kreuzlingen 1466:Bottighofen 1444:Switzerland 1361:Langenargen 1329:Dingelsdorf 1229:Settlements 1216:Kreuzlingen 1173:Switzerland 823:Catholicism 797:Switzerland 653:Swabian Alb 623:During the 591:Hohenkrähen 553:Switzerland 351: / 326:Coordinates 3028:Categories 2963:Wasserburg 2933:Überlingen 2898:Stahringen 2888:Sipplingen 2883:Seebleiche 2873:Sandbüchel 2858:Romanshorn 2833:Radolfzell 2823:Nonnenhorn 2738:Kressbronn 2633:Ermatingen 2568:Allensbach 2550:Vorarlberg 2545:St. Gallen 2181:Gürtelbahn 1972:Zeller See 1892:Hohentwiel 1791:High Rhine 1749:Brunnisach 1713:Vogelinsel 1615:Wolfhalden 1588:Tägerwilen 1568:Salenstein 1548:Romanshorn 1533:Lutzenberg 1503:Gottlieben 1476:Ermatingen 1435:Wasserburg 1411:Überlingen 1401:Sipplingen 1391:Radolfzell 1381:Nonnenhorn 1356:Kressbronn 1349:Wallhausen 1319:Immenstaad 1309:Gaienhofen 1289:Allensbach 1211:Frauenfeld 1189:St. Gallen 1120:Vorarlberg 891:References 535:pursued a 520:High Twiel 456:Zeller See 435:region of 425:Hohentwiel 389:Hohentwiel 336:47°45′53″N 296:Hohentwiel 218:newspapers 43:improve it 2958:Wartensee 2903:Steckborn 2863:Ruderbach 2848:Rorschach 2678:Güttingen 2628:Eriskirch 2588:Berlingen 2323:Lake Line 2099:Touristic 1983:Buildings 1952:Gnadensee 1913:Landmarks 1904:Seerücken 1848:Mountains 1703:Reichenau 1668:Entlibühl 1593:Tägermoos 1578:Steckborn 1553:Rorschach 1508:Güttingen 1493:Frasnacht 1461:Berlingen 1396:Reichenau 1371:Meersburg 1299:Eriskirch 1194:Rorschach 884:Geography 872:Volcanoes 751:phonolite 747:Tithonian 693:tuff cone 595:Mägdeberg 576:Geography 557:Alemannic 482:phonolite 364:Geography 339:8°49′08″E 316:Elevation 248:June 2008 148:talk page 85:in German 49:talk page 2913:Steinach 2843:Rheineck 2828:Nussdorf 2788:Lustenau 2718:Konstanz 2560:Stations 2540:Bodensee 1962:Rheinsee 1947:Untersee 1808:Schussen 1796:Seerhein 1759:Leiblach 1573:Steinach 1563:Salmsach 1416:Hödingen 1386:Öhningen 1339:Paradies 1324:Konstanz 1258:Hörbranz 1151:Konstanz 1100:Bodensee 833:See also 815:Imperial 795:(now in 685:Riedheim 681:Höwenegg 649:European 613:the Alps 465:medieval 446:Hausberg 429:volcanic 405:Location 124:provide 2793:Mammern 2703:Kesswil 2638:Eschenz 2603:Bregenz 2167:Railway 1920:Obersee 1860:Pfänder 1827:Valleys 1764:Lipbach 1651:Islands 1538:Mammern 1523:Kesswil 1498:Goldach 1488:Eschenz 1406:Stetten 1282:Germany 1268:Gaissau 1263:Fussach 1243:Bregenz 1236:Austria 1201:Thurgau 1158:Bavaria 1135:Germany 1125:Bregenz 1114:Austria 1043:18 June 860:Germany 846:Portals 825:in the 763:moraine 645:African 606:Geology 543:in his 514:  475:Miocene 441:Germany 417:Germany 232:scholar 146:to the 128:in the 87:. 3001:People 2948:Uttwil 2693:Heiden 2618:Egnach 2573:Altnau 2532:S-Bahn 2211:Thurbo 2201:Seehas 1803:Rotach 1727:Rivers 1693:Mainau 1688:Lindau 1605:Uttwil 1513:Heiden 1471:Egnach 1451:Altnau 1366:Lindau 1314:Hagnau 1273:Lochau 1253:Höchst 1163:Lindau 1019:  962:  937:  911:2 June 759:facies 563:root ' 451:Singen 234:  227:  220:  213:  205:  2985:Films 2893:Staad 2688:Hegne 2578:Arbon 2440:IRE 3 2431:RB 31 2409:IRE 3 2400:RB 32 2391:RB 31 2280:RB 93 1877:Hegau 1774:Rhine 1739:Argen 1456:Arbon 1206:Arbon 701:magma 697:tuffs 657:Hegau 587:Rhine 549:Twiel 537:Latin 529:Twiel 478:epoch 433:Hegau 239:JSTOR 225:books 108:DeepL 2698:Horn 2311:RE 2 2206:SWEG 1734:Aach 1718:Werd 1600:Thal 1518:Horn 1376:Moos 1248:Hard 1045:2021 1017:ISBN 960:ISBN 935:ISBN 913:2024 755:mica 712:The 647:and 597:and 511:lit. 211:news 122:must 120:You 101:View 2369:RE1 2360:S44 2351:S14 1678:Hoy 683:to 194:by 110:or 3030:: 2520:S7 2511:S3 2502:S1 2480:R5 2471:S7 2462:S3 2342:S7 2333:S1 2302:S6 2258:S7 2249:S5 2240:S4 2231:S2 1035:. 921:^ 745:, 741:, 737:, 687:. 593:, 565:tu 415:, 411:, 52:. 1102:) 1090:e 1083:t 1076:v 1047:. 968:. 943:. 915:. 848:: 523:' 517:' 459:( 279:) 273:( 261:) 255:( 250:) 246:( 236:· 229:· 222:· 215:· 188:. 157:. 150:. 59:) 55:( 20:.

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Hohentwiel (Radar)
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Elevation
Coordinates
47°45′53″N 8°49′08″E / 47.76472°N 8.81889°E / 47.76472; 8.81889
Hohentwiel is located in Baden-Württemberg

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