ผลต่างระหว่างรุ่นของ "ผู้ใช้:EZBELLA/กระบะทราย6"

|-

| rowspan="2" | [[ดาวศุกร์]]

| {{convert|abbr=on|6.4|km|mi|1}} (ค่าประมาณ)<ref name = "planetology">{{cite book| title = Planetology : Unlocking the secrets of the solar system|author1=Jones, Tom |author2=Stofan, Ellen | date = 2008| publisher = National Geographic Society| location = Washington, D.C.| page = 74| isbn = 978-1-4262-0121-9| url = https://books.google.com/books?id=SL-BszT15s0C&pg=PA74}}</ref>

| 0.11

|-

| rowspan="5" | [[โลก]]

| {{convert|abbr=on|10.2|km|mi|1}}<ref name = "Highest_Points">{{cite web |url=http://science.nationalgeographic.com/science/earth/surface-of-the-earth/mountains-article/ |title=Mountains: Highest Points on Earth |publisher=National Geographic Society |accessdate=19 September 2010}}</ref>

| 0.16

| 4.6&nbsp;km on north face, 3.6&nbsp;km on south face;{{refn |Peak is {{convert|abbr=on|8.8|km|mi|1}} above sea level, and over {{convert|abbr=on|13|km|mi|1}} above the oceanic [[abyssal plain]].| group = n }} listed only because it has the highest elevation (8.8&nbsp;km) above sea level

<!-- K2 is probably not #4 |-

|{{convert|abbr=on|2.8|to|3.2|km|mi|1}} -->

|-

| rowspan="3" | [[ดวงจันทร์]]

| {{convert|abbr=on|5.5|km|mi|1}}<ref name="price"/><ref name="moore"/>

| 0.32

| Formed by the [[Mare Imbrium|Imbrium impact]]

|-

| {{convert|abbr=on|4.5|km|mi|1}}<ref name="price">{{cite book | author=Fred W. Price | title=The Moon observer's handbook | publisher=Cambridge University Press | location=London | date=1988 | isbn= 0-521-33500-0}}</ref><ref name="moore">{{cite book | last=Moore | first=Patrick | authorlink = Patrick Moore | title=On the Moon | publisher=Cassell & Co | location=London | date=2001 }}</ref>

| 0.26

| Formed by the [[Mare Imbrium|Imbrium impact]]

|-

| {{convert|abbr=on|1.1|km|mi|2}}<ref name="laps07">{{Citation

|author1=Wöhler, C. |author2=Lena, R. |author3=Pau, K. C. | title=The Lunar Dome Complex Mons Rümker: Morphometry, Rheology, and Mode of Emplacement

|-

| rowspan=7| [[ดาวอังคาร]]

| {{convert|abbr=on|21.9|km|mi|0}}<ref name="Plescia2004">{{cite journal|last1=Plescia|first1=J. B.|title=Morphometric properties of Martian volcanoes|journal=Journal of Geophysical Research|volume=109|issue=E3|date=2004|issn=0148-0227|doi=10.1029/2002JE002031|bibcode = 2004JGRE..109.3003P }}</ref><ref name="Carr2007" />

| 0.65

| Rises 26&nbsp;km above northern plains,<ref name="Comins2012">{{cite book|last=Comins|first=Neil F.| title=Discovering the Essential Universe|url=https://books.google.com/books?id=qK_4mNve1DYC&pg=PA148&dq=mons+olympus+height&hl=en&sa=X&ei=YzCQT-GpIcH22AXz852ABQ&ved=0CDoQ6AEwAQ#v=onepage&q=mons%20olympus%20height&f=false|accessdate=23 December 2012|date=4 January 2012|publisher=Macmillan|isbn=978-1-4292-5519-6}}</ref> 1000&nbsp;km away. Summit calderas are 60 x 80&nbsp;km wide, up to 3.2&nbsp;km deep;<ref name="Carr2007">{{cite book|author=Carr, Michael H.|title=The Surface of Mars|url=https://books.google.com/books?id=uLHlJ6sjohwC|date=11 January 2007|publisher=Cambridge University Press|isbn=978-1-139-46124-5|page=51}}</ref> scarp around margin is up to 8&nbsp;km high.<ref name="Lopes1982">{{cite journal|last1=Lopes|first1=R.|last2=Guest|first2=J. E.|last3=Hiller|first3=K.|last4= Neukum|first4= G.|title=Further evidence for a mass movement origin of the Olympus Mons aureole|journal=Journal of Geophysical Research|volume=87|issue= B12|date=January 1982|pages= 9917–9928|doi= 10.1029/JB087iB12p09917|bibcode=1982JGR....87.9917L}}</ref>

