2136:
2124:
663:
167:
53:
1106:
2994:
679:
1091:
2276:
second-generation
Japanese Americans (Nisei), during which the 442nd charged straight up the mountain to rescue the 1st Battalion of the 36th Infantry, formerly the Texas Guard—also known as the "Lost Battalion"—who were cut off and stranded on the mountainside under heavy fire from the Germans. Two previous rescues failed. The 442nd suffered 800 casualties, rescued the Texans, and took the mountain.
687:
671:
552:
695:
654:, a major extensional basin. When such basins form, the thinning of the crust causes uplift immediately adjacent to the basin, decreasing with distance from the basin. Thus, the highest range of peaks rises immediately adjacent to the basin and increasingly lower mountains rise further from the basin.
1120:
the difference between the eastern and western mean slopes of the range is very marked. The main air streams come generally from the west and southwest, so the
Alsatian central plains just under the Hautes-Vosges receive much less water than the south-west front of the Vosges Mountains. The highlands
1125:
of
Remiremont receive as annual rainfall or snowfall more than 2,000 mm (79 in) of precipitation yearly, whereas some dry countryside near Colmar receives less than 500 mm (20 in) of water in the event of insufficient storms. The temperature is much lower in the west front of the
2275:
The Vosges saw extensive fighting during the world wars. During World War I, there was severe and almost continuous fighting in the mountains. During World War II in
October 1944, there was a fierce battle between German forces and the U.S. 442nd Regiment, a segregated unit composed of
641:
since both lie within the same degrees of latitude, have similar geological formations and are characterized by forests on their lower slopes, above which are open pastures and rounded summits of a rather uniform altitude. Both areas exhibit steeper slopes towards the
630:(a French name for a Triassic rose sandstone) are embedded sometimes up to more than 500 m (1,600 ft) in thickness. The Lower Vosges in the north are dislocated plates of various sandstones, ranging from 300 to 600 m (1,000 to 2,000 ft) high.
2209:
valley, for example, there was an influx of Saxon miners and mining specialists. From time to time, wars, plagues and religious conflicts saw the depopulation of territories – in their wake it was not uncommon for people to be relocated there from other areas.
1126:
mountains than in the low plains behind the massif, especially in summer. On the eastern slope economic vineyards reach to a height of 400 m (1,300 ft); on the other hand, in the mountains, it is a land of pasture and forest.
477:. The latter area logically continues the same Vosges geologic structure but traditionally receives this different name for historical and political reasons. From 1871 to 1918 the Vosges marked for the most part the border between
2746:, Tome 1 à 4 et index alphabétique général, Auguste Picard éditeur, Paris, 1924. Anastaltic impression in Belgium by the éditions Culture et Civilisation, Bruxelles, 1978. (large and more sophisticated evenemential history)
542:
In addition, the term "Central Vosges" is used to designate the various lines of summits, especially those above 1,000 m (3,300 ft) in elevation. The French department of Vosges is named after the range.
583:. From a scientific view, the Vosges Mountains are not mountains as such, but rather the western edge of the unfinished Alsatian graben, stretching continuously as part of the larger Tertiary formations. Erosive
345:
2217:
side are numerous castles, generally in ruins, testifying to the importance of this crucial crossroads of Europe, violently contested for centuries. At several points on the main ridge, especially at
2225:(German: Rappoltsweiler), are the remains of a wall of unmortared stone with tenons of wood, about 1.8 to 2.2 m (6 to 7 ft) thick and 1.3 to 1.7 m (4 to 6 ft) high, called the
366:
2378:
region in the south. For a long time the distribution of languages and dialects basically correlated with the pattern of settlement movements. However, the switch from German to French as the
2174:
Over the centuries, settlement population density grew gradually, as was typical for a forested region. Forests were cleared for agriculture, livestock and early industrial factories (such as
734:
to 1,247 m (4,091 ft). The Col de Saales, between the Higher and
Central Vosges, reaches nearly 579 m (1,900 ft), both lower and narrower than the Higher Vosges, with
2426:
2307:
in the northwest. Contrary to widespread belief, the main ridge of the Vosges coincided with the historical Roman-Germanic language boundary only in the southern Vosges. Old
Romance (
3028:
1192:
1064:
2674:
Mémoire sur quelques anciennes fortifications des Vosges, ou l'on examine la question de savoir quel peuple au temps de Jules-César, était établi dans la Haute-Alsace
1079:
2923:
1172:, and green meadows provide pasture for large herds of cattle, with views of the Rhine valley, the Black Forest and the distant, snow-covered Swiss mountains.
