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Ditemukan 9393 dari pencarian Anda melalui kata kunci: author="."
Hal. Awal Sebelumnya 1 2 3 4 5 Berikutnya Hal. Akhir
cover
The Kelud, Volcanic Earthquakes At Lamongan Volcano In 1924
Komentar Bagikan
N.J.M TaverneS. W. Visser

Volcanic quakes occurred since September 20,1924. E and Ne of Ranu Klakah treasures were formed. The tromometers Klakah repetend in October 135, in September 81, in December 105 shocks.

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
18 hml.; tabel
Judul Seri
-
No. Panggil
PVG E.23-1
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The Lamongan in 1922
Komentar Bagikan
N.J.M Taverne

During 1922 the G. Lamongan was often visited by the volcano guideship survey namely in April, June and August.

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
6 hml.; tabel
Judul Seri
-
No. Panggil
PVG E.22-2
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The Aquatic Transportation of The Semeru - Products The Wet Danger
Komentar Bagikan
G. L. L. Kemmerling

of much more importance of the surrounding plains of the Senera is tow aquatic transportaton of the ejected products, the was danger. When we travel the area between Lunajang and Pasirian and the S foot of the volcano till the Kali Glidik, then it becomes clear to anybody which role the aquatic transportation of the Semeru products fulfils in the economic life of the here established populat…

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
12 hml
Judul Seri
-
No. Panggil
PVG E.22-3
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
Small Eruption on December 6-7, 1920 in the Craterlake of G. Kelud
Komentar Bagikan
G. L. L. Kemmerling

Except by the already quite quickly after-supply of water in the crater established calving off of the craterwall, the topography of the crater and therefore the correctness of the calculation of the supplied water was much more seriously hindered by a small eruption in the craterlake, which took place in the night of December6 to 7, 1928 (The big eruption lasted May 1920, 1919. Translater).

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
3 hml
Judul Seri
-
No. Panggil
PVG E.20-2
Ketersediaan1
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The Eruptions In Kawah Baru, G.Papandayan In 1924, The Activity In Kawah Nang…
Komentar Bagikan
N.J.M Taverne

The eruptions, which in the course of 1924 took place in Kavah Baru, were all of relative short duration. In many cases the activity was restricted to the geyserlike spouting-up of mud from one of the crater openings, which in the course of 1923 were born. Sometines also new craterlats were formed, or except mud also stones were ejected. Naturally the gaspressure at lastnaned eruptions was much…

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
15 hml
Judul Seri
-
No. Panggil
PVG E.25-2
Ketersediaan1
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The G. Kelud in 1924
Komentar Bagikan
N. J. M. Taverne

Phenomena which would indicate on an increased activity on the Kelut were not observed during 1924 and in the beginning of 1925. A fow light earthshocks, which were felt in the lowercamp, appeared to be of tectonic origin.

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
7 hml.; tabel
Judul Seri
-
No. Panggil
PVG E.24-4
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The 1885 Disaster of Semeru Volcano
Komentar Bagikan
G.L.L Kemmerling

In 1885 a part of the southen collapse due to the pressure of the lava in the Semeru

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
5hlm
Judul Seri
-
No. Panggil
PVG E.24-2
Ketersediaan1
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The G. Lamongan
Komentar Bagikan
N.J.M Taverne

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.

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
7 hml
Judul Seri
-
No. Panggil
PVG E.23-2
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
Excentric Eruptions of G.Lamongan
Komentar Bagikan
G. L. L. Kemmerling

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…

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
15 hml.; tabel
Judul Seri
-
No. Panggil
PVG E.22-1
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
cover
The Lamongan
Komentar Bagikan
G. L. L. Kemmerling

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 …

Edisi
-
ISBN/ISSN
-
Deskripsi Fisik
11 hml
Judul Seri
-
No. Panggil
PVG E.21-8
Ketersediaan2
Tambahkan ke dalam keranjang
Unduh MARCSitasi
Hal. Awal Sebelumnya 1 2 3 4 5 Berikutnya Hal. Akhir
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