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Roussillon to the north and the plan of Empordà to the south. The mountains on the right side of the Tech, to the west, the boundary is uncertain and almost impossible to determine. To the south, the Cap de Creus massif is sometimes considered to be part of the Albères. It culminates at 1,256 meters above sea level, at Puig Neulós.
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The Albères massif is located at the eastern end of the axial zone of the
Pyrenees mountain range. This area is mainly made up of Paleozoic and older formations (dating from around 550 millions of years to around 300 millions of years) which outcrop in a broader range, running from west to east, from
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On its northern slope, the Albères fault (which extends approximately from west to east from around Le Boulou to around Argelès) marks a clear geological and topographical limit between the
Paleozoic and older formations of the Massif des Albères and the Neogene deposits of the Roussillon basin.
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The summit ridge of the Albères helps making the demarcation of the border between France and Spain. Thus, the massif is geographically part of the
Pyrenees. Administratively, it is located in the department of Pyrénées-Orientales in France, and in the province of Girona in Catalonia (Spain).
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The Albères massif is bounded to the west by the Col du
Perthus and the Rome river, which separate it from the Salines massif, to the east by the Mediterranean Sea between Argelès-sur-Mer in France and Port-Bou and Llançà in Spain. The Albères dominate the lower Tech valley and the plain of
502:". However, this explanation is considered unsatisfactory because the massif is not white in color. Rarely snow-covered, it likely did not show white rocks in the Middle Ages, as it was covered with forests. It could also come from
533:, used for a rounded, lower relief covered with bushes, as seen in the region in names such as the commune Corbère-les-Cabanes or the Corbières massif. This hypothesis aligns with the layout of the places in question.
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The Tour
Madeloc ridge, at the eastern end of the Albères (Albera) massif. The ridge is situated on a zone consisting of fine-grained sandstones of volcanosedimentary origin ("Grès de la Tour Madeloc").
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In the Albères massif, the two main groups of formations are metamorphosed formations of sedimentary origin (notably schists), and formations of plutonic origin (mainly granites and gneisses).
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and in the plural in French. Thus, in French, the expression "les Albères" refers to the massif, while L'Albère is the name of a French commune located within this massif.
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Of mainly siliceous geological origin, this massif produces acidic soils; hence the presence of maquis and not scrubland (present on limestone soils).
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The name first appeared in Latin in 844 in a text by the future
Emperor Charles the Bald, which mentions a place located
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On the northern slopes of the massif, the Albères fault (which runs roughly west to east from near
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mountain range. As in most of that zone, the geological formations in the massif are mostly of
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Paratge
Natural d'Interès Nacional de l'Albera. Col·lecció 1:25.000. Espais naturals protegits
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the Hautes-Pyrénées to the
Canigou massif and the Vermeille coast, passing through Andorra.
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is problematic due to a lack of ancient documents (the earliest being dated to the
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century) and because several very common roots seem to correspond with the name.
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Notice explicative de la feuille Argelès-sur-Mer - Cerbère (1097) à 1/50 000
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would designate a steep, high mountain but rich in pasture, in contrast to
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The Albera Range became the border between France and Spain following the
879:, Springer International Publishing, Kindle edition, 2022, pages 314-333.
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have just labeled this article as needing attention, please add
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Marc Calvet, Magali Delmas, Yanni
Gunnell, Bernard Laumonier,
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Northeastern Spain and
Southern France Mediterranean forests
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Puig de Sant Cristau, towards the western end of the massif.
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The massif is at the eastern end of the "Axial Zone" of the
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Knowledge (XXG):Pages needing translation into English
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One popular hypothesis is that it may derive from the
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Most of the southern side of the range is part of the
824:, Barcelona, Institut CartogrĂ fic de Catalunya, 1999
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513:Lluis Basseda favors another hypothesis: the root
245:. It is the main easternmost prolongation of the
33:The northern side of the Albera Massif seen from
510:found in many mountain names in Western Europe.
517:followed either by the Latin collective suffix
912:Centre de reproducciĂł de tortugues de l'Albera
893:Paratge Natural d'Interès Nacional de l'Albera
877:Geology and Landscapes of the Eastern Pyrenees
258:Paratge Natural d'Interès Nacional de l'Albera
737:Puig Sallfort seen from the Tour de Querroig.
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268:marks the western boundary of the massif.
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460:Learn how and when to remove this message
260:natural reserve. There are some ancient
905:50 ascensions fĂ cils pel Pirineu catalĂ
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350:ceded a part of the Spanish kingdom to
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898:Requesens - Puig NeulĂłs hiking route
398:adding citations to reliable sources
295:) being the predominant formations.
16:Mountain range in France and Spain
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127:Location in the Pre-Pyrenees area
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521:or the Iberian-Basque suffix
927:Mountain ranges of Catalonia
323:Lac de Villeneuve-de-la-Raho
52:1,256 m (4,121 ft)
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472:The etymology of the word
249:. Its highest peak is the
907:, Valls, CossetĂ nia, 2008
806:Topographical map extract
321:The massif seen from the
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903:Manel Figuera i Abadal,
229:located in the south of
761:Granite outcrop, above
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279:and earlier ages, with
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782:Mountains of Catalonia
777:Treaty of the Pyrenees
344:Treaty of the Pyrenees
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35:Sant GenĂs de Fontanes
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394:improve this article
360:Historical Catalonia
80:42.48194°N 2.94694°E
352:Louis XIV of France
231:Pyrénées-Orientales
141:Pyrénées-Orientales
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356:Northern Catalonia
348:Philip IV of Spain
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42:Highest point
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187:Easiest route
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392:Please help
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176:First ascent
157:Parent range
763:La Jonquera
725:Puig NeulĂłs
609:section on
581:"languages"
571:from French
569:translation
525:. The term
498:, meaning "
354:, dividing
291:(and other
251:Puig NeulĂłs
194:La Jonquera
83: /
58:Coordinates
921:Categories
849:GĂ©oportail
810:GĂ©oportail
793:References
632:Topography
420:newspapers
312:Roussillon
237:, between
68:42°28′55″N
620:July 2024
548:Geography
450:July 2024
300:Le Boulou
277:Paleozoic
262:megaliths
235:Catalonia
149:Catalonia
96:Geography
71:2°56′49″E
48:Elevation
932:Pyrenees
771:See also
607:WP:PNTCU
366:Toponymy
302:to near
273:Pyrenees
247:Pyrenees
170:Climbing
164:Pyrenees
137:Location
664:Gallery
645:Geology
531:Corbera
488:Albaria
474:Albères
434:scholar
346:, when
338:History
314:basin.
308:Neogene
304:Argelès
289:schists
281:granite
225:) is a
211:Catalan
180:Unknown
145:EmpordĂ
583:list.
542:Albera
527:Albera
436:
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287:, and
285:gneiss
239:France
219:French
198:Sureda
523:-erri
519:-aria
500:white
496:albus
492:-aria
485:Latin
441:JSTOR
427:books
358:from
243:Spain
192:From
847:(in
808:(in
601:~~~~
504:alba
413:news
241:and
205:The
588:you
586:If
515:Alp
508:Alp
396:by
196:or
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856:^
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