292:; overlap relations indicate that the plains are younger than the more densely cratered units. The plains also embay the Caloris Formation and account in particular for the skeletal map pattern of the Van Eyck Formation. The ubiquitous distribution of smooth plains in topographically low regions supports the hypothesis that these materials were deposited in a fluid or semifluid state as basin ejecta or volcanic flows. The plains are thought to be slightly younger but dose to the same age as the Caloris Basin materials; thus parts of the plains are probably Caloris ejecta, either impact melt or very fluid debris flows. No obvious secondary craters from Caloris have been recognized on the smooth plains. The presence of large patches of smooth plains in the floor of the Tolstoj Basin and in irregular depressions in the extreme southeastern part of the map indicates that at least some of these materials may be volcanic. However, the absence of unequivocal lava-flow fronts and well-defined volcanic vents such as those of the
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northwest limit of recognizable
Tolstoj ejecta, is a subdued scarp some 450 km long. Rejuvenation of earlier faults or fractures by subsequent impacts probably occurred throughout the history of the planet. Thus, except for the lobate compressional scarps, it is difficult to separate internally produced structures from those of the complex impact history of Mercury. The azimuthal trends of all lineaments mapped within the quadrangle are, however, dominantly northwest (315°) and northeast (35°â40°). A minor, almost north-south trend is also observed. This situation is reminiscent of the so-called lunar grid on the Moon, which is generally ascribed to planetwide internal causes.
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with the smooth plains material. Certain patches of these intermediate plains, where clearly rougher and possibly older, are mapped as the intermediate plains material. These patches occur mostly within the floors of ancient craters and are distinguished by a slightly greater density of small craters and a lower incidence of small bright-halo craters than are found on the smooth plains material. The presence of plains intermediate in roughness and crater density between the oldest plains and the post-Caloris plains suggests that plains formation was a more or less continuous process that spanned much of the early geologic history of
Mercury.
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period was followed by impact of the asteroid that created the
Caloris Basin and deposits of the Caloris Group. Although the intermediate plains were resurfaced at the time of the Caloris impact, their formation actually extended from the end of the intercrater plains-forming period through the end of formation of c3 craters. At about the time the last c3 craters and the first c4 craters were being formed, the upper surface of the smooth plains and Caloris floor plains were being emplaced. Part of the smooth plains and Caloris floor plains materials may have been deposited during or immediately after the Caloris event.
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control of the ejecta pattern by prebasin structures, (2) preferential burial along structural trends of an originally symmetrical ejecta blanket by the intercrater plains material, or (3) formation of
Tolstoj by an oblique impact from the northwest that produced an ejecta blanket with bilateral symmetry and little or no deposition uprange. Analysis of stereo-photography of Tolstoj ejecta northeast of the crater suggests that this deposit has been upwarped to a higher elevation relative to the surrounding plains.
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cratering events on
Mercury, according to apparent superposition relations. In particular, the unit appears to overlap the entire northwest side of the Tolstoj Basin, a feature indicating that the intercrater plains in this region probably do not represent the remains of the primordial surface of the planet. A complex history of contemporaneous craters and plains formation is therefore suggested. A detailed discussion of the origin of the intercrater plains on the Moon and Mercury was given by Strom.
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outer scarp is present around most of the visible part of
Caloris, better seen in the Shakespeare quadrangle to the north. This scarp is generally coincident with the transition between the massifs of the Caloris Montes Formation and the lineated facies of the Van Eyck Formation. The roughly rectilinear outlines of massifs within the Caloris Montes suggest structural control by a prebasin fracture pattern. The much lower, discontinuous outer scarp is considered to be the feeble equivalent of the
43:
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that we have adopted on the present map. This stratigraphy is patterned after that used in and around the
Orientale Basin on the Moon and should aid in the future recognition of pre- and post-Caloris events over a broad expanse of the surface of Mercury. Crater degradation chronologies, such as the one modified from Trask, and correlations between plains units on the basis of crater frequency may aid in tying much of the remainder of the surface of Mercury to the Caloris event.
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and the fractures cutting them have a crude rhombic pattern that led Strom and others to conclude that the plains materials subsided and then were gently uplifted to produce the open tension fractures observed. The ridges in the floor of
Caloris lack the crenulated crests that are common on lunar ridges. Regardless of the origin and tectonic history of these plains, it seems clear that they represent a deep basin fill that obscures the original floor of the Caloris Basin.
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appearance and their general lack of well-defined craters larger than about 50 km in diameter. Malin showed the plains to contain highly eroded remnants of large craters and basins that are only very shallow circular depressions. These intercrater plains are, however, marked by a very high density of superposed craters that are small (5â10 km diameter), elongate, shallow, and probably
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side. Diffuse patches of material of dark albedo lie outside the innermost ring. The central part of the basin is covered by smooth plains material. Hapke and others have suggested that the dark-albedo materials associated with the
Tolstoj Basin margins are distinctly bluer than the surrounding terrain, whereas the plains filling the interior are distinctly redder.
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particularly Strom and others, Melosh, and Melosh and
Dzurisin, have ascribed these ridges to compression and a slight shortening of the crust of Mercury after formation of most of the present surface. Some ridges, however, may represent flow fronts, but their estimated heights of several hundred meters would require formation by extraordinarily viscous lavas.
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an extensive radial ridge-and-valley system with minor concentric scarps and lineaments. These features are considered for the most part as gouges and depositional plumes from secondary cratering within the Van Eyck; the remarkably straight ridges and steep walls, however, suggest formation by fracturing.
