Geography of Japan

The Japanese archipelago is relatively far away from the Asian continent. Kyushu is closest to the southernmost point of the Korean peninsula with a distance of 190 km (120 mi), which is almost 6 times farther away than from England to France across the English Channel. Thus historically Kyushu was the gateway between Asia and Japan. China is separated by 800 km (500 mi) of sea from Japan's big main islands. Hokkaido is near Sakhalin, which was occupied by Japan from 1905 to 1945. Most of the population lives on the Pacific coast side of Honshū. The west coast facing the Sea of Japan is less densely populated.[21]

The Japanese archipelago was difficult to reach since before ancient history. During the Paleolithic period around 20,000 BCE at the height of the Last Glacial Maximum, there was a land bridge between Hokkaido and Sakhalin which linked Japan with the Asian continent. The land bridge disappeared when the sea levels rose in the Jōmon period around 10,000 BCE.[22]

Japan's remote location, surrounded by vast seas, rugged, mountainous terrain and steep rivers make it secure against invaders and uncontrolled migration from the Asian continent. The Japanese can close their civilization with an isolationist foreign policy. During the Edo period the Tokugawa Shogunate enforced the Sakoku policy which prohibited most foreign contact and trade from 1641 to 1853.[23] In modern times, the inflow of people is managed via the seaports and airports. Thus Japan is fairly insulated from continental issues.

Throughout history, Japan was never fully invaded nor colonized by foreigners. The Mongols tried to invade Japan twice and failed in 1274 and 1281. Japan capitulated only once after nuclear attacks in World War II. At the time Japan did not have nuclear technology. The insular geography is a major factor for the isolationist, semi-open and expansionist periods of Japanese history.

The mountainous islands of the Japanese archipelago form a crescent off the eastern coast of Asia.[24] They are separated from the continent by the Sea of Japan, which serves as a protective barrier. Japan has 108 active volcanoes (10% of the world's active volcanoes) because of active plate tectonics in the Ring of Fire.[16]

The Japanese islands are the summits of mountain ridges uplifted near the outer edge of the continental shelf.[24] About 73 percent of Japan's area is mountainous, and scattered plains and intermontane basins (in which the population is concentrated) cover only about 27 percent.[24] A long chain of mountains runs down the middle of the archipelago, dividing it into two halves, the "face", fronting on the Pacific Ocean, and the "back", toward the Sea of Japan.[24] On the Pacific side are steep mountains 1,500 to 3,000 meters high, with deep valleys and gorges.[24]

Central Japan is marked by the convergence of the three mountain chains—the Hida, Kiso, and Akaishi mountains—that form the Japanese Alps (Nihon Arupusu), several of whose peaks are higher than 3,000 metres (9,800 ft).[24] The highest point in the Japanese Alps is Mount Kita at 3,193 metres (10,476 ft).[24] The highest point in the country is Mount Fuji (Fujisan, also erroneously called Fujiyama), a volcano dormant since 1707 that rises to 3,776 m (12,388 ft) above sea level in Shizuoka Prefecture.[24] On the Sea of Japan side are plateaus and low mountain districts, with altitudes of 500 to 1,500 meters.[24]

Map of the Kantō Plain

There are three major plains in central Honshū. The largest is the Kantō Plain which covers 17,000 km² (6,600 sq mi) in the Kantō region. The capital Tokyo and the largest metropolitan population is located there. The second largest plain is the Nōbi Plain 1,800 km² (690 sq mi) with the third-most-populous urban area Nagoya. The third largest plain is the Osaka Plain which covers 1,600 km² (620 sq mi) in the Kinki region. It features the second largest urban area of Osaka (part of the Keihanshin metropolitan area). Osaka and Nagoya extend inland from their bays until they reach steep mountains. The Osaka Plain is connected with Kyoto and Nara. Kyoto is located in the Yamashiro Basin 827.9 km² (319.7 sq mi) and Nara is in the Nara Basin 300 km² (120 sq mi).

The Kantō Plain, Osaka Plain and Nōbi Plain are the most important economic, political and cultural areas of Japan. These plains had the largest agricultural production and large bays with ports for fishing and trade. This made them the largest population centers. Kyoto and Nara are the ancient capitals and cultural heart of Japan. The Kantō Plain became Japan's center of power, because it is the largest plain with a central location and historically it had the most agricultural production that could be taxed. The Tokugawa Shogunate established a bakufu in Kamakura in 1603.[25] This evolved into the capital of Tokyo by 1868.

Hokkaido has multiple plains such as the Ishikari Plain 3,800 km² (1,500 sq mi), Tokachi Plain 3,600 km² (1,400 sq mi), the Kushiro Plain is the largest wetland in Japan 2,510 km² (970 sq mi) and Sarobetsu Plain 200 km² (77 sq mi). There are many farms that produce a plethora of agricultural products. The average farm size in Hokkaido is 26 hectares per farmer in 2013. That is nearly 11 times larger than the national average of 2.4 hectares. This made Hokkaido the most agriculturally rich prefecture of Japan.[26] Nearly one fourth of Japan's arable land and 22% of Japan's forests are in Hokkaido.[27]

Another important plain is the Sendai Plain around the city of Sendai in northeastern Honshū.[24] Many of these plains are along the coast, and their areas have been increased by land reclamation throughout recorded history.[24]

Aerial view of Shinano River

Rivers are generally steep and swift, and few are suitable for navigation except in their lower reaches. Although most rivers are less than 300 km (190 mi) in length, their rapid flow from the mountains is what provides hydroelectric power.[24] Seasonal variations in flow have led to extensive development of flood control measures.[24] The longest, the Shinano River, which winds through Nagano Prefecture to Niigata Prefecture and flows into the Sea of Japan, is 367 km (228 mi) long.[24][28]

These are the 10 longest rivers of Japan.[28]

Aerial view of Lake Biwa

The largest freshwater lake is Lake Biwa 670.3 km² (258.8 sq mi), northeast of Kyoto in Shiga Prefecture.[29] Lake Biwa is an ancient lake and estimated to be the 13th oldest lake in the world dating to at least 4 million years ago.[30][29] It has consistently carried water for millions of years. Lake Biwa was created by plate tectonics in an active rift zone. This created a very deep lake with a maximum depth of 104 m (341 ft). Thus it has not naturally filled with sediment. Over the course of millions of years, a diverse ecosystem evolved in the lake. It has more than 1,000 species and subspecies. There are 46 native fish species and subspecies,[31] including 11 species and 5 subspecies that are endemic or near-endemic.[29] Approximately 5,000 water birds visit the lake each year.

