Scientific paper reveals massive historic Tenerife volcano flank collapse
Last update: October 6, 2011 at 10:57 am by By Armand Vervaeck
Written by Dave Petley
Dave Petley is the Wilson Professor of Hazard and Risk in the Department of Geography at Durham University in the United Kingdom. His blog provides a commentary on landslide events occurring worldwide, including the landslides themselves, latest research, and conferences and meetings.
This post provides a brief review of a new paper that describes a newly discovered catastrophic landslide deposit in Tenerife.
One of the most intriguing but poorly understood landslide types is that of thevolcanic flank collapse. In a volcanic flank collapse, the side of a volcano fails, usually catastrophically, generating a landslide. These slides can be really big – tens or even hundreds of cubic kilometers – and they can travel huge distances along the sea floor. Such failures grabbed attention a few years ago due to the potential (overstated, in my opinion) for generating a catastrophic tsunami.
However, we understand such phenomena really poorly. There are a number of reasons for this, principally that:
a. They occur rarely (globally about one in every 25 years on average), so actually recording one is a challenge
b. the remains tend to lie in a very dispersed state on the floor of the deep ocean. Fieldwork at 4 km water depth remains difficult, even if you are really good at holding your breath.
However, it is one particular aspect of these landslides that remains elusive, but is crucially important. This is the trigger of the collapse event (i.e. of the landslide itself). Numerous mechanisms have been proposed, including sea level change, climate change, hydrothermal pressure, intrusion of volcanic material, and various others. It has proven very difficult to ascertain the importance of each of these. This is an important question if we are to reliably estimate the hazard associated with future potential collapses.
In a paper published in Geology this month, Harris et al. 2011 report a very interesting find on the island of Tenerife, one of the Canary Islands. This is the remains of an ancient collapse event on the south-eastern part of Cañadas volcano. The landslide deposit, which is up to 50 metres thick, has been mapped across a large area – 90 square kilometres – and this is just the onshore component of the mass, which may extend another 50 km offshore. The deposit consists of a classic debris avalanche material, with large (typically up to 12 m long axis), shattered blocks in a highly disrupted, unsorted matrix. This is typical of a highly energetic, very large collapse event. Intriguingly, in the upper part of the deposit some fluviolacustrine (water/lake) sediments are found in the remains of hollows, indicating that in the aftermath of the landslide shallow lakes formed on the surface, presumably as a result of blockages created by the landslide. Associated with the landslide deposit are the remains of pyroclastic flows.