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White-washed hermitage built into tan rocky hillside with sparse vegetation and barren mountains in background

Barranco de las Peñitas
— Volcanic Ravine in Fuerteventura’s Central Highlands

Canarina / CC BY-SA 3.0 — via Wikimedia Commons
🧭 Overview

Barranco de las Peñitas is a volcanic ravine in Fuerteventura’s central highlands, known for its steep rock formations, narrow valley floor and dry inland terrain. Its dramatic geology makes it one of the island’s most distinctive inland landscapes.

Barranco de las Peñitas lies south of Betancuria, a narrow volcanic ravine shaped by steep cliffs, dry slopes and erosion patterns typical of Fuerteventura’s central highlands. The ravine forms one of the most dramatic inland landscapes on the island, with exposed rock walls rising sharply above the valley floor.

The terrain consists of rugged volcanic formations, scattered vegetation and terraced ground adapted to the highland climate. The ravine’s narrow profile creates a strong contrast with the softer valley terrain of nearby Vega de Río Palmas.

Walking routes follow the ravine toward Embalse de las Peñitas, a small reservoir set within the same geological system. The combination of water, volcanic cliffs and dry highland terrain gives the area a unique inland character.

Barranco de las Peñitas forms part of the broader inland route connecting Betancuria, Vega de Río Palmas and the western highlands near Ajuy. Its dramatic geology and quiet atmosphere make it one of Fuerteventura’s most distinctive inland features.

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