2127:
1466:
1050:
982:
994:
958:
1038:
2031:
910:
26:
934:
1155:
898:
613:
1763:
946:
605:
1022:
2279:
2005:
1478:
1682:
429:
77:
1526:
1981:
2225:
504:
2043:
1502:
970:
1257:
2019:
1514:
922:
1490:
1993:
1006:
1163:
1075:
488:
664:). In his typology of mountain and rock formations of the Wasgau, Geiger distinguishes the following six forms: hill blocks with rock outcrops, table hills; rock slabs; ridges with rock faces, hill cones with rock blocks; hill cones with rock towers and domed hills. In addition there is a host of hilltop observation towers (e.g. on the Grand Wintersberg, Rehberg,
1320:) the various rock formations are less strongly arched and therefore their surface layers were not as severely eroded. For this reason, younger rocks of the Middle and Upper Bunter form the surface of the hills, whilst Rehberg and Trifels beds only occur in deep V-shaped valleys. Also, south of a line from
1311:
or
Saarbach do they dive permanently beneath the younger strata of the Middle Bunter Sandstein, for example, the Karlstal beds, so that the landscape of the western Wasgau appears similar to that of the Middle Palatinate Forest. This also applies to the southern part of Wasgau because, in the area of
1869:
have settled on a host of rocks, so that restrictions have had to be introduced for climbers, walkers and special users. In order to avoid conflicts of usage these regulations (out-of-bounds areas and the guarding of breeding rocks) are laid down annually by the
Palatine Climbing Association and the
2151:
is 229 persons per km. Similarly, the number of settlements is lower in the natural region; the German part of the Wasgau has only about 50 and the French part, about 40, i.e. a total of about 90 communities. These relatively small settlements only occupy 5% of the total area, and are surrounded by
1816:
Many castles in the Wasgau were built on rock terraces or blocks of rock; especially prominent examples are the "castle trinity" of
Trifels, Anebos and Scharfenberg near Annweiler and Lindelbrunn Castle, a few kilometres to the southwest. Well known rock castles also include the Berwartstein near
2134:
About 237,000 inhabitants live in the
Palatine Forest-North Vosges Biosphere Reserve, spread over 215 municipalities. With a total area of 3,105 km this gives a population density of slightly more than 76 inhabitants per km. On the German side, the density is higher, with an average of 89
2160:
in the
Palatinate and in Lorraine, and, in the southwest, the tourist destination of La Petite-Pierre; the latter settlements being in the high, plateau-like, transition region between the red sandstone landscape of the Wasgau and the limestone formations of the Westrich Plateau.
394:
towards the south and, near
Phalsbourg, finally reaches the fault zone of the narrow Col de Saverne; this separates the Wasgau from the "real" (North) Vosges immediately to the south, although this transition is rather gradual and the dividing line not particularly clear.
1271:
Had the rock strata been undisturbed, the typical landscape structure of the rock country would end shortly after
Annweiler due to their inclination. Tectonic processes, however, led to the shifting and displacement of individual layers of rock so that, west of the
2112:
in
Graufthal; in three houses that are built into the rock face, up to 37 people have lived over the centuries. After the death of their last inhabitant in 1958 the rock dwellings were preserved as a cultural monument and may be viewed today as an open-air museum.
1182:, for example, the Annweiler and Speyerbach beds, consist more of fine-grained sandstones with clayey binding and shales and therefore have a softer consistency, this material could be more easily carried awayl leaving the older rocks of the Zechstein and
1332:, the main distribution zone of Bunter sandstone from the eastern edge of the trough to the rocks of the Lower Muschelkalk in the west narrows from a width of about 15 km to a minimum of 7 km in the area of the Col de Saverne (see map above).
1137:
induced displacements that have had a significance impact on the appearance of the landscape of the Wasgau today. At that time the edges of the Rhine Graben were uplifted and the layers of bunter sandstone and, in places also older rocks (Zechstein,
1689:
The Wasgau
Felsenland ("rock country") is rich in bizarre sandstone rock formations, which have been formed over the millennia by the weathering and erosion of strata of differing hardness belonging to the Lower and Middle Bunter (see
1173:
Due to the synclinal-anticlinal structure of the hills on the left bank of the Rhine which runs from southwest to northeast, these bulges in the northern and central parts of the Wasgau, i.e. in the region of the South
Palatine Saddle
1422:), however, there is now a tendency to go the opposite way: both parts of the range are see as a single, cross-border, natural-regional and cultural-historical unit. So in addition to the use of the official landscape names of
1694:
section). In the Palatine part of the Wasgau alone there are over 200 rock massifs and free-standing rock pinnacles. Depending on the erosion of the Trifels, Rehberg and Karlstal beds they are classified as rock terraces
2135:
inhabitants per km, but, on the French side, it drops to just 59 inhabitants per km. The biosphere reserve includes not only the actual forest-covered mountains, but also densely populated areas along the edge of the
440:
The uplands of the Wasgau differ from those of the central Palatine Forest that border it to the north. The landscape of the Wasgau has a characteristically variable nature, with numerous conical hills
2574:
636:, 547 m), especially near the edge of the Rhine trough (e.g. the Grand Winterberg, 581 m, and the Rehberg, 577 m), while the bunter sandstone block in the west and south descends from about 500 m (
2311:
via Dahn to Bad Bergzabern. On the other side of the border, the well-developed departement road, the D 662, along the western edge of the Wasgau, links Bitche with Niederbronn-le-Bain and
1253:). This rock country extends from Annweiler in the northeast roughly to the stream of the Falkensteiner Bach at Phillipsburg in the southwest and forms the actual core area of the Wasgau.
1106:
were formed with a thickness of about 500 metres, of different strengths, thicknesses and colouring, and comprising mainly strongly hardened, silica-cemented, medium- and coarse-grained
620:
Due to its small-scale relief, the uplands of the Wasgau are characterized by considerable diversity of forms with rather isolated individual peaks - particularly the conical hills or
2152:
vast, desolate forests (some 70-90 % of the total land area), and lie mainly in the valleys and on the plateaux of the low mountain range. Exceptions are upland villages such as
2143:. If these areas are excluded to leave the area of the actual natural region itself, the population density is only about 20-30 inhabitants per km (e.g. 24 inhabitants per km in
2477:
1049:
676:
The columns in the table are based on the Natural Region Division Concept of the Wasgau. Each column shows the important hills of each sub-region in order of height.
831:
1438:; in keeping with the historical development of the name, these terms are used not just for the Palatine, but also for the Alsace-Lorraine part of the region.
