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Marsquake

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California, the event was estimated to have a Richter magnitude of 2.7 at a distance of roughly 110 kilometers. However, the wind speed was only measured 20 minutes previously, and 45 minutes after, at 2.6 and 3.6 meters per second, respectively. While a sudden wind gust of 16 m/s would have been required to produce the event, it could not be completely ruled out. The Sol 80 event was later identified as a marsquake. The earlier Sol 53 event initially received much interest as a possible marsquake, but was correlated with wind and not considered further. Following the re-evaluation of the Sol 80 event as a marsquake, a re-evaluation of the Sol 53 event showed that it was unique among all Viking daytime recorded waveforms and the only one with a waveform with a rapid rise time and duration similar to Sol 80. Consequently Sol 53 was identified as a marsquake. Comparing Viking with InSight events, using technologies 43 years apart is challenging, but comparison of the two Viking events with some InSight events showed that the similarity of waveforms was reasonable.
2344: 196: 217: 276: 161: 130: 267: 2350: 227: 20: 2356: 2215: 2227: 1222: 285: 184:(SEIS) on 19 December 2018 to search for marsquakes and analyze Mars's internal structure. Even if no seismic events are detected, the seismometer is expected to be sensitive enough to detect possibly several dozen meteors causing airbursts in Mars's atmosphere per year, as well as meteorite impacts. It will also investigate how the Martian 229: 233: 232: 228: 86:. Marsquakes were first detected but not confirmed by the Viking mission in 1976. Marsquakes were detected and confirmed by the InSight mission in 2019. Using InSight data and analysis, the Viking marsquakes were confirmed in 2023. Compelling evidence has been found that Mars has in the past been seismically more active, with clear 234: 288: 293: 291: 287: 286: 292: 231: 212:
A faint seismic signal, believed to be a small marsquake, was measured and recorded by the InSight lander on 6 April 2019. The lander's seismometer detected ground vibrations while three distinct kinds of sounds were recorded, according to NASA. Three other events were recorded on 14 March, 10 April,
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on the InSight lander. In October 2023 the results of a collaborative international project to scan the surface of Mars for a new impact crater created at the time of the 4 May 2022 seismic event, known as S1222a, was published. It was estimated that a crater of at least 300m in diameter would be
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Viking 2 recorded two possible marsquakes on Sol 53 (daytime during windy period) and Sol 80 (nighttime during low wind period). Due to the inability to separate ground motion from wind-driven lander vibrations and the lack of other collaborating possible marsquakes, the Sol 53 and Sol 80 events
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Fernando, Benjamin; Wójcicka, Natalia; Marouchka, Froment; Maguire, Ross; Stähler, Simon; Rolland, Lucie]; Collins, Gareth; Karatekin, Ozgur; Larmat, Carene; Sansom, Eleanor; Teanby, Nicholas; Spiga, Aymeric; Karakostas, Foivos; Leng, Kuangdai; Nissen-Meyer, Tarje; Kawamura, Taichi; Giardini,
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lander's mission (roughly November 23, 1976), the on-board seismometer detected an unusual acceleration event during a period of relatively low wind speed. Based on the features of the signal and assuming Mars's crust behaves similar to Earth's crust near the lander's testing site in Southern
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detected during the Apollo program. It could have been caused by activity internal to the planet or by a meteorite striking the surface. The epicenter was believed to be within 100 km of the lander. As of 30 September 2019, SEIS had reported 450 events of various types.
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could not be confirmed during the Viking mission. It was possible to rule out frequent and large marsquakes at that time. The low detection rate and evaluation when the windspeed was low at the Viking 2 site, allowed limits to be placed on seismic activity on Mars.
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with two landers, Viking 1 & 2 in 1976, with seismometers mounted on top of the lander. The seismometer on the Viking 1 lander failed. The Viking 2 seismometer collected data for 2100 hours (89 days) of data over 560 sols of lander recorded.
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NASA's Mars Perseverance Rover will act as a seismic source of known temporal and spatial localization as it lands on the surface. The InSight lander will evaluate whether the signals produced by this event will be detectable by 3,452 km away.
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created to produce the seismic waves, which reverberated round the planet for six hours. The survey of satellite images from five different orbiters concluded that the event was not the result of an impact event.
