Roque Cinchado, Rock formation in Teide National Park, Tenerife, Spain
This volcanic rock formation stands approximately 27 meters tall and consists primarily of volcaniclastic sedimentary rocks with lava intrusions strengthening its upper layers against erosion.
The formation developed from remnants of Tenerife's ancient volcanic summit and has been shaped over centuries by natural erosion processes that created its distinctive narrow profile.
The rock formation appeared on Spanish one-thousand peseta banknotes alongside Mount Teide, establishing its status as a recognized symbol of Tenerife and the Canary Islands.
Visitors can access the site via a well-marked hiking trail in Teide National Park, with parking available near Parador Nacional and viewpoints offering close observation opportunities.
The formation's name derives from its constricted middle section, creating a shape that appears pinched or belted, as if tied at its center by natural forces.
Part of: Roques de García
GPS coordinates: 28.22467,-16.63174
Latest update: November 26, 2025 16:08
This collection guides travelers to locations that remain outside mainstream tourism circuits. The selection includes natural sites and cultural places that receive limited visitor attention. These destinations provide opportunities to observe local daily life and regional traditions without commercial tourism infrastructure.
Rock pillars and spires shaped by erosion stand as natural monuments across various locations worldwide. These geological structures, known as hoodoos, display different colors and shapes based on their mineral composition and environmental conditions. From the red rocks of Utah to the limestone formations of Turkey, these sites present geological formations created over millions of years through wind and water erosion. These formations develop through differential erosion, where softer rock layers erode faster than harder layers, leaving slender columns often capped with protective harder rock. Visitors find such structures in desert landscapes, canyons, and plateaus where conditions favor their formation and preservation. The color palette ranges from white to orange, red, and gray, depending on the minerals present such as iron oxide, limestone, or clay.
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