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Coordinates: 35°22′16″N 133°32′47″E / 35.37111°N 133.54639°E / 35.37111; 133.54639
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{{Short description|Stratovolcano on the island of Honshu in Japan}}
{{Infobox mountain
{{Infobox mountain
| name = Daisen
| name = Mount Daisen
| other_name = 大山
| other_name = 大山
| translation = Big Mountain
| translation = Big Mountain
| language = [[Japanese language|Japanese]]
| language = [[Japanese language|Japanese]]
| pronunciation = {{IPA-ja|daiseɴ|lang}}
| pronunciation = {{IPA|ja|daiseɴ|lang}}
| photo = Mt Daisen Full View.jpg
| photo = Mt Daisen Full View.jpg
| photo_size =
| photo_size =
| photo_caption = Mount Daisen from the West
| photo_alt =
| photo_caption = Daisen from the West
| elevation =
| elevation_m = 1729
| elevation_m = 1729
| elevation_ref = <ref name="peaklist">[http://www.peaklist.org/WWlists/ultras/japan.html "Japan Ultra-Prominences"]. Peaklist.org. Retrieved 2013-03-22.</ref>
| elevation_ft =
| elevation_ref =
| range = [[Chūgoku Mountains]]
| range = [[Chūgoku Mountains]]
| prominence =
| prominence_m = 1634
| prominence_ref = <ref name="peaklist"/>
| prominence_m =
| prominence_ft =
| prominence_ref =
| parent_peak =
| parent_peak =
| listing = [[Ultra prominent peak|Ultra]]<br />[[List of mountains and hills of Japan by height]]
| location = [[Tottori Prefecture]], [[Japan]]
| location = [[Tottori Prefecture]], [[Japan]]
| map = Japan
| map = Japan
| map_alt =
| map_caption = Japan
| map_caption =
| map_size =
| map_size =
| label = Daisen
| label = Mount Daisen
| label_position = top
| label_position = top
| coordinates = {{coord|35|22|16|N|133|32|47|E|type:mountain_scale:100000|format=dms|display=inline,title}}
| lat_d = 35
| lat_m = 22
| coordinates_ref =
| lat_s = 16
| lat_NS = N
| long_d = 133
| long_m = 32
| long_s = 47
| long_EW = E
| region =
| coordinates = {{coord|35|22|16|N|133|32|47|E|type:mountain|display=inline,title}}| coordinates_ref =
| topo =
| topo =
| type = [[Complex volcano]]
| type = [[Complex volcano]]
| volcanic_arc/belt=
| volcanic_arc/belt=
| age =
| age =
| last_eruption = Estimated 20,000 years ago
| last_eruption = Estimated 17,000-18,000 years ago
| first_ascent =
| first_ascent =
| easiest_route = [[Hiking]]
| easiest_route = [[Hiking]]
| grid_ref_UK =
| grid_ref_UK =
| grid_ref_Ireland =
| grid_ref_Ireland =
| listing = [[List of mountains and hills of Japan by height]]
}}
}}


{{nihongo|'''Daisen'''|大山|Daisen}}, is a [[volcano|volcanic]] mountain located in [[Tottori Prefecture]], [[Japan]]. It has an [[Topographical summit|elevation]] of 1,729 metres. This mountain is the highest in the [[Chūgoku region]], and the most important volcano on the [[Daisen volcanic belt]]. The Daisen volcanic belt is a part of Southwest Honshu volcanic arc, where the [[Philippine Sea Plate]] is subducting under the [[Amurian Plate]].
{{nihongo|'''Mount Daisen'''|大山|Daisen}} is a dormant [[stratovolcano]] in [[Tottori Prefecture]], [[Japan]]. It has an [[Topographical summit|elevation]] of 1,729 metres. This mountain is the highest in the [[Chūgoku region]], and the most important volcano on the Daisen [[volcanic belt]], which is a part of the Southwestern Honshu volcanic arc, where the [[Philippine Sea Plate]] is subducting under the [[Amurian Plate]].{{fact|date=September 2022}}