The following are the 10 largest lakes of Japan.[32]

Seto Inland Sea

Extensive coastal shipping, especially around the Seto Inland Sea, compensates for the lack of navigable rivers.[24] The Pacific coastline south of Tokyo is characterized by long, narrow, gradually shallowing inlets produced by sedimentation, which has created many natural harbors.[24] The Pacific coastline north of Tokyo, the coast of Hokkaidō, and the Sea of Japan coast are generally unindented, with few natural harbors.[24]

Kobe Airport in Osaka Bay

The Japanese archipelago has been transformed by humans into a sort of continuous land, in which the four main islands are entirely reachable and passable by rail and road transportation thanks to the construction of huge bridges and tunnels that connect each other and various islands.[33]

Approximately 0.5% of Japan's total area is reclaimed land (umetatechi).[34] It began in the 12th century.[34] Land was reclaimed from the sea and from river deltas by building dikes and drainage and rice paddies on terraces carved into mountainsides.[24] The majority of land reclamation projects occurred after World War II during the Japanese economic miracle. Reclamation of 80% to 90% of all the tidal flatland was done. Large land reclamation projects with landfill were done in coastal areas for maritime and industrial factories, such as Higashi Ogishima in Kawasaki, Osaka Bay and Nagasaki Airport. Port Island, Rokkō Island and Kobe Airport were built in Kobe. Late 20th and early 21st century projects include artificial islands such as Chubu Centrair International Airport in Ise Bay, Kansai International Airport in the middle of Osaka Bay, Yokohama Hakkeijima Sea Paradise and Wakayama Marina City.[34] The village of Ogata in Akita, was established on land reclaimed from Lake Hachirōgata (Japan's second largest lake at the time) starting in 1957. By 1977, the amount of land reclaimed totaled 172.03 square kilometres (66.42 sq mi).[35]

Examples of land reclamation in Japan include:

• Kyogashima, Kobe – first man-made island built by Tairano Kyomori in 1173[34]
• The Hibiya Inlet, Tokyo – first large scale reclamation project started in 1592[34]
• Dejima, Nagasaki – built during Japan's national isolation period in 1634. It was the sole trading post in Japan during the Sakoku period and was originally inhabited by Portuguese and then Dutch traders.[34]
• Tokyo Bay, Japan – 249 square kilometres (96 sq mi)[36] artificial island (2007).
  • This includes the entirety of Odaiba, a series of island forts constructed to protect Tokyo from sea attacks (1853).[34]
• Kobe, Japan – 23 square kilometres (8.9 sq mi) (1995).[34]
• Isahaya Bay in the Ariake Sea – approximately 35 square kilometres (14 sq mi) is reclaimed with tide embankment and sluice gates (2018).
• Yumeshima, Osaka – 390 hectares (960 acres) artificial island (2025).
• Central Breakwater - 989 hectares (2,440 acres)

Much reclaimed land is made up of landfill from waste materials, dredged earth, sand, sediment, sludge and soil removed from construction sites. It is used to build man-made islands in harbors and embankments in inland areas.[34] From November 8, 2011, Tokyo City began accepting rubble and waste from the 2011 Tōhoku earthquake and tsunami region. This rubble was processed, and when it had the appropriate radiation levels it was used as landfill to build new artificial islands in Tokyo Bay. Yamashita Park in Yokohama City was made with rubble from the great Kantō earthquake in 1923.[34]

There is a risk of contamination on artificial islands with landfill and reclaimed land if there was industry that spilled (toxic) chemicals into the ground. For example, the artificial island Toyosu was once occupied by a Tokyo gas factory. Toxic substances were discovered in the soil and groundwater at Toyosu. The Tokyo Metropolitan Government spent an additional 3.8 billion yen ($33.5 million) to pump out groundwater by digging hundreds of wells.[37] In June 2017, plans to move the Tsukiji fish market were restarted[38] but delayed in July to the autumn of 2018.[39] After the new site was declared safe following a cleanup operation, Toyosu Market was opened.[40]

The Japanese archipelago is the result of subducting tectonic plates over several 100 millions of years from the mid-Silurian (443.8 Mya) to the Pleistocene (11,700 years ago). Approximately 15,000 km (9,300 mi) of oceanic floor has passed under the Japanese archipelago in the last 450 million years, with most being fully subducted. It is considered a mature island arc.

The islands of Japan were created by tectonic plate movements

• Tohoku (upper half of Honshu), Hokkaido, Kuril islands and Sakhalin are located on the Okhotsk Plate. This is a minor tectonic plate bounded to the north by the North American Plate.[41][42] The Okhotsk Plate is bounded on the east by the Pacific Plate at the Kuril-Kamchatka Trench and the Japan Trench. It is bounded on the south by the Philippine Sea Plate at the Nankai Trough. On the west it is bounded by the Eurasian Plate and possibly on the southwest by the Amurian Plate. The northeastern boundary the Ulakhan Fault.[43]
• The southern half of Honshu, Shikoku and most of Kyushu are located on the Amurian Plate.
• The southern tip of Kyushu and the Ryukyu islands are located on the Okinawa Plate.
• The Nanpō Islands are on the Philippine Sea Plate.

