güneş sistemi'nin en yüksek dağlarının listesi ne demek?

Bu Güneş Sistemi'ndeki en yüksek dağların bir listesi; bâzı durumlarda, Dünya'daki farklı sınıfların en yüksek zirveleri de listelenmiştir. 21,9 km yükseklikte, Mars'taki büyük kalkan volkanı Olympus Mons, herhangi bir gezegen üzerindeki en yüksek dağdır. 1971 yılında keşfi ardından 40 yıl boyunca Güneş Sistemi'nin bilinen en yüksek dağı idi. Ancak 2011 yılında asteroid ve protoplanet Vesta üzerindeki Rheasilvia Krateri'nin merkezî tepesinin karşılaştırılabilir bir yükseklikte olduğu tespit edilmiştir.

Liste

Diğer dünyalarda deniz seviyesinden yüksekliğe hiçbir keyfî olmayan eşdeğer olmadığından yükseklikler, bazdan tepeye verilmiştir.

<table> <thead> <tr class="header"> <th><p>Dünya</p></th> <th><p>En yüksek zirve(ler)</p></th> <th><p>Yükseklik</p></th> <th><p>yarıçapın %'si<span class="mw-ref" id="cxcite_ref-2" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-2"></p></th> <th><p>Başlangıcı</p></th> <th><p>Notlar</p></th> </tr> </thead> <tbody> <tr class="odd"> <td><p><a href="Merkür" title="wikilink">Merkür</a></p></td> <td><p><a href="Caloris_Montes" title="wikilink">Caloris Montes</a></p></td> <td><p>≤ 3 km<a href="#fn1" class="footnote-ref" id="fnref1" role="doc-noteref"><sup>1</sup></a><a href="#fn2" class="footnote-ref" id="fnref2" role="doc-noteref"><sup>2</sup></a></p></td> <td><p>0,12</p></td> <td><p><a href="Çarpma_krateri" title="wikilink">çarpma</a><a href="#fn3" class="footnote-ref" id="fnref3" role="doc-noteref"><sup>3</sup></a></p></td> <td><p>Caloris çarpışıyla şekillendi</p></td> </tr> <tr class="even"> <td><p><a href="Venüs" title="wikilink">Venüs</a></p></td> <td><p><a href="Skadi_Mons" title="wikilink">Skadi Mons</a></p></td> <td><p>6,4 km (takriben) <a href="#fn4" class="footnote-ref" id="fnref4" role="doc-noteref"><sup>4</sup></a></p></td> <td><p>0,11</p></td> <td><p><a href="Orojenez" title="wikilink">tektonik</a><a href="#fn5" class="footnote-ref" id="fnref5" role="doc-noteref"><sup>5</sup></a></p></td> <td><p>Radarca parlak yamaçları muhtemelen kurşun sülfit olan metalik Venüs karından dolayı vardır.<a href="#fn6" class="footnote-ref" id="fnref6" role="doc-noteref"><sup>6</sup></a></p></td> </tr> <tr class="odd"> <td><p><a href="Maat_Mons_Yanardağı" title="wikilink">Maat Mons</a></p></td> <td><p>4,9 km (takriben)<a href="#fn7" class="footnote-ref" id="fnref7" role="doc-noteref"><sup>7</sup></a></p></td> <td><p>0,081</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a><a href="#fn8" class="footnote-ref" id="fnref8" role="doc-noteref"><sup>8</sup></a></p></td> <td><p>Venüs'teki en yüksek volkan</p></td> <td></td> </tr> <tr class="even"> <td><p><a href="En_yüksek_dağlar_listesi" title="wikilink">Dünya</a></p></td> <td><p><a href="Mauna_Kea" title="wikilink">Mauna Kea</a> ve <a href="Mauna_Loa_Dağı" title="wikilink">Mauna Loa</a></p></td> <td><p>10,2 km<a href="#fn9" class="footnote-ref" id="fnref9" role="doc-noteref"><sup>9</sup></a></p></td> <td><p>0,16</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p>Bunun 4,2 km'si su seviyesinin üstündedir</p></td> </tr> <tr class="odd"> <td><p><a href="Teide_Yanardağı" title="wikilink">Pico del Teide</a></p></td> <td><p>7,5 km<a href="#fn10" class="footnote-ref" id="fnref10" role="doc-noteref"><sup>10</sup></a></p></td> <td><p>0,12</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p>Rises 3,7 km above sea level<a href="#fn11" class="footnote-ref" id="fnref11" role="doc-noteref"><sup>11</sup></a></p></td> <td></td> </tr> <tr class="even"> <td><p><a href="Denali" title="wikilink">Denali</a></p></td> <td><p>5,3 