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or gouges; others may represent traces of an ancestral structural pattern that partly controlled the excavation of the craters and basin. The lineaments may have been enhanced or preserved by the gentle upwarping of this region of Tolstoj ejecta discussed above. The largest lineament, which marks the
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to the north. Undoubtedly, the ejecta also influences a large part of the as-yet-unseen terrain to the west. A stratigraphic and structural comparison between the Orientale and Caloris Basins has been made by McCauley. McCauley and others have proposed a formal rock stratigraphy for the Caloris Basin
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After the emplacement of most of the smooth plains, some late c3 craters and all c4 and c5 craters, including the large crater Mozart, were superposed on all previous deposits. The recognizable geologic history of the quadrangle ends with these events probably several billion years ago. A summary of
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scarp around Orientale. Like the Cordillera, it probably lies outside the limit of the crater of excavation. Its poor development and spacing much closer to the edge of the basin may be due to the greater mercurian gravity, as described by Gault and others. The Van Eyck Formation is characterized by
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Patches of less cratered, smoother, less rolling plains occur throughout the quadrangle, but their recognition is highly dependent on the resolution and lighting of individual Mariner 10 frames. Therefore, because their distribution cannot now be mapped accurately, many of these patches are included
874:
Prepared for the National Aeronautics and Space Administration by U.S. Department of the Interior, U.S. Geological Survey. Published in hardcopy as USGS Miscellaneous Investigations Series Map Iâ1199, as part of the Atlas of Mercury, 1:5,000,000 Geologic Series. (Hardcopy is available for sale from
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to the many large craters superposed on the plains. Superposition of crater ejecta over parts of intercrater plains in other areas indicates that some large craters formed in a preexisting intercrater plains unit. On the other hand, the intercrater plains material partly postdates some of the major
91:
deposits of the Caloris Group that are embayed and covered by broad expanses of smooth plains. The southeast half of the quadrangle is dominated by ancient crater deposits, by nondescript rolling to hummocky plains materials between individual craters, and by isolated patches of nondescript plains.
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Lobate scarps or ridges, which are best seen within the smooth plains material and vary locally within the intercrater plains material, are generally steep on one side and gently dipping on the other. Some, like the lunar mare ridges, appear to mark the outlines of subjacent craters. Most workers,
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The Tolstoj Basin is encompassed by parts of at least three ragged and discontinuous inward-facing scarps. Lineated ejecta is best developed in the vicinity of and beyond the outer scarp, whereas blocky materials occur between the inner and outer scarps. These relations are similar to those around
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are the most prominent structural features in the quadrangle. The main Caloris Montes scarp is thought to approximate the edge of the basin of excavation of Caloris and is probably a structural and stratigraphic counterpart of the Montes Rook scarp around the Orientale Basin on the Moon. A subdued
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in the floor of Orientale on the Moon but do not show the radial and circumferential ridges characteristic of the Maunder that led to its interpretation as a basin floor unit. The Caloris floor plains have a more open, coarser fracture pattern than does the Maunder. In addition, the Caloris ridges
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Unlike the Imbrium-related stratigraphy of Shoemaker and Hackman, that devised for Mercury is a rock rather than a time stratigraphy. It recognizes the existence of an orderly, in essence isochronous sequence of mappable units around Caloris that are similar in character to those recognized around
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occurred very early in the history of the quadrangle. Two ragged, discontinuous rings approximately 356 km and 510 km in diameter encompass the structure but are poorly developed on its north and northeast sides; a third partial ring with a diameter of 466 km occurs on its southeast
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related to the formation of individual craters and therefore may not represent late-stage volcanic fill or volcanic modification of the more youthful mercurian craters. Schultz suggested compositional differences or endogenic modification as possible causes of the color contrasts among the floor,
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The interpretable geologic history within the Tolstoj quadrangle begins with the period of formation of the intercrater plains, which persisted until shortly after impact of the asteroid that created the Tolstoj Basin. After this event was a period of only slightly less intense bombardment. This
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The sharpness of the single rim-scarp of Mozart reflects the youth (younger than the smooth plains) of this large impact. The position of Mozart at the west terminator of the Mariner 10 image data precludes visibility of its floor and thus hides any evidence of a possible central uplift or inner
219:
blanket around two-thirds of its circumference. The ejecta tends to be blocky and only weakly lineated between the inner and outer rings. Radial lineations with a slight swirly pattern are best seen on the southwest side of Tolstoj. The unusual rectilinear map pattern of the ejecta suggests: (1)
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The rolling to hummocky plains that lie between large craters in the southeastern part of the quadrangle make up the oldest recognizable map unit, the intercrater plains material. The plains were originally described as intercrater by Trask and Guest, who noted their level to gently rolling
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spacecraft, which orbited Mercury from 2008 to 2015, mapped the planet in its entirety at much higher resolution and in more wavelengths of light than Mariner 10. It obtained topographic, reflectance, magnetic, gravitational, and other types of geophysical data from orbit in addition to the
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Only a small part of the ridge and fracture system that characterizes the floor of Caloris is within the quadrangle. The ridges in the floor of Caloris, which are like those within the smooth plains, do not appear to be as complex as lunar mare ridges and are cut by numerous open
316:(67 km diameter). The dark ejecta and floors plains of these craters are distinctly redder than the surrounding plains, whereas their anomalously bright floor patches, central peaks, and wall areas are distinctly bluer. None of these dark-halo craters has associated bright
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passage. The "hot pole" at 180° lies within the Tolstoj quadrangle; at perihelion, equatorial temperatures range from about 100 K at local midnight to 700 K at local noon. This daily range of 600 K is greater than that on any other body in the solar system.
288:âbut many smaller patches occur in crater floors and other topographic depressions within the heavily cratered terrain in the southeastern part of the quadrangle. The plains are characterized by a relatively sparse crater density and an abundance of mare-type
320:, although secondary craters are well preserved. Compositional implications of contrasting color differences for mercurian crater and plains materials have been discussed by Hapke and others. The bright, bluish areas in these craters are now known to be
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Shoemaker, E. M., and Hackman, R. J., 1962, Stratigraphic basis for a lunar time scale, in Kopal, Zdenek, and Mikhailov, Z. K., eds., The Moon: International Astronomical Union Symposium, 14th, Leningrad, U.S.S.R., 1960: London, Academic Press, p.
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on the Moon, it is surrounded by an extensive and well-preserved ejecta blanket. As on the Moon, where ejecta from the better preserved basins was used to construct a stratigraphy, the ejecta from the Caloris Basin also can be used as a
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International Astronomical Union, Commission 16, 1977, Physical study of planets and satellites, in Proceedings 16th General Assembly 1976, International Astronomical Union Transactions, v. 16B, p. 325, 331â336,
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Numerous faint lineaments are visible within the quadrangle, especially in the area between the Tolstoj Basin and the large crater Zeami to the northeast. Many of these lineaments may be faint secondary-
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Scott, D. H., McCauley, J. F., and West, M. N., 1977, Geologic map of the west side of the Moon: U.S. Geological Survey Miscellaneous Investigations Series Map I-1034, scale 1:5,000,000.
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100:(285 km diameter) is a prominent feature in the western part of the area; its extensive ejecta blanket and secondary crater field are superposed on the smooth plains of
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Despite Tolstoj's great age and its embayment by the ancient inter-crater plains, it retains an extensive and remarkably well preserved, radially lineated
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Schultz, P. H., 1977, Endogenic modification of impact craters on Mercury: Physics of the Earth and Planetary Interiors, v. 15, no. 2â3, p. 202â219.
