The Albera Massif (; ) is a
mountain range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have aris ...
located in the south of
Pyrénées-Orientales
Pyrénées-Orientales (; ; ; ), also known as Northern Catalonia, is a departments of France, department of the Regions of France, region of Occitania (administrative region), Occitania, Southern France, adjacent to the northern Spain, Spanish ...
and the north of
Catalonia
Catalonia is an autonomous community of Spain, designated as a ''nationalities and regions of Spain, nationality'' by its Statute of Autonomy of Catalonia of 2006, Statute of Autonomy. Most of its territory (except the Val d'Aran) is situate ...
, between
France
France, officially the French Republic, is a country located primarily in Western Europe. Overseas France, Its overseas regions and territories include French Guiana in South America, Saint Pierre and Miquelon in the Atlantic Ocean#North Atlan ...
and
Spain
Spain, or the Kingdom of Spain, is a country in Southern Europe, Southern and Western Europe with territories in North Africa. Featuring the Punta de Tarifa, southernmost point of continental Europe, it is the largest country in Southern Eur ...
. It is the main easternmost prolongation of the
Pyrenees
The Pyrenees are a mountain range straddling the border of France and Spain. They extend nearly from their union with the Cantabrian Mountains to Cap de Creus on the Mediterranean coast, reaching a maximum elevation of at the peak of Aneto. ...
. Its highest peak is the
Puig Neulós
Puig Neulós () is the highest mountain of Albera Range, an eastern prolongation of the Pyrenees in Catalonia, between France and Spain. It has an elevation of 1,256 metres above sea level.
There are some antennas on the summit and there is a pav ...
, with an elevation of 1,256 metres.
Most of the southern side of the range is part of the Paratge Natural d'Interès Nacional de l'Albera natural reserve. There are some ancient
megalith
A megalith is a large stone that has been used to construct a prehistoric structure or monument, either alone or together with other stones. More than 35,000 megalithic structures have been identified across Europe, ranging geographically f ...
s in the range. The
Col du Perthus marks the western boundary of the massif.
The massif is at the eastern end of the "Axial Zone" of the
Pyrenees
The Pyrenees are a mountain range straddling the border of France and Spain. They extend nearly from their union with the Cantabrian Mountains to Cap de Creus on the Mediterranean coast, reaching a maximum elevation of at the peak of Aneto. ...
mountain range. As in most of that zone, the geological formations in the massif are mostly of
Paleozoic
The Paleozoic ( , , ; or Palaeozoic) Era is the first of three Era (geology), geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma a ...
and earlier ages, with
granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly coo ...
,
gneiss
Gneiss (pronounced ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. This rock is formed under p ...
, and
schist
Schist ( ) is a medium-grained metamorphic rock generally derived from fine-grained sedimentary rock, like shale. It shows pronounced ''schistosity'' (named for the rock). This means that the rock is composed of mineral grains easily seen with a l ...
s (and other
metasediments) being the predominant formations.
[Notice explicative de la feuille Argelès-sur-Mer - Cerbère (1097) à 1/50 000](_blank)
BRGM Éditions, Orléans, 2015.
On the northern slopes of the massif, the Albères fault (which runs roughly west to east from near
Le Boulou to near
Argelès) marks a clear geological and topographical boundary between the Palaeozoic and older formations of the Albera massif and the
Neogene
The Neogene ( ,) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period million years ago. It is the second period of th ...
deposits of the
Roussillon
Roussillon ( , , ; , ; ) was a historical province of France that largely corresponded to the County of Roussillon and French Cerdagne, part of the County of Cerdagne of the former Principality of Catalonia. It is part of the region of ' ...
basin.
[Marc Calvet, Magali Delmas, Yanni Gunnell, Bernard Laumonier, ''Geology and Landscapes of the Eastern Pyrenees'', Springer International Publishing, Kindle edition, 2022, pages 314-333.]
History
The Albera Range became the border between France and Spain following the
Treaty of the Pyrenees
The Treaty of the Pyrenees(; ; ) was signed on 7 November 1659 and ended the Franco-Spanish War that had begun in 1635.
Negotiations were conducted and the treaty was signed on Pheasant Island, situated in the middle of the Bidasoa River on ...
