Gunung Bombalai: Perbedaan antara revisi
Konten dihapus Konten ditambahkan
←Membuat halaman berisi ''''Gunung Bombalai''' adalah gunung kerucut piroklastik di Divisi Tawau Sabah, Malaysia.<ref>{{cite web|url=https://www.theborneopost.com/2017/10/31/ministry-exploring-volcano-tourism-in-tawau/|title=Ministry exploring volcano tourism in Tawau|author=Shalina R.|publisher=The Borneo Post|date=31 October 2017|accessdate=20 May 2019|quote=In Sabah, Tawau's Bombalai volcano is currently a dormant volcano and, since it estimated to have erupted thousands of years...' Tag: Suntingan perangkat seluler Suntingan peramban seluler Suntingan seluler lanjutan |
Tidak ada ringkasan suntingan Tag: Suntingan perangkat seluler Suntingan peramban seluler Suntingan seluler lanjutan |
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{{Infobox mountain
'''Gunung Bombalai''' adalah gunung [[kerucut piroklastik]] di Divisi Tawau Sabah, Malaysia.<ref>{{cite web|url=https://www.theborneopost.com/2017/10/31/ministry-exploring-volcano-tourism-in-tawau/|title=Ministry exploring volcano tourism in Tawau|author=Shalina R.|publisher=The Borneo Post|date=31 October 2017|accessdate=20 May 2019|quote=In Sabah, Tawau's Bombalai volcano is currently a dormant volcano and, since it estimated to have erupted thousands of years ago, it can be regarded as an ancient crater. Bombalai cinder cone is only a half-an-hour jungle walk from the entrance of Tawau Hills National Park.|archiveurl=https://web.archive.org/web/20190520073009/https://www.theborneopost.com/2017/10/31/ministry-exploring-volcano-tourism-in-tawau/|archivedate=20 May 2019|url-status=dead}}</ref> Ketinggiannya Mencapai sekitar 531 meter.<ref>{{cite book|author=Malaysia. Jabatan Penyiasatan Kajibumi. Borneo Region|title=Memoir|url=https://books.google.com/books?id=PdUdAQAAIAAJ|year=1962}}</ref>▼
| name = Gunung Bombalai
| native_name =
| photo =
| photo_caption =
| map = Malaysia
| map_caption = Lokasi
| elevation_m = 531
| elevation_ref =
| prominence_m = 212
| coordinates = {{coord|4|23|41|N|117|52|35|E|type:mountain_region:MY|display=inline,title}}
| location = Divisi Tawau, [[Sabah]], [[Malaysia]]
| range =
| topo =
| age =
| type =
| last_eruption = [[Holosen]]
| first_ascent =
| easiest_route =
}}
▲'''Gunung Bombalai''' adalah gunung [[kerucut piroklastik]] di Divisi Tawau, [[Sabah]], [[Malaysia]].<ref>{{cite web|url=https://www.theborneopost.com/2017/10/31/ministry-exploring-volcano-tourism-in-tawau/|title=Ministry exploring volcano tourism in Tawau|author=Shalina R.|publisher=The Borneo Post|date=31 October 2017|accessdate=20 May 2019|quote=In Sabah, Tawau's Bombalai volcano is currently a dormant volcano and, since it estimated to have erupted thousands of years ago, it can be regarded as an ancient crater. Bombalai cinder cone is only a half-an-hour jungle walk from the entrance of Tawau Hills National Park.|archiveurl=https://web.archive.org/web/20190520073009/https://www.theborneopost.com/2017/10/31/ministry-exploring-volcano-tourism-in-tawau/|archivedate=20 May 2019|url-status=dead}}</ref> Ketinggiannya Mencapai sekitar 531 meter.<ref>{{cite book|author=Malaysia. Jabatan Penyiasatan Kajibumi. Borneo Region|title=Memoir|url=https://books.google.com/books?id=PdUdAQAAIAAJ|year=1962}}</ref>
==Geologi==
Gunung ini merupakan bagian dari [[medan vulkanik]] Tawau yang berkontribusi terhadap ciri topografi yang menonjol di Semenanjung Semporna di timur laut [[Kalimantan]] dan sisi barat lembah di bagian tengahnya.<ref>{{cite book|author=North Borneo. Geological Survey Department|title=Annual Report of the Geological Survey Department|url=https://books.google.com/books?id=2DUdAQAAIAAJ|year=1960}}</ref><ref>{{cite book|author=Borneo, British Territories. Geological Survey Dept|title=Annual Report of the Geological Survey Department, British Territories in Borneo|url=https://books.google.com/books?id=fmgJAQAAMAAJ|year=1960|publisher=Government Printer.}}</ref><ref>{{cite book|author=T. R. Paton|title=A Reconnaissance Soil Survey of the Semporna Peninsula, North Borneo|url=https://books.google.com/books?id=2gl-Ui5SVfQC|year=1963|publisher=H.M. Stationery Office}}</ref> Kerucut vulkanik rendah berada di utara [[Pulau Sebatik]] dan memiliki kawah selebar sekitar 300 m di selatan. Dua aliran lava muda memanjang hampir sampai ke dataran pantai. Aliran tersebut dianggap lebih muda dari aliran radiokarbon lava yang berumur sekitar 27.000 tahun sebelum sekarang, dan ekstrusi lava basaltik kemungkinan berlanjut hingga zaman Holosen.<ref>{{cite book|author=Peter S. Bellwood|title=Archaeological Research in South-eastern Sabah|url=https://books.google.com/books?id=n6AsAAAAIAAJ|year=1988|publisher=Sabah Museum and State Archives|isbn=978-983-99532-0-6}}</ref> Kehadiran aktivitas [[energi panas bumi]] telah dilaporkan di pegunungan sekitarnya.<ref>{{cite book|author1=Rosemary Gillespie|author2=D. A. Clague|title=Encyclopedia of Islands|url=https://books.google.com/books?id=g9ZogGs_fz8C&pg=PA112|year=2009|publisher=University of California Press|isbn=978-0-520-25649-1|page=112}}</ref><ref>{{cite web|url=http://www.gsm.org.my/products/702001-100488-PDF.pdf|title=Geochemical characterization of volcanic soils from Tawau, Sabah|author1=Baba Musta|author2=Hennie Fitria W. Soehady E.|author3=Sanudin Tahir|work=Bulletin of the Geological Society of Malaysia|publisher=Geology Programme, School of Science and Technology, [[Universiti Malaysia Sabah]]|year=2008|accessdate=22 October 2017|archiveurl=https://web.archive.org/web/20171022040017/http://www.gsm.org.my/products/702001-100488-PDF.pdf|archivedate=22 October 2017|url-status=dead}}</ref>
==Referensi==
{{Reflist}}
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