2125:
2113:
652:
333:
156:
354:
42:
1095:
2983:
668:
1080:
676:
660:
541:
2265:
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.
684:
643:, 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.
1109:
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
1114:
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
2264:
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
630:
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
619:(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.
2198:
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.
1115:
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.
466:. 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
2735:, 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)
531:
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.
572:. 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
334:
2206:
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
2214:(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
355:
2367:
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
2163:
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
723:
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
2296:
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 (
2663:
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
2415:
2313:
1161:, 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.
3017:
890:
2371:
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.
976:
1181:
928:
884:
1053:
992:
2188:
1068:
908:
2912:
970:
922:
902:
2687:
1126:
which have as tributaries other, shorter but sometimes powerful streams coming like the last two from the Vosges
Mountains. The rivers
392:
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
2437:
97:
5,500 km (2,100 sq mi)up to 6,000 km (2,300 sq mi) depending on the natural region boundaries selected
200:
1153:
which once covered the top of the Vosges. The mountain lakes caused by the original glacial phenomena are surrounded by pines,
3012:
3007:
2854:
2840:
2553:
2380:
1064:
2880:
1037:
516:
2921:
2385:
2650:
Brown, James Daniel, Facing the
Mountain, a True Story of Japanese American Heroes in WWII (Viking, 2021), Chapter 18.
2589:
2442:
2905:
2762:
2747:
2714:
2107:
315:
2528:
2117:
607:
masses or other volcanic intrusions. The north, south and west parts are less eroded by glaciers, and here Vosges
2272:
crashed into the Vosges
Mountains while circling to land at Strasbourg International Airport, killing 87 people.
1033:
2781:
2343:
the historical linguistic boundary turns to the northwest and runs between Donon and
Mutzigfelsen heading for
2129:
519:, a sandstone plateau ranging from 300 metres (1,000 ft) to 560 metres (1,850 ft) high, between the
1045:
2152:, was extended to the vast woods covering the region. Later, German speakers referred to the same region as
2898:
2124:
193:
2849:, Actes du colloque tenu à Epinal du 4 au 6 septembre 2008, Conseil général des Vosges, 2009, 348 pages.
2757:, guide régionaux, collection dirigée par Charles Pomerol, 2° édition, Masson, Paris, 1984, 184 pages.
2614:
2390:
501:
Vosges or Middle Vosges (50 km, 31 mi), between the Permian Basin of Saint-Die including the
186:
3022:
2724:, Flammarion, 1977, 288 pages (a geogropher's view of this part of France who gives theirs waters to
2636:
2238:
896:
377:
365:
136:
2982:
2112:
2845:
Isabelle Chave (dir.) avec Magali Delavenne, Jean-Claude Fombaron, Philippe Nivet, Yann Prouillet,
361:
348:
2681:
2630:
1012:
635:
and a more gradual descent on the other side. Both the Vosges and the Black Forest were formed by
2453:
2318:
2868:
730:
The highest mountains and peaks of the Vosges (with Alsatian or German names in brackets) are:
2339:, which lie north of the Breusch valley, fall within the Germanic-speaking area because, from
2280:
In pre-Roman times, the Vosges was empty of settlements or was colonized and dominated by the
20:
2356:
2269:
2242:
577:
405:
8:
2410:
960:
471:
247:
24:
2250:
1172:
874:
858:
720:
651:
486:), extending in the southern part of the range from Belfort to the river valley of the
266:
253:
2179:. Concentrations of settlement and immigration took place and not only in areas where
2864:
2850:
2836:
2758:
2743:
2710:
1002:
982:
459:
421:
177:
2471:
808:
2937:
2742:, La bibliothèque du naturaliste, Delachaux et Niestlé, Lausanne, 1998, 352 pages.
2360:
2359:
region and cultural area. The Romance-speaking areas are traditionally part of the
2352:
790:
750:
712:
436:
298:
258:
2812:
2257:
in the north with the lands east of it being incorporated into Germany as part of
2193:
3002:
2884:
2825:
2661:
2476:
2258:
1131:
1083:
1041:
636:
393:
385:
340:
327:
155:
121:
2629:
727:
at 1,008 m (3,307 ft) being the highest point of this Nordic section.
