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2019_KittitasCountyHMP_Volume 1_For Adoption
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2019-09-03 10:00 AM - Commissioners' Agenda
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2019_KittitasCountyHMP_Volume 1_For Adoption
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8/29/2019 12:06:14 PM
Creation date
8/29/2019 12:02:23 PM
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Meeting
Date
9/3/2019
Meeting title
Commissioners' Agenda
Location
Commissioners' Auditorium
Address
205 West 5th Room 109 - Ellensburg
Meeting type
Regular
Meeting document type
Supporting documentation
Supplemental fields
Alpha Order
l
Item
Request to Approve a Resolution to Adopt the 2019 Kittitas County Hazard Mitigation Plan as Approved by the Federal Emergency Management Agency
Order
12
Placement
Consent Agenda
Row ID
56110
Type
Resolution
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CHAPTER 10. EARTHQUAKE <br />10-3 <br />• Micro—Mw < 3 <br />Estimates of moment magnitude roughly match the local magnitude scale (ML) commonly called the <br />Richter scale. One advantage of the moment magnitude scale is that, unlike other magnitude scales, it does <br />not saturate at the upper end. That is, there is no value beyond which all large earthquakes have about the <br />same magnitude. For this reason, moment magnitude is now the most often used estimate of large <br />earthquake magnitudes. <br />Intensity <br />Currently the most commonly used intensity scale is the modified Mercalli intensity scale, with ratings <br />defined as follows (USGS, 1989): <br />• I. Not felt except by a very few under especially favorable conditions <br />• II. Felt only by a few persons at rest, especially on upper floors of buildings. <br />• III. Felt quite noticeably by persons indoors, especially on upper floors of buildings. Many <br />people do not recognize it is an earthquake. Standing cars may rock slightly. Vibrations similar <br />to the passing of a truck. Duration estimated. <br />• IV. Felt indoors by many, outdoors by few during the day. At night, some awakened. Dishes, <br />windows, doors disturbed; walls make cracking sound. Sensation like a heavy t ruck striking <br />building. Standing cars rocked noticeably. <br />• V. Felt by nearly everyone; many awakened. Some dishes, windows broken. Unstable objects <br />overturned. Pendulum clocks may stop. <br />• VI. Felt by all; many frightened. Some heavy furniture moved; a few instances of fallen plaster. <br />Damage slight. <br />• VII. Damage negligible in buildings of good design and construction; slight in well -built <br />ordinary structures; considerable in poorly built or badly designed structures. Some chimneys <br />broken. <br />• VIII. Damage slight in specially designed structures; considerable damage in ordinary <br />buildings with partial collapse. Damage great in poorly built structures. Fall of chimneys, <br />factory stacks, columns, monuments, walls. Heavy furniture overturned. <br />• IX. Damage considerable in specially designed structures; well-designed frame structures <br />thrown out of plumb. Damage great in substantial buildings, with partial collapse. Buildings <br />shifted off foundations. <br />• X. Some well-built wooden structures destroyed; most masonry and frame structures destroyed <br />with foundations. Rails bent. <br />• XI. Few, if any (masonry) structures remain standing. Bridges destroyed. Rails bent greatly. <br />• XII. Damage total. Lines of sight and level are distorted. Objects thrown into the air. <br />10.1.3 Ground Motion <br />Earthquake hazard assessment is also based on expected ground motion. This involves determining the <br />annual probability that certain ground motion accelerations will be exceeded, then summing the annual <br />probabilities over the time period of interest. The most commonly mapped ground motion parameters are <br />the horizontal and vertical peak ground accelerations (PGA) for a given soil or rock type. Instruments called <br />accelerographs record levels of ground motion due to earthquakes at stations throughout a region. These <br />readings are recorded by state and federal agencies that monitor and predict seismic activity.
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