A family will introduce the situation of Oze photoed for the travel in June this time.
Oze is located in each border between prefectures in Gumma Katashina-mura, Fukushima Hinoemata-mura, and Yunotani-mura,
Niigata, and 4km of 6km of east-and-west north-south gross area is the greatest high moor in a certain Japan also like about 8700 ha(s).
If the weather avoids as sung with "recollections of summer", it can just be going to carry out skilled [ of the wonderful scenery ].
Oze is specified as the quasi-national park of the country as Nikko National Park in 1934 (Showa 9). Moreover, it was specified as the special refuge in Nikko National Park after that in 1953 (Showa 28), and is specified also as the special natural treasure in 1960 (Showa 35). This is because many very precious plants exist even if it finds scientifically that the plant of the glacial epoch age grows wild still now etc., since chill [ the climate of Oze ]. Oze is divided roughly into two areas of Ozenuma with an altitude of 1665m located in Ozegahara which is in the altitude of 1400m and is located in Gumma Prefecture, and the Fukushima side. It is the section from the entrance of Ozegahara Gumma to a Hatomachi peak - Yamanohana-Ushikubi-ShimonoOohori-Ryugujyujiro which the family's person performed this time. Since it is too much vast, in a day's trip, it cannot finish being going just turning at all. It is said that the Tadami river was dammed up by the process of the volcanic activity with an altitude of 2356m which belongs to Nasu volcanic zone by the highest peak of the Tohoku district of Hiuchigadake by the lava flow by pre- eruption activities in about 8000, and the history of Oze was able to do Ozenuma. The water which flows out of the Oze marshland serves as the origin of the Tadami river through the waterfall of Sanjyo which is the only exit for the basin which had the four quarters surrounded by mountains with the Mt. Shibutsu altitude of 2228m, Hiuchigadake, a Hakamagoshi mountain altitude of 2042m, and a Nakahara mountain altitude of 1969m. The Oze marshland is covered with the exit of the water which merely flows out of the Oze marshland only for here one place, without melted snow and the rain which fell gathering and falling out in the geographical feature on a basin, it spends years there further, and is the influence of the cold, cool climate of five annual average temperature order,It is said that it deposits without the withered aquatic plant and swamp vegetation rotting, a 5-m-thick high-rise peat bed is made, and the high moor of present Oze was made. It is said that it was a reason that it is inconvenient for man walking along a marshland those days which built the first mokudo to the interesting thing although a way called mokudo in which Oze has about 57km of the total extension being made, and coming down into a marshland directly was forbidden. That is, when mokudo was made in order to take care of the person included in Oze, is it? It is said that it changed to the purpose of protecting a marshland conversely as the conservation movement increased. There is history that that to which the Tokyo Electric Power which is also an owner of the land here Gumma was going to build the dam for water-power generation here for electric power shortage dissolution of the Kanto district before once suffered a setback in the opposition movement. Although I myself was not carrying out this time, the weather seemed to be unsatisfactory in the midst of the rainy season. Since a family's person is taking a photograph, the lightweight Tamron lens is used.