Surface-wave Magnitude
Surface-Wave Magnitude is a quantitative measure of an earthquake's size, belonging to the class of magnitude scales, that is distinguished by its derivation from the amplitude and period of surface waves propagating along the Earth's crust at distant seismograph stations.
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10.4K
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271
Authors
132
Institutions
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2017–2026
14
Variants
MsSurface Wave Magnitude
Parents
137
MAGNITUDE AND ENERGY OF EARTHQUAKES
B. Gutenberg, C. F. Richter · Annals of Geophysics · 1956 · 814 citations · Full text
Magnitude and Energy of Earthquakes
B. Gutenberg, C. F. Richter · Nature · 1955 · 732 citations
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California Institute of Technology
Pasadena, United States
8 h-index
16 publications
2.5K citations

Imperial College London
London, United Kingdom
7 h-index
9 publications
1.3K citations
United States Geological Survey
Reston, United States
7 h-index
14 publications
1.3K citations
Planetary Science Institute
Tucson, United States
4 h-index
5 publications
308 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
4 h-index
9 publications
1.2K citations
Columbia University
New York, United States
4 h-index
9 publications
1.2K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
4 h-index
6 publications
332 citations
GNS Science
Lower Hutt, New Zealand
4 h-index
5 publications
131 citations
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BSSA · 48 publications · 3.8K citations
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GJI · 15 publications · 859 citations
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JGR · 7 publications · 833 citations
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5 publications · 376 citations
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4 publications · 176 citations
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