2698:
2382:
which took place between the 17th and the 20th century across the whole of Alsace was not accompanied by any further significant movements of population.
3023:
3018:
2865:
2851:
2564:
2391:
1075:
1048:
527:
1137:
which have as tributaries other, shorter but sometimes powerful streams coming like the last two from the Vosges
Mountains. The rivers
2932:
2396:
403:
unit and low mountain range of around 8,000 km (3,100 sq mi) in area. It runs in a north-northeast direction from the
2916:
2773:
2758:
2725:
2448:
2135:
2118:
326:
108:
5,500 km (2,100 sq mi)up to 6,000 km (2,300 sq mi) depending on the natural region boundaries selected
2539:
2128:
211:
1164:
which once covered the top of the Vosges. The mountain lakes caused by the original glacial phenomena are surrounded by pines,
2792:
1044:
2891:
2140:
2123:
1056:
2909:
204:
2661:
Brown, James Daniel, Facing the
Mountain, a True Story of Japanese American Heroes in WWII (Viking, 2021), Chapter 18.
2600:
2453:
2993:
2401:
197:
618:
masses or other volcanic intrusions. The north, south and west parts are less eroded by glaciers, and here Vosges
388:
3033:
2647:
2283:
crashed into the Vosges
Mountains while circling to land at Strasbourg International Airport, killing 87 people.
2249:
907:
376:
147:
372:
359:
2354:
the historical linguistic boundary turns to the northwest and runs between Donon and
Mutzigfelsen heading for
1023:
530:, a sandstone plateau ranging from 300 metres (1,000 ft) to 560 metres (1,850 ft) high, between the
2464:
2163:, was extended to the vast woods covering the region. Later, German speakers referred to the same region as
662:
2860:, Actes du colloque tenu à Epinal du 4 au 6 septembre 2008, Conseil général des Vosges, 2009, 348 pages.
901:
31:
2768:, guide régionaux, collection dirigée par Charles Pomerol, 2° édition, Masson, Paris, 1984, 184 pages.
2625:
512:
Vosges or Middle Vosges (50 km, 31 mi), between the Permian Basin of Saint-Die including the
939:
895:
2735:, Flammarion, 1977, 288 pages (a geogropher's view of this part of France who gives theirs waters to
2367:
2324:
2280:
2253:
588:
416:
987:
2856:
Isabelle Chave (dir.) avec Magali Delavenne, Jean-Claude Fombaron, Philippe Nivet, Yann Prouillet,
1003:
971:
482:
258:
35:
2692:
2641:
919:
646:
and a more gradual descent on the other side. Both the Vosges and the Black Forest were formed by
166:
2329:
885:
277:
264:
2879:
2261:
2199:
1183:
981:
933:
913:
869:
731:
1105:
741:
The highest mountains and peaks of the Vosges (with Alsatian or German names in brackets) are:
2875:
2861:
2847:
2769:
2754:
2721:
2350:, which lie north of the Breusch valley, fall within the Germanic-speaking area because, from
2291:
In pre-Roman times, the Vosges was empty of settlements or was colonized and dominated by the
1013:
993:
819:
678:
470:
432:
188:
2948:
2823:
2371:
2363:
801:
761:
723:
447:
309:
269:
1090:
3013:
2895:
2836:
2487:
2269:
1142:
1094:
1052:
647:
404:
396:
351:
338:
132:
2421:
2968:
2963:
2339:
2222:
2148:
1134:
1122:
1071:
889:
807:
783:
535:
531:
498:
497:), extending in the southern part of the range from Belfort to the river valley of the
466:
2190:. Concentrations of settlement and immigration took place and not only in areas where
3007:
2687:
2379:
2375:
2312:
2257:
835:
599:
400:
2482:
2753:, La bibliothèque du naturaliste, Delachaux et Niestlé, Lausanne, 1998, 352 pages.
