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Cascadia

Cascadia is a bioregion and political movement for increased or complete regional autonomy in western North America, encompassing the watersheds of major rivers such as the Columbia and Fraser that drain into the Pacific Ocean through the temperate rainforest zone, primarily including the U.S. states of Washington and Oregon, the Canadian province of British Columbia, and portions of Idaho. The concept emerged in the 1970s and 1980s as part of bioregionalism, emphasizing ecological boundaries over political ones to promote sustainable living aligned with natural systems like mountain ranges, forests, and river basins. This framework has fostered a regional identity tied to environmental stewardship, with cultural symbols including the Douglas fir-inspired "Doug" flag and advocacy for decentralized governance. The Cascadia megaregion, centered on the urban corridor from Portland through Seattle to Vancouver, supports approximately 10 million residents and generates an economy valued at around $600 billion annually, driven by technology, trade, and natural resources. While the bioregional idea has influenced local environmental policies and cross-border cooperation, the associated independence movement, formalized in 2005, seeks political autonomy but remains marginal, with limited empirical support for secession amid strong economic integration with the U.S. and Canada. Proponents highlight potential benefits like tailored sustainability measures, yet critics note the movement's ties to radical activism, including affiliations with antifa-style protests, which have drawn scrutiny for prioritizing ideological disruption over pragmatic regionalism. Despite occasional media attention ranking it among speculative separatist efforts, no viable pathway to independence exists, as public sentiment favors federal ties and bioregionalism manifests more as cultural affinity than causal driver for political rupture.

Geography and Bioregion

Boundaries and Definition

The Cascadia bioregion is delineated by natural features such as watersheds draining into the Pacific Ocean through the North American temperate rainforest belt, encompassing diverse ecoregions shaped by the Cascade Range, coastal ecosystems, and inland plateaus rather than political borders. This bioregional framework, rooted in the bioregionalism movement, prioritizes ecological continuity over arbitrary human divisions like state or provincial lines, with boundaries typically following ridges, peaks, river basins, and ocean margins. Geographically, Cascadia extends approximately 2,500 miles along the Pacific coast from Cape Mendocino in northern California (around 40°N latitude) northward to the Copper River in southeastern Alaska (up to about 60°N), though core definitions often limit the northern extent to southern British Columbia or Haida Gwaii. Westward, it is bounded by the Pacific Ocean; eastward, by the Rocky Mountains or the Continental Divide, incorporating the Columbia River basin and high plateaus; and southward, variably including portions of Idaho, Montana, Nevada, Wyoming, Utah, and Alberta depending on watershed delineations. The region comprises 75 distinct ecoregions, reflecting a gradient from coastal rainforests and fjords to alpine meadows and volcanic highlands, with the Cascadia Subduction Zone influencing subsurface geology but not strictly defining surface bioregional limits. Definitions among bioregional advocates, such as those from the Cascadia Bioregion organization, emphasize this holistic scope to highlight shared environmental dynamics, including salmon runs, old-growth forests, and seismic influences, though precise inland extents can vary based on specific watershed mappings. The bioregion's total area is estimated at around 388,000 square miles in narrower interpretations focused on British Columbia, Washington, Oregon, and northern California, expanding to over 500,000 square miles when including peripheral watersheds in Idaho, Montana, and southern Alaska.

Physical Features

The Cascadia bioregion exhibits diverse topography shaped by tectonic activity and erosion, encompassing parallel north-south trending mountain ranges, broad river valleys, coastal lowlands, and inland plateaus across an area of approximately 535,000 square miles (1,385,000 km²). Its Pacific coastline extends over 2,500 miles, featuring rugged fjords, islands, and sandy beaches from northern California to southern Alaska, with the continental shelf sloping sharply into the ocean depths. Inland, the terrain rises abruptly to form the Coast Ranges and Olympic Mountains along the western margin, transitioning eastward to the higher Cascade Range, which acts as a climatic divide with wetter western slopes and drier eastern interiors. The Cascade Range dominates the region's central highlands, stretching more than 600 miles from British Columbia through Washington and Oregon into northern California, with volcanic peaks and ridges averaging 7,000 feet (2,100 m) in elevation in the northern sections. Prominent stratovolcanoes include Mount Rainier, rising to 14,410 feet (4,390 m) as the highest point in the bioregion, alongside Mount Hood at 11,249 feet (3,429 m) and Mount Shasta at 14,179 feet (4,322 m). These mountains, formed by subduction-related volcanism, feature glaciated summits, U-shaped valleys, and lava plateaus, while the eastern flank gives way to the Columbia Plateau, a vast expanse of basaltic uplands averaging 2,000–4,000 feet (600–1,200 m) in elevation, incised by canyons. Hydrologically, Cascadia is defined by extensive river systems draining toward the Pacific, with the Columbia River forming the backbone—a 1,243-mile (2,000 km) waterway whose watershed spans 258,000 square miles (668,000 km²), originating in the Canadian Rockies and carving the Columbia Gorge through the Cascades. Tributaries such as the Fraser River (850 miles or 1,370 km long, draining much of interior British Columbia) and Snake River contribute to fertile alluvial valleys like the Willamette and Puget Sound lowlands, where sediment deposition supports deep soils amid estuaries and tidal flats. These features, combined with geothermal hot springs and volcanic fields, underscore the region's dynamic physiography influenced by ongoing plate interactions.

