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Mount Dana is a mountain in the U.S. state of California. Its summit marks the eastern boundary of Yosemite National Park and the western boundary of the Ansel Adams Wilderness. At an elevation of 13,061 feet (3,981 m), it is the second highest mountain in Yosemite (after Mount Lyell), and the northernmost summit in the Sierra Nevada which is over 13,000 feet (3,962.4 m) in elevation. Mount Dana is the highest peak in Yosemite that is a simple hike to the summit. The mountain is named in honor of James Dwight Dana, who was a professor of natural history and geology at Yale.[6]

Mount Dana
Mount Dana seen from Gaylor Peak.
The hike to the top goes up this west face.
Highest point
Elevation13,061 ft (3,981 m) NAVD 88[1]
Prominence2,417 ft (737 m)[2]
Parent peakMount Lyell[3]
ListingCalifornia highest major peaks 18th
Coordinates37°54′00″N 119°13′16″W[1]
Geography
LocationMono / Tuolumne counties, California, U.S.
Parent rangeSierra Nevada
Topo mapUSGS Mount Dana
Geology
Age of rockCretaceous
Mountain typeMetamorphic rock
Climbing
First ascentJune 28, 1863 by Whitney, Brewer, and Hoffmann[4]
Easiest routeHike, class 1[5]

Mount Dana is composed of prebatholithic rock that is mostly reddish metamorphic rock, which was composed by metavolcanics of surfacing magma from the Mesozoic Era.[7][8]

Mount Dana's northern face includes a small, receding glacier known as the Dana Glacier. The Dana Meadows lie at the foot of the mountain. From the top, lakes throughout Dana Meadows, Mono Lake, Tioga Peak and many other mountains are in view.


Hike


From the Tioga Pass Road there are many easy routes. (class 1), available that lead to the summit along the mountain's western or southern slopes. These routes rise 3,108 feet (947 m) in elevation in 2.9 miles (4.7 km), (a 20.3% average grade). The trail is not frequently maintained.

Mount Dana Topographic Map
Mount Dana Topographic Map

There is a clearly marked path leading just above tree line. After topping a ridge, a set of use-paths and ducked routes are present, with the main path running along the easterly ridgeline. Additionally, numerous alternate trail segments begin and end at various points on the southwestern face, making parts of this hike a difficult class 2. The path segments turn into scree toward the summit, where a shallow stone-walled shelter and register are found. Significant snow fields on the mountain slopes can exist late into the summer season. Total round trip hiking time can be anywhere between 3 and 12 hours depending many factors, such as acclimatization to elevation.

After reaching a plateau above the tree line, almost all vegetation disappears with the exception of lichen and a few high alpine Sky Pilot (Polemonium eximium). Fauna are largely limited to spiders and insects, such as black/brown grasshoppers. The only mammals other than humans are marmots and American Pikas which are lagomorphs related to rabbits.

Thunderstorms are known to arise suddenly, making the rocks slippery, and the hiking dangerous year round.

Even experienced hikers can face altitude sickness, due to the high elevation.[9]

In the summer of 2009, an NPS employee died after falling on a technical rock climbing route on the northeast face of Mount Dana.[citation needed]

Panoramic Photograph of Mount Dana, Yosemite National Park taken from Tioga Pass Park Entrance
The view from the summit encompasses much of Yosemite National Park and Mono Lake

References


  1. "Mount Dana". NGS Data Sheet. National Geodetic Survey, National Oceanic and Atmospheric Administration, United States Department of Commerce.
  2. "Mount Dana, California". Peakbagger.com. Retrieved 2009-08-05.
  3. "Mount Dana". ListsOfJohn.com. Retrieved 2012-04-01.
  4. Farquhar, Francis P. (March 1925). "Exploration of the Sierra Nevada". California Historical Society Quarterly. 4 (1): 3–58. doi:10.2307/25177743. hdl:2027/mdp.39015049981668. JSTOR 25177743.
  5. Secor, R.J. (2009). The High Sierra Peaks, Passes, and Trails (3rd ed.). Seattle: The Mountaineers. pp. 397f. ISBN 978-0898869712.
  6. Browning, Peter (1986). Place Names of the Sierra Nevada. Berkeley: Wilderness Press. p. 51. ISBN 0899971199.
  7. "America's Volcanic Past - Yosemite National Park". USGS/Cascades Volcano Observatory. September 20, 2002. Archived from the original on May 16, 2006. Retrieved July 11, 2006.
  8. "Biology 314 — Sierra Nevada". Sonoma State University. pp. 69–94. Retrieved 2006-07-08.
  9. Cymerman, A; Rock, PB. "Medical Problems in High Mountain Environments. A Handbook for Medical Officers". USARIEM-TN94-2. US Army Research Inst. of Environmental Medicine Thermal and Mountain Medicine Division Technical Report. Archived from the original on 2009-04-23. Retrieved 2009-03-05. {{cite journal}}: Cite journal requires |journal= (help)CS1 maint: unfit URL (link)



На других языках


[de] Mount Dana

Der Mount Dana ist ein 3982 m[2] hoher Berg in der Sierra Nevada im Bundesstaat Kalifornien der Vereinigten Staaten. Er liegt auf der Grenze zwischen dem Mono County und dem Tuolumne County. Der Gipfel bildet die zweithöchste Erhebung im Yosemite-Nationalpark.[3] Der Berg ist nach dem Geologen James Dwight Dana benannt.
- [en] Mount Dana

[es] Monte Dana

Mount Dana es una montaña en el estado estadounidense de California. Su cumbre marca el límite oriental del parque nacional de Yosemite y el límite occidental de Ansel Adams Wilderness. Con una altura de 13 061 pies (3981 m), es la segunda montaña más alta de Yosemite (después del monte Lyell) y la cumbre más septentrional de la Sierra Nevada. La montaña recibe su nombre en honor a James Dwight Dana, quien fue profesor de historia natural y geología en Yale . [1] La cara norte del monte Dana incluye un pequeño glaciar en retroceso conocido como el glaciar Dana. Desde la cima se pueden ver lagos a lo largo de Dana Meadows, Mono Lake, Tioga Peak y muchas otras montañas de la zona.

[fr] Mont Dana

Le mont Dana est une montagne à l'est du parc national de Yosemite et est le second plus haut sommet du parc après le mont Lyell. La région appelée Dana Meadows s'étend au pied de la montagne, elle tient son nom du professeur de géologie James Dwight Dana qui enseignait à Yale. Le mont Dana est composé de roches métamorphiques rougeâtres.



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