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- Q5535338 subject Q6964962.
- Q5535338 subject Q6977665.
- Q5535338 abstract "Template:SeealsoAndorra is located in the Axial Zone of the central Pyrenees mountain range in south western Europe, which means that it has intensely folded and thrusted rocks formed when the Iberian peninsula was rotated onto the European continent.Rocks from the Cambrian or Ordovician occur in the form of conglomerate, limestone, phyllite, quartzite, and slate. Diapirs of slate from the Silurian Period are found in the Llavirsi syncline near Bixessarri in the south west. Gneiss and schist are found in the cores of anticlines in the north east of the country. This gneiss contains muscovite. The antiforms are connected with near horizontal shear zones, containing nappes of metamorphosed sediments. Younger overlying Paleozoic metamorphosed sediments found over most of Andorra have also been steeply folded.In the south east of the country is an alkaline granite from a batholith called Mt-Louis-Andorra Batholith. It extends into Spain and covers an area of 600 km2 (230 sq mi). Different rock composition zones occur, with monzogranite found at the centre, quartz diorite at the edge and granodiorite in intermediate parts. The batholith has caused metamorphism on its western edge. The base of the batholith is exposed in the east of Andorra.In the Central and Eastern Pyrenees, which includes Andorra, no fossils older than the Ordovician Caradoc 450–460 million years ago have been found.".
- Q5535338 thumbnail Andorra_Geology.PNG?width=300.
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- Q5535338 wikiPageWikiLink Q6964962.
- Q5535338 wikiPageWikiLink Q6977665.
- Q5535338 wikiPageWikiLink Q731880.
- Q5535338 wikiPageWikiLink Q75507.
- Q5535338 wikiPageWikiLink Q79064.
- Q5535338 wikiPageWikiLink Q810808.
- Q5535338 wikiPageWikiLink Q943898.
- Q5535338 type Thing.
- Q5535338 comment "Template:SeealsoAndorra is located in the Axial Zone of the central Pyrenees mountain range in south western Europe, which means that it has intensely folded and thrusted rocks formed when the Iberian peninsula was rotated onto the European continent.Rocks from the Cambrian or Ordovician occur in the form of conglomerate, limestone, phyllite, quartzite, and slate. Diapirs of slate from the Silurian Period are found in the Llavirsi syncline near Bixessarri in the south west.".
- Q5535338 label "Geology of Andorra".
- Q5535338 seeAlso Q740736.
- Q5535338 depiction Andorra_Geology.PNG.