993:
981:
2304:
1923:
1037:
933:
2343:
848:
770:
2296:
957:
2157:
1299:
in Alsace the rock forming Trifels beds were uplifted by about 80 to 100 metres and so these rocks continue to shape the surface of the landscape in the
587:
industry, that was practised until the end of the 19th century. These dams were able to trap logs after temporary flooding which, after the opening of a
405:
2978:
2237:
2030:
1411:. During the time from 1871 to 1919, when Alsace and parts of Lorraine temporarily belonged to Germany, the Vosges was generally referred to as the
1142:) were exposed after the overlying rock was eroded away. This resulted in tilting, bulging (thrusting and folding) and the fracturing (formation of
897:
909:
2144:
1403:
Gradually the names branched and developed separately due to the Franco-German border. Today the Alsace-Lorraine part of the range is called the
1187:
811:
876:
882:
310:
1086:
The Wasgau, as part of the Palatine Forest and the North Vosges, is characterized by rock strata of bunter sandstone and, to a lesser extent,
1186:
exposed. This resulted in erosion surfaces and broad valleys, as are particularly characteristic of the northeastern Wasgau, for example, in
644:, 513 m) to an average of about 350–400 m at the Saverne. Also typical is the number of variably shaped rock formations, mainly rocks of the
736:
2998:
2973:
2097:), which has an exhibition of the Palatine Forest-North Vosges Biosphere Reserve. Also in La Petite-Pierre is the Alsace Seal Museum (
945:
825:
125:
1393:
2963:
1890:
a variety of different options which, thanks to the highly variable nature and weathering of sandstone rock, offer a wide range of
1021:
969:
1178:) are particularly prominent, with the result that their surface layers were more heavily eroded. Because the formations of the
2371:
2147:
in Canton de Bitche) which, for Central Europe, are extremely low values. For example, the population density for the whole of
2066:
2216:
in Lorraine, and Eppenbrunn and Pirmasens in the Palatinate, the last-named being the largest town on the edge of the Wasgau.
2875:
Kurt Reh (1981), Michael Geiger; et al. (eds.), "Der Pfälzerwald : Eine Einführung in Landschaft und Namengebung",
2267:
2262:, which has now become the main source of income. In addition to mere relaxation, active holidays are offered, for example,
1953:). Whilst most rocks remain the province of professional climbers, certain rock terraces may be accessed on foot (e. g. the
1465:
2295:
federal highway along the northern edge of the Wasgau, the region is accessible on the Palatine side in the east from the
1794:
1167:
1005:
1650:
2078:
921:
2807:
1513:
2460:
2192:. The eastern edge of the range includes the settlements of Albersweiler and Bad Bergzabern in the Palatinate, and
1786:
1446:
2130:
Typical settlement structure in the Wasgau: view looking east from the Nedingfelsen rocks over parts of Hauenstein
2126:
565:
and Baerenthal, which have been mainly used for tourism since the closure of the last ironworks in 1923. Even the
2988:
1640:
2993:
2983:
2918:
2900:
2866:
2789:
2771:
2753:
2586:
2695:
2544:
Jost Haneke; Michael Weidenfeller (2010). "Die geologischen Baueinheiten der Pfalz". In Michael Geiger (ed.).
2780:
Michael Geiger (1987), "Der Pfälzerwald im geographischen Überblick", in Michael Geiger; et al. (eds.),
2652:
Klaus Hünerfauth (2010). "Natur- und Kulturlandschaften der Pfalz im Überblick"". In Michael Geiger (ed.).
118:
1875:
1773:
Small scale weathering of narrow strata with varying hardness has produced rock openings, rock gateways (
1660:
1612:
1569:
1557:
2208:
in Alsace. In the southwest to northwest running strip on the edge of the Wasgau lie the settlements of
1933:
In order to enable walkers to experience this rock landscape at closer hand, in recent years a range of
2968:
2185:
1630:
792:
2018:
2359:
2232:
Iron production and processing, which was important in earlier times (for example, iron smelting in
2181:
2086:
2004:
1396:
region which is adjacent to the Vosges to the southwest, whose name derives from the feminine form
1626:
1449:
used to run through the Wasgau; today it is more of touristic rather than religious significance.
776:
433:
2708:
Bernhard Köppen (2010). "Aspekte zur Bevölkerungsdynamik in der Pfalz". In Michael Geiger (ed.).
2082:
1752:
1732:
1285:
2042:
1665:
747:
645:
2270:. There are several well-maintained cycle paths that mainly follow the valleys in the Wasgau.
1980:
1477:
2327:
2197:
359:
287:
248:
30:
Typical Wasgau countryside with conical hills and plains: view looking southwest from Rehberg
1525:
25:
2165:
1810:
1767:
1720:
1122:
that, in the case of the bunter sandstone region, comprise Lower, Middle and Upper levels.
299:
256:
244:
110:
98:
2913:(in German), Stuttgart: Deutscher Wanderverlag Dr. Mair & Schnabel, pp. 176–226,
2362:
between Paris and Strasbourg, which will cross under the Col de Saverne through a tunnel.
404:, which extends from the Queich valley near Annweiler in the northeast to the area of the
8:
2559:
1992:
1841:
with particularly hardy and undemanding sandstone vegetation, that is mainly composed of
1748:
1645:
1635:
1573:
1561:
1292:
1210:, the so-called Trifels and Rehberg beds remained, because they mostly consist of harder
1154:
331:
182:
338:
coincides with the course of the River Queich, to the Col de Saverne and a line between
2748:(in German) (7th ed.), Landau/Pfalz: Pfälzische Verlagsanstalt, pp. 200–337,
2667:
2323:
and the D 604 cross the Col de Saverne, right in the south of the natural region.
2177:
2173:
2074:
2062:
2010:
1821:, the Drachenfels near Busenberg and the Fleckenstein near Hirschthal and Lembach (see
1818:
1756:
1740:
1617:
1501:
1489:
1419:
1378:
1296:
1288:
1226:
1203:
1195:
1126:
1095:
1056:
612:
194:
169:
86:
2891:
Martina Schönberger (2005), Landesamt für Geologie und Bergbau Rheinland-Pfalz (ed.),
2292:
2233:
625:
573:
has become a major tourist centre with swimming facilities, boat rentals and camping.
283:
2914:
2896:
2880:
2862:
2846:
2830:
2803:
2785:
2767:
2749:
2582:
2070:
1762:
1603:
1300:
1238:
1091:
759:
702:
399:
391:
387:
363:
279:
44:
2861:(in German) (2nd ed.), Landau/Pfalz: Verlag Pfälzer Kunst Dr. Hans Blinn,
2627:
604:
566:
515:
in the Wasgau, but especially in the area of the Saarbach stream, historic ponds or
2308:
2255:
2189:
2140:
2109:
2090:
1866:
1798:
1744:
1545:
1325:
1207:
1103:
730:
588:
375:
367:
303:
295:
200:
48:
2510:. Deutscher Wanderverlag Dr. Mair & Schnabel & Co., Stuttgart 1983, p. 81.
2358:
to Strasbourg mainly serves regional traffic. Currently under construction is the
1870:
Palatine Conservation Clubs (e. g. the Peregrine Conservation Working Group (
1797:). On many rocks - for example, the almost two-kilometre-long rock terrace of the
1191:
696:
641:
2958:
2054:
1854:
1607:
1595:
1565:
1273:
1143:
378:
that dominates the Wasgau. This natural boundary runs roughly from Pirmasens via
260:
225:
217:
165:
82:
2933:
2346:
in the west there are excursion services on Sundays and holidays. The line from
2278:
2300:
2247:-related industry and small businesses dominated, especially those involved in
2176:. On the French, in addition to the aforementioned places, are the villages of
1891:
1846:
1599:
1585:
1580:
1541:
1313:
1304:
1277:
1246:
1012:
584:
558:
550:
542:
492:
477:
457:
409:
351:
335:
272:
240:
157:
2798:
Michael Geiger (2010), "Die Landschaften der Pfalz", in Michael Geiger (ed.),
2347:
2335:
570:
452:
The Wasgau is drained mostly towards the east by left-hand tributaries of the
102:
2952:
2820:(in German), Braunschweig und Berlin: Georg Westermann Verlag, pp. 10–32
2355:
2351:
1895:
1887:
1842:
1553:
1308:
473:
465:
449:). Between the hills are conspicuously level plains, some of them extensive.
