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Moment magnitude scale

Updated: 12/30/2025, 12:48:24 PM Wikipedia source

The moment magnitude scale (MMS; denoted explicitly with Mw  or Mwg and generally implied with use of a single M for magnitude) is a measure of an earthquake's magnitude ("size" or strength) based on its seismic moment. Mw  was defined in a 1979 paper by Thomas C. Hanks and Hiroo Kanamori. Similar to the local magnitude/Richter scale (ML ) defined by Charles Francis Richter in 1935, it uses a logarithmic scale; small earthquakes have approximately the same magnitudes on both scales. Despite the difference, news media often use the term "Richter scale" when referring to the moment magnitude scale. Moment magnitude (Mw ) is considered the authoritative magnitude scale for ranking earthquakes by size. It is more directly related to the energy of an earthquake than other scales, and does not saturate – that is, it does not underestimate magnitudes as other scales do in certain conditions. It has become the standard scale used by seismological authorities like the United States Geological Survey for reporting large earthquakes (typically M > 4), replacing the local magnitude (ML ) and surface-wave magnitude (Ms ) scales. Subtypes of the moment magnitude scale (Mww , etc.) reflect different ways of estimating the seismic moment.

Tables

· Comparative energy released by two earthquakes › Comparison with TNT equivalents
3
3
Mw
3
ES(Joules)
2.0 · 1090
TNT-equivalency(tons)
-
equivalence Hiroshima-bomb(12.5 kT TNT)
-
4
4
Mw
4
ES(Joules)
6.3 · 1010
TNT-equivalency(tons)
00,000,000,015
equivalence Hiroshima-bomb(12.5 kT TNT)
0,000,000.0012
5
5
Mw
5
ES(Joules)
2.0 · 1012
TNT-equivalency(tons)
00,000,000.475
equivalence Hiroshima-bomb(12.5 kT TNT)
0,000,000.0380
6
6
Mw
6
ES(Joules)
6.3 · 1013
TNT-equivalency(tons)
00,000,015,000
equivalence Hiroshima-bomb(12.5 kT TNT)
0,000,001.2000
7
7
Mw
7
ES(Joules)
2.0 · 1015
TNT-equivalency(tons)
00,000,475,000
equivalence Hiroshima-bomb(12.5 kT TNT)
0,000,038.0000
8
8
Mw
8
ES(Joules)
6.3 · 1016
TNT-equivalency(tons)
00,015,000,000
equivalence Hiroshima-bomb(12.5 kT TNT)
0,001,200.0000
9
9
Mw
9
ES(Joules)
2.0 · 1018
TNT-equivalency(tons)
00,475,000,000
equivalence Hiroshima-bomb(12.5 kT TNT)
0,038,000.0000
10
10
Mw
10
ES(Joules)
6.3 · 1019
TNT-equivalency(tons)
15,000,000,000
equivalence Hiroshima-bomb(12.5 kT TNT)
1,200,000.0000
Mw
ES(Joules)
TNT-equivalency(tons)
equivalence Hiroshima-bomb(12.5 kT TNT)
3
2.0 · 1090
-
-
4
6.3 · 1010
00,000,000,015
0,000,000.0012
5
2.0 · 1012
00,000,000.475
0,000,000.0380
6
6.3 · 1013
00,000,015,000
0,000,001.2000
7
2.0 · 1015
00,000,475,000
0,000,038.0000
8
6.3 · 1016
00,015,000,000
0,001,200.0000
9
2.0 · 1018
00,475,000,000
0,038,000.0000
10
6.3 · 1019
15,000,000,000
1,200,000.0000