The Pacific Plate and Philippine Sea Plate are subduction plates. They are deeper than the Eurasian plate. The Philippine Sea Plate moves beneath the continental Amurian Plate and Okinawa Plate to the south. The Pacific Plate moves under the Okhotsk Plate to the north. These subduction plates have pulled Japan eastward and opened the Sea of Japan by back-arc spreading around 15 million years ago.[14] The Strait of Tartary and the Korea Strait opened much later. La Pérouse Strait formed about 60,000 to 11,000 years ago closing the path used by mammoths which had earlier moved to northern Hokkaido.[44]

The subduction zone is where the oceanic crust slides beneath the continental crust or other oceanic plates. This is because the oceanic plate's litosphere has a higher density. Subduction zones are sites that usually have a high rate of volcanism and earthquakes.[45] Additionally, subduction zones develop belts of deformation[46] The subduction zones on the east side of the Japanese archipelago cause frequent low intensity earth tremors. Major earthquakes, volcanic eruptions and tsunamis occur several times per century. It is part of the Pacific Ring of Fire.[14] Northeastern Japan, north of Tanakura fault, had high volcanic activity 14–17 million years before present.[47]

Red line represents Median Tectonic Line. Orange shaded region is Fossa Magna, bounded by the Itoigawa-Shizuoka Tectonic Line (western blue line).

The Japan Median Tectonic Line (MTL) is Japan's longest fault system.[48][49] The MTL begins near Ibaraki Prefecture, where it connects with the Itoigawa-Shizuoka Tectonic Line (ISTL) and the Fossa Magna. It runs parallel to Japan's volcanic arc, passing through central Honshū to near Nagoya, through Mikawa Bay, then through the Seto Inland Sea from the Kii Channel and Naruto Strait to Shikoku along the Sadamisaki Peninsula and the Bungo Channel and Hōyo Strait to Kyūshū.[49]

The MTL moves right-lateral strike-slip, at about 5–10 millimeters per year.[50] The sense of motion is consistent with the direction of the Nankai Trough's oblique convergence. The rate of motion on the MTL is much less than the rate of convergence at the plate boundary. This makes it difficult to distinguish the motion on the MTL from interseismic elastic straining in GPS data.[51]

Map depicts the Kuril–Kamchatka Trench, Japan Trench, Izu-Ogasawara Trench and Mariana Trench

East of the Japanese archipelago are three oceanic trenches.

• The Kuril–Kamchatka Trench is in the northwest Pacific Ocean. It lies off the southeast coast of Kamchatka and parallels the Kuril Island chain to meet the Japan Trench east of Hokkaido.[52]
• The Japan Trench extends 8,000 km (4,971 mi) from the Kuril Islands to the northern end of the Izu Islands. Its deepest part is 8,046 m (26,398 ft).[53] The Japan Trench is created as the oceanic Pacific Plate subducts beneath the continental Okhotsk Plate. The subduction process causes bending of the down going plate, creating a deep trench. Continuous movement on the subduction zone associated with the Japan Trench is one of the main causes of tsunamis and earthquakes in northern Japan, including the megathrust 2011 Tōhoku earthquake and tsunami. The rate of subduction associated with the Japan Trench has been recorded at about 7.9–9.2 cm (3.1–3.6 in)/yr.[15]
• The Izu-Ogasawara Trench is south of the Japan Trench in the western Pacific Ocean. It consists of the Izu Trench (at the north) and the Bonin Trench (at the south, west of the Ogasawara Plateau).[54] It stretches to the northernmost section of the Mariana Trench.[55] The Izu-Ogasawara Trench is an extension of the Japan Trench. There the Pacific Plate is being subducted beneath the Philippine Sea Plate, creating the Izu Islands and Bonin Islands on the Izu-Bonin-Mariana Arc system.[56]

The Japanese islands are formed of the mentioned geological units parallel to the subduction front. The parts of islands facing the Pacific Ocean's Plate are typically younger and display a larger proportion of volcanic products, while island parts facing the Sea of Japan are mostly heavily faulted and folded sedimentary deposits. In northwest Japan are thick quaternary deposits. This makes determination of the geological history and composition difficult and it is not yet fully understood.[57]

The Japanese island arc system has distributed volcanic series where the volcanic rocks change from tholeiite—calc-alkaline—alkaline with increasing distance from the trench.[58][59] The geologic province of Japan is mostly basin and a bit extended crust.[60]

During the Pleistocene (2.58 million years BCE) glacial cycles, the Japanese islands may have occasionally been connected to the Eurasian Continent via the Korea Strait and the Korean Peninsula or Sakhalin. The Sea of Japan was considered to be a frozen inner lake because of the lack of the warm Tsushima Current. Various plants and large animals, such as the Palaeoloxodon naumanni migrated into the Japanese archipelago.[71]

The Sea of Japan was a landlocked sea when the land bridge of East Asia existed circa 18,000 BCE. During the glacial maximum the marine elevation was 200 meters lower than present. Thus Tsushima island in the Korea Strait was a land bridge that connected Kyushu and the southern tip of Honshu with the Korean peninsula. There was still several kilometers of sea to the west of the Ryukyu islands, and most of the Sea of Japan was open sea with a mean depth of 1,752 m (5,748 ft). Comparatively, most of the Yellow Sea (Yellow Plane) had a semi-arid climate (dry steppe), because it was relatively shallow with a mean depth of 44 m (144 ft). The Korean Peninsula was landlocked on the entire west and south side in the Yellow Plane.[72] The onset of formation of the Japan Arc was in the Early Miocene (23 million years ago).[73] The Early Miocene period was when the Sea of Japan started to open, and the northern and southern parts of the Japanese archipelago separated from each other.[73] The Sea of Japan expanded during the Miocene.[73]

The northern part of the Japanese archipelago was further fragmented until orogenesis of the northeastern Japanese archipelago began in the Late Miocene. The orogenesis of the high mountain ranges in northeastern Japan started in the Late Miocene and lasted in the Pliocene.[73] The south part of the Japanese archipelago remained as a relatively large landmass. The land area expanded northward during the Miocene.[73]

Vegetation during the Last Glacial Maximum period 16,000 BCE

During the advance of the last Ice Age, the world sea level dropped. This dried and closed the exit straits of the Sea of Japan one by one. The deepest, and thus the last to close, was the western channel of the Korea Strait. There is controversy as to whether the Sea of Japan became a huge cold inland lake.[71] The Japanese archipelago had a taiga biome (open boreal woodlands). It was characterized by coniferous forests consisting mostly of pines, spruces and larches. Hokkaido, Sakhalin, and the Kuril islands had mammoth steppe biome (steppe-tundra). The vegetation was dominated by palatable high-productivity grasses, herbs and willow shrubs.

