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Giordano Bruno (crater)

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kilograms) of debris, triggering a week-long, blizzard-like meteor storm on Earth – yet no accounts of such a noteworthy storm of unprecedented intensity are found in any known historical records, including the European, Chinese, Arabic, Japanese and Korean astronomical archives. This discrepancy is a major objection to the theory that Giordano Bruno was formed at that time. Also, much older craters, e.g.,
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the Moon throbbed like a wounded snake. Afterwards it resumed its proper state. This phenomenon was repeated a dozen times or more, the flame assuming various twisting shapes at random and then returning to normal. Then, after these transformations, the Moon from horn to horn, that is along its whole length, took on a blackish appearance.
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From the midpoint of the division a flaming torch sprang up, spewing out, over a considerable distance, fire, hot coals and sparks. Meanwhile the body of the Moon which was below writhed, as it were in anxiety, and to put it in the words of those who reported it to me and saw it with their own eyes,
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of Earth (orbiting the Sun with the same period and phase as the Earth, appearing to orbit the Earth when viewed from there) was found to have a chemical composition similar to that of the lunar surface. After limiting crater size based on simulations of impacts that could eject a piece this large
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This raises the question of what the monks saw. An alternative theory holds that the monks just happened to be in the right place at the right time to see an exploding meteor coming at them and aligned with the Moon. This would explain why the monks were the only people known to have witnessed the
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However, these observations do not resolve the question of the crater's age. The expected odds of formation of a lunar crater of that size in the last 3,000 years are on the order of 0.1%. The impact creating the 22-km-wide crater would have kicked up 10 million tonnes (10 billion
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measurements of its libration in longitude were judged to be of the expected magnitude for such an event. In addition, the location recorded fits in well with the crater's location. Additional evidence of Giordano Bruno's youth is its spectacular
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into a quasi-satellite orbit, and limiting crater age to between 1 and 10 million years based on the instability of the asteroid's orbit, a 2024 study found that the most likely origin is the Giordano Bruno crater.
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Morota, T.; Haruyama, J.; Miyamoto, H.; Honda, C.; Ohtake, M.; Yokota, Y.; Matsunaga, T.; Hirata, N.; Demura, H.; Takeda, H.; Ogawa, Y.; Kimura, J. (2009). "Formation age of the lunar crater Giordano Bruno".
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than the surrounding surface. The ray material extends for over 150 kilometres (93 mi) and has not been significantly darkened by space erosion. Some of the ejecta appear to extend as far as the crater
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impact on the Moon would create a plume of ejecta rising up from the surface, which is consistent with the monks' description. The impact would be expected to perturb the Moon's motions, and
278:. The ratio of the length of these rays to the diameter of the crater is the largest for a large crater on the Moon, suggesting it is the youngest such crater. Because 588: 856:
