This geographical feature's descriptive name has been officially adopted by the U.S. Board on Geographic Names.[2] The 1889–90 Seattle Press Expedition originally named it the "Holmes Range".[3] The expedition, led by James Halbold Christie and Charles Adams Barnes, had also christened Mount Deception as "Mount Holmes", in honor of John H. Holmes of the Boston Herald.
Climate
Based on the Köppen climate classification, the Needles range is located in the marine west coast climate zone of western North America.[4] Most weather fronts originate in the Pacific Ocean, and travel east toward the Olympic Peninsula. As fronts approach, they are forced upward by the peaks, causing moisture to drop in the form of rain or snowfall (Orographic lift). As a result, the range experiences high precipitation, especially during the winter months. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. The months July through September offer the most favorable weather for visiting The Needles.
Johnson, Sweat Spire, Gasp Pinnacle to left. Clark and Sundial to right.
Martin, Incisor, Johnson, Clark, and Sundial seen from Marmot Pass
Mt. Deception (left), The Needles centered, Tyler Peak along right edge, as seen from near Port Townsend
Geology
The Olympic Mountains are composed of obductedclastic wedge material and oceanic crust, primarily Eocenesandstone, turbidite, and basaltic oceanic crust.[16] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.