[Chokaisan and Tobishima Geopark: Yusa and Sakata Edition] Shonai Hirano is moist with the blessings of Mt. Chokaisan

Mt. Chokai is a rare mountain with two peaks (East Chokaisan Shinzan and Nishichokaisan Nabemori) that continue from 0m above the Sea of ​​Japan to the summit at 2,236m. Because of the beauty of his appearance, he is called "Dewa Fuji."

It is an active volcano, and people living at Yusa, Sakata, and Zogata (Kisakata, Nikaho City, Akita Prefecture) and Yuri (Yuri, Yurihonjo City, Akita Prefecture) are sometimes ignite and fear Mount Chokai, which shakes the earth, and have also worshiped it as a mountain where God resides as an entity that brings rich water.


Mt. Chokai took its current form due to a large eruption during the Edo period.

Mt. Chokai began operating about 550,000 years ago, and it is said that lava covered the surface of Mt. Nishichokai (Nabemori Lava Dome/Nabemori Yogan Dome/Altitude 1,652m) about 160,000 to 20,000 years ago.

About 20,000 years ago, it was the time when Mount East Chokai was formed in the eastern part of the mountain body, and about 2,600 years ago, the summit of Mount East Chokai collapsed, and the lava formed a crater (caldera), and the deposits created the topography at the foot of the mountain.

Of the two central crater cones on Higashi-Chokaisan, Shinzan (2,236m) is a lava dome that occurred in the eruption in 1801 (Kyowa 1), and is also known as Kyowa-dake.

Mt. Chokai eruptions occurred frequently until the late Heian period (900s). After that, there were no records of eruptions in the mid-1600s, and activity started again around 1659. In 1801, the largest eruption in history occurred.

Mt. Chokai topographic map © Geographical Survey Institute of Japan

Traces of a large eruption left on the mountain and the Shonai Plain

The phreatic eruptions that began in 1800 gradually became more intense, and in late August 1801 a large explosion occurred, killing eight climbers. In 1804 (Bunka 1), a large earthquake (Shogata Earthquake) occurred, causing extensive damage to the area at the foot of the mountain.

No large-scale eruptions have occurred since then. The most recent eruption was a small-scale phreatic eruption that occurred near Mt. Shinzan in 1974, with mudflow and ash fall confirmed. Additionally, in 1987 (Showa 62), an earthquake swarm occurred.

The active volcano, Mt. Chokai, changed the shape of the earth every time an eruption or earthquake occurred, and attacked people. The traces still remain as terrain unique to the Shonai region, such as faults and lava flows. Its unique terrain is certified as , Mt. Chokai and Tobishima Geopark

Mt. Chokai and Tobishima Geopark <Information>

Lava dome Shinzan with the remains of a violent explosion

New mountain. The main shrine at the summit of Mt. Chokai Omonoki Shrine can be seen on the lower right of Mt. Shinzan ©Mt. Chokai/Tobishima Geopark

Niiyama is a lava dome that was formed during the major explosion on Mt. Higashi Chokai in 1801 , and is 70m tall from the crater field.

You can climb up to Niyama, about 5 hours and 30 minutes from the Ohiraguchi hiking trail (Yusa Town, Yamagata Prefecture) and Hokodate hiking trail (Nikaho City, Akita Prefecture), and about 20 minutes from the Omuro hut (Omuro visitor cedar/Omuro sanrojo/accommodation) located next to the main shrine of Chokaisan Omono Imijinja.

The large rock near the main shrine of the mountain peak is a volcanic bullet that flew at the time of the birth of Niiyama, weighing 300 tons. It shows how intense the Niiyama eruption was.

Lake Chokai, a crater lake full of water from melting snow

Lake Chokai, the crater lake of Mt. Nishichokai ©Mt. Chokai/Tobishima Geopark

Lake Chokai (Chokaiko/Torinoumi/Torinoumi) is a crater lake located about 1,600m above West Chokaisan, about 3km west of Niiyama (Higashi Chokaisan).

It has a diameter of about 200m and has an oval shape that is long north and south. The water is the melting of snow, and in the harsh winter, everything freezes to the bottom of the lake, which is 4.7m deep. Nearby is Torinoumi Mihama Shrine, and the accommodation facility, Mihama Hut (Mihama Shrine Cage).

