2141:
2129:
668:
167:
53:
1111:
2999:
684:
1096:
2281:
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.
692:
676:
557:
700:
659:, 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.
1125:
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
1130:
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
2280:
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
646:
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
635:(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.
2214:
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.
1131:
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.
482:. 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
2751:, 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)
547:
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.
588:. 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:
2222:
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
2230:(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
371:
2383:
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
2179:
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
739:
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
2431:
352:
2312:
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 (
3033:
1197:
1069:
2679:
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
1084:
2928:
1177:, 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.
2703:
2387:
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.
3028:
3023:
2870:
2856:
2569:
2396:
1080:
1053:
532:
1142:
which have as tributaries other, shorter but sometimes powerful streams coming like the last two from the Vosges
Mountains. The rivers
2937:
2401:
408:
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
2921:
2778:
2763:
2730:
2453:
2140:
2123:
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
2544:
2133:
211:
1169:
which once covered the top of the Vosges. The mountain lakes caused by the original glacial phenomena are surrounded by pines,
2797:
1049:
2896:
2145:
2128:
1061:
2914:
204:
2666:
Brown, James Daniel, Facing the
Mountain, a True Story of Japanese American Heroes in WWII (Viking, 2021), Chapter 18.
2605:
2458:
2998:
2406:
197:
623:
masses or other volcanic intrusions. The north, south and west parts are less eroded by glaciers, and here Vosges
393:
3038:
2652:
2288:
crashed into the Vosges
Mountains while circling to land at Strasbourg International Airport, killing 87 people.
2254:
912:
381:
147:
377:
364:
2359:
the historical linguistic boundary turns to the northwest and runs between Donon and
Mutzigfelsen heading for
1028:
535:, a sandstone plateau ranging from 300 metres (1,000 ft) to 560 metres (1,850 ft) high, between the
2469:
2168:, was extended to the vast woods covering the region. Later, German speakers referred to the same region as
667:
2865:, Actes du colloque tenu à Epinal du 4 au 6 septembre 2008, Conseil général des Vosges, 2009, 348 pages.
906:
31:
2773:, guide régionaux, collection dirigée par Charles Pomerol, 2° édition, Masson, Paris, 1984, 184 pages.
2630:
517:
Vosges or Middle Vosges (50 km, 31 mi), between the Permian Basin of Saint-Die including the
944:
900:
2740:, Flammarion, 1977, 288 pages (a geogropher's view of this part of France who gives theirs waters to
2372:
2329:
2285:
2258:
593:
421:
992:
2861:
Isabelle Chave (dir.) avec Magali Delavenne, Jean-Claude Fombaron, Philippe Nivet, Yann Prouillet,
1008:
976:
487:
258:
35:
2697:
2646:
924:
651:
and a more gradual descent on the other side. Both the Vosges and the Black Forest were formed by
166:
2334:
890:
277:
264:
2884:
2266:
2204:
1188:
986:
938:
918:
874:
736:
1110:
746:
The highest mountains and peaks of the Vosges (with Alsatian or German names in brackets) are:
2880:
2866:
2852:
2774:
2759:
2726:
2355:, which lie north of the Breusch valley, fall within the Germanic-speaking area because, from
2296:
In pre-Roman times, the Vosges was empty of settlements or was colonized and dominated by the
1018:
998:
824:
683:
475:
437:
188:
2953:
2828:
2376:
2368:
806:
766:
728:
452:
309:
269:
1095:
3018:
2900:
2841:
2492:
2274:
1147:
1099:
1057:
652:
409:
401:
356:
338:
132:
2426:
2973:
2968:
2344:
2227:
2153:
1139:
1127:
1076:
894:
812:
788:
540:
536:
503:
502:), extending in the southern part of the range from Belfort to the river valley of the
471:
2195:. Concentrations of settlement and immigration took place and not only in areas where
3012:
2692:
2384:
2380:
2317:
2262:
840:
604:
405:
2487:
2758:, La bibliothèque du naturaliste, Delachaux et Niestlé, Lausanne, 1998, 352 pages.
