Description
The Sierra Nevada de Mérida, approximately 500 kilometres long, forms the continuation of the Colombian Eastern Cordillera into Venezuelan territory. In its central sections, it consists of gneiss and granite, with young sedimentary rocks overlying both flanks. As a result of significant Tertiary uplift, the central mountain block reaches extraordinary heights. It culminates in the 5,003-metre-high Pico Bolívar, but the peaks of Pico Humboldt (4,942 m) and Pico Bonpland (4,883 m), visible on the right of the picture, are only slightly lower. - Book: Picture 9 - Venezuela - 1977
Description
The Sierra Nevada de Mérida, approximately 500 kilometres long, forms the continuation of the Colombian Eastern Cordillera into Venezuelan territory. In its central sections, it consists of gneiss and granite, with young sedimentary rocks overlying both flanks. As a result of significant Tertiary uplift, the central mountain block reaches extraordinary heights. It culminates in the 5,003-metre-high Pico Bolívar, but the peaks of Pico Humboldt (4,942 m) and Pico Bonpland (4,883 m), visible on the right of the picture, are only slightly lower. - Book: Picture 9 - Venezuela - 1977