The Sea of Japan has a surface area of 978,000 km² (378,000 sq mi), a mean depth of 1,752 m (5,748 ft) and a maximum depth of 3,742 m (12,277 ft). It has a carrot-like shape, with the major axis extending from southwest to northeast and a wide southern part narrowing toward the north. The coastal length is about 7,600 km (4,700 mi) with the largest part (3,240 km or 2,010 mi) belonging to Russia. The sea extends from north to south for more than 2,255 km (1,401 mi) and has a maximum width of about 1,070 km (660 mi).[74]

There are three major basins: the Yamato Basin in the southeast, the Japan Basin in the north and the Tsushima Basin in the southwest.[44] The Japan Basin has an oceanic crust and it is the deepest part of the sea, whereas the Tsushima Basin is the shallowest with depths below 2,300 m (7,500 ft). The Yamato Basin and Tsushima Basin have thick ocean crusts.[74] The continental shelves of the sea are wide on the eastern shores along Japan. On the western shores, they are narrow particularly along the Korean and Russian coast, averaging about 30 km (19 mi).

The geographical location of the Japanese archipelago has defined the Sea of Japan for millions of years. Without the Japanese archipelago it would just be the Pacific Ocean. The term has been the international standard since at least the early 19th century.[75] The International Hydrographic Organization, the international governing body for the naming bodies of water around the world, in 2012 recognized the term "Sea of Japan" as the only title for the sea.[76]

There are small deposits of coal, oil, iron and minerals in the Japanese archipelago.[2] Japan is scarce in critical natural resources and has long been heavily dependent on imported energy and raw materials.[2][83] The oil crisis in 1973 encouraged the efficient use of energy.[84] Japan has therefore aimed to diversify its sources and maintain high levels of energy efficiency.[85] In regards to agricultural products, the self-sufficiency rate of most items is less than 100% except for rice. Rice has a 100% food self-sufficiency. This makes it difficult to meet Japan's food demand without imports.

Japan's exclusive economic zones:

  Japan's EEZ

  Joint regime with Republic of Korea

  EEZ claimed by Japan, disputed by others

The Exclusive economic zone of Japan has an estimated large quantities of mineral resources such as methane clathrate, natural gas, metallic minerals and rare-earth mineral reserves. Seabed mineral resources such as manganese nodules, cobalt-rich crust and submarine hydrothermal deposits are located at depths over 1,000 m (3,300 ft).[5] Most of these deep sea resources are unexplored at the seabed. Japan's mining law restricts offshore oil and gas production. There are technological hurdles to mine at such extreme depths and to limit the ecological impact. There are no successful commercial ventures that mine the deep sea yet. So currently there are few deep sea mining projects to retrieve minerals or deepwater drilling on the ocean floor.

It is estimated that there are approximately 40 trillion cubic feet of methane clathrate in the eastern Nankai Trough of Japan.[86] As of 2019, the methane clathrate in the deep sea remains unexploited, because the necessary technology is not established yet. This is why currently Japan has very limited proven reserves like crude oil.

The Kanto region alone is estimated to have over 400 billion cubic meters of natural gas reserves. It forms a Minami Kantō gas field in the area spanning Saitama, Tokyo, Kanagawa, Ibaraki, and Chiba prefectures. However, mining is strictly regulated in many areas because it is directly below Tokyo, and is only slightly mined in the Bōsō Peninsula. In Tokyo and Chiba Prefecture, there have been frequent accidents with natural gas that was released naturally from the Minami Kantō gas field.[87]

In 2018, 250 km (160 mi) south of Minami-Tori-shima at 5,700 m (18,700 ft) deep, approximately 16 million tons of rare-earth minerals were discovered by JAMSTEC in collaboration with Waseda University and the University of Tokyo.[88]

Japan maintains one of the world's largest fishing fleets and accounts for nearly 15% of the global catch (2014).[2] In 2005, Japan ranked sixth in the world in tonnage of fish caught.[6] Japan captured 4,074,580 metric tons of fish in 2005, down from 4,987,703 tons in 2000 and 9,864,422 tons in 1980.[89] In 2003, the total aquaculture production was predicted at 1,301,437 tonnes.[90] In 2010, Japan's total fisheries production was 4,762,469 fish.[91] Offshore fisheries accounted for an average of 50% of the nation's total fish catches in the late 1980s although they experienced repeated ups and downs during that period.[24]

As of 2011, 46.1% of energy in Japan was produced from petroleum, 21.3% from coal, 21.4% from natural gas, 4.0% from nuclear power and 3.3% from hydropower. Nuclear power is a major domestic source of energy and produced 9.2 percent of Japan's electricity, as of 2011, down from 24.9 percent the previous year.[92] Following the 2011 Tōhoku earthquake and tsunami disaster in 2011, the nuclear reactors were shut down. Thus Japan's industrial sector became even more dependent than before on imported fossil fuels. By May 2012 all of the country's nuclear power plants were taken offline because of ongoing public opposition following the Fukushima Daiichi nuclear disaster in March 2011, though government officials continued to try to sway public opinion in favor of returning at least some of Japan's 50 nuclear reactors to service.[93] Shinzo Abe’s government seeks to restart the nuclear power plants that meet strict new safety standards and is emphasizing nuclear energy's importance as a base-load electricity source.[2] In 2015, Japan successfully restarted one nuclear reactor at the Sendai Nuclear Power Plant in Kagoshima prefecture, and several other reactors around the country have since resumed operations. Opposition from local governments has delayed several restarts that remain pending.