2375:
region and cultural area. The Romance-speaking areas are traditionally part of the
2301:
2243:
2223:
1151:
1135:
1103:
860:
800:
750:
724:
712:
656:
639:
581:
444:
75:
52:
2273:
in the north with the lands east of it being incorporated into Germany as part of
2209:
884:
429:
2677:
2645:
2239:
2235:
1118:
1045:
794:
760:
743:
at 1,008 m (3,307 ft) being the highest point of this Nordic section.
620:
448:
433:
2515:
691:
2360:
2321:
2270:
2192:
2188:
2184:
1122:
778:
772:
740:
732:
425:
2832:, Nancy (Lotharingist wrintings since 1820, nowadays trimestrial périodical,
2261:. From 1871 to 1918, they formed the main border line between France and the
226:
213:
2906:
2897:
Illustrated article on the Vosges battlefields of WWI at Battlefields Europe
2356:
960:
675:
628:
569:
556:
525:
522:
514:
463:
294:
290:
193:
531:
The Lower Vosges or Low Vosges (48 km, 30 mi), commonly known as
2473:
1670:
2983:
2958:
2696:
2548:
2305:
2196:
2180:
1155:
850:
830:
818:
624:
518:
417:
2707:. Vol. 28 (11th ed.). Cambridge University Press. p. 214.
2351:). By contrast, those parts of the northern Vosges and the whole of the
1075:
In the late 20th century, a wide area of the massif was included in two
699:
2963:
2573:
2119:
1166:
1162:
1143:
1138:
coming from south Alsace (or Sundgau), and the Bruche d'Andlau and the
970:
616:
608:
589:
585:
483:
479:
413:
397:
286:
248:
58:
17:
1205:
1183:
2978:
2463:
2352:
2309:
2219:
2200:
1065:
612:
577:
573:
565:
491:
467:
447:
is the highest peak at 1,424 m (4,672 ft), followed by the
389:
282:
181:
82:
2849:
Guide des sources de la Grande Guerre dans le département des Vosges
2785:
List of majors periodicals concerning Lorraine and South Lorraine:
2756:
L'Alsace et les Vosges, géologie, milieux naturels, flore et faune
2520:
2297:
2139:
2127:
1174:
1170:
1109:
1094:
954:
698:
690:
682:
674:
666:
648:
643:
555:
404:
to the north on the German side of the border, they form a single
2863:
La Grande Guerre dans les Vosges : sources et état des lieux
1165:, boulders and polished rocks testify to the former existence of
2948:
2741:
2682:(in French). de l'imprimerie de F.G. Levrault, imprimeur du Roi.
2247:
2910:
576:
and the uplift of the bedrock plates of the Vosges, in eastern
2367:). The Germanic areas of the Vosges mountains are part of the
638:
The Vosges are very similar to the corresponding range of the
599:
The Vosges in their southern and central parts are called the
318:
2371:
region and cultural area and, in the north, also part of the
2218:
On the lower heights and buttresses of the main chain on the
315:
2879:édité par la Société Philomatique Vosgienne, , 68 pages.
2316:) is spoken east of the main ridge: in the valley of the
2432:
The American Heritage Dictionary of the English Language
1064:
on the German side of the border form the cross-border
592:
action was the primary catalyst for development of the
2851:, Conseil général de Vosges, Epinal, 2008, 296 pages.
2749:
Histoire de Lorraine (Meurthe, Meuse, Moselle, Vosges)
2606:"Parc naturel régional des Ballons des Vosges | PnrBV"
2588:
2586:
2584:
2582:
506:. The rounded summits of the Hautes Vosges are called
139:
2324:, the valley of Lièpvrette (nowadays also called the
327:
2257:, 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:
2516:"Vogesen | Rechtschreibung, Bedeutung, Definition"
2875:"La guerre aérienne dans les Vosges. 1914–1919",
2738:Atlas et géographie de l'Alsace et de la Lorraine
2656:. New York: P. F. Collier & Son Company.