ilâ 5,9 km<a href="#fn12" class="footnote-ref" id="fnref12" role="doc-noteref"><sup>12</sup></a></p></td> <td><p>0,093</p></td> <td><p><a href="Orojenez" title="wikilink">tektonik</a></p></td> <td><p>Karada tabandan zirveye en yüksek dağ<a href="#fn13" class="footnote-ref" id="fnref13" role="doc-noteref"><sup>13</sup></a><span class="mw-ref" id="cxcite_ref-15" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-15"></p></td> <td></td> </tr> <tr class="odd"> <td><p><a href="Everest_Dağı" title="wikilink">Everest Dağı</a></p></td> <td><p>3,6 ilâ 4,6 km<a href="#fn14" class="footnote-ref" id="fnref14" role="doc-noteref"><sup>14</sup></a></p></td> <td><p>0,072</p></td> <td><p><a href="Orojenez" title="wikilink">tektonik</a></p></td> <td><p>Kuzey tarafında 4,6 km, güney tarafında 3,6 km.<span class="mw-ref" id="cxcite_ref-17" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-17"></p></td> <td></td> </tr> <tr class="even"> <td><p><a href="Ay" title="wikilink">Ay</a></p></td> <td><p><a href="Mons_Huygens" title="wikilink">Mons Huygens</a></p></td> <td><p>5,5 km<a href="#fn15" class="footnote-ref" id="fnref15" role="doc-noteref"><sup>15</sup></a><a href="#fn16" class="footnote-ref" id="fnref16" role="doc-noteref"><sup>16</sup></a></p></td> <td><p>0,32</p></td> <td><p><a href="Çarpma_krateri" title="wikilink">çarpma</a></p></td> <td><p><a href="Mare_Imbrium" title="wikilink">Imbrium</a> çarpışıyla şekillendi</p></td> </tr> <tr class="odd"> <td><p><a href="Mons_Hadley" title="wikilink">Mons Hadley</a></p></td> <td><p>4,5 km<a href="#fn17" class="footnote-ref" id="fnref17" role="doc-noteref"><sup>17</sup></a><a href="#fn18" class="footnote-ref" id="fnref18" role="doc-noteref"><sup>18</sup></a></p></td> <td><p>0,26</p></td> <td><p><a href="Çarpma_krateri" title="wikilink">çarpma</a></p></td> <td><p><a href="Mare_Imbrium" title="wikilink">Imbrium</a> çarpışıyla şekillendi</p></td> <td></td> </tr> <tr class="even"> <td><p><a href="Mons_Rümker" title="wikilink">Mons Rümker</a></p></td> <td><p>1,1 km<a href="#fn19" class="footnote-ref" id="fnref19" role="doc-noteref"><sup>19</sup></a></p></td> <td><p>0,063</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p>Ay'daki en büyük volkanik yapı<a href="#fn20" class="footnote-ref" id="fnref20" role="doc-noteref"><sup>20</sup></a></p></td> <td></td> </tr> <tr class="odd"> <td><p><a href="Mars" title="wikilink">Mars</a></p></td> <td><p><a href="Olympus_Mons" title="wikilink">Olympus Mons</a></p></td> <td><p>21,9 km<a href="#fn21" class="footnote-ref" id="fnref21" role="doc-noteref"><sup>21</sup></a><a href="#fn22" class="footnote-ref" id="fnref22" role="doc-noteref"><sup>22</sup></a></p></td> <td><p>0,65</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p>Kuzey yaylalarının 26 km üzerine yükselir,<a href="#fn23" class="footnote-ref" id="fnref23" role="doc-noteref"><sup>23</sup></a> 1000 km uzaktadır.</p></td> </tr> <tr class="even"> <td><p><a href="Ascraeus_Mons" title="wikilink">Ascraeus Mons</a></p></td> <td><p>14,9 km<a href="#fn24" class="footnote-ref" id="fnref24" role="doc-noteref"><sup>24</sup></a></p></td> <td><p>0,44</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p><a href="Tharsis_Montes" title="wikilink">Tharsis Montes</a>'in en büyüğü</p></td> <td></td> </tr> <tr class="odd"> <td><p><a href="Elysium_Mons" title="wikilink">Elysium Mons</a></p></td> <td><p>12,6 km<a href="#fn25" class="footnote-ref" id="fnref25" role="doc-noteref"><sup>25</sup></a></p></td> <td><p>0,37</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p>Elysium'daki en yüksek