Aseismic creep
In
Causes
Aseismic creep accommodates
Measurements
Knowing how creep rates vary temporally and spatially along faults has important implications for predicting the timing, locations, and potential sizes of future earthquakes as well as the mechanics of fault behavior. Measurements of inter-seismic strain, as well as the associated pattern of coupling, are also crucial because they reveal the pockets where stress is building up and may be released in future seismic ruptures.[2] The emergence of space-based geodesy and newly developed remote sensing techniques are used to monitor crustal deformation in order to track aseismic creep on a fault.[2] Theodolite surveys are used with alignment arrays to track the creep. These data may then be used to restrict a fault's seismic capacity.
Examples
Aseismic creep exists along the Calaveras Fault in Hollister, California. Streets crossing the fault in Hollister show significant offset. Several houses sitting atop the fault are notably twisted, yet still habitable. The city attracts geologists and geology students almost weekly.
Other examples of faults that have experienced aseismic creep include a
See also
References
External links
- Tour of the Hayward Fault - California State University at Hayward web site with images showing fault creep on the Hayward Fault.
- Fremont Earthquake Exhibit - The Hayward Fault Exposed msnucleus.org, K-12 math and science education site.