==Outline==
==Outline==
Daisen is a [[complex volcano]], made by repeated volcanic activity over thousands of years. Eruptions in this area started 1.8 million years ago and resulted in ''Old Daisen'' some 500,000 years ago. The Daisen of today, ''New Daisen'', resulted from a second group of eruptions which started 50,000 years ago and ended 10,000 years ago in the caldera of Old Daisen. 50,000 years ago, this mountain had a [[plinian eruption]] from which volcanic ash can be found as far away as the [[Tohoku Region]] of Japan. This mountain is one of [[List of the 100 famous mountains in Japan|the 100 famous mountains in Japan]], and also one of the [[Chūgoku 100 mountains]].
Mount Daisen is a [[complex volcano]], made by repeated volcanic activity over thousands of years. Eruptions in this area started 1.8 million years ago and resulted in ''Old Daisen'' some 500,000 years ago{{fact|date=August 2024}}. The Mount Daisen of today, ''New Daisen'', resulted from a second group of eruptions which started 50,000 years ago and ended 10,000 years ago in the caldera of Old Daisen. 50,000 years ago, this mountain had a [[plinian eruption]] from which volcanic ash can be found as far away as the [[Tohoku Region]] of Japan. Daisen is one of [[List of the 100 famous mountains in Japan|the 100 famous mountains in Japan]], and also one of the [[Chūgoku 100 mountains]].
[[File:Daisen Volcano & Hiruzen Volcano Group Relief Map, SRTM-1.jpg|thumb|left|180px|Relief Map]]


==History and Religion==
==History and religion==
Daisen, which stands directly on the Sea of Japan, was regarded as one of the most important mountains for Japanese [[Shugendo]]. According to the ''[[Izumo Kokudo Fudoki]]'', completed in 733, this mountain was called ''Ōkami-take'', literally, ''Mountain of the great god''.
Mount Daisen, which stands directly on the Sea of Japan, was regarded as one of the most important mountains for Japanese [[Shugendō|Shugendō religion]]. According to the ''[[Izumo Kokudo Fudoki]]'', completed in 733, it was called ''Ōkami-take'', literally, ''Mountain of the great god''.


Daisen has been called Hōki Fuji and Izumo Fuji, depending on which side of the mountain the viewer is standing on. These names are based on the old [[Hōki Province|Hōki]] and [[Izumo Province|Izumo]] provinces.<ref name="Hunt">Paul Hunt, ''Hiking in Japan: An Adventurer's Guide to the Mountain Trails'', pg 73</ref>
Mount Daisen has been called Hōki Fuji and Izumo Fuji, depending on which side of the mountain the viewer is standing on. These names are based on the old [[Hōki Province|Hōki]] and [[Izumo Province|Izumo]] provinces.<ref name="Hunt">Paul Hunt, ''Hiking in Japan: An Adventurer's Guide to the Mountain Trails'', pg 73</ref>


In the middle of the mountain, there is a Buddhist temple, called ''[[Daisen-ji]]''. This temple has existed as a centre of worship since the [[Heian Period]]. The temple was founded by the [[Tendai]] sect in 718.<ref name="Hunt" />
Halfway up the mountain stands a Buddhist temple, ''[[Daisen-ji]]''. This has existed as a centre of worship since the [[Heian period]]. It was founded by the [[Tendai]] sect in 718.<ref name="Hunt" />


Climbing the mountain used to be severely prohibited without a selected monk of Daisen-ji, and common people could not access the mountain until the [[Edo Period]].
Climbing the mountain used to be severely prohibited without a selected monk of Daisen-ji, and common people could not access the mountain until the [[Edo period]].


The mountain has also been important to the mountain ascetics of the [[Shugendō]] sect. Just above the temple is the [[Ōgamiyama Jinja]], literally, ''shrine of the mountain of the great god''.<ref name="Hunt" />
The mountain has also been important to the mountain ascetics of the [[Shugendō]] sect. Just above the temple is the [[Ōgamiyama Jinja]], literally, ''shrine of the mountain of the great god''.<ref name="Hunt" />


