Mount Shari 斜里岳

Mount Shari (only) is a volcano located in the Intangular Peninsula at Hokkaido east. The top of the mountain is located at the border of three cities. The altitude is 1,547 meters. It's the fourth volcano that was active some 300,000 to 250,000 years ago, and the volcano is made up of compound volcanoes and lava domes. From the top of the mountain to the side of the mountain is designated Mount Shari Road Park. Also selected as one of the the 100 Famous Japanese Mountainss by Harada Kun.

A geographical name

To the south of the semi-arid plain, we can connect the volcano range to the well-known mountain and to the Axe Square. Depending on how you look at it, there are great differences in mountain formations, and from the coastal city, there are proportionate triangles and two peaks that stand out from the city side. In the south, the ridges follow Mount Shari from the top of the mountain. It's also called the "Ohotsk Man." Aine is called "onnepone-nupuri," meaning "great old mountain." In modern history, the names of the mountains are already on record, and in Kondo's book "The Sasai's Deity," the "Saiyama" is seen as "Saiyama." At Ming's Ming period, it is listed as "Samiji" and "Santa," "Hokkaido" and "The Business Report" by the pioneers.

Geological formation history

This is Hokkaido. According to the Centers for Scientific Technology and Geological Survey, the main period of activity is the midterm update, and the age of activity is dated around 300,000 to 250,000 years ago. The volcano is made up of compound volcanoes and lava domes, and the main rocks are Fukuyama, Daily, and basalt rocks. Akira Takeda and her friends divide the history of the formation of the volcano into two stages between the ages and the new phases. During the old age, lava eruptions formed major volcanic layers, and some of them had rock pulses. During the time of the subsequent infestation, in the new period, basalt and pyongous lava poured out to cover the slopes of the ancient volcano. Rocks that go from basalt to Fukuyama to Fukuyama, and rocks that are obscurially characteristic of the Soratic system.

The natural environment

Mount Shari is designated as Mount Shari Natural Park. The park was designated in November 1980 (of 1980) and the whole area is a national forest. Near Mount Shari, there is part of a mountain range that separates the ocean from the base, and there is a difference in climate on both sides. During the winter months, seasonal weather from the northwest will affect the snowfall, and there will be more snow on the ocean side. During the summer months, while the roots receive the effects of ocean fog that flows from the Pacific side, the ocean's influence is weakened by the mountains. The vegetation changes according to altitude. At the foot of the mountain, there will be leafy leaves and needle - mixed forests consisting of Missouri, Hari, and Tomati, and at the base of the mountain there will be forested leaves and coniferous forests, which will be the main growth of the dakecana. At altitudes of 1,000 meters or higher, you can see alpine growths with ridge muscles centered at the center of the mountain. In August 1996, a group of 219 plants and plants on the Shingo track were identified and combined with the previous research records, the zXQ022X phytoplankton was identified with 272 other species, 5 other species and 1 species. The isolation of tatastas, lyngumma, honeydrills and so forth, as well as the isolation of the tadpolos, esolys, esolylys, moi pygmy, and tasionos are also characteristic of the ZX QQ022X plant group. In animals, brown bears, esosicas, ezoris, ezoangas, strip squirrels, and kita foxes live in animals. Birds are found in the forest under the mountains, in the forests of the mountains, in the forests of the sea, in the trees of the mountains, in the mountains, in the mountains, and in the high mountains in the high mountains, in the hibi.

History

According to Hokkaido's record, Shira and Nakano went up first in the winter on March 27. In 1935, the shrine of the Mount Shari was founded on top of the mountain. The following year, in 1936, when everyone was on a pre-sumption diet, international surveyors visited the countryside, and Mount Shari became the scene of observation. In the early days of the Showa, a Mount Shari area was introduced as a tourist attraction.

Climbing

On the way up the mountain in the summer, there's the Haraji and the Rural Coast on the other side of the city. Shizuru's path divides into old roads through the haiku and new roads through the ridges. These are all led together as three mountain routes. The mountaineering of the Shikoku course is located in the fifth cabin and village. Following Hanzawa from the mountain pass down to the lower two feet, we will branch out here on the old roads and the new roads. The old road follows a course that goes back to one of the most lofty mountains in the world, where the waterfalls of the water groups, the waterfalls of the feather, the waterfalls of the feather, the waterfalls of the sky, the waterfalls of the view, the seven waterfalls of the dragon god, the waterfalls of the river. The new road will reach the ridge from the bottom of the mountain and meet with the old road at the top of the mountain. As the altitude rises on the ridges, the vegetation changes from the daquecanba forest to the hinami belt. This is a route that climbs from the remote side of the town. From the mountain range, we move to the mountain peak, which is called "Akigishi."