417:
366:. In the west the hills transition smoothly into the landscape region of the
140:
127:
2943:
2827:
Pfalz mit Weinstraße : Landschaft, Geschichte, Kultur, Kunst, Volkstum
2802:(in German), Landau/Pfalz: Verlag Pfälzische Landeskunde, pp. 92–113,
2283:
2136:
1728:
1681:
1183:
1139:
1134:
1115:
1099:
719:
637:
481:
428:
347:
76:
2422:
Landesamt für Vermessung und Geobasisinformation Rheinland-Pfalz (pub.):
2331:
2224:
2193:
1965:) or may be climbed, with care, with the aid of ladders and steps (e. g.
1934:
1899:
1549:
1430:("Southern Palatine Forest"), the range is called by the overall term of
1329:
1281:
939:
The Schlossberg (Hohenburg) (Wasgau Felsenland): view from the Wegelnburg
583:) were constructed, for example on the Wieslauter stream, as part of the
562:
538:
534:
530:
522:
453:
371:
355:
2482:
1572:
was destroyed because part of it had belonged to the rebellious knight,
1256:
1241:, that is characterized by diversely-shaped, often conical and isolated
628:. The highest peaks are in the northern and central Wasgau (such as the
2884:
2850:
2834:
2320:
2209:
1802:
1712:
1655:
1622:
1265:
1234:
1218:
753:
713:
629:
576:
553:
was used during the 18th and 19th centuries for processing iron in the
546:
496:
413:
379:
339:
1937:
has been established. In the Wasgau these include the Dahn Rock Path (
1544:, which was partially restored during the 20th century, was where the
1392:("Wasgen Forest"). Linguistically these terms are also related to the
1110:, but also some fine-grained sandstones, bonded with clay cement, and
656:
beds, that are found on many hills in the Wasgau (see the sections on
561:. To that end, several larger and smaller ponds were laid out between
2201:
2058:
1915:
1834:
1778:
1700:
1590:
1321:
1214:
1199:
1179:
1130:
1111:
1107:
1087:
1028:
554:
503:
327:
204:
2579:
Die Kelten : Ihre Geschichte von den Anfängen bis zur Gegenwart
2108:
Another attraction are the rock dwellings a few kilometres south of
1260:
Middle Bunter Sandstone with Karlstal beds and Upper Rock zone: the
2879:(in German), vol. 1, Landau/Pfalz: Selbstverlag, p. 381,
2845:(in German) (14th ed.), Ludwigshafen/Rhein: Waldkirch Verlag,
2829:(in German), Heroldsberg: Glock und Lutz Verlag, pp. 191–238,
2423:
2312:
2263:
2244:
2153:
1568:, called "Hans Trapp", has been restored, is occupied and managed.
1162:
252:
106:
1715:
near Annweiler; the Erbsenfelsen near Egelshardt) and rock walls (
1133:
period (66–23.8 million years ago), these rock strata experienced
608:
The Rehberg (577 m), the highest hill on German soil in the Wasgau
2938:
2818:
Der Pfälzerwald : Ein Beitrag zur Landeskunde der Rheinpfalz
2259:
2258:, the shoe industry waned and the economy increasingly turned to
2236:) came to an end in the late 19th century. A number of so-called
2205:
2148:
1838:
1806:
1354:
1230:
1222:
1158:
Summit region of the Rehberg: rock formations of the Rehberg beds
1074:
343:
237:
2895:(in German), Stuttgart: Schweizerbart’sche Verlagsbuchhandlung,
2730:(in German). Rhineland-Palatinate Ministry of Economic Affairs.
2723:
2543:
2339:
2213:
1537:
1358:, who was adopted by the Romans who incorporated it into their
1211:
1119:
383:
291:
268:
264:
233:
2712:. Landau/Pfalz: Verlag Pfälzische Landeskunde. p. 192 ff.
2548:. Landau/Pfalz: Verlag Pfälzische Landeskunde. pp. 82–84.
1415:
in order to emphasise the distance from the Roman-Latin term.
1069:
903:
Observation tower on the Grand Wintersberg (Wasgau Felsenland)
2666:
Naturschutzbund Deutschland e. V. (NABU) in Rheinland-Pfalz:
2561:
Geologischer Kartenausschnitt Zaberner Steige und Nordvogesen
2455:
2453:
2316:
1898:
include the regions around Annweiler (e. g. the Asselstein),
1850:
1576:. Other castles of the region include (from north to south):
1359:
1349:
487:
306:, which is the highest summit on German soil in the Wasgau.
2656:. Landau/Pfalz: Verlag Pfälzische Landeskunde. p. 158.
2630:. Website des Wanderportals Pfalz. Retrieved 12 March 2012.
2342:, but has been repeatedly downgraded in importance. On the
2248:
2240:
fountains bear witness to this traditional industry today.
2169:
1862:
1858:
1704:
1242:
1233:
period (23.8 to 2.8 million years ago), and especially the
999:
View from the Rehberg towards Treutelsberg (eastern Wasgau)
526:
517:
512:
398:
A central sub-region of the Wasgau is the Dahn-Annweilerer-
2784:(in German), Landau/Pfalz: Verlag Pfälzische Landeskunde,
2485:*Blatt 160: Landau/Pfalz (Adalbert Pemöller 1969; 47 pp.).
2450:
975:
The Mohnenberg (eastern Wasgau): view from Schöneck Castle
2642:"Der Pfälzerwald im geographischen Überblick", pp. 39–43.
2618:"Der Pfälzerwald im geographischen Überblick", pp. 18–19.
2534:"Der Pfälzerwald im geographischen Überblick", pp. 24–29.
2497:"Der Pfälzerwald im geographischen Überblick", pp. 40–41.
2478:
Die naturräumlichen Einheiten in Einzelblättern 1:200.000
2766:(in German) (4th ed.), Meckenheim: Warlich Verlag,
1149:
1043:
The Ebersberg (Wasgau Felsenland): view from the Rehberg
624:- which reach an average height of 400–500 metres above
507:
The Hanauer Weiher with Waldeck Castle in the background
1685:
The Asselstein: view from northwest of its broader side
1237:
period (2.8 to 0.01 million years ago), as a result of
987:
The Föhrlenberg (eastern Wasgau): view from the Rehberg
951:
Hohe Derst (eastern Wasgau): view from the Stäffelsberg
668:
and Wasenkoepfel) that offer visitors a 360° panorama.