volkan</p></td> <td></td> </tr> <tr class="even"> <td><p><a href="Arsia_Mons" title="wikilink">Arsia Mons</a></p></td> <td><p>11,7 km<a href="#fn26" class="footnote-ref" id="fnref26" role="doc-noteref"><sup>26</sup></a></p></td> <td><p>0,35</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p>Zirve <a href="kaldera" title="wikilink">kalderası</a> boydan boya 108 ilâ 138 km'dir<a href="#fn27" class="footnote-ref" id="fnref27" role="doc-noteref"><sup>27</sup></a></p></td> <td></td> </tr> <tr class="odd"> <td><p><a href="Pavonis_Mons" title="wikilink">Pavonis Mons</a></p></td> <td><p>8,4 km<a href="#fn28" class="footnote-ref" id="fnref28" role="doc-noteref"><sup>28</sup></a></p></td> <td><p>0,25</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p>Zirve kalderası 4,8 km derinliğindedir<a href="#fn29" class="footnote-ref" id="fnref29" role="doc-noteref"><sup>29</sup></a></p></td> <td></td> </tr> <tr class="even"> <td><p><a href="Anseris_Mons" title="wikilink">Anseris Mons</a></p></td> <td><p>6,2 km<a href="#fn30" class="footnote-ref" id="fnref30" role="doc-noteref"><sup>30</sup></a></p></td> <td><p>0,18</p></td> <td><p><a href="Çarpma_krateri" title="wikilink">çarpma</a></p></td> <td><p>Mars'ta Hellas çarpmasıyla meydana gelen volkanik olmayan en yüksek tepelerdendir.</p></td> <td></td> </tr> <tr class="odd"> <td><p><a href="Aeolis_Mons" title="wikilink">Aeolis Mons</a> ("Sivri Dağ")</p></td> <td><p>4,5 ilâ 5,5 km<a href="#fn31" class="footnote-ref" id="fnref31" role="doc-noteref"><sup>31</sup></a><span class="mw-ref" id="cxcite_ref-26" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-26"></p></td> <td><p>0,16</p></td> <td><p>çökelme<span class="mw-ref" id="cxcite_ref-28" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-28"></p></td> <td><p>Gale Krateri'ndeki çökelmelerinden meydana gelmiştir; <a href="Curiosity_(keşif_aracı)" title="wikilink">MSL keşif aracı</a><a href="#fn32" class="footnote-ref" id="fnref32" role="doc-noteref"><sup>32</sup></a> oraya doğru yükselecektir</p></td> <td></td> </tr> <tr class="even"> <td><p><a href="4_Vesta" title="wikilink">Vesta</a></p></td> <td><p><a href="Rheasilvia" title="wikilink">Rheasilvia</a> merkezî zirvesi</p></td> <td><p>22 km<a href="#fn33" class="footnote-ref" id="fnref33" role="doc-noteref"><sup>33</sup></a><a href="#fn34" class="footnote-ref" id="fnref34" role="doc-noteref"><sup>34</sup></a></p></td> <td><p>8,4</p></td> <td><p><a href="Çarpma_krateri" title="wikilink">çarpma</a></p></td> <td><p>Ayrıca <a href="Güneş_Sistemi&#39;ndeki_en_büyük_kraterlerin_listesi" title="wikilink">Güneş Sistemi'ndeki en büyük kraterlerin listesine</a> bakınız</p></td> </tr> <tr class="odd"> <td><p><a href="Ceres" title="wikilink">Ceres</a></p></td> <td><p><a href="Ahuna_Mons" title="wikilink">Ahuna Mons</a></p></td> <td><p>4 km<a href="#fn35" class="footnote-ref" id="fnref35" role="doc-noteref"><sup>35</sup></a></p></td> <td><p>0,85</p></td> <td><p>belirsiz</p></td> <td><p>Nispeten düz bölgede tecrit edilmeş dik yamaçlı doma</p></td> </tr> <tr class="even"> <td><p><a href="İo_(uydu)" title="wikilink">İo</a></p></td> <td><p><a href="Boösaule_Montes" title="wikilink">Boösaule Montes</a> "South"<a href="#fn36" class="footnote-ref" id="fnref36" role="doc-noteref"><sup>36</sup></a></p></td> <td><p>17,5 ilâ 18,2 km<a href="#fn37" class="footnote-ref" id="fnref37" role="doc-noteref"><sup>37</sup></a></p></td> <td><p>1,0</p></td> <td><p><a href="Orojenez" title="wikilink">tektonik</a></p></td> <td><p>GB tarafında 15 km yüksekliğinde uçurumu vardır<a href="#fn38" class="footnote-ref" id="fnref38" role="doc-noteref"><sup>38</sup></a></p></td> </tr> <tr