With regard to the earliest times to histories report have received. From the fluent as well an from the positions of both canes follows, that the Malkan or consent said, the mount.
Naar aanleiding van de hooge tamperaturen, die in de eerate helft van Februari 1934 in de Kawah as van den Papandajan sijn gemeten, werd ik op 18 Februari or been gezonden on den toestand na te gaan.
In de Kawah Tjikuloewoeng had vermoedelijk begin Februari een stoomexplosie plaats, waarbij het bosch in westelijke rich-ting tot op 500 m afstand met modder bedekt werd. Een soort-gelijke explosie werd verder bericht van de Kawah Tjibodas einde Mei of begin Juni. In Kawah Tjika loewoeng werden in Februari temperaturen tot 145°, in Juni tot 138° gevonden, terwijl de hoogste temperatuur in Kaw…
Volcanoes with an entirely different character, which frequently caused gigantic destructions, are those which outbursts wen acampamied by wedusgembel.
Ten einde een juiste beeld te krijgen van werkingvan den Semerce is de onderstaande, lijst en grafiek (Plaat ) samengesteld uit de geschriften welke ter be-schikking staan. Daaruit blijkt niet, dat de vulkaan voort-durend gewekt heeft, wel echter dat hij herhaaldelijk uitbars-tingen heeft vertoond. Zeer zeker is de lijst onvolledig en de eruptieve werking telkens van langer duur geweest, dan hi…
After the volcanic destruction in 1931 the W foot of the mountain was harassed by heavy banjirs, which beat in pieces the bridges and covered fields with sand. The banjir problem of the Merapi was studied in detail by K.G.R. Schmidt, a separate detailed report about this is in preparation by him.
A good 20 km2 terrain, with 13 kampungs completely and 20 kampungs has partly destroyed by the big eruptions of December 18 and 19, 1930, causing 1369 men and a good 2100 big cattle killed and more than 1100 house lost.
After the December eruption 1930, the laducourses of Merapi Volcano, Central Java previously showed no water circulation, expect at big rainfall, which caused shorthliving banjirs.
The ladumasses were deeper cut in the course of the mouths and it appears always clearer, that they were built of a heterogen, lightbrown colored sand mass, where in-between irregularly scattered, the stones occurred as individuals or as bouldertrails.
Almost all authors are the opinion, that the well - known wedusgembel, which caused death and destruction on the western slope of the Merapi, originated from the hot lava avalanches (glowing avalanches), which rolled down along the slides, whereas 'shout-out' wedusgmbel have not taken place.