Reforms of the electricity and gas sectors, including full liberalization of Japan's energy market in April 2016 and gas market in April 2017, constitute an important part of Prime Minister Abe's economic program.[2]

Japan has the third largest geothermal reserves in the world. Geothermal energy is being heavily focused on as a source of power following the Fukushima disaster. The Ministry of Economy, Trade, and Industry is exploring over 40 locations for potential geothermal energy plants.[94]

On 3 July 2018, Japan's government pledged to increase renewable energy sources from 15% to 22–24% including wind and solar by 2030. Nuclear energy will provide 20% of the country's energy needs as an emissions-free energy source. This will help Japan meet climate change commitments.[95]

Lake Tōya and Shōwa-shinzan in Shikotsu-Tōya National Park

Japan has 34 National Parks (国立公園, Kokuritsu Kōen) and 56 Quasi-National Parks (国定公園, Kokutei Kōen) in 2019. These are designated and managed for protection and sustainable usage by the Ministry of the Environment under the Natural Parks Law (自然公園法) of 1957.[96] The Quasi-National Parks have slightly less beauty, size, diversity, or preservation. They are recommended for ministerial designation and managed by the prefectures under the supervision of the Ministry of the Environment.[97]

The Japanese archipelago has diverse landscapes.[7] For example, the northern part of Hokkaido has a taiga biome.[98] Hokkaido has 22% of Japan's forestland with coniferous trees (Sakhalin fir and Sakhalin spruce) and broad-leaved trees (Japanese oak, birch and Painted maple). The seasonal views change throughout the year.[99] In the south, the Yaeyama Islands are in the subtropics with numerous species of subtropical and tropical plants, and mangrove forests.[100][101] Most natural islands have mountain ranges in the center with coastal plains.

• List of National Parks of Japan
• List of National Geoparks in Japan
• Wildlife Protection Areas in Japan
• List of Ramsar sites in Japan
• Cultural Landscapes

Ritsurin Garden, Takamatsu, Japan

The Places of Scenic Beauty and Natural Monuments are selected by the government via the Agency for Cultural Affairs in order to protect Japan's cultural heritage.[102] As of 2017, there are 1,027 Natural Monuments (天然記念物, tennen kinenbutsu) and 410 Places of Scenic Beauty (名勝, meishō). The highest classification are 75 Special Natural Monuments (特別天然記念物, tokubetsu tennen kinenbutsu) and 36 Special Places of Scenic Beauty (特別名勝, tokubetsu meishō).

The Three Views of Japan (日本三景, Nihon Sankei) is the canonical list of Japan's three most celebrated scenic sights, attributed to 1643 and scholar Hayashi Gahō.[103] These are traditionally the pine-clad islands of Matsushima in Miyagi Prefecture, the pine-clad sandbar of Amanohashidate in Kyoto Prefecture, and Itsukushima Shrine in Hiroshima Prefecture. In 1915, the New Three Views of Japan were selected with a national election by the Jitsugyo no Nihon Sha (株式会社実業之日本社). In 2003, the Three Major Night Views of Japan were selected by the New Three Major Night Views of Japan and the 100 Night Views of Japan Club (新日本三大夜景・夜景100選事務局).

• 
  Pine-clad islands of Matsushima
• 
  Sandbar of Amanohashidate
• 
  Torii at Itsukushima Shrine

Kabira Bay on Ishigaki Island, Okinawa Prefecture in March

Sakura blossoms with Himeji Castle in Hyōgo Prefecture in April

Mount Yari, Nagano Prefecture in August

Japan's varied geographical features divide it into six principal climatic zones.

• Hokkaido belongs to the humid continental climate, with long, cold winters and cool summers. Precipitation is sparse; however, winter brings large snowfalls of hundreds of inches in areas such as Sapporo and Asahikawa.
• In the Sea of Japan, the northwest seasonal wind in winter gives heavy snowfall, which south of Tohoku mostly melts before the beginning of spring. In summer, it is a little less rainy than the Pacific area but sometimes experiences extreme high temperatures because of the foehn wind phenomenon.
• Central Highland: a typical inland climate gives large temperature variations between summers and winters and between days and nights. Precipitation is lower than on the coast because of rain shadow effects.
• Seto Inland Sea: the mountains in the Chūgoku and Shikoku regions block the seasonal winds and bring mild climate and many fine days throughout the year.
• Pacific Ocean: the climate varies greatly between the north and the south, but generally winters are significantly milder and sunnier than those of the side that faces the Sea of Japan. Summers are hot because of the southeast seasonal wind. Precipitation is very heavy in the south and heavy in the summer in the north. The climate of the Ogasawara Island chain ranges from a humid subtropical climate (Köppen climate classification Cfa) to tropical savanna climate (Köppen climate classification Aw) with temperatures being warm to hot all year round.
• The climate of the Ryukyu Islands ranges from humid subtropical climate (Köppen climate classification Cfa) in the north to tropical rainforest climate (Köppen climate classification Af) in the south with warm winters and hot summers. Precipitation is very high and is especially affected by the rainy season and typhoons.

Japan is generally a rainy country with high humidity.[24] Because of its wide range of latitude,[24] seasonal winds and different types of ocean currents, Japan has a variety of climates, with a latitude range of the inhabited islands from 24°N - 46°N, which is comparable to the range between Nova Scotia and The Bahamas in the east coast of North America.[24] Tokyo is between 35°N - 36°N, which is comparable to that of Tehran, Athens, or Las Vegas.[24]

As Mount Fuji and the coastal Japanese Alps provide a rain shadow, Nagano and Yamanashi Prefectures receive the least precipitation in Honshu, though it still exceeds 900 millimetres (35 in) annually. A similar effect is found in Hokkaido, where Okhotsk Subprefecture receives as little as 750 millimetres (30 in) per year. All other prefectures have coasts on the Pacific Ocean, Sea of Japan, Seto Inland Sea or have a body of salt water connected to them. Two prefectures—Hokkaido and Okinawa—are composed entirely of islands.

