"Sulfur dioxide (SO2) is one of the main gases emitted from volcanic eruptions. It’s poisonous with an irritating, pungent, and rotten smell. Inhalation can cause breathing difficulty, disease, and premature death. When released from volcanic eruptions it poses a hazard to people, animals, and vegetation. Local to the eruption it can cause acid rain and air pollution. If large volumes of sulphur dioxide aerosols are injected into the stratosphere it can deplete the earth’s ozone layer and lower surface temperatures.
Komatiites are submarine lavas that erupted at high temperature (1600°C compared with 1100 to 1250°C for basalt lavas). Thus, they were extremely fluid, and flowed rapidly like water across the surface, compare with basaltic lava, which flows like honey. Komatiite was named after the Komati River in South Africa, which is its type locality.
Like basaltic lava, komatiite lava originated when part of the mantle rock inside the earth melted. The difference between komatiite and basalt is that, because of the higher temperatures involved, a greater proportion (around 50%) of the mantle rock melted producing the komatiite lava. As a result komatiites are rich in magnesium oxide (MgO).
The Archean is regarded as the period from 2.5 billion to 4.0 billion years ago, within the evolutionary, long-age paradigm. Komatiites are mainly restricted to rocks of Archean ‘age’. Within evolutionary thinking, the restriction to the Archean is explained as:
From the abstract of Prof Fiorentini’s lecture we read:
Komatiites are submarine lavas that erupted at high temperature (1600°C compared with 1100 to 1250°C for basalt lavas). Thus, they were extremely fluid, and flowed rapidly like water across the surface, compare with basaltic lava, which flows like honey. Komatiite was named after the Komati River in South Africa, which is its type locality.
Like basaltic lava, komatiite lava originated when part of the mantle rock inside the earth melted. The difference between komatiite and basalt is that, because of the higher temperatures involved, a greater proportion (around 50%) of the mantle rock melted producing the komatiite lava. As a result komatiites are rich in magnesium oxide (MgO).
The Archean is regarded as the period from 2.5 billion to 4.0 billion years ago, within the evolutionary, long-age paradigm. Komatiites are mainly restricted to rocks of Archean ‘age’. Within evolutionary thinking, the restriction to the Archean is explained as:
- the early earth having a much higher temperature due to residual heat after the planet supposedly accreted, and
- a greater heat production due to more radioactive elements in the mantle.
From the abstract of Prof Fiorentini’s lecture we read:
Komatiites are ancient submarine lavas that erupted over 2.5 billion years ago. These hot and highly turbulent flows entrained discrete sulfide liquids that concentrated nickel, copper and the platinum group elements locally to economic proportions. … measurements on sulfides from komatiites and local volcanogenic and sedimentary country rocks indicate that sulfur degassing during volcanism may have played a key role in the mineralizing process. … pervasive (>90%) sulfur loss from sulfide-saturated komatiite lavas, dominantly in the form of SO2 gas. This … had the potential to influence the geochemical evolution of the atmosphere and ocean on Archean Earth. Rapid sulfur degassing
associated with such voluminous and cataclysmic eruptions was most likely a contributing factor for economic mineralization.
*Notice the komatiite lavas are described as “hot and highly turbulent”, and as erupting under water. *Notice too that the volcanic eruptions are pictured as “voluminous and cataclysmic”, which is much more dramatic than the volcanic eruptions that are occurring today.
*And finally, the abstract says that the sulphur gasses released had the potential to significantly alter the atmosphere.
associated with such voluminous and cataclysmic eruptions was most likely a contributing factor for economic mineralization.
*Notice the komatiite lavas are described as “hot and highly turbulent”, and as erupting under water. *Notice too that the volcanic eruptions are pictured as “voluminous and cataclysmic”, which is much more dramatic than the volcanic eruptions that are occurring today.
*And finally, the abstract says that the sulphur gasses released had the potential to significantly alter the atmosphere.