2370:
region and cultural area. The Romance-speaking areas are traditionally part of the
2296:
2238:
2218:
1146:
1130:
1098:
855:
795:
745:
719:
707:
651:
634:
576:
439:
75:
52:
2268:
in the north with the lands east of it being incorporated into Germany as part of
2204:
879:
424:
2672:
2640:
2234:
2230:
1113:
1040:
789:
755:
738:
at 1,008 m (3,307 ft) being the highest point of this Nordic section.
615:
443:
428:
17:
2510:
686:
2355:
2316:
2265:
2187:
2183:
2179:
1117:
773:
767:
735:
727:
420:
2827:, Nancy (Lotharingist wrintings since 1820, nowadays trimestrial périodical,
2256:. From 1871 to 1918, they formed the main border line between France and the
226:
213:
2901:
2892:
Illustrated article on the Vosges battlefields of WWI at Battlefields Europe
2351:
955:
670:
623:
564:
551:
520:
517:
509:
458:
294:
290:
193:
526:
The Lower Vosges or Low Vosges (48 km, 30 mi), commonly known as
2468:
1665:
2978:
2953:
2691:
2543:
2300:
2191:
2175:
1150:
845:
825:
813:
619:
513:
412:
2702:. Vol. 28 (11th ed.). Cambridge University Press. p. 214.
2346:). By contrast, those parts of the northern Vosges and the whole of the
1070:
In the late 20th century, a wide area of the massif was included in two
694:
2958:
2568:
2114:
1161:
1157:
1138:
1133:
coming from south Alsace (or Sundgau), and the Bruche d'Andlau and the
965:
611:
603:
584:
580:
478:
474:
408:
392:
286:
248:
58:
1200:
1178:
2973:
2458:
2347:
2304:
2214:
2195:
1060:
607:
572:
568:
560:
486:
462:
442:
is the highest peak at 1,424 m (4,672 ft), followed by the
384:
282:
181:
82:
2844:
Guide des sources de la Grande Guerre dans le département des Vosges
2780:
List of majors periodicals concerning Lorraine and South Lorraine:
2751:
L'Alsace et les Vosges, géologie, milieux naturels, flore et faune
2515:
2292:
2134:
2122:
1169:
1165:
1104:
1089:
949:
693:
685:
677:
669:
661:
643:
638:
550:
399:
to the north on the German side of the border, they form a single
2858:
La Grande Guerre dans les Vosges : sources et état des lieux
1160:, boulders and polished rocks testify to the former existence of
2943:
2736:
2677:(in French). de l'imprimerie de F.G. Levrault, imprimeur du Roi.
2242:
2905:
571:
and the uplift of the bedrock plates of the Vosges, in eastern
2362:). The Germanic areas of the Vosges mountains are part of the
633:
The Vosges are very similar to the corresponding range of the
594:
The Vosges in their southern and central parts are called the
318:
2366:
region and cultural area and, in the north, also part of the
2213:
On the lower heights and buttresses of the main chain on the
315:
2874:édité par la Société Philomatique Vosgienne, , 68 pages.
2311:) is spoken east of the main ridge: in the valley of the
2427:
The American Heritage Dictionary of the English Language
1059:
on the German side of the border form the cross-border
587:
action was the primary catalyst for development of the
2846:, Conseil général de Vosges, Epinal, 2008, 296 pages.
2744:
Histoire de Lorraine (Meurthe, Meuse, Moselle, Vosges)
2601:"Parc naturel régional des Ballons des Vosges | PnrBV"
2583:
2581:
2579:
2577:
501:. The rounded summits of the Hautes Vosges are called
139:
2319:, the valley of Lièpvrette (nowadays also called the
327:
2252:, on 13 July 1794, the Vosges were the scene of the
312:
276:
257:
247:
242:
203:
187:
177:
158:
117:
112:
104:
96:
91:
81:
71:
66:
45:
2511:"Vogesen | Rechtschreibung, Bedeutung, Definition"
2870:"La guerre aérienne dans les Vosges. 1914–1919",
2733:Atlas et géographie de l'Alsace et de la Lorraine
2651:. New York: P. F. Collier & Son Company.