289: 737: 330:(SEIS) detected one magnitude 1–2 seismic event on April 6, 2019. Three other unconfirmed candidate seismic events were detected on March 14, April 10 and April 11, 2019. The quake is similar to 240: 423:
Anderson, Don L.; Miller, W. F.; Latham, G. V.; Nakamura, Y.; Toksoz, M. N.; Dainty, M. N.; Duennebier, F. K.; Lazarewicz, A. R.; Kovach, R. L.; Knight, T. C. D. (September 30, 1977).
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detections. In 2023, a re-evaluation of Viking 2 using InSight data and analysis, and Viking wind data, confirmed that the two Viking events on Sol 53 and 80 were marsquakes.
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In 2013, data from the InSight mission (see below) led to an increased interest in the Viking data set, and further analysis may reveal one of the largest collection of
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and 11 April, but these signals were even smaller and more ambiguous in origin, making it difficult to determine their cause.
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fault. The first confirmed seismic event emanating from Valles Marineris, a quake with a magnitude of 4.2, was detected by
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over a large region of southern Mars. Magnetic striping on Earth is often a sign of a region of particularly thin
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as a result of the sudden release of energy. Such quakes may occur in the planet's interior, such as the result of
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Stevanović, J.; Teanby, N. A.; Wookey, J.; Selby, N.; Daubar, I. J.; Vaubaillon, J.; Garcia, R. (9 January 2017).
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respond to the effects of meteorite impacts, which gives clues to the planet's inner structure.
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Banerdt, W. Bruce; Smrekar, Suzanne E.; Banfield, Don; Giardini, Domenico; Golombek, Matthew;
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Mars lander, launched in May 2018, landed on Mars on 26 November 2018 and deployed a
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On 4 May 2022, a large marsquake, estimated at magnitude 5, was detected by the
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Domenico; Lognonné, Philippe; Banerdt, Bruce; Daubar, Ingrid (April 2021).
118: 60: 706: 424: 67:. The detection and analysis of marsquakes are informative to probing the 2283: 1922: 1917: 1380: 1159: 1142: 1032: 1007: 690: 665: 503: 249: 177: 110: 738:"Bolide Airbursts as a Seismic Source for the 2018 Mars InSight Mission" 2453: 2030: 2015: 1350: 1280: 487: 331: 44: 2182: 2118: 1752: 1006:
Lorenz, Ralph D.; Nakamura, Yosio; Murphy, James R. (November 2017).
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Lorenz, Ralph D.; Nakamura, Yosio; Murphy, James R. (November 2017).
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The first attempts to detect seismic activity on Mars were with the
2192: 1904: 1885: 1757: 603:"Viking Seismometer Record: Data Restoration and Dust Devil Search" 551: 526: 314: 922:"Marsquake! NASA's InSight Lander Feels Its 1st Red Planet Tremor" 2405: 2274: 1395: 807:"Listening to meteorites hitting Mars will tell us what's inside" 323: 201: 172: 114: 1139: 567:"Two Largest Marsquakes To Date Recorded From Planet's Far Side" 28: 24: 1080: 784:"NASA and French Space Agency Sign Agreement for Mars Mission" 55:, from which most quakes on Earth originate, or possibly from 892:
Brown, Dwayne; Johnson, Alana; Good, Andrew (23 April 2019).
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Despite the drawbacks of significant wind interference, on
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splitting and spreading, forming new land in the slowly
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Good, Andrew; Fox, Karen; Johnson, Alana (9 May 2022).
