The Volcanological History of The G.Kelud According To The Existing Literatur…

A few volcanoes of Indonesia posses such a voluminous literature lize the G. Kelut. The are less the volcanic phenomena, than the destructions caused by the mudstreams (lahar), which all times attracked attention. It in true that our through knowledge of out bursts does reach farther than until the begin of the ninetienth century, but the literature of that era is so rich of date, that we howev…

Laporan Pengeboran Air Tanah di Daerah Sulit Air/Desa Tertinggal di Desa Gunu…

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Deskripsi Fisik

iii, 17 hlm.:ill;gbr;tab;lamp

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No. Panggil

PAG L2025-224

Laporan Pengeboran Air Tanah di Daerah Sulit Air/Desa Tertinggal di Desa Tega…

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iii, 18 hlm.:ill;gbr;tab;lamp

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No. Panggil

PAG L2025-223

Laporan Petrokimia Batuan G. Ruang, Sulawesi Utara

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Deskripsi Fisik

14hlm; gbr; tabel

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No. Panggil

PVG S.95-12

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…

Laporan Pengeboran Air Tanah di Daerah Sulit Air/Desa di Kabupaten Tegal, Pro…

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iii, 16 hlm.:ill;gbr;tab;lamp

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No. Panggil

PAG L2025-222

Laporan Pengeboran Air Tanah di Daerah Sulit Air/Desa di Kabupaten Bandung Ba…

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iii, 22 hlm.:ill;gbr;tab;lamp

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No. Panggil

PAG L2025-221

Laporan Penyelidikan Geofisika Terpadu Magnet dan Potensial Diri (SP) G. Loko…

G. Lokon yang terdiri dari Puncak Lokon dan G. Empung merupakan gunung api aktif yang letusannya telah dikenal sebagai eksplosif. Frekuensi letusannya menunjukan peningkatan terhadap selang waktu terjadinya letusan. Hal ini dapat dilihat dari sejarahnya dimana sebelum th.1800 mempunyai selang waktu letusan yang sangat lama (400th), meningkat 2 kali terjadi letusan dalam kurun watu 100 tahun kem…

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…

Laporan Pengeboran Air Tanah di Daerah Sulit Air/Desa di Kabupaten Rembang, P…

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ISBN/ISSN

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Deskripsi Fisik

iv, 24 hlm.:ill;gbr;tab;lamp

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No. Panggil

PAG L2025-220