How could the instability of Rattlesnake Ridge affect Central Washington?
Potential ridge collapse could threaten the Yakima River's flow in Central Washington. The instability of Rattlesnake Ridge, which forms boundaries of the Union Gap, poses a threat of collapse that could block the Yakima River. The report notes that the ridge is subject to landslides if enough moisture seeps into the formation and a backstop fails. If the river were blocked, the resulting disruption to the Yakima River's flow would impact the water outlook and agricultural activity within Central Washington.
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- When
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How it reaches Central Washington
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The Yakima River cut through ridges as they rose in the Yakima Valley. Rattlesnake Ridge, which forms a boundary of the Union Gap, has shown fissures since 2017. While the fissure remains, the sliding earth has slowed down, forming a natural barrier at the base of the ridge. The ridges themselves are composed of basalt from lava flows and sedimentary material.
The full event1independent outlet -
The Yakima River is a geographical feature whose water outlook impacts agricultural activity within Central Washington. The threat of a landslide blocking the river would directly affect this water outlook.
No report states this step directly. Brind drew it from the reporting on each side of it, so treat it as an informed guess.
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region in Washington, United States
Everything about Central Washington
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The facts so far
As reported. Each one links to where it comes from.
- Rattlesnake Ridge forms the boundaries of the Union Gap and divides the upper and lower valley.yakimaherald.com
- The Yakima River formed the Selah and Union gaps as the rock formations buckled and rose.yakimaherald.com
- The ridge is a sandwich of basalt from lava flows and sedimentary material.yakimaherald.com
- Columbia Asphalt and Gravel moved its operations away from the area due to the cracks on Rattlesnake Ridge.yakimaherald.com
Why it matters
The stability of Rattlesnake Ridge is critical because its potential collapse could block the Yakima River, which is a vital water source for the region. If the river's flow were disrupted, it would directly threaten the agricultural activity and water outlook of Central Washington.
Geologically, the ridges in the Valley are the result of forces exerted over millions of years. The threat of landslides is not new, as the report references the 2009 slide that buried a quarter-mile of State Route 410 and the 2014 Oso Slide.
What we don't know yet
- What specific conditions (e.g., moisture levels) are required for the sedimentary rock to fail?
- What is the likelihood of the landslide widening and deepening to the point of blocking the river?
What would change this answer
— Other considerations
Beyond this explainer
Questions worth asking
Ideas the web ties closely to this story that the explainer doesn't mention. These are prompts for your own research: Brind hasn't answered them.
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About Waterproofing
Given that the ridge is a sandwich of basalt and sedimentary material, how does the inherent waterproofing of this specific rock structure affect its susceptibility to moisture-induced failure?
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About Joints
Since the ridge is subject to landslides when moisture seeps into the formation, do existing joints or fractures in the rock act as primary pathways for water infiltration?
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Who else could feel it
Other possible ripples from the same event.
Reporting
- yakimaherald.comOct 18
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Brind's analysis is written by AI from the reporting linked above and can be wrong. This explainer is a possibility worth considering, not a forecast: steps marked as Brind's reasoning are not stated in the reporting. It is not investment advice; do your own research.