West Quartzite Range [SEP] continent
West Quartzite Range
West Quartzite Range () is a mountain range, the western of two parallel quartzite ranges, situated at the east side of Houliston Glacier in the Concord Mountains, Antarctica. Named by the Northern Party of NZFMCAE, 1962–63, after the distinctive geological formation of the feature.
Geology of Andorra
Andorra 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.
Overview.
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