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The Caloris floor plains material is a special problem and is not included in the Caloris Group. The plains have some features in common with the
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Gault, D. E.; Guest, J. E.; Murray, J. B.; Dzurisin, D.; Malin, M. C. (1975). "Some comparisons of impact craters on Mercury and the Moon".
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Small patches of very smooth plains material occur in the floors of many of the youngest craters. The patches may consist of fallback and
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Melosh, H. J., and Dzurisin, Daniel, 1978, Mercurian global tectonics: A consequence of tidal despinning?: Icarus, v. 35, p 227â236.
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McCauley, J. F.; Guest, J. E.; Schaber, G. G.; Trask, N. J.; Greeley, Ronald (1980). "Stratigraphy of the Caloris Basin, Mercury".
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Hapke, Bruce; Danielson, G. E. Jr; Klaasen, Kenneth; Wilson, Lionel (1975). "Photometric observations of Mercury from Mariner 10".
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multiring basin, about 350 km in diameter, is in the south-central part of the quadrangle. The large, well-preserved crater
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Caloris, although Tolstoj is less than half its size and is much more severely degraded by later impact cratering.
251:. This ejecta is recognizable to a distance of about one basin diameter in the Tolstoj quadrangle and the adjacent
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of 87.97 days. Therefore, at its equator, longitudes 0° and 180° are subsolar points ("hot poles") near alternate
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runs from 144 to 216° longitude and -25 to 25° latitude. It was provisionally called "Tir", but renamed after
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edited by Sean C. Solomon, Larry R. Nittler, and Brian J. Anderson. Cambridge Planetary Science. Chapter 12.
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the generalized geology history of Mercury was given by Guest and O'Donnell and Davies and others.
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photographic coverage was available for only the eastern two-thirds of the Tolstoj quadrangle. The
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are the only two on Mercury where tensional forces can now be seen to have shaped the surface.
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The largest single expanse of the smooth plains material surrounds the Caloris Basinâmostly in
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Blewett, D. T., Ernst, C. M., Murchie, S. L., and Vilas, F., 2018. Mercury's Hollows. In
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U.S. Geological Survey, Information Services, Box 25286, Federal Center, Denver, CO 80225)
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87:. This basin, about 1550 km in diameter, is surrounded by a discontinuous annulus of
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Strom, R. G.; Trask, N. J.; Guest, J. E. (1975). "Tectonism and volcanism on Mercury".
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Strom, R. G., 1977, Origin and relative age of lunar and mercurian intercrater plains:
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Melosh, H. J., 1977, Global tectonics of a despun planet: Icarus, v. 31, p. 221â243.
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Trask, N. J.; Guest, J. E. (1975). "Preliminary geologic terrain map of Mercury".
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Guest, J. E.; OâDonnell, W. P. (1977). "Surface history of Mercury: A review".
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the better preserved impact basins of the Moon such as Orientale, Imbrium, and
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Mercury's rotation period of 58.64 days is in two-thirds resonance with its
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by the International Astronomical Union in 1976. Also called Phaethontias.
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Part of eastern Tolstoj quadrangle is shown in the foreground, including
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Malin, M. C. (1976). "Observations of intercrater plains on Mercury".
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is especially significant from a stratigraphic standpoint. Like the
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Davies, M. E.; Dwornik, S. E.; Gault, D. E.; Strom, R. G. (1978).
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Davies, M. E.; Dwornik, S. E.; Gault, D. E.; Strom, R. G. (1978).
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465:. National Aeronautics and Space Administration. pp. 1â128.
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435:. National Aeronautics and Space Administration. p. 15.
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867:"Geologic Map Of The Tolstoj (H-8) Quadrangle Of Mercury"
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81:, which is the largest and best preserved basin seen by
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prevents a firm conclusion regarding volcanic origin.
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The Triumph of the Farmer or Industry and Parasitism
334:
The circumbasin scarps around Caloris, Tolstoj, and
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690:McCauley, J. F. (1977). "Orientale and Caloris".
417:"Bizarre spider scar found on Mercury's surface"
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865:Schaber, Gerald G.; John F. McCauley (1980).
304:wall, and rim areas of the dark-halo craters
8:
3691:Posthumous Notes of the Hermit FĂ«dor Kuzmich
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693:Physics of the Earth and Planetary Interiors
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598:Physics of the Earth and Planetary Interiors
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352:gashes. This area and its antipode in the
156:is to the west of Tolstoj quadrangle, and
3923:Surface features of Mercury by quadrangle
3773:Lev Tolstoy and the Russia of Nicholas II
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168:are to the northwest and northeast, and
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3205:Walk in the Light While There is Light
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2933:
2921:
2909:
2883:
2871:
2859:
2847:
7:
429:For location of albedo features see
176:are to the southwest and southeast.
119:, appears to be associated with the
23:Tolstoj quadrangle as mapped by the
3285:Recollections of a Billiard-marker
14:
77:It contains the southern part of
3892:
3891:
3633:The Kingdom of God Is Within You
3550:The Light Shines in the Darkness
2773:
2762:
2761:
419:. NewScientist.com news service.
415:Shiga, David (30 January 2008).
819:Journal of Geophysical Research
660:Journal of Geophysical Research
617:Journal of Geophysical Research
493:Journal of Geophysical Research
3467:A Dialogue Among Clever People
3418:How Much Land Does a Man Need?
3390:Evil Allures, But Good Endures
1:
3453:The Two Brothers and the Gold
3327:God Sees the Truth, But Waits
1305:Skinakas (hypothetical basin)
601:, v. 15, no. 2â3, p. 156â172.
475:. Special Publication SP-423.
445:. Special Publication SP-423.
