1. The rate of tectonic uplift is directly related to the amount of sediment available and volcanoclastic debris.
  2. Exposed in the middle of the mountain range is an assemblage of deformed andesite to dacite lava flows and volcanoclastic sediments.
  3. The Vizcachera formation which underpins the volcanic field is of Eocene-Miocene age, while the volcanoclastic and sedimentary Filo Blanco sequence was formed 10.8-8.8 mya ago.


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