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The 4,000 km (2,500 mi) long canyon system,
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Design and development of a silicon micro-seismometer
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Mars – Seismic wave simulation (artist concept; 2019)
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Quakes have been observed and well-documented on the
1005: 663: 587: 456:"NASA's InSight Detects Two Sizable Quakes on Mars" 303: 1087:"Initial results from the InSight mission on Mars" 610:44th Lunar and Planetary Science Conference (2013) 2471: 891: 840:(Ph.D.). Imperial College London. Archived from 729: 630: 704: 639:"'Marsquakes' Could Shake Up Planetary Science" 488:"Viking Marsquakes 1976 -- Seismic Archaeology" 950:"NASA's InSight Records Monster Quake on Mars" 947: 600: 518: 2258: 1248: 941: 885: 165:Mars – InSight Lander – Seismometer (Sol 110) 977:"Source of largest ever Mars quake revealed" 913: 705:Goins, N. R.; Lazarewicz, A. R. (May 1979). 381: 208:seismometer underneath the white windshield 2304:Rotation and Interior Structure Experiment 2265: 2251: 1255: 1241: 868:"First "Marsquake" Detected on Red Planet" 601:Lorenz, Ralph D.; Nakamura, Yosio (2013). 485: 2312:(flyby relay ('bent pipe' communication)) 2298:Seismic Experiment for Interior Structure 2292:Heat Flow and Physical Properties Package 1168: 1158: 1031: 689: 657: 550: 354:Seismic Experiment for Interior Structure 328:Seismic Experiment for Interior Structure 182:Seismic Experiment for Interior Structure 636: 575:(Press release). SpaceRef. 26 April 2022 492:Journal of Geophysical Research: Planets 453: 339:Experimental (artificial) seismic events 225: 215: 194: 159: 128: 18: 1057:"Nasa lander 'detects first Marsquake'" 919: 786:(Press release). NASA. 10 February 2014 725:– via American Geophysical Union. 514:– via American Geophysical Union. 443:– via American Geophysical Union. 239:Mars – InSight Lander – Seismic Event ( 117:on 25 August 2021, proving it to be an 2472: 486:Lazarewicz, Andrew R. (10 July 2023). 387: 2400:Vandenberg AFB Space Launch Complex 3 2246: 1236: 865: 830: 804: 388:Kornei, Katherine (22 January 2022). 23:Illustration of the shadow zone of a 1054: 481: 479: 477: 475: 418: 416: 414: 412: 98:; a prime example of this being the 75:continue to be volcanically active. 524: 13: 866:Witze, Alexandra (24 April 2019). 136:Mars InSight Lander (May 17, 2022) 14: 2506: 2319:Temperature and Winds for InSight 1189: 920:Bartels, Meghan (23 April 2019). 831:Kumar, Sunil (1 September 2006). 645:. NASA. Jet Propulsion Laboratory 472: 409: 2354: 2348: 2342: 2225: 2214: 2213: 1220: 1055:Amos, Jonathan (23 April 2019). 637:Greicius, Tony (28 March 2018). 572:Seismological Society of America 304:Candidate natural seismic events 283: 274: 265: 259:Mars quake detected (4 May 2022) 124: 82:, and there is evidence of past 2315:Auxiliary Payload Sensor Suite 1133: 1074: 1048: 969: 859: 824: 798: 776: 698: 429:Journal of Geophysical Research 16:Seismic event occurring on Mars 805:Boyle, Rebecca (4 June 2015). 559: 447: 31:don't penetrate the outer core 1: 454:Greicius, Tony (2021-04-01). 