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Kipas aluvial - Riwayat revisi
2026-09-15T23:55:18Z
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Maintenance script: Presentation V4: sitasi, referensi, Math, Wikimedia Commons, dan atribusi
2026-08-29T23:10:31Z
<p>Presentation V4: sitasi, referensi, Math, Wikimedia Commons, dan atribusi</p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Revisi sebelumnya</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revisi per 29 Agustus 2026 23.10</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Baris 1:</td>
<td colspan="2" class="diff-lineno">Baris 1:</td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>'''Kipas aluvial''' adalah [[endapan]] [[sedimen]] yang berbentuk seperti [[kipas]] dan terbentuk oleh aliran [[sungai]]. Aliran tersebut berasal dari satu titik di ujung kipas. Kipas aluvial biasanya dapat ditemui di wilayah [[pegunungan]] yang sedang ber[[erosi]]. [[Banjir]] sering kali terjadi di kipas aluvial.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[File:Mahakam_delta_geologic_map.jpg|thumb|right|280px|Mahakam delta geologic map]]</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div> </div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>'''Kipas aluvial''' adalah [[endapan]] [[sedimen]] yang berbentuk seperti [[kipas]] dan terbentuk oleh aliran [[sungai]]. Aliran tersebut berasal dari satu titik di ujung kipas. Kipas aluvial biasanya dapat ditemui di wilayah [[pegunungan]] yang sedang ber[[erosi]]. [[Banjir]] sering kali terjadi di kipas aluvial.<ins style="font-weight: bold; text-decoration: none;"><ref>Dan Cazanacli. ''Experimental Steep, Braided Flow: Application to Flooding Risk on Fans''. ''Journal of Hydraulic Engineering''. 2002. Vol. 128 (3). hlm. 322. doi:10.1061/(ASCE)0733-9429(2002)128:3(322).</ref><ref>Committee on Alluvial Fan Flooding, Water Science and Technology Board, Commission on Geosciences, Environment, and Resources, National Research Council. [https://archive.org/details/alluvialfanflood0000unse Alluvial fan flooding]. National Academy Press. 1996. ISBN 0-309-05542-3.</ref></ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Di [[Tata Surya]] ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Di [[Tata Surya]] ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Kipas aluvial dapat ditemui di planet [[Mars]], seperti yang ditemukan di [[kawah Gale]]. Kenampakan ini juga telah diamati oleh misi [[Cassini-Huygens]] di [[Titan (satelit)|Titan]] dengan menggunakan alat Synthetic Aperture [[RADAR]] (SAR. Kipas tersebut lebih banyak tersebar di wilayah lintang tengah yang lebih kering di ujung sungai [[metana]]/[[etana]] yang sering kali menjadi basah atau kering akibat [[presipitasi]], layaknya kipas kering di Bumi. Pencitraan radar menunjukkan bahwa materi kipas kemungkinan besar terdiri dari butiran-butiran es air atau [[senyawa organik]] padat dengan diameter dua sentimeter.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Kipas aluvial dapat ditemui di planet [[Mars]],<ins style="font-weight: bold; text-decoration: none;"><ref>[http://www.sciencedirect.com/science/article/pii/S0019103507004733 Erin R. Kraal, Erik Asphaug, Jeffery M. Moore, Alan Howard, Adam Bredt, ''Catalogue of large alluvial fans in martian impact craters,'' Icarus, Volume 194, Issue 1, Maret 2008, Pages 101-110, ISSN 0019-1035, 10.1016/j.icarus.2007.09.028.]</ref> </ins>seperti yang ditemukan di [[kawah Gale]].<ins style="font-weight: bold; text-decoration: none;"><ref>[http://www.cbsnews.com/8301-205_162-57521772/mars-rover-curiosity-finds-ancient-stream-bed/ ''Mars rover Curiosity finds ancient stream bed,'' CBS News, 27 September 2012].</ref> </ins>Kenampakan ini juga telah diamati oleh misi [[Cassini-Huygens]] di [[Titan (satelit)|Titan]] dengan menggunakan alat Synthetic Aperture [[RADAR]] (SAR.<ins style="font-weight: bold; text-decoration: none;"><ref>[http://www.lpi.usra.edu/meetings/lpsc2013/pdf/2641.pdf Radebaugh et al. (2013) ''Alluvial Fans on Titan Reveal Materials, Processes and Regional Conditions,'' 44th Lunar and Planetary Science Conference]</ref> </ins>Kipas tersebut lebih banyak tersebar di wilayah lintang tengah yang lebih kering di ujung sungai [[metana]]/[[etana]] yang sering kali menjadi basah atau kering akibat [[presipitasi]], layaknya kipas kering di Bumi. Pencitraan radar menunjukkan bahwa materi kipas kemungkinan besar terdiri dari butiran-butiran es air atau [[senyawa organik]] padat dengan diameter dua sentimeter.</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div> </div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">== Catatan kaki ==</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Pranala luar ==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>== Pranala luar ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>*</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>* </div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [http://www.waterlog.info/pdf/punata.pdf] Irrigation in the alluvial fan of Punata, Bolivia</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [http://www.waterlog.info/pdf/punata.pdf] Irrigation in the alluvial fan of Punata, Bolivia</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [http://www.waterlog.info/pdf/garmsar.pdf] Irrigation in the alluvial fan of Garmsar, Iran</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [http://www.waterlog.info/pdf/garmsar.pdf] Irrigation in the alluvial fan of Garmsar, Iran</div></td></tr>