References

  1. These are normally not bolded. In the technical literature a single bolded "M" – with or without italicization – is used
  2. Bormann, Wendt & Di Giacomo 2013, p. 86.
  3. Bormann, Wendt & Di Giacomo 2013, p. 18.
  4. The "USGS Earthquake Magnitude Policy" for reporting earthquake magnitudes to the public as formulated by the USGS Earth
    https://earthquake.usgs.gov/aboutus/docs/020204mag_policy.php
  5. Miyake 2017, p. 112.
  6. Suzuki 2001, p. 121. See also Figure 2-22 in Richter 1958 (copy in Bormann, Wendt & Di Giacomo 2013, p. 60), which repli
  7. Gutenberg & Richter 1956a.
  8. Richter 1935.
  9. See Bormann & Saul 2009 for an overview.
  10. Gutenberg 1945a.
  11. Gutenberg 1945b, Gutenberg & Richter 1956b.
  12. See Seismic magnitude scales.
  13. Kanamori 1977, p. 2981.
  14. ISC-EHB Event 879136 [IRIS]. ISC-EHB Event 869809 [IRIS].
    https://www.isc.ac.uk/cgi-bin/web-db-v4?event_id=879136&out_format=IMS1.0&request=COMPREHENSIVE
  15. Miyake 2017, pp. 112–113; Stauder 1962, p. 39.
  16. Miyake 2017, p. 115.
  17. Ben-Menahem 1995, p. 1210; Maruyama 1963, p. 484.
  18. Ben-Menahem 1995, p. 1210.
  19. Miyake 2017, p. 115. See Byerly 1960 for a contemporary account of why many seismologists favored a single couple model.
  20. Miyake 2017, pp. 116, 117.
  21. Pujol 2003b, p. 164.
  22. Pujol 2003b, p. 165; Miyake 2017, pp. 117–118.
  23. Aki 1966b, p. 84; Pujol 2003b, p. 167.
  24. Julian, Miller & Foulger 1998, §2.2.1.
  25. Miyake 2017, pp. 114, 117; Maruyama 1963, p. 483.
  26. Miyake 2017, p. 117.
  27. Steketee 1958b, pp. 1168–1169.
  28. Stauder 1962, p. 42; Aki & Richards 2002, p. 48.
  29. Honda 1962, pp. 32, 65, and see bibliography; Ben-Menahem 1995, p. 1212; Udías 1991, p. 90; Maruyama 1963, p. 467.
  30. Miyake 2017, p. 467; Steketee 1958a, 1958b.
  31. Udías 1991 provides a partial overview.
  32. Pujol 2003b, pp. 165, 167; Miyake 2017, p. 118.
  33. Bormann, Wendt & Di Giacomo 2013, p. 14.
  34. Aki 1966b, p. 73; Kassaras & Kapetanidis 2018, p. 410.
  35. Beroza & Kanamori 2015, p. 5.
  36. Dziewonski, Chou & Woodhouse 1981, p. 2826; Aki 1966b.
  37. Aki 1966a, pp. 24, 36.
  38. Aki 1966a, p. 24.
  39. Bormann, Wendt & Di Giacomo 2013, p. 12, equation 3.1.
  40. Aki 1966b, p. 84.
  41. Bormann, Wendt & Di Giacomo 2013, p. 14; Bormann & Di Giacomo 2011, p. 412.
  42. Bormann, Wendt & Di Giacomo 2013, pp. 39–40.
  43. Bormann, Wendt & Di Giacomo 2013, p. 7.
  44. Deichmann 2006, p. 1268.
  45. Abe 1982, p. 322.
  46. Kanamori & Anderson 1975, p. 1076.
  47. Kanamori 1977.
  48. Boyle 2008.
  49. Bormann, Wendt & Di Giacomo 2013, p. 86
  50. Kanamori 1977.
  51. Hanks & Kanamori 1979.
  52. Das, Menesis & Urrutia 2023
  53. Kostrov 1974; Dahlen 1977.
  54. Choy & Boatwright 1995
  55. FAQs – Measuring Earthquakes: How much energy is released in an earthquake? United States Geological Survey
    https://web.archive.org/web/20120314043321/https://earthquake.usgs.gov/learn/faq/?faqID=33
  56. "Erdbeben – wenn die Erde zurückschlägt"
    https://www.wdr.de/tv/applications/fernsehen/wissen/quarks/pdf/Q_Erdbeben.pdf
  57. "Technical Terms used on Event Pages" n.d.
  58. Tsuboi et al. 1995.
  59. Bormann, Wendt & Di Giacomo 2013, §3.2.8.2, p. 135.
  60. Bormann, Wendt & Di Giacomo 2013, §3.2.8.3, pp. 137–128.
  61. Geophysical Research Letters
    https://agupubs.onlinelibrary.wiley.com/doi/10.1002/2017GL073801
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