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Revision as of 23:48, 8 July 2017 view sourceJ. Johnson (talk | contribs)Autopatrolled, Extended confirmed users, IP block exemptions19,647 edits Undid revision 789690752 by DePiep (talk) Please do not break the template simply because you don't like theformat.← Previous edit Revision as of 23:54, 8 July 2017 view source DePiep (talk | contribs)Extended confirmed users294,285 edits Undid revision 789694079 by J. Johnson (talk) 1. I did not break anything. 2. the testcases page now is double again. 3. another personal jab in your es (why?)Next edit →
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Revision as of 23:54, 8 July 2017

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WarningThis template is used on approximately 2,200 pages and changes may be widely noticed. Test changes in the template's /sandbox or /testcases subpages, or in your own user subpage. Consider discussing changes on the talk page before implementing them.
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Shortcut
  • {{M}}
  • For the "small letter m with dot below" please copy-and-paste: ṃ

Given a valid code (see table), outputs an earthquake magnitude scale label, either the generic M, or a subtype (such as Mw or mbLg), conformable with the labels most commonly used by the major seismological authorities. The article is automatically added to a tracking category. Optionally adds a value or relation, identifies a source, or links to explanatory text at Seismic magnitude scales.

Usage

The full name serves to better identify this template's purpose. For most practical purposes, the shortcut {{M}} is used as described below.

  • {{ M | <code*> | <value or relation> | src = <source> | link=y }}

A valid code is required (see table), other parameters are optional.

Examples

Label only:

  • {{M|w}} → Mw

With a value or range:

  • {{M|s|5.1}} → Ms  5.1.
  • {{M|w|6.2 – 6.5}} → Mw  6.2 – 6.5

Label wikilinked to explanatory text (useful for first mention):

To show that a magnitude is from a particular catalog or source use |src=:

  • {{M|w|8.1|src=HRV}}, {{M|e|8.8|src=USGS-PDE}} → Mw  8.1,   Me  8.8
(Note: this is not suitable for purposes of WP:Verification.)

There are multiple magnitude scales. To maintain accuracy and avoid error please use the proper code (see below). If you are uncertain use the special maintenance code "?", which flags this instance for further attention:

  • {{M|?}} → Unknown mag. scale

Typical use in article text, with in-line citation:

  • The 1964 Alaska earthquake, magnitude {{M|w|6.7|src=NEIC}}<ref>{{short-isc|EHB|869809}}.</ref> ....

The special code "magnitude" produces a suitable wikilink for generic use:

  • A Code invalid. 7 earthquake ....

The special codes "M" and "mag" produce a suitably wikilinked caption for use in tables:

  • {{M|M}} → Mm; {{M|mag}} → Code invalid.

The standard symbol for seismic moment can be produced as straight text, or as a math variable (applies CSS 'texhtml' styling using {{mvar}}):

  • {{M|0}} → M0; {{M|0tex}} → Code invalid.

 Important note: Please do NOT specify a magnitude as "Richter scale" just because a newspaper or other popular media says "Richter". That is usually incorrect. Earthquake magnitudes reported by the U.S. Geological Survey (USGS) and other seismological authorities now generally use the moment magnitude scale for magnitudes greater than 4.0. While most newspapers and other popular media refer to this as the "Richter" magnitude, that is not correct. Richter's original scale, explicitly denoted with the symbol "ML" or "ML" (where "L" indicates "Local"), was developed for measuring the magnitude of earthquakes in the vicinity of southern California. While the "Richter" and moment magnitude scales are similar, they do differ, particularly for earthquakes stronger than about M 6.5, or deeper than about 50 km.

In general: where any source specifies magnitude on a scale other than "Richter", or uses "M" (or "m") with one or more other letters (such as ML, Mw, Ms, or mb), that can be relied on; use the table below to match the label and determine the proper code.

Where a newspaper or other popular media refers to the scale or magnitude of a recent earthquake as "Richter" it is probably the popular mis-identification of the moment magnitude scale. Best practice is to check with an authoritative source, such as the USGS or the International Seismic Centre (see below). USGS policy is that magnitudes in press releases, indicated as "M" without any additional characters, are implicitly moment magnitude. But: do not use the "w" code if the source does not actually say "Mw" or "moment magnitude scale". If you have a strong basis for believing moment magnitude is meant – e.g., because it is a USGS press release – use the "dot" code to indicate an implicit Mw. E.g.: {{M|.|5.7}}M  5.7; {{M|.|link=y}}Moment mag. scale.

If you are not sure of the scale, use {{M|?}}. See below on how to find authoritative magnitudes.

Data sources

Newspapers and other mass media are not reliable sources for earthquake magnitudes. It is preferable that earthquake magnitudes always be obtained from authoritative sources, such as the following.