Normal fault group of Mt. Chokai running along the mountainside

The Arizawa Fault seen from the viewing platform ©Mt. Chokai/Tobishima Geopark

There is a group of active faults unique to volcanoes on the mountainside of Mt. Chokai. Many of them are distributed from the horseshoe-shaped caldera of Mt. Nishichokai (Nishichokaiba-shaped caldera) to the west slope, and near Gassan Mori (1,650 m).

The active fault on Mt. Chokai is a normal fault, which is commonly found in Kyushu in Japan, and is a rare fault in northern Japan. The one on the Nishiyama side is called the Azami Fault, and it lasts for 2.5km of cliffs with a maximum drop of about 30m. The Gassanmori Fault is 1.5km long with a maximum drop of approximately 50m.


The Shonai Plain east edge fault zone continues in a straight line for 35km.

The Shonai Plain eastern edge fault zone continues in a straight line for 35km ©Mt. Chokai/Tobishima Geopark

Active faults continue in the Shonai Plain, stitching the edges of the plains. the Shonai Plain Eastern Fault Zone , and runs 35km south of Yusacho, the base of Mt. Chokai, and continues to Sakata City, Shonai Town, and Tsuruoka City.

As of 2022, the earthquake rate within 100 years in the Shonai Plain Eastern Fault Zone is 0% in the north and within 20% in the south (published on October 19, 2009, Earthquake Headquarters, Earthquake and Disaster Prevention Research Division, Ministry of Education, Culture, Sports, Science and Technology Research and Development Bureau, Ministry of Education, Culture, Sports, Science and Technology), but in the past it is said that the Shonai earthquake in 1894 (Meiji 27), and since it is a live fault, sufficient vigilance is required.


The rich water of Mt. Chokai that nourishes the Shonai plains

Marukatsu Water, one of the Yusa Motomachi springs ©Mt. Chokai/Tobishima Geopark

The Motomachi district in the center of Yuza Town is located on the alluvial fan of the Gekko River, which originates from Mt. Chokai, and is extremely rich in groundwater. Therefore, when the wells are dug, water gushes out, and there are approximately 300 of them, producing an amount of 4,200 tons per day.

Yusa Motomachi Spring Park a walking course along the Gekko River from in front of Yusa Station , offers free access to 14 self-splitting wells, with the kindness of the owner. However, although testing is OK, it is not sterilized so you can drink it at your own risk.

Yusa Motomachi Spring Group <Information>

  • Facility name: Yusa Motomachi Yusui Group (Machimeguri Park)
  • Location: Around JR Yusa Station, Yuza-cho, Yamagata Prefecture
  • Phone number: 0234-72-5666 (Yusachokai Tourism Association)
  • URL: Machimeguri Park

“Miko no Mizu” is a blessing from the mountain of God that is essential for daily life.

“Miko no Mizu”, which is carefully used as sacred spring water ©Mt. Chokai/Tobishima Geopark

The water from the Kamiko is a washing area using spring water located in Mega village in Yusa Town.

Eka is a shoreline village where the foot of the gods mountain, Chokai, sinks into the Sea of ​​Japan, and the spring water is named "Shinsen Water" because it is water drawn from the gods mountain. The spring is divided into six aquariums, divided by use.

Miko's Water <Information>

  • Facility name: Miko no Mizu
  • Location: 64 Fukiura Mega, Yusa-machi, Akumi-gun, Yamagata Prefecture
  • Phone number: 0184-62-9777 (Mt. Chokai/Tobishima Geopark Promotion Council Secretariat)
  • access
  • Car: From Yamagata Expressway Sakata Minato IC, take National Route 7 towards Akita for about 25 minutes.
  • Railway/Approximately 5 minutes walk from JR Uetsu Main Line Mega Station
  • Toilet: None
  • Parking: None
  • URL: Miko no Mizu

Google Map


Ushiwatari River and Maruike made of spring water

Mr. Maruike ©Mt. Chokai/Tobishima Geopark

The Ushiwatarigawa is a short river with a total length of about 4km in the area on the Sea of ​​Japan side of Mt. Chokai, and almost 100% of the flow is spring water. The water temperature is around 11°C throughout the year, and salmon travels upstream in autumn.

Maruike-sama (Maruike-sama) is a spring-fed pond with a diameter of approximately 20m and a depth of 3.5m located near the Ushiwatari River. It is one of the sources of the Ushiwata River, and on its banks is Maruike Shrine, whose deity is Maruike-sama.

