Knowledge (XXG)

Imuta-ike

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Imuta-ike is surrounded by mountains; Funamidake (498.8 metres (1,636 ft)), San-o-dake (491 metres (1,611 ft)), Katagi-yama (508.8 metres (1,669 ft)), Tōmigashiro (477 metres (1,565 ft)), Ī-moriyama (432 metres (1,417 ft), known due to its beauty also as Imuta-fuji), and
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mats. In autumn, villagers used to cut and bundle rushes. Between 1741 and 1763, a 380-meter tunnel water lane was made at the eastern end of the pond, and 15 hectares of rice fields were made. In 1953, Imuta-ike was made a
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there is no incoming large river. The outgoing water flows into Sendai River and Hiwagi River. Imuta-ike is in the last stage of the lake-pond formation cycle and is shrinking with the deposition of
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is 6.8; the water of the pond contains organic substances. There are many cherry trees around the pond. About one third of its area, to the northwest, is wetland; dotted by
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List of Special Places of Scenic Beauty, Special Historic Sites and Special Natural Monuments
398:. The lava dome formed Iimori-yama. The depression collected water and Imuta-ike was formed. 277: 559: 431: 343: 269: 407: 616: 402: 312: 232: 126: 316: 228: 131: 252: 38: 439: 391: 375: 332: 297: 225: 109: 96: 301: 288:
a Natural Monument as the "peat forming vegetation of Imuta-ike" in 1921.
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Between 300,000 and 400,000 years ago, there were groups of
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0.0005 cubic kilometres (18,000,000 cu ft)
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Index


Kagoshima Prefecture
Ramsar Site
Location of Imuta-ike in Japan.
Kagoshima Prefecture
31°49′N 130°28′E / 31.817°N 130.467°E / 31.817; 130.467
Type
caldera lake
Ramsar Wetland
freshwater
caldera lake
Satsumasendai
Kagoshima Prefecture
Imutaike Prefectural Natural Park
Natural Monument of Japan
wetlands
Ramsar Site
sediment
Forel-Ule scale
pH
floating islands
peat
designated
phragmites
wild rice
brasenia
water caltrop
Zacco platypus
Black bass
Carassius langsdorfii

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