2957:
2952:
2499:
2328:
2137:
1123:
1111:
1094:
1060:
796:
772:
524:
520:
487:
455:
2211:
878:
667:
2996:
2816:, Nancy (Lotharingist wrintings since 1820, nowadays trimestrial périodical,
2676:
2368:
2364:
2301:
2246:
2245:. From 1871 to 1918, they formed the main border line between France and the
824:
588:
389:
215:
202:
2890:
2881:
Illustrated article on the Vosges battlefields of WWI at Battlefields Europe
1079:
2285:
2227:
2207:
1135:
1119:
1087:
844:
784:
734:
708:
696:
640:
623:
565:
515:
The Lower Vosges or Low Vosges (48 km, 30 mi), commonly known as
428:
64:
2457:
868:
413:
2680:
2532:
2223:
2219:
1102:
1029:
778:
744:
604:
432:
2691:. Vol. 28 (11th ed.). Cambridge University Press. p. 214.
2335:). By contrast, those parts of the northern Vosges and the whole of the
1059:
In the late 20th century, a wide area of the massif was included in two
417:
2557:
2344:
2305:
2254:
2176:
2172:
2168:
1122:
coming from south Alsace (or Sundgau), and the Bruche d'Andlau and the
1106:
762:
756:
724:
716:
409:
41:
2340:
944:
612:
553:
509:
506:
498:
447:
431:
is the highest peak at 1,424 m (4,672 ft), followed by the
283:
279:
182:
2833:
Guide des sources de la Grande Guerre dans le département des Vosges
2967:
2942:
2769:
List of majors periodicals concerning Lorraine and South Lorraine:
2289:
2180:
2164:
1139:
834:
814:
802:
675:
608:
502:
401:
2740:
L'Alsace et les Vosges, géologie, milieux naturels, flore et faune
388:
to the north on the German side of the border, they form a single
2947:
2847:
La Grande Guerre dans les Vosges : sources et état des lieux
2103:
1150:
1149:, boulders and polished rocks testify to the former existence of
1146:
1127:
954:
659:
600:
592:
573:
569:
540:
467:
463:
397:
381:
275:
237:
47:
2666:(in French). de l'imprimerie de F.G. Levrault, imprimeur du Roi.
2962:
2447:
2336:
2293:
2203:
2184:
1049:
596:
561:
560:
and the uplift of the bedrock plates of the Vosges, in eastern
557:
549:
475:
451:
373:
271:
170:
71:
2351:). The Germanic areas of the Vosges mountains are part of the
683:
622:
The Vosges are very similar to the corresponding range of the
583:
The Vosges in their southern and central parts are called the
307:
2504:
2355:
region and cultural area and, in the north, also part of the
2281:
2202:
On the lower heights and buttresses of the main chain on the
1158:
1154:
938:
632:
627:
2932:
2725:
2231:
304:
2863:édité par la Société Philomatique Vosgienne, , 68 pages.
2300:) is spoken east of the main ridge: in the valley of the
2416:
The American Heritage Dictionary of the English Language
1048:
on the German side of the border form the cross-border
576:
action was the primary catalyst for development of the
2835:, Conseil général de Vosges, Epinal, 2008, 296 pages.
2733:
Histoire de Lorraine (Meurthe, Meuse, Moselle, Vosges)
2590:"Parc naturel régional des Ballons des Vosges | PnrBV"
2572:
2570:
2568:
2566:
490:. The rounded summits of the Hautes Vosges are called
128:
2308:, the valley of Lièpvrette (nowadays also called the
316:
2241:, on 13 July 1794, the Vosges were the scene of the
301:
2563:
1023:
2500:"Vogesen | Rechtschreibung, Bedeutung, Definition"
2859:"La guerre aérienne dans les Vosges. 1914–1919",
2722:Atlas et géographie de l'Alsace et de la Lorraine
2640:. New York: P. F. Collier & Son Company.
2994:
2120:in the Vosges was built during the 12th century.
1654:
1189:
1167:
1054:Palatinate Forest-North Vosges Biosphere Reserve
512:of Schirmeck-Moyenmoutier and the Col de Saverne
478:is divided south to north into three sections:
2709:, éditions Serpenoise, Metz, 1991, 224 pages.
