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Battle Ground Lake

From Oregon Hikers Field Guide

Looking at the park from the west side of the lake (Steve Hart)
There are many fallen trees lining the shore (Steve Hart)

Description

Battle Ground Lake is the centerpiece of Battle Ground Lake State Park. The roughly circular lake is fed by springs and precipitation and has no inlet or outlet streams. The water level remains nearly the same year round.

The lake was created as a "maar" volcano. Magma rising to the surface came in contact with a large amount of underground water. The water was turned to steam and the resulting steam explosion blasted a hole. After the system became inactive and cooled, water from rain and underground springs filled the lake. The explosive nature of the original eruption left scattered boulders of lava in the area, rather than solid masses of basalt. Centuries of erosion and plant growth have covered most of the lava with soil, but there are still large boulders visible on the west shore of the lake. Battle Ground Lake is about 105,000 years old.

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Oregon Hikers Field Guide is built as a collaborative effort by its user community. While we make every effort to fact-check, information found here should be considered anecdotal. You should cross-check against other references before planning a hike. Trail routing and conditions are subject to change. Please contact us if you notice errors on this page.

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