2131:in the Vosges was built during the 12th century.
1065:Palatinate Forest-North Vosges Biosphere Reserve
523:of Schirmeck-Moyenmoutier and the Col de Saverne
489:is divided south to north into three sections:
2720:, éditions Serpenoise, Metz, 1991, 224 pages.
2323:; "Valley of Silver"), parts of the canton of
2917:
2800:Bulletin de la Société Philomatique Vosgienne
2229:(Pagan Wall). It was used for defence in the
1149:and their numerous affluents all rise on the
431:line), and forms the western boundary of the
383:) are a range of medium mountains in Eastern
8:
2811:Société d'Histoire et d'Archéologie lorraine
2804:Mémoire des Vosges Histoire Société Coutumes
2605:Parc naturel régional des Ballons des Vosges
1080:Parc naturel régional des Ballons des Vosges
124:
718:rises to 1,424 m (4,672 ft); the
3029:Mountain ranges of Bourgogne-Franche-Comté
2924:
2910:
2902:
2561:Germany: A Regional and Economic Geography
2260:. The demarcation line stretched from the
2237:are divided as to whether it was built by
42:
2802:, Saint-Dié, from 1875 to 1999 (nowadays
730:to 1,350 m (4,429 ft); and the
2822:Société d'Histoire de la Lorraine &
2587:
2089:Average max. and min. temperatures in °F
1643:Average max. and min. temperatures in °C
1156:In the High Moselle and Meurthe basins,
1076:Parc naturel régional des Vosges du Nord
2728:(simple historic approach for children)
2413:
446:(1,366 m, 4,482 ft), and the
2392:Northern Vosges Regional Natural Park
888:(highest point in the département of
726:to 1,364 m (4,475 ft); the
722:to 1,366 m (4,482 ft); the
626:remains are found in large beds. The
461:, the Vosges Mountains are wholly in
358:
337:
7:
2563:(2nd ed.). London: Methuen, p. 540.
1109:View from Mont Saint-Odile in Autumn
1049:Northern Vosges Regional Nature Park
2555:
2553:
2551:
559:From a geological point of view, a
2639:Reynolds, Francis J., ed. (1921).
2397:Vosges and Jura coal mining basins
1129:The only rivers in Alsace are the
650:in response to the opening of the
493:The Higher Vosges or High Vosges (
419:line) to the Börrstadt Basin (the
25:
2119:Battle of Vosges (disambiguation)
2992:
2776:(a precise geologic description)
2761:(global view of nature and land)
1035:Nature parks and protected areas
602:mountain eroded just before the
505:in French, literally "balloons".
308:
165:
51:
567:period caused the formation of
450:(1,364 m, 4,475 ft).
272:stratigraphic unit: 252–243 mya
2793:Société d'Émulation des Vosges
2766:Guide géologique Vosges-Alsace
2488:Merriam-Webster.com Dictionary
2303:also settled in the east, and
2097:Precipitation totals in inches
1078:(established in 1976) and the
1045:Ballons des Vosges Nature Park
946:) 1,008 m (3,307 ft)
930:) 1,098 m (3,602 ft)
892:) 1,216 m (3,990 ft)
876:) 1,247 m (4,091 ft)
866:) 1,272 m (4,173 ft)
852:) 1,292 m (4,239 ft)
842:) 1,302 m (4,272 ft)
832:) 1,302 m (4,272 ft)
780:) 1,330 m (4,364 ft)
752:) 1,424 m (4,672 ft)
702:The highest points are in the
263:Gneiss, granite and vulcanite
1:
2898: (archived 20 April 2012)
2785:Annales de l'Est (et du Nord)
2671:Golbéry, Philippe de (1823).
2430:(5th ed.). HarperCollins
1057:Palatinate Forest Nature Park
3024:Mountain ranges of Grand Est
3019:Biosphere reserves of France
2813:, Metz (from 1890, nowadays
2559:Dickinson, Robert E (1964).
