ANDEAN GEOSYNCLINE

a linear trough in the Earth's crust in which rocks of the Mesozoic Era (245 to 66.4 million years ago) and Cenozoic Era (66.4 years ago to the present) were deposited in South America. An intense orogenic (mountain-building) event affected the older sediments in the geosyncline in the Late Cretaceous Epoch (97.5 to 66.4 million years ago) and, combined with later deformational episodes, produced a pattern of scattered marine deposition in basins along the western margin of the geosyncline. The total area of deposition was great enough for some geosynclinal segments to be separately namede.g., the Venezuelan-Peruvian Geosyncline. The rising highland belts provided much coarse sediment, and thicknesses as great as 6,080 m (20,000 feet) are known from early Cenozoic sequences. During middle Cenozoic time, another orogenic phase occurred, accompanied by widespread volcanism. A complex history of intermittent uplift, block faulting, and erosion in late Cenozoic time led to a series of extensive uplifted erosion surfaces in Peru, Bolivia, and elsewhere. Uplift continued through the late Pleistocene Epoch (1,600,000 to 10,000 years ago), giving rise to the present configuration of the Andes. Elevations of 4,600 m (15,200 feet) are widespread, and many peaks attain 6,000 m (19,800 feet) or more.