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…
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…
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…
Pada tanggal 17 Juni 1981 dengan SPPD No. 677/P/81 dan 678/P/81 Sdr. Effendi dan saya ditugaskan oleh Kepala Seksi Pemetaan Topografi Sub Dit Pemetaan Gunungapi mengadakan pemetaan topografi puncak Gunung Kerinci di Kabupaten Sungai Penuh Provinsi Jambi selama 25 hari.
Gunung Sangeangapi adalah salah satu Gunungapi aktip yang diamati secara terus-menerus dari Kampung Tawali. Pemeriksaan ke puncak/ke Kawah dilakukan sewaktu-waktu, tergantung surat perintah dari Bandung. Letak Gunung Sangeangapi di Pulau Sangeang di sebelah Timur-laut Pulau Sumbawa, dengan jumlah penduduk saat ini 1254 jiwa atau 232 Kepala keluarga, masuk Kecamatan Wera, Kabupaten Bima. Tinggi …
Still a single word on the built up of the volcano as appears from the exposures out side the crater. In all ravines visited by the author, this are the lahar Badak, the lahar Siwalan, the Kali Ijir and the lahar ligobo, the number of lava out flows was not to be called a few. On portrait 17 we see more of such andesite break-through exposed in the ravine of the lahar Ngobo. Remarkable is the f…
Walaupun Gunung Kunyit digolongkan dalam tipe B, tetapi Kasi Pemetaan Topografi menugaskan saya untuk melakukan pengukuran situasi puncak/kawah Gunung Kunyit Kabupaten Sungai Penuh Provinsi Jambi., karena peta yang ada di Perpustakaan iala peta tahun 1925, diperkirakan sekarang telah banyak mengalami perubahan - perubahan.
The active Colo volcano is situated on the island of Una-Una in the Gulf of Gorontalo (0°10'S and 121°35'E). This isolated volcano is located in a peculiar tectonic position, ca 70 km south of the extinct northern volcanic arm of Sulawesi and ca 40 km north of the volcanic extinct Togian Islands. There are two known historic eruptions: 1-2 May 1898 and 23 July 1983. During the latest eruption…
As far as we can conclude from the volcanical history of the G.Kelut, after each out burst a craterlake was formed (Portrait of the Craterlake anong others in 'Geweldige Natuurkrachten' by Vissering in J.v.h. Mijnwezen 1907, Verhandeling Hugo Cool and a.m.). As most of the strate volcanoes has no craterlake there must be extraordinary conditions present, when at such volcano body craterlakes…