Menzel, D. H.; Minnaert, M.; Levin, B.; Dollfus, A.; Bell, B. (1971). "Report on Lunar Nomenclature by the Working Group of Commission 17 of the IAU".
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Camale, O.; Mulholland, J. D. (1978). "Lunar Crater Giordano Bruno: A.D. 1178 Impact Observations Consistent with Laser Ranging Results".
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In 1976, the geologist Jack B. Hartung proposed that this described the formation of the crater Giordano Bruno.
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million years, much too old for the hypothesis. Further scientific studies have strengthened this age.
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constantly rain down, they kick up enough dust to quickly (in geological terms) erode a ray system.
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event; such an alignment would only be observable from a specific spot on the Earth's surface.
1017: 998: 976: 952: 926: 907: 822: 801: 608: 535: 168: 163:, just beyond the northeastern limb. It lies in an area that can be viewed during a favorable 873: 691: 669: 656:"Lunar-like silicate material forms the Earth quasi-satellite (469219) 2016 HO3 Kamoʻoalewa" 629: 519: 477: 458:"Was the Formation of a 20-km Diameter Impact Crater on the Moon Observed on June 18, 1178?" 405: 401: 172: 137: 333: 302: 869: 687: 562: 515: 473: 948: 482: 457: 409: 279: 199: 129: 1080: 990: 970: 897: 893: 885: 750: 721:"Earth's weird 'quasi-moon' Kamo'oalewa is a fragment blasted out of big moon crater" 705: 547: 417: 346: 219: 192: 152: 434: 102: 366: 31: 816: 523: 789: 438: 696: 655: 1051: 785: 275: 238: 179: 654:
Sharkey, Ben; Reddy, Vishnu; Malhotra, Renu; et al. (11 November 2021).
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When viewed from orbit, Giordano Bruno is at the center of a symmetrical
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Who's Who on the Moon: A Biographical Dictionary of Lunar Nomenclature
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at an estimated 800 million years, still have prominent ray systems.
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Lunar probe Kaguya overflight of Giordano Bruno crater (video)
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High-resolution images obtained by the Japanese satellite
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within it and its ejecta deposits. This gave an age of
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In 2021, the 40–100 m (130–330 ft) asteroid
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USGS Astrogeology Research Program. 7: 241:reported to the abbey's chronicler, 836:McDowell, Jonathan (15 July 2007). 390:Meteoritics & Planetary Science 371:Gazetteer of Planetary Nomenclature 563:"Historic lunar impact questioned" 483:10.1111/j.1945-5100.1976.tb00319.x 410:10.1111/j.1945-5100.2009.tb01211.x 14: 794:The Clementine Atlas of the Moon 218:showing the extent of the rays. 1057:Giordano Bruno, The Big Picture 975:(6th revised ed.). Dover. 765:Blue, Jennifer (25 July 2007). 758:Catalogue of Lunar Nomenclature 151:is a 22-kilometre (14 mi) 1073:Featured Image, 25 August 2011 997:. Cambridge University Press. 925:. Cambridge University Press. 587:Stiles, Lori (20 April 2001). 1: 719:Lea, Robert (23 April 2024). 561:Kettlewell, Jo (1 May 2001). 1063:Featured Image, 26 June 2012 923:The Moon Observer's Handbook 524:10.1126/science.199.4331.875 303:counting the smaller craters 995:Mapping and Naming the Moon 222:is in the right foreground. 1118: 1092:Impact craters on the Moon 798:Cambridge University Press 697:10.1038/s43247-021-00303-7 1067:Outside of Giordano Bruno 1012:Wlasuk, Peter T. (2000). 613:: CS1 maint: unfit URL ( 456:Jack B., Hartung (1976). 367:"Giordano Bruno (crater)" 290:at 108 million years and 29: 1045:in the foreground, from 1102:12th century in science 921:Price, Fred W. (1988). 