2136:in the Vosges was built during the 12th century.
1070:Palatinate Forest-North Vosges Biosphere Reserve
528:of Schirmeck-Moyenmoutier and the Col de Saverne
494:is divided south to north into three sections:
2725:, éditions Serpenoise, Metz, 1991, 224 pages.
2328:; "Valley of Silver"), parts of the canton of
2922:
2805:Bulletin de la Société Philomatique Vosgienne
2234:(Pagan Wall). It was used for defence in the
1154:and their numerous affluents all rise on the
436:line), and forms the western boundary of the
388:) are a range of medium mountains in Eastern
8:
2816:Société d'Histoire et d'Archéologie lorraine
2809:Mémoire des Vosges Histoire Société Coutumes
2610:Parc naturel régional des Ballons des Vosges
1085:Parc naturel régional des Ballons des Vosges
124:
723:rises to 1,424 m (4,672 ft); the
3034:Mountain ranges of Bourgogne-Franche-Comté
2929:
2915:
2907:
2566:Germany: A Regional and Economic Geography
2265:. The demarcation line stretched from the
2242:are divided as to whether it was built by
42:
2807:, Saint-Dié, from 1875 to 1999 (nowadays
735:to 1,350 m (4,429 ft); and the
2827:Société d'Histoire de la Lorraine &
2592:
2094:Average max. and min. temperatures in °F
1648:Average max. and min. temperatures in °C
1161:In the High Moselle and Meurthe basins,
1081:Parc naturel régional des Vosges du Nord
2733:(simple historic approach for children)
2418:
451:(1,366 m, 4,482 ft), and the
2397:Northern Vosges Regional Natural Park
893:(highest point in the département of
731:to 1,364 m (4,475 ft); the
727:to 1,366 m (4,482 ft); the
631:remains are found in large beds. The
466:, the Vosges Mountains are wholly in
363:
337:
7:
2568:(2nd ed.). London: Methuen, p. 540.
1114:View from Mont Saint-Odile in Autumn
1054:Northern Vosges Regional Nature Park
2560:
2558:
2556:
564:From a geological point of view, a
2644:Reynolds, Francis J., ed. (1921).
2402:Vosges and Jura coal mining basins
1134:The only rivers in Alsace are the
655:in response to the opening of the
498:The Higher Vosges or High Vosges (
424:line) to the Börrstadt Basin (the
25:
2124:Battle of Vosges (disambiguation)
2997:
2781:(a precise geologic description)
2766:(global view of nature and land)
1040:Nature parks and protected areas
607:mountain eroded just before the
510:in French, literally "balloons".
308:
165:
51:
572:period caused the formation of
455:(1,364 m, 4,475 ft).
272:stratigraphic unit: 252–243 mya
2798:Société d'Émulation des Vosges
2771:Guide géologique Vosges-Alsace
2493:Merriam-Webster.com Dictionary
2308:also settled in the east, and
2102:Precipitation totals in inches
1083:(established in 1976) and the
1050:Ballons des Vosges Nature Park
951:) 1,008 m (3,307 ft)
935:) 1,098 m (3,602 ft)
897:) 1,216 m (3,990 ft)
881:) 1,247 m (4,091 ft)
871:) 1,272 m (4,173 ft)
857:) 1,292 m (4,239 ft)
847:) 1,302 m (4,272 ft)
837:) 1,302 m (4,272 ft)
785:) 1,330 m (4,364 ft)
757:) 1,424 m (4,672 ft)
707:The highest points are in the
263:Gneiss, granite and vulcanite
1:
2903: (archived 20 April 2012)
2790:Annales de l'Est (et du Nord)
2676:Golbéry, Philippe de (1823).
2435:(5th ed.). HarperCollins
1062:Palatinate Forest Nature Park
3029:Mountain ranges of Grand Est
3024:Biosphere reserves of France
2818:, Metz (from 1890, nowadays
2564:Dickinson, Robert E (1964).