432:
The small-scale structure of the Wasgau: View from the
2724:"Welcome to the Rhineland-Palatinate Cycle Wonderland"
2330:
which runs parallel to the B 10, was once part of the
2522:"Der Pfälzerwald im geographischen Überblick", p. 41.
2036:
Administration centre of the North Vosges Nature Park
963:
The Hohenberg (eastern Wasgau): view from the Rehberg
915:
The Rehberg and Asselstein (left) (Wasgau Felsenland)
480:
extends southwards via its right-hand tributary, the
2459:
Landesamt für Geologie und Bergbau Rheinland-Pfalz:
2053:
Amongst the other attractions of the Wasgau are the
1699:, e. g. the Heidenpfeiler and Buhlsteinpfeiler near
472:
in North Alsace. setzt. There it is followed by the
2890:
1759:), which are mainly found on top of conical hills.
616:
View from the Wegelnburg over the Wasgau Felsenland
2418:
2416:
2414:
2164:Other, larger settlements on the German side are
1098:(251–243 million years ago), predominantly under
927:The Schlossberg (Wegelnburg) (Wasgau Felsenland)
346:in the south. Its eastern boundary, running from
294:. Next, at 577 m is the only slightly lower
81:Location of the Wasgau (highlit) in the southern
2950:
2651:
2291:In addition to the main transport artery of the
1348:have the same linguistic source: the originally
1166:Small scale weathering in the Rehberg beds: the
2782:Der Pfälzerwald : Porträt einer Landschaft
2761:
2707:
2326:The railway line from Pirmasens to Landau, the
2315:in the Rhine plain. The A 4 motorway from
2228:Inscription on the Gienanth Fountain in Schönau
2893:Geologie und Erdgeschichte von Rheinland-Pfalz
2856:
2815:
2797:
2779:
2694:Biosphärenreservat Pfälzerwald-Vosges du Nord:
2639:
2615:
2573:
2531:
2519:
2494:
2411:
1881:
1373:("Vosegus Wood"). This name became the French
1078:Trifels strata visible on a rock terrace: the
591:could be transported downstream on the water.
533:or to utilize their water in the operation of
311:Palatine Forest-North Vosges Biosphere Reserve
2934:Biosphärenreservat Pfälzerwald–Vosges du Nord
2908:
2859:Der Wasgau mit seinen Felsen und Felsenburgen
2743:
2391:Der Wasgau mit seinen Felsen und Felsenburgen
2116:
1540:in the region, several have written history.
278:The highest hill in the entire Wasgau is the
259:. It is formed from the southern part of the
1519:View of the Fleckenstein from the Hohenbourg
1217:and are therefore particularly resistant to
370:; from there the younger rock strata of the
2840:
2462:Geologische Übersichtskarte Rheinland-Pfalz
2445:Cartes Topographiques 1:25.000 und 1:50.000
1070:Formation and deposition of the rock strata
271:in the north over the French border to the
2824:
2685:. GeoHist Verlag, Neu-Anspach 2000, p. 76.
2600:
2402:
309:The Wasgau forms the southern part of the
2567:
2439:
2437:
2435:
2266:in the South Palatinate Climbing Area or
1303:and Schönau Felsenland. Only west of the
2979:Natural regions of the Palatinate Forest
2874:
2277:
2223:
2125:
1949:) and the Annweiler Red Sandstone Path (
1761:
1680:
1255:
1161:
1153:
1073:
611:
603:
502:
486:
427:
47:(581 m above NHN) for the whole Wasgau;
2103:Musée des Arts et Traditions populaires
1229:of the Wasgau was developed during the
1206:. At the same time, parts of the Lower
569:, a pond a few miles east of Bitche in
2951:
2443:Institut Géographique National (ed.):
2432:
2287:train to Landau at Dahn station (2008)
1560:, Trifels is the symbol of Annweiler.
1094:(256–251 million years ago) and early
1059:of Mont Saint-Michel (southern Wasgau)
2085:and the administrative centre of the
1150:Development of the present topography
51:(577 m above NHN) for the German part
2303:, and in the west and south via the
671:
661:
491:A former timber rafting weir on the
445:) as well as clearly rounded domes (
326:The Wasgau runs from a line between
187:Bunter sandstone 251–243 M years ago
1837:perspective many rock regions form
1723:). Other rock forms are pinnacles (
1335:
64:1,300 km (500 sq mi)
13:
2669:Wanderfalkenschutz Rheinland-Pfalz
2581:(in German), München: C. H. Beck,
1828:
1671:
1090:, which was deposited in the late
529:that were artificially created to
14:
3010:
2999:Landforms of Moselle (department)
2974:Geography of Rhineland-Palatinate
2939:Biosphärenhaus mit Baumwipfelpfad
2927:
2372:Südliche Weinstraße Wildlife Park
2067:Südliche Weinstraße Wildlife Park
2447:. Paris, verschiedene Jahrgänge.
2243:In the 19th and 20th centuries,
2041:
2029:
2017:
2003:
1991:
1979:
1865:. In addition, since the 1980s,
1548:were kept for a time during the
1524:
1512:
1500:
1488:
1476:
1464:
1418:As part of the European treaty (
1048:
1036:
1020:
1004:
992:
980:
968:
956:
944:
932:
920:
908:
896:
75:
24:
2964:Regions of Rhineland-Palatinate
2716:
2701:
2688:
2675:
2660:
2645:
2633:
2621:
2609:
2594:
2552:
2537:
2525:
2474:Bundesanstalt für Landeskunde:
1945:) the Hauenstein Cobbler Path (
1886:The Wasgauer Felsenland offers
1872:Arbeitskreis Wanderfalkenschutz
1777:, e.g. the Eilöchelfelsen near
1564:owned by the legendary knight,
1552:. Together with the castles of
1100:desert-like climatic conditions
2513:
2500:
2488:
2476:Geographische Landesaufnahme.
2468:
2429:; retrieved, 13 February 2012.
2396:
2383:
2101:) and a local history museum (
1910:), as well as the Dahn (e. g.
1703:; the Lämmerfelsen rocks near
1146:) of the various rock strata.
464:in its upper reaches) and the
1:
2737:
2481:. Bad Godesberg 1952–1994. →
2465:, retrieved 13 February 2012.
2377:
2121:
1951:Annweilerer Buntsandsteinpfad
1727:, e. g. the Hundsfelsen near
1441:The so-called "South Route" (
1407:and the Palatine part is the
1384:, which further evolved into
484:, beyond the Col de Saverne.
267:, and extends from the River
263:and the northern part of the
189:Zechstein 256–251 M years ago
2628:Die Felsen des Pfälzerwaldes
2273:
1941:), the Busenberg Clog Path (
1822:
1789:near Dahn) and rock tables (
1691:
1249:(the Wasgau Rock Country or
1125:During the formation of the
678:
657:
423:
316:
7:
2365:
1922:), to which the well known
1882:Sports climbers and walkers
1857:), and, in wet areas, also
321:
10:
3015:
2354:through the valley of the
2219:
2117:Economy and infrastructure
2024:Shoe Museum: shoe size 180
1972:
1457:
1064:
787:Brissetischer Kopf (529 m)
599:
2746:Die Pfalz und die Pfälzer
2698:. Retrieved 6 March 2012.