class="odd"> <td><p><a href="İonian_Mons" title="wikilink">İonian Mons</a> doğu sırtı</p></td> <td><p>12,7 km (takriben)<a href="#fn39" class="footnote-ref" id="fnref39" role="doc-noteref"><sup>39</sup></a><a href="#fn40" class="footnote-ref" id="fnref40" role="doc-noteref"><sup>40</sup></a></p></td> <td><p>0,70</p></td> <td><p><a href="Orojenez" title="wikilink">tektonik</a></p></td> <td><p>Eğilmiş çift sırt şeklindedir</p></td> <td></td> </tr> <tr class="even"> <td><p><a href="Euboea_Montes" title="wikilink">Euboea Montes</a></p></td> <td><p>10,3 ilâ 13,4 km<a href="#fn41" class="footnote-ref" id="fnref41" role="doc-noteref"><sup>41</sup></a></p></td> <td><p>0,74</p></td> <td><p><a href="Orojenez" title="wikilink">tektonik</a></p></td> <td><p>KB yamacı toprak kayması, 25.000 km³'lük bir enkaz apronu bıraktı.<a href="#fn42" class="footnote-ref" id="fnref42" role="doc-noteref"><sup>42</sup></a><span class="mw-ref" id="cxcite_ref-41" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-41"></p></td> <td></td> </tr> <tr class="odd"> <td><p>isimsiz (245° W, 30° S)</p></td> <td><p>2,5 km (takriben)<a href="#fn43" class="footnote-ref" id="fnref43" role="doc-noteref"><sup>43</sup></a><a href="#fn44" class="footnote-ref" id="fnref44" role="doc-noteref"><sup>44</sup></a></p></td> <td><p>0,14</p></td> <td><p><a href="Yanardağ" title="wikilink">volkanik</a></p></td> <td><p>Tipik olmayan konik şekli olan İo'nun birçok volkanının en yükseklerinden<a href="#fn45" class="footnote-ref" id="fnref45" role="doc-noteref"><sup>45</sup></a><span class="mw-ref" id="cxcite_ref-44" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-44"></p></td> <td></td> </tr> <tr class="even"> <td><p><a href="Mimas" title="wikilink">Mimas</a></p></td> <td><p><a href="Herschel_Dağı" title="wikilink">Herschel</a> merkezî zirve</p></td> <td><p>7 km (takriben)<a href="#fn46" class="footnote-ref" id="fnref46" role="doc-noteref"><sup>46</sup></a></p></td> <td><p>3.5</p></td> <td><p><a href="Çarpma_krateri" title="wikilink">çarpma</a></p></td> <td><p>Ayrıca <a href="Güneş_Sistemi&#39;ndeki_en_büyük_kraterlerin_listesi" title="wikilink">Güneş Sistemi'ndeki en büyük kraterlerin listesine</a> bakınız</p></td> </tr> <tr class="odd"> <td><p><a href="Dione" title="wikilink">Dione</a></p></td> <td><p><a href="Janiculum_Dorsa" title="wikilink">Janiculum Dorsa</a></p></td> <td><p>1,5 km<a href="#fn47" class="footnote-ref" id="fnref47" role="doc-noteref"><sup>47</sup></a></p></td> <td><p>0,27</p></td> <td><p><a href="Orojenez" title="wikilink">tektonik</a>{{refn|Bâriz şekilde büzülmeyle meydana gelmiştir.<ref name = "Beddingfield_2014">{{Kaynak</p></td> <td><p>ad1 = C. B. | soyadı1 = Beddingfield | ad2 = J. P. | soyadı2 = Emery | ad3 = D. M. | soyadı3 = Burr</p></td> </tr> <tr class="even"> <td><p><a href="Titan_(uydu)" title="wikilink">Titan</a></p></td> <td><p><a href="Mithrim_Montes" title="wikilink">Mithrim Montes</a></p></td> <td><p>2,0 km<a href="#fn48" class="footnote-ref" id="fnref48" role="doc-noteref"><sup>48</sup></a></p></td> <td><p>0,078</p></td> <td><p><a href="Orojenez" title="wikilink">tektonik</a> (?)</p></td> <td><p>Küresel çekilmeyle meydana gelmiş olabilir<a href="#fn49" class="footnote-ref" id="fnref49" role="doc-noteref"><sup>49</sup></a></p></td> </tr> <tr class="odd"> <td><p><a href="Doom_Mons" title="wikilink">Doom Mons</a></p></td> <td><p>1,45 km<a href="#fn50" class="footnote-ref" id="fnref50" role="doc-noteref"><sup>50</sup></a></p></td> <td><p>0,056</p></td> <td><p>buz-volkanik (?)