Indianola, Miller Bay

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Indianola, Miller Bay

by | Oct 13, 2023

Indianola lies on the eastern shore of the Kitsap Peninsula and the north shore of Port Madison, about 13 miles (21 km) northwest of Seattle and six miles (10 km) east of Poulsbo, Washington. This part of the peninsula lies between Puget Sound to the east and Hood Canal to the west. A gravel spit partially encloses Miller Bay, just west of Indianola, which divides the Port Madison Indian Reservation into two parcels. The towns of Suquamish and Indianola both lie within its bounds. The landscape is glacial. Sand and gravel left by meltwater as the Puget lobe of the Fraser glaciation retreated now blanket the area, part of the Everson and Vashon drifts. The ice reached the site of present-day Seattle about 18,000 years ago, was roughly 3,300 feet (1,000 m) thick, and had retreated north of there by about 16,000 years ago. As it withdrew, seawater flooded the Puget Lowland, beginning the Everson Interstade. The interstade ended when rebound of the crust, freed from the ice’s weight, outpaced sea-level rise and the land emerged.

Humans had reached western Washington by about 13,800 years ago, and the ancestors of the Suquamish Tribe have lived around Puget Sound for at least 10,000 years. Their ancestral language is southern Lushootseed. The Treaty of Point Elliott of 1855 authorized the Port Madison Indian Reservation, and some Coast Salish neighbors, including the Duwamish and Sammamish, also moved there. The reservation’s 7,657 acres (3,099 ha) were meant for tribal members alone, but allotment and sales to non-Natives eroded that. The land under Indianola was allotted to KaKue of the Suquamish in 1886 and passed through his heirs. In 1916 the Indianola Beach Land Company began selling lots, and the community was established as a summer retreat, with a dock and store to lure buyers. The Mosquito Fleet of small steamers carried most traffic on Puget Sound. A steamer called at Indianola every weekend by 1918, and by 1929 three boats a day left for Seattle. A road finally linked Indianola to Suquamish in 1939.

Economic development since the early 1990s has let the Suquamish Tribe buy back allotment-era land, and the tribe and its members now own roughly 57% of the reservation, though Indianola’s 3,664 residents (in 2020) are mostly non-Native. Salmon still struggle: culverts and old pond dams block fish passage on Grovers Creek, which feeds Miller Bay and shelters threatened steelhead. The tribe’s Merle Hayes Salmon Enhancement Center, operating on the creek since the early 1980s, releases about 500,000 Chinook and 250,000 chum a year. Watershed conservation by the Great Peninsula Conservancy and partners has protected the 329-acre (133 ha) Grovers Creek Preserve, much of it bought from Pope Resources (since acquired by Rayonier) and from private families. It belongs to a wider effort to conserve 4,000 acres (1,619 ha) between Kingston and Port Gamble. The preserve and the adjacent North Kitsap Heritage Park sit at the center of a forest corridor of nearly 1,700 acres (688 ha). Read more here and here. Explore more of Indianola and Miller Bay here:

About the background graphic

This ‘warming stripe’ graphic is a visual representation of the change in global temperature from 1850 (top) to 2022 (bottom). Each stripe represents the average global temperature for one year. The average temperature from 1971-2000 is set as the boundary between blue and red. The color scale goes from -0.7°C to +0.7°C. The data are from the UK Met Office HadCRUT4.6 dataset. 

Credit: Professor Ed Hawkins (University of Reading). Click here for more information about the #warmingstripes.

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