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The Debris Flows or Ladu's of the Merapi, Central Java In 1930

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The wedusgenbels originated because big amounts of gas-rich, but toughliquid magna were ejected, came down along the volcano slope and landed in the very deep ravines, which are situated in the mountain foot on ca. 1400 na.s. Due to their great mobility they have still covered considerable distances in the terrain gullion. It is striking through which sharp turns (portrait 7, 8 and 10), particularly of the Jurangjero the ladu has dragged. From this the loose composition clearly appears, which the heavy part of the wedungenbel should have had during the forewards moving. The outer edges of the turns e.q. on the Blongkong edge on the opposite of the previous observatory post Maron were then many times covered by stone accumulations.

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Ketersediaan

Informasi Detail

Judul Seri

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No. Panggil

PVG E.30-4

Penerbit

Bandung, Jawa Barat, Indonesia : Pusat Vulkanologi dan Mitigasi Bencana Geologi., 1930

Deskripsi Fisik

18 hml.; tabel

Bahasa

English

ISBN/ISSN

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Klasifikasi

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Tipe Isi

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Tipe Media

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Tipe Pembawa

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Edisi

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Subjek

G. Merapi

Info Detail Spesifik

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Pernyataan Tanggungjawab

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Informasi Lainnya

Kode Wilayah

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Pulau Dan Lembar Peta

Lainnya

Provinsi

Jawa Barat

Koordinat - Latitude

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Koordinat - Longitude

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Versi lain/terkait

Lampiran Berkas