Ecology and Biodiversity

The Cascadia bioregion encompasses diverse ecosystems, including coastal temperate rainforests, montane forests, riverine habitats, and marine environments, which collectively support exceptional biodiversity due to the region's mild, wet climate and topographic complexity. These systems feature old-growth conifers in rainforests that sequester vast amounts of carbon, with seven of the world's top ten carbon-absorbing forests located here. Annual salmon runs in rivers like the Columbia and Fraser provide nutrient subsidies that sustain terrestrial and aquatic food webs, linking marine, freshwater, and forest ecosystems. The bioregion qualifies as a global ecological hotspot owing to its relatively intact native habitats and high species richness across taxa. Temperate rainforests the coastal zones, characterized by towering old-growth such as Pseudotsuga menziesii (Douglas-fir) and Thuja plicata (western redcedar), alongside understories in epiphytes, ferns, and fungi. diversity includes over 40 in British Columbia portions alone, extending to dry , boreal, and alpine types inland. These habitats multi-taxa , including threatened like the northern spotted owl (Strix occidentalis caurina) and Pacific fisher (Pekania pennanti), which rely on structural for and . Reptilian diversity stands at 48 , complemented by hundreds of fungi and taxa that decomposition and symbiosis. Aquatic and marine realms amplify Cascadia's biodiversity, with kelp forests and coastal wetlands supporting vibrant invertebrate communities and sediment carbon storage. River systems teem with anadromous salmonids, such as Chinook salmon (Oncorhynchus tshawytscha), whose migrations deliver marine-derived nutrients to riparian zones, enhancing riparian tree growth and invertebrate productivity. Offshore waters harbor cetaceans like orcas (Orcinus orca) and gray whales (Eschrichtius robustus), alongside seabirds including tufted puffins (Lunda cirrhata). Overall, the bioregion sustains over 350 bird and mammal species, thousands of invertebrates, and soil organisms, underscoring interconnected trophic dynamics.

Geology and Seismic Activity

The Cascadia Subduction Zone

The (CSZ) is a convergent plate extending approximately ,000 kilometers along the , from northern in to Cape Mendocino in northern California. At this margin, fragments of the ancient —primarily the , along with the smaller Explorer and Gorda plates— eastward beneath the overriding . The is shallow, with the descending at a low dip, facilitating the formation of a megathrust fault interface that spans the zone's length. Subduction mechanics in the CSZ involve the denser of the (typically 5–10 million years old) being forced beneath the continental crust due to plate motion driven by slab pull and forces. This generates an of deformed sediments scraped from the subducting plate, which accumulates along the , and contributes to the of the where the slab reaches depths of about 100 kilometers, and producing . The shallow portion of the megathrust, extending to depths of roughly 15–30 kilometers, is largely locked, accumulating from the relative plate , while deeper sections exhibit aseismic slip. , occurring at 20–40 kilometer depths below the locked , periodically release some stress without generating significant earthquakes. Geophysical , including seismic profiles and GPS measurements, indicate near-full on the shallow megathrust in the central CSZ, implying high seismic potential from buildup, though the of locking varies along-strike to upper-plate heterogeneity and slab fragmentation. Recent subsurface has refined understanding of fault , revealing how the young, fragments within the seismogenic , influencing rupture . The zone's , compiled in of paleoseismic, geophysical, and tectonic datasets, underscores its as a for studying subduction hazards, with marine geohazards like landslides adding complexity to the tectonic regime.

