The caldera was at first considered to be large with a centre around, coinciding with the Vilama depression and with vents on the eastern margin beneath the Cerro Caucani, Cerro Solterío, Campanario and Coyaguayma volcanoes, which generate the Abra Granada volcanic complex.
Vents were localized on the eastern margin beneath the Cerro Caucani, Cerro Solterío, Campanario and Coyaguayma volcanoes, which in turn make up the Abra Granada volcanic complex. The caldera was at first considered to be large with a centre around, coinciding with the Vilama depression.
The caldera was at first considered to be large with a centre around, coinciding with the Vilama depression. Vents were localized on the eastern margin beneath the Cerro Caucani, Cerro Solterío, Campanario and Coyaguayma volcanoes, which in turn make up the Abra Granada volcanic complex.
The caldera was at first considered to be large with a centre around, coinciding with the Vilama depression. Vents were localized on the eastern margin beneath the Cerro Caucani, Cerro Solterío, Campanario and Coyaguayma volcanoes, which in turn make up the Abra Granada volcanic complex.