Geomorphology of the Iberian Massif: Relief and Landforms
Relief Units of the Iberian Peninsula
The Iberian Massif Central (The Plateau)
1. The Peneplains
Located in the western peninsula, the peneplains are characterized by:
- Central Granite: Granite outcrops as small balls, becoming altered into highly permeable sandy mantles. Features include V-shaped valleys and granite domes.
- Slate Peneplains: Generally flat areas between 800 and 1000 meters in altitude, decomposed into reddish clay and rubble. These follow SE-NW alignments.
- Zamora Slate: Displays significant erosion in valleys with quartzite crests remaining as highlights.
2. Mountains of Blocks
Formed within the Iberian Massif Central due to the Alpine Orogeny:
- Central System: Divides the Northern and Southern Submeseta.
- Montes de Toledo: Separates the