374: 238: 220: 199:Cutaway illustration showing 164: 133: 2335:Instrument Deployment System 1670:Recurring slope lineae (RSL) 711:Geophysical Research Letters 7: 2324:Pressure Sensor & Inlet 2272: 2104:Inspiration Mars Foundation 347: 10: 2511: 2139:Artificial objects on Mars 69:interior structure of Mars 2421: 2392: 2363: 2340: 2282: 2208: 2156:List of films set on Mars 2131: 2082: 2064: 2008: 1999: 1979: 1971:C/2013 A1 (Siding Spring) 1963: 1884: 1836: 1789: 1780: 1768:Classical albedo features 1738: 1526: 1419: 1321: 1288: 1279: 1270: 1197:Video (2:48) – MarsQuakes 1111:10.1038/s41561-020-0544-y 762:10.1007/s11214-016-0327-3 2434:Deep Space Network (DSN) 2074:List of missions to Mars 1262: 243:; Sol 128; 6 April 2019) 2232:Solar System portal 1147:Earth and Space Science 1024:2017E&SS....4..681L 1012:Earth and Space Science 723:10.1029/GL006i005p00368 682:2017E&SS....4..681L 670:Earth and Space Science 525:Yin, A. (4 June 2012). 441:10.1029/JS082i028p04524 134:Inside Mars InfoGraphic 1846:Solar eclipses on Mars 1705:"Swiss cheese" feature 1561:Concentric crater fill 245: 223: 209: 167: 138: 32: 2459:Mars InSight Roadshow 1083:Johnson, Catherine L. 742:Space Science Reviews 498:(e2022JE007660): 20. 356:(SEIS, instrument on 237: 219: 198: 163: 132: 22: 2046:Permanent settlement 1160:10.1029/2020EA001585 1033:10.1002/2017ea000306 707:"Martian Seismicity" 691:10.1002/2017EA000306 504:10.1029/2022JE007660 425:"Seismology on Mars" 43:which, much like an 2449:Exploration of Mars 2188:Timekeeping on Mars 1865:Planetary transits 1850:Satellite transits 1763:Observation history 1611:Lobate debris apron 1103:2020NatGe..13..183B 872:Scientific American 754:2017SSRv..211..525S 618:2013LPI....44.1178L 543:2012Lsphe...4..286Y 369:Volcanology of Mars 326:lander mission the 2377:Elysium quadrangle 1170:20.500.11937/90005 987:on 18 October 2023 395:The New York Times 322:On Sol 128 of the 246: 224: 210: 168: 139: 100:Mid-Atlantic Ridge 33: 2490:Planetary science 2467: 2466: 2429:Discovery Program 2240: 2239: 2193:Sol (day on Mars) 2161:Martian scientist 2144:Memorials on Mars 2127: 2126: 2098:The Case for Mars 1995: 1994: 1776: 1775: 1710:Terrain softening 1675:Ring mold craters 1643:North Polar Basin 1566:Dark slope streak 1411:Vastitas Borealis 1308:Dust devil tracks 1091:Nature Geoscience 364:Tectonics of Mars 294: 235: 88:magnetic striping 2502: 2408:(Launch Vehicle) 2382:Elysium Planitia 2358: 2352: 2346: 2267: 2260: 2253: 2244: 2243: 2230: 2229: 2228: 2217: 2216: 2091:The Mars Project 2006: 2005: 1954: 1944: 1934: 1912: 1910: 1909: 1787: 1786: 1648:Ocean hypothesis 1498:Outflow channels 1286: 1285: 1257: 1250: 1243: 1234: 1233: 1225: 1224: 1223: 1216: 1198: 1183: 1182: 1172: 1162: 1137: 1131: 1130: 1078: 1072: 1071: 1069: 1067: 1052: 1046: 1045: 1035: 1003: 997: 996: 994: 992: 983:. 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1653:Ore resources 1651: 1649: 1646: 1644: 1641: 1639: 1636: 1632: 1629: 1627: 1624: 1623: 1622: 1619: 1617: 1614: 1612: 1609: 1607: 1604: 1602: 1599: 1597: 1594: 1592: 1589: 1587: 1584: 1582: 1579: 1577: 1574: 1572: 1569: 1567: 1564: 1562: 1559: 1557: 1554: 1552: 1549: 1547: 1546:Chaos terrain 1544: 1542: 1539: 1537: 1536:Brain terrain 1534: 1533: 1531: 1529: 1525: 1519: 1516: 1514: 1511: 1509: 1506: 1504: 1501: 1499: 1496: 1494: 1491: 1487: 1484: 1483: 