Morphological Changes due to Anthropogenic Interferences in Gendol River Valley, Merapi Volcano
This research aims to identify the morphological changes in Gendol river, Merapi volcano. After the eruption 2010, Gendol river filled up by pyroclastic materials, then utilized as mining area. As the volcanic materials are abundance in Gendol river, sand mining activities are dominant, causing antr...
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| Format: | Article |
| Language: | English |
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Universitas Muhammadiyah Surakarta
2020-01-01
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| Series: | Forum Geografi |
| Subjects: | |
| Online Access: | http://journals.ums.ac.id/index.php/fg/article/view/8766 |
| _version_ | 1797428466183831552 |
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| author | Mukhamad Ngainul Malawani Tiara Handayani Jundi Muhammad Bariq Radikal Lukafiardi |
| author_facet | Mukhamad Ngainul Malawani Tiara Handayani Jundi Muhammad Bariq Radikal Lukafiardi |
| author_sort | Mukhamad Ngainul Malawani |
| collection | DOAJ |
| description | This research aims to identify the morphological changes in Gendol river, Merapi volcano. After the eruption 2010, Gendol river filled up by pyroclastic materials, then utilized as mining area. As the volcanic materials are abundance in Gendol river, sand mining activities are dominant, causing antrophogenic interferences that changes the morphology of Gendol valley. In this study, the morphological changes is measured by terrestrial survey, aerial mapping, and materials analysis through petrographic and granulometric analysis. Aerial mapping was conducted in February and August 2019 in order to identify the dynamic changes during 6 months observation. Vertical changes is found in the active mining zone, in western-side of research area, while horizontal changes was found in eastern-side. The comparison of widening and narrowing valley is 13:1 due to horizontal changes. Result of petrographic analysis showes that three different sampling locations originated from similar provenance, which is undissected arc provenance but may differ in period of sedimentation. Grain material found in research are categorized as suitable material for mining with the 0,733 mm grain size. However, the mining activities should be aware of material availability to minimize the riverbank failure. |
| first_indexed | 2024-03-09T08:58:10Z |
| format | Article |
| id | doaj.art-752d80a465f542e2a5aa71e0f87244ce |
| institution | Directory Open Access Journal |
| issn | 0852-0682 2460-3945 |
| language | English |
| last_indexed | 2024-03-09T08:58:10Z |
| publishDate | 2020-01-01 |
| publisher | Universitas Muhammadiyah Surakarta |
| record_format | Article |
| series | Forum Geografi |
| spelling | doaj.art-752d80a465f542e2a5aa71e0f87244ce2023-12-02T12:21:31ZengUniversitas Muhammadiyah SurakartaForum Geografi0852-06822460-39452020-01-0133220921810.23917/forgeo.v33i2.87665171Morphological Changes due to Anthropogenic Interferences in Gendol River Valley, Merapi VolcanoMukhamad Ngainul Malawani0Tiara Handayani1Jundi Muhammad Bariq2Radikal Lukafiardi3Department of Environmental Geography UGMCentre for Disaster Study, Univeritas Gadjah Mada,Laboratory Assistant, Environmental Geomorphology and Disaster Mitigation Laboratory, UGMLaboratory Assistant, Environmental Geomorphology and Disaster Mitigation Laboratory, UGMThis research aims to identify the morphological changes in Gendol river, Merapi volcano. After the eruption 2010, Gendol river filled up by pyroclastic materials, then utilized as mining area. As the volcanic materials are abundance in Gendol river, sand mining activities are dominant, causing antrophogenic interferences that changes the morphology of Gendol valley. In this study, the morphological changes is measured by terrestrial survey, aerial mapping, and materials analysis through petrographic and granulometric analysis. Aerial mapping was conducted in February and August 2019 in order to identify the dynamic changes during 6 months observation. Vertical changes is found in the active mining zone, in western-side of research area, while horizontal changes was found in eastern-side. The comparison of widening and narrowing valley is 13:1 due to horizontal changes. Result of petrographic analysis showes that three different sampling locations originated from similar provenance, which is undissected arc provenance but may differ in period of sedimentation. Grain material found in research are categorized as suitable material for mining with the 0,733 mm grain size. However, the mining activities should be aware of material availability to minimize the riverbank failure.http://journals.ums.ac.id/index.php/fg/article/view/8766anthropogenicmorphologyriver valleyvolcano |
| spellingShingle | Mukhamad Ngainul Malawani Tiara Handayani Jundi Muhammad Bariq Radikal Lukafiardi Morphological Changes due to Anthropogenic Interferences in Gendol River Valley, Merapi Volcano Forum Geografi anthropogenic morphology river valley volcano |
| title | Morphological Changes due to Anthropogenic Interferences in Gendol River Valley, Merapi Volcano |
| title_full | Morphological Changes due to Anthropogenic Interferences in Gendol River Valley, Merapi Volcano |
| title_fullStr | Morphological Changes due to Anthropogenic Interferences in Gendol River Valley, Merapi Volcano |
| title_full_unstemmed | Morphological Changes due to Anthropogenic Interferences in Gendol River Valley, Merapi Volcano |
| title_short | Morphological Changes due to Anthropogenic Interferences in Gendol River Valley, Merapi Volcano |
| title_sort | morphological changes due to anthropogenic interferences in gendol river valley merapi volcano |
| topic | anthropogenic morphology river valley volcano |
| url | http://journals.ums.ac.id/index.php/fg/article/view/8766 |
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