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<td colspan="2" class="diff-lineno">Baris 14:</td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [http://waterwiki.net/index.php/Irrigation_of_alluvial_fans Irrigation of alluvial fans]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>* [http://waterwiki.net/index.php/Irrigation_of_alluvial_fans Irrigation of alluvial fans]</div></td></tr>
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<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">== Referensi ==</ins></div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">== Sumber dan atribusi ==</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>== <del style="font-weight: bold; text-decoration: none;">Sumber </del>dan <del style="font-weight: bold; text-decoration: none;">atribusi ==</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title</ins>=<ins style="font-weight: bold; text-decoration: none;">Kipas+aluvial&oldid</ins>=<ins style="font-weight: bold; text-decoration: none;">29437581 Wikipedia bahasa Indonesia], revisi 29437581 (2026-07-09T23:36:24Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi-BerbagiSerupa (CC BY-SA). Gambar pada artikel ini bersumber dari Wikimedia Commons </ins>dan <ins style="font-weight: bold; text-decoration: none;">mengikuti ketentuan lisensi masing-masing berkas. Mohon gunakan konten dan media secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title=Kipas+aluvial&oldid=29437581 Wikipedia bahasa Indonesia], revisi 29437581 (2026</del>-<del style="font-weight: bold; text-decoration: none;">07</del>-<del style="font-weight: bold; text-decoration: none;">09T23:36:24Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi</del>-<del style="font-weight: bold; text-decoration: none;">BerbagiSerupa (CC BY</del>-<del style="font-weight: bold; text-decoration: none;">SA). Mohon gunakan konten ini secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><!</ins>-- <ins style="font-weight: bold; text-decoration: none;">WIKI_UNISSULA_PRESENTATION_V4 </ins>--<ins style="font-weight: bold; text-decoration: none;">></ins></div></td></tr>
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Maintenance script: Impor teks terkontrol dari Wikipedia bahasa Indonesia; revisi 29437581; atribusi sumber disertakan.
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<p>Impor teks terkontrol dari Wikipedia bahasa Indonesia; revisi 29437581; atribusi sumber disertakan.</p>
<p><b>Halaman baru</b></p><div>'''Kipas aluvial''' adalah [[endapan]] [[sedimen]] yang berbentuk seperti [[kipas]] dan terbentuk oleh aliran [[sungai]]. Aliran tersebut berasal dari satu titik di ujung kipas. Kipas aluvial biasanya dapat ditemui di wilayah [[pegunungan]] yang sedang ber[[erosi]]. [[Banjir]] sering kali terjadi di kipas aluvial.<br />
<br />
== Di [[Tata Surya]] ==<br />
Kipas aluvial dapat ditemui di planet [[Mars]], seperti yang ditemukan di [[kawah Gale]]. Kenampakan ini juga telah diamati oleh misi [[Cassini-Huygens]] di [[Titan (satelit)|Titan]] dengan menggunakan alat Synthetic Aperture [[RADAR]] (SAR. Kipas tersebut lebih banyak tersebar di wilayah lintang tengah yang lebih kering di ujung sungai [[metana]]/[[etana]] yang sering kali menjadi basah atau kering akibat [[presipitasi]], layaknya kipas kering di Bumi. Pencitraan radar menunjukkan bahwa materi kipas kemungkinan besar terdiri dari butiran-butiran es air atau [[senyawa organik]] padat dengan diameter dua sentimeter.<br />
<br />
== Catatan kaki ==<br />
<br />
<br />
== Pranala luar ==<br />
*<br />
* [http://www.waterlog.info/pdf/punata.pdf] Irrigation in the alluvial fan of Punata, Bolivia<br />
* [http://www.waterlog.info/pdf/garmsar.pdf] Irrigation in the alluvial fan of Garmsar, Iran<br />
* [http://www.waterlog.info/pdf/molapos.pdf] Flood recession cropping in the alluvial fan of Okavango, Botswana<br />
* [http://www.waterlog.info/pdf/baluchistan.pdf] Irrigation in alluvial fans in Baluchistan<br />
* [http://waterwiki.net/index.php/Irrigation_of_alluvial_fans Irrigation of alluvial fans]<br />
<br />
<br />
<br />
== Sumber dan atribusi ==<br />
<br />
Konten artikel ini diadaptasi dari [https://id.wikipedia.org/w/index.php?title=Kipas+aluvial&oldid=29437581 Wikipedia bahasa Indonesia], revisi 29437581 (2026-07-09T23:36:24Z), yang tersedia berdasarkan lisensi Creative Commons Atribusi-BerbagiSerupa (CC BY-SA). Mohon gunakan konten ini secara bijak serta sesuai dengan ketentuan lisensi yang berlaku.</div>
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