The climate from June to September is marked by hot, wet weather brought by tropical airflows from the Pacific Ocean and Southeast Asia.[24] These air flows are full of moisture and deposit substantial amounts of rain when they reach land.[24] There is a marked rainy season, beginning in early June and continuing for about a month.[24] It is followed by hot, sticky weather.[24] Five or six typhoons pass over or near Japan every year from early August to early October, sometimes resulting in significant damage.[24] Annual precipitation averages between 1,000 and 2,500 mm (40 and 100 in) except for the areas such as Kii Peninsula and Yakushima Island which is Japan's wettest place[104] with the annual precipitation being one of the world's highest at 4,000 to 10,000 mm.[105]

Maximum precipitation, like the rest of East Asia, occurs in the summer months except on the Sea of Japan coast where strong northerly winds produce a maximum in late autumn and early winter. Except for a few sheltered inland valleys during December and January, precipitation in Japan is above 25 millimetres (1 in) of rainfall equivalent in all months of the year, and in the wettest coastal areas it is above 100 millimetres (4 in) per month throughout the year.

Mid June to mid July is generally the rainy season in Honshu, Shikoku and Kyushu, excluding Hokkaidō since the seasonal rain front or baiu zensen (梅雨前線) dissipates in northern Honshu before reaching Hokkaido. In Okinawa, the rainy season starts early in May and continues until mid June. Unlike the rainy season in mainland Japan, it rains neither everyday nor all day long during the rainy season in Okinawa. Between July and October, typhoons, grown from tropical depressions generated near the equator, can attack Japan with furious rainstorms.

A village in Niigata Prefecture in January

In winter, the Siberian High develops over the Eurasian land mass and the Aleutian Low develops over the northern Pacific Ocean.[24] The result is a flow of cold air southeastward across Japan that brings freezing temperatures and heavy snowfalls to the central mountain ranges facing the Sea of Japan, but clear skies to areas fronting on the Pacific.[24]

The warmest winter temperatures are found in the Nanpō and Bonin Islands, which enjoy a tropical climate due to the combination of latitude, distance from the Asian continent, and warming effect of winds from the Kuroshio, as well as the Volcano Islands (at the latitude of the southernmost of the Ryukyu Islands, 24° N). The coolest summer temperatures are found on the northeastern coast of Hokkaidō in Kushiro and Nemuro Subprefectures.

Sunshine, in accordance with Japan's uniformly heavy rainfall, is generally modest in quantity, though no part of Japan receives the consistently gloomy fogs that envelope the Sichuan Basin or Taipei. Amounts range from about six hours per day in the Inland Sea coast and sheltered parts of the Pacific Coast and Kantō Plain to four hours per day on the Sea of Japan coast of Hokkaidō. In December there is a very pronounced sunshine gradient between the Sea of Japan and Pacific coasts, as the former side can receive less than 30 hours and the Pacific side as much as 180 hours. In summer, however, sunshine hours are lowest on exposed parts of the Pacific coast where fogs from the Oyashio current create persistent cloud cover similar to that found on the Kuril Islands and Sakhalin.

The highest recorded temperature in Japan was 41.1 °C (106.0 °F) on 23 July 2018, an unverified record of 42.7 °C was taken in Adachi on 20 July 2004. The lowest was −41.0 °C (−41.8 °F) in Asahikawa on 25 January 1902. However an unofficial −41.5 °C was taken in Bifuka on 27 January 1931. Mount Fuji broke the Japanese record lows for each month except January, February, March, and December. Record lows for any month were taken as recent as 1984.

Minami-Tori-shima has a tropical savanna climate (Köppen climate classification Aw) and the highest average temperature in Japan of 25 degrees Celsius.[106]

Honshū (本州) is the largest island of Japan and the 2nd most populous island in the world. It has a population of 104,000,000 with a population density of 450/km² (1,200/sq mi) (2010).[108] Honshu is roughly 1,300 km (810 mi) long and ranges from 50 to 230 km (31 to 143 mi) wide, and the total area is 225,800 km² (87,200 sq mi). It is the 7th largest island in the world.[109] This makes it slightly larger than the island of Great Britain 209,331 km² (80,823 sq mi).[109]

The Greater Tokyo Area on Honshu is the largest metropolitan area (megacity) in the world with 38,140,000 people (2016).[110][111] The area is 13,500 km² (5,200 sq mi)[112] and has a population density of 2,642 square kilometres (1,020 sq mi).

Kyushu (九州) is the third largest island of Japan of the five main islands.[9][113] As of 2016, Kyushu has a population of 12,970,479 and covers 36,782 km² (14,202 sq mi).[114] It has the second highest population density of 307.13 km² (118.58 sq mi) (2016).

Shikoku (四国) is the second smallest of the five main islands (after Okinawa island), 18,800 km² (7,300 sq mi). It is located south of Honshu and northeast of Kyushu. It has the second smallest population of 3,845,534 million (2015)[9][115] and the third highest population density of 204.55 km² (78.98 sq mi).

Hokkaido (北海道) is the second largest island of Japan, and the largest and northernmost prefecture. The Tsugaru Strait separates Hokkaido from Honshu.[116] It has the third largest population of the five main islands with 5,383,579 (2015)[9][108] and the lowest population density with just 64.5 km² (24.9 sq mi) (2016). The island area ranks 21st in the world by area. It is 3.6% smaller than the island of Ireland.

Okinawa Prefecture (沖縄県) is the southernmost prefecture of Japan.[117] It encompasses two thirds of the Ryukyu Islands over 1,000 kilometres (620 mi) long. It has a population of 1,445,812 (2017) and a density of 622 km² (240 sq mi). Okinawa Island (四国) is the smallest and most southwestern of the five main islands, 1,206.98 km² (466.02 sq mi).[9] It has the smallest population of 1,301,462 (2014) and the highest population density of 1,083.6 km² (418.4 sq mi).

Nanpō Islands (南方諸島) are the groups of islands that are located to the south and east of the main islands of the Japanese archipelago. They extend from the Izu Peninsula west of Tokyo Bay southward for about 1,200 kilometres (750 mi), to within 500 kilometres (310 mi) of the Mariana Islands. The Nanpō Islands are all administered by Tokyo Metropolis. Approximately 0.7% of the Japanese population lives there.

