Sandstone cliff of the Tajo Gorge, formed by the Río Guadalevín. This rock was also used as building material for the more than 100 m high Puente Nuevo (right edge of the photo), having crossed the gorge since 1793 after decades of construction works. This bridge connects different parts of the historic centre of Ronda.

Keywords

bridge, cultural landscape, fluvial erosion, fluvial processes, mirror of the past, palace, sedimentary rocks, traffic, Zonobiome IV

Created

Tuesday 11 February 2020 by Martin Mergili in Europe / Spain (1126 visits)