Devore Peak: Difference between revisions
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{{short description|Mountain in Washington (state), United States}} |
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{{Infobox mountain |
{{Infobox mountain |
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| name = Devore Peak |
| name = Devore Peak |
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| photo = Devore Peak, from White Goat Mountain.jpg |
| photo = Devore Peak, from White Goat Mountain.jpg |
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| photo_caption = Devore Peak seen from [[White Goat Mountain]] |
| photo_caption = Devore Peak seen from [[White Goat Mountain]] |
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| elevation_ft = |
| elevation_ft = 8382 |
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| elevation_ref = |
| elevation_ref =<ref name="listsofjohn">{{cite web|url=https://listsofjohn.com/peak/48742|title=Devore Peak - 8,382' WA|website=listsofjohn.com|accessdate=2024-04-07}}</ref> |
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| prominence_ft = |
| prominence_ft = 1762 |
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| prominence_ref = |
| prominence_ref =<ref name="listsofjohn"/> |
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| isolation_mi = 3.37 |
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| isolation_ref =<ref name="listsofjohn"/> |
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| map = Washington#USA |
| map = Washington#USA |
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| map_caption = Location in Washington |
| map_caption = Location in Washington |
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| map_size = 260 |
| map_size = 260 |
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| country = United States |
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| location = [[Chelan County, Washington|Chelan County]]<br/>[[Washington (U.S. state)|Washington]], [[United States|U.S.]] |
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| state = [[Washington (U.S. state)|Washington]] |
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| region = [[Chelan County, Washington|Chelan]] |
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| region_type = County |
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| part_type = Protected area | part = [[Glacier Peak Wilderness]]<ref name="pb">{{cite peakbagger|1900|Devore Peak, Washington}}</ref> |
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| range = [[North Cascades]]<br />[[Cascade Range]] |
| range = [[North Cascades]]<br />[[Cascade Range]] |
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| coordinates = {{coord|48.276774|N|120.7653|W|type:mountain_region:US-WA_scale:100000_source:ngs|format=dms|display=inline,title}} |
| coordinates = {{coord|48.276774|N|120.7653|W|type:mountain_region:US-WA_scale:100000_source:ngs|format=dms|display=inline,title}} |
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| rock = [[Granodiorite]] |
| rock = [[Granodiorite]] |
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| age = |
| age = |
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| first_ascent = July 28, 1940 by Everett Darr, Ida Darr, Abigail Avery, Stuart B. Avery, Jane Foster McConnell, Grant McConnell, Paul Parker<ref>[http://www.rhinoclimbs.com/WA100HighestFAChronology.htm |
| first_ascent = July 28, 1940 by Everett Darr, Ida Darr, Abigail Avery, Stuart B. Avery, Jane Foster McConnell, Grant McConnell, Paul Parker<ref>[http://www.rhinoclimbs.com/WA100HighestFAChronology.htm Washington's Highest Mountains First Ascent Chronology], Rhinoclimbs.com</ref> |
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FIRST ASCENT CHRONOLOGY Rhinoclimbs.com</ref> |
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'''Devore Peak''' is an {{ |
'''Devore Peak''' is an {{Convert|8382|ft|m|lk=off|abbr=off|adj=on}} mountain summit located in the [[Glacier Peak Wilderness]] of the [[North Cascades]] in [[Washington (U.S. state)|Washington]] state.<ref name="gnis"> |
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{{cite gnis |
{{cite gnis |
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| id = 1518731 |
| id = 1518731 |
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| name = Devore Peak |
| name = Devore Peak |
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| accessdate = 2019-05-06}}</ref> The mountain is situated in [[Chelan County, Washington|Chelan County]], on land managed by [[Wenatchee National Forest]]. Its nearest higher peak is [[Martin Peak (Washington)|Martin Peak]], {{convert|3.36|mi|km|abbr=on}} to the southwest, and [[Tupshin Peak]] lies {{convert|1.55|mi|km|abbr=on}} to the north-northeast.<ref name="pb"/> Precipitation [[Surface runoff|runoff]] from the peak drains to nearby [[Lake Chelan]] via tributaries of the [[Stehekin River]] and Devore Creek. |
| accessdate = 2019-05-06}}</ref> The mountain is situated in [[Chelan County, Washington|Chelan County]], on land managed by [[Wenatchee National Forest]]. Its nearest higher peak is [[Martin Peak (Washington)|Martin Peak]], {{convert|3.36|mi|km|abbr=on}} to the southwest, and [[Tupshin Peak]] lies {{convert|1.55|mi|km|abbr=on}} to the north-northeast.<ref name="pb"/> Precipitation [[Surface runoff|runoff]] from the peak drains to nearby [[Lake Chelan]] via tributaries of the [[Stehekin River]] and Devore Creek. |
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==Climate== |
==Climate== |
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[[Weather front]]s originating in the Pacific Ocean travel northeast toward the [[Cascade Mountains]]. As fronts approach the [[North Cascades]], they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades ([[Orographic lift]]). As a result, the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall.<ref name="Beckey, Fred W 2008">Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.</ref> 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.<ref name="Beckey, Fred W 2008"/> |
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==Geology== |
==Geology== |
