Isidis Planitia

Coordinates: 12°54′N 87°00′E / 12.9°N 87.0°E / 12.9; 87.0
From English Wikipedia @ Freddythechick
Isidis Planitia
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Topography of Isidis Planitia
LocationNorth of Hellas Planitia, east of Syrtis Major Planum, Mars
Coordinates12°54′N 87°00′E / 12.9°N 87.0°E / 12.9; 87.0
Diameter1,900 km (1,200 mi)[1]
EponymIsis is the Egyptian goddess of heaven and fertility.

Isidis Planitia is a plain located within a giant impact basin on Mars, located partly in the Syrtis Major quadrangle and partly in the Amenthes quadrangle. At approximately 1,900 km (1,200 mi) in diameter,[1] it is the third-largest confirmed impact structure on the planet, after the Hellas and Utopia basins. Isidis was likely the last major basin to be formed on Mars, having formed approximately 3.9 billion years ago during the Noachian period,[2] by an impactor around 200 kilometres (120 mi) in diameter.[3] Due to dust coverage, it typically appears bright in telescopic views, and was mapped as a classical albedo feature, Isidis Regio, visible by telescope in the pre-spacecraft era.

A study reported in Icarus described the complex geologic history of parts of Isidis, especially areas near the Deuteronilus contact. This contact is the supposed edge of a vast Martian ocean. The researchers found evidence of a Late Hesperian/Early Amazonian Sea in the area. The sea would have quickly frozen over. Eskers formed under the ice.[4]

Just to the west of Isidis is Syrtis Major Planum, a low-relief shield volcano that is a prominent dark albedo feature of Mars, which formed after the basin.[5] The westernmost extent is bounded by a subregion, Northeast Syrtis with diverse geology. Around the Isidis basin magnesium carbonate was found by the Mars Reconnaissance Orbiter. This mineral indicates that water was present and that it was not acidic, pH conditions more favorable for the evolution of life.[6]

The name Isidis Planitia follows the earlier name Isidis Regio ('region of Isis'). Isis is the Egyptian goddess of heaven and fertility.

Gallery

Beagle 2

The Beagle 2 lander was about to land in the eastern part of Isidis Planitia in December 2003, when contact with the craft was lost. In January 2015, NASA reported the Beagle 2 had been found on the surface in Isidis Planitia (location is about 11°31′35″N 90°25′46″E / 11.5265°N 90.4295°E / 11.5265; 90.4295).[7][8] High-resolution images captured by the Mars Reconnaissance Orbiter identified the lost probe, which appears to be intact.[9][10][11] (see discovery images here)

Overview
Context
Close-up
Discovery images of Beagle 2, taken by the Mars Reconnaissance Orbiter in November and December 2014.[9]

Mars 2020 mission

In 2018 the Jezero (crater) in the north west rim of the Isidis basin was selected as a landing site for the Mars 2020 mission, including the Perseverance rover.

Interactive Mars map

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Image:Mars Map.JPG|thumb|center|620px|alt=Map of Mars|The image above contains clickable linksInteractive image map of the global topography of Mars. Hover your mouse over the image to see the names of over 60 prominent geographic features, and click to link to them. Coloring of the base map indicates relative elevations, based on data from the Mars Orbiter Laser Altimeter on NASA's Mars Global Surveyor. Whites and browns indicate the highest elevations (+12 to +8 km); followed by pinks and reds (+8 to +3 km); yellow is 0 km; greens and blues are lower elevations (down to −8 km). Axes are latitude and longitude; Polar regions are noted.