207:The impact that produced the
3765:Departure of a Grand Old Man
3334:The Prisoner of the Caucasus
2594:Hypothetical moon of Mercury
754:10.1016/0019-1035(81)90166-4
714:10.1016/0031-9201(77)90033-4
583:10.1016/0083-6656(77)90006-X
523:Geophysical Research Letters
3558:The Fruits of Enlightenment
312:(97 km diameter), and
3944:
2642:Mercury-crossing asteroids
227:
3887:
3656:The Inevitable Revolution
3495:Work, Death, and Sickness
3474:The Coffee-House of Surat
3271:The Cutting of the Forest
3068:
3009:
2945:
2897:
2833:
2828:
2756:
928:
802:Mercury: The View After
92:The ancient and degraded
3802:Story of One Appointment
3197:The Death of Ivan Ilyich
308:(129 km diameter),
268:Younger plains materials
3869:Aylmer and Louise Maude
2723:Colonization of Mercury
886:Tolstoj quadrangle maps
831:10.1029/jb080i017p02444
672:10.1029/jb080i017p02478
638:10.1029/JB080i017p02431
543:10.1029/GL003i010p00581
505:10.1029/jb080i017p02461
174:Michelangelo quadrangle
3874:Translators of Tolstoy
3593:A History of Yesterday
2822:Quadrangles on Mercury
253:Shakespeare quadrangle
185:Older plains materials
166:Shakespeare quadrangle
59:
39:
28:
3534:The Power of Darkness
3376:Where Love Is, God Is
3165:A Landowner's Morning
2068:Kuan Han-Chʻing
45:
34:
22:
16:Quadrangle on Mercury
3664:A Calendar of Wisdom
2118:Li Chʻing-Chao
354:Discovery quadrangle
162:Raditladi quadrangle
158:Beethoven quadrangle
107:Low-albedo features
3759:Christian anarchism
3649:A Letter to a Hindu
3625:What Is to Be Done?
3609:The Gospel in Brief
3574:The Cause of It All
3542:The First Distiller
3369:An Old Acquaintance
3278:Sevastopol Sketches
3213:The Kreutzer Sonata
2574:Inter-crater plains
746:1981Icar...47..184M
706:1977PEPI...15..220M
630:1975JGR....80.2431H
575:1977VA.....20..273G
563:Vistas in Astronomy
535:1976GeoRL...3..581M
154:Eminescu quadrangle
3918:Tolstoj quadrangle
3833:Tolstoj quadrangle
3776:(1928 documentary)
3754:Tolstoyan movement
3460:A Lost Opportunity
3397:Wisdom of Children
3355:Diary of a Lunatic
3320:The Porcelain Doll
66:in the equatorial
64:Tolstoj quadrangle
60:
40:
29:
3905:
3904:
3864:Vladimir Chertkov
3566:The Living Corpse
3411:Promoting a Devil
3404:The Three Hermits
3245:The Forged Coupon
3028:
3027:
3023:
3022:
2788:
2787:
2731:
2730:
2650:
2649:
2582:
2581:
1628:ChĆng ChʼĆl
1623:Chiang Kʻui
1262:Santa MarĂa Rupes
1131:Mearcair Planitia
1116:Borealis Planitia
1111:ApÄrangi Planitia
825:(17): 2444â2460.
666:(17): 2478â2507.
624:(17): 2431â2443.
499:(17): 2461â2477.
472:978-1-114-27448-8
442:978-1-114-27448-8
364:structural ring.
341:Montes Cordillera
274:Maunder Formation
170:Neruda quadrangle
160:is to the east.
109:Solitudo Neptunii
68:region of Mercury
3935:
3895:
3894:
3879:Tolstoy scholars
3789:The Last Station
3439:Croesus and Fate
3362:Quench the Spark
3348:What Men Live By
3181:Family Happiness
3055:
3048:
3041:
3032:
2831:
2815:
2808:
2801:
2792:
2777:
2765:
2764:
2661:
2607:
2128:Liang Kʻai
1333:Africanus Horton
1257:Resolution Rupes
1247:Enterprise Rupes
1227:Antoniadi Dorsum
1194:Goldstone Vallis
1189:Goldstone Catena
1161:Utaridi Planitia
1146:Stilbon Planitia
1126:Caloris Planitia
946:
915:
908:
901:
892:
873:
871:
853:
850:
844:
841:
835:
834:
814:
808:
798:
792:
789:
780:
776:
770:
767:
758:
757:
727:
718:
717:
700:(2â3): 220â250.
687:
676:
675:
655:
642:
641:
611:
602:
593:
587:
586:
558:
547:
546:
518:
509:
508:
488:
477:
476:
463:Atlas of Mercury
458:
447:
446:
433:Atlas of Mercury
427:
421:
420:
412:
406:
402:
380:Geologic history
244:Orientale Basins
79:Caloris Planitia
3943:
3942:
3938:
3937:
3936:
3934:
3933:
3932:
3908:
3907:
3906:
3901:
3883:
3844:
3816:
3749:Yasnaya Polyana
3742:Life and legacy
3737:
3696:
3683:The Decembrists
3670:
3580:
3521:
3509:Alyosha the Pot
3502:Three Questions
3251:
3152:
3077:
3064:
3059:
3029:
3024:
3014:
3000:
2988:
2976:
2964:
2950:
2938:
2926:
2914:
2902:
2888:
2876:
2864:
2852:
2838:
2824:
2819:
2789:
2784:
2752:
2727:
2711:
2694:
2665:
2646:
2628:
2598:
2578:
2552:
2473:Sholem Aleichem
1309:
1300:Rembrandt Basin
1295:Raditladi Basin
1290:Pantheon Fossae
1277:
1271:
1242:Discovery Rupes
1232:Adventure Rupes
1219:
1213:
1204:Haystack Vallis
1199:Haystack Catena
1171:
1165:
1151:Suisei Planitia
1141:Sobkou Planitia
1103:
1097:
1085:
1079:
991:
975:
956:Albedo features
937:
924:
919:
882:
869:
864:
861:
856:
851:
847:
842:
838:
816:
815:
811:
799:
795:
790:
783:
777:
773:
768:
761:
729:
728:
721:
689:
688:
679:
657:
656:
645:
613:
612:
605:
594:
590:
560:
559:
550:
529:(10): 581â584.
