North Cascades National Park map with three "must see" locations marked.
Bedrock and Surficial Geology: The area around Diablo Lake is characterized by a mix of metamorphic and granite rocks. The metamorphic rocks, primarily gneiss and schist, originated from sedimentary and volcanic materials that were subjected to high-pressure and high-temperature conditions during the Mesozoic era. Granite intrusions occurred later, adding to the geological diversity. Glacial activity during the Pleistocene sculpted the landscape, creating the U-shaped valleys and deepened basins now occupied by lakes.
Significance: Diablo Lake is notable for its striking turquoise color, resulting from glacial flour suspended in the water. The overlook provides beautiful panoramic views of the lake and surrounding peaks, showing the impact of glaciation and tectonic activity on the landscape. The area is a popular stop for tourists traveling along the North Cascades Highway, offering educational insights into the region's geological history.
Getting There: From Marblemount, Washington, drive east on the North Cascades Highway (WA-20) for about 20 miles. The Diablo Lake Overlook is a well-marked pullout on the north side of the highway. The overlook is wheelchair accessible and provides restrooms and picnic facilities. The area is generally accessible from late spring to early fall.
Diablo Lake and its unique turquoise color (Google images).
The view from Diablo Lake Overlook (Google images).
Mount Shuksan seen reflecting off Picture Lake (Google images).
Mount Shuksan's peak (Google images).
Bedrock and Surficial Geology: Mount Shuksan is renowned for its complex geology, primarily composed of metamorphic rocks from the Easton Terrane. These rocks include schist and phyllite, originally made from sedimentary and volcanic rocks, which later changed due to heat and pressure during the late Paleozoic era. The mountain has also been intruded by younger granite type rocks. Tectonic activity, including accretion and faulting, has significantly deformed these rocks, contributing to the rugged topography of the area.
Significance: Mount Shuksan serves as an example of the complex geological history of the North Cascades, showcasing the processes of terrane accretion and metamorphism. Its scenic appearance, featuring the combination of metamorphic and igneous rocks, makes it a popular subject for photographers and a destination for climbers and hikers. The mountain's diverse geology offers insights into the tectonic evolution of the region.
Getting There: From the town of Glacier, Washington, drive east on the Mount Baker Highway (WA-542) for around 23 miles to reach the Heather Meadows area. The trailhead for the Lake Ann Trail, which offers views of Mount Shuksan, is located here. The hike to Lake Ann is about 8 miles round trip with an elevation gain of approximately 1,900 feet, considered a moderate to strenuous hike. The trail is generally accessible from late July through October.
Bedrock and Surficial Geology: The peaks surrounding Washington Pass Overlook, like the Liberty Bell Mountain and the Early Winters Spires, are mostly composed of the Golden Horn Batholith, an intrusive igneous formation of true granite. This granite formed approximately 50 million years ago during the Eocene epoch from molten rock that cooled and solidified beneath the Earth's surface. The Golden Horn Batholith is notable for being one of the few true granite intrusions in the North Cascades.
Significance: Washington Pass Overlook offers panoramic views of the surrounding granite peaks, showcasing the region's unique geological features. The area is a popular destination for tourists and geology enthusiasts, providing informative signs that explain the geological history. The overlook is also a favored spot for photographers, especially during the autumn months when the surrounding trees turn a beautiful golden color.
Getting There: From Newhalem, Washington, drive east on the North Cascades Highway (WA-20) for around 42 miles to milepost 162. Turn left onto the signed overlook road. The trailhead for the Washington Pass Overlook is located here. The trail is a 0.3-mile loop, paved and wheelchair accessible, leading to viewpoints of Liberty Bell Mountain and Early Winters Spires. The area is generally accessible from late spring to early fall.
The view from Washington Pass Overlook (Google images).
The view from Washington Pass Overlook at sunset (Google images).