</p></td> <td><p>1,7 km derinliğinde yıkıntı yeri olan Sotra Patera'ya komşu collapse feature<a href="#fn51" class="footnote-ref" id="fnref51" role="doc-noteref"><sup>51</sup></a></p></td> <td></td> </tr> <tr class="even"> <td><p><a href="İapetus_(uydu)" title="wikilink">İapetus</a></p></td> <td><p>ekvator sırta</p></td> <td><p>20 km (takriben)<a href="#fn52" class="footnote-ref" id="fnref52" role="doc-noteref"><sup>52</sup></a></p></td> <td><p>2,7</p></td> <td><p>belirsiz{{refn|Meydana geliş hipotezi, kabuğun tekrar düzenlenmesiyle beraber bağıl kilitlenme (<a href="İng." title="wikilink">İng.</a> <em></em>) ile <a href="yassılaşmış_sferoid" title="wikilink">yassılaşmasını</a> içerip<ref name="Porco2005">{{Dergi kaynağı | soyadı1=Porco | ad1=C. C.| yazarbağı = Carolyn Porco</p></td> <td><p>yazarlarıgöster=etal</p></td> </tr> <tr class="odd"> <td><p><a href="Oberon_(uydu)" title="wikilink">Oberon</a></p></td> <td><p>isimsiz ("limb mountain")</p></td> <td><p>11 km (takriben)<a href="#fn53" class="footnote-ref" id="fnref53" role="doc-noteref"><sup>53</sup></a></p></td> <td><p>1.4</p></td> <td><p><a href="Çarpma_krateri" title="wikilink">çarpma</a> (?)</p></td> <td><p><em>Voyager 2</em> buluşmasından kısa bir müddet sonra 6 km değeri söylendi<a href="#fn54" class="footnote-ref" id="fnref54" role="doc-noteref"><sup>54</sup></a></p></td> </tr> <tr class="even"> <td><p><a href="Plüton" title="wikilink">Plüton</a></p></td> <td><p><a href="Piccard_Mons" title="wikilink">Piccard Mons</a><span class="mw-ref" id="cxcite_ref-Pluto_58-0" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-Pluto_58-0"><a href="#fn55" class="footnote-ref" id="fnref55" role="doc-noteref"><sup>55</sup></a><a href="#fn56" class="footnote-ref" id="fnref56" role="doc-noteref"><sup>56</sup></a></p></td> <td><p>~5,6 km<a href="#fn57" class="footnote-ref" id="fnref57" role="doc-noteref"><sup>57</sup></a></p></td> <td><p>0,47</p></td> <td><p>buz-volkanik (?)</p></td> <td><p>~220 km çapında<a href="#fn58" class="footnote-ref" id="fnref58" role="doc-noteref"><sup>58</sup></a></p></td> </tr> <tr class="odd"> <td><p><a href="Wright_Mons" title="wikilink">Wright Mons</a><span class="mw-ref" id="cxcite_ref-Pluto_58-1" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-Pluto_58-1"><a href="#fn59" class="footnote-ref" id="fnref59" role="doc-noteref"><sup>59</sup></a><a href="#fn60" class="footnote-ref" id="fnref60" role="doc-noteref"><sup>60</sup></a></p></td> <td><p>~4,0 km<a href="#fn61" class="footnote-ref" id="fnref61" role="doc-noteref"><sup>61</sup></a></p></td> <td><p>0,34</p></td> <td><p>buz-volkanik (?)</p></td> <td><p>~160 km boyunda;<a href="#fn62" class="footnote-ref" id="fnref62" role="doc-noteref"><sup>62</sup></a> zirvedeki çukur ~56 km çapında<a href="#fn63" class="footnote-ref" id="fnref63" role="doc-noteref"><sup>63</sup></a></p></td> <td></td> </tr> <tr class="even"> <td><p><a href="Norgay_Montes" title="wikilink">Norgay Montes</a><span class="mw-ref" id="cxcite_ref-Pluto_58-2" rel="dc:references" contenteditable="false" data-sourceid="cite_ref-Pluto_58-2"><a href="#fn64" class="footnote-ref" id="fnref64" role="doc-noteref"><sup>64</sup></a></p></td> <td><p>≤ 3,5 km<a href="#fn65" class="footnote-ref" id="fnref65" role="doc-noteref"><sup>65</sup></a></p></td> <td><p>0,30</p></td> <td><p>tektonik<a href="#fn66" class="footnote-ref" id="fnref66" role="doc-noteref"><sup>66</sup></a> (?)</p></td> <td><p>Su buzundan meydana gelir;<a href="#fn67" class="footnote-ref" id="fnref67" role="doc-noteref"><sup>67</sup></a> Tenzing Norgay'dan adını almıştır.