520:
519:
512:
490:
489:
480:
473:
460:
459:
450:
443:
430:
428:
424:
414:
413:
409:
403:
399:
395:
382:
332:
270:
232:
226:
205:
203:Basin materials
187:
182:
17:
12:
11:
5:
3941:
3939:
3931:
3930:
3925:
3920:
3910:
3909:
3903:
3902:
3900:
3899:
3888:
3885:
3884:
3882:
3881:
3876:
3871:
3866:
3861:
3852:
3850:
3846:
3845:
3843:
3842:
3841:
3840:
3830:
3824:
3822:
3818:
3817:
3815:
3814:
3806:
3798:
3793:
3785:
3777:
3769:
3761:
3756:
3751:
3745:
3743:
3739:
3738:
3736:
3735:
3729:
3723:
3717:
3711:
3704:
3702:
3698:
3697:
3695:
3694:
3687:
3678:
3676:
3672:
3671:
3669:
3668:
3660:
3652:
3645:
3637:
3629:
3621:
3617:What I Believe
3613:
3605:
3597:
3588:
3586:
3582:
3581:
3579:
3578:
3570:
3562:
3554:
3546:
3538:
3529:
3527:
3523:
3522:
3520:
3519:
3516:After the Ball
3512:
3505:
3498:
3491:
3484:
3481:The Young Tsar
3477:
3470:
3463:
3456:
3449:
3442:
3435:
3428:
3421:
3414:
3407:
3400:
3393:
3386:
3379:
3372:
3365:
3358:
3351:
3344:
3337:
3330:
3323:
3316:
3309:
3302:
3295:
3288:
3281:
3274:
3267:
3259:
3257:
3253:
3252:
3250:
3249:
3241:
3237:Father Sergius
3233:
3229:Master and Man
3225:
3217:
3209:
3201:
3193:
3185:
3177:
3169:
3160:
3158:
3154:
3153:
3151:
3150:
3142:
3134:
3126:
3118:
3110:
3102:
3094:
3085:
3083:
3079:
3078:
3076:
3075:
3069:
3066:
3065:
3060:
3058:
3057:
3050:
3043:
3035:
3026:
3025:
3021:
3020:
3007:
3006:
2994:
2982:
2970:
2957:
2956:
2944:
2932:
2920:
2908:
2895:
2894:
2882:
2870:
2858:
2845:
2844:
2829:
2826:
2825:
2820:
2818:
2817:
2810:
2803:
2795:
2786:
2785:
2783:
2782:
2770:
2757:
2754:
2753:
2751:
2750:
2745:
2739:
2737:
2733:
2732:
2729:
2728:
2726:
2725:
2719:
2717:
2713:
2712:
2710:
2709:
2702:
2700:
2696:
2695:
2693:
2692:
2691:(2018âpresent)
2686:
2678:
2669:
2667:
2658:
2652:
2651:
2648:
2647:
2645:
2644:
2638:
2636:
2630:
2629:
2627:
2626:
2621:
2615:
2613:
2604:
2600:
2599:
2597:
2596:
2590:
2588:
2584:
2583:
2580:
2579:
2577:
2576:
2571:
2566:
2560:
2558:
2554:
2553:
2551:
2550:
2545:
2540:
2535:
2530:
2525:
2520:
2515:
2510:
2505:
2500:
2495:
2490:
2485:
2480:
2475:
2470:
2465:
2460:
2455:
2450:
2445:
2440:
2435:
2430:
2425:
2420:
2415:
2410:
2405:
2400:
2395:
2390:
2385:
2380:
2375:
2370:
2365:
2360:
2355:
2350:
2345:
2340:
2335:
2330:
2325:
2320:
2315:
2310:
2305:
2300:
2295:
2290:
2285:
2280:
2275:
2270:
2265:
2260:
2255:
2250:
2245:
2240:
2235:
2230:
2225:
2220:
2215:
2210:
2205:
2200:
2195:
2190:
2185:
2180:
2175:
2170:
2165:
2160:
2155:
2150:
2145:
2140:
2135:
2130:
2125:
2120:
2115:
2110:
2105:
2100:
2095:
2090:
2085:
2080:
2075:
2070:
2065:
2060:
2055:
2050:
2045:
2040:
2035:
2030:
2025:
2020:
2015:
2010:
2005:
2000:
1995:
1990:
1985:
1980:
1975:
1970:
1965:
1960:
1955:
1950:
1945:
1940:
1935:
1930:
1925:
1920:
1915:
1910:
1905:
1900:
1895:
1890:
1885:
1880:
1875:
1870:
1868:Guido d'Arezzo
1865:
1860:
1855:
1850:
1845:
1840:
1835:
1830:
1825:
1820:
1815:
1810:
1805:
1800:
1795:
1790:
1785:
1780:
1775:
1770:
1765:
1760:
1755:
1750:
1745:
1740:
1735:
1730:
1725:
1720:
1715:
1710:
1705:
1700:
1695:
1690:
1685:
1680:
1675:
1670:
1665:
1660:
1655:
1650:
1645:
1640:
1635:
1630:
1625:
1620:
1615:
1610:
1605:
1600:
1595:
1590:
1585:
1580:
1575:
1570:
1565:
1560:
1555:
1550:
1545:
1540:
1535:
1530:
1525:
1520:
1515:
1510:
1505:
1500:
1495:
1490:
1485:
1480:
1475:
1470:
1465:
1460:
1455:
1450:
1445:
1440:
1435:
1430:
1425:
1420:
1415:
1410:
1405:
1400:
1395:
1390:
1385:
1380:
1375:
1370:
1365:
1360:
1355:
1350:
1345:
1340:
1335:
1330:
1325:
1319:
1317:
1311:
1310:
1308:
1307:
1302:
1297:
1292:
1287:
1281:
1279:
1273:
1272:
1270:
1269:
1267:Victoria Rupes
1264:
1259:
1254:
1249:
1244:
1239:
1234:
1229:
1223:
1221:
1215:
1214:
1212:
1211:
1206:
1201:
1196:
1191:
1186:
1184:Arecibo Vallis
1181:
1179:Arecibo Catena
1175:
1173:
1167:
1166:
1164:
1163:
1158:
1153:
1148:
1143:
1138:
1133:
1128:
1123:
1118:
1113:
1107:
1105:
1099:
1098:
1096:
1095:
1093:Caloris Montes
1089:
1087:
1081:
1080:
1078:
1077:
1072:
1067:
1062:
1057:
1052:
1047:
1042:
1037:
1032:
1027:
1022:
1017:
1012:
1007:
1001:
999:
993:
992:
990:
989:
983:
981:
977:
976:
974:
973:
971:Magnetic field
968:
963:
958:
952:
950:
943:
939:
938:
936:
935:
929:
926:
925:
920:
918:
917:
910:
903:
895:
889:
888:
881:
880:External links
878:
877:
876:
860:
857:
855:
854:
845:
836:
809:
793:
781:
771:
759:
740:(2): 184â202.
719:
677:
643:
603:
588:
569:(2): 273â300.