1035:) 550 m (1,804 ft)
1025:) 581 m (1,906 ft)
1015:) 650 m (2,130 ft)
1005:) 764 m (2,507 ft)
983:) 956 m (3,136 ft)
967:) 992 m (3,255 ft)
957:1,008 m (3,307 ft)
941:1,074 m (3,524 ft)
921:1,123 m (3,684 ft)
915:1,148 m (3,766 ft)
909:1,191 m (3,907 ft)
903:1,200 m (3,937 ft)
887:1,229 m (4,032 ft)
827:1,303 m (4,275 ft)
821:1,305 m (4,281 ft)
815:1,306 m (4,285 ft)
809:1,306 m (4,285 ft)
803:1,311 m (4,301 ft)
797:1,314 m (4,311 ft)
791:1,316 m (4,318 ft)
775:1,350 m (4,429 ft)
769:1,363 m (4,472 ft)
763:1,366 m (4,482 ft)
87:1,424 m (4,672 ft)
2379:region in the west and the
2146:Château du Grand-Geroldseck
2134:Château du Haut-Kœnigsbourg
1048:lie within the Vosges: the
603:. These consist of a large
171:Map of the Vosges Mountains
3055:
2653:Collier's New Encyclopedia
2407:Flora of the Vosges massif
2117:
2098:
2090:
1673:
1660:
1656:Precipitation totals in mm
1652:
1644:
1121:, as a consequence of the
995:837 m (2,746 ft)
989:901 m (2,956 ft)
973:965 m (3,166 ft)
715:, in ancient times called
560:Upper Vosges Mountains map
57:Houses on the slopes near
29:
2995:
2944:
2938:Mountain ranges of France
2877:Mémoire des Vosges H.S.C.
2255:French Revolutionary Wars
913:Planche des Belles Filles
474:separating them from the
163:
50:
2647:"Vosges Mountains"
568:at the beginning of the
100:120 km (75 mi)
27:Mountain range in France
2704:Encyclopædia Britannica
2470:Oxford University Press
1087:(established in 1989).
486:and France, due to the
385:
198:Bourgogne-Franche-Comté
140:
2822:, trimestrial review).
2149:
2137:
1115:
1107:
704:
696:
688:
680:
672:
561:
539:and the source of the
360:
125:
34:of the same name, see
2769:Jean-Paul von Eller,
2466:UK English Dictionary
2143:
2131:
2118:Further information:
1113:
1098:
702:
694:
686:
678:
670:
559:
253:Medium mountain range
2825:Publications of the
2820:Les Cahiers Lorrains
2814:Publications of the
2801:, Epinal, from 1826.
2723:Histoire de Lorraine
2286:Air Inter Flight 148
2259:Battle of Trippstadt
2248:before their arrival
2152:The massif known in
1661:Source: Meteociel.fr
1060:Nature Park and the
717:Ballon de Guebwiller
400:. Together with the
32:department of France
2349:Vallée de la Bruche
2343:) and parts of the
2284:On 20 January 1992
2199:were found. In the
1674:Imperial conversion
981:Hartmannsweilerkopf
977:Hartmannswillerkopf
580:, and those in the
488:Franco-Prussian War
365:[voˈɡeːzn̩]
267:: about 419–252 mya
265:stratigraphic units
223: /
36:Vosges (department)
2754:Yves Sell (dir.),
2736:Etienne Julliard,
2547:maps available on
2150:
2138:
1116:
1108:
1023:Großer Wintersberg
891:Ballon de Servance
721:Ballon de Murbach,
705:
697:
689:
681:
673:
562:
67:Highest point
3006:
3005:
2871:978-2-86088-067-1
2857:978-2-86088-062-6
2496:. Merriam-Webster
2369:Alemannic dialect
2110:
2109:
2106:
2105:
1665:
1664:
1019:Grand Wintersberg
999:Mont Sainte-Odile
476:Palatinate Forest
438:Upper Rhine Plain
300:
299:
205:Range coordinates
16:(Redirected from
3046:
3039:Horsts (geology)
3001:
2954:Armorican Massif
2931:
2924:
2917:
2908:
2747:Robert Parisot,
2708:
2700:
2684:
2683:
2673:
2667:
2664:
2658:
2657:
2649:
2641:
2635:
2634:
2631:"気象庁｜過去の気象データ検索"
2627:
2621:
2620:
2618:
2616:
2602:
2596:
2590:
2577:
2562:
2551:
2542:
2536:
2534:
2532:
2530:
2512:
2506:
2505:
2503:
2501:
2484:
2478:
2477:
2476:on 5 March 2020.