2312:; "Valley of Silver"), parts of the canton of
2920:
2906:
2789:Bulletin de la Société Philomatique Vosgienne
2218:(Pagan Wall). It was used for defence in the
1138:and their numerous affluents all rise on the
420:line), and forms the western boundary of the
372:) are a range of medium mountains in Eastern
2800:Société d'Histoire et d'Archéologie lorraine
2793:Mémoire des Vosges Histoire Société Coutumes
2594:Parc naturel régional des Ballons des Vosges
1069:Parc naturel régional des Ballons des Vosges
113:
707:rises to 1,424 m (4,672 ft); the
3018:Mountain ranges of Bourgogne-Franche-Comté
2913:
2899:
2550:Germany: A Regional and Economic Geography
2249:. The demarcation line stretched from the
2226:are divided as to whether it was built by
2791:, Saint-Dié, from 1875 to 1999 (nowadays
2409:
719:to 1,350 m (4,429 ft); and the
2811:Société d'Histoire de la Lorraine &
2675:
2627:
2576:
2123:
2111:
2078:Average max. and min. temperatures in °F
1632:Average max. and min. temperatures in °C
1145:In the High Moselle and Meurthe basins,
1093:
1078:
1065:Parc naturel régional des Vosges du Nord
682:
674:
666:
658:
650:
539:
2717:(simple historic approach for children)
2659:
435:(1,366 m, 4,482 ft), and the
2995:
2894:
2381:Northern Vosges Regional Natural Park
877:(highest point in the département of
715:to 1,364 m (4,475 ft); the
711:to 1,366 m (4,482 ft); the
615:remains are found in large beds. The
450:, the Vosges Mountains are wholly in
347:
326:
2552:(2nd ed.). London: Methuen, p. 540.
1098:View from Mont Saint-Odile in Autumn
1038:Northern Vosges Regional Nature Park
2544:
2542:
2540:
548:From a geological point of view, a
13:
2696:
2628:Reynolds, Francis J., ed. (1921).
2522:
2386:Vosges and Jura coal mining basins
1118:The only rivers in Alsace are the
639:in response to the opening of the
482:The Higher Vosges or High Vosges (
408:line) to the Börrstadt Basin (the
14:
3034:
2874:
2108:Battle of Vosges (disambiguation)
2981:
2765:(a precise geologic description)
2750:(global view of nature and land)
2537:
1024:Nature parks and protected areas
591:mountain eroded just before the
494:in French, literally "balloons".
297:
154:
40:
2653:
2644:
2621:
556:period caused the formation of
439:(1,364 m, 4,475 ft).
261:stratigraphic unit: 252–243 mya
2782:Société d'Émulation des Vosges
2755:Guide géologique Vosges-Alsace
2607:
2582:
2492:
2477:Merriam-Webster.com Dictionary
2464:
2431:
2403:
2292:also settled in the east, and
2086:Precipitation totals in inches
1067:(established in 1976) and the
1034:Ballons des Vosges Nature Park
935:) 1,008 m (3,307 ft)
919:) 1,098 m (3,602 ft)
881:) 1,216 m (3,990 ft)
865:) 1,247 m (4,091 ft)
855:) 1,272 m (4,173 ft)
841:) 1,292 m (4,239 ft)
831:) 1,302 m (4,272 ft)
821:) 1,302 m (4,272 ft)
769:) 1,330 m (4,364 ft)
741:) 1,424 m (4,672 ft)
691:The highest points are in the
252:Gneiss, granite and vulcanite
1:
2887: (archived 20 April 2012)
2774:Annales de l'Est (et du Nord)
2660:Golbéry, Philippe de (1823).
2419:(5th ed.). HarperCollins
2396:
1046:Palatinate Forest Nature Park
3013:Mountain ranges of Grand Est
3008:Biosphere reserves of France
2802:, Metz (from 1890, nowadays
2548:Dickinson, Robert E (1964).
