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Resolution_2025 Kittitas County Hazard Mitigation Plan
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2025-08-05 10:00 AM - Commissioners' Agenda
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Resolution_2025 Kittitas County Hazard Mitigation Plan
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Last modified
7/31/2025 12:07:24 PM
Creation date
7/31/2025 12:04:00 PM
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Meeting
Date
8/5/2025
Meeting title
Commissioners' Agenda
Location
Commissioners' Auditorium
Address
205 West 5th Room 109 - Ellensburg
Meeting type
Regular
Meeting document type
Supporting documentation
Supplemental fields
Item
Request to Approve a Resolution to Adopt the 2025 Kittitas County Hazard Mitigation Plan as Approved by the Federal Emergency Management Agency
Order
11
Placement
Consent Agenda
Row ID
133785
Type
Resolution
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2025 Hazard Mitigation Plan <br />Kittitas County, Washington <br /> <br /> <br />Chapter 4: Hazard Identification and Risk Assessment 182 <br />Volcano Eruption History <br />Glacier Peak <br />Glacier Peak erupts frequently. The eruptions are typically explosive and occasionally <br />voluminous. Most eruptions involve tephra, but many were accompanied by far reaching <br />lahars and dome building. <br /> <br />Glacier Peak has erupted multiple times in the last 15,000 years. About 13,000 years ago, <br />a series of large tephra eruptions occurred, accompanied by numerous lahars. One (1) <br />eruption was many times the size of the Mount St. Helens 1980 eruption. Within th e last <br />5,000 years, the volcano has produced frequent lava dome eruptions and subsequent dome <br />collapses and lahars. The most recent eruption was approximately 300 years ago. <br />Mount Rainier <br />Mount Rainier started erupting about 500,000 years ago with intermittent eruptions and <br />mudflows thereafter, and it still issues steam and gases from fumaroles near the summit <br />crater. Heat from the fumaroles melts the snow and ice at the crater, as well as the summit <br />icecap, forming caves beneath the ice. <br />Mount St. Helens <br />Mount St. Helens was formed from four (4) eruptive stages starting approximately 275,000 <br />years ago, and intermittent eruptions currently occur. The most significant eruption occurred <br />in 1980 after a series of earthquakes, steam explosions, and small eruptions at the summit <br />signaled a new eruptive phase of the volcano. By mid-April 1980, a large bulge of new <br />volcanic material had formed on the north flank of the mountain and moved outward at an <br />average rate of five (5) feet per day. In addition to ash, pyroclastic flows and lahars traveled <br />swiftly across the Pumice Plain and down the North Fork Toutle and Cowlitz Rivers, <br />destroying houses and bridges along the way. <br /> <br />Dome building eruptions occurred between 1980 and 1986, and 2004 and 2008. <br />4.6.8.6. Vulnerability and Impacts <br />According to the 2023 Washington State Enhanced Mitigation Plan, Kittitas County is not at risk of <br />exposure to lahar or lava flow. However, ashfall can travel much further and all of Kittitas County is <br />vulnerable to ashfall from any of the active volcanoes in the region. The following vulnerabilities and <br />impacts will mostly focus on ashfall. <br /> <br />Life Safety and Health: The entire Kittitas County population is vulnerable to the hazards of volcanic <br />activity due to its proximity to volcanoes in the Cascade Range. Life safety and health concerns after a <br />volcanic eruption include, but are not limited to, infectious disease, respiratory illness, burns, injuries from <br />falls, and vehicle accidents related to the slippery, hazy conditions caused by ash. Volcanic ash particles <br />can scratch the front of the eyes; and ash particles contain crystalline silica which is a material that causes <br />respiratory diseases such as silicosis. Ash particles can be so fine that they can be inhaled deep into the <br />lungs and with high exposure even healthy individuals can experience respiratory issues. Although <br />volcanic gases tend to quickly get blown away, heavy gases (e.g., carbon dioxide, hydrogen oxide) can <br />remain stagnant in low-lying areas which can irritate the nose, eyes, and throat. At higher elevations, <br />gases can cause rapid breathing, headache, dizziness, swelling, spasm of the throat, and suffocation. <br />Sulfur dioxide can cause breathing problems for both healthy and people with asthma and other <br />respiratory problems.232F <br />232 <br /> <br />Property Damage and Critical Facilities: The closer the property and critical facilities are to the volcano, <br />the higher the exposure to property damage from volcanic related hazards. Impacts to property and <br />critical facilities can range from minor to catastrophic. Volcanic ash can severely disrupt transportation <br />systems (e.g., roads, cars, railways, and aircraft) over extremely large areas for hours to days. Heavy <br />ashfall can affect general road conditions by reducing visibility on highways and railways. Additionally, <br /> <br />232 Centers for Disease Control and Prevention. (2024). Volcanoes and Your Safety. Retrieved from <br />https://www.cdc.gov/volcanoes/about/index.html.
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