Third Quarter Hanford Seismic report for Fiscal year 2003

Hartshorn, Donald C. ; Reidel, Steve P. ; Rohay, Alan C.

Pacific Northwest National Laboratory (U.S.)

关键词: Columbia River;    Sediments;    Geologic Structures;    Basalt;    Waste Management Columbia Basin;   

DOI  :  10.2172/15010369
RP-ID  :  PNNL-11557-23
RP-ID  :  AC05-76RL01830
RP-ID  :  15010369

美国|英语

来源: UNT Digital Library

【 摘 要 】

Hanford Seismic Monitoring provides an uninterrupted collection of high-quality raw and processed seismic data from the Hanford Seismic Network for the U.S. Department of Energy and its contractors. Hanford Seismic Monitoring also locates and identifies sources of seismic activity and monitors changes in the historical pattern of seismic activity at the Hanford Site. The data are compiled, archived, and published for use by the Hanford Site for waste management, Natural Phenomena Hazards assessments, and engineering design and construction. In addition, the seismic monitoring organization works with the Hanford Site Emergency Services Organization to provide assistance in the event of a significant earthquake on the Hanford Site. The Hanford Seismic Network and the Eastern Washington Regional Network consist of 41 individual sensor sites and 15 radio relay sites maintained by the Hanford Seismic Monitoring staff. For the Hanford Seismic Network, there were 356 triggers during the third quarter of fiscal year 2003. Of these triggers, 141 were earthquakes. Thirty-four earthquakes of the 141 earthquakes were located in the Hanford Seismic Network area. Stratigraphically 15 occurred in the Columbia River basalt, 13 were earthquakes in the pre-basalt sediments, and 6 were earthquakes in the crystalline basement. Geographically, 22 earthquakes occurred in swarm areas, 1 earthquake was associated with a major geologic structure, and 11 were classified as random events. During the third quarter, an earthquake swarm consisting of 15 earthquakes occurred on the south limb of Rattlesnake Mountain. The earthquakes are centered over the northwest extension of the Horse Heaven Hills anticline and probably occur at the base of the Columbia River Basalt Group.