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The North Cascades feature some of the most rugged topography in the [[Cascade Range]] with craggy peaks, spires, ridges, and deep [[glacial valley]]s. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences. |
The North Cascades feature some of the most rugged topography in the [[Cascade Range]] with craggy peaks, spires, ridges, and deep [[glacial valley]]s. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences. |
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The history of the formation of the Cascade Mountains dates back millions of years ago to the late [[Eocene]] Epoch.<ref name=Kruckeberg>{{cite book|last=Kruckeberg|first=Arthur|title=The Natural History of Puget Sound Country|publisher=University of Washington Press|year=1991}}</ref> With the [[North American Plate]] overriding the [[Pacific Plate]], episodes of [[volcano|volcanic igneous activity]] persisted.<ref name=Kruckeberg/> Glacier Peak, a [[stratovolcano]] that is {{convert|19.74|mi|km|abbr=on}} southwest of Devore Peak, began forming in the mid-[[Pleistocene]].<ref name="Beckey, Fred W 2008"/> In addition, small fragments of the [[oceanic lithosphere|oceanic]] and [[continental lithosphere]] called [[terrane]]s created the [[North Cascades]] about 50 million years ago.<ref name=Kruckeberg/> |
The history of the formation of the Cascade Mountains dates back millions of years ago to the late [[Eocene]] Epoch.<ref name=Kruckeberg>{{cite book|last=Kruckeberg|first=Arthur|title=The Natural History of Puget Sound Country|publisher=University of Washington Press|year=1991}}</ref> With the [[North American Plate]] overriding the [[Pacific Plate]], episodes of [[volcano|volcanic igneous activity]] persisted.<ref name=Kruckeberg/> Glacier Peak, a [[stratovolcano]] that is {{convert|19.74|mi|km|abbr=on}} southwest of Devore Peak, began forming in the mid-[[Pleistocene]].<ref name="Beckey, Fred W 2008"/> In addition, small fragments of the [[oceanic lithosphere|oceanic]] and [[continental lithosphere]] called [[terrane]]s created the [[North Cascades]] about 50 million years ago.<ref name=Kruckeberg/> |
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During the [[Pleistocene]] period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.<ref name=Kruckeberg/> The |
During the [[Pleistocene]] period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.<ref name=Kruckeberg/> The U-shaped cross section of the river valleys is a result of recent glaciation. [[orogeny|Uplift]] and [[fault (geology)|fault]]ing in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area. |
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==See also== |
==See also== |
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*[[List of mountain peaks of Washington (state)]] |
*[[List of mountain peaks of Washington (state)]] |
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* [[Geology of the Pacific Northwest]] |
* [[Geology of the Pacific Northwest]] |
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* {{Portal-inline|Mountains|size=tiny}} |
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==References== |
==References== |
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==External links== |
==External links== |
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* Weather forecast: [https://www.yr.no/ |
* Weather forecast: [https://www.yr.no/en/forecast/daily-table/2-5792349/United%20States/Washington/Chelan/Devore%20Peak Devore Peak] |
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[[Category:Mountains of Washington (state)]] |
[[Category:Mountains of Washington (state)]] |
Latest revision as of 01:20, 8 April 2024
Devore Peak | |
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Highest point | |
Elevation | 8,382 ft (2,555 m)[1] |
Prominence | 1,762 ft (537 m)[1] |
Parent peak | Martin Peak (8,511 ft)[1] |
Isolation | 3.37 mi (5.42 km)[1] |
Coordinates | 48°16′36″N 120°45′55″W / 48.276774°N 120.7653°W[2] |
Geography | |
Country | United States |
State | Washington |
County | Chelan |
Protected area | Glacier Peak Wilderness[2] |
Parent range | North Cascades Cascade Range |
Topo map | USGS Mount Lyall |
Geology | |
Rock type | Granodiorite |
Climbing | |
First ascent | July 28, 1940 by Everett Darr, Ida Darr, Abigail Avery, Stuart B. Avery, Jane Foster McConnell, Grant McConnell, Paul Parker[3] |
Easiest route | Climbing class 4[1] |
Devore Peak is an 8,382-foot (2,555-metre) mountain summit located in the Glacier Peak Wilderness of the North Cascades in Washington state.[4] The mountain is situated in Chelan County, on land managed by Wenatchee National Forest. Its nearest higher peak is Martin Peak, 3.36 mi (5.41 km) to the southwest, and Tupshin Peak lies 1.55 mi (2.49 km) to the north-northeast.[2] Precipitation runoff from the peak drains to nearby Lake Chelan via tributaries of the Stehekin River and Devore Creek.
Climate
[edit]Weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall.[5] 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.[5]
Geology
[edit]The North Cascades feature some of the most rugged topography in the Cascade Range with craggy peaks, spires, ridges, and deep glacial valleys. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences.
The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.[6] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.[6] Glacier Peak, a stratovolcano that is 19.74 mi (31.77 km) southwest of Devore Peak, began forming in the mid-Pleistocene.[5] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.[6]
During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.[6] The U-shaped cross section of the river valleys is a result of recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area.
See also
[edit]References
[edit]- ^ a b c d e "Devore Peak - 8,382' WA". listsofjohn.com. Retrieved 2024-04-07.
- ^ a b c "Devore Peak, Washington". Peakbagger.com.
- ^ Washington's Highest Mountains First Ascent Chronology, Rhinoclimbs.com
- ^ "Devore Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2019-05-06.
- ^ a b c Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
- ^ a b c d Kruckeberg, Arthur (1991). The Natural History of Puget Sound Country. University of Washington Press.
External links
[edit]- Weather forecast: Devore Peak