1030:) 550 m (1,804 ft)
1020:) 581 m (1,906 ft)
1010:) 650 m (2,130 ft)
1000:) 764 m (2,507 ft)
978:) 956 m (3,136 ft)
962:) 992 m (3,255 ft)
952:1,008 m (3,307 ft)
936:1,074 m (3,524 ft)
916:1,123 m (3,684 ft)
910:1,148 m (3,766 ft)
904:1,191 m (3,907 ft)
898:1,200 m (3,937 ft)
882:1,229 m (4,032 ft)
822:1,303 m (4,275 ft)
816:1,305 m (4,281 ft)
810:1,306 m (4,285 ft)
804:1,306 m (4,285 ft)
798:1,311 m (4,301 ft)
792:1,314 m (4,311 ft)
786:1,316 m (4,318 ft)
770:1,350 m (4,429 ft)
764:1,363 m (4,472 ft)
758:1,366 m (4,482 ft)
87:1,424 m (4,672 ft)
2374:region in the west and the
2141:Château du Grand-Geroldseck
2129:Château du Haut-Kœnigsbourg
1043:lie within the Vosges: the
598:. These consist of a large
171:Map of the Vosges Mountains
3050:
2648:Collier's New Encyclopedia
2402:Flora of the Vosges massif
2112:
2093:
2085:
1668:
1655:
1651:Precipitation totals in mm
1647:
1639:
1116:, as a consequence of the
990:837 m (2,746 ft)
984:901 m (2,956 ft)
968:965 m (3,166 ft)
710:, in ancient times called
555:Upper Vosges Mountains map
57:Houses on the slopes near
29:
2990:
2939:
2933:Mountain ranges of France
2872:Mémoire des Vosges H.S.C.
2250:French Revolutionary Wars
908:Planche des Belles Filles
469:separating them from the
163:
50:
2642:"Vosges Mountains"
563:at the beginning of the
100:120 km (75 mi)
27:Mountain range in France
2699:Encyclopædia Britannica
2465:Oxford University Press
1082:(established in 1989).
481:and France, due to the
380:
198:Bourgogne-Franche-Comté
140:
2817:, trimestrial review).
2144:
2132:
1110:
1102:
699:
691:
683:
675:
667:
556:
534:and the source of the
355:
125:
34:of the same name, see
2764:Jean-Paul von Eller,
2461:UK English Dictionary
2138:
2126:
2113:Further information:
1108:
1093:
697:
689:
681:
673:
665:
554:
253:Medium mountain range
2820:Publications of the
2815:Les Cahiers Lorrains
2809:Publications of the
2796:, Epinal, from 1826.
2718:Histoire de Lorraine
2281:Air Inter Flight 148
2254:Battle of Trippstadt
2243:before their arrival
2147:The massif known in
1656:Source: Meteociel.fr
1055:Nature Park and the
712:Ballon de Guebwiller
395:. Together with the
32:department of France
2344:Vallée de la Bruche
2338:) and parts of the
2279:On 20 January 1992
2194:were found. In the
1669:Imperial conversion
976:Hartmannsweilerkopf
972:Hartmannswillerkopf
575:, and those in the
483:Franco-Prussian War
360:[voˈɡeːzn̩]
267:: about 419–252 mya
265:stratigraphic units
223: /
36:Vosges (department)
2749:Yves Sell (dir.),
2731:Etienne Julliard,
2542:maps available on
2145:
2133:
1111:
1103:
1018:Großer Wintersberg
886:Ballon de Servance
716:Ballon de Murbach,
700:
692:
684:
676:
668:
557:
67:Highest point
3001:
3000:
2866:978-2-86088-067-1
2852:978-2-86088-062-6
2491:. Merriam-Webster
2364:Alemannic dialect
2105:
2104:
2101:
2100:
1660:
1659:
1014:Grand Wintersberg
994:Mont Sainte-Odile
471:Palatinate Forest
433:Upper Rhine Plain
300:
299:
205:Range coordinates
16:(Redirected from
3041:
3034:Horsts (geology)
2996:
2949:Armorican Massif
2926:
2919:
2912:
2903:
2742:Robert Parisot,
2703:
2695:
2679:
2678:
2668:
2662:
2659:
2653:
2652:
2644:
2636:
2630:
2629:
2626:"気象庁｜過去の気象データ検索"
2622:
2616:
2615:
2613:
2611:
2597:
2591:
2585:
2572:
2557:
2546:
2537:
2531:
2529:
2527:
2525:
2507:
2501:
2500:
2498:
2496:
2479:
2473:
2472:
2471:on 5 March 2020.
