Sputnik Planitia

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Sputnik Planitia
Sputnik Planitia nomenclature.png
Annotated map of Sputnik Planitia on Pluto
Location Tombaugh Regio, Pluto
Coordinates 20°N 180°E / 20°N 180°E / 20; 180Coordinates: 20°N 180°E / 20°N 180°E / 20; 180
Eponym Sputnik 1

Sputnik Planitia /ˈspʌtnɪk pləˈnɪʃiə/,[note 1][note 2], originally Sputnik Planum,[2] is a high-albedo ice-covered basin on Pluto, about 1,050 by 800 km (650 by 500 mi) in size[3], named after Earth's first artificial satellite. It constitutes the western lobe of the heart-shaped Tombaugh Regio. Sputnik Planitia lies mostly in the northern hemisphere, but extends across the equator. Much of it has a surface of irregular polygons separated by troughs, interpreted as convection cells in the relatively soft nitrogen ice. The polygons average about 33 km (21 mi) across.[3] In some cases troughs are populated by blocky mountains or hills, or contain darker material.[4] There appear to be wind streaks on the surface with evidence of sublimation.[5][6][7] The dark streaks are a few kilometers long and all aligned in the same direction.[4] The planitia also contains pits apparently formed by sublimation.[4] No craters were detectable by New Horizons, implying a surface less than 10 million years old.[8] Modeling sublimation pit formation yields a surface age estimate of 180000+90000
−40000
years.[9] Near the northwest margin is a field of transverse dunes (perpendicular to the wind streaks), spaced about 0.4 to 1 km apart, that are thought to be composed of 200-300 μm diameter particles of methane ice derived from the nearby Al-Idrisi Montes.[10][11]

Composition[edit]

The ice composing the basin is thought to consist primarily of nitrogen ice, with smaller fractions of carbon monoxide and methane ice, although relative proportions are uncertain.[12] At Pluto's ambient temperature of 38 K (−235.2 °C; −391.3 °F), nitrogen and carbon monoxide ices are denser and much less rigid than water ice, making glacial-like flows possible; nitrogen ice is the most volatile.[3]

Origin[edit]

Sputnik Planitia may have originated as an impact basin that subsequently collected volatile ices.[3] The size of the hypothetical impactor has been estimated as 150-300 km.[13] Alternatively, it has been suggested that the accumulation of ices in this location depressed the surface there, leading to formation of a basin via a positive feedback process without an impact.[14]

The accumulation of several kilometers of nitrogen ice in the basin was in part a consequence of its higher surface pressure, which leads to a higher N2 condensation temperature.[15] The positive temperature gradient of Pluto's atmosphere contributes to making a topographic depression a cold trap.[16][17]

A high seasonal thermal inertia of Pluto's surface is an important driver of deposition of nitrogen ice at low latitudes. These latitudes receive less annual insolation than Pluto's polar regions due to its high obliquity (122.5°).[18] The coldest regions on Pluto, on average, are at 30° N. and S. latitude; early in Pluto's history, ice would tend to accumulate at these latitudes in a runaway process due to the positive feedback association of increased albedo, cooling and further ice deposition (similar to the ice segregation that occurred on Iapetus). Simulations suggest that over a period of about a million years, the runaway process would collect much of the ice into a single cap even in the absence of a preexisting basin.[19]

The accumulation of dense nitrogen ice would have contributed to making Sputnik Planitia a positive gravity anomaly, but by itself would not have been sufficient to overcome the topographic depression associated with the basin. However, other effects of an impact event (see below) could have also contributed to such an anomaly. A positive gravity anomaly could have caused polar wander, reorienting the spin axis of Pluto to put the planitia near the Pluto-Charon tidal axis (the minimum-energy configuration).[16][17] Sputnik Planitia is presently close to the anti-Charon point on Pluto, a result that has less than a 5% probability of arising by chance.[17] If Sputnik Planitia was created by an impact, then explaining the positive gravity anomaly requires the presence of a subsurface liquid water ocean; isostatic uplift of the ocean under the basin would account for most of the anomaly.[20] Gradual freezing of such an ocean, in combination with polar wander and the loading of Sputnik Planitia with ice, would also explain the extensional tectonic features seen across Pluto.[17][20] Alternatively, if the accumulation of ice in a single cap (without an impact) created a positive gravity anomaly that reoriented Pluto prior to formation of a basin, the tidal bulge raised by Charon would tend to maintain Pluto's orientation even if the positive anomaly later disappeared.[19]

Convection cells[edit]

Geologic map of Sputnik Planitia and surroundings (context), with convection cell margins outlined in black

