Perpustakaan Badan Geologi

Kementerian Energi dan Sumber Daya Mineral

  • Beranda
  • Informasi
  • Berita
  • Area Pustakawan
  • Area Anggota
  • Pilih Bahasa :
    Bahasa Arab Bahasa Bengal Bahasa Brazil Portugis Bahasa Inggris Bahasa Spanyol Bahasa Jerman Bahasa Indonesia Bahasa Jepang Bahasa Melayu Bahasa Persia Bahasa Rusia Bahasa Thailand Bahasa Turki Bahasa Urdu

Pencarian berdasarkan :

SEMUA Pengarang Subjek ISBN/ISSN Pencarian Spesifik

Pencarian terakhir:

{{tmpObj[k].text}}

Ditapis dengan

  • Tahun Penerbitan
    -
  • Ketersediaan
  • Lampiran
  • Tipe Koleksi
    Lihat Lebih Banyak
  • Format Fisik Dokumen
    Lihat Lebih Banyak
  • Lokasi
    Lihat Lebih Banyak
  • Bahasa
    Lihat Lebih Banyak
  • Pulau dan Lembar Peta
    Lihat Lebih Banyak
  • Provinsi
    Lihat Lebih Banyak
Ditemukan 173 dari pencarian Anda melalui kata kunci: subject="Merapi"
Hal. Awal Sebelumnya 1 2 3 4 5 Berikutnya Hal. Akhir
cover
Destructions by the Paroxysm of the Merapi Volcano Eruption In 1931
Komentar Bagikan
M. Neumann van Padang

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.

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
23 hlm
Judul Seri
-
No. Panggil
PVG E.33-4
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
Thermal Waters On Ladu's Of Merapi Volcano In 1931
Komentar Bagikan
M. Hartmann

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.

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
3hlm
Judul Seri
-
No. Panggil
PVG E.33-3
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The Debrismasses of Merapi Volcano In 1931-1932
Komentar Bagikan
M. Neumann van Padang

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
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
Directed Shot-Out Wedusgembel at Merapi Volcano, Central Jawa
Komentar Bagikan
J. B. Grandjean

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
Ketersediaan1
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
On Plugforming and The Eruption Character of G. Merapi
Komentar Bagikan

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
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The Old Mantle of G .Merapi(See Plate IIIa and IV)., A Few Considerations On …
Komentar Bagikan
G. L. L. Kemmerling

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
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
Fertility Of The Merapi Products Sand Transportation Of The Neutral Wor…
Komentar Bagikan
G. L. L. Kemmerling

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
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
Wedusgembel Of The Merapi Volcano In 1920
Komentar Bagikan
G. L. L. Kemmerling

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
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
USGS/USAID Suport of the Seismic Program at the Merapi Volcano Observatory, M…
Komentar Bagikan
Robert Y. KoyanagiU. S. Geological SurveyHawaiian Volcano ObservatoryHawaiian National Park, Hawaii 96718

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
Ketersediaan1
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
Penyelidikan Awan Panas dan Lahar 1993 - 1994 Di Lereng Barat Daya G. Merapi
Komentar Bagikan
Kelompok Kerja Geologi/Laharan

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
Ketersediaan1
Tambahkan ke dalam keranjang
Unduh MARCSitasi
Hal. Awal Sebelumnya 1 2 3 4 5 Berikutnya Hal. Akhir
Perpustakaan Badan Geologi
  • Informasi
  • Berita
  • Area Pustakawan
  • Area Anggota

Perpustakaan

  • Pusat Survei Geologi
  • Pusat Vulkanologi dan Mitigasi Bencana Geologi
  • Pusat Sumber Daya Mineral, Batubara dan Panas Bumi
  • Pusat Air Tanah dan Geologi Tata Lingkungan
  • Balai Besar Survei dan Pemetaan Geologi Kelautan
  • Balai Penyelidikan dan Pengembangan Teknologi Kebencanaan Geologi

Cari

masukkan satu atau lebih kata kunci dari judul, pengarang, atau subjek


Badan Geologi - 2026

Kementerian Energi dan Sumber Daya Mineral

Pilih subjek yang menarik bagi Anda
  • Karya Umum
  • Filsafat
  • Agama
  • Ilmu-ilmu Sosial
  • Bahasa
  • Ilmu-ilmu Murni
  • Ilmu-ilmu Terapan
  • Kesenian, Hiburan, dan Olahraga
  • Kesusastraan
  • Geografi dan Sejarah
Icons made by Freepik from www.flaticon.com
Pencarian Spesifik
Kemana ingin Anda bagikan?