Damage occurred from landsliding and mass movement on the steep slopes of terraces and from subsidence and inundation in the swampy central zone of Llanquihue. Large structures located on well-drained terraces were undamaged. The glacial history of Lake Llanquihue is discussed.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.