Mount Ōdaigahara 大台ヶ原山

The highest grade triangle is the Mount Ōdaigahara, but a map by the National Geographic Museum describes it as an altitude of 1695.1m. Administratively spreading to NaraYOYOYOYOYOYOYOYO and to the Mie The area that extends around us at 1,300 feet [1600 m] above sea level is called Otahara. Otahara was designated as part of Yoshinobu's National Park and is designated as a special protected area to protect the landscape. In 1980, the United Nations Educational, Scientific, and Cultural Organization's Biosphere Reserve was registered as the "Sakihara, Oyama, and Osama Valley." As "Mount Ōdaigahara," he was chosen by Harada Kunji the 100 Famous Japanese Mountains. It's also chosen as "Mount Ōdaigahara" and as "Otahara/ Ojidani" for 100 secret Japanese borders.

Overview

The main building is located south of the central structure line, and as the ocean plate crawls below the Eulerian plate, sandstones and charts deposited on the ocean plate are thought to have been pushed up to the edge of the Eurasian plate and raised. In Japan, Otahara is described as the rare non - volcanocite ridge level. On the other hand, if you look at the earth's geological structure around you, there is a theory that a giant eruption occurred 15 million years ago, that a great caldera was formed, and that it forms a subsoil caldron, which was then destroyed by an infestation. The main building contains mountains between 2,500 and 1,600 meters above sea level, such as Mount Mizugawa and Akiyama. The west and the south form a terrain with a depth of 1,000 meters by mountain ridges and grindings, and a surface made of hard rocks. The southeast is the real coast facing Kunobu, and the main building is at the top of the steep slope from the coast. Since the steep southeast slope is blown from the sea by a wet wind, it is such a rainy land that it has more rainfall throughout the year and is said to line up on the island. Especially as a typhoon passes through the Pacific side of the Japanese islands, the wind from the southeast increases, and there is much rainfall around the center of October. In the 1920 ' s, we recorded 8,214 millimeters of rain a year, and on September 14th, 1923, we have 1,011 millimeters of rain records per day.

Eclipse

In the southeast of Otahara, in the southeast of Takakigahara, and in the bull-sahara, you can see the dead and the dead. This was due to the typhoons that swept through the area in 1959, which destroyed the forest, and brought sunshine to the surface, and the moss began to decline, and the mexosa began to thrive. The dense vegetation of the miya palm has led to an increase in the number of elk that feed on these animals, and trees and bark that make up the forest of the main forest are being eaten on the deer. Other factors, such as human and global environmental change, are thought to be in the process of deforesting the forest. Although the Ministry of Environment has conducted (a control of the population as a large effect on the environment), conservation groups have agreed that the effect of the deer's change is unknown and that it should not be eliminated. And that's what we're going to do. It's called the "Dai-ga-hara-Sanfish." Akagera. Nihon deer. It's called the Snoopy Bear. Nihon deer. Toads. Rilivitaki. The warbler.

The climbing sightseeing

The main building is designated as part of Yoshinobu's National Park, and at a point around the center, at altitudes of 1,573.7 meters, there is the "Great Hotel Visitors Center" building as a facility to introduce the nature and history of the main building. The Visitors Center has more than 200 parking lots available, and stores, restaurants and shelters are available around it. In addition to having multiple routes to go around the Visitors Center, mountaineering has been established from the Great Valley at the foot of the east side. It is estimated that since the main highway opened in 1961, the easy way to reach mountains and the increase in mountain climbers and tourists has also had an effect on nature.

Tohoku Ota

The area east of the Visitors Center is called the Tohoku main, and the course for the mountain climbers is equipped with the "East Line of Natural Observation." The summit of Mount Hagu is located at the northeastern end of the Tohoku Line, and the mountain roads pass southwest along the ridges and through the boulders.

I'll take care of it

(The western sector from the Visitors Center is called the Western main building, so that it will maintain its natural environment and provide natural experience, and so the Department of Environment has a limited number of people coming in each day, 30 to 100 per day, depending on the day of the week or season.) Also, you have to apply to get in and get your fee and receive a lecture by the end of the day. It's the principle that the application be done in advance, but with the frame, you can also do it on the day. To the west tower is a gate through the Visitors Center and through the southwest reverse pass.

Forestry

A four-day newspaper bought 8000 square feet of forest in Tohokuga. We built an exit route that combined inkline, research, and easy-to-go railways to the town of Mie. From 1916 to 1972, they cut down the trees, cut down the trees, cut down the trees, cut down the trees, brought them out. When White-Trouro of Tokyo's Imperial University gave a speech on the subject, the conservation movement was more active than the local Kusada-sama men. In 1925, and with all four-day paper combined, he's got a lot of expensive logging costs and the low timber market, so he stopped logging in the east. After that, the forest there was designated a security forest.

The main mountain around us

From the top of the mountain and from the top of the mountain, you can look across Iseyama in both the north and the west. The source is the National Geographic Society's Standards and View Service.