2472:. Archived from
2451:
2445:
2444:
2442:
2440:
2423:
2377:Lorrain language
2373:Frankish dialect
2338:
2269:in the south to
2213:
2101:
2093:
2084:
2079:
2068:
2053:
2048:
2037:
2022:
2017:
2006:
1991:
1986:
1975:
1960:
1955:
1944:
1929:
1924:
1913:
1898:
1893:
1882:
1867:
1862:
1851:
1836:
1831:
1820:
1805:
1800:
1789:
1774:
1769:
1758:
1743:
1738:
1727:
1671:
1655:
1647:
1638:
1633:
1622:
1607:
1602:
1591:
1576:
1571:
1560:
1545:
1540:
1529:
1514:
1509:
1498:
1483:
1478:
1467:
1452:
1447:
1436:
1421:
1416:
1405:
1390:
1385:
1374:
1359:
1354:
1343:
1328:
1323:
1312:
1297:
1292:
1281:
1206:
1184:
1119:Meteorologically
945:Rocher de Mutzig
879:Elsässer Belchen
807:Haut de Falimont
653:isostatic uplift
627:and Permian red
596:massif feature.
490:. The elongated
470:, far above the
406:geomorphological
382:Alemannic German
375:
374:
373:
367:
355:
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:
3054:
3053:
3049:
3048:
3047:
3045:
3044:
3043:
3009:
3008:
3007:
3002:
2993:
2940:
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1100:Schiessrothried
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1077:protected areas
1058:Northern Vosges
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2698:"Vosges"
2695:, ed. (1911).
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2613:. Retrieved
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2527:. Retrieved
2519:
2510:
2498:. Retrieved
2491:
2482:
2474:the original
2462:
2449:
2437:. Retrieved
2430:
2421:
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2330:Villé valley
2326:Val d'Argent
2325:
2314:Altromanisch
2313:
2300:. After the
2295:
2283:
2279:
2252:
2231:
2224:Sainte Odile
2217:
2203:area of the
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2169:
2166:Vogesus mons
2165:
2164:, sometimes
2162:Vosego silva
2161:
2158:Vosago mons
2157:
2151:
1187:
1179:
1160:
1133:
1123:Foehn effect
1117:
1104:glacial lake
1074:
1068:-designated
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925:Champ du Feu
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865:Kahler Wasen
864:
861:Petit Ballon
854:
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801:Batteriekopf
782:
754:
751:Grand Ballon
745:
725:Storckenkopf
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716:
713:Grand Ballon
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671:Grand Ballon
657:Rhine Graben
640:Black Forest
637:
633:grès vosgien
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611:Period with
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582:Black Forest
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533:North Vosges
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445:Grand Ballon
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278:Type of rock
76:Grand Ballon
40:
2529:17 February
2525:(in German)
2500:17 February
2439:17 February
2333: [
2253:During the
2236:Middle Ages
2228:Ribeauvillé
2208: [
2193:water power
2189:water mills
1198:explanation
1003:Odilienberg
895:Haute-Saône
845:Sulzereneck
795:Lauchenkopf
761:Storkenkopf
679:Storkenkopf
642:across the
621:porphyritic
449:Storkenkopf
392:, near its
259:Age of rock
230: /
118:Native name
3013:Categories
2574:B000IOFSEQ
2549:Géoportail
2413:References
2361:Sarrebourg
2322:Lapoutroie
2271:Mont Donon
2244:the Romans
2205:Lièpvrette
2187:) and the
2185:glassworks
2183:works and
2174:Wasgenwald
1029:Hohenbourg
987:Ungersberg
939:Baerenkopf
919:Molkenrain
779:Klintzkopf
773:Kastelberg
741:Mont Donon
733:Kastelberg
695:Kastelberg
426:Winnweiler
378:Franconian
92:Dimensions
2885:1626-5238
2456:(US) and
2357:Schirmeck
2232:Mur Païen
1033:Hohenburg
961:Taennchel
933:Firstfeld
885:Brézouard
783:Klinzkopf
663:Mountains
629:sandstone
570:Paleogene
523:Dinantian
515:sandstone
459:Geography
430:Börrstadt
353:‹See Tfd›
295:sandstone
291:vulcanite
194:Grand Est
159:Geography
83:Elevation
61:in France
2984:Pyrenees
2959:Ardennes
2792:, Nancy.