2672:. Retrieved 14 June 2012.
2564:. Retrieved 9 March 2012.
2156:in the eastern Hochwald,
1947:Hauensteiner Schusterpfad
1943:Busenberger Holzschuhpfad
1719:, e. g. the Dimberg near
1676:
1452:
854:(Hoch) Ebersberg (423 m)
842:Gr. Stephansberg (456 m)
468:, which continues as the
456:, namely the Queich, the
350:in the Queich valley via
193:
181:
176:
156:
117:
94:
73:
68:
60:
55:
40:
35:
23:
18:
2762:Rüdiger Bernges (2005),
2683:Zu Fuß durch die Vogesen
2087:North Vosges Nature Park
1906:) and Hauenstein (e. g.
868:Duerrberg(kopf) (421 m)
646:Lower Triassic sandstone
594:
364:edge of the Rhine Graben
334:in the north that, from
2857:Emil Knöringer (1985),
2816:Daniel Häberle (1913),
2744:August Becker (2005) ,
2099:Musée du sceau alsacien
2048:Rock homes in Graufthal
1731:; the Hühnerstein near
873:Kl. Biesenberg (451 m)
859:Hoher Warsberg (451 m)
837:Hollaenderberg (423 m)
727:Gr. Mückenkopf (485 m)
521:have survived from the
243:in the German state of
2989:Hill ranges of Germany
2909:Heinz Wittner (1981),
2877:Pfälzische Landeskunde
2764:Felsenburgen im Wasgau
2696:The Reserve in figures
2506:Heinz Wittner et al.:
2288:
2229:
2131:
1908:Spirkelbacher Rauhfels
1770:
1686:
1362:names for the region,
1268:
1170:
1159:
1083:
617:
609:
508:
500:
437:
229:
221:
2994:Mountains of Bas-Rhin
2984:Hill ranges of France
2944:Burgenparadies Wasgau
2841:Emil Heuser (1979) ,
2640:Michael Geiger (1987)
2616:Michael Geiger (1987)
2532:Michael Geiger (1987)
2520:Michael Geiger (1987)
2495:Michael Geiger (1987)
2427:1:25.000 und 1:50.000
2328:Queich Valley Railway
2281:
2227:
2198:Niederbronn-les-Bains
2129:
1765:
1684:
1428:Südlicher Pfälzerwald
1426:("North Vosges") and
1352:hill and forest god,
1316:or Pfalzburg Trough (
1259:
1165:
1157:
1104:Sedimentary sequences
1077:
615:
607:
511:There are no natural
506:
490:
431:
360:Niederbronn-les-Bains
288:Niederbronn-les-Bains
141:49.04822°N 7.662191°E
2800:Geographie der Pfalz
2710:Geographie der Pfalz
2654:Geographie der Pfalz
2604:Pfalz mit Weinstraße
2546:Geographie der Pfalz
2425:Topografische Karten
2406:Pfalz mit Weinstraße
2299:, from Annweiler to
2166:Annweiler am Trifels
1811:honeycomb weathering
1809:-like overhangs and
1768:Bride and Bridegroom
845:Wasserstein (512 m)
245:Rhineland-Palatinate
99:Rhineland-Palatinate
2825:Karl Heinz (1976),
1574:Franz von Sickingen
1562:Berwartstein Castle
1293:Niederschlettenbach
1027:The Rothenberg mit
1015:(Wasgau Felsenland)
1011:The Sonnenberg and
865:Mittelkopf (515 m)
862:Engenteich (496 m)
822:Braunsberg (463 m)
808:Schwobberg (524 m)
805:Hoher Kopf (467 m)
789:or Brissetish Kopf
541:. The water of the
401:Wasgauer Felsenland
137: /
2911:Großer Pfalzführer
2344:Wieslauter Railway
2289:
2230:
2132:
2079:Glass Shoe Factory
2075:German Shoe Museum
2057:with its adjacent
2011:German Shoe Museum
1969:near Hauenstein).
1813:may also be seen.
1771:
1687:
1570:Drachenfels Castle
1445:) of the historic
1420:Schengen Agreement
1379:Middle High German
1269:
1204:Fischbach bei Dahn
1171:
1160:
1127:Upper Rhine Graben
1114:. These rocks are
1084:
1057:Saint-Jean-Saverne
888:Hochfirst (421 m)
849:Krummer Ellenbogen
742:Immenkopf (494 m)
709:Großer Wintersberg
685:Wasgau Felsenland
618:
610:
525:. These are small
509:
501:
438:
420:in the southwest.
362:to Saverne is the
282:(581 m above
146:49.04822; 7.662191
36:Highest point
2969:Regions of Europe
2843:Neuer Pfalzführer
2681:Thomas Striebig:
2601:Karl Heinz (1976)
2403:Karl Heinz (1976)
1939:Dahner Felsenpfad
1928:Pferchfeldfelsen)
1916:Erfweiler regions
1867:peregrine falcons
1781:), rock columns (
1318:Pfalzburger Mulde
1301:Dahner Felsenland
1251:Wasgau Felsenland
1176:Südpfälzer Sattel
892:
891:
817:Hochkopf (429 m)
793:Mont Saint-Michel
765:Arnsberg (479 m)
760:Bobenthaler Knopf
703:Grand Wintersberg
672:Detailed overview
632:, 572 m, and the
406:Falkensteinerbach
280:Grand Wintersberg
210:
209:
119:Range coordinates
45:Grand Wintersberg
3006:
2923:
2905:
2887:
2871:
2853:
2837:
2821:
2812:
2794:
2776:
2758:
2732:
2731:
2720:
2714:
2713:
2705:
2699:
2692:
2686:
2679:
2673:
2664:
2658:
2657:
2649:
2643:
2637:
2631:
2625:
2619:
2613:
2607:
2598:
2592:
2591:
2571:
2565:
2556:
2550:
2549:
2541:
2535:
2529:
2523:
2517:
2511:
2504:
2498:
2492:
2486:
2472:
2466:
2457:
2448:
2441:
2430:
2420:
2409:
2400:
2394:
2389:Emil Knöringer:
2387:
2309:Hinterweidenthal
2256:Second World War
2190:Wingen-sur-Moder
2141:Westrich Plateau
2110:La Petite-Pierre
2091:La Petite-Pierre
2045:
2033:
2021:
2007:
1995:
1983:
1924:Bärenbrunner Tal
1799:Altschlossfelsen
1745:Vorderweidenthal
1598:, consisting of
1546:imperial regalia
1536:Of the numerous
1528:
1516:
1504:
1492:
1480:
1468:
1447:Way of St. James
1367:("Vosegus Hill")
1336:Name and history
1326:Wingen-sur-Moder
1262:Altschlossfelsen
1208:Bunter Sandstone
1052:
1040:
1031:(eastern Wasgau)
1024:
1008:
996:
984:
972:
960:
948:
936:
924:
912:
900:
691:Southern Wasgau
679:
376:bunter sandstone
368:Westrich Plateau
304:South Palatinate
265:Vosges mountains
201:bunter sandstone
168:(south) and the
160:
152:
151:
149:
148:
147:
142:
138:
135:
134:
133:
130:
79:
28:
16:
15:
3014:
3013:
3009:
3008:
3007:
3005:
3004:
3003:
2949:
2948:
2930:
2921:
2903:
2869:
2810:
2792:
2774:
2756:
2740:
2735:
2722:
2721:
2717:
2706:
2702:
2693:
2689:
2680:
2676:
2665:
2661:
2650:
2646:
2638:
2634:
2626:
2622:
2614:
2610:
2599:
2595:
2589:
2572:
2568:
2557:
2553:
2542:
2538:
2530:
2526:
2518:
2514:
2505:
2501:
2493:
2489:
2473:
2469:
2458:
2451:
2442:
2433:
2421:
2412:
2401:
2397:
2388:
2384:
2380:
2368:
2276:
2251:manufacturing.