|-

|{{convert|abbr=on|14.9|km|mi|1}}<ref name="Plescia2004"/>

| 0.44

| Tallest of the three [[Tharsis Montes]]

|-

|{{convert|abbr=on|12.6|km|mi|1}}<ref name="Plescia2004"/>

| 0.37

| Highest volcano in [[Elysium (volcanic province)|Elysium]]

|-

| {{convert|abbr=on|11.7|km|mi|1}}<ref name="Plescia2004"/>

| 0.35

| Summit [[caldera]] is {{convert|abbr=on|108|to|138|km|mi|0}} across<ref name="Plescia2004"/>

|-

| {{convert|abbr=on|8.4|km|mi|1}}<ref name="Plescia2004"/>

| 0.25

| Summit caldera is {{convert|abbr=on|4.8|km|mi|1}} deep<ref name="Plescia2004"/>

|-

| {{convert|abbr=on|6.2|km|mi|1}}<ref name = "MOLA">JMARS MOLA elevation dataset. Christensen, P.; Gorelick, N.; Anwar, S.; Dickenshied, S.; Edwards, C.; Engle, E. (2007) "[http://adsabs.harvard.edu/abs/2007AGUFM.P11E..01C New Insights About Mars From the Creation and Analysis of Mars Global Datasets];" American Geophysical Union, Fall Meeting, abstract #P11E-01.</ref>

| 0.18

| Among the highest nonvolcanic peaks on Mars, formed by the [[Hellas Planitia|Hellas impact]]

|-

| {{convert|abbr=on|4.5|to|5.5|km|mi|1}}<ref name="themis">{{cite web

| url = http://themis.asu.edu/features/galecrater

|-

| [[4 เวสตา]]

|{{convert|abbr=on|22|km|mi|0}}<ref name="Vega">{{cite web

|last=Vega

|-

| [[ซีรีส]]

| {{convert|abbr=on|4|km|mi|1}}<ref name = "Ceres">{{cite web

| title = Dawn's First Year at Ceres: A Mountain Emerges | website = JPL Dawn website

|-

| rowspan="4" | [[ไอโอ (ดาวบริวาร)|ไอโอ]]

| last = Perry | first = Jason | title = Boösaule Montes

| work = Gish Bar Times blog

| Has a {{convert|abbr=on|15|km|mi|0}} high scarp on its SE margin<ref name="SchenkHargitai2001">{{cite journal|last1=Schenk|first1=P.|last2=Hargitai|first2=H.|last3=Wilson|first3=R.|last4=McEwen|first4=A.|last5=Thomas|first5=P.|title=The mountains of Io: Global and geological perspectives from Voyager and Galileo|journal= Journal of Geophysical Research|volume= 106|issue= E12|date= 2001|pages= 33201|issn=0148-0227|doi=10.1029/2000JE001408|bibcode = 2001JGR...10633201S }}</ref>

|-

| {{convert|abbr=on|12.7|km|mi|1}} (ค่าประมาณ)<ref name="SchenkHargitai2001"/><ref name = "Ionian Mons">{{cite web

| last = Schenk | first = P. | authorlink =

| Has the form of a curved double ridge

|-

| {{convert|abbr=on|10.3|to|13.4|km|mi|1}}<ref name = "Euboea Montes">{{cite web

| last = Schenk | first = P. | authorlink =

| accessdate = 30 June 2012}}</ref>{{refn |Among the Solar System's largest<ref name = "Martel"/>| group = n }}

|-

|{{convert|abbr=on|2.5|km|mi|1}} (ค่าประมาณ)<ref name="MooreMcEwen1986">{{cite journal|last1=Moore|first1=J. M.|last2=McEwen|first2=A. S.|last3=Albin|first3=E. F.|last4=Greeley|first4=R.|title=Topographic evidence for shield volcanism on Io|journal=Icarus |volume=67|issue=1 |date=1986|pages=181–183 |issn=0019-1035|doi=10.1016/0019-1035(86)90183-1|bibcode = 1986Icar...67..181M }}</ref><ref name = "unnamed_Io">{{cite web

| last = Schenk | first = P. | authorlink =

|-

| [[ไมมัส (ดาวบริวาร)|ไมมัส]]

| {{convert|abbr=on|7|km|mi|0}} (ค่าประมาณ)<ref name="Moore Schenk et al. 2004">{{cite journal| doi = 10.1016/j.icarus.2004.05.009| last1 = Moore| first1 = Jeffrey M.| last2 = Schenk| first2 = Paul M.| last3 = Bruesch| first3 = Lindsey S.| last4 = Asphaug| first4 = Erik| last5 = McKinnon| first5 = William B.| date=October 2004 | title = Large impact features on middle-sized icy satellites| journal = Icarus| volume = 171| issue = 2| pages = 421–443| url = http://planets.oma.be/ISY/pdf/article_Icy.pdf| format = PDF| bibcode = 2004Icar..171..421M| ref = {{sfnRef|Moore Schenk et al.|2004}}