1019:) 550 m (1,804 ft)
1009:) 581 m (1,906 ft)
999:) 650 m (2,130 ft)
989:) 764 m (2,507 ft)
967:) 956 m (3,136 ft)
951:) 992 m (3,255 ft)
941:1,008 m (3,307 ft)
925:1,074 m (3,524 ft)
905:1,123 m (3,684 ft)
899:1,148 m (3,766 ft)
893:1,191 m (3,907 ft)
887:1,200 m (3,937 ft)
871:1,229 m (4,032 ft)
811:1,303 m (4,275 ft)
805:1,305 m (4,281 ft)
799:1,306 m (4,285 ft)
793:1,306 m (4,285 ft)
787:1,311 m (4,301 ft)
781:1,314 m (4,311 ft)
775:1,316 m (4,318 ft)
759:1,350 m (4,429 ft)
753:1,363 m (4,472 ft)
747:1,366 m (4,482 ft)
646:
442:
76:1,424 m (4,672 ft)
7:
2374:
2363:region in the west and the
2275:
2130:Château du Grand-Geroldseck
2118:Château du Haut-Kœnigsbourg
1032:lie within the Vosges: the
587:. These consist of a large
160:Map of the Vosges Mountains
10:
3039:
2637:Collier's New Encyclopedia
2391:Flora of the Vosges massif
2101:
2097:
2082:
2074:
1657:
1644:
1640:Precipitation totals in mm
1636:
1628:
1105:, as a consequence of the
1074:
979:837 m (2,746 ft)
973:901 m (2,956 ft)
957:965 m (3,166 ft)
699:, in ancient times called
544:Upper Vosges Mountains map
535:
46:Houses on the slopes near
18:
2979:
2928:
2922:Mountain ranges of France
2861:Mémoire des Vosges H.S.C.
2239:French Revolutionary Wars
897:Planche des Belles Filles
458:separating them from the
265:
246:
236:
231:
192:
176:
166:
152:
147:
106:
101:
93:
85:
80:
70:
60:
55:
39:
34:
2631:"Vosges Mountains"
552:at the beginning of the
89:120 km (75 mi)
16:Mountain range in France
2688:Encyclopædia Britannica
2454:Oxford University Press
1071:(established in 1989).
470:and France, due to the
369:
187:Bourgogne-Franche-Comté
129:
2806:, trimestrial review).
2133:
2121:
1099:
1091:
688:
680:
672:
664:
656:
545:
523:and the source of the
344:
114:
23:of the same name, see
2753:Jean-Paul von Eller,
2450:UK English Dictionary
2127:
2115:
2102:Further information:
1097:
1082:
686:
678:
670:
662:
654:
543:
242:Medium mountain range
2809:Publications of the
2804:Les Cahiers Lorrains
2798:Publications of the
2785:, Epinal, from 1826.
2707:Histoire de Lorraine
2270:Air Inter Flight 148
2243:Battle of Trippstadt
2232:before their arrival
2136:The massif known in
1645:Source: Meteociel.fr
1044:Nature Park and the
701:Ballon de Guebwiller
384:. Together with the
21:department of France
2333:Vallée de la Bruche
2327:) and parts of the
2268:On 20 January 1992
2183:were found. In the
1658:Imperial conversion
965:Hartmannsweilerkopf
961:Hartmannswillerkopf
564:, and those in the
472:Franco-Prussian War
349:[voˈɡeːzn̩]
256:: about 419–252 mya
254:stratigraphic units
212: /
25:Vosges (department)
2738:Yves Sell (dir.),
2720:Etienne Julliard,
2531:maps available on
2134:
2122:
1100:
1092:
1007:Großer Wintersberg
875:Ballon de Servance
705:Ballon de Murbach,
689:
681:
673:
665:
657:
546:
56:Highest point
2990:
2989:
2855:978-2-86088-067-1
2841:978-2-86088-062-6
2480:. Merriam-Webster
2353:Alemannic dialect
2094:
2093:
2090:
2089:
1649:
1648:
1003:Grand Wintersberg
983:Mont Sainte-Odile
460:Palatinate Forest
422:Upper Rhine Plain
289:
288:
194:Range coordinates
3030:
3023:Horsts (geology)
2985:
2938:Armorican Massif
2915:
2908:
2901:
2892:
2891:
2731:Robert Parisot,
2692:
2684:
2668:
2667:
2657:
2651:
2648:
2642:
2641:
2633:
2625:
2619:
2618:
2615:"気象庁｜過去の気象データ検索"
2611:
2605:
2604:
2602:
2600:
2586:
2580:
2574:
2561:
2546:
2535:
2526:
2520:
2518:
2516:
2514:
2496:
2490:
2489:
2487:
2485:
2468:
2462:
2461:
2460:on 5 March 2020.