2467:. Archived from
2446:
2440:
2439:
2437:
2435:
2418:
2372:Lorrain language
2368:Frankish dialect
2333:
2264:in the south to
2208:
2096:
2088:
2079:
2074:
2063:
2048:
2043:
2032:
2017:
2012:
2001:
1986:
1981:
1970:
1955:
1950:
1939:
1924:
1919:
1908:
1893:
1888:
1877:
1862:
1857:
1846:
1831:
1826:
1815:
1800:
1795:
1784:
1769:
1764:
1753:
1738:
1733:
1722:
1666:
1650:
1642:
1633:
1628:
1617:
1602:
1597:
1586:
1571:
1566:
1555:
1540:
1535:
1524:
1509:
1504:
1493:
1478:
1473:
1462:
1447:
1442:
1431:
1416:
1411:
1400:
1385:
1380:
1369:
1354:
1349:
1338:
1323:
1318:
1307:
1292:
1287:
1276:
1201:
1179:
1114:Meteorologically
940:Rocher de Mutzig
874:Elsässer Belchen
802:Haut de Falimont
648:isostatic uplift
622:and Permian red
591:massif feature.
485:. The elongated
465:, far above the
401:geomorphological
377:Alemannic German
370:
369:
368:
362:
349:
348:
347:
341:
336:
330:
325:
324:
321:
320:
317:
314:
270:Bunter sandstone
238:
237:
235:
234:
233:
228:
224:
221:
220:
219:
216:
169:
151:
148:Alemannic German
143:
136:
128:
55:
43:
21:
18:Vosges mountains
3049:
3048:
3044:
3043:
3042:
3040:
3039:
3038:
3004:
3003:
3002:
2997:
2988:
2935:
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1088:
1072:protected areas
1053:Northern Vosges
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2693:"Vosges"
2690:, ed. (1911).
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2608:. Retrieved
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2522:. Retrieved
2514:
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2493:. Retrieved
2486:
2477:
2469:the original
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2444:
2432:. Retrieved
2425:
2416:
2359:
2343:
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2325:Villé valley
2321:Val d'Argent
2320:
2309:Altromanisch
2308:
2295:. After the
2290:
2278:
2274:
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2226:
2219:Sainte Odile
2212:
2198:area of the
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2168:
2164:
2161:Vogesus mons
2160:
2159:, sometimes
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2156:
2153:Vosago mons
2152:
2146:
1182:
1174:
1155:
1128:
1118:Foehn effect
1112:
1099:glacial lake
1069:
1063:-designated
1041:nature parks
1038:
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944:Mutzigfelsen
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920:Champ du Feu
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863:
860:Kahler Wasen
859:
856:Petit Ballon
849:
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796:Batteriekopf
777:
749:
746:Grand Ballon
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720:Storckenkopf
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711:
708:Grand Ballon
703:
701:
666:Grand Ballon
652:Rhine Graben
635:Black Forest
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628:grès vosgien
627:
606:Period with
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577:Black Forest
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528:North Vosges
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440:Grand Ballon
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278:Type of rock
76:Grand Ballon
40:
2524:17 February
2520:(in German)
2495:17 February
2434:17 February
2328: [
2248:During the
2231:Middle Ages
2223:Ribeauvillé
2203: [
2188:water power
2184:water mills
1193:explanation
998:Odilienberg
890:Haute-Saône
840:Sulzereneck
790:Lauchenkopf
756:Storkenkopf
674:Storkenkopf
637:across the
616:porphyritic
444:Storkenkopf
387:, near its
259:Age of rock
230: /
118:Native name
3008:Categories
2569:B000IOFSEQ
2544:Géoportail
2408:References
2356:Sarrebourg
2317:Lapoutroie
2266:Mont Donon
2239:the Romans
2200:Lièpvrette
2182:) and the
2180:glassworks
2178:works and
2169:Wasgenwald
1024:Hohenbourg
982:Ungersberg
934:Baerenkopf
914:Molkenrain
774:Klintzkopf
768:Kastelberg
736:Mont Donon
728:Kastelberg
690:Kastelberg
421:Winnweiler
373:Franconian
92:Dimensions
2880:1626-5238
2451:(US) and
2352:Schirmeck
2227:Mur Païen
1028:Hohenburg
956:Taennchel
928:Firstfeld
880:Brézouard
778:Klinzkopf
658:Mountains
624:sandstone
565:Paleogene
518:Dinantian
510:sandstone
454:Geography
425:Börrstadt
295:sandstone
291:vulcanite
194:Grand Est
159:Geography
83:Elevation
61:in France
2979:Pyrenees
2954:Ardennes
2787:, Nancy.
