Ditapis dengan
Volcanic Outbursts Accompannied by Wedus Gembel
Volcanoes with an entirely different character, which frequently caused gigantic destructions, are those which outbursts wen acampamied by wedusgembel.
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- ISBN/ISSN
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- Deskripsi Fisik
- 11 hlm
- Judul Seri
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- No. Panggil
- PVG E.33-5
Semeroe De Werking Van Den Semeroe En De Verplaatsing Van Zyn Krater
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…
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- ISBN/ISSN
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- Deskripsi Fisik
- 20 hml.; gmbr,; peta
- Judul Seri
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- No. Panggil
- PVG E.35-3
The Banjirs at Merapi Volcano In 1931., The Wedusgembel Hazard of Merapi Volcano
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.
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- ISBN/ISSN
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- 20 hlm
- Judul Seri
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- No. Panggil
- PVG E.31-1
Destructions by the Paroxysm of the Merapi Volcano Eruption In 1931
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.
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- ISBN/ISSN
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- Deskripsi Fisik
- 23 hlm
- Judul Seri
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- No. Panggil
- PVG E.33-4
Thermal Waters On Ladu's Of Merapi Volcano In 1931
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.
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- Deskripsi Fisik
- 3hlm
- Judul Seri
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- No. Panggil
- PVG E.33-3
The Debrismasses of Merapi Volcano In 1931-1932
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.
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- 4 hlm
- Judul Seri
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- No. Panggil
- PVG E.33-2
Directed Shot-Out Wedusgembel at Merapi Volcano, Central Jawa
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.
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- Deskripsi Fisik
- 9 hlm
- Judul Seri
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- No. Panggil
- PVG E.31-2
Laporan Lapangan Penjajakan Pengukuran Kubah Lava Baru G.Semeru, Dalam Rangka…
Pengukuran kubah lava ini bertujuan untuk mengetahui volum pen-dekatan. Penulis memberi istilah volum pendekatan disini, karena berdasarkan atas sifat pengukuran pengukurannya, antara lain s a. pengukuran puncak kubah lava baru dengan cara aanpeilingen" jarak jauh dari dua titik totap (titik pengamatan) G. Sasur dan Sumberbulus (PANDI. K., 1977). b. disesuaikan dengan seket dari potret ba…
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- ISBN/ISSN
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- Deskripsi Fisik
- 9 hml.; gmbr.; tabel
- Judul Seri
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- No. Panggil
- PVG E.78-17
Temperature Observations at Papandayan Volcano, Extension and Intersity Of Th…
As mentioned, during the observation, extensive temperature observations were carried out. From this on the first place appeared, that within the crater groups of solfatara's and hot springs can be distinguished, which temperature strongly varied. The distribution of the temperatures is for a fixed day (September 2, 1924) given on Plate II. We see from this, that the highest temperature occurre…
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- ISBN/ISSN
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- Deskripsi Fisik
- 14 hml
- Judul Seri
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- No. Panggil
- PVG E.25-1
The G. Lamongan in 1924
The crater of the Lamongan vas visited for the last time in July 1925. Although since that tine no reports on abnornal phenomena were received, the crater was again reconnoitred at the beginning of February 1924, as we must be always on our alert, that the rostful situation of these previously so active volcano suddenly might change.
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- Deskripsi Fisik
- 7 hml.; tabel
- Judul Seri
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- No. Panggil
- PVG E.24-3
Karya Umum 
Filsafat 
Agama 
Ilmu-ilmu Sosial 
Bahasa 
Ilmu-ilmu Murni 
Ilmu-ilmu Terapan 
Kesenian, Hiburan, dan Olahraga 
Kesusastraan 
Geografi dan Sejarah