==Route==
==Route==
After the Great Tottori Earthquake in 2000, some of Daisen's peaks are on the verge of collapse. It is prohibited to ascend the mountain's highest peak, the Kengamine ({{convert|1729|m|ft}}). Climbers are able to access the Misen Peak ({{convert|1709.4|m|ft}}).<ref name="GSI">{{cite web|url=http://watchizu.gsi.go.jp/watchizu.aspx?b=352216&l=1333224|title=伯耆大山|year=2008|publisher=Geographical Survey Institute|language=Japanese|accessdate=2008-07-21}}</ref> The most popular route is from Daisen-ji to the Misen Peak. It takes three hours to reach the summit.
After the [[2000 Tottori earthquake]], some of Mount Daisen's peaks are on the verge of collapse. It is prohibited to ascend the mountain's highest peak, the Kengamine ({{convert|1729|m|ft}}). Climbers are able to access the Misen Peak ({{convert|1709.4|m|ft}}).<ref name="GSI">{{cite web|url=http://watchizu.gsi.go.jp/watchizu.aspx?b=352216&l=1333224|script-title=ja:伯耆大山|year=2008|publisher=Geographical Survey Institute|language=ja|access-date=2008-07-21}}</ref> The most popular route is from Daisen-ji to the Misen Peak. It takes three hours to reach the summit.
{{-}}

==Gallery==
==Gallery==
<gallery>
<gallery mode=packed style="font-size:90%">
File:Daisen south wall.jpg|South Wall of Daisen
File:Daisen 2016-03-21 (25887648161).jpg|NW side
File:Daisen in Autumn.jpg|In Autumn
File:Daisen 2014-10-24 (14997796814).jpg|South wall
File:Daisen highest peak.jpg|Kengamine Peak, the Highest Peak of Daisen
File:Daisen 2016-03-07 (25502160362).jpg|WNW side
File:Daisen2.JPG|North Wall of Daisen
File:Daisen highest peak.jpg|Kengamine Peak, the highest peak of Mount Daisen
Mount Daisen 2015-05-03 (17214768368).jpg|Looking NW
File:daisen2.jpg|A view around Misen Peak of Daisen
File:32 View from Summit.JPG|Mount Hiruzen from Daisen
File:View of Hiruzen from Daisen Summit.JPG|Looking SSW
File:The Famous Scenes of the Sixty States 41 Hoki.jpg|[[Hiroshige]]
</gallery>
</gallery>


==See also==
==See also==
*[[Tourism in Japan]]
* [[List of mountains in Japan]]
* [[List of volcanoes in Japan]]
* [[List of Ultras of Japan]]


==References==
==References==
{{Commons category|Mount Daisen}}
{{Commons category|Daisen (mountain)}}
{{reflist}}
{{reflist}}
* [http://www.gsi.go.jp/ENGLISH/index.html Geographical Survey Institute]
* [http://www.gsi.go.jp/ENGLISH/index.html Geographical Survey Institute]
* Paul Hunt, ''Hiking in Japan: An Adventurer's Guide to the Mountain Trails'', [[Tokyo]], [[Kodansha|Kodansha International Ltd.]], 1988. ISBN 0-87011-893-5 and ISBN 4-7700-1393-0 C0075
* Paul Hunt, ''Hiking in Japan: An Adventurer's Guide to the Mountain Trails'', [[Tokyo]], [[Kodansha|Kodansha International Ltd.]], 1988. {{ISBN|0-87011-893-5}} and {{ISBN|4-7700-1393-0}} C0075

==External links==
*[http://en.go-to-japan.jp/daisenguide/ Daisen Guide]


== External links ==
* {{cite gvp|name=Daisen|vn=283811|access-date=2021-06-25}}
* [https://gbank.gsj.jp/volcano/Quat_Vol/volcano_data/H17.html Daisen] - Geological Survey of Japan
* [http://en.go-to-japan.jp/daisenguide/ Daisen Guide] - Houki town
{{100 Famous Japanese Mountains}}
{{100 Famous Japanese Mountains}}


{{Authority control}}
{{DEFAULTSORT:Daisen}}

{{DEFAULTSORT:Daisen, Mount}}
[[Category:Mountains of Tottori Prefecture]]
[[Category:Mountains of Tottori Prefecture]]
[[Category:Volcanoes of Honshū]]
[[Category:Volcanoes of Honshū]]
[[Category:Complex volcanoes]]
[[Category:Complex volcanoes]]
[[Category:Visitor attractions in Tottori Prefecture]]
[[Category:Volcanoes of Tottori Prefecture]]
[[Category:Highest points of Japanese national parks]]