842:Jonathan's Space Report 402:2009M&PS...44.1115M 904:Sterling Publishing Co 256: 234: 223: 145: 858:Space Science Reviews 634:University of Hawaiʻi 593:University of Arizona 229: 213: 171:to the northwest and 140: 838:"Lunar Nomenclature" 821:. Tudor Publishers. 870:1971SSRv...12..136M 688:2021ComEE...2..231S 516:1978Sci...199..875C 474:1976Metic..11..187H 153:lunar impact crater 67: /  26: 21:Feature on the moon 1014:Observing the Moon 878:10.1007/BF00171763 749:Andersson, L. E.; 330:469219 Kamoʻoalewa 271:laser rangefinding 235: 230:Oblique view from 224: 214:Oblique view from 186:that has a higher 175:to the southeast. 146: 1023:978-1-85233-193-1 1004:978-0-521-62248-6 991:Whitaker, Ewen A. 982:978-0-486-20917-3 958:978-0-913135-17-4 945:Atlas of the Moon 932:978-0-521-33500-3 913:978-0-304-35469-6 828:978-0-936389-27-1 807:978-0-521-81528-4 431:The Cosmic Winter 135: 134: 1109: 1027: 1008: 986: 967:Webb, Rev. T. 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A. 748: 744: 739: 729: 727: 718: 717: 713: 653: 652: 648: 638: 636: 628:Martel, Linda. 627: 626: 622: 605: 598: 596: 586: 585: 581: 571: 569: 560: 559: 555: 501: 500: 491: 455: 454: 445: 429: 425: 386: 385: 378: 365: 364: 360: 356: 343: 334:quasi-satellite 326: 311: 309: 308: 306: 280:micrometeorites 208: 119:258° at sunrise 92: 75: 73: 69: 66: 61: 58: 56: 54: 53: 43: 22: 17: 12: 11: 5: 1115: 1113: 1105: 1104: 1099: 1097:Giordano Bruno 1094: 1089: 1079: 1078: 1075: 1074: 1064: 1054: 1049: 1034: 1033:External links 1031: 1029: 1028: 1022: 1009: 1003: 987: 981: 963: 957: 949:Kalmbach Books 937: 931: 918: 912: 894:Moore, Patrick 890: 864:(2): 136–186. 853: 833: 827: 812: 806: 782: 762: 745: 743: 740: 738: 737: 711: 646: 620: 579: 553: 489: 468:(3): 187–194. 443: 423: 376: 357: 355: 352: 351: 350: 342: 339: 325: 322: 207: 204: 200:Giordano Bruno 149:Giordano Bruno 133: 132: 130:Giordano Bruno 127: 121: 120: 117: 111: 110: 105: 99: 98: 90: 84: 83: 71:35.9°N 102.8°E 51: 45: 44: 35: 25:Giordano Bruno 20: 15: 13: 10: 9: 6: 4: 3: 2: 1114: 1103: 1100: 1098: 1095: 1093: 1090: 1088: 1085: 1084: 1082: 1072: 1068: 1065: 1062: 1058: 1055: 1053: 1050: 1048: 1044: 1040: 1037: 1036: 1032: 1025: 1019: 1015: 1010: 1006: 1000: 996: 992: 988: 984: 978: 974: 973: 968: 964: 960: 954: 950: 946: 942: 941:Rükl, Antonín 938: 934: 928: 924: 919: 915: 909: 905: 901: 900: 895: 891: 887: 883: 879: 875: 871: 867: 863: 859: 854: 843: 839: 834: 830: 824: 820: 819: 813: 809: 803: 799: 795: 791: 787: 783: 772: 768: 763: 759: 757: 752: 747: 746: 741: 726: 722: 715: 712: 707: 703: 698: 693: 689: 685: 680: 675: 671: 667: 663: 662: 657: 650: 647: 635: 631: 624: 621: 616: 610: 594: 590: 583: 580: 568: 564: 557: 554: 549: 545: 541: 537: 533: 529: 525: 521: 517: 513: 509: 505: 498: 496: 494: 490: 484: 479: 475: 471: 467: 463: 459: 452: 450: 448: 444: 440: 436: 432: 427: 424: 419: 415: 411: 407: 403: 399: 395: 391: 383: 381: 377: 372: 368: 362: 359: 353: 348: 347:5148 Giordano 345: 344: 340: 338: 335: 332:, which is a 331: 323: 321: 317: 304: 300: 295: 293: 289: 283: 281: 277: 272: 268: 264: 259: 255: 250: 248: 244: 240: 233: 228: 221: 220:Mare Marginis 217: 212: 205: 203: 201: 196: 194: 189: 185: 181: 176: 174: 170: 166: 162: 158: 154: 150: 143: 139: 131: 128: 126: 122: 118: 116: 112: 109: 106: 104: 100: 96: 91: 89: 85: 80: 52: 50: 46: 42: 40: 33: 28: 19: 1039:AS08-12-2209 1016:. Springer. 1013: 994: 971: 944: 922: 898: 861: 857: 845:. Retrieved 817: 796:. New York: 793: 774:. Retrieved 754: 728:. Retrieved 724: 714: 665: 659: 649: 637:. Retrieved 623: 597:. Retrieved 582: 570:. 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Index


NASA
Coordinates
35°54′N 102°48′E / 35.9°N 102.8°E / 35.9; 102.8
Diameter
km
Depth
Colongitude
Eponym
Giordano Bruno

LRO
lunar impact crater
far side
Moon
libration
Harkhebi
Szilard
ray system
ejecta
albedo
Boss
Giordano Bruno

Apollo 11
Mare Marginis

Apollo 16
Canterbury
Gervase

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