2456:. Archived from
2435:
2429:
2428:
2426:
2424:
2407:
2361:Lorrain language
2357:Frankish dialect
2322:
2253:in the south to
2197:
2085:
2077:
2068:
2063:
2052:
2037:
2032:
2021:
2006:
2001:
1990:
1975:
1970:
1959:
1944:
1939:
1928:
1913:
1908:
1897:
1882:
1877:
1866:
1851:
1846:
1835:
1820:
1815:
1804:
1789:
1784:
1773:
1758:
1753:
1742:
1727:
1722:
1711:
1655:
1639:
1631:
1622:
1617:
1606:
1591:
1586:
1575:
1560:
1555:
1544:
1529:
1524:
1513:
1498:
1493:
1482:
1467:
1462:
1451:
1436:
1431:
1420:
1405:
1400:
1389:
1374:
1369:
1358:
1343:
1338:
1327:
1312:
1307:
1296:
1281:
1276:
1265:
1190:
1168:
1103:Meteorologically
929:Rocher de Mutzig
863:Elsässer Belchen
791:Haut de Falimont
637:isostatic uplift
611:and Permian red
580:massif feature.
474:. The elongated
454:, far above the
390:geomorphological
366:Alemannic German
359:
358:
357:
351:
338:
337:
336:
330:
325:
319:
314:
313:
310:
309:
306:
303:
259:Bunter sandstone
227:
226:
224:
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2818:Le Pays Lorrain
2701:General texts:
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1173:Ballon d'Alsace
1164:
1084:Schiessrothried
1077:
1061:protected areas
1042:Northern Vosges
1026:
859:Ballon d'Alsace
853:Kleiner Belchen
721:Ballon d'Alsace
649:
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510:volcanic massif
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394:Burgundian Gate
386:Palatine Forest
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2679:, ed. (1911).
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521:Col de Saverne
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456:Col de Saverne
448:Geographically
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2813:Musée Lorrain
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2748:2-603-01100-6
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2716:
2715:2-87692-088-3
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2577:Chisholm 1911
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2569:
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2559:
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2545:
2543:
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2519:or Wasgenwald
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2369:lingua franca
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2365:Frainc-Comtou
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2329:Bruche valley
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2247:German Empire
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1116:
1113:
1108:
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1096:
1090:in the Vosges
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826:
825:Soultzereneck
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693:Hautes Vosges
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642:
638:
634:
629:
625:
620:
618:
614:
610:
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589:Carboniferous
586:
585:Hautes Vosges
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542:
533:
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484:Hautes Vosges
481:
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328:[voʒ]
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2635:
2623:
2609:
2597:. Retrieved
2593:
2584:
2549:
2524:
2511:. Retrieved
2503:
2494:
2482:. Retrieved
2475:
2466:
2458:the original
2446:
2433:
2421:. Retrieved
2414:
2405:
2348:
2332:
2324:
2314:Villé valley
2310:Val d'Argent
2309:
2298:Altromanisch
2297:
2284:. After the
2279:
2267:
2263:
2236:
2215:
2208:Sainte Odile
2201:
2187:area of the
2162:
2157:
2153:
2150:Vogesus mons
2149:
2148:, sometimes
2146:Vosego silva
2145:
2142:Vosago mons
2141:
2135:
1171:
1163:
1144:
1117:
1107:Foehn effect
1101:
1088:glacial lake
1058:
1052:-designated