Taiheiyō Belt

The Taiheiyō Belt is a megalopolis that includes the Greater Tokyo Area and Keihanshin megapoles. It is almost 1,200 km (750 mi) long from Ibaraki Prefecture in the northeast to Fukuoka Prefecture in the southwest. Satellite images at night show a dense and continuous strip of light (demarcating urban zones) that delineates the region with overlapping metropolitan areas in Japan.[118] It has a total population of approximately 81,859,345 (2016).

• Taiheiyō Belt – includes Ibaraki, Saitama, Chiba, Tokyo, Kanagawa, Shizuoka, Aichi, Gifu, Mie, Kyoto, Osaka, Hyōgo, Wakayama, Okayama, Hiroshima, Yamaguchi, Fukuoka, and Ōita. (81,859,345 people)[119][120]
  • Greater Tokyo Area – Part of the larger Kantō region, broadly includes Tokyo and Yokohama. (38,000,000 people)[121]
  • Keihanshin – Part of the larger Kansai region, includes Osaka, Kyoto, Kobe. (19,341,976 people)[122]

There are plans to build underwater habitats in Japan's Exclusive Economic Zone. Currently no underwater city is constructed yet. For example, the Ocean Spiral by Shimizu Corporation would have a floating dome 500 meters in diameter with hotels, residential and commercial complexes. It could be 15 km long. This allows mining of the seabed, research and production of methane from carbon dioxide with micro-organisms. The Ocean Spiral was co-developed with JAMSTEC and Tokyo University.[123][124]

The five main islands of Japan are Hokkaidō, Honshū, Kyūshū, Shikoku and Okinawa. These are also called the mainland.[9] All of these points are accessible to the public.

The Kuril Islands with Russian names. Borders of Shimoda Treaty (1855) and Treaty of St. Petersburg (1875) shown in red. Currently all islands northeast of Hokkaido are administered by Russia.

Japan has a longstanding claim of the Southern Kuril Islands (Etorofu, Kunashiri, Shikotan, and the Habomai Islands). These islands were occupied by the Soviet Union in 1945.[128] The Kuril Islands historically belong to Japan.[129] The Kuril Islands were first inhabited by the Ainu people and then controlled by the Japanese Matsumae clan in the Edo Period.[130] The Soviet Union did not sign the San Francisco Treaty in 1951. The U.S. Senate Resolution of April 28, 1952, ratifying of the San Francisco Treaty, explicitly stated that the USSR had no title to the Kurils.[131] This dispute has prevented the signing of a peace treaty between Japan and Russia.

Geographically the Kuril Islands are a northeastern extension of Hokkaido. Kunashiri and the Habomai Islands are visible from the northeastern coast of Hokkaido. Japan considers the northern territories (aka Southern Chishima) part of Nemuro Subprefecture of Hokkaido Prefecture.

The aftermath of the 2011 Tōhoku earthquake and tsunami

Japan is substantially prone to earthquakes, tsunami and volcanoes because of its location along the Pacific Ring of Fire.[133] It has the 15th highest natural disaster risk as measured in the 2013 World Risk Index.[134]

As many as 1,500 earthquakes are recorded yearly, and magnitudes of 4 to 6 are common.[24] Minor tremors occur almost daily in one part of the country or another, causing slight shaking of buildings.[24] Undersea earthquakes also expose the Japanese coastline to danger from tsunamis (津波).[24]

Destructive earthquakes, often resulting in tsunami, occur several times each century.[16] The 1923 Tokyo earthquake killed over 140,000 people.[135] More recent major quakes are the 1995 Great Hanshin earthquake and the 2011 Tōhoku earthquake, a 9.1-magnitude[136] quake which hit Japan on March 11, 2011. It triggered a large tsunami and the Fukushima Daiichi nuclear disaster, one of the worst disasters in the history of nuclear power.[137]

The 2011 Tōhoku earthquake was the largest ever recorded in Japan and is the world's 4th largest earthquake to strike since 1900, according to the U.S. Geological Service. It struck offshore about 371 kilometres (231 mi) northeast of Tokyo and 130 kilometres (81 mi) east of the city of Sendai, and created a massive tsunami that devastated Japan's northeastern coastal areas. At least 100 aftershocks registering a 6.0 magnitude or higher have followed the main shock. At least 15,000 people died as a result.

Reclaimed land and man-made islands are particularly susceptible to liquefaction during an earthquake. As a result, there are specific earthquake resistance standards and ground reform work that applies to all construction in these areas. In an area that was possibly reclaimed in the past, old maps and land condition drawings are checked and drilling is carried out to determine the strength of the ground. However this can be very costly, so for a private residential block of land, a Swedish weight sounding test is more common.[34]

Japan has become a world leader in research on causes and prediction of earthquakes.[24] The development of advanced technology has permitted the construction of skyscrapers even in earthquake-prone areas.[24] Extensive civil defence efforts focus on training in protection against earthquakes, in particular against accompanying fire, which represents the greatest danger.[24]

Sakurajima eruption on October 3, 2009

Japan has 108 active volcanoes. That's 10% of all active volcanoes in the world. Japan has stratovolcanoes near the subduction zones of the tectonic plates. During the 20th century several new volcanoes emerged, including Shōwa-shinzan on Hokkaido and Myōjin-shō off the Bayonnaise Rocks in the Pacific.[16] In 1991, Japan's Unzen Volcano on Kyushu about 40 km (25 mi) east of Nagasaki, awakened from its 200-year slumber to produce a new lava dome at its summit. Beginning in June, repeated collapse of this erupting dome generated ash flows that swept down the mountain's slopes at speeds as high as 200 km/h (120 mph). Unzen erupted in 1792 and killed more than 15,000 people. It is the worst volcanic disaster in the country's recorded history.[138]

Mount Fuji is a dormant stratovolcano that last erupted on 16 December 1707 till about 1 January 1708.[139][140] The Hōei eruption of Mount Fuji did not have a lava flow, but it did release some 800 million cubic metres (28×10^⁹ cu ft) of volcanic ash. It spread over vast areas around the volcano and reached Edo almost 100 kilometres (60 mi) away. Cinders and ash fell like rain in Izu, Kai, Sagami, and Musashi provinces.[141] In Edo, the volcanic ash was several centimeters thick.[142] The eruption is rated a 5 on the Volcanic Explosivity Index.[143]

Mount Aso 4 pyroclastic flow and the spread of Aso 4 tephra (90,000 to 85,000 years ago). The pyroclastic flow reached almost the whole area of Kyushu, and volcanic ash was deposited of 15 cm in a wide area from Kyushu to southern Hokkaido.

