Shimokita Peninsula

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Shimokita Peninsula
Shimokita Peninsula Relief Map, SRTM-1.jpg
Topographic map
LocationAomori Prefecture, Japan
Surface elevation0 meters
Highest point
 – elevation
Mount Kamafuse
879 meters
Area1,876.86 square kilometres (724.66 sq mi)
Location of Shimokita Peninsula in Japan

Shimokita Peninsula (下北半島, Shimokita-hantō) is the remote northeastern cape of the Japanese island of Honshū, stretching out towards Hokkaidō. It is bordered by the Pacific Ocean to the east, Tsugaru Strait to the north and Mutsu Bay to the west and south. Shaped like an axe pointing west, the peninsula has a thin "axe handle" connecting the mountainous "axe blade" to the mainland of Honshū to the south. The peninsula contains the northernmost point on Honshū, Cape Ōma, and the largest sand dunes in Japan (the Sarugamori Sand Dunes).

Administratively the area is a part of Aomori Prefecture, and the bulk of the area falls within the jurisdiction of the city of Mutsu, with a number of small towns and villages along the periphery. Most of the inhabitants live in coastal areas rather than the mountainous interior.

Portions of the peninsula are within the borders of Shimokita Hantō Quasi-National Park, including Cape Ōma, the coastline of the village of Sai to the south, including seaside cliffs said to resemble Buddhas at Hotokegaura, Cape Shiriya to the northeast, and the volcanic interior of the peninsula, including Mount Osore and Lake Usori. Tourist attractions include Yagen Valley, known for its hot springs.

Economically, the mainstays of the local economy are commercial fishing, forestry, and seasonal tourism. The main commercial centre is the city of Mutsu. The village of Rokkasho, at the southern end of Shimokita Peninsula, home to a range of nuclear facilities.

In 2012, Japan set a new world record for ocean drilling depth, reaching 2,111 meters below the seafloor off Shimokita Peninsula.[1]

Since the Eemian interglacial some 125,000 years ago the coast of the eastern tip of the peninsula has been uplifted on average 0.14–0.25 meters every thousand years (m/kyr). Slightly to the west the a north-facing sandy coast has uplift rates of 0.14–0.23 m/kyr for the same period. Further to the west, on top of the trace line of the volcanic front rates over the same period are in the order of 0.09–0.18 m/kyr.[2] This uplift is related to the activity of offshore geological faults that has bended strata into an anticline.[2]

This peninsula is also called “ Axe Peninsula ” from the shape.

See also[edit]

External links[edit]

Media related to Shimokita Peninsula at Wikimedia Commons Shimokita Peninsula travel guide from Wikivoyage


  1. ^ "Chikyu sets a new world drilling-depth record of scientific ocean drilling". Science Daily. September 6, 2012. Retrieved 4 March 2017.
  2. ^ a b Matsu'ura, Tabito; Kimura, Haruo; Komatsubara, Junko; Goto, Norihisa; Yanagida, Makoto; Ichikawa, Kiyoshi; Furusawa, Akira (2014). "Late Quaternary uplift rate inferred from marine terraces, Shimokita Peninsula, northeastern Japan: A preliminary investigation of the buried shoreline angle". Geomorphology. 209: 1–17.