Historical Earthquakes and Tsunamis

The most recent great along the occurred on , , at approximately 9:00 , with an estimated of 9.0. This megathrust ruptured over ,000 kilometers of the fault, from northern to northern , causing widespread coastal of to in and . The earthquake generated a massive tsunami with run-up heights exceeding 10 along parts of the and coasts, evidenced by eroded bluffs, buried soils, and sheets overlying Native village sites. This tsunami propagated , striking Japan's eastern coast on , 1700 (local time), with up to 3-5 high and no local earthquake precursor, as recorded in historical Japanese documents. Oral histories from groups, such as the and , describe the event as causing the land to "rise and fall" for hours, followed by flooding that destroyed villages and canoes. Paleoseismic evidence from tree-ring dating of "ghost forests" (killed by sudden subsidence and saltwater intrusion), coastal marsh stratigraphy, and offshore turbidite deposits indicates at least 19 great earthquakes (magnitude ~8-9) along Cascadia in the past 10,000 years, with recurrence intervals averaging 300-600 years. Prior events include ruptures around 7,000 years ago and clusters in the late Holocene, such as circa 1300-1500 CE, inferred from synchronized turbidite layers and onshore subsidence records spanning northern and southern segments. Tsunami signatures from these events, including boulder deposits and inlet infilling, show run-ups of 5-15 meters, highlighting recurring coastal inundation risks.

Current Risks and Recent Developments

The poses a significant of a exceeding 9.0, capable of generating tsunamis up to high and causing widespread that could coastal areas by several feet. Geological indicate recurrence intervals of 300 to 500 years, with the last major event occurring on January 26, 1700, placing the region overdue by over three centuries. Scientific estimates assess a 37% probability of a 7.1 or greater event within the next 50 years, with potential fatalities exceeding 14,000 in and Washington alone from shaking, liquefaction, and inundation. Recent paleoseismic and modeling studies highlight compounded threats, including post-event sea-level rise exacerbating permanent coastal reconfiguration through and erosion. Emerging research in 2025 has identified potential synchronization between Cascadia and the San Andreas Fault, where a Cascadia rupture could trigger a subsequent magnitude 7.8+ event on the San Andreas within hours to days, based on historical stratigraphic evidence of correlated turbidite deposits spanning 30 years of data recovery. Seismicity in the zone remains low, with no major events recorded in 2024 or 2025; the Pacific Northwest Seismic Network cataloged hundreds of minor quakes (magnitudes up to 4.0), primarily crustal, alongside aftershocks from a December 2024 magnitude 7.0 event near the southern Mendocino Triple Junction. Advancements in include expansions of the for seconds-scale warnings and ongoing USGS efforts in tectonic detection to forecast slow-slip preceding ruptures. initiatives intensified in , with issuing an on mandating seismic retrofits for and the USGS hosting a Meeting in to refine models. Commemorations of the 325th anniversary of the 1700 quake, including public drills and documentaries, underscore regional emphasis on resilience planning amid static probability assessments.

Independence and Autonomy Movements

Origins and Historical Context

The concept of Cascadia as a distinct political entity traces its earliest roots to the early 19th century, when American and British interests vied for control of the Oregon Country (encompassing present-day Washington, Oregon, Idaho, parts of Montana, and British Columbia). In 1811, fur trader John Jacob Astor established Fort Astoria as a foothold for what he envisioned as an independent Pacific empire, a notion echoed in post-War of 1812 discussions by U.S. Secretary of State John Quincy Adams regarding an "empire of Astoria" free from European dominance. These proposals reflected geographic isolation and economic ambitions but dissolved amid U.S.-British treaties and settlement pressures, with no sustained independence effort materializing. Mid-19th-century sentiments resurfaced during the amid sectional tensions preceding the , as some advocated a "Pacific Republic" to avoid entanglement in eastern conflicts, peaking under Whig administration uncertainties. However, loyalty to the prevailed, and the idea faded post-1860s with statehood for (1859) and Washington Territory's . These episodic autonomy calls highlighted the region's peripheral relative to eastern centers, fostering a latent regional identity tied to natural resources and distance from national capitals. The Cascadia emerged in the late through , a philosophy prioritizing ecological boundaries over artificial political , gaining traction amid 1970s . Callenbach's 1975 Ecotopia popularized of a seceded, sustainable Northwest , influencing cultural . In 1981, McCloskey coined "Cascadia" to describe the defined by the , Salish Sea, and shared watersheds, formalizing it at the 1986 Cascadia Bioregional Congress at The Evergreen State College. This era emphasized grassroots sustainability and Indigenous perspectives over separatism, though it laid groundwork for autonomy by critiquing centralized governance's misalignment with local ecosystems. Explicit independence advocacy crystallized in the 2000s, with activist Brandon Letsinger founding CascadiaNow! in 2005 as the Cascadia Independence Project to promote bioregional sovereignty through education and referenda. Building on bioregional congresses and cultural symbols like the Doug flag (designed in the 1990s), the movement framed secession as a means to achieve decentralized democracy, environmental stewardship, and cross-border unity, distinct from earlier economic-driven proposals. By 2014, CascadiaNow! incorporated as a nonprofit, marking institutionalization amid broader North American secession discussions.