poly 377 357 423 380 407 405 369 389 Acheron Fossae poly 1316 75 1305 231 992 408 677 224 651 71 1069 169 Acidalia Planitia poly 564 320 555 402 464 416 449 348 489 317 Alba Mons poly 160 408 355 401 311 594 156 594 Amazonis Planitia poly 832 741 903 744 897 793 749 880 776 950 831 1052 829 1121 510 1126 653 854 Aonia Planitia poly 1186 320 1477 394 1040 732 960 635 952 525 Arabia Terra poly 155 70 578 72 580 258 156 429 377 238 284 224 308 283 158 408 Arcadia Planitia poly 875 1108 872 1128 956 1131 957 1041 906 1047 904 1084 Argentea Planum poly 871 871 935 887 926 942 884 967 837 918 Argyre Planitia poly 880 356 962 441 889 505 824 412 Chryse Planitia poly 515 777 575 751 671 792 684 835 580 854 Claritas Fossae poly 981 456 992 493 1076 412 1044 386 Cydonia Mensae poly 346 685 514 740 526 838 363 797 Daedalia Planum poly 1858 405 1968 412 1954 514 1860 505 Elysium Mons poly 1692 500 1945 509 2009 342 2092 588 2085 671 2007 689 Elysium Planitia poly 1848 617 1870 616 1882 638 1878 637 1848 639 Gale crater poly 1645 865 1675 858 1645 782 1600 789 Hadriaca Patera poly 1378 766 1418 783 1392 882 1356 874 Hellas Montes poly 1410 772 1515 769 1618 869 1493 943 1387 894 Hellas Planitia poly 1599 731 1610 599 1711 593 1750 717 Hesperia Planum poly 928 703 919 746 960 761 959 726 Holden crater poly 524 827 588 867 564 900 511 881 Icaria Planum poly 1587 447 1672 520 1619 575 1555 568 1538 500 Isidis Planitia poly 1531 475 1518 514 1547 516 1552 484 Jezero crater poly 1032 72 1030 87 1112 94 1124 166 1032 170 Lomonosov crater poly 153 569 280 579 293 650 156 651 Lucus Planum poly 356 411 400 451 357 486 329 465 Lycus Sulci poly 1243 254 1311 258 1309 310 1244 304 Lyot crater poly 738 489 823 493 792 597 704 573 Lunae Planum poly 1367 964 1552 989 1531 1099 1361 1078 Malea Planum poly 832 1047 920 1048 916 1124 839 1125 Maraldi crater poly 572 326 612 356 676 303 658 276 Mareotis Fossae poly 664 301 752 369 700 454 628 400 Mareotis Tempe poly 872 491 976 477 1054 609 953 635 Margaritifer Terra poly 1853 283 1857 333 1903 330 1899 281 Mie crater poly 309 233 346 235 344 265 303 267 Milankovič crater poly 1694 508 1665 562 1767 637 1798 575 Nepenthes Mensae poly 801 855 931 819 941 861 871 857 848 883 Nereidum Montes poly 1529 438 1446 412 1462 371 1525 404 Nilosyrtis Mensae poly 1197 672 994 834 978 1072 1276 1086 1365 785 Noachis Terra poly 471 410 547 418 532 488 479 470 Olympica Fossae poly 390 417 481 505 373 547 353 483 Olympus Mons poly 137 1061 139 1144 2102 1143 2103 1063 Planum Australe poly 1804 1124 1844 649 1663 650 1592 1129 Promethei Terra poly 1276 219 1262 253 1373 329 1383 302 Protonilus Mensae poly 151 729 314 737 323 852 156 885 Sirenum poly 1370 899 1432 952 1373 972 1339 933 Sisyphi Planum poly 585 631 784 692 697 823 574 807 Solis Planum poly 570 638 608 673 574 707 531 670 Syria Planum poly 602 232 645 243 595 314 561 306 Tantalus Fossae poly 727 306 790 260 840 392 731 497 693 567 Tempe Terra poly 1850 652 2080 675 2086 1128 1799 1125 Terra Cimmeria poly 1403 483 1547 596 1476 690 1350 749 1242 696 1214 642 Terra Sabaea poly 158 816 589 900 655 1124 171 1123 Terra Sirenum poly 547 484 611 530 488 714 413 656 Tharsis Montes poly 576 385 604 401 585 445 564 428 Tractus Catena poly 1583 607 1782 679 1762 800 1604 771 1531 738 Tyrrhena Terra poly 452 529 505 568 475 583 445 570 Ulysses Patera poly 608 432 641 439 633 467 605 456 Uranius Patera poly 1413 79 1421 296 1627 447 1820 471 1853 364 1832 277 1894 254 1918 311 1829 476 2079 214 2078 80 Utopia Planitia poly 589 582 907 651 865 716 572 655 Valles Marineris poly 139 51 142 132 2103 133 2104 53 Vastitas Borealis poly 824 475 915 593 889 632 789 604 Xanthe Terra

