| University of Alaska Geophysicial Institute | ||||
| Anchorage Region Strong-Motion Network | ||||
| Site Characteristics* | ||||
| Station code | Latitude | Longitude | NEHRP Site Class | 30m shear-wave vel (m/s) |
| K2-01 | 61.235 | -149.869 | D | 238 |
| K2-02 | 61.224 | -149.822 | C/D | 366 |
| K2-03 | 61.219 | -149.718 | C | 474 |
| K2-04 | 61.177 | -150.010 | D | - |
| K2-05 | 61.200 | -149.911 | D | 284 |
| K2-06 | 61.191 | -149.822 | C | 491 |
| K2-07 | 61.160 | -150.001 | D | 270 |
| K2-08 | 61.177 | -149.919 | D | 274 |
| K2-09 | 61.185 | -149.744 | C | 582 |
| K2-10 | 61.130 | -149.928 | D | 269 |
| K2-11 | 61.149 | -149.855 | C | - |
| K2-12 | 61.156 | -149.792 | C | 514 |
| K2-13 | 61.113 | -149.856 | C/D | 354 |
| K2-14 | 61.124 | -149.766 | C | - |
| K2-15 | 61.087 | -149.750 | C | 412 |
| K2-16 | 61.099 | -149.685 | B | - |
| K2-17 | 61.396 | -149.513 | - | - |
| K2-18 | 61.598 | -149.133 | - | - |
| K2-19 | 61.190 | -149.985 | D | - |
| K2-20 | 61.155 | -150.053 | D | - |
| K2-21 | 61.153 | -149.949 | D | - |
| K2-22 | 61.088 | -149.834 | C | - |
| * From Table 3, p. 99, Martirosyan et al (2002) | ||||
| References | ||||
| Dutta, U., Biswas, N. N., Martirosyan, A. H., Nath, S., Dravinski, M., Papageorgiou, A., and | ||||
| Combellick, R., 2000. Delineation of spatial variation of shear wave velocity with high- | ||||
| frequency Rayleigh waves in Anchorage, Alaska, Geophysics Jour. Int., V. 143, pp. 365-375. | ||||
| Dutta, U., Martirosyan, A. H., Biswas, N. N., Papageorgiou, A., Dravinski, M., and Combellick, | ||||
| R., 2001. Estimation of S-wave site response in Anchorage, Alaska from weak motion data | ||||
| using generalized inversion method, Bull. Seismol. Soc. Am., V. 91, No. 2, pp. 335-346. | ||||
| Martirosyan, A., Dutta, U., Biswas, N., Papageorgiou, A., and Combellick, R., 2002, | ||||
| Determination of site response in Anchorage, Alaska, on the basis of spectral ratio methods, | ||||
| Earthquake Spectra, V. 18, No. 1, pp. 85-104. | ||||