The polygonal structure is a sign of convection of the nitrogen/carbon monoxide ice, with ice warmed by heat from the interior welling up in the center of cells, spreading and then sinking at the ridged margins.[21][22] Convection cells have about 100 m of vertical relief, with the highest points being at their centers.[23][24] Modeling of nitrogen ice convection cells suggests a depth of about one tenth their width, or 3–4 km for most of the planitia, and a maximum flow rate of about 7 cm per year.[3] Cell margins can become pinched off and abandoned as cells evolve.[23] Many of the cells are covered by Sublimation pits. These pits grow larger by sublimation during transport from the centers to the edges of convection cells. Using their size distribution, scientists have estimated a convection velocity of 13.8+4.8
−3.8
cm per year, implying a surface age of 180000+90000
−40000
years.[9]

Other obvious indications of ice flow visible in images of the planitia include examples of valley-type glaciers flowing down into the basin from adjacent eastern highlands (the right lobe of Tombaugh Regio), presumably in response to deposition of nitrogen ice there,[12] as well as ice from the planitia flowing into and filling adjacent depressions. The planitia has numerous blocky hills (one to several km across) that form aggregations at cell margins up to 20 km across; these may represent floating chunks of detached water ice crust that were carried onto the planitia by glacial flow and were then collected into troughs by the convection.[3] In some cases the hills seem to form chains along the entry paths of glaciers. The hills may also congregate in nonconvecting regions when they get stuck at locations where the nitrogen ice becomes too shallow.[25]

The planitia has numerous pits that are thought to result from fracturing and sublimation of nitrogen ice; these pits also collect in the margins of convection cells.[3] Often the bottoms of the pits are dark, which may represent an accumulation of tholins left behind by the subliming ice, or a dark substrate below the planitia, if the pits penetrate all the way through the ice. In regions of the planitia where convection cells are not apparent, the pits are more numerous.

Bordering montes[edit]

A topographic image of the Sputnik Planitia basin, showing the rising scarps bordering the glacial plains. The banding is an artefact of the camera.

On its northwest, Sputnik Planitia is bordered by a chaotic set of blocky mountains, the al-Idrisi Montes, which may have formed via the collapse of adjacent water ice highlands onto the planitia.[3]

On its southwest, the planitia is bordered by the Hillary Montes, rising 1.6 km (0.99 mi; 5,200 ft)[26] above the surface, and, further south, the Norgay Montes, rising 3.4 km (2.1 mi; 11,000 ft)[27] above the surface. These mountains also have a chaotic, blocky character. The mountains were named after Sir Edmund Hillary, New Zealand mountaineer, and Nepalese Sherpa mountaineer Tenzing Norgay, who were the first climbers to reach the summit of the highest peak on Earth, Mount Everest, on 29 May 1953.[28] Some groups of hills in the basin are named after spacecraft; for example, “Coleta de Dados”, in honor of the first Brazilian satellite launched into space.[29]

Immediately to the southwest of the Norgay Montes (context) is a large, circular mountain with a central depression, Wright Mons. It has been identified as a possible cryovolcano.[30][31]

Naming[edit]

The informal name Sputnik Planum was first announced by the New Horizons team on a press conference on 24 July 2015. A planum is a flat region of higher elevation (a plateau). When topographical data was analyzed in early 2016,[32] it became clear that Sputnik is actually a basin, and the informal name was changed to Sputnik Planitia later that year.[2][33] The name was still informal because it had not yet been adopted by the International Astronomical Union (IAU). On 7 September 2017, the name was officially approved together with the names of Tombaugh Regio and 12 other nearby surface features.[34]

Gallery[edit]

High resolution LORRI mosaic of a convecting region of Sputnik Planitia (context), up to its northwestern 'shoreline' (released 7 January 2016). Note isolated quadruple cell junction at lower right.[23]
Floating water ice hills in Sputnik Planitia (context) aggregate along convection cell margins.[25]
Closeup of sublimation pits (context) at the edge of the planitia's cellular terrain (illumination is from the upper left)
Additional views of sublimation pits (context) in convecting (left) and nonconvecting regions; some (left) have dark material within
High-resolution view of sublimation pits (context) in southeast Sputnik Planitia
High-resolution enhanced-color views of Sputnik Planitia's northwestern (top; context) and western (context) margins, showing the transition (left to right) from ancient cratered highland (Viking Terra), to disrupted, blocky terrain (the al-Idrisi Montes), to the young, flat, textured surface of the planitia, with a few water ice hills (the Coleta de Dados Colles, bottom). Near the top of the lower image, at the border between the highlands and the montes, is a flat feature 30 km across (at its widest), Alcyonia Lacus, a frozen body of nitrogen[36][37] similar to the 'dark cellular plains' area of Sputnik Planitia.[38] In both images, fields of methane ice particle dunes are visible within the convection cells.[10]
Pluto - Norgay Montes (left foreground); Hillary Montes (skyline); Sputnik Planitia (right)
Near-sunset view includes several layers of atmospheric haze.