1030:nature parks
1027:
1016:
1006:
996:
986:
964:
948:
933:Mutzigfelsen
932:
916:
912:
909:Champ du Feu
862:
852:
849:Kahler Wasen
848:
845:Petit Ballon
838:
828:
818:
785:Batteriekopf
766:
738:
735:Grand Ballon
729:
709:Storckenkopf
704:
700:
697:Grand Ballon
692:
690:
655:Grand Ballon
641:Rhine Graben
624:Black Forest
621:
617:grès vosgien
616:
595:Period with
584:
582:
566:Black Forest
547:
530:
517:North Vosges
491:
483:
446:
429:Grand Ballon
426:
292:
290:
267:Type of rock
65:Grand Ballon
29:
2513:17 February
2509:(in German)
2484:17 February
2423:17 February
2317: [
2237:During the
2220:Middle Ages
2212:Ribeauvillé
2192: [
2177:water power
2173:water mills
1182:explanation
987:Odilienberg
879:Haute-Saône
829:Sulzereneck
779:Lauchenkopf
745:Storkenkopf
663:Storkenkopf
626:across the
605:porphyritic
433:Storkenkopf
376:, near its
248:Age of rock
219: /
107:Native name
2997:Categories
2558:B000IOFSEQ
2533:Géoportail
2397:References
2345:Sarrebourg
2306:Lapoutroie
2255:Mont Donon
2228:the Romans
2189:Lièpvrette
2171:) and the
2169:glassworks
2167:works and
2158:Wasgenwald
1013:Hohenbourg
971:Ungersberg
923:Baerenkopf
903:Molkenrain
763:Klintzkopf
757:Kastelberg
725:Mont Donon
717:Kastelberg
679:Kastelberg
410:Winnweiler
362:Franconian
81:Dimensions
2869:1626-5238
2440:(US) and
2341:Schirmeck
2216:Mur Païen
1017:Hohenburg
945:Taennchel
917:Firstfeld
869:Brézouard
767:Klinzkopf
647:Mountains
613:sandstone
554:Paleogene
507:Dinantian
499:sandstone
443:Geography
414:Börrstadt
284:sandstone
280:vulcanite
183:Grand Est
148:Geography
72:Elevation
50:in France
2968:Pyrenees
2943:Ardennes
2776:, Nancy.
2599:10 March
2472:"Vosges"
2443:"Vosges"
2438:"Vosges"
2411:"Vosges"
2375:See also
2349:Saarburg
2290:Alemanni
2276:Language
2204:Alsatian
2181:minerals
2165:charcoal
1151:glaciers
1147:moraines
1140:Lorraine
1036:and the
997:Dagsburg
949:Tännchel
913:Hochfeld
891:Rossberg
835:Le Tanet
819:Ringbühl
815:Ringbuhl
803:Rainkopf
687:Le Tanet
609:Triassic
601:granites
578:highland
503:Devonian
418:Göllheim
402:Ronchamp
216:48°N 7°E
19:For the
2948:Corsica
2883:at the
2824:On the
2304:around
2154:Vogesen
2104:Vosagus
2098:History
1155:beeches
1132:Meurthe
1128:Moselle
1110:of the
1075:Climate
955:Climont
885:Drumont
839:Tanneck
751:Hohneck
713:Hohneck
671:Hohneck
593:Permian
574:glacial
570:Germany
536:Geology
492:ballons
468:Germany
464:Germany
437:Hohneck
398:Belfort
382:Germany
345:Vogesen
324:French:
276:granite
238:Orogeny
232:Geology
167:Country
115:Vogesen
48:Bussang
3003:Vosges
2973:Vosges
2963:Morvan
2867:
2853:
2839:
2761:
2746:
2713:
2556:
2507:online
2448:Lexico
2337:Wasgau
2294:Franks
2210:above
2185:mining
2058:
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2016:
2013:
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1159:maples
1142:side.
1124:Bruche
1063:, the
1050:UNESCO
1040:. The
695:: the
597:gneiss
562:France
558:Alsace
550:graben
525:Lauter
488:Bruche
476:massif
452:France
378:border
374:France
370:Vogese
341:German
293:Vosges
272:Gneiss
178:Region
171:France
133:
130:Vogese
122:German
118:
102:Naming
86:Length
35:Vosges
2505:Duden
2321:]
2302:Weiss
2288:era,
2286:Roman
2282:Celts
2230:, or
2196:]
2175:used
2138:Latin
1136:Sarre
939:Donon
633:Rhine
628:Rhine
568:, in
396:(the
380:with
318:VOHZH
221:48; 7
2933:Alps
2865:ISSN
2851:ISBN
2837:ISBN
2759:ISBN
2744:ISBN
2726:Rhin
2711:ISBN
2601:2024
2554:ASIN
2515:2019
2486:2019
2425:2019
2222:and
2128:The
2116:The
2106:and
1157:and
1134:and
1086:, a
1028:Two
993:Dabo
497:The
427:The
406:Lure
364:and
291:The
204:48°N
94:Area
61:Peak
2529:IGN
2156:or
2144:or
2140:as
2020:8.5
1989:8.3
1958:6.1
1927:6.2
1896:5.9
1865:5.3
1803:4.9
1772:7.7
1710:9.9
1605:289
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207:7°E
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