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Large numbers of pioneer settlers began arriving in the Willamette Valley in the 1830s via the Oregon Trail, though life was originally centered in nearby Oregon City.
To the west of the Tualatin Mountains lies the Oregon Coast Range, and to the east lies the actively volcanic Cascade Range. Other bridges outside the downtown area include the Sellwood Bridge (built 2016) to the south; and the St.
Portland's access to the Pacific Ocean via the Willamette and the Columbia rivers, as well as its easy access to the agricultural Tualatin Valley via the "Great Plank Road" (the route of current-day U. Route 26), provided the pioneer city with an advantage over other nearby ports, and it grew very quickly.
Portland remained the major port in the Pacific Northwest for much of the 19th century, until the 1890s, when Seattle's deepwater harbor was connected to the rest of the mainland by rail, affording an inland route without the treacherous navigation of the Columbia River.
These massive floods occurred during the last ice age and filled the Willamette Valley with 300 to 400 feet (91 to 122 m) of water.
Before American pioneers began arriving in the 1800s, the land that eventually became Portland and surrounding Multnomah County was inhabited for many centuries by two bands of indigenous Chinook people— the Multnomah and the Clackamas peoples.
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The Willamette River, which flows north through downtown, serves as the natural boundary between east and west Portland.