2222:
2186:Niedersteinbach
2124:
2119:
2055:Biosphere House
2049:
2046:
2037:
2034:
2025:
2022:
2013:
2008:
1999:
1998:Baumwipfel Path
1996:
1987:
1986:Biosphere House
1984:
1975:
1926:belongs (e. g.
1904:Luger Friedrich
1892:climbing grades
1884:
1855:wavy hair-grass
1831:
1829:Fauna und Flora
1787:Bride and Groom
1707:), rock faces (
1679:
1674:
1672:Rock formations
1596:Castles of Dahn
1566:Hans von Trotha
1532:
1529:
1520:
1517:
1508:
1505:
1496:
1493:
1484:
1481:
1472:
1469:
1460:
1455:
1338:
1247:rock formations
1152:
1072:
1067:
1060:
1053:
1044:
1041:
1032:
1025:
1016:
1009:
1000:
997:
988:
985:
976:
973:
964:
961:
952:
949:
940:
937:
928:
925:
916:
913:
904:
901:
796:
788:
780:
706:
688:Eastern Wasgau
682:Western Wasgau
674:
662:rock formations
602:
597:
426:
324:
319:
261:Palatine Forest
247:and the French
188:
166:Palatine Forest
158:
145:
143:
139:
136:
131:
128:
126:
124:
123:
90:
89:
83:Palatine Forest
31:
12:
11:
5:
3012:
3002:
3001:
2996:
2991:
2986:
2981:
2976:
2971:
2966:
2961:
2947:
2946:
2941:
2936:
2929:
2928:External links
2926:
2925:
2924:
2919:
2906:
2901:
2888:
2872:
2867:
2854:
2838:
2822:
2813:
2808:
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2790:
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2772:
2759:
2754:
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2733:
2715:
2700:
2687:
2674:
2659:
2644:
2632:
2620:
2608:
2593:
2587:
2575:Bernhard Maier
2566:
2551:
2536:
2524:
2512:
2508:Vogesen – Nord
2499:
2487:
2467:
2449:
2431:
2410:
2408:, pp. 197–199.
2395:
2381:
2379:
2376:
2375:
2374:
2367:
2364:
2301:Bad Bergzabern
2275:
2272:
2221:
2218:
2123:
2120:
2118:
2115:
2051:
2050:
2047:
2040:
2038:
2035:
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2026:
2023:
2016:
2014:
2009:
2002:
2000:
1997:
1990:
1988:
1985:
1978:
1974:
1971:
1896:climbing areas
1888:sport climbers
1883:
1880:
1847:common heather
1830:
1827:
1735:) and blocks (
1678:
1675:
1673:
1670:
1669:
1668:
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1658:
1653:
1648:
1643:
1638:
1633:
1620:
1615:
1610:
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1588:
1583:
1542:Trifels Castle
1534:
1533:
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1523:
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1497:
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1487:
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1482:
1475:
1473:
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1463:
1459:
1456:
1454:
1451:
1424:Vosges du Nord
1337:
1334:
1314:Col de Saverne
1278:Wilgartswiesen
1274:Elmstein Fault
1151:
1148:
1080:Jungfernsprung
1071:
1068:
1066:
1063:
1062:
1061:
1054:
1047:
1045:
1042:
1035:
1033:
1026:
1019:
1017:
1013:Trifels Castle
1010:
1003:
1001:
998:
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989:
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785:
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723:
717:
711:
700:
693:
692:
689:
686:
683:
673:
670:
601:
598:
596:
593:
585:timber rafting
567:Étang de Hanau
559:blast furnaces
551:Pays de Bitche
543:Zinsel du Nord
478:catchment area
425:
422:
410:Zinsel du Nord
358:in Alsace and
352:Bad Bergzabern
336:Wilgartswiesen
323:
320:
318:
315:
275:in the south.
273:Col de Saverne
208:
207:
197:
191:
190:
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42:
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33:
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29:
21:
20:
9:
6:
4:
3:
2:
3011:
3000:
2997:
2995:
2992:
2990:
2987:
2985:
2982:
2980:
2977:
2975:
2972:
2970:
2967:
2965:
2962:
2960:
2957:
2956:
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2945:
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2940:
2937:
2935:
2932:
2931:
2922:
2916:
2912:
2907:
2904:
2898:
2894:
2889:
2886:
2882:
2878:
2873:
2870:
2864:
2860:
2855:
2852:
2848:
2844:
2839:
2836:
2832:
2828:
2823:
2819:
2814:
2811:
2809:9783981297409
2805:
2801:
2796:
2793:
2787:
2783:
2778:
2775:
2769:
2765:
2760:
2757:
2751:
2747:
2742:
2741:
2729:
2728:Radwanderland
2725:
2719:
2711:
2704:
2697:
2691:
2684:
2678:
2671:
2670:
2663:
2655:
2648:
2641:
2636:
2629:
2624:
2617:
2612:
2605:
2602:
2597:
2590:
2584:
2580:
2576:
2570:
2563:
2562:
2555:
2547:
2540:
2533:
2528:
2521:
2516:
2509:
2503:
2496:
2491:
2484:
2483:Online-Karten
2480:
2479:
2471:
2464:
2463:
2456:
2454:
2446:
2440:
2438:
2436:
2428:
2426:
2419:
2417:
2415:
2407:
2404:
2399:
2392:
2386:
2382:
2373:
2370:
2369:
2363:
2361:
2357:
2353:
2352:Sarreguemines
2349:
2345:
2341:
2337:
2333:
2329:
2324:
2322:
2318:
2314:
2310:
2306:
2302:
2298:
2294:
2286:
2285:
2280:
2271:
2269:
2265:
2261:
2257:
2252:
2250:
2246:
2241:
2239:
2235:
2226:
2217:
2215:
2211:
2207:
2203:
2199:
2195:
2191:
2187:
2183:
2182:Obersteinbach
2179:
2175:
2171:
2167:
2162:
2159:
2155:
2150:
2146:
2145:Phillipsbourg
2142:
2138:
2128:
2114:
2111:
2106:
2104:
2100:
2096:
2092:
2088:
2084:
2080:
2076:
2072:
2068:
2064:
2060:
2056:
2044:
2039:
2032:
2027:
2020:
2015:
2012:
2006:
2001:
1994:
1989:
1982:
1977:
1976:
1970:
1968:
1964:
1960:
1959:Heidenpfeiler
1956:
1952:
1948:
1944:
1940:
1936:
1931:
1929:
1925:
1921:
1917:
1913:
1909:
1905:
1901:
1897:
1894:. Well known
1893:
1889:
1879:
1877:
1873:
1868:
1864:
1860:
1856:
1852:
1848:
1844:
1843:mountain pine
1840:
1836:
1826:
1824:
1820:
1814:
1812:
1808:
1804:
1800:
1796:
1795:Devil's Table
1792:
1788:
1784:
1780:
1776:
1769:
1764:
1760:
1758:
1754:
1750:
1746:
1742:
1738:
1734:
1730:
1726:
1722:
1718:
1714:
1710:
1706:
1702:
1698:
1693:
1683:
1667:
1664:
1662:
1659:
1657:
1654:
1652:
1649:
1647:
1644:
1642:
1639:
1637:
1634:
1632:
1628:
1624:
1621:
1619:
1616:
1614:
1611:
1609:
1605:
1601:
1597:
1594:
1592:
1589:
1587:
1584:
1582:
1579:
1578:
1577:
1575:
1571:
1567:
1563:
1559:
1555:
1551:
1547:
1543:
1539:
1527:
1522:
1515:
1510:
1503:
1498:
1491:
1486:
1479:
1474:
1467:
1462:
1461:
1450:
1448:
1444:
1439:
1437:
1433:
1429:
1425:
1421:
1416:
1414:
1410:
1406:
1401:
1399:
1395:
1391:
1387:
1383:
1380:
1376:
1372:
1371:Silva Vosegus
1368:
1365:
1361:
1357:
1356:
1351:
1347:
1343:
1333:
1331:
1327:
1323:
1319:
1315:
1310:
1306:
1305:(Wies-)Lauter
1302:
1298:
1294:
1290:
1287:
1283:
1279:
1276:roughly from
1275:
1267:
1263:
1258:
1254:
1252:
1248:
1245:with bizarre
1244:
1240:
1236:
1232:
1228:
1224:
1220:
1216:
1213:
1209:
1205:
1201:
1197:
1193:
1192:Völkersweiler
1189:
1188:Gossersweiler
1185:
1181:
1177:
1169:
1168:Devil's Table
1164:
1156:
1147:
1145:
1141:
1136:
1132:
1128:
1123:
1121:
1118:into various
1117:
1113:
1109:
1105:
1101:
1097:
1093:
1089:
1081:
1076:
1058:
1051:
1046:
1039:
1034:
1030:
1023:
1018:
1014:
1007:
1002:
995:
990:
983:
978:
971:
966:
959:
954:
947:
942:
935:
930:
923:
918:
911:
906:
899:
894:
893:
887:
884:
881:
878:
875:
872:
871:
867:
864:
861:
858:
857:
853:
850:
847:
844:
841:
840:
836:
833:
830:
827:
824:
821:
820:
816:
813:
812:Schletterberg
810:
807:
804:
803:
800:
794:
791:
786:
784:
778:
775:
772:
769:
768:
764:
761:
758:
755:
752:
749:
746:
745:
741:
738:
735:
732:
729:
726:
725:
721:
718:
715:
712:
710:
704:
701:
698:
695:
694:
690:
687:
684:
681:
680:
677:
669:
667:
663:
659:
655:
651:
647:
643:
642:Großer Eyberg
639:
635:
631:
627:
623:
614:
606:
592:
590:
586:
582:
578:
574:
572:
568:
564:
560:
556:
552:
548:
544:
540:
536:
532:
528:
524:
520:
519:
514:
505:
499:north of Dahn
498:
494:
489:
485:
483:
479:
475:
471:
467:
463:
459:
455:
450:
448:
444:
436:looking north
435:
430:
421:
419:
418:Philippsbourg
415:
411:
407:
403:
402:
396:
393:
389:
385:
381:
377:
373:
369:
365:
361:
357:
353:
349:
345:
341:
337:
333:
329:
314:
312:
307:
305:
301:
297:
293:
289:
285:
281:
276:
274:
270:
266:
262:
258:
254:
250:
246:
242:
239:
235:
231:
227:
223:
219:
215:
206:
202:
198:
196:
192:
186:
184:
180:
175:
171:
167:
163:
161:
155:
150:
122:
120:
116:
112:
108:
104:
100:
97:
93:
88:
85:and northern
84:
78:
72:
67:
63:
59:
54:
50:
46:
43:
39:
34:
27:
22:
17:
2910:
2892:
2876:
2858:
2842:
2826:
2817:
2799:
2781:
2763:
2745:
2727:
2718:
2709:
2703:
2690:
2682:
2677:
2668:
2662:
2653:
2647:
2635:
2623:
2611:
2603:
2596:
2578:
2569:
2560:
2554:
2545:
2539:
2527:
2515:
2507:
2502:
2490:
2475:
2470:
2461:
2444:
2424:
2405:
2398:
2390:
2385:
2325:
2290:
2284:Regionalbahn
2282:
2253:
2242:
2231:
2163:
2137:Rhine Graben
2133:
2107:
2102:
2098:
2094:
2052:
1966:
1962:
1958:
1954:
1950:
1946:
1942:
1938:
1935:themed walks
1932:
1927:
1919:
1912:Lämmerfelsen
1911:
1907:
1903:
1885:
1871:
1832:
1815:
1790:
1782:
1774:
1772:
1749:Fleckenstein
1736:
1729:Waldrohrbach
1724:
1716:
1708:
1696:
1688:
1646:Wasigenstein
1636:Fleckenstein
1558:Scharfenberg
1535:
1483:Berwartstein
1442:
1440:
1435:
1431:
1427:
1423:
1417:
1412:
1408:
1404:
1402:
1397:
1389:
1385:
1381:
1374:
1370:
1366:
1364:Vosegus mons
1363:
1353:
1345:
1341:
1339:
1317:
1270:
1261:
1250:
1225:. The micro-
1184:Rotliegendes
1175:
1172:
1140:Rotliegendes
1135:tectonically
1124:
1085:
1079:
883:Treutelsberg
799:Michaelsberg
798:
782:
720:Wasenkoepfel
708:
675:
666:Stäffelsberg
665:
653:
649:
640:, 526 m and
638:Wasenkoepfel
633:
621:
619:
580:
575:
539:hammer mills
516:
510:
469:
461:
460:(called the
451:
446:
442:
439:
400:
397:
348:Albersweiler
325:
308:
290:in northern
277:
213:
211:
195:Type of rock
159:Parent range
103:Départements
2348:Saarbrücken
2336:Saarbrücken
2332:trunk route
2194:Wissembourg
2095:Lützelstein
1967:Hühnerstein
1963:Rötzenstein
1849:and simple
1793:, e.g. the
1791:Tischfelsen
1785:, e.g. the
1783:Felsspalten
1741:Lindelbrunn
1711:, e.g. the
1661:Lichtenberg
1651:Falkenstein
1641:Blumenstein
1618:Lindelbrunn
1550:Middle Ages
1531:Lichtenberg
1495:Drachenfels
1330:Diemeringen
1282:Spirkelbach
1264:rocks near
577:Splash dams
571:Éguelshardt
563:Mouterhouse
523:Middle Ages
454:River Rhine
408:stream and
372:muschelkalk
356:Wissembourg
249:departments
199:Rock units
183:Age of rock
144: /
101:(Germany);
2953:Categories
2920:3813401065
2902:3510652657
2885:B0025WB9GK
2868:3922580165
2851:B0043G3V6M
2835:B01KOIENVO
2791:3980114716
2773:3930376253
2755:3898571939
2738:Literature
2588:3406460941
2378:References
2321:Strasbourg
2305:B 427
2254:After the
2210:Phalsbourg
2174:Hauenstein
2122:Settlement
2083:Hauenstein
1955:Buhlsteine
1920:Heegerturm
1825:section).