548:
510:
478:
471:
448:
441:
422:
407:
396:
394:
391:
381:
378:
331:
328:
290:wrinkle ridges
286:Budh Planitiae
269:
266:
249:marker horizon
228:Main article:
225:
222:
204:
201:
186:
183:
181:
178:
128:orbital period
117:Solitudo Maiae
113:Solitudo Helii
15:
13:
10:
9:
6:
4:
3:
2:
3940:
3929:
3926:
3924:
3921:
3919:
3916:
3915:
3913:
3898:
3890:
3889:
3886:
3880:
3877:
3875:
3872:
3870:
3867:
3865:
3862:
3859:
3858:
3854:
3853:
3851:
3847:
3839:
3836:
3835:
3834:
3831:
3829:
3826:
3825:
3823:
3819:
3812:
3811:
3807:
3804:
3803:
3799:
3797:
3794:
3791:
3790:
3786:
3783:
3782:
3778:
3775:
3774:
3770:
3767:
3766:
3762:
3760:
3757:
3755:
3752:
3750:
3747:
3746:
3744:
3740:
3733:
3730:
3727:
3724:
3721:
3718:
3715:
3712:
3709:
3706:
3705:
3703:
3699:
3692:
3688:
3685:
3684:
3680:
3679:
3677:
3673:
3666:
3665:
3661:
3658:
3657:
3653:
3650:
3646:
3643:
3642:
3638:
3635:
3634:
3630:
3627:
3626:
3622:
3619:
3618:
3614:
3611:
3610:
3606:
3603:
3602:
3598:
3595:
3594:
3590:
3589:
3587:
3583:
3576:
3575:
3571:
3568:
3567:
3563:
3560:
3559:
3555:
3552:
3551:
3547:
3544:
3543:
3539:
3536:
3535:
3531:
3530:
3528:
3524:
3517:
3513:
3510:
3506:
3503:
3499:
3496:
3492:
3489:
3485:
3482:
3478:
3475:
3471:
3468:
3464:
3461:
3457:
3454:
3450:
3447:
3443:
3440:
3436:
3433:
3429:
3426:
3422:
3419:
3415:
3412:
3408:
3405:
3401:
3398:
3394:
3391:
3387:
3384:
3383:Ivan the Fool
3380:
3377:
3373:
3370:
3366:
3363:
3359:
3356:
3352:
3349:
3345:
3342:
3341:The Bear Hunt
3338:
3335:
3331:
3328:
3324:
3321:
3317:
3314:
3310:
3307:
3303:
3300:
3296:
3293:
3292:The Snowstorm
3289:
3286:
3282:
3279:
3275:
3272:
3268:
3265:
3261:
3260:
3258:
3256:Short stories
3254:
3247:
3246:
3242:
3239:
3238:
3234:
3231:
3230:
3226:
3223:
3222:
3218:
3215:
3214:
3210:
3207:
3206:
3202:
3199:
3198:
3194:
3191:
3190:
3186:
3183:
3182:
3178:
3175:
3174:
3170:
3167:
3166:
3162:
3161:
3159:
3155:
3148:
3147:
3143:
3140:
3139:
3135:
3132:
3131:
3130:Anna Karenina
3127:
3124:
3123:
3122:War and Peace
3119:
3116:
3115:
3111:
3108:
3107:
3103:
3100:
3099:
3095:
3092:
3091:
3087:
3086:
3084:
3080:
3074:
3071:
3070:
3067:
3063:
3056:
3051:
3049:
3044:
3042:
3037:
3036:
3033:
3018:
3013:
3008:
3004:
2999:
2992:
2987:
2980:
2975:
2968:
2963:
2958:
2954:
2949:
2942:
2937:
2930:
2925:
2918:
2913:
2906:
2901:
2896:
2892:
2887:
2880:
2875:
2868:
2863:
2856:
2851:
2846:
2842:
2837:
2832:
2827:
2823:
2816:
2811:
2809:
2804:
2802:
2797:
2796:
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2608:
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2570:
2569:Ghost craters
2567:
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2539:
2536:
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2209:
2206:
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2159:
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2154:
2151:
2149:
2146:
2144:
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2126:
2124:
2121:
2119:
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2111:
2109:
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2036:
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2031:
2029:
2026:
2024:
2023:Judah Ha-Levi
2021:
2019:
2016:
2014:
2011:
2009:
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2004:
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1996:
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1336:
1334:
1331:
1329:
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1320:
1318:
1316:
1312:
1306:
1303:
1301:
1298:
1296:
1293:
1291:
1288:
1286:
1285:Caloris Basin
1283:
1282:
1280:
1274:
1268:
1265:
1263:
1260:
1258:
1255:
1253:
1250:
1248:
1245:
1243:
1240:
1238:
1235:
1233:
1230:
1228:
1225:
1224:
1222:
1216:
1210:
1209:Simeiz Vallis
1207:
1205:
1202:
1200:
1197:
1195:
1192:
1190:
1187:
1185:
1182:
1180:
1177:
1176:
1174:
1168:
1162:
1159:
1157:
1154:
1152:
1149:
1147:
1144:
1142:
1139:
1137:
1136:Odin Planitia
1134:
1132:
1129:
1127:
1124:
1122:
1121:Budh Planitia
1119:
1117:
1114:
1112:
1109:
1108:
1106:
1100:
1094:
1091:
1090:
1088:
1084:Mountains and
1082:
1076:
1073:
1071:
1068:
1066:
1063:
1061:
1058:
1056:
1053:
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1048:
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1036:
1033:
1031:
1028:
1026:
1023:
1021:
1018:
1016:
1013:
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1008:
1006:
1003:
1002:
1000:
998:
994:
988:
985:
984:
982:
978:
972:
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967:
964:
962:
959:
957:
954:
953:
951:
947:
944:
940:
934:
931:
930:
927:
923:
916:
911:
909:
904:
902:
897:
896:
893:
887:
884:
883:
879:
868:
863:
862:
858:
849:
846:
840:
837:
832:
828:
824:
820:
813:
810:
806:
805:
797:
794:
788:
786:
782:
775:
772:
766:
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760:
755:
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747:
743:
739:
735:
734:
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724:
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707:
703:
699:
695:
694:
686:
684:
682:
678:
673:
669:
665:
661:
654:
652:
650:
648:
644:
639:
635:
631:
627:
623:
619:
618:
610:
608:
604:
600:
599:
592:
589:
584:
580:
576:
572:
568:
564:
557:
555:
553:
549:
544:
540:
536:
532:
528:
524:
517:
515:
511:
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502:
498:
494:
487:
485:
483:
479:
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468:
464:
457:
455:
453:
449:
444:
438:
434:
426:
423:
418:
411:
408:
401:
398:
392:
390:
386:
379:
377:
374:
373:crater chains
369:
365:
361:
357:
355:
351:
345:
342:
337:
329:
327:
325:
324:
319:
315:
311:
307:
302:
297:
295:
291:
287:
283:
278:
275:
267:
265:
263:
257:
254:
250:
245:
241:
237:
236:Caloris Basin
231:
230:Caloris Group
224:Caloris group
223:
221:
218:
213:
210:
209:Tolstoj Basin
202:
200:
196:
193:
184:
179:
177:
175:
171:
167:
163:
159:
155:
151:
150:photography.