<a href="#fn68" class="footnote-ref" id="fnref68" role="doc-noteref"><sup>68</sup></a></p></td> <td></td> </tr> </tbody> </table> <section class="footnotes footnotes-end-of-document" role="doc-endnotes"> <hr /> <ol> <li id="fn1" role="doc-endnote"><a href="#fnref1" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn2" role="doc-endnote"><a href="#fnref2" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn3" role="doc-endnote"><a href="#fnref3" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn4" role="doc-endnote"><a href="#fnref4" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn5" role="doc-endnote"><a href="#fnref5" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn6" role="doc-endnote"><a href="#fnref6" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn7" role="doc-endnote"><a href="#fnref7" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn8" role="doc-endnote"><a href="#fnref8" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn9" role="doc-endnote"><a href="#fnref9" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn10" role="doc-endnote"><a href="#fnref10" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn11" role="doc-endnote"><a href="#fnref11" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn12" role="doc-endnote"><a href="#fnref12" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn13" role="doc-endnote"><a href="#fnref13" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn14" role="doc-endnote"><em>Mount Everest</em> (1:50.000 scale map), prepared under the direction of Bradford Washburn for the Boston Museum of Science, the Swiss Foundation for Alpine Research, and the <a href="National_Geographic_Society" title="wikilink">National Geographic Society</a>, 1991, <a href=":en:Special:BookSources/3855151059" title="wikilink">ISBN 3-85515-105-9</a><a href="#fnref14" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn15" role="doc-endnote"><a href="#fnref15" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn16" role="doc-endnote"><a href="#fnref16" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn17" role="doc-endnote"><a href="#fnref17" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn18" role="doc-endnote"><a href="#fnref18" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn19" role="doc-endnote"><a href="#fnref19" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn20" role="doc-endnote"><a href="#fnref20" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn21" role="doc-endnote"><a href="#fnref21" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn22" role="doc-endnote">Carr, M.H., 2006, The Surface of Mars, Cambridge, 307 p.<a href="#fnref22" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn23" role="doc-endnote"><a href="#fnref23" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn24" role="doc-endnote"><a href="#fnref24" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn25" role="doc-endnote"><a href="#fnref25" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn26" role="doc-endnote"><a href="#fnref26" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn27" role="doc-endnote"><a href="#fnref27" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn28" role="doc-endnote"><a href="#fnref28" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn29" role="doc-endnote"><a href="#fnref29" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn30" role="doc-endnote">JMARS MOLA elevation dataset.