Geomorphological Mapping of The Prambanan Hills Yogyakarta
Understanding geomorphological characteristics must provide morphographic, morphometric,morphogenetic, and morphochronological information. This study aims to identify geomorphological characteristics in the Prambanan hills area compiled in the form of a geomorphological map. The research is based o...
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| Format: | Article |
| Language: | English |
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EDP Sciences
2022-01-01
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| Series: | MATEC Web of Conferences |
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| Online Access: | https://www.matec-conferences.org/articles/matecconf/pdf/2022/19/matecconf_icst2022_05009.pdf |
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| author | Purnomo Nugroho Hari Budiyantot Eko Muzayanah Kurniawati Aida Prasetyo Ketut Dewi Magita Nastiti Sigra |
| author_facet | Purnomo Nugroho Hari Budiyantot Eko Muzayanah Kurniawati Aida Prasetyo Ketut Dewi Magita Nastiti Sigra |
| author_sort | Purnomo Nugroho Hari |
| collection | DOAJ |
| description | Understanding geomorphological characteristics must provide morphographic, morphometric,morphogenetic, and morphochronological information. This study aims to identify geomorphological characteristics in the Prambanan hills area compiled in the form of a geomorphological map. The research is based on maps, previous research reports, and field observations in the form of field checks on theelements studied. The geomorphological mapping system used is the ITC system. The main analysis in this research is spatial analysis in the form of overlapping spatial data. The relationship between landform units,lithology, and slopes is information that is analyzed descriptively. The results showed that on a map with a scale of 1: 30,000, 9 geomorphological units could be identified. The 9 geomorphological units are a combination of morphometry, genetics, and lithology. The combination consists of 2 landforms, namelytraditional and structural hills, and slopes; The lithology consists of 3 layers, namely the Lapili Formation of Semilir, Sand Formation of Kebo Butak, and Tuff Formation of Semilir. While the morphometry is in theform of slope units, namely 8-15%, 15-25%, 25-45%, and >45%. While the age based on lithology is Late Oligocene – Early Miocene in the Kebo Butak Formation and Early Miocene – Middle Miocene in theSemilir Formation. |
| first_indexed | 2024-04-13T07:07:53Z |
| format | Article |
| id | doaj.art-a1425e2acb9143c2b976774c6cbc8e50 |
| institution | Directory Open Access Journal |
| issn | 2261-236X |
| language | English |
| last_indexed | 2024-04-13T07:07:53Z |
| publishDate | 2022-01-01 |
| publisher | EDP Sciences |
| record_format | Article |
| series | MATEC Web of Conferences |
| spelling | doaj.art-a1425e2acb9143c2b976774c6cbc8e502022-12-22T02:56:56ZengEDP SciencesMATEC Web of Conferences2261-236X2022-01-013720500910.1051/matecconf/202237205009matecconf_icst2022_05009Geomorphological Mapping of The Prambanan Hills YogyakartaPurnomo Nugroho Hari0Budiyantot Eko1Muzayanah2Kurniawati Aida3Prasetyo Ketut4Dewi Magita Nastiti Sigra5Department of Geography Education, Faculty of Social Sciences and Law, Universitas Negeri SurabayaDepartment of Geography Education, Faculty of Social Sciences and Law, Universitas Negeri SurabayaDepartment of Geography Education, Faculty of Social Sciences and Law, Universitas Negeri SurabayaDepartment of Geography Education, Faculty of Social Sciences and Law, Universitas Negeri SurabayaDepartment of Geography Education, Faculty of Social Sciences and Law, Universitas Negeri SurabayaLearning Activity Studio, Kaliloam Lor SurabayaUnderstanding geomorphological characteristics must provide morphographic, morphometric,morphogenetic, and morphochronological information. This study aims to identify geomorphological characteristics in the Prambanan hills area compiled in the form of a geomorphological map. The research is based on maps, previous research reports, and field observations in the form of field checks on theelements studied. The geomorphological mapping system used is the ITC system. The main analysis in this research is spatial analysis in the form of overlapping spatial data. The relationship between landform units,lithology, and slopes is information that is analyzed descriptively. The results showed that on a map with a scale of 1: 30,000, 9 geomorphological units could be identified. The 9 geomorphological units are a combination of morphometry, genetics, and lithology. The combination consists of 2 landforms, namelytraditional and structural hills, and slopes; The lithology consists of 3 layers, namely the Lapili Formation of Semilir, Sand Formation of Kebo Butak, and Tuff Formation of Semilir. While the morphometry is in theform of slope units, namely 8-15%, 15-25%, 25-45%, and >45%. While the age based on lithology is Late Oligocene – Early Miocene in the Kebo Butak Formation and Early Miocene – Middle Miocene in theSemilir Formation.https://www.matec-conferences.org/articles/matecconf/pdf/2022/19/matecconf_icst2022_05009.pdfgeomorphologicalmappingprambananhills |
| spellingShingle | Purnomo Nugroho Hari Budiyantot Eko Muzayanah Kurniawati Aida Prasetyo Ketut Dewi Magita Nastiti Sigra Geomorphological Mapping of The Prambanan Hills Yogyakarta MATEC Web of Conferences geomorphological mapping prambanan hills |
| title | Geomorphological Mapping of The Prambanan Hills Yogyakarta |
| title_full | Geomorphological Mapping of The Prambanan Hills Yogyakarta |
| title_fullStr | Geomorphological Mapping of The Prambanan Hills Yogyakarta |
| title_full_unstemmed | Geomorphological Mapping of The Prambanan Hills Yogyakarta |
| title_short | Geomorphological Mapping of The Prambanan Hills Yogyakarta |
| title_sort | geomorphological mapping of the prambanan hills yogyakarta |
| topic | geomorphological mapping prambanan hills |
| url | https://www.matec-conferences.org/articles/matecconf/pdf/2022/19/matecconf_icst2022_05009.pdf |
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