148:
147:
142:
141:
136:
133:
129:
124:
122:
121:Tolstoj Basin
118:
114:
110:
105:
103:
99:
95:
90:
86:
85:
80:
75:
73:
69:
65:
57:
53:
49:
44:
37:
33:
26:
21:
3855:
3832:
3828:Tolstoy Farm
3808:
3800:
3792:(1990 novel)
3788:
3779:
3771:
3764:
3681:
3662:
3654:
3641:What Is Art?
3639:
3631:
3623:
3615:
3607:
3599:
3591:
3572:
3564:
3556:
3548:
3540:
3532:
3313:Three Deaths
3243:
3235:
3227:
3219:
3211:
3203:
3195:
3187:
3179:
3171:
3163:
3144:
3138:Resurrection
3136:
3128:
3120:
3114:The Cossacks
3112:
3104:
3096:
3088:
3073:Bibliography
2986:Michelangelo
2923:
2772:
2760:
2680:
2672:
2493:SveinsdĂłttir
2398:Rachmaninoff
2223:Michelangelo
2218:Mendes Pinto
2153:Ma Chih-Yuan
1808:Gainsborough
1613:Chao Meng-Fu
1558:Brunelleschi
1388:Amru Al-Qays
1368:Al-Hamadhani
1237:Beagle Rupes
1156:Tir Planitia
1069:
1050:Michelangelo
848:
839:
822:
818:
812:
801:
796:
774:
737:
731:
697:
691:
663:
659:
621:
615:
596:
591:
566:
562:
526:
522:
496:
492:
462:
432:
425:
410:
400:
387:
383:
370:
366:
362:
358:
346:
333:
321:
298:
279:
271:
258:
233:
214:
206:
197:
188:
180:Stratigraphy
152:
144:
138:
137:
125:
106:
102:Tir Planitia
82:
76:
63:
61:
3928:Leo Tolstoy
3813:(2022 film)
3805:(2018 film)
3784:(1984 film)
3781:Lev Tolstoy
3768:(1912 film)
3726:Lev Lvovich
3585:Non-fiction
3173:Two Hussars
3146:Hadji Murat
3062:Leo Tolstoy
2874:Shakespeare
2689:BepiColombo
2685:(2004â2015)
2677:(1973â1975)
2656:Exploration
2523:Villa-Lobos
2503:To Ngoc Van
2468:Shakespeare
2403:Raden Saleh
2288:Mussorgskij
1968:Hovnatanian
1728:Dostoevskij
1608:Chaikovskij
1573:Callicrates
1453:Baranauskas
1423:Aristoxenes
1418:Apollodorus
1170:Canyons and
1060:Shakespeare
997:Quadrangles
987:Quadrangles
301:impact melt
294:lunar maria
72:Leo Tolstoy
38:photomosaic
3912:Categories
3796:2009 film)
3734:(daughter)
3716:(daughter)
3675:Unfinished
3601:Confession
3446:Kholstomer
3432:Repentance
3189:PolikĂșshka
2674:Mariner 10
2483:Stravinsky
2383:Praxiteles
2378:Polygnotus
2258:Monteverdi
2228:Mickiewicz
2183:Mark Twain
1763:Enheduanna
1663:Cunningham
1533:Botticelli
1448:Balanchine
1408:Anguissola
1338:Ahmad Baba
1276:Basins and
1252:Hero Rupes
1218:Ridges and
1102:Plains and
961:Atmosphere
393:References
350:grabenlike
140:Mariner 10
132:perihelion
84:Mariner 10
36:Mariner 10
27:spacecraft
3714:Alexandra
3488:Too Dear!
3425:The Grain
3221:The Devil
3090:Childhood
2998:Discovery
2936:Beethoven
2862:Raditladi
2748:Sub-Earth
2706:Mercury-P
2682:MESSENGER
2634:Asteroids
2603:Astronomy
2538:Xiao Zhao
2513:VelĂĄzquez
2458:Scarlatti
2423:Rembrandt
2408:Raditladi
2393:Qi Baishi
2388:Prokofiev
2138:Lovecraft
2108:Lermontov
2008:Izquierdo
1923:Hiroshige
1913:Hemingway
1898:Hawthorne
1893:Hauptmann
1803:Futabatei
1703:Derzhavin
1693:Delacroix
1643:Coleridge
1598:Cervantes
1523:Boccaccio
1493:Belinskij
1483:Beethoven
1428:AĆvaghoáčŁa
1358:Al-Akhtal
1353:Akutagawa
1328:Abu Nuwas
1086:volcanoes
1065:Raditladi
1030:Discovery
1010:Beethoven
942:Geography
804:MESSENGER
330:Structure
310:Tyagaraja
192:secondary
146:MESSENGER
52:Sophocles
25:MESSENGER
3897:Category
3810:A Couple
3693:" (1905)
3651:" (1908)
3518:" (1911)
3511:" (1905)
3504:" (1903)
3497:" (1903)
3490:" (1897)
3483:" (1894)
3476:" (1893)
3469:" (1892)
3462:" (1889)
3455:" (1886)
3448:" (1886)
3441:" (1886)
3434:" (1886)
3427:" (1886)
3420:" (1886)
3413:" (1886)
3406:" (1886)
3399:" (1885)
3392:" (1885)
3385:" (1885)
3378:" (1885)
3371:" (1885)
3364:" (1885)
3357:" (1884)
3350:" (1881)
3343:" (1872)
3336:" (1872)
3329:" (1872)
3322:" (1863)
3315:" (1859)
3308:" (1858)
3301:" (1857)
3294:" (1856)
3287:" (1855)
3280:" (1855)
3273:" (1855)
3266:" (1852)
3264:The Raid
3157:Novellas
3017:features
3003:features
2991:features
2979:features
2967:features
2953:features
2941:features
2929:features
2917:features
2912:Eminescu
2905:features
2891:features
2886:Victoria
2879:features
2867:features
2855:features
2841:features
2836:Borealis
2767:Category
2716:See also
2699:Proposed
2666:and past
2611:Transits
2488:Sullivan
2463:Schubert
2358:Petrarch
2283:Murasaki
2278:MunkĂĄcsy
2208:Melville
2148:Lysippus
2103:Leopardi
2098:Larrocha
2088:Kurosawa
2083:Kunisada
2028:Kalidasa
1933:Hodgkins
1928:Hitomaro
1888:Harunobu
1823:Ghiberti
1793:Flaubert
1788:Firdousi
1778:Faulkner
1758:Eminescu
1718:Dominici
1678:De Graft
1658:Couperin
1583:Carducci
1543:Bramante
1528:Boethius
1518:Bjornson
1443:Balagtas
1373:Al-JÄhiz
1104:plateaus
1075:Victoria
1035:Eminescu
1015:Borealis
966:Features
779:289â300.
