Commencement Bay, Pierce County, WA -- Where Tacoma Actually Started

Tacoma waterfront / Old TownIndustrial Waterfront, Genuinely Rebuilt, Not a Resort Town

This page covers the historic waterfront and Old Town section of Tacoma specifically -- not the whole city of roughly 220,000 people, but the strip of Commencement Bay shoreline running from the Thea Foss Waterway downtown, north along Ruston Way, to Point Defiance Park. Old Town is where Tacoma itself began: Job Carr built a cabin near this shore in 1865, ahead of the Northern Pacific Railroad's arrival, and developer Morton McCarver platted "Tacoma City" here in 1868 after buying most of Carr's claim. What grew up around that original townsite is a genuinely industrial waterfront -- a working deepwater port chosen by the Northern Pacific Railroad as its western terminus in 1873, a copper smelter that operated at the north end of this same shoreline for nearly a century, and a waterway so contaminated by the 1980s that federal regulators listed it as a Superfund site. All of that has been substantially, verifiably rebuilt into residential and public space over the last three decades: the Thea Foss Waterway's industrial shoreline is now a public esplanade lined with condos and restaurants, the former ASARCO smelter site is now the mixed-use Point Ruston development, and the city's 1885 forced expulsion of its Chinese residents -- a real, documented event -- is now memorialized at Chinese Reconciliation Park on the same waterfront where it happened. This page treats that industrial-to-residential redevelopment story as the core identity of Tacoma's waterfront, distinct from Gig Harbor's small nautical-village character across the Narrows or Olympia's state-capital identity at the south end of the Sound. Where a figure could not be independently confirmed -- an exact current insurance premium, a precise Old Town population count separate from the whole city, or a confirmed feet-per-year liquefaction displacement figure -- this page says so rather than inventing a number.

Origin
Job Carr's 1865 cabin near this shore marks the original "Tacoma" townsite, platted as Tacoma City by Morton McCarver in 1868 -- predating the "New Tacoma" townsite that became downtown
Population & Setting
220,182 residents citywide at the 2020 Census; this page covers the Old Town/Ruston Way/Foss Waterway shoreline specifically, not the full city
Price Point
Citywide median home value roughly $465,000-$479,000 across 2025-2026 Redfin/Zillow snapshots; Old Town waterfront specifically cited in the $750,000-$1.3 million range, with view/waterfront properties reported frequently exceeding $2 million per a single 2025 brokerage source, not independently cross-verified
Seismic Reality
No hurricane risk on Puget Sound. The real hazard is Cascadia Subduction Zone and Seattle/Tacoma Fault earthquake risk, with documented liquefaction susceptibility in Commencement Bay's artificial-fill Tideflats and port areas
At a glance — the numbers agents don't quote
Tidal Puget Sound Flooding, Not Ocean Wave Action
Old Town and the Ruston Way shoreline front Commencement Bay, a deep, protected saltwater inlet of Puget Sound -- flood risk here comes from tidal surge and king-tide events pushing into low-lying shoreline parcels, not open-ocean wave action. FEMA flood mapping applies to specific Commencement Bay parcels the way it does on any tidal shoreline.
This page does not state a per-parcel flood zone. Confirm a specific address's flood zone designation with the City of Tacoma's Planning and Development Services Department or FEMA's Flood Map Service Center before budgeting a flood insurance figure.
Pacific Northwest Windstorms, Not Hurricanes
Puget Sound sees no landfalling hurricanes -- the cold Pacific water off Washington's coast doesn't sustain tropical cyclones. The real, recurring wind risk here is Pacific Northwest winter windstorms and atmospheric river events, well documented by the National Weather Service and University of Washington Atmospheric Sciences research.
The most dramatic documented consequence of wind in this exact area wasn't a hurricane -- it was the November 7, 1940 collapse of the original Tacoma Narrows Bridge ("Galloping Gertie"), brought down by sustained wind-driven aerodynamic flutter, not a storm surge. No Old-Town-specific outage-frequency figure was confirmed this research pass.
Artificial Fill and Documented Liquefaction Susceptibility
Commencement Bay's Tideflats and much of the industrial port shoreline near Old Town sit on artificial fill, which the Washington State Department of Natural Resources' own liquefaction susceptibility mapping for Central Puget Sound cities -- including Tacoma -- identifies as a real, elevated-risk soil condition in a major earthquake.
This is a genuine, documented geotechnical hazard, not a generic disclaimer -- WA DNR's Seismic Scenario Catalog runs loss-estimate scenarios specifically naming the Cascadia Subduction Zone, the Seattle Fault, and a separate Tacoma Fault. No parcel-specific liquefaction risk figure is stated here; have any waterfront or fill-adjacent property evaluated by a licensed geotechnical engineer.
Real Earthquake Precedent: the 2001 Nisqually Quake
The magnitude 6.8 Nisqually earthquake on February 28, 2001 -- epicenter roughly 11 miles northeast of Olympia -- caused an estimated $4 billion in regional damage. Tacoma itself saw comparatively less structural damage than nearby areas due to local soil and bedrock variation, but a roughly 1,000-cubic-meter landslide at Salmon Beach, on Tacoma's own Puget Sound bluff, destroyed two homes.
This is real, documented, relatively recent earthquake history for this exact region -- not a hypothetical. The Cascadia Subduction Zone offshore is capable of a substantially larger event than Nisqually; treat both as real, current planning factors, not settled probabilities.

