Galician Massif

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Galician Massif
Macizo Galaico
Manzaneda invierno.jpg
View of Cabeza de Manzaneda in winter
Highest point
Peak Pena Trevinca
Elevation 2,127 m (6,978 ft)
Coordinates 42°14′33″N 6°47′45″W / 42.24250°N 6.79583°W / 42.24250; -6.79583
Geography
Galicia Topo.svg
Topographic map of Galicia
Country Spain
States/Provinces Galicia and Castile and León
Range coordinates 42°30′N 8°06′W / 42.5°N 8.1°W / 42.5; -8.1Coordinates: 42°30′N 8°06′W / 42.5°N 8.1°W / 42.5; -8.1
Geology
Orogeny Variscan orogeny
Period Paleozoic
Type of rock Schist, gneiss and granite

The Galician Massif, Spanish: Macizo Galaico, also known as Macizo Galaico-Leonés, is a system of mountain ranges in the northwestern corner of the Iberian Peninsula. It is located in Galicia with its southeastern end reaching into the provinces of Zamora and León of Castile and León. Its highest point is 2,127 m high Pena Trevinca. Another important peak is Cabeza de Manzaneda (1,781 m).

In traditional local folklore the forests of the Galician System are said to be inhabited by a variety of elves, fairies, ghosts and witches (meigas).

Geography[edit]

Geomorphologically the Galician Massif is a northwestern prolongation of the Meseta Central, the inner Iberian plateau and has great affinity with the geology of the Tras os Montes Portuguese region, so that it is considered as a whole under the name 'Galicia-Trás-os-Montes Zone'.[1] It is composed of Paleozoic materials (granite) with metamorphic rocks such as gneiss, slate and schist in the center and west, which were subject to Alpine folding. Its eastern end merges with the Cantabrian Mountains.[2]

The relief of the system, with an average height of 500 m, is relatively smooth compared with other Iberian ranges. It is however very complex, having no defined structural alignment owing to the heavy fluvial erosion that has fragmented the terrain.

Generally the system includes mountains that are rounded in shape, often topped by small rocky outcrops, as well as horsts, basins and faults, roughly aligned in a N-S direction.

Vegetation[edit]

Since rain is abundant in Galicia, the undisturbed areas of the massif have a soft soil texture and are covered in dense vegetation of temperate deciduous forest where Quercus petraea and Quercus robur oaks predominate. The woods alternate with shrubland and wide natural meadows.[3]

The vegetation is quite homogeneous throughout the massif[4] and there is great plant biodiversity in the Galician mountains. Many of the species found in the mountains were used in Galician traditional medicine.[5]

The Serra dos Ancares was declared a UNESCO Biosphere Reserve in 2006.[6]

Mountain ranges[edit]

From the southeast to the northwest the Galician Massif has three physiographic longitudinal sections:

List of ranges[edit]

Paraño Mountains in Ourense Province seen from N-541 road

Main ranges and features[edit]

Fold formation in Campodola-Leixazos, Serra do Courel, Lugo Province 
Mountain peaks near Verín 
View of Serra do Faro 

See also[edit]

References[edit]

This article incorporates information from this version of the equivalent article on the Galician Wikipedia.

External links[edit]