The most remarkable phenomenon, which is observed at the Lamongan, which apart from it, in whole Jawa is never seen at no single volcano, is the amount of small lakes which are situated on several distances from each other, but are surrounding the cone volcano in a line following each other in a wide circle.
Atas perintah Sdr. Kepala Urusan Gn. Api dan jang telah disetudjui oleh Sdr. Kep. Djawatan Geologi, maka pada tg. 11 Djan. 1954, kami brangkat dari Bandung menudju ke Gn. Semeru, untuk mendjalankan tugas jang lamanja 2 bulan, akan tetapi berhubung jang mengaplos telat datangnja, karena ada sesuatu hal maka tugas kami diperpandjang 1 bulan lagi. Pengawasan Gn. Semeru dari Pos Bs. Sat, Gn. Saw…
Atas perintah Sdr. Kepala Urusan Gunung Berapi disetujui oleh Kepala Djawatan Geologi, maka kami dengan Sdr. Rd. Suwignjo, berangkat pada tanggal 4/9-53 dari Bandung -Yogyakarta. Di Yogyakarta mengambil tempo satu hari, guna membereskan tugas - tugas dengan Sdr. Surjo, dikantor Cabang Pertambangan Bintaran Lor 22 Yogyakarta.
Among the number of active volcanes of Jawa this is the lowest and smallest in dimension. Seen from the western shore of the lake (ranu) Lamongan or Glagah, his right summit, which his a cone-shaped form is visible under a view angle of 9'54', and his sharp angular left summit under an angle of 7' 22' above the horizon.
With regard to the earliest times to histories report have received. From the fluent as well an from the positions of both canes follows, that the Malkan or consent said, the mount.
The crater of the Lamongan vas visited for the last time in July 1925. Although since that tine no reports on abnornal phenomena were received, the crater was again reconnoitred at the beginning of February 1924, as we must be always on our alert, that the rostful situation of these previously so active volcano suddenly might change.
During 1922 the G. Lamongan was often visited by the volcano guideship survey namely in April, June and August.
Although several times from the surroundings of the Lamongan nevs arrived on eruptions of the volcano, after further investigation appeared, that the observed abnormal phonomena are not to be ascribed to volcanic activity.
Of more importance than the flank eruptions are the excentric eruptions, which are fed from a much more deeper lavaniveau than the first mentioned, whereas the breakthrough mostly takes place in the area of the volcano foot. Also excentric eruptions may entirely independently become active fron the main crater, which at flankeruptions is not likely possible. Also the phenomena, with which excen…
At the end of February 1920 by the Sectionhead of the Irrigation at Lumajang was reported, that in that month an abnormal drop of the waterlevel of the Ranu's Klakah and Pakis had taken place. If the Ranu Klakah in normal times always flowed through his nator al outlet, at present it is not like this, as the lake level has drop till 1.5 m below the outlet This even happens during the full W …