Ushiwatagawa and Maruike <Information>

  • Facility name: Ushiwatari River and Maruike-sama
  • Phone number: 0234-72-5666 (Yusachokai Tourism Association)
  • access
  • Car: From Yamagata Expressway Sakata Minato IC, take National Route 7 towards Akita for about 25 minutes.
  • About 5 minutes by car from Fukiura Station on the Railway/JR Uetsu Main Line
  • Toilet: Available (temporary)
  • Parking: Available (free)

Google Map


Chokaisan Omonoki Shrine, whose object of worship is Mt. Chokai, the mountain of the gods.

Main shrine at the summit of Mt. Chokai Omonoki Shrine © Yusa Chokai Tourism Association

Chokaisan Daimonoki Shrine is a shrine where prayers were offered to calm the wrath of Mt. Chokai, and is said to have been founded in 564 (25th year of the 29th Emperor Kinmei Reign), in the late Kofun period. The main shrine of the summit of Mt. Chokaisan Daimono-i Shrine, at its headquarters, is located on the summit of Mt. Chokaisan, near Niiyama, and at the foot of the shrine is home to two villages called "Kuchinomiya" in two locations: Fukiura (Fukura/Touraisan Daimono-i Shrine Fukiuraguchinomiya) and Warabioka (Warabioka/Touraisan Daimono-i Shrine Warabiokaguchinomiya).

In the late Heian period, it was ranked as the No. 1 shrine in Dewa Province and is the highest shrine in Dewa Province. The main shrine at the top of the mountain is rebuilt every 20 years, just like Ise Grand Shrine.

Chokaisan Daimono-i Shrine, the main shrine of the summit <Information>

  • Facility name: Mt. Chokai Daimono I Shrine, main shrine
  • Location: Mt. Chokai summit
  • Phone number: 0234-77-2301
  • Official URL: Chokaisan Daimono I Shrine

Google Map


Mt. Chokai Omonoki Shrine Fukiuraguchinomiya © Mt. Chokai/Tobishima Geopark

Chokaisan Daimono I Shrine Fukiuraguchinomiya <Information>

  • Facility name: Mt. Chokai Daimono I Shrine Fukiuraguchinomiya
  • Location: 1 Fukura, Fukiura, Yusa-machi, Akumi-gun, Yamagata Prefecture
  • Phone number: 0234-77-2301
  • Official URL: Chokaisan Daimono I Shrine

Google Map


Mt. Chokai Omonoki Shrine Warabiokaguchinomiya ©Mt. Chokai/Tobishima Geopark

Chokaisan Daimono I Shrine Warabiokaguchinomiya <Information>

  • Facility name: Warabiokaguchinomiya, Mt. Chokaisan Daimonomi Shrine
  • Location: 51 Matsugaoka, Kamwaraoka, Yuza-machi, Akumi-gun, Yamagata Prefecture
  • Phone number: 0234-77-2301
  • Official URL: Chokaisan Daimono I Shrine

Google Map


16 Arhat Rocks carved into lava to commemorate marine accidents

16 Arhat Rocks with 22 Buddha statues carved ©Travel to Yamagata

The Jurokurakaniwa is a cliff Buddha carved into lava carved into the lava that flows out of Mt. Chokai on the coast near Fukiura Fishing Port facing the Sea of ​​Japan. There are 22 Buddhas carved together, including 16 Arhat statues (a saint who has achieved the highest level of practice), Monjubosatsu and Fugen Bodhisattva.

The Magaibutsu was carved in the first year of the Meiji era, mainly by the priest Kankai of Fukiura Kaizenji Temple, as a memorial service for the fishermen who died in maritime accidents, and a prayer for safety at sea.

16 Rakan Rocks<Information>

  • Facility name: Juroku Rakan Rock
  • Location: Fukiura Nishitate, Yusa-machi, Akumi-gun, Yamagata Prefecture
  • Phone number: 0234-72-5666 (Yusachokai Tourism Association)
  • Free tour
  • access
  • Car: Approximately 15 minutes from Yusahiko IC on the Nihonkai-Tohoku Expressway
  • Railway/Approximately 15 minutes walk from Fukiura Station on the JR Uetsu Main Line
  • URL: 16 Rakan Rocks

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