  • The ANSS (Advanced National Seismic System) Composite Catalog, commonly known as "ComCat" is a near-realtime repository of earthquake information from the USGS (United States Geological Survey) and various regional data centers, with additional data from seismic networks around the world. Event pages for significant events generally have an executive summary, a tectonic overview, past earthquake history of that area, ShakeMaps, and other material. ComCat can be accessed in several ways:
  • Latest Earthquakes. In most cases there is an initial report within 10 to 30 minutes of all magnitude 5.0+ earthquakes globally, and magnitude 4.0+ earthquakes within the contiguous U.S. Note that the magnitudes and locations in the initial reports are only first-order approximations, which get revised in the following hours, days, and months.
All of these access methods link to event pages in the ANSS Comprehensive Catalog (ComCat), which can be cited using {{short-anss}} and {{cite_anss}}.
  • The On-Line Bulletin (IRIS mirror) incorporates several catalogs (databases). There are catalog-specific search functions for finding events constrained by date period, magnitude range, or region (by latitude and longitude, or Flinn-Engdahl regions). Data may be revised years later as more data is obtained or processes refined. This is the most complete, most authoritative, and preferred source for earthquake magnitudes and epicenters.
  • Event Bibliography (IRIS mirror) of scientific articles for notable events, indexed chronologically. (Useful for finding ISC event id.)
  • The ISC-GEM Global Instrumental Earthquake Catalogue: Definitive magnitudes for selected earthquakes since 1900. (Source id: GEM.)
Data from the ISC can cited using {{short-isc}} and {{cite isc}}.

Earthquake magnitudes are given on different scales because they measure different aspects of the event, or are measured in different ways. It is valid to list multiple magnitudes for an event (not to be confused with multiple events such as foreshocks, aftershocks, and doublet earthquakes). Estimates of magnitude may differ between networks and across time because of differences or changes in how the seismograms are read and the data processed. For details see the NMSOP-2 documentation (below).

Table of codes

These are the most commonly found scales of earthquake magnitude. Any scale not found in this table is mostly likely one of the following:

  • An intensity scale. See Seismic intensity scales for explanation. This template does not cover intensity scales.
  • A regional (or "local") scale used by some particular seismic network (or country). In general it is preferable to use one of the better known scales from the table. Exceptions are for historical reports; you will need to explicitly format as appropriate. If the scale has been properly calibrated (see MNSOP-2, Chapter 3, §3.2.4.3, p. 65) then "L" may be appropriate, along with the |src= parameter.
  • A technical scale. While these might come up in an article related to seismology, they are not appropriate for general description of earthquakes. If needed, please format appropriately. On first use be sure to add a footnote explaining the scale.

Be careful to distinguish upper- and lower-case "M/m", "B/b", "L/l", and "I/i". Other than that case is generally not significant, nor italicization or subscripting.

The examples in the table are representative, even comprehensive, but not complete.