2610:10 March
2483:"Vosges"
2454:"Vosges"
2449:"Vosges"
2422:"Vosges"
2386:See also
2360:Saarburg
2301:Alemanni
2287:Language
2215:Alsatian
2192:minerals
2176:charcoal
1162:glaciers
1158:moraines
1151:Lorraine
1047:and the
1008:Dagsburg
960:Tännchel
924:Hochfeld
902:Rossberg
846:Le Tanet
830:Ringbühl
826:Ringbuhl
814:Rainkopf
698:Le Tanet
620:Triassic
612:granites
589:highland
514:Devonian
429:Göllheim
413:Ronchamp
227:48°N 7°E
30:For the
2959:Corsica
2894:at the
2835:On the
2315:around
2165:Vogesen
2115:Vosagus
2109:History
1166:beeches
1143:Meurthe
1139:Moselle
1121:of the
1086:Climate
966:Climont
896:Drumont
850:Tanneck
762:Hohneck
724:Hohneck
682:Hohneck
604:Permian
585:glacial
581:Germany
547:Geology
503:ballons
479:Germany
475:Germany
448:Hohneck
409:Belfort
393:Germany
356:Vogesen
335:French:
287:granite
249:Orogeny
243:Geology
178:Country
126:Vogesen
59:Bussang
3014:Vosges
2984:Vosges
2974:Morvan
2878:
2864:
2850:
2772:
2757:
2724:
2567:
2518:online
2459:Lexico
2348:Wasgau
2305:Franks
2221:above
2196:mining
2069:
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2007:
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1996:
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1268:
1170:maples
1153:side.
1135:Bruche
1074:, the
1061:UNESCO
1051:. The
706:: the
608:gneiss
573:France
569:Alsace
561:graben
536:Lauter
499:Bruche
487:massif
463:France
389:border
385:France
381:Vogese
352:German
304:Vosges
283:Gneiss
189:Region
182:France
144:
141:Vogese
133:German
129:
113:Naming
97:Length
46:Vosges
2516:Duden
2332:]
2313:Weiss
2299:era,
2297:Roman
2293:Celts
2241:, or
2207:]
2186:used
2149:Latin
1147:Sarre
950:Donon
644:Rhine
639:Rhine
579:, in
407:(the
391:with
329:VOHZH
232:48; 7
2944:Alps
2876:ISSN
2862:ISBN
2848:ISBN
2770:ISBN
2755:ISBN
2737:Rhin
2722:ISBN
2612:2024
2565:ASIN
2526:2019
2497:2019
2436:2019
2233:and
2139:The
2127:The
2117:and
1168:and
1145:and
1097:, a
1039:Two
1004:Dabo
508:The
438:The
417:Lure
375:and
302:The
215:48°N
105:Area
72:Peak
2540:IGN
2167:or
2155:or
2151:as
2031:8.5
2000:8.3
1969:6.1
1938:6.2
1907:5.9
1876:5.3
1814:4.9
1783:7.7
1721:9.9
1616:289
1585:215
1554:211
1523:154
1492:157
1461:149
1430:135
1399:179
1368:124
1337:197
1306:204
1275:252
1131:Ill
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714:or
473:in
218:7°E
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1949:65
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1918:65
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1861:43
1856:56
1830:36
1825:49
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1794:40
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1763:35
1737:26
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1565:10
1534:14
1508:11
1503:18
1477:11
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1441:17
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1353:−1
1322:−4
1291:−3
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316:oʊ
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