Detecting hydrothermal vents in volcanic lakes

In fact, chemical composition of lake water may indicate inflow of fluids from a volcanic system, but it does not provide spatial information on the location of hydrothermal vents, their abundance and current state of activity.

Changes in the behaviour of hydrothermal vents may be indicative of changes in the volcanic system underneath, thus being a useful precursor for the next generation of early warning systems.

Increased volcanic activity beneath volcanic lakes could also trigger increased gas input, in particular CO2, which could again result in catastrophic gas outbursts as reported from Lake Nyos or Lake Monoun in Cameroon. New exploration approaches will help improving site-specific risk assessment and monitoring concepts by taking a closer look at hydrothermal vents.

The study describes an integrated approach of (1) bathymetry, (2) thermal mapping of the lake floor, and (3) gas emission measurements at the water surface, which was tested successfully at Lake Ngozi in Tanzania. Multiple hydrothermal feed zones could be identified by hole-like structures and increased lake floor temperatures, in combination with increased CO2 emissions from the lake surface.

The developed approach has the advantage that (1) it does not require a complex technical setup, (2) data can be obtained in-situ, and (3) it is transferable to other volcanic lakes for mapping hydrothermal feed sources.

Further research activities at volcanic lakes and in shallow marine environments with hydrothermal activity (e.g., Iceland, Italy) are currently in preparation with partners from the Scientific Diving Centre (SDC) at the Technical University Bergakademie Freiberg, Germany, and the Marine and Freshwater Research Institute in Reykjavik, Iceland. This will also include research related to future offshore geothermal exploration.

Research Report: "Detecting gas-rich hydrothermal vents in Ngozi Crater Lake using integrated exploration tools"