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The Eruptions In Kawah Baru, G.Papandayan In 1924, The Activity In Kawah Nangklak, G.Papandayan, December 1924 March 1925, The Waterlevel In The Craterlets and Waterpools Of The Papandayan
The eruptions, which in the course of 1924 took place in Kavah Baru, were all of relative short duration. In many cases the activity was restricted to the geyserlike spouting-up of mud from one of the crater openings, which in the course of 1923 were born. Sometines also new craterlats were formed, or except mud also stones were ejected. Naturally the gaspressure at lastnaned eruptions was much bigger than at the sud-eruptions. The ejected material consisted except one exception exclusively
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