The Core Region of the Tsloch Sea had water reaching a depth of 18 kilometres. The sea bed was ripe with volcanic activity, constantly releasing lava into the sea water.
As the lava cooled down, more spurted out from the pressure vents, resulting in the formation of a series of underwater mountain ranges.
Towards the surface, floating around like they were ships were mountains, each reaching a height of two kilometres on average. Their base had been expanded to resemble ice bergs in terms of structure, providing stability.
The volcanic activity at the sea bed released heavy amounts of minerals into the water, which were carried by water currents reaching the top. These currents congregated under the mountains, increasing the water density at the area in comparison to the rest of the sea region.
The higher water density increased the stability of the mountain structure. And that's how the series of mountains floated around.