1803:Eppenbrunn
1753:Hirschthal
1737:Felsklötze
1733:Hauenstein
1717:Felsmauern
1713:Asselstein
1656:Wasenbourg
1631:Lœwenstein
1627:Hohenbourg
1623:Wegelnburg
1604:Grafendahn
1413:Wasgenwald
1390:Wasgenwald
1377:, and the
1340:The names
1286:Schwanheim
1266:Eppenbrunn
1235:Quaternary
1219:weathering
1196:Hauenstein
1194:, also in
1108:sandstones
1055:View from
877:Jüngstberg
832:Dürrenberg
777:Hohenbourg
754:Wegelnburg
737:Mohnenberg
714:Hohe Derst
697:Gr. Eyberg
634:Mohnenberg
630:Wegelnburg
622:Kegelberge
547:Baerenthal
535:watermills
531:breed fish
497:splash dam
493:Wieslauter
462:Wieslauter
443:Kegelberge
414:Baerenthal
380:Eppenbrunn
374:cover the
340:Phalsbourg
241:hill range
129:49°02′54″N
56:Dimensions
2606:, p. 198.
2297:B 48
2293:B 10
2274:Transport
2202:Ingwiller
2093:(German:
2063:Fischbach
2059:tree walk
1835:botanical
1819:Erlenbach
1779:Busenberg
1775:Torfelsen
1725:Felstürme
1709:Felswände
1701:Busenberg
1697:Felsriffe
1666:Hunebourg
1591:Madenburg
1322:Ingweiler
1289:Erlenbach
1215:sandstone
1200:Busenberg
1180:Zechstein
1131:Paleogene
1088:Zechstein
1082:near Dahn
1029:Madenburg
783:Hohenburg
771:Erlenkopf
748:Hohe List
626:sea level
555:ironworks
434:Hohenburg
424:Structure
328:Pirmasens
317:Geography
300:Annweiler
205:Zechstein
132:7°39′44″E
69:Geography
2577:(2000),
2393:, p. 14.
2366:See also
2360:TGV link
2334:between
2313:Haguenau
2264:climbing
2245:forestry
2238:Gienanth
2154:Climbach
2139:and the
1839:biotopes
1739:, e. g.
1608:Tanstein
1443:Südroute
1436:Vasgovie
1398:*Vosagia
1324:through
1096:Triassic
885:(505 m)
879:(491 m)
851:(515 m)
834:(521 m)
828:(515 m)
814:(521 m)
795:(437 m)
779:(551 m)
773:(472 m)
762:(534 m)
756:(572 m)
750:(476 m)
739:(547 m)
733:(577 m)
722:(526 m)
716:(561 m)
705:(581 m)
699:(513 m)
537:or iron
476:, whose
466:Saarbach
392:Lorraine
322:Location
253:Bas-Rhin
230:Vasgovie
113:(France)
107:Bas-Rhin
2307:, from
2260:tourism
2234:Schönau
2220:Economy
2206:Saverne
2178:Lembach
2149:Germany
1973:Gallery
1918:(e. g.
1902:(e. g.
1853:(e. g.
1851:grasses
1833:From a
1823:Castles
1807:cornice
1757:Lembach
1721:Dimbach
1692:Geology
1613:Landeck
1600:Altdahn
1586:Neudahn
1581:Lemberg
1538:castles
1507:Altdahn
1471:Trifels
1458:Castles
1382:Wasigen
1355:Vosegus
1297:Lembach
1239:erosion
1231:Neogene
1223:erosion
1129:in the
1116:divided
1092:Permian
1065:Geology
826:Maimont
731:Rehberg
658:Geology
654:Rehberg
650:Trifels
600:General
581:ecluses
549:in the
388:Lemberg
344:Saverne
302:in the
296:Rehberg
286:) near
257:Moselle
232:) is a
177:Geology
172:(north)
164:of the
111:Moselle
49:Rehberg
2959:Wasgau
2917:
2899:
2883:
2865:
2849:
2833:
2806:
2788:
2770:
2752:
2585:
2558:BRGM:
2340:Munich
2268:hiking
2214:Bitche
2077:, the
2073:, the
2065:, the
1914:) and
1859:mosses
1677:Shapes
1554:Anebos
1453:Sights
1432:Wasgau
1409:Wasgau
1405:Vosges
1386:Wasgau
1375:Vosges
1350:Celtic
1346:Vosges
1342:Wasgau
1295:up to
1227:relief
1212:quartz
1144:faults
1120:strata
1112:shales
648:, the
458:Lauter
447:Kuppen
384:Bitche
332:Landau
292:Alsace
269:Queich
238:German
234:Franco
226:French
222:Wasgau
218:German
214:Wasgau
170:Vosges
87:Vosges
19:Wasgau
2356:Moder
2317:Paris
1874:) of
1863:ferns
1801:near
1751:near
1743:near
1360:Latin
1309:Sauer
1243:hills
797:Ger:
781:Ger:
707:Ger:
595:Hills
545:near
527:lakes
518:woogs
513:lakes
495:at a
474:Moder
470:Sauer
412:near
298:near
95:State
2915:ISBN
2897:ISBN
2881:ASIN
2863:ISBN
2847:ASIN
2831:ASIN
2804:ISBN
2786:ISBN
2768:ISBN
2750:ISBN
2583:ISBN
2350:via
2338:and
2249:shoe
2212:and
2204:and
2188:and
2172:and
2170:Dahn
2158:Lviv
2071:Silz
1961:and
1876:NABU
1861:and
1766:The
1755:and
1705:Dahn
1629:and
1606:and
1556:and
1394:Vôge
1388:and
1369:and
1344:and
1312:the
1307:and
1221:and
1190:and
660:and
652:and
589:weir
557:and
482:Zorn
416:and
386:and
330:and
255:and
212:The
203:and
109:and
61:Area
41:Peak
2319:to
2105:).
2089:in
2081:in
2069:in
2061:in
1900:Lug
1878:).
1434:or
1328:to
1202:or
390:in
342:to
284:NHN
251:of
105:of
2955::
2726:.
2452:^
2434:^
2413:^
2200:,
2196:,
2184:,
2180:,
2168:,
1957:,
1930:.
1845:,
1805:–
1747:;
1625:,
1602:,
1400:.
1291:,
1284:,
1280:,
1198:,
1102:.
382:,
354:,
313:.
228::
224:,
220::
1695:(
1174:(
579:(
441:(
236:-
216:(
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
