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The study of the geomorphological process of the Borobudur plain in Indonesia.
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- Kato Hirotaka
- Komabatoho High School
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- Haruyama Shigeko
- Tokyo University
Bibliographic Information
- Other Title
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- インドネシア・ボロブドゥール平野の地形発達史からの考察
- The effects of Mt.Merapi on geographical features around C.Borobudur.
- メラピ火山噴火がボロブドゥール寺院周辺へ与える影響
Description
This study deals with the geomorphological process of the Borobudur plain in Indonesia, based on whether the eruption of Mt. Merapi in 1016 ruined C. Borobudur directly. We can see that the Borobudur plain has two characteristics types of the geographical features, to make the geomorphological landform classification map. The eastern part of this area is the fluviovolcanic footslope of Mt. Merapi, while the western part is the alluvial plain of the Progo river. So it is certain that mudflood (Lahar and Banjir) from Mt. Merapi has not reach at C. Borobudur. That is, the eruption of Mt. Merapi in 1016 did not ruined C. Borobudur directly.
Journal
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- Proceedings of the General Meeting of the Association of Japanese Geographers
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Proceedings of the General Meeting of the Association of Japanese Geographers 2003s (0), 000023-000023, 2003
The Association of Japanese Geographers
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Keywords
Details 詳細情報について
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- CRID
- 1390282680670515328
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- NII Article ID
- 130007016707
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- Data Source
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- JaLC
- CiNii Articles
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- Abstract License Flag
- Disallowed
