Download PDF by Renata Dmowska: Advances in Geophysics, Vol. 47

By Renata Dmowska

ISBN-10: 0120188473

ISBN-13: 9780120188475

Advances in Geophysics quantity forty five provides major issues of famous curiosity to the geophysical group. the 1st subject is ice debris within the surroundings. Mathematical descriptions of ice particle shapes, their progress charges, and their effect on cloud improvement are awarded. the second one subject is earthquakes and seismological mapping. The authors current their examine related to predicting the positioning and depth of earthquakes.

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The most recent terrace at Middleton Island dates from 1300 years ago. However, the Middleton Island estimate may not be representative. Along Turnagain and Knik Arms of Cook Inlet, Combellick (1993) estimated an average recurrence interval of 590– 780 yr, in closer agreement with the longer of the estimates from geodetic data. Similarly, Plafker et al. (1992) reported an age of 665 –895 yr for the most recent earthquake uplift in the Copper River delta. Combellick (1992) obtained evidence from Girdwood, along the Turnagain Arm, that the penultimate great earthquake in the Anchorage region occurred 700 –900 yr ago.

There is far better consistency from analyst-to-analyst in the horizontal velocities than the vertical ones, as is typically the case. 4. Models of Southcentral Alaska Preseismic and Postseismic Crustal Deformation In the preceding sections we have focused on the geodetic measurements themselves and direct inferences from those measurements that do not depend strongly on specific model assumptions. This is not to say that model assumptions have not entered either implicitly or explicitly into the results we reviewed.

1999) nor Zweck et al. (2002) model allows CRUSTAL DEFORMATION IN THE SOUTHCENTRAL ALASKA 43 Fig. 18. Velocity profiles in the Katmai–Kodiak Island region relative to site Kdr2 (on Kodiak Island) as a function of the distance N328W from the trench. The error bars are two standard deviations. , in the N328W direction), while the lower panel shows the trench parallel velocities. 3 km. Although the sites are shown as a function of distance from the trench there are considerable alongstrike variations in their locations as well.

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Advances in Geophysics, Vol. 47 by Renata Dmowska


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