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See also

References

  1. ^ 1.0 1.1 Tornabene, Livio L.; Moersch, Jeffery E.; McSween, Harry Y.; et al. (October 2008). "Surface and crater-exposed lithologic units of the Isidis Basin as mapped by coanalysis of THEMIS and TES derived data products". Journal of Geophysical Research. 113 (E10). Bibcode:2008JGRE..11310001T. doi:10.1029/2007JE002988.
  2. ^ Ritzer, J.; Hauck, S. (June 2009), "Lithospheric structure and tectonics at Isidis Planitia, Mars", Icarus, 201 (2): 528–539, Bibcode:2009Icar..201..528R, doi:10.1016/j.icarus.2009.01.025
  3. ^ Branco, Hely C.; Miljkovic, Katarina; Plesa, Ana‐Catalina (April 2024). "New Numerically Derived Scaling Relationships for Impact Basins on Mars". Journal of Geophysical Research: Planets. 129 (4). doi:10.1029/2023JE008217. ISSN 2169-9097.
  4. ^ Erkeling, G.; Reiss, D.; Hiesinger, H.; Ivanov, M.A.; Hauber, E.; Bernhardt, H. (November 2014). "Landscape formation at the Deuteronilus contact in southern Isidis Planitia, Mars: Implications for an Isidis Sea?" (PDF). Icarus. 242: 329–351. Bibcode:2014Icar..242..329E. doi:10.1016/j.icarus.2014.08.015.
  5. ^ Hiesinger, H.; Head, J. W. (2004-01-08), "The Syrtis Major volcanic province, Mars: Synthesis from Mars Global Surveyor data", Journal of Geophysical Research: Planets, 109 (E1): E01004, Bibcode:2004JGRE..109.1004H, doi:10.1029/2003JE002143, E01004
  6. ^ Murchie, S. L.; Mustard, J. F.; Ehlmann, B. L.; Milliken, R. E.; Bishop, J. L.; McKeown, N. K.; Noe Dobrea, E. Z.; Seelos, F. P.; Buczkowski, D. L.; Wiseman, S. M.; Arvidson, R. E.; Wray, J. J.; Swayze, G.; Clark, R. N.; Des Marais, D. J.; McEwen, A. S.; Bibring, J.-P. (February 2009). "A synthesis of Martian aqueous mineralogy after 1 Mars year of observations from the Mars Reconnaissance Orbiter" (PDF). Journal of Geophysical Research: Planets. 114 (E2): E00D06. Bibcode:2009JGRE..114.0D06M. doi:10.1029/2009JE003342. ISSN 0148-0227.
  7. ^ Ellison, Doug (16 January 2015). "re Beagle 2 location on Mars => "Using HiView on image ESP_039308_1915_COLOR.JP2 I get 90.4295E 11.5265N"". Twitter & JPL. Retrieved 19 January 2015.
  8. ^ Grecicius, Tony; Dunbar, Brian (16 January 2015). "Components of Beagle 2 Flight System on Mars". NASA. Retrieved 18 January 2015.
  9. ^ 9.0 9.1 Webster, Guy (16 January 2015). "'Lost' 2003 Mars Lander Found by Mars Reconnaissance Orbiter". NASA. Archived from the original on 24 February 2017. Retrieved 16 January 2015.
  10. ^ "Mars Orbiter Spots Beagle 2, European Lander Missing Since 2003". New York Times. Associated Press. 16 January 2015. Retrieved 17 January 2015.
  11. ^ Amos, Jonathan (16 January 2015). "Lost Beagle2 probe found 'intact' on Mars". BBC. Retrieved 16 January 2015.

External links

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