Animated videos[edit]

See also[edit]

References[edit]

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  8. ^ Marchis, F.; Trilling, D. E. (20 January 2016). "The Surface Age of Sputnik Planum, Pluto, Must Be Less than 10 Million Years". PLOS ONE. 11 (1): e0147386. arXiv:1601.02833Freely accessible. Bibcode:2016PLoSO..1147386T. doi:10.1371/journal.pone.0147386. PMC 4720356Freely accessible. PMID 26790001. 
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  10. ^ a b Telfer, M.W.; Parteli, E.R.J.; Radebaugh, J.; et al. (2018-06-01). "Dunes on Pluto". Science. 360 (6392): 992–997. Bibcode:2018Sci...360..992T. doi:10.1126/science.aao2975. 
  11. ^ Hayes, A.G. (2018-06-01). "Dunes across the Solar System". Science. 360 (6392): 960–961. Bibcode:2018Sci...360..960H. doi:10.1126/science.aat7488. 
  12. ^ a b Umurhan, O. (8 January 2016). "Probing the Mysterious Glacial Flow on Pluto's Frozen 'Heart'". blogs.nasa.gov. NASA. Retrieved 24 January 2016. 
  13. ^ McKinnon, William B.; Schenck, P. M. (23 March 2017). "Impact origin of Sputnik Planitia basin, Pluto" (PDF). 48th Lunar and Planetary Science Conference. 
  14. ^ Witze, A. (21 October 2016). "Icy heart could be key to Pluto's strange geology". Nature. 538 (7626): 439–439. Bibcode:2016Natur.538..439W. doi:10.1038/nature.2016.20856. PMID 27786223. 
  15. ^ Bertrand, T.; Forget, F. (19 September 2016). "Observed glacier and volatile distribution on Pluto from atmosphere–topography processes". Nature. 540 (7631): 86–89. Bibcode:2016Natur.540...86B. doi:10.1038/nature19337. PMID 27629517. 
  16. ^ a b Keane, J. T.; Matsuyama, I. (2016). "Pluto followed its heart: true polar wander of Pluto due to the formation and evolution of Sputnik Planum" (PDF). 47th Lunar and Planetary Science Conference. Woodlands, Texas. p. 2348. 
  17. ^ a b c d Keane, J. T.; Matsuyama, I.; Kamata, S.; Steckloff, J. K. (16 November 2016). "Reorientation and faulting of Pluto due to volatile loading within Sputnik Planitia". Nature. 540 (7631): 90–93. Bibcode:2016Natur.540...90K. doi:10.1038/nature20120. PMID 27851731. 
  18. ^ Bertrand, T.; Forget, F. (19 September 2016). "Observed glacier and volatile distribution on Pluto from atmosphere–topography processes". Nature. 540 (7631): 86–89. Bibcode:2016Natur.540...86B. doi:10.1038/nature19337. PMID 27629517. 
  19. ^ a b Hamilton, D. P.; Stern, S. A.; Moore, J. M.; Young, L. A. (30 November 2016). "The rapid formation of Sputnik Planitia early in Pluto's history". Nature. 540 (7631): 97–99. Bibcode:2016Natur.540...97H. doi:10.1038/nature20586. PMID 27905411. 
  20. ^ a b Nimmo, F.; et al. (16 November 2016). "Reorientation of Sputnik Planitia implies a subsurface ocean on Pluto". Nature. 540 (7631): 94–96. Bibcode:2016Natur.540...94N. doi:10.1038/nature20148. PMID 27851735. 
  21. ^ McKinnon, W. B.; et al. (1 June 2016). "Convection in a volatile nitrogen-ice-rich layer drives Pluto's geological vigour". Nature. 534 (7605): 82–85. Bibcode:2016Natur.534...82M. doi:10.1038/nature18289. 
  22. ^ Trowbridge, A. J.; Melosh, H. J.; Steckloff, J. K.; Freed, A. M. (1 June 2016). "Vigorous convection as the explanation for Pluto's polygonal terrain". Nature. 534 (7605): 79–81. Bibcode:2016Natur.534...79T. doi:10.1038/nature18016. PMID 27251278. 
  23. ^ a b c Keeter, B. (11 January 2016). "'X' Marks a Curious Corner on Pluto's Icy Plains". NASA. Retrieved 24 January 2016. 
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  38. ^ White, O. L.; et al. (1 May 2017). "Geological mapping of Sputnik Planitia on Pluto" (PDF). Icarus. 287: 261–286. Bibcode:2017Icar..287..261W. doi:10.1016/j.icarus.2017.01.011. 

Notes[edit]

  1. ^ Also /ˈspʊtnɪk pləˈnɪʃiə/
  2. ^ "Planitia" means "low plain".[1]