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 4 dari pencarian Anda melalui kata kunci: subject="Merapi Vulcano"
cover
The Banjirs at Merapi Volcano In 1931., The Wedusgembel Hazard of Merapi Volcano
Komentar Bagikan
M. Neumann van Padang

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.

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
20 hlm
Judul Seri
-
No. Panggil
PVG E.31-1
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
cover
Characteristics of A Rain - Triggered Lahar In Boyong River, Merapi Volcano, …
Komentar Bagikan
Lahusen RickLavigne FranckDr. Ir, Mas Atje PurbawinataIr. Dewi Sri Sayudi

A rain-triggered lahar occured in K.Boyong (Southern slope of Merapi volcano) on 19 February 1995. This lahar was the biggest in this channel since 22 November, 1994 Merapi eruption which left more than 2 million cubic meters of pyroclastic flow deposits as far as 6 km from the summit.

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
10 hlm
Judul Seri
-
No. Panggil
PVG E.95-19
cover
Analysis of EDM Data In Association With The 1992 Eruption at Merapi Volcano,…
Komentar Bagikan
Ony Kurnia Suganda

The EDM measurement at the summit area of Merapi volcano had been done periodically in 1988, 1990, 1991, and 1992. By using the data of trilateration, horizontal strain components were calculated to evaluate strain pattern changes with time. During the period of 1988 - 1990, seismic and eruptive activities were rather low. In the period of 1990 - 1991, HFA and HFB type earthquakes increased and…

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
16 hlm
Judul Seri
-
No. Panggil
PVG E.92-56