Ideology, Symbols, and Organizations

The ideology of the Cascadian independence movement is rooted in bioregionalism, a philosophy that defines human societies and activities in relation to natural ecosystems, emphasizing local knowledge, cultural ties to place, and sustainable practices over imposed political boundaries. Advocates argue that aligning governance with the Cascadia bioregion—encompassing watersheds, forests, and geological features—enables better stewardship of resources, such as addressing shared environmental challenges like salmon runs and old-growth forests, which span state and national lines. This approach prioritizes decentralization, community empowerment, and democratic processes to foster ethical, resilient local economies, often critiquing centralized federal policies for neglecting regional specifics. While some early groups framed Cascadia as ideologically , the broadly rejects rigid left-right spectra, instead promoting based on bioregional , borders, and practical without ethnic or cultural mandates. proponents a through voluntary, democratic means, potentially forming an autonomous focused on environmental , systems, and reduced reliance on distant , though such goals remain aspirational amid low . The chief symbol of Cascadia is the Doug Flag, an unofficial banner designed in 1994 by Alexander Baretich, consisting of three horizontal stripes—blue for skies, waters, and rivers; white for clouds and snow-capped mountains; and green for forests—with a central black silhouette of a Douglas fir tree denoting resilience and the bioregion's coniferous dominance. This flag, often displayed at regional events and on apparel, encapsulates bioregional ethos by evoking the landscape's elemental features rather than political heraldry, and has gained informal recognition in Pacific Northwest subcultures since the 1990s. Prominent organizations advancing Cascadian include CascadiaNow!, a supporter-driven group established to raise bioregional through , , and projects linking ecological, economic, and cultural across the . The Cascadia of Bioregion organizes assemblies and initiatives for neighborhood-level , aiming to build sustainable models via participation and ethical . Cascadia supports through publications, , and the Cascadian , which outlines democratic pathways to bioregional while disparate groups. These entities, often volunteer-led and grant-funded, collaborate on like bioregional congresses but operate as loose networks without centralized authority, reflecting the movement's decentralized principles.

Support, Polling, and Viability

Support for Cascadian independence remains marginal, with no large-scale, representative polls specifically public opinion on forming a spanning , , , and adjacent areas. A of -level indicated that 23% of their seceding from the , while 51% opposed it outright. In , a 2020 survey found 27% favoring provincial from Canada, with rising to higher levels among younger demographics (18-34 years old), though this pertains to BC alone rather than a cross-border Cascadia. Broader regional secession sentiment, as captured in a 2021 University of Virginia poll, showed elevated interest among West Coast Democrats for dividing the U.S. into regional entities, but overall figures hovered below 50% and did not address Cascadia explicitly. Advocacy groups within the , such as the Cascadia of , cite a 2018 Zogby survey showing 39% U.S. for and 68% to the idea; however, this poll addressed or regional rather than Cascadia, and regional breakdowns indicated Pacific states at around 40-50% without to . Internal surveys, like the 2020 of Cascadia , reported 95% of respondents favoring a referendum on independence, but these drew from self-identified supporters and lack methodological transparency or random sampling, rendering them unrepresentative of the broader population. Viability assessments highlight formidable barriers, including U.S. precedent in (1869) deeming unilateral unconstitutional without , which applies to any Cascadian effort involving American states. Canadian constitutional requirements for provincial separation, as outlined in the (2000), demand clear referenda and negotiations, further complicated by Quebec precedents showing low odds without overwhelming . Economic analyses underscore interdependence: the proposed Cascadia's GDP, estimated at around $1.5 if including California peripherally, relies heavily on , , and , with risking disruptions under NAFTA/USMCA frameworks. Political momentum is constrained by the movement's niche status, with no endorsements and urban-rural divides in the mirroring rather than coalescing around bioregional . observers, including reviews, characterize full as improbable absent catastrophic , positioning Cascadia more as a cultural or cooperative framework than a feasible polity.