<a href="#fnref30" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn31" role="doc-endnote"><a href="#fnref31" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn32" role="doc-endnote"><a href="#fnref32" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn33" role="doc-endnote"><a href="#fnref33" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn34" role="doc-endnote"><a href="#fnref34" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn35" role="doc-endnote"><a href="#fnref35" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn36" role="doc-endnote"><a href="#fnref36" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn37" role="doc-endnote"><a href="#fnref37" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn38" role="doc-endnote"><a href="#fnref38" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn39" role="doc-endnote"><a href="#fnref39" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn40" role="doc-endnote"><a href="#fnref40" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn41" role="doc-endnote"><a href="#fnref41" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn42" role="doc-endnote"><a href="#fnref42" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn43" role="doc-endnote"><a href="#fnref43" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn44" role="doc-endnote"><a href="#fnref44" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn45" role="doc-endnote"><a href="#fnref45" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn46" role="doc-endnote"><a href="#fnref46" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn47" role="doc-endnote"><a href="#fnref47" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn48" role="doc-endnote"><a href="#fnref48" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn49" role="doc-endnote"><a href="#fnref49" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn50" role="doc-endnote"><a href="#fnref50" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn51" role="doc-endnote"><a href="#fnref51" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn52" role="doc-endnote"><a href="#fnref52" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn53" role="doc-endnote"><a href="#fnref53" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn54" role="doc-endnote"><a href="#fnref54" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn55" role="doc-endnote"><a href="#fnref55" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn56" role="doc-endnote"><a href="#fnref56" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn57" role="doc-endnote"><a href="#fnref57" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn58" role="doc-endnote"><a href="#fnref58" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn59" role="doc-endnote"><a href="#fnref59" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn60" role="doc-endnote"><a href="#fnref60" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn61" role="doc-endnote"><a href="#fnref61" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn62" role="doc-endnote"><a href="#fnref62" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn63" role="doc-endnote"><a href="#fnref63" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn64" role="doc-endnote"><a href="#fnref64" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn65" role="doc-endnote"><a href="#fnref65" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn66" role="doc-endnote"><a href="#fnref66" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn67" role="doc-endnote"><a href="#fnref67" class="footnote-back" role="doc-backlink">↩︎</a></li> <li id="fn68" role="doc-endnote"><a href="#fnref68" class="footnote-back" role="doc-backlink">↩︎</a></li> </ol> </section>

Galeri

Aşağıdaki resimler tabandan tepeye yüksekliği azalan şekilde gösterilmiştir.

