Drumming Spring


The effect of the Drumming Spring which was heard before it was seen is due to the intense magma activities of the undersurface fault under whose high temperature and pressure the mixed gas and water eager to find the exit which was blocked by a boulder, and finally spout out from a fissure about 0.2 m long and 0.05 m wide. From here, you can listen to the sound of war drums from the depths of the earth, the stampeding of thousands of horses, as if you were in the midst of a fierce battle. This spring has a temperaure of 96℃, a pH value of 9.9, and a flow rate of 1.19 L/S, topping the water flow of the whole Themal Sea.

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