description The Phoenix Overview
Near Cascade Falls in Yosemite Valley, California, The Phoenix follows a short but demanding granite crack. Ray Jardine made its first free ascent in 1977, and the route is commonly graded 5.13a. Its place in the development of hard American free climbing comes from the difficulty of climbing the line without using equipment to assist upward movement, rather than from the length of the route. A steep, continuous finger crack requires precise jams and careful foot placement while placing sustained demands on strength.
It suits experienced crack climbers already comfortable with difficult granite and the protection practices of traditional climbing. The compact line concentrates its challenge instead of spreading it across a long ascent. Despite the Joshua Tree tag supplied with the item, this particular route belongs to Yosemite.
help The Phoenix FAQ
Where is the famous climbing route called The Phoenix?
The historically important Phoenix is a crack climb in Yosemite Valley, California, not a Smith Rock sport route. It is located near Cascade Creek and is known for steep, technically demanding jamming.
Why is The Phoenix important in climbing history?
Ray Jardine made the first free ascent in 1977, and the climb became widely recognized as an early benchmark at 5.13a. It helped demonstrate how far specialized crack technique and training were pushing free climbing.
What type of climbing does The Phoenix require?
The crux is a steep, thin crack that demands precise finger locks, powerful movement, and effective footwork. Protection is placed with traditional gear rather than preinstalled sport-climbing bolts.
How does The Phoenix differ from Smith Rock's early sport routes?
The Phoenix is a Yosemite crack protected with removable gear. Smith Rock became central to American sport-climbing history through bolted face routes such as Chain Reaction and later To Bolt or Not to Be.
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