Criticisms and Practical Challenges

The Cascadia independence movement faces substantial legal obstacles, as unilateral secession from the United States violates the Constitution according to the Supreme Court's ruling in Texas v. White (1869), which held that the Union is perpetual and states cannot withdraw without consent from other states. In Canada, the Clarity Act of 2000 requires a clear referendum question and substantial majority for negotiations, a threshold unmet in regional polls and complicated by federal opposition to territorial fragmentation. These barriers render full independence improbable absent extraordinary circumstances like national dissolution, as historical precedents such as the American Civil War demonstrate the coercive response to secession attempts. Economic viability poses further challenges, given the region's deep integration into North American supply chains, with ports in , , and handling over $200 billion in annual trade reliant on U.S. and Canadian infrastructure and markets. Independence would necessitate establishing a new , regime, and apparatus, potentially disrupting tech sectors in (e.g., , contributing ~15% of Washington's GDP) and resource extraction in British Columbia, while federal transfers and protection underpin current stability. Critics note that the bioregion's economy, generating ~$1.5 trillion combined GDP across proposed territories, thrives on cross-border ties rather than isolation, risking capital flight and recession akin to post-secession struggles in regions like Catalonia. Internal political fragmentation undermines , with stark urban-rural divides: coastal areas with conservative eastern Washington and Oregon, where movements to join reflect opposition to Cascadian and policies. This disunity, evidenced by failed local secession bids like Greater Idaho (garnering ~10-20% in rural counties as of 2020), could spawn counter-secessions, diluting any unified front. Ideologically, detractors contend the movement deviates from bioregionalism's ecological focus toward nationalism, manifesting in flags, anthems, and cultural revival efforts like Chinook Jargon that foster exclusionary identity rather than resource-based interdependence. Such tendencies risk attracting authoritarian elements, contradicting the movement's anti-statist roots, while low mainstream support—hovering below 25% in broader Pacific Northwest secession polls—highlights its fringe status amid competing regional loyalties. Proponents' pivot to "autonomy" over outright independence sidesteps some hurdles but evades rigorous feasibility testing, positioning Cascadia more as aspirational rhetoric than actionable policy.

