Topographical Features of Fuerteventura

Central Ridge and Volcanic Formations

Fuerteventura’s landscape is characterized by an elongated central ridge running northeast to southwest, with its highest point at Pico de la Zarza at 28.3577°N, 14.0048°W, with an elevation of 807 meters. This central ridge divides the island into distinct northern and southern regions. The terrain is less rugged compared to other Canary Islands, featuring rolling hills and low volcanic peaks, indicative of ancient volcanic activity and significant erosion over time. The northern slope descends gradually, presenting a smoother landscape, while the southern slope has a more varied terrain influenced by the central ridge’s gradient.

Coastal Periphery and Plain Networks

Fuerteventura’s coastal periphery is defined by extensive plains and sandy beaches, especially on the eastern coast. The western coast features more rugged cliffs and rocky shores. The island’s flat landscape results from prolonged erosion and sediment deposition. The intricate network of plains and minor ravines is more pronounced in the central and southern regions, forming a less complex drainage system compared to other islands in the archipelago. The plains, such as those in the Jandía Peninsula, have fertile soils formed by alluvial deposits, reflecting Fuerteventura’s dynamic geological past. The topographical simplicity, from the central ridge to the coastal edges, makes Fuerteventura a unique geographical entity within the Canary Islands.

Fig1. Illustration of the topography of the island of Fuerteventura.

Fig2. 3D topography rendering of the island of Fuerteventura.