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A creepmeter is an instrument that monitors the slow surface displacement of an active geologic fault in the Earth.[1] Its function is to record the slow, aseismic creep between earthquakes. The measurement range of a creepmeter is usually limited to 10–30 mm. Approximately 40 creepmeters are in operation in California—most are operated by the United States Geological Survey (USGS), but nine are maintained by the University of Colorado.
^"Monitoring Instruments". U.S. Geological Survey. Retrieved 11 February 2016.
A creepmeter is an instrument that monitors the slow surface displacement of an active geologic fault in the Earth. Its function is to record the slow...
distance of two ends of rod-type creepmeter also change associatively, resulting in different data output. Two aligned creepmeters were placed across the fault...
North Coulombmeter electrostatic charge of a material colorimeter color creepmeter slow surface displacement of an active geologic fault in the Earth corrator...
predict future earthquakes, installed an elaborate array of seismometers, creepmeters, strainmeters, and other instruments in and around Parkfield starting...
faulting along the Atacama Fault System and its relation to the subduction zone seismic cycle: a creepmeter study in N-Chile', EGU general assembly, pg.4298....
(0.59 in) occurred. Minor vertical displacements were also recorded. Creepmeters also indicated that several millimeters of slip occurred on the San Andreas...
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