, when
Philip IV of Spain
Philip IV (, ; 8 April 160517 September 1665), also called the Planet King (Spanish: ''Rey Planeta''), was King of Spain from 1621 to his death and (as Philip III) King of Portugal from 1621 to 1640. Philip is remembered for his patronage of the ...
ceded a part of the Spanish kingdom to
Louis XIV of France
LouisXIV (Louis-Dieudonné; 5 September 16381 September 1715), also known as Louis the Great () or the Sun King (), was King of France from 1643 until his death in 1715. His verified reign of 72 years and 110 days is the List of longest-reign ...
, dividing
Northern Catalonia
Northern Catalonia, North Catalonia or French Catalonia is the Catalan language, Catalan-speaking and cultural territory ceded to France by Spain through the signing of the Treaty of the Pyrenees in 1659 in exchange for France's effective renu ...
from
Historical Catalonia.
Toponymy
The etymology of the word ''Albères'' is largely unknown due to a lack of documentation (the earliest being dated to the
9th century) and because several very common roots seem to correspond with the name.
One of the more notable proposed hypotheses is that it may derive from the
Latin
Latin ( or ) is a classical language belonging to the Italic languages, Italic branch of the Indo-European languages. Latin was originally spoken by the Latins (Italic tribe), Latins in Latium (now known as Lazio), the lower Tiber area aroun ...
''Albaria'' by adding the collective suffix ''-aria'' to the adjective ''albus'', meaning "
white
White is the lightest color and is achromatic (having no chroma). It is the color of objects such as snow, chalk, and milk, and is the opposite of black. White objects fully (or almost fully) reflect and scatter all the visible wa ...
". However, this explanation is considered unreliable 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 ''alba'', dawn, because it is the easternmost of the Pyrenees, or from the pre-Latin root ''Alp'' found in many mountain names in Western Europe.
Lluis Basseda favors another hypothesis: the root ''Alp'' followed either by the Latin collective suffix ''-aria'' or the Iberian-Basque suffix ''-erri''. The term ''Albera'' would designate a steep, high mountain but rich in pasture, in contrast to ''Corbera'', 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.
The name first appeared in Latin in 844 in a text by the future Emperor Charles the Bald, which mentions a place located ''in monte Albario''. The term is found interchangeably in the singular or plural during the Middle Ages. It eventually became fixed in the singular in Catalan as ''Albera'' 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.
Geography
Topography
The Albères massif is bounded to the west by the Col du Perthus and the Rome river, which separates 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 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.
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).
Geology
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 the Hautes-Pyrénées to the Canigou massif and the Vermeille coast, passing through Andorra.
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).
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.
Of mainly siliceous geological origin, this massif produces acidic soils; hence the presence of maquis and not scrubland (present on limestone soils).
Gallery
Massís de l'Albera (Alt Empordà) - 4.jpg, Albera Massif
Massís de l'Albera (Alt Empordà) - 2.jpg, Albera Massif
Massís de l'Albera (Alt Empordà) - 3.jpg, Albera Massif
Massís de l'Albera (Alt Empordà) - 1.jpg, Albera Massif
Pic Neulós Albères.jpg, Puig Neulós
Puig Sallfort depuis la tour de Querroig 2.jpg, Puig Sallfort seen from the Tour de Querroig.
Sant Cristau côté sud.jpg, Puig de Sant Cristau, towards the western end of the massif.
Formation granitique La Jonquera.jpg, Granite outcrop, above La Jonquera
La Jonquera (; ) is a municipality in the ''Comarques of Catalonia, comarca'' of Alt Empordà, l'Alt Empordà, in Catalonia, Spain. It is situated next to the border with Northern Catalonia, nowadays France, opposite the municipality of Le Perthu ...
.
See also
*
Treaty of the Pyrenees
The Treaty of the Pyrenees(; ; ) was signed on 7 November 1659 and ended the Franco-Spanish War that had begun in 1635.
Negotiations were conducted and the treaty was signed on Pheasant Island, situated in the middle of the Bidasoa River on ...
*
Mountains of Catalonia
This is a list of mountains in Catalonia, Spain.
See also
*Montserrat (mountain), Montserrat
*List of mountains in Aragon
References
{{DEFAULTSORT:Mountains Of Catalonia
Lists of mountains of Spain, Catalonia
Mountains ...
*
Coll de Banyuls
References
External links
Paratge Natural d'Interès Nacional de l'AlberaRequesens - Puig Neulós hiking routeManel Figuera i Abadal, ''50 ascensions fàcils pel Pirineu català'', Valls, Cossetània, 2008Centre de reproducció de tortugues de l'Albera
{{Authority control
Mountain ranges of Catalonia
Pyrenees
Northeastern Spain and Southern France Mediterranean forests