There are three VEI-7 volcanoes in Japan. These are the Aira Caldera, Kikai Caldera and Aso Caldera. These giant caldera are remnants of past eruptions. Mount Aso is the largest active volcano in Japan. 300,000 to 90,000 years ago there were four eruptions of Mount Aso which emitted huge amounts of volcanic ash that covered all of Kyushu and up to Yamaguchi Prefecture.

• The Aira Caldera is 17 kilometers long and 23 km wide located in south Kyushu. The city of Kagoshima and the Sakurajima volcano are within the Aira Caldera. Sakurajima is the most active volcano in Japan.[144]
• The Aso Caldera stretches 25 kilometers north to south and 18 kilometers east to west in Kumamoto Prefecture, Kyushu. It has erupted 4 times: 266,000 and 141,000 years ago with 32 DRE km3 (dense-rock equivalent) each; 130,000 years ago with 96 DRE km3; and 90,000 years ago with 384 DRE km3.[145]
• The Kikai Caldera is a massive, mostly submerged caldera up to 19 kilometres (12 mi) in diameter in the Ōsumi Islands of Kagoshima Prefecture, Japan. It is the remains of the ancient eruption of a colossal volcano. Kikai Caldera was the source of the Akahoya eruption, one of the largest eruptions during the Holocene (10,000 years ago to present). About 4,300 BC, pyroclastic flows from that eruption reached the coast of southern Kyūshū up to 100 km (62 mi) away, and ash fell as far as Hokkaidō. The eruption produced about 150 km³ of tephra,[146] giving it a Volcanic Explosivity Index of 7[147] The Jōmon culture of at least southern Kyushu was destroyed, and it took nearly 1,000 years to recover.[148]

Surveys by KOBEC (Kobe Ocean-Bottom Exploration Center) confirm that a giant lava dome of 23 cubic kilometers formed after the Kikai Caldera erupted in 4,300 BC. There is a 1% chance of a giant caldera eruption in the Japanese archipelago within the next 100 years. Appropriately 40 cubic kilometers of magma would be released in one burst and cause enormous damage.[149]

According to a 2014 study by KOBEC of Kobe University, in a worst-case scenario if there is a VEI-7 eruption of the Aso Caldera and if the volcanic ash is carried by westerly winds, then pyroclastic flows would cover the 7 million population near the Aso Caldera within two hours. The pyroclastic flows could reach much of Kyushu. Beyond the pyroclastic area is volcanic ash that falls from the sky. If the volcanic ash continuously flows eastward, then the ash fall would make it impossible to live in most parts of Japan (the main islands) because of a paralysis of traffic and lifelines for a limited period until the eruption subsides. In this scenario, the exception would be eastern and northern Hokkaido (the Ryukyu Islands and southern Nanpo Islands would also be excepted). Professor Yoshiyuki Tatsumi, head of KOBEC told the Mainichi Shimbun “the probability of a gigantic caldera eruption hitting the Japanese archipelago is 1 percent in the next 100 years” with a death toll of many 10s of millions of people and wildlife.[148] The potential exists for tens of millions of humans and other living beings to die during a VEI-7 volcanic eruption with significant short-term effects on the global climate. If in another scenario, the wind blows in a different direction then the Volcanic ash could flow westward or southward and affect e.g. the East Asian continent or South-East Asia. Since the Kikai Caldera is submerged, it is unclear how much damage the hot ash clouds would cause if much volcanic ash stays below the ocean surface. The underwater ash would be swept away by ocean currents.

Improving technology and methods to predict volcano and giant caldera eruptions would help to prepare and evacuate people earlier. Technology is needed to accurately capture the state of the magma chamber that spreads thinly with a thickness of less than several kilometers around the middle of the crust. The underground area of Kyushu must be monitored, because it is a dangerous area with a potential caldera eruption.

The most protective measure is to stop the hot ash clouds from spreading and devastating areas near the eruption so that people don't need to evacuate. There are currently no protective measures to minimize the spread of millions of tons of deadly hot ash during a VEI-7 eruption.

In 2018 NASA published a theoretical plan to prevent a volcanic eruption by pumping large quantities of cold water down a borehole into the hydrothermal system of a supervolcano. The water would cool the huge body of magma in the chambers below the volcano so that the liquid magma becomes semi-solid. Thus enough heat could be extracted to prevent an eruption. The heat could be used by a geothermal plant to generate geothermal energy and electricity.[151]

Since recording started in 1951, an average of 2.6 typhoons reached the main islands of Kyushu, Shikoku, Honshu and Hokkaido per year. Approximately 10.3 typhoons approach within the 300 kilometer range near the coast of Japan. Okinawa is, due to its geographic location, most vulnerable to typhoons with an average of 7 storms per year. The most destructive was Isewan Typhoon with 5,000 casualties in the Tokai region in September 1959. In October 2004, Typhoon Tokage caused heavy rain in Kyushu and central Japan with 98 casualties. Until the 1960s the death toll was hundreds of people per typhoon. Since the 1960s improvements in construction, flood prevention, high tides detection and early warnings substantially reduced the death toll which rarely exceeds a dozen people per typhoon. Japan also has special search and rescue units to save people in distress.[152]

Heavy snowfall during the winter in the snow country regions cause landslides, flooding, and avalanches.