Rikuzentakata
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Rikuzentakata
is a city located in Iwate Prefecture, Japan. In the census of 2010, the city had a population of 23,302 (2005: 24,709), and a population density of 100 persons per km². The 2011 Tōhoku earthquake and tsunami caused extensive damage to the city. , the city had an estimated population of 19,062, and a population density of 82 persons per km² in 7,593 households. The total area of the city is . Geography Rikuzentakata is located in the far southeast corner of Iwate Prefecture, bordered by the Pacific Ocean to the east. The city contained Lake Furukawanuma until the 2011 tsunami destroyed it. Parts of the coastal area of the city are within the borders of the Sanriku Fukkō National Park. Neighboring municipalities Iwate Prefecture * Ōfunato * Ichinoseki * Sumita Miyagi Prefecture * Kesennuma Climate Rikuzentakata has a humid climate ( Köppen climate classification ''Cfa'') bordering on an oceanic climate ( Köppen climate classification ''Cfb'') with warm summers and ...
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2011 Tōhoku Earthquake And Tsunami
The occurred at 14:46 JST (05:46 UTC) on 11 March. The magnitude 9.0–9.1 (M) undersea megathrust earthquake had an epicenter in the Pacific Ocean, east of the Oshika Peninsula of the Tōhoku region, and lasted approximately six minutes, causing a tsunami. It is sometimes known in Japan as the , among other names. The disaster is often referred to in both Japanese and English as simply 3.11 (read in Japanese). It was the most powerful earthquake ever recorded in Japan, and the fourth most powerful earthquake in the world since modern record-keeping began in 1900. The earthquake triggered powerful tsunami waves that may have reached heights of up to in Miyako in Tōhoku's Iwate Prefecture,Yomiuri Shimbun evening edition 2-11-04-15 page 15, nearby Aneyoshi fishery port (姉吉漁港)(Google map E39 31 57.8, N 142 3 7.6) 2011-04-15大震災の津波、宮古で38.9 m…明治三陸上回るby okayasu Akio (岡安 章夫) and which, in the Sendai area, traveled at a ...
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Sanriku Fukkō National Park
(''lit''. "Sanriku Reconstruction National Park") is a national park extending along the Sanriku Coast of Japan from Hachinohe in Aomori Prefecture through Iwate Prefecture to Kesennuma in Miyagi Prefecture. The national park was created on 24 May 2013 and covers a land area of History On 2 May 1955 the was created in the Tōhoku region of Honshū in northern Japan. The park extended for 180 kilometers from north to south along the coastline of the Pacific Ocean from northern Miyagi prefecture to northern Iwate prefecture. It had a land area of . On 24 May 2013 the park was incorporated into Sanriku Fukkō National Park. This was in the aftermath of the 2011 Tōhoku earthquake and tsunami. It also includes the former Tanesashi Kaigan Hashikamidake Prefectural Natural Park. On 31 March 2015, the Ministry of the Environment extended the park to include the former Minami Sanriku Kinkasan Quasi-National Park. Subsequently, the park will be extended to include Kesennuma Prefectural ...
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Iwate Prefecture
is a prefecture of Japan located in the Tōhoku region of Honshu. It is the second-largest Japanese prefecture at , with a population of 1,210,534 (as of October 1, 2020). Iwate Prefecture borders Aomori Prefecture to the north, Akita Prefecture to the west, and Miyagi Prefecture to the south. Morioka is the capital and largest city of Iwate Prefecture; other major cities include Ichinoseki, Ōshū, and Hanamaki. Located on Japan's Pacific Ocean coast, Iwate Prefecture features the easternmost point of Honshu at Cape Todo, and shares the highest peaks of the Ōu Mountains—the longest mountain range in Japan—at the border with Akita Prefecture. Iwate Prefecture is home to famous attractions such as Morioka Castle, the Buddhist temples of Hiraizumi including Chūson-ji and Mōtsū-ji, the Fujiwara no Sato movie lot and theme park in Ōshū, and the Tenshochi park in Kitakami known for its huge, ancient cherry trees. Iwate has the lowest population density of any prefecture ...
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Sumita, Iwate
is a town located in Iwate Prefecture, Japan. , the town had an estimated population of 5,315, and a population density of 16 persons per km² in 2142 households. The total area of the town is . Geography Sumita is located in a basin in southeastern Iwate Prefecture in the southern Kitakami Mountains, surrounded by peaks with an elevation of between 600 and 1500 meters an all sides. Approximately 90% of the town’s area is covered by forest and mountains. Neighboring municipalities Iwate Prefecture * Ōfunato *Rikuzentakata *Ichinoseki * Tōno *Kamaishi *Ōshū Climate Sumita has a humid climate (Köppen climate classification ''Dfa'') with warm summers and cold winters. The average annual temperature in Sumita is 10.4 °C. The average annual rainfall is 1379 mm with September as the wettest month and January as the driest month. The temperatures are highest on average in August, at around 23.1 °C, and lowest in January, at around -1.2 °C. Demographic ...
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Kesennuma, Miyagi
is a city in Miyagi Prefecture, Japan. , the city had an estimated population of 59,803 and a population density of in 26,390 households. The total area of the city is . Large sections of the city were destroyed by the 2011 Tōhoku earthquake and tsunami and major fires on March 11, 2011. Geography Kesennuma is in the far northeastern corner of Miyagi Prefecture. The city wraps around the western part of Kesennuma Bay and also includes the island of Ōshima. Its deeply indented rias coastline forms the southern boundary of the Sanriku Fukkō National Park, which stretches north to Aomori Prefecture. The city borders Hirota Bay, Kesennuma Bay, and the Pacific Ocean to the east and Minamisanriku, Miyagi to the south. Iwate Prefecture makes up the remainder of its borders, with the city of Ichinoseki to the west, and the city of Rikuzen-Takata to the north. The highest point in Kesennuma is the high Mount Ōmori, on the border with Motoyoshi, while the lowest point is at sea lev ...
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Tōhoku Region
The , Northeast region, or consists of the northeastern portion of Honshu, the largest island of Japan. This traditional region consists of six prefectures (''ken''): Akita, Aomori, Fukushima, Iwate, Miyagi, and Yamagata. Tōhoku retains a reputation as a remote, scenic region with a harsh climate. In the 20th century, tourism became a major industry in the Tōhoku region. History Ancient & Classical period In mythological times, the area was known as Azuma (吾妻, あづま) and corresponded to the area of Honshu occupied by the native Emishi and Ainu. The area was historically the Dewa and the Michinoku regions, a term first recorded in (654). There is some variation in modern usage of the term "Michinoku". Tōhoku's initial historical settlement occurred between the seventh and ninth centuries, well after Japanese civilization and culture had become firmly established in central and southwestern