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Tiger Mountain

What is it and why visit?

Waterfall on Fifteenmile Creek
Waterfall on Fifteenmile Creek
Photo by Rachel Noonan, WGS/DNR

You don’t need to venture deep into the Cascades for great vistas—the view from the top of Tiger Mountain is spectacular. On a clear day, visitors can gaze out over a broad valley of lush green trees and distant lakes stretching to the edges of Redmond, Seattle, and the Olympic Mountains. This serene peak stands tall at an elevation of more than 3,000 feet, dominating the nearby landscape while humbly nodding at Mount Rainier to the south. With extensive, accessible trails and an active tectonic story, this forest playground on the edge of urban bustle is a good place for visitors to enjoy both geology and great views. The forest, which covers more than 18,000 acres of land managed by the Department of Natural Resources, even has a popular paragliding ledge at Poo Poo Point. Take to the skies on your next visit and float among the broad vistas of Issaquah and Bellevue.

Paragliders take off from Poo Poo Point
Paragliders take off from Poo Poo Point
DNR

Geologic story

Mossy boulder along Master Link trail on East Tiger Mountain
Mossy boulder along Master Link trail on East Tiger Mountain
Photo by David Balderrama
As the faults lift up the land, the rocks of Tiger Mountain have been exposed to erosion by wind and rain

Before faults deformed the area, Tiger Mountain was a low-lying wetland where rivers met the sea. It was coastal real estate more than 40 million years too early for the Northwest boom. Layers of sand, silt, and clay containing fossils of sea creatures document the gradual retreat of the ancient seashore. As the water drew back, deep marine environments gave way to shallow deltas, rivers, and swamps, leaving behind loose sediments and muds. Around the same time, an ancient volcano near modern-day Issaquah erupted explosively, spreading volcanic rocks across Tiger Mountain. Lahars—massive floods of volcanic mud—periodically inundated these ancient swamp river valleys.

Snowy bridge on Master Link trail cuts through dense forest
Snowy bridge on Master Link trail cuts through dense forest
Photo by Maria Furtney, WGS/DNR

Tiger Mountain State Forest is bound by two large fault zones. A broad swath of several faults comprises the Seattle Fault Zone, which extends from Issaquah, through Seattle, west to Bainbridge Island, and all the way to Hood Canal. The neighboring Rattlesnake Mountain fault zone runs north–northwest through the area. Movement along these faults is compressing and squishing the rocks between them, pushing up the “Issaquah Alps”. Tiger Mountain is the center of these miniature “alps.”

Tiger Mountain (West and East) and the Issaquah Alps are bound by the Seattle fault zone and the Rattlesnake Mountain fault zone
Tiger Mountain (West and East) and the Issaquah Alps are bound by the Seattle fault zone and the Rattlesnake Mountain fault zone
WGS/DNR

As the faults lift up the land, the rocks of Tiger Mountain have been exposed to erosion by wind and rain. The loose swamp sediments were easily removed by these forces, leaving behind the resistant volcanic rocks and sandstones that form the backbone of the mountain. Great ice sheets advanced and retreated during the ice age, leaving a blanket of gravelly deposits in the valleys of Tiger Mountain State Forest.

Paragliding into the valley from Poo Poo Point, West Tiger Mountain—Lake Sammamish in the distance
Paragliding into the valley from Poo Poo Point, West Tiger Mountain—Lake Sammamish in the distance
DNR

In the late 19th century, prospectors dug coal mines on Tiger Mountain as part of the mining boom that fed the growth of Issaquah and Newcastle. Coal from Tiger Mountain fueled railways on the mountain that transported timber to market. The Iverson Railroad Trail is an example of one of these timber railroad grades.

Fun Fact

Scientists and collectors have found amber alongside the coal deposits on Tiger Mountain. These gemstones form when buried ancient tree resin is heated and pressurized by the Earth. They contain not only insect fossils but also microfossils of ancient bacteria.