Labels and codes for various earthquake magnitude scales
As seen in sources WP Code Mag. scale Cat. # Comments
IASPEI NMSOP USGS ISC BSSA
-- -- -- -- -- Unknown mag. scale ? Unspecified M_? 0 WP: scale is unspecified or indeterminate.
-- -- -- -- -- Scale/mag. questioned ?? Needs verification M_?? 0 WP: the scale and/or magnitude needs verification.
-- -- -- -- -- Richter mag. scale R? Dubious "Richter" M_R? 0 WP: "Richter" scale is asserted, but dubious.
UK Code invalid. uk Unknown M_uk 0 Source says "unknown" scale. Might be 1954 MGR or MPAS mag.; see below (gr), or here.
ML Ml ML ML ML 'Local' mag. scale l Local ("Richter") M_L 0 §4.1. "Local" to Southern Calif. Adapted for other regions, but not necessarily comparable.
MJMA Mj MJMA Code invalid. jma JMA "Local" mag. M_jma 0 §3.2.4.7. Japanese Meteorological Agency. Also MJ or MJMA, but not Mw(JMA).
Mh Mh Code invalid. h by "hand" M_h 0 Ad hoc methods for special cases
M0, M0 M0 M0 Scalar moment 0 seismic moment M_0 0 "M zero". A physical value, basis of Mw. In Newton-meters or dyne-centimeters
M0 Code invalid. 0tex seismic moment M_0tex 0 "M zero" as a math variable in text
M M Moment mag. scale . moment mag. M_w. 0 dot: implicit Mw.
Mw Mw, w Mw Moment mag. scale w moment mag. M_w 0 §4.7. Use only for explicit Mw, Mw, or mw.
Mww, ww Mw mag. from W-phase ww M_ww 0 Mw from centroid m.t.i. (moment tensor inversion) of W-phase.
Mwc, wc Mw mag. from centroid wc M_wc 0 Mw from centroid m.t.i. of long-period surface waves.
Mwb, wb Mw mag. from body-waves wb M_wb 0 Mw from m.t.i. of long-period body waves.
Mwr, wr Mw mag. at regional distance wr M_wr 0 Mw from m.t.i. of whole seismogram at regional distances.
Mwp, wp Mw mag. from P-waves wp M_wp 0 Mw from integrated p-wave §3.2.8.2
Mwpd Code invalid. wpd M_wpd 0 Mwp w/ duration §3.2.8.3
Mi Code invalid. i M_i 0 Only if lower-case "i"! USGS synonym for Mwp
mb mb mb Mb mb Body-wave mag. b body-wave, short-period M_b 0 §4.3. Case sensitive: use "b"
mB mB -- M Mb(BB) Body-wave mag. B body-wave, broadband M_B 0 §4.2; Gutenberg, 1945b,c. Case sensitive: use "B".
mB_BB mB -- M Mb(BB) Body-wave mag. bbb body-wave, broadband M_Bbb 0 §4.2
mb_Lg mbLg mb_Lg, MLg mb(Lg) Lg-wave mag. blg mb from Lg wave M_bLg 0 §3.2.4.4; §4.6; Nuttli, 1986. North America east of the Rocky Mountains, and other cratons
Mn MN Nuttli (Lg-wave) mag. n mb from Lg wave M_N 0 §3.2.4.4; §4.6; Nuttli, 1973. Same as mbLg
mBc Code invalid. bc Cumulative body-wave M_Bc 0 §3.2.8.1
Ms Ms Ms Surface-wave mag. s surface wave M_s 0 §4.4. small "s": Gutenberg (1945a) ~20 s period s.w.; Ms_20
Ms MS MS Surface-wave mag. S surface wave M_S 0 §4.4. Big "S": broadband s.w. (Ms_BB), or (older sources) mis-capitalized Ms
Ms_20 Ms Ms Ms Ms(20) Surface-wave mag. s20 surface-wave 20s M_s20 0 §4.4. 20 s period s.w. mag. per IASPEI
Ms_BB Ms -- MS Ms(BB) Surface-wave mag. sbb surface wave broadband M_sbb 0 §4.5. Broadband s.w. mag. per IASPEI
Mz Surface-wave mag. z surface wave, vertical M_z 0 Measured from the vertical phase before that became standard.
Ms7 MS7 Code invalid. s7 surface wave M_s7 0 Vertical phase on Chinese seismograph
MSn Code invalid. sn surface wave M_sn 0 1-second period per Nuttli, 1983
MGR MGR Code invalid. gr Gutenberg-Richter M_gr 0 1954 G-R version of Ms. Includes MPAS ("Pasadena")
MR Code invalid. r Rothe M_r 0 Not "Richter"! Averaged Ms per Rothe 1969
MLH Code invalid. lh Russian Ms M_LH 0 Parts of Russia (Obninsk)
Mc Mc Coda length mag. c coda length M_c 0 §3.2.4.5
Md Md MD MD Duration mag. d duration M_d 0 §3.2.4.5. Many variants. Not JMA displacement mag.
Mt Tsunami mag. scale t tsunami mag. M_t 0 §3.2.6.7. Used by PTWC
Mm mantle mag. scale m mantle mag. M_m 0 §3.2.8.5. Used by PTWC
Me Me Energy mag. scale e energy mag. M_e 0 §3.2.7.2
K K-class K 0 See Energy class. Use Template:K
M(K) K-class mag. scale k K-class mag. M_K 0 Mag. calculated from "energy class" K
Mms Macroseismic mag. ms macroseismic M_ms 0 §3.2.6.6. Generic mag. estimated from macroseismic effects
Mfa, FA Mfa Felt-area mag. scale fa mb from felt-area M_fa 0 Stover & Coffman, 1999. Est. from extent of felt-area. Multiple methods.
MLa Code invalid. la ML from felt-area M_la 0 ML est. from intensity reports; for Calif. and Hawaii
MI Code invalid. I ML from intensity M_I 0 Only if upper-case "I"! Est. from epicentral intensity.

Examples of use are from the International Association of Earth Physics and Interior (IASPEI), the first edition of the New Manual of Seismological Practice (NMSOP)(the second edition follows the IASPEI), the United States Geological Survey (USGS) National Earthquake Information Center (NEIC), the International Seismological Centre (ISC), and the Bulletin of the Seismological Society of America (BSSA), as summarized in table 3 of the IASPEI/MNSOP-2 Information Sheet 3.3. Additional magnitude scales from Chapter 3 of MNSOP-2, ISC documentation, the USGS, and a review of the literature. Section numbers under "Comments" are for either Chapter 3, or Information Sheet 3.3

Principal references on usage are:

These sources also have extensive discussion and references on the derivation and comparison of the various scales.

The nomenclature style implemented here is adapted from IASPEI/MNSOP-2 Information Sheet 3.3. This style differs from IASPEI style mainly in using subscripts rather than underscores, and from BSSA style mainly in not using parentheses.

"Cat.": the Categories for tracking use of these various scales. "#" is the number of articles in that category.

See also

The above documentation is transcluded from Template:Earthquake magnitude/doc. (edit | history)
Editors can experiment in this template's sandbox (edit | diff) and testcases (edit) pages.
Add categories to the /doc subpage. Subpages of this template. Categories: