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Nolte State Park preserves a forest sanctuary surrounding Deep Lake, favored for swimming and picnicking on hot summer days. The lake’s attractively cool waters are due to its 76-foot depth and cold water coming into the lake from Deep Creek, with its headwaters in the 3,000-foot-high foothills of the Cascade Mountains.

The lake has no outlet, as outflow percolates through gravels left as meltwater outwash from the great Ice Age glaciers that filled the Puget Sound lowlands.

The Bay of Despond

Today’s Jarrell Cove State Park was covered by glacial ice during the most recent ice age. The fingerlike waterways of South Puget Sound including the inverted Y shape of Jarrell Cove and Pickering Passage outside its entrance were excavated by highly pressurized meltwater streams that developed as the thousands-of-feet-thick ice began to melt. The park’s namesake cove features deep waters and a tall tidal range. Low tides yield extensive muddy banks.

Lake Wenatchee owes its existence to giant glaciers that widened and deepened the headwaters of the Wenatchee River. Gravel and rock carried in the glacier was deposited at the glacier’s end, forming a moraine, a natural dam to impound the lake. Lake Wenatchee State Park is situated on that moraine.

“To know the land, one must feel it out inch by inch with the feet.” –Harvey Manning

A generous land donation and the hard work of community activists has ensured that Squak Mountain State Park will be an enduring piece of wilderness close to the homes of millions of urban residents.

Yakima Sportsman State Park owes its preservation and its distinctive name to the generosity of a group of waterfowl hunting enthusiasts who purchased lands in the Yakima River floodplain in the 1940s.

Folds, Floods, Meanders and Mines

The park is situated in a geographic area called the Yakima Fold Belt, an area of central Washington where tectonic compression of the layered Columbia River Basalt lava flows results in a series of parallel ridges that run perpendicular to the force of the stress—kind of like kicking a rug creates ridges in the fabric.

Cape Disappointment State Park spreads over the land north of the point where the Columbia River and the Pacific Ocean meet. The park includes three headlands of basalt rock cliffs: Cape Disappointment overlooking the river, North Head above the strand of Long Beach, and McKenzie Head, midway between the other two headlands. The basalt bedrock of these wave-pounded cliffs are ancient lava flows that erupted on the ocean floor. Encountering the cold ocean water, the lava quickly hardened into bulbous masses geologists call pillow lava.