Dosya:Vesta 20110701 cropped.jpg |100.000 km'den Dawn tarafından görüntülenen Vesta'nın kratere Rheasilvia'nın merkezî zirve. Dosya:Olympus Mons alt.jpg |Viking 1'in 1978 yılında gördüğü şekliyle Mars Olympus Mons Dosya:Iapetus equatorial ridge.jpg |İapetus'un ekvator sırtının Cassini görüntüsü Dosya:PIA00323 Boösaule Montes crop2 sharp.png |İo'nun en yüksek tepesi olan Boösaule Montes "Güney"'in Voyager 1 fotoğrafı Dosya:Ascraeus Mons Flank Terraces.jpg |Ascraeus Mons (MOLA altimetre ile THEMIS IR, 3× dikey uzatması), Mars Dosya:PIA00327 crop 2x.png |İo'nun Euboea Montes'i (sol üst altta), Haemus Montes (sağ alt); kuzey soldadır Dosya:Mauna Kea from Mauna Loa Observatory, Hawaii - 20100913.jpg |Mauna Kea (Mauna Loa'dan), Hawaii Dosya:Teide 2011.jpg|Teide, Kanarya Adaları Dosya:Herschel crater on Mimas PIA12570 crop.jpg |Mimas'ın üzerindeki Herschel Krateri'nin fotoğrafı ve merkezî zirvesinin Cassini fotoğrafı Dosya:Maxwell Montes of planet Venus.jpg |Venüs üzerindeki Maxwell Montes'deki Skadi Mons'un Magellan tarafından çekilen radar görüntüsü Dosya:Mount McKinley Denali Closeup 2800px.jpg |Denali (McKinley Dağı), Alaska Dosya:673885main PIA15986-full full.jpg |Aeolis Mons ("Sivri Dağ"), Mars (Curiosity keşif aracından 6 Ağustos 2012'de çekilmiş resmi).[a] Dosya:Venus - 3D Perspective View of Maat Mons.jpg |Maat Mons, Venüs (radar resmi artı altimetre, 10× dikeyde mübalaga edilmiştir) Dosya:Apollo 15 Rover, Irwin.jpg |Apollo 15'in iniş yerine yakın çekilmiş (1971) Ay'daki Mons Hadley Dosya:Everest kalapatthar.jpg |Everest Dağı (Chomolungma/Sagarmāthā), Tibet/Nepal Dosya:PIA20349 crop - Ceres' Ahuna Mons side view.jpg |Dawn'ın LAMO aletiyle çekilmiş Ceres'deki Ahuna Mons Dosya:Pluto possible cryovolcano - Wright Mons.jpg |Plüton'un muhtemel buz volkanı Wright Mons'ın merkezî çöküntüsü Dosya:Pluto's Norgay Montes.png |New Horizons'un Plüton'daki sırla Norgay Montes'ten çektiği resim

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