What to see and do

Getting There

For West Tiger Highpoint trailhead, take Interstate 90 to exit 20. Trailheads are along SE 79th Street, including Cable Line trailhead and Highpoint trailhead.

For West Tiger Poo Poo Point trailhead, take Issaquah-Hobart Road SE (Front Street S in Issaquah) 2.3 miles south of downtown Issaquah (Sunset Way and Front Street) to Poo Poo Point trailhead parking lot, adjacent to the east side of the road.

For East Tiger Summit trailhead, take State Route 18 to Tiger Summit trailhead; watch your speed on this busy section of highway for the turnoff to the East Tiger Mountain Summit parking lot; access to multiple trails.

Nearby Amenities

Photo gallery

Bibliography

Brocher, T. M.; Blakely, R. J.; Wells, R. E., 2004, Interpretation of the Seattle Uplift, Washington, as a Passive-Roof Duplex: Bulletin of the Seismological Society of America, v. 94, no. 4, p. 1379–1401. [https://doi.org/10.1785/012003190]

Brownfield, M. E.; Affolter, R. H.; Cathcart, J. D.; Johnson, S. Y.; Brownfield, I. K.; Rice, C. A., 2005, Geologic setting and characterization of coals and the modes of occurrence of selected elements from the Franklin coal zone, Puget Group, John Henry No. 1 mine, King County, Washington, USA: International Journal of Coal Geology, v. 63, no. 3–4, p. 247–275. [https://doi.org/10.1016/j.coal.2005.03.021]

Dragovich, J. D.; Anderson, M. L.; Walsh, T. J.; Johnson, B. L.; Adams, T. L., 2007, Geologic map of the Fall City 7.5-minute quadrangle, King County, Washington: Washington Division of Geology and Earth Resources Geologic Map GM-67, 1 sheet, scale 1:24,000, with 16 p. text.

Evans, G. W., 1924, Coal-mining problems in the State of Washington: Bureau of Mines Bulletin, v. 190, 79 p.

Johnson, S. Y.; Blakely, R. J.; Brocher, T. M.; Haller, K. M.; Barnett, E. A.; Bucknam, R. C.; Haeussler, P. J.; Pratt, T. L.; Nelson, A. R.; Sherrod, B. L.; Wells, R. E.; Lidke, D. J.; Harding, D. J.; Kelsey, H. M., compilers, 2016, Fault number 570, Seattle Fault zone: Quaternary fault and fold database of the United States. [https://earthquake.usgs.gov/hazards/qfaults/].

Liberty, L. M.; Pratt, T. L., 2008, Structure of the eastern Seattle Fault zone, Washington State: new insights from seismic reflection data: Bulletin of the Seismological Society of America, v. 98, no. 4, p. 1681–1695. [https://doi.org/10.1785/0120070145]

Mullineaux, D. R., 1970, Geology of the Renton, Auburn, and Black Diamond quadrangles, King County, Washington: U.S. Geological Survey Professional Paper 672, 97 p.

Mustoe, G. E., 1985, Eocene amber from the Pacific coast of North America: Geological Society of America Bulletin, v. 96, no. 12, p. 1530–1536. [https://doi.org/10.1130/0016-7606(1985)96<1530:EAFTPC>2.0.CO;2]

Vine, J. D., 1969, Geology and coal resources of the Cumberland, Hobart, and Maple Valley quadrangles, King County, Washington: U.S. Geological Survey Professional Paper 624, 67 p., 4 plates.

Waggoner, B., 1993, Fossil actinomycetes and other bacteria in Eocene amber from Washington State, USA: Tertiary Research, v. 14, no. 4, p. 155–160.

Walsh, Timothy, 1990, Geologic history of the Tiger Mountain State Forest. In Washington Division of Geology and Earth Resources, Washington Geologic Newsletter: Washington Division of Geology and Earth Resources, v. 18, no. 1, p. 35–36. [https://www.dnr.wa.gov/Publications/ger_washington_geology_1990_v18_no1.pdf]