What Actually Makes Tacoma's Waterfront and Old Town Different

Start with the fact that separates this page from every ocean-beach market on this site: Tacoma's waterfront is not, and has never tried to be, a resort destination. It is a working industrial harbor that has been substantially rebuilt into residential and public space over roughly three decades, and understanding that history -- not just the current amenities -- is essential to understanding what a buyer is actually purchasing here. Old Town itself is the literal origin point: Job Carr built a cabin near this shore in 1865, ahead of the Northern Pacific Railroad's decision to make Commencement Bay its western terminus, and developer Morton McCarver bought most of Carr's claim in 1868 to plat "Tacoma City." A separate townsite, "New Tacoma," grew up around the railroad's actual terminus and eventually merged with Old Town into the single city known today -- meaning Old Town's identity as the original settlement, distinct from downtown, is a real, documented historical fact, not marketing language. Two of Old Town's buildings carry that history forward physically: St. Peter's Church, Tacoma's oldest existing building, and Slavonian Hall, built by Croatian immigrants who settled here starting in the 1880s -- both on the National Register of Historic Places.

Commencement Bay was chosen as the Northern Pacific Railroad's western terminus in 1873 specifically because it could dock more than 50 ships at once and was deep enough for vessels of any draft -- a real geographic advantage that turned this shoreline into a major industrial harbor rather than a beach town. That legacy is still visible and economically active today: the Port of Tacoma now controls more than 2,400 acres along Commencement Bay's waterfront and, operating jointly with the Port of Seattle as the Northwest Seaport Alliance, ranks among North America's busier container ports. This isn't background trivia -- it directly shapes what it means to live on this waterfront. A buyer here is choosing genuine proximity to an active working port and its associated freight, rail, and industrial activity, a fundamentally different daily reality than a market built purely around tourism and recreation.

The most consequential single redevelopment story on this waterfront is the Thea Foss Waterway. Named for Thea Foss, who founded the Foss Maritime Company on this inlet in 1889, the waterway grew into a dense industrial hub of shipyards and manufacturers -- and by the 1980s had been largely abandoned, with decades of industrial activity leaving the soil, groundwater, and sediment contaminated enough that the EPA listed the Thea Foss and adjacent Wheeler-Osgood waterways as part of the broader Commencement Bay Nearshore/Tideflats Superfund site. The City of Tacoma commissioned the Foss Waterway Development Authority in 1996 to implement a redevelopment plan finalized in 1998; dredging and sediment capping wrapped up in 2006. What exists today is a genuine, verifiable transformation: a public esplanade running the length of the waterway, Thea's Landing as the first residential development in the formerly derelict industrial shoreline, the Museum of Glass with its free, 24/7, 500-foot Chihuly Bridge of Glass connecting the waterfront to downtown, and Dock Street Marina hosting yachts up to 120 feet. This is a Superfund-to-residential-neighborhood story with real dates and real regulatory documentation behind it, not a developer's talking point.