405:355â362.
262:Nectaris
58:craters.
3849:Related
3732:Tatyana
3299:Lucerne
3098:Boyhood
2962:Debussy
2924:Tolstoj
2850:Hokusai
2743:Fiction
2736:Related
2708:(~2031)
2664:Current
2564:Geology
2528:Vivaldi
2508:Tolstoj
2418:Raphael
2368:Picasso
2363:Phidias
2348:Oskison
2333:Neumann
2323:Nureyev
2303:Nampeyo
2298:Nabokov
2248:MoliĂšre
2238:Mistral
2203:Matisse
2198:Matabei
2193:Martial
2168:Mansart
2158:Machaut
2143:Lu Hsun
2113:Lessing
2078:Kulthum
2058:Kipling
2048:Kertész
2013:JanĂĄÄek
1998:Imhotep
1993:Ictinus
1978:Hun Kal
1948:Holberg
1943:Holbein
1938:Hokusai
1878:Han Kan
1813:Gauguin
1798:Flaiano
1773:Equiano
1768:Enwonwu
1748:Eastman
1733:Dowland
1713:Dickens
1708:Desprez
1683:Debussy
1648:Copland
1603:CĂ©zanne
1593:Calvino
1588:Carolan
1553:Bruegel
1513:Bernini
1478:Beckett
1403:Angelou
1398:Aneirin
1363:Alencar
1348:Aksakov
1315:Craters
1172:valleys
1070:Tolstoj
1040:Hokusai
1020:Debussy
980:Regions
949:General
933:Outline
922:Mercury
859:Sources
742:Bibcode
702:Bibcode
626:Bibcode
571:Bibcode
531:Bibcode
323:hollows
240:Imbrium
94:Tolstoj
3860:(1888)
3838:crater
3821:Honors
3710:(wife)
3708:Sophia
3701:Family
3686:(1884)
3667:(1910)
3659:(1909)
3644:(1897)
3636:(1894)
3628:(1886)
3620:(1884)
3612:(1883)
3604:(1882)
3596:(1851)
3577:(1910)
3569:(1900)
3561:(1891)
3553:(1890)
3545:(1886)
3537:(1886)
3306:Albert
3248:(1904)
3240:(1898)
3232:(1895)
3224:(1889)
3216:(1889)
3208:(1888)
3200:(1886)
3192:(1860)
3184:(1859)
3176:(1856)
3168:(1856)
3149:(1912)
3141:(1899)
3133:(1878)
3125:(1869)
3117:(1863)
3109:(1856)
3101:(1854)
3093:(1852)
3082:Novels
2974:Neruda
2948:Kuiper
2900:Derain
2779:Portal
2498:Titian
2453:Sander
2448:Rudaki
2433:Rivera
2428:Renoir
2413:Rameau
2338:Nizami
2318:Neruda
2313:Nawahi
2268:Mozart
2243:Mofolo
2233:Milton
2173:Mansur
2163:Mahler
2073:Kuiper
2053:Khansa
1983:Hurley
1963:Horace
1918:Hesiod
1883:Handel
1848:Goethe
1838:Glinka
1833:Giotto
1828:Gibran
1818:Geddes
1753:Eitoku
1743:Dvorak
1698:Derain
1653:Copley
1638:Chu Ta
1633:Chopin
1618:Chekov
1578:CamÔes
1548:Brontë
1538:Brahms
1508:Berkel
1503:Benoit
1463:BartĂłk
1458:Balzac
1383:Amaral
1323:Abedin
1278:fossae
1055:Neruda
1045:Kuiper
1025:Derain
733:Icarus
469:
439:
336:Mozart
314:Balzac
217:ejecta
98:Mozart
89:ejecta
54:, and
3728:(son)
3722:(son)
3526:Plays
3106:Youth
3010:H-15
2996:H-11
2984:H-12
2972:H-13
2960:H-14
2898:H-10
2619:Earth
2587:Moons
2557:Other
2543:Yeats
2533:Vyasa
2518:Verdi
2478:Sinan
2443:Rodin
2438:Rizal
2328:Nervo
2308:Navoi
2293:Myron
2273:Munch
2263:Moody
2253:Monet
2188:MartĂ
2178:March
2133:Liszt
2123:Li Po
2093:Lange
2063:KĆshĆ
2043:Kenko
2038:Keats
2033:Karsh
2018:Jokai
1988:Ibsen
1958:Homer
1953:Holst
1908:Heine
1903:Haydn
1863:Grieg
1853:Gogol
1843:Gluck
1738:Durer
1723:Donne
1688:Degas
1673:Dario
1568:Byron
1563:Burns
1498:Bello
1473:BashĆ
1468:Barma
1433:Atget
1413:Anyte
1393:Andal
1378:Alver
1343:Ailey
1220:rupes
870:(PDF)
306:Zeami
48:Zeami
3720:Ilya
3012:Bach
2946:H-6
2934:H-7
2922:H-8
2910:H-9
2884:H-2
2872:H-3
2860:H-4
2848:H-5
2834:H-1
2624:Mars
2548:Zola
2353:Ovid
2343:Okyo
2213:Mena
2003:Ives
1973:Hugo
1873:Hals
1858:Goya
1668:Dali
1438:Bach
1005:Bach
467:ISBN
437:ISBN
318:rays
284:and
242:and
234:The
172:and
164:and
111:and
62:The
56:Goya
2373:Poe
1783:Fet
1488:Bek
827:doi
750:doi
710:doi
668:doi
634:doi
579:doi
539:doi
501:doi
282:Tir
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