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PLENARY SESSION 2: Transforming the Seattle Waterf ...
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The speaker explains how Seattle’s geological and human history informs modern waterfront engineering. Glaciation, volcanic deposits, earthquakes, rivers, and later land reclamation created highly variable ground conditions. Historical maps and photographs reveal former shorelines, marshes, sawmill waste, loose fill, buried timber piles, and other obstructions that may remain underground.<br /><br />These conditions shaped major infrastructure projects. The replacement seawall used jet grouting to form a stable mass despite buried timber and soft soils. The Alaskan Way Viaduct was replaced by a deep-bored tunnel, which required managing mixed ground, groundwater, settlement, and construction-related dewatering. Current waterfront redevelopment also involved challenging retaining walls, lightweight cellular concrete, and measures to prevent new foundations from affecting historic buildings and a century-old railroad tunnel.<br /><br />A central design concern is seismic risk: loose, saturated fill can liquefy and spread laterally, threatening waterfront structures. The speaker’s main lesson is that engineers should investigate not only geology but also a site’s human history. Historical research, combined with borings and monitoring, can reveal hidden risks and help teams plan safer, more buildable projects.
Keywords
Seattle waterfront
geological history
seismic risk
liquefaction
land reclamation
jet grouting
deep-bored tunnel
retaining walls
historical research
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