Wood–Anderson torsion seismometer

E77001

The Wood–Anderson torsion seismometer is an early 20th-century mechanical seismograph designed to measure local earthquake ground motion with high sensitivity, forming the instrumental basis for the original Richter magnitude scale.

All labels observed (2)

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf mechanical seismograph ⓘ
scientific instrument ⓘ
seismometer ⓘ
torsion seismometer ⓘ
calibrationReferenceFor Richter local magnitude ML ⓘ
component damped horizontal pendulum ⓘ
lightweight mirror ⓘ
photographic recording drum ⓘ
torsion wire ⓘ
dampingType aperiodic damping ⓘ
dataUsedFor earthquake catalogs in early 20th century ⓘ
designedBy Harry O. Wood ⓘ
John A. Anderson ⓘ
developedInPeriod early 20th century ⓘ
eraOfMainUse 1930s ⓘ
mid-20th century ⓘ
field seismology ⓘ
formsBasisOf Richter magnitude scale ⓘ
surface form: original Richter magnitude scale
hasInfluenceOn standardization of earthquake magnitude measurements ⓘ
hasKeyRoleIn Richter magnitude scale ⓘ
hasOutput seismogram ⓘ
historicalSignificance provided first standardized instrumental basis for earthquake magnitude ⓘ
inspiredDevelopmentOf later standardized short-period seismometers ⓘ
locationOfOriginalUse Southern California ⓘ
measurementType horizontal ground motion ⓘ
namedAfter Harry O. Wood ⓘ
John A. Anderson ⓘ
notOptimizedFor teleseismic (distant) earthquakes ⓘ
operatingPrinciple torsional suspension of a horizontal pendulum ⓘ
optimizedFor local and regional earthquakes ⓘ
orientation typically installed in orthogonal horizontal components ⓘ
recordingMethod optical recording on smoked paper or photographic paper ⓘ
relatedTo Richter magnitude scale ⓘ
surface form: Richter scale

local magnitude scale ⓘ
replacedBy modern broadband seismometers ⓘ
requires careful mechanical calibration ⓘ
requiresInstallation rigid pier or foundation ⓘ
sensitivity high sensitivity to local earthquakes ⓘ
standardInstrumentFor original local magnitude (ML) scale ⓘ
status largely obsolete ⓘ
typicalMagnification about 2800 at 0.8 seconds ⓘ
typicalNaturalPeriod approximately 0.8 seconds ⓘ
usedAt Seismological Laboratory at Caltech ⓘ
usedBy early 20th-century seismological observatories in California ⓘ
usedFor determining earthquake magnitude ⓘ
measuring local earthquake ground motion ⓘ
recording seismic waves ⓘ

How these facts were elicited

Referenced by (4)

Full triples — surface form annotated when it differs from this entity's canonical label.

Richter magnitude scale → definedUsing → Wood–Anderson torsion seismometer ⓘ
Harry O. Wood → coDeveloperOf → Wood–Anderson torsion seismometer ⓘ
this entity surface form: Wood–Anderson seismograph
Harry O. Wood → notableWork → Wood–Anderson torsion seismometer ⓘ
John A. Anderson → notableWork → Wood–Anderson torsion seismometer ⓘ