Ditapis dengan
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.
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 4 hlm
- Judul Seri
- -
- 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.
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 9 hlm
- Judul Seri
- -
- No. Panggil
- PVG E.31-2
On Plugforming and The Eruption Character of G. Merapi
The summit of G. Merapi is formed by a lava-plug; a cratershaped decline, such as the most volcanoes possess, is not present. However it is known,-thanks to the many interest, with which the G. Herapi in the pant century obtained, that the volcano in another stage of eruptive activity certainly owed such a cratershaped decline.
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 10 hml
- Judul Seri
- -
- No. Panggil
- PVG E.21-7
The Old Mantle of G .Merapi(See Plate IIIa and IV)., A Few Considerations On …
As already earlier mentioned the G. Herapi exists of two morphologic clearly to be distinguished parts, an older eastern and a younger western part. From the sunnit of the old ringdike, only a small part remains (see portrait 14), of which the eastern part is named G. Pusunglondon (2694.3 a.s.) and the northern G. Paseban (2679= a.s.). The old volcano mantle of the G. Merapi has grown much more…
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 9 hml.; tabel
- Judul Seri
- -
- No. Panggil
- PVG E.21-6
Fertility Of The Merapi Products Sand Transportation Of The Neutral Wor…
The spreading of the Herapi products is of a great agrogeologic Importance, as the Merapi products compared with the rocks of other Java volcanoes are extraordinary fosforrich. Only towards one side these products could develop feely, namely in the plane of Solo, whare they border to that of the Lavu. To the S the spreading was stopped by the southern mountains, only in the area of the kali Opa…
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 5 hml
- Judul Seri
- -
- No. Panggil
- PVG E.21-5
Wedusgembel Of The Merapi Volcano In 1920
On October 12, 1920 the inhabitants of the most high laying kampungs in the vicinity of the Blongkengravine were surprised by hot dustclouds and were killed by the burns. It appeared inmediately, that there was no outburst at all, as the summit slopes of the Merapi were, as far as they were overgrown in August and September, were still green as before (the reports from news papers concerning th…
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 9 hml
- Judul Seri
- -
- No. Panggil
- PVG E.21-3
USGS/USAID Suport of the Seismic Program at the Merapi Volcano Observatory, M…
The purpose of this assignment wa to provvide support to the seissmic program at the Merapi Vulcano Observatory (MVO) of the Vulcanological Survey of Indonesia (VSI). Instrument maintenance and data analysis support were provided for by Bruce Furukawa and Bob Koyanagi between 13 to 24 May; additional assistance in instrument maintenance was provi MVO ed by Furukawa from 25cMay to 9June. Logisti…
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 22hlm
- Judul Seri
- -
- No. Panggil
- PVG E.88-15
Penyelidikan Awan Panas dan Lahar 1993 - 1994 Di Lereng Barat Daya G. Merapi
Penyelidikan geologi dan laharan yang dilakukan di lereng Baratdaya G.Merapi yang meliputi K. Senowo, K.Sat, K. Bebeng dan K.Krasak dimaksudkan untuk mengevaluasi sebaran awan panas dan lahar 1993 - 1994 serta endapan sebelumnya yang diperkirakan terjadi pada bulan Agustus 1993 - Mei 1994.
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 14 hlm
- Judul Seri
- -
- No. Panggil
- PVG E.94-38
Laporan Kegiatan Gunung Merapi April - Juni 1999
Status aktivitas G. Merapi pada triwulan I (April - Juni 1999) berada pada status "aktif normal" yang berlaku sejak pertengahan bulan Januari 1999, secara visual tercermin dengan asap solfatar berwarna putih tebal, tekanan lemah, tinggi asap maksimum berkisar antara 100 - 600 meter, kecuali pada tgl 11 Juni 1999 tinggi asap maksimum mencapai 1000 meter terukur dari Pos Pengamatan Selo pada jam …
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 16 hlm
- Judul Seri
- -
- No. Panggil
- PVG E.99-27
Studi Deformasi Di G. Merapi
Pemahaman fenomena - fenomena magmatik dan pengawasan gunung - gunung api tidak bisa terlepas dari studi deformasi. Di G.Merapi, gunungapi tipe strato dan kubah lava, yang aktivitasnya tidak berhenti sejak tahun 1992, sehingga dilakukan pengukuran tahunan jaringan GPS sejak bulan Sepetember 1993.
- Edisi
- -
- ISBN/ISSN
- -
- Deskripsi Fisik
- 26 hlm
- Judul Seri
- -
- No. Panggil
- PVG E.97-4
Karya Umum 
Filsafat 
Agama 
Ilmu-ilmu Sosial 
Bahasa 
Ilmu-ilmu Murni 
Ilmu-ilmu Terapan 
Kesenian, Hiburan, dan Olahraga 
Kesusastraan 
Geografi dan Sejarah