1482: 1479: 1477: 1474: 1472: 1469: 1467: 1464: 1462: 1459: 1457: 1454: 1452: 1451:Chaos terrain 1449: 1447: 1444: 1442: 1439: 1436: 1432: 1429: 1428: 1426: 1424: 1418: 1412: 1409: 1407: 1404: 1402: 1399: 1397: 1394: 1392: 1389: 1387: 1384: 1382: 1379: 1377: 1374: 1372: 1369: 1367: 1366:Planum Boreum 1364: 1362: 1359: 1357: 1356:Olympia Undae 1354: 1352: 1349: 1347: 1346:Eridania Lake 1344: 1342: 1339: 1337: 1334: 1332: 1329: 1328: 1326: 1324: 1320: 1314: 1311: 1309: 1306: 1304: 1301: 1299: 1296: 1295: 1293: 1291: 1287: 1284: 1282: 1278: 1274: 1269: 1265: 1258: 1253: 1251: 1246: 1244: 1239: 1238: 1235: 1228: 1218: 1217: 1214: 1206: 1203: 1199: 1194: 1193: 1180: 1176: 1171: 1166: 1161: 1156: 1152: 1148: 1144: 1136: 1128: 1124: 1120: 1116: 1112: 1108: 1104: 1100: 1096: 1092: 1088: 1084: 1077: 1062: 1058: 1051: 1043: 1039: 1034: 1029: 1025: 1021: 1017: 1013: 1009: 1002: 986: 982: 978: 972: 957: 956: 951: 944: 929: 928: 923: 916: 901: 900: 895: 888: 873: 869: 862: 843: 836: 835: 827: 812: 811:New Scientist 808: 801: 785: 779: 771: 767: 763: 759: 755: 751: 747: 743: 739: 732: 724: 720: 716: 712: 708: 701: 692: 687: 683: 679: 675: 671: 667: 660: 644: 640: 633: 619: 615: 611: 604: 597: 595: 593: 591: 574: 573: 568: 562: 553: 548: 544: 540: 536: 532: 528: 521: 513: 509: 505: 501: 497: 493: 489: 482: 480: 478: 476: 461: 457: 450: 442: 438: 434: 430: 426: 419: 417: 415: 413: 397: 396: 391: 384: 380: 370: 367: 365: 362: 359: 355: 352: 351: 345: 336: 333: 329: 325: 320: 317: 316: 311: 277: 268: 254: 251: 242: 218: 214: 204: 203: 197: 193: 191: 187: 183: 179: 175: 174: 162: 158: 156: 151: 147: 144: 131: 125:Detectability 122: 120: 116: 112: 108: 103: 101: 97: 93: 89: 85: 81: 76: 74: 70: 66: 62: 58: 54: 50: 46: 42: 38: 30: 26: 21: 2443: 2439:Mars landing 2364:Landing site 2327:Magnetometer 2273: 2178:Life on Mars 2173:Flag of Mars 2114:Mars Society 2096: 2089: 2056:Terraforming 2051:Colonization 1821:Swift crater 1663:polar wander 1615: 1391:Terra Sabaea 1331:Arabia Terra 1227:Solar System 1150: 1146: 1135: 1094: 1090: 1076: 1064:. Retrieved 1060: 1050: 1015: 1011: 1001: 989:. Retrieved 985:the original 981:ScienceDaily 980: 971: 959:. Retrieved 953: 943: 931:. Retrieved 925: 915: 903:. Retrieved 897: 887: 875:. Retrieved 871: 861: 849:. Retrieved 842:the original 833: 826: 814:. Retrieved 810: 800: 788:. Retrieved 778: 745: 741: 731: 714: 710: 700: 673: 669: 659: 647:. Retrieved 642: 632: 621:. Retrieved 609: 577:. Retrieved 570: 561: 534: 530: 520: 495: 491: 463:. Retrieved 459: 449: 432: 428: 399:. Retrieved 393: 383: 360:Mars lander) 357: 342: 321: 313: 307: 247: 211: 200: 171: 169: 152: 148: 140: 119:active fault 104: 77: 61:Olympus Mons 36: 34: 2414:(2nd stage) 2402:(Launchpad) 2001:Exploration 1923:5261 Eureka 1591:Groundwater 1556:Composition 1381:Tempe Terra 1371:Quadrangles 1298:Circulation 790:11 February 649:21 November 531:Lithosphere 250:seismometer 178:seismometer 111:strike-slip 27:for Earth. 2495:Seismology 2474:Categories 2454:Mars flyby 1658:Polar caps 1638:Mud cracks 1621:Meteorites 1606:Lava tubes 1541:Carbonates 1476:Labyrinthi 1351:Iani Chaos 1290:Atmosphere 991:23 October 623:2019-04-24 465:2021-07-24 435:(28): 22. 