Sobo,_Katamuki_and_Okue_Biosphere_Reserve

Sobo, Katamuki and Okue Biosphere Reserve

Sobo, Katamuki and Okue Biosphere Reserve

Biosphere Reserve in Japan

The Sobo, Katamuki and Okue Biosphere Reserve also known as Sobokatakue Unesco Eco Park (祖母傾大崩ユネスコエコパーク, Sobokatamuki Okuzure yunesukoekopāku) was created in 2017.[2][3] It incorporates the 1965 quasi national parks of Sobo Katamuki Prefectural Natural Park (Ōita)[4] (also previously known as the Sobo-Katamuki Quasi-National Park, Sobo Katamuki Prefectural Natural Park (祖母傾県立自然公園, Sobo Katamuki kenritsu shizen kōen)) and Sobo Katamuki Prefectural Natural Park (Miyazaki).

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Geography

The reserve derives its name from Mount Sobo (1,756 m (5,761 ft)), Mount Katamuki (傾山) (1,602 m (5,256 ft)) and Mount Ōkueyama (大崩山), also known as Mount Ōkue (1,643 m (5,390 ft)).[5][6] The Quasi-National Park borders two homonymous Prefectural Parks, namely the Sobo Katamuki Prefectural Natural Park (Ōita) and Sobo Katamuki Prefectural Natural Park (Miyazaki).[7][8]

Geology

The landforms of the Biosphere Reserve are the heavily modified result of volcanic activity over the last 14 million years. A massive eruption about 13.7 million years ago involved the Okueyama Volcano-plutonic Complex,[9] and measured 8.0 on the Volcanic Explosivity Index.[10] This formed the almost rectangular Okueyama Caldera with the eruption of an estimated dense rock equivalent (DRE) volume of 1,029 km3 (247 cu mi) leaving a caldera orientated to NW to SE that was 33 km (21 mi) by 23 km (14 mi) in size. Further eruptions over only a few million years formed the smaller more elliptical Sobo Caldera which was 18 km (11 mi) by 13 km (8.1 mi) in size on a NNE to SSW axis with a DRE erupted volume of 177 km3 (42 cu mi) and the Katamukiyama Caldera again on a NW to SE axis which was 11 km (6.8 mi) by 6 km (3.7 mi) in size with a DRE erupted volume of 50 km3 (12 cu mi).[10] Later, most recently about 90,000 years ago, mainly the lower lying land was modified by pyroclastic deposits from the Aso Caldera to the west whose eruption was 384 km3 (92 cu mi).[11]

Biosphere

There is a large amount of farmland in the large transition zone but the more rugged buffer and core areas are important flora and fauna habitats.

Flora

In the lower core and buffer areas the cover is by old-growth forest including Japanese beech and Tsuga. Rhododendron kiusianum, Japanese gentian and the Japanese maple grow in great numbers. At higher levels, the vegetation changes from evergreen (glossy-leaved) forest to conifer forest and then to Suzu-take and beech closer to mountain summits. A rare plant Angelica ubatakensis is found in the Sobo mountain range.

Fauna

The southern range limit of the Special Natural monument (特別天然記念物, tokubetsu tennen kinen-butsu), the Japanese serow lies in the Sobo mountain range. The Sobo salamander, a new species, was found here in 2014.[1] The Japanese national butterfly, the great purple emperor, an endangered species, has been seen.[1] Rare sightings have been made of the Asian black bear. Japanese dormice and sika deer are much more commonly seen.

References

  1. [1]
    "Sobo, Katamuki and Okue Biosphere Reserve (pdf)" (PDF). Sobo, Katamuki and Okue Biosphere Reserve Promotion Council. Retrieved 1 October 2022.
  2. [2]
    "Sobo, Katamuki and Okue Biosphere Reserve, Japan". UNESCO. Retrieved 1 October 2022.
  3. [3]
    "Sobo, Katamuki and Okue Biosphere Reserve". Retrieved 1 October 2022.
  4. [4]
    "Designation of the Natural Parks of Ōita Prefecture" (PDF). Ōita Prefecture. Archived from the original (PDF) on 16 January 2004. Retrieved 7 February 2012.
  5. [5]
    "壱岐対馬／九州中央山地／日豊海岸／祖母傾". National Parks Association of Japan. Archived from the original on 23 March 2012. Retrieved 7 February 2012.
  6. [6]
    "List of National Parks". Ministry of the Environment. Retrieved 7 February 2012.
  7. [7]
    "Designation of the Natural Parks of Miyazaki Prefecture" (PDF). Miyazaki Prefecture. Retrieved 7 February 2012.
  8. [8]
    "Designation of the Natural Parks of Ōita Prefecture" (PDF). Ōita Prefecture. Archived from the original (PDF) on 16 January 2004. Retrieved 7 February 2012.
  9. [9]
    Takahashi, Masaki (1986). "Anatomy of a middle Miocene Valles-type caldera cluster: Geology of the Okueyama volcano-plutonic complex, southwest Japan". Journal of Volcanology and Geothermal Research. 29 (1–4): 33–70. doi:10.1016/0377-0273(86)90039-9.
  10. [10]
    Daisuke, Miura; Yutaka, Wada (2007). "Middle Miocene ash-flow calderas at the compressive margin of southwest Japan arc: Review and synthesis". The Journal of the Geological Society of Japan. 113 (7): 283–295. doi:10.5575/geosoc.113.283. Retrieved 8 August 2019.
  11. [11]
    "Aso GeoPark Annex 2：Geological Heritage" (PDF). Retrieved 25 September 2022.
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