-
Mount Rainier
This
silent, snowcapped sentinel, the centerpiece of Mount Rainier National
Park, is an awe-inspiring active volcano rising 14,410-ft (4,392-m)
above sea level. Since the cataclysmic explosion of Mount St. Helens in
1980, the Grand Dame of the Cascades commands new respect for its
potentially devastating force.

View of Mount Rainier

Hikers at Paradise, Mount Rainier
-
Issaquah Alps
This
series of foothills west of the Cascades are remnants of mountains that
predate the higher and more visited peaks to the east. Cougar, Squak,
Tiger, and Rattlesnake Mountains are four main park areas that attract
individuals and families seeking woodland walks without steep drops or
high altitude. -
Snoqualmie Falls
Local
Native American tribes regarded Snoqualmie Falls as a sacred place. The
276-ft (84-m) waterfall, beautifully divided in two sections by a
convenient rock outcropping, marks the end of the Cascade Plateau, where
the Snoqualmie River begins its final descent to the sea. An
observation deck and a steep path to the river allow for close-up
breathtaking views.

Snoqualmie Falls
-
Twin Falls
Hikers
wanting a short spell of deep woods and water head to Olallie State
Park, where a 3-mile (5-km) trail to Twin Falls awaits. The park’s
amazing plant life includes giant ferns and salmonberry, and some of the
Cascades’ few old-growth trees. One Douglas fir has a circumference of
14 ft (4 m). -
Staircase Rapids
The
ferry crossing and subsequent scenic drive along the Hood Canal enhance
the journey to these rapids. The popular route inches near the
fast-flowing Skokomish River as it pours down the eastern slopes of the
Olympic Range on its way to Lake Cushman. Look out for kingfishers,
harlequin ducks, and giant salamanders on the 2-mile (3-km) loop. -
Big Four Ice Caves
Global
warming has taken a toll on ice caves, but the attraction at the base
of 6,153-ft (1,875-m) Big Four Mountain in the North Cascades is still
vital. Hike the 1-mile (1.6-km) trail off the Mountain Loop Highway to
the Ice Caves, the unusual result of alpine avalanches and climate
conditions impacting the ice field at the mountain’s base.