2615:10 March
2488:"Vosges"
2459:"Vosges"
2454:"Vosges"
2427:"Vosges"
2391:See also
2365:Saarburg
2306:Alemanni
2292:Language
2220:Alsatian
2197:minerals
2181:charcoal
1167:glaciers
1163:moraines
1156:Lorraine
1052:and the
1013:Dagsburg
965:Tännchel
929:Hochfeld
907:Rossberg
851:Le Tanet
835:Ringbühl
831:Ringbuhl
819:Rainkopf
703:Le Tanet
625:Triassic
617:granites
594:highland
519:Devonian
434:Göllheim
418:Ronchamp
227:48°N 7°E
30:For the
2964:Corsica
2899:at the
2840:On the
2320:around
2170:Vogesen
2120:Vosagus
2114:History
1171:beeches
1148:Meurthe
1144:Moselle
1126:of the
1091:Climate
971:Climont
901:Drumont
855:Tanneck
767:Hohneck
729:Hohneck
687:Hohneck
609:Permian
590:glacial
586:Germany
552:Geology
508:ballons
484:Germany
480:Germany
453:Hohneck
414:Belfort
398:Germany
361:Vogesen
335:French:
287:granite
249:Orogeny
243:Geology
178:Country
126:Vogesen
59:Bussang
18:Vogesen
3019:Vosges
2989:Vosges
2979:Morvan
2883:
2869:
2855:
2777:
2762:
2729:
2572:
2523:online
2464:Lexico
2353:Wasgau
2310:Franks
2226:above
2201:mining
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1175:maples
1158:side.
1140:Bruche
1079:, the
1066:UNESCO
1056:. The
711:: the
613:gneiss
578:France
574:Alsace
566:graben
541:Lauter
504:Bruche
492:massif
468:France
394:border
390:France
386:Vogese
357:German
304:Vosges
283:Gneiss
189:Region
182:France
144:
141:Vogese
133:German
129:
113:Naming
97:Length
46:Vosges
2521:Duden
2337:]
2318:Weiss
2304:era,
2302:Roman
2298:Celts
2246:, or
2212:]
2191:used
2154:Latin
1152:Sarre
955:Donon
649:Rhine
644:Rhine
584:, in
412:(the
396:with
329:VOHZH
232:48; 7
2949:Alps
2881:ISSN
2867:ISBN
2853:ISBN
2775:ISBN
2760:ISBN
2742:Rhin
2727:ISBN
2617:2024
2570:ASIN
2531:2019
2502:2019
2441:2019
2238:and
2144:The
2132:The
2122:and
1173:and
1150:and
1102:, a
1044:Two
1009:Dabo
513:The
443:The
422:Lure
380:and
302:The
215:48°N
105:Area
72:Peak
2545:IGN
2172:or
2160:or
2156:as
2036:8.5
2005:8.3
1974:6.1
1943:6.2
1912:5.9
1881:5.3
1819:4.9
1788:7.7
1726:9.9
1621:289
1590:215
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1528:154
1497:157
1466:149
1435:135
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478:in
218:7°E
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1539:14
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1358:−1
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350:;
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316:oʊ
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