}}</ref>

|-

| [[ไดโอนี]]

| {{convert|abbr=on|1.5|km|mi|1}}<ref name = "Hammond2013">{{Cite journal | doi = 10.1016/j.icarus.2012.12.021| title = Flexure on Dione: Investigating subsurface structure and thermal history| journal = [[Icarus (journal)|Icarus]]| volume = 223| issue = 1| pages = 418–422| date = March 2013| last1 = Hammond | first1 = N. P. | last2 = Phillips | first2 = C. B. | last3 = Nimmo | first3 = F.| last4 = Kattenhorn | first4 = S. A. | bibcode = 2013Icar..223..418H}}</ref>

| 0.27

|-

| rowspan="2" | [[ไททัน (ดาวบริวาร)|ไททัน]]

| ≤ {{convert|abbr=on|3.3|km|mi|1}}<ref name = "PIA20023">{{cite web | url = http://photojournal.jpl.nasa.gov/catalog/PIA20023 | title = PIA20023: Radar View of Titan's Tallest Mountains | date = 2016-03-24 | website = Photojournal.jpl.nasa.gov | publisher = [[Jet Propulsion Laboratory]] | access-date = 2016-03-25}}</ref>

| 0.13

| doi = 10.1029/2010JE003592 | accessdate = 5 July 2012 |bibcode = 2010JGRE..11510002M }}</ref>

|-

| {{convert|abbr=on|1.45|km|mi|2}}<ref name = "Lopes_2013">{{cite journal

| last = Lopes | first = R. M. C. | authorlink = Rosaly Lopes-Gautier

|-

| [[ไอแอพิตัส (ดาวบริวาร)|ไอแอพิตัส]]

| {{convert|abbr=on|20|km|mi|0}} (ค่าประมาณ)<ref name="GieseDenk2008">{{cite journal|last=Giese|first=B.|author2=Denk, T. |author3=Neukum, G. |author4=Roatsch, T. |author5=Helfenstein, P. |author6=Thomas, P. C. |author7=Turtle, E. P. |author8=McEwen, A. |author9= Porco, C. C. |title=The topography of Iapetus' leading side|journal=Icarus|volume=193|issue=2|date=2008|pages=359–371|issn=0019-1035|url= http://www.geoinf.fu-berlin.de/publications/denk/2008/GieseEtAl_IapetusTopography_Icarus_2008.pdf |doi=10.1016/j.icarus.2007.06.005|bibcode = 2008Icar..193..359G }}</ref>

| 2.7

|-

| [[โอเบอร็อน (ดาวบริวาร)|โอเบอร็อน]]

| {{convert|abbr=on|11|km|mi|0}} (ค่าประมาณ)<ref name="Moore Schenk et al. 2004"/>

| 1.4

|-

| rowspan="3" | [[พลูโต]]

| url = http://pluto.jhuapl.edu/News-Center/News-Article.php?page=20151109

| title = At Pluto, New Horizons Finds Geology of All Ages, Possible Ice Volcanoes, Insight into Planetary Origins

| access-date = 2015-11-09}}</ref>

|-

| ~{{convert|abbr=on|4.0|km|mi|1}}<ref name = "News2015-11-09"/>

| 0.34

| access-date = 2015-11-09}}</ref>

|-

| last1 = Hand | first1 = E. | last2 = Kerr | first2 = R.

| title = Potential geysers spotted on Pluto

|-

| rowspan="2" | {{sort|15|[[แครอน (ดาวบริวาร)|แครอน]]}}

| {{sort|045| ≥ {{convert|abbr=on|4.5|km|mi|1}}<ref name="Beyer2018" />}}

| {{sort|0743|0.74}}

| [[Vulcan Planitia]], the southern plains, has several isolated peaks, possibly tilted crustal blocks<ref name="Beyer2018" />

|-

| {{sort|040| ~{{convert|abbr=on|4.0|km|mi|1}}<ref name="Beyer2018" />}}

| {{sort|0660|0.66}}