Vesper Peak

Vesper Peak
Photo of Vesper Peak from Mount Dickerman
Highest point
Elevation6,221 ft (1,896 m)[1]
Prominence1,574 ft (480 m)[2]
Coordinates48°00′47″N 121°31′04″W / 48.012989783°N 121.517901789°W / 48.012989783; -121.517901789[1]
Geography
LocationSnohomish County, Washington, U.S.
Parent rangeNorth Cascades, Cascade Range
Topo mapUSGS Silverton
Climbing
First ascentBefore 1918, possibly by Louis C. Fletcher et al. (surveyors)
Easiest routeEast Ridge: moderate scramble, (class 2)

Vesper Peak is a peak along the Mountain Loop Highway region of the North Cascades of Washington state. It is about 18 miles (29 km) south of Darrington and 21 miles (34 km) east of Granite Falls, in the Mount Baker-Snoqualmie National Forest. Its gentle south and east slopes contrast with a sheer north face which offers "excellent technical routes".[3]

Geology

Vesper Peak consists of biotite-quartz diorite that intrudes metamorphosed Mesozoic ribbon cherts. The ribbon chert underlies its south and southwest slopes.[4][5] This Oligocene biotite-quartz diorite stock is an offshoot and extension of the Index batholith that outcrops south of this peak.[6]

Historic Mining

Vesper Peak lies in the eastern part of the Sultan Mining District. Directly associated with Vesper Peak are the now-depleted Vesper Peak Garnet Deposit, also known as the 48-58 Prospect, which lies near it summit and the Sunrise Copper Prospect, which lies near its base. Grossular garnets and other gem quality minerals were mined from a lens of fine- to coarse-grained skarn composed of hedenbergite, grossular, quartz, and wollastonite. The pod formed from the hydrothermal alteration of limestone that was completely enclosed in chert near the chert-diorite contact. This lens was about 30 m (98 ft) long, 20 m (66 ft) wide, and at it thickest about 120 m (390 ft) thick.[4][7] The Sunrise Copper Prospect lies less than a 1 km (0.62 mi) southeast of Vesper Peak at altitudes of about 1,200 to 1,500 m (3,900 to 4,900 ft) in rough and precipitous terrain. It consists of a large mass of quartz-cemented tectonic breccia which contains chalcopyrite and molybdenite as the primary ore minerals.[7][8] In 1976, an unsuccessful proposal was made to develop the Sunrise Copper Prospect as a major molybdenum mine on Vesper Peak.[9]

The maps of Broughton,[8] Carithers,[7] and others,[10] show the presence of addiotional open cut pits and underground workings from historic mineral exploration in the immediate vicinity of Vesper Peak. For example, numerous copper prospects, including underground mine workings, can be found about 5 to 6.5 km (3.1 to 4.0 mi) north and northwest of Vesper Peak between Copper Lake and Marble Pass. In addition, about 2 km (1.2 mi) west and southwest of Vesper Peak, lie additional mineral prospects, e,g, Ala-Dickson and Mountain Cedar prospects, containing open cut pits, audits, and shafts. Other unmapped and unrecorded, mine works may exist in the area of Vesper Peak.[7][8]

Climbing and recreation

The peak was ascended in 1918 during a Mountaineers outing, but "they were likely preceded by prospectors and a geological survey party led by Louis C. Fletcher".[3] The steep north face was first climbed in 1968 by Bruce Garrett and Jim Langdon; several routes exist on the face, with difficulties in the 5.6 to 5.10 range.[3]

The summit can be reached from the Sunrise Mine Road (No. 4065), off the Mountain Loop Highway.[11] The hike is a 10-mile (16 km) round trip with an elevation gain of 4,114 feet (1,254 m).[12] The summit affords views of Glacier Peak, Sloan Peak, Mount Dickerman, Mount Pugh, Mount Rainier, Mount Stuart and a bit of the top of Mount Adams.

This Location is the first scene the player sees, and an optional destination in the "Postcards" section in the VR Demo The Lab.

References

  1. ^ a b "Vesper Peak". NGS Data Sheet. National Geodetic Survey, National Oceanic and Atmospheric Administration, United States Department of Commerce. Retrieved October 23, 2008.
  2. ^ "Vesper Peak, Washington". Peakbagger.com. Retrieved April 9, 2008.
  3. ^ a b c Beckey, Fred W. (1996). Cascade Alpine Guide, Vol. 2, Stevens Pass to Rainy Pass (2nd ed.). Mountaineers Books. pp. 48–53. ISBN 0-89886-152-7.
  4. ^ a b Cannon, B., 1991. The Vesper Peak Garnet Deposit: Snohomish County, Washington Rocks & Minerals, 66(6), pp.478-484.
  5. ^ Tabor, R.W., Booth, D.B., Vance, J.A. and Ford, A.B., 2002. Geologic map of the Sauk River 30-by 60-minute quadrangle, Washington. U.S. Geological Survey, Geologic Investigations Series Map, I-2592, scale 1:100,000, pamphlet, 67 pp.
  6. ^ Yeats, R.S., and Engels, J.C., 1971. Potassium-argon ages of plutons in the Skykomish-Stillaguamish areas, north Cascades, Washington. U.S. Geological Survey Professional Paper, 750-D, pp. D34–D38.
  7. ^ a b c d Carithers, W., and Guard, A.K., 1945. Geology and ore deposits of the Sultan Basin, Snohomish County, Washington. Washington Division of Mines and Geology Bulletin, 36, 90 pp.
  8. ^ a b c Broughton, W.A., 1942. Inventory of mineral properties in Snohomish County. Washington. Washington Division of Geology Report of Investigations, 6, 64 pp.
  9. ^ Forest Supervisor, 1976, The Sunrise mine proposal: and the role of the U.S. Forest Service in applying the National Environmental Policy Act to a major mining proposal. Seattle, Washington, Mt. Baker-Snoqualmie National Forest, United States Forest Service. 4 pp.
  10. ^ Mineral & Land Records System, Department of Interior, Washington, DC.
  11. ^ "Vesper Peak's East Ridge, Via Sunrise Mine Trail and Headlee Pass". SummitPost.org.
  12. ^ Sykes, Karen (September 13, 2001). "Hike of the Week: Vesper Peak is a rewarding challenge for hikers stout of heart and boot". Seattle Post-Intelligencer.
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