401:22 January 375:References 332:moonquakes 312:80 of the 45:earthquake 2480:Tectonics 2444:Marsquake 2183:Sub-Earth 2166:Mythology 2119:Mars race 1886:Asteroids 1782:Astronomy 1753:Hesperian 1748:Amazonian 1720:Volcanism 1695:Spherules 1616:Marsquake 1571:Dichotomy 1486:by height 1481:Mountains 1281:Geography 1179:2333-5084 1127:211266334 1119:1752-0894 1042:2333-5084 927:Space.com 770:125102926 512:259927674 37:marsquake 2219:Category 2083:Advocacy 2066:Missions 2009:Concepts 1838:Transits 1809:Monolith 1758:Noachian 1730:Yardangs 1626:on Earth 1586:Glaciers 1431:"Canals" 1423:features 1421:Physical 1066:6 August 933:23 April 905:23 April 877:25 April 717:(7): 3. 579:26 April 348:See also 315:Viking 2 59:such as 57:hotspots 2422:Related 2412:Centaur 2406:Atlas V 2370:Planet 2321:(TWINS) 2284:Payload 2275:InSight 2151:Fiction 2132:Related 2026:Landing 2021:Orbiter 1980:General 1949:2007 NS 1939:1999 UJ 1929:1998 VF 1918:Trojans 1905:2007 WD 1894:Impacts 1874:Mercury 1740:History 1700:Surface 1631:on Mars 1596:Gullies 1581:Geysers 1528:Geology 1518:Gravity 1513:Valleys 1466:Gullies 1456:Craters 1446:Catenae 1441:Canyons 1396:Tharsis 1341:Cydonia 1323:Regions 1313:Methane 1303:Climate 1202:YouTube 1099:Bibcode 1020:Bibcode 851:15 July 750:Bibcode 678:Bibcode 614:Bibcode 539:Bibcode 358:InSight 324:InSight 202:InSight 180:called 173:InSight 115:InSight 63:or the 29:S-waves 2306:(RISE) 2300:(SEIS) 2223:  2212:  1964:Comets 1859:Deimos 1854:Phobos 1816:Deimos 1799:Phobos 1503:Plains 1471:Mensae 1461:Fossae 1213:Portal 1177:  1125:  1117:  1040:  961:10 May 816:5 June 768:  510:  206:'s 190:mantle 25:P-wave 2031:Rover 2016:Flyby 1987:Orbit 1869:Earth 1791:Moons 1725:Water 1601:Lakes 1551:Color 1401:Undae 1153:(4). 1123:S2CID 845:(PDF) 838:(PDF) 766:S2CID 606:(PDF) 508:S2CID 186:crust 92:crust 41:quake 39:is a 2372:Mars 2294:(HP) 1690:Soil 1435:list 1264:Mars 1205:NASA 1175:ISSN 1115:ISSN 1068:2019 1038:ISSN 993:2023 963:2022 955:NASA 935:2019 907:2019 899:NASA 879:2019 853:2015 818:2015 792:2014 651:2018 643:NASA 581:2022 460:NASA 403:2022 188:and 170:The 80:Moon 49:Mars 2330:PAE 1200:on 1165:hdl 1155:doi 1107:doi 1061:BBC 1028:doi 758:doi 746:211 719:doi 686:doi 547:doi 500:doi 496:128 437:doi 310:Sol 2476:: 1931:31 1173:. 1163:. 1149:. 1145:. 1121:. 1113:. 1105:. 1095:13 1093:. 1089:. 1059:. 1036:. 1026:. 1014:. 1010:. 979:. 952:. 924:. 896:. 870:. 809:. 764:. 756:. 744:. 740:. 713:. 709:. 684:. 672:. 668:. 641:. 608:. 589:^ 569:. 545:. 533:. 529:. 506:. 494:. 490:. 474:^ 458:. 433:82 431:. 427:. 411:^ 392:. 121:. 35:A 2266:e 2259:t 2252:v 1951:2 1941:7 1908:5 1437:) 1433:( 1256:e 1249:t 1242:v 1215:: 1181:. 1167:: 1157:: 1151:8 1129:. 1109:: 1101:: 1070:. 1044:. 1030:: 1022:: 1016:4 995:. 965:. 937:. 909:. 881:. 855:. 820:. 794:. 772:. 760:: 752:: 721:: 715:6 694:. 688:: 680:: 674:4 653:. 626:. 616:: 583:. 555:. 549:: 541:: 535:4 502:: 468:. 439:: 405:.

Index


P-wave
S-waves
quake
earthquake
Mars
plate tectonics
hotspots
Olympus Mons
Tharsis Montes
interior structure of Mars
many volcanoes
Moon
quakes on Venus
magnetic striping
crust
separating rifts
Mid-Atlantic Ridge
Valles Marineris
strike-slip
InSight
active fault

Viking program
Mars dust devil

InSight
seismometer
Seismic Experiment for Interior Structure
crust

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