Royal Mount Vema Geological Survey

​Vema Seamount Terrain -  The Vema Seamount summit substrate is rocky, with phonolite outcrops, bedrock of volcanic ash agglomerates, and calcareous accretions. The seamount's plateau-like summit is approximately 14 kilometers in diameter, with the highest peak located on the southern flank of the island. However the mean base diameter of the country is about 60 kilometers.
The Royal Mount Vema Geological Survey was formed by His Majesty King Peter Goldishman in May, 12th 2017, to advance geoscientific knowledge of the Kingdom of Mount Vema by means of systematic surveying, research, monitoring and study Vema Seamount's volcanology, and hazardous, to predict and record eruptive activity, and to mitigate volcanic hazards to life and property.
The RMVGS Observatory advises His Mount Vema Majesty’s Government on all aspects of geoscience, as well as providing impartial advice on geological matters to the public, academics and industry.

The scientific agency employs teams of volcanologists to study and organize frequently underwater visits to Vema Seamount. Although Vema is a dormant volcano, the agency will maintain a close observation.  The major focus is to predict eruptions, as there is currently no accurate way to do this, but predicting it, just like predicting earthquakes, could save many lives.

Open vacancies are available for volcanologists.
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