Culture and Identity

Bioregionalism and Environmentalism

The Cascadia bioregion represents a foundational in , delineating a geographic area aligned with watersheds, ecoregions, and ecosystems rather than political borders. This typically spans the , incorporating the watersheds of such as the , Fraser, and Klamath, extending from southeastern southward to Cape Mendocino in and eastward along the . , as applied here, promotes human adaptation to local environmental limits through practices like permaculture, watershed stewardship, and decentralized economies that prioritize ecological carrying capacity over industrial expansion. The philosophy originated in collaborations between thinkers like Peter Berg and Raymond Dasmann in the mid-1970s, influencing Cascadian applications by emphasizing "reinhabitation"—reconnecting communities to their biotic communities. In Cascadia, intertwined with during the 1970s and 1980s, emerging from broader against , , and in temperate rainforests. The term "Cascadia" was coined in 1981 by Seattle University professor David McCloskey to a shared regional rooted in natural features like the and routes. This gained at the First Cascadia in July 1986, where over 100 ecologically minded participants at The Evergreen State College discussed bioregional mapping, sustainable forestry, and opposition to transboundary pollution from sources like U.S. and Canadian industrial effluents. Environmental within Cascadian has focused on preserving old-growth forests, restoring habitats, and advocating for transitions, often critiquing policies that prioritize over . Organizations like the Cascadia of promote initiatives such as and councils to foster and reduce carbon footprints tied to long-distance . These efforts align with bioregional trends but emphasize Cascadia's temperate , where exceeds inches in coastal zones, supporting keystone like the and populations. Proponents argue that bioregional could mitigate risks from seismic activity and climate-driven wildfires by decentralizing to those with ecological stakes. In sports, the represents a prominent expression of bioregional through among clubs from the core Cascadia cities: the , , and . Initiated in by fan groups including the , Supporters, and Vancouver Southsiders, the cup awards points based on results from interclub , with the highest-scoring claiming the annually. captured the 2025 edition on September 27, marking their record eighth and highlighting the rivalry's , which draws tens of thousands of attendees to matches and features elaborate tifos—large choreographed banners—depicting Cascadian symbols like the Douglas fir tree. Complementary events include the Cascadia Dirt Cup, a mountain biking series emphasizing the bioregion's trails and outdoor ethos. Music tied to Cascadia often reflects its environmental and bioregional themes. Cascadian black metal, originating in the Olympia, Washington scene around the early 2000s, integrates motifs of , , and anti-urbanism, with bands such as pioneering atmospheric soundscapes inspired by the Pacific Northwest's landscapes; the genre's name explicitly nods to the . Vancouver indie rock group released the Cascadia in 2011, incorporating regional references to , , and local . Folk traditions include "Cascadia the ," a song by Littlebear and the Fostervillagers evoking autonomy and natural harmony. Additionally, "O'Cascadia" served as the anthem for the 2018 CONIFA World Football Cup, blending folk elements with calls for bioregional solidarity. In media and literature, Cascadia influences narratives centered on ecology, autonomy, and seismic risks. Ernest Callenbach's 1975 novel Ecotopia depicts a seceded state prioritizing steady-state economics and environmental restoration, providing a foundational utopian vision that shaped bioregionalist discourse. H.W. "Buzz" Bernard's 2016 thriller Cascadia simulates a magnitude 9.0 earthquake along the subduction zone, underscoring regional vulnerabilities based on geological data. Documentaries like Occupied Cascadia (2012) examine Indigenous decolonization efforts across the bioregion. The Cascadia International Women's Film Festival, based in Bellingham, Washington, has screened region-specific works since 2016, including those by Indigenous filmmakers, and marked its 10th anniversary with expanded programming in 2026. Local critics, via the Cascadian Film and Television Critics Association founded in 2022, analyze productions, reinforcing cultural self-awareness.

Places and Other Uses

Named Locations

Cascadia is an unincorporated community in , situated along the Santiam River at the with Soda Creek. The community originated as a in 1890, deriving its name from the nearby , and developed around natural springs that attracted early visitors for their purported benefits. Adjacent to the community lies Cascadia County Park (formerly Cascadia State Park), a recreational area spanning 38 acres along the South Santiam River, offering camping, picnicking, fishing, and access to hiking trails leading to Soda Creek Falls, a 90-foot waterfall. The park's infrastructure includes a historic covered bridge built in 1955, riverfront day-use areas, and group camping facilities, with its history tied to a 19th-century resort era centered on the mineral springs. Management transferred from state to county oversight in the late 20th century to preserve local access amid budget constraints. No other prominent geographic locations bear the name Cascadia, though the term occasionally appears in informal or branded contexts unrelated to permanent settlements, such as temporary event sites or fictional mappings.

Organizations, Brands, and Media

The Cascadia Department of Bioregion is a 501(c)(3) nonprofit organization established to promote bioregional awareness and sustainability in the Pacific Northwest, maintaining a directory of affiliated groups and initiatives focused on ecological and cultural ties across the region. Similarly, Cascadia Wildlands, founded in the 1990s from forest defense efforts, operates as a conservation group advocating for old-growth forest protection through legal, grassroots, and policy actions in Oregon, Washington, and surrounding areas. Cascadia Research Collective, incorporated in 1979, conducts marine mammal studies primarily funded by government grants, contributing data on cetacean populations off the U.S. West Coast. Other entities include the Cascadia Association Football Federation (CAFF), which organizes soccer and promotes regional through , and CascadiaNow!, a stewardship-focused group supporting bioregional projects like climate and habitat since the 2000s. Cascadia Community College, opened in in Bothell, Washington, serves local students with programs in , , and , drawing its name from the surrounding bioregion. In media, Cascadia Daily News, launched in 2021 as an outlet in , covers , , and in Whatcom and Skagit counties via and weekly print editions, emphasizing outside traditional paywalls for elections. Cascadia Times focuses on spanning , , , and adjacent states, highlighting bioregional issues like threats and responses. Brands named Cascadia are less centralized but include niche products tied to regional themes; for instance, Cascadia-themed merchandise such as maps, posters, and apparel is distributed through bioregional outlets to foster and sustainability . Organizational directories also initiatives like Cascadia , which promotes local , though commercial remain fragmented without a dominant .

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