[[Category:Stratovolcanoes of Japan]]
[[de:Daisen (Berg)]]
[[Category:Pleistocene stratovolcanoes]]
[[et:Daiseni vulkaan]]
[[Category:Calderas of Honshū]]
[[ja:大山 (鳥取県)]]
[[zh:大山 (鳥取縣)]]

Latest revision as of 22:00, 24 September 2024

Mount Daisen
大山
Mount Daisen from the West
Highest point
Elevation1,729 m (5,673 ft)[1]
Prominence1,634 m (5,361 ft)[1]
ListingUltra
List of mountains and hills of Japan by height
Coordinates35°22′16″N 133°32′47″E / 35.37111°N 133.54639°E / 35.37111; 133.54639
Naming
English translationBig Mountain
Language of nameJapanese
PronunciationJapanese: [daiseɴ]
Geography
Mount Daisen is located in Japan
Mount Daisen
Mount Daisen
Japan
LocationTottori Prefecture, Japan
Parent rangeChūgoku Mountains
Geology
Mountain typeComplex volcano
Last eruptionEstimated 17,000-18,000 years ago
Climbing
Easiest routeHiking

Mount Daisen (大山, Daisen) is a dormant stratovolcano in Tottori Prefecture, Japan. It has an elevation of 1,729 metres. This mountain is the highest in the Chūgoku region, and the most important volcano on the Daisen volcanic belt, which is a part of the Southwestern Honshu volcanic arc, where the Philippine Sea Plate is subducting under the Amurian Plate.[citation needed]

Outline

[edit]

Mount Daisen is a complex volcano, made by repeated volcanic activity over thousands of years. Eruptions in this area started 1.8 million years ago and resulted in Old Daisen some 500,000 years ago[citation needed]. The Mount Daisen of today, New Daisen, resulted from a second group of eruptions which started 50,000 years ago and ended 10,000 years ago in the caldera of Old Daisen. 50,000 years ago, this mountain had a plinian eruption from which volcanic ash can be found as far away as the Tohoku Region of Japan. Daisen is one of the 100 famous mountains in Japan, and also one of the Chūgoku 100 mountains.

Relief Map

History and religion

[edit]

Mount Daisen, which stands directly on the Sea of Japan, was regarded as one of the most important mountains for Japanese Shugendō religion. According to the Izumo Kokudo Fudoki, completed in 733, it was called Ōkami-take, literally, Mountain of the great god.

Mount Daisen has been called Hōki Fuji and Izumo Fuji, depending on which side of the mountain the viewer is standing on. These names are based on the old Hōki and Izumo provinces.[2]

Halfway up the mountain stands a Buddhist temple, Daisen-ji. This has existed as a centre of worship since the Heian period. It was founded by the Tendai sect in 718.[2]

Climbing the mountain used to be severely prohibited without a selected monk of Daisen-ji, and common people could not access the mountain until the Edo period.

The mountain has also been important to the mountain ascetics of the Shugendō sect. Just above the temple is the Ōgamiyama Jinja, literally, shrine of the mountain of the great god.[2]

Route

[edit]

After the 2000 Tottori earthquake, some of Mount Daisen's peaks are on the verge of collapse. It is prohibited to ascend the mountain's highest peak, the Kengamine (1,729 metres (5,673 ft)). Climbers are able to access the Misen Peak (1,709.4 metres (5,608 ft)).[3] The most popular route is from Daisen-ji to the Misen Peak. It takes three hours to reach the summit.

[edit]

See also

[edit]

References

[edit]
  1. ^ a b "Japan Ultra-Prominences". Peaklist.org. Retrieved 2013-03-22.
  2. ^ a b c Paul Hunt, Hiking in Japan: An Adventurer's Guide to the Mountain Trails, pg 73
  3. ^ 伯耆大山 (in Japanese). Geographical Survey Institute. 2008. Retrieved 2008-07-21.
[edit]