A second, parallel redevelopment sits at the north end of this same waterfront, adjacent to Old Town and Point Defiance Park: Point Ruston, built on the former ASARCO copper smelter site. That smelter began as the Ryan Smelter in 1888, became the Tacoma Smelting and Refining Company in 1890, and was sold in 1905 to the American Smelting and Refining Company (ASARCO), which converted it to copper smelting in 1912 and operated it until closing in 1985. The site was designated a Superfund cleanup location in 1983, and the plant's smokestack -- once the world's largest -- was demolished on January 17, 1993. EPA-overseen soil sampling covered 3,570 properties across Ruston and North Tacoma, with soil replaced at 2,436 of them, reflecting how far the smelter's contamination -- the "Tacoma Smelter Plume" -- actually spread beyond the plant footprint itself. Point Ruston, LLC purchased the site in 2006 and took over cleanup and redevelopment; what exists today is a mixed-use waterfront district of condos, restaurants, and shops at the north end of Ruston Way. A buyer evaluating property anywhere near this footprint should understand that legacy directly rather than assume it away -- ask specifically about soil testing and remediation status for any parcel near the former smelter site.

Between those two redevelopment zones runs Ruston Way, a roughly 3.2-mile paved waterfront path along Commencement Bay connecting a real string of public parks: Chinese Reconciliation Park, Jack Hyde Park, Old Town Dock, Dickman Mill Park, Les Davis Pier, Judge Jack Tanner Park, and Cummings Park, ending at Dune Peninsula inside Point Defiance Park. Chinese Reconciliation Park deserves to be named plainly and taken seriously, not glossed over: it commemorates the November 3, 1885 forced expulsion of Tacoma's roughly 200 Chinese residents -- men, women, and whole families rounded up and marched out of the city in an event that became known nationally as "the Tacoma Method" for its organized, non-violent-on-the-surface execution, and their homes were burned to the ground the following day. No Chinese residents returned to Tacoma until the 1920s. The City Council formally approved a Chinese Reconciliation Resolution on November 30, 1993, and the park itself -- sited near the location of the original Chinese settlement, known as "Little Canton" -- opened its first two phases in late 2010. This is real, documented civic history that any honest account of this waterfront has to include.

At the north end of Ruston Way sits Point Defiance Park, a 760-acre urban park founded in 1888 -- nearly 400 acres of it old-growth forest -- drawing more than three million visitors a year. It holds the Point Defiance Zoo & Aquarium (the zoo dating to 1905, the aquarium to 1935, together spanning 29 acres with more than 9,000 specimens across 367 species) and, distinct from any Seattle-area ferry route, the Point Defiance-Tahlequah ferry, a genuine Washington State Ferries route connecting this exact shoreline directly to Vashon Island. For a waterfront buyer here, that ferry access is a real, practical amenity, not a scenic backdrop.

Getting into Tacoma from the Kitsap Peninsula side means crossing the Tacoma Narrows Bridge -- and this page is written specifically from the Tacoma side of that crossing, distinct from any coverage of the bridge's western landing near Gig Harbor. The original span, nicknamed "Galloping Gertie," opened July 1, 1940 and collapsed in a windstorm just over four months later, on November 7, 1940 -- no human lives were lost, though a dog named Tubby died in the collapse -- and the failure fundamentally reshaped structural and aerodynamic bridge engineering worldwide. A replacement span opened October 14, 1950, and a second, parallel span opened in 2007 to double capacity; that second span's construction cost is repaid through tolling, with 2026 passenger-car tolls running $4.50 with a Good To Go transponder, $5.50 by cash or credit, or $6.50 pay-by-mail, charged only on trips heading into Tacoma. For anyone weighing a Tacoma waterfront purchase against a Gig Harbor or Kitsap Peninsula property, that toll is a real, recurring cost of any regular westbound-to-eastbound commute pattern -- confirm current rates directly at wsdot.wa.gov before assuming a fixed number holds.

Finally, be honest about what this page could not pin down with full confidence. No Old-Town-specific population figure separate from Tacoma's citywide 220,182 (2020 Census) was found. Old Town waterfront home price figures in the $750,000 to $1.3 million range, with view/waterfront properties reportedly exceeding $2 million, come from a single 2025 brokerage source and were not independently cross-verified against a second source the way this page's citywide figures were. And no parcel-specific liquefaction displacement figure, insurance premium, or exact soil-remediation status for any specific address near the former ASARCO site is stated here. Confirm all of these directly with a Tacoma-focused buyer's agent, the Pierce County Assessor-Treasurer, a Washington-licensed insurance agent, and the City of Tacoma's Planning and Development Services Department before making a purchase decision.

Property Tax
Pierce County reassesses annually at true and fair market value (unlike some counties' multi-year cycles). Combined rates cited around $10.50-$12.54 per $1,000 of assessed value depending on the exact Tacoma location and taxing district overlap; effective rate cited around 1.05%, per multiple 2025-2026 aggregator sources -- confirm the exact current rate for a specific parcel via the Pierce County Assessor-Treasurer's ATIP portal
Sales Tax
10.5% combined in Tacoma (6.5% Washington state + 4% Tacoma local), among the higher combined rates in the county; unincorporated Pierce County runs a lower minimum around 8.2%. No state income tax anywhere in Washington
Median Home Price
Citywide: roughly $465,000-$479,000 across 2025-2026 Redfin/Zillow snapshots. Old Town waterfront specifically: cited in the $750,000-$1.3 million range with view/waterfront properties reportedly exceeding $2 million, per a single 2025 source not independently cross-verified
Bridge Toll (Tacoma Narrows)
2026 passenger-car tolls: $4.50 with a Good To Go transponder, $5.50 cash/credit, $6.50 pay-by-mail -- charged only heading into Tacoma. A real, recurring cost for anyone commuting from the Kitsap Peninsula/Gig Harbor side

Independent research. No ads. No sponsored listings. Facts here are drawn from: the City of Tacoma's own website (tacoma.gov, cms.tacoma.gov) and Metro Parks Tacoma (parkstacoma.gov) for Point Defiance Park history and acreage, shoreline planning documents, and the Chinese Reconciliation Park; HistoryLink.org for Tacoma's founding history, Job Carr's 1865 cabin, Morton McCarver's 1868 platting of Tacoma City, Point Defiance Park's 1888 founding, and the ASARCO smokestack's 1993 demolition; Wikipedia and kids.kiddle.co (cross-checked against HistoryLink and Pierce County's own site) for Old Tacoma/Old Town's history, St. Peter's Church, and Slavonian Hall; movetotacoma.com and livingintacoma.org for Old Town's neighborhood boundaries and Job Carr Cabin Museum details; the Washington State Department of Ecology (ecology.wa.gov) for the Tacoma Smelter Plume's history, EPA soil-sampling scope, and the Thea Foss Waterway's Superfund cleanup timeline; the U.S. EPA (epa.gov) and Washington Department of Ecology's Making Waves blog for Point Ruston's redevelopment and the 2019 Dune Peninsula park opening; Wikipedia's Thea Foss Waterway and Port of Tacoma entries, the National Working Waterfront Network's Thea Foss case study, and Mithun's project page for Thea's Landing, cross-checked for the Foss Waterway Development Authority's 1996 formation and the 1998 development plan; the Chinese Reconciliation Project Foundation (crpftacoma.org) and tacomachinesepark.org for the 1885 expulsion's documented details ("the Tacoma Method") and the park's 1993 resolution and 2010 opening; WSDOT's own Tacoma Narrows Bridge history pages (wsdot.wa.gov/tnbhistory) for the 1940 Galloping Gertie collapse, the 1950 replacement span, and the 2007 second span; WSDOT's current tolling page for 2026 toll rates; PNSN.org, USGS publications on Pacific Northwest earthquake hazards, and Washington DNR's own liquefaction susceptibility mapping report for Central Puget Sound cities (including Tacoma) for seismic and liquefaction hazard information; the Washington Military Department and PNSN for the February 28, 2001 Nisqually earthquake's magnitude, damage estimate, and the Salmon Beach landslide; the U.S. Census Bureau (2020 Census) for Tacoma's citywide population; the Port of Tacoma's own site and Northwest Seaport Alliance materials for port acreage and container-traffic ranking; sale-tax.com, salestaxhandbook.com, and the Washington Department of Revenue for current sales tax rates; and Redfin, Zillow, and a single Old-Town-focused brokerage blog (caringrealestate.com) for home price figures, the latter explicitly flagged as a single, not independently cross-verified source. Facts not independently confirmed and not invented here include: a population figure for Old Town specifically, separate from citywide Tacoma; a second independent source for the $750,000-$1.3 million/$2 million+ Old Town waterfront price range; parcel-specific flood zones, liquefaction risk, or soil-remediation status near the former ASARCO site; and current insurance premiums specific to this waterfront. Confirm all current facts directly with the City of Tacoma, the Pierce County Assessor-Treasurer, a Washington-licensed insurance agent, and a Tacoma-focused buyer's agent before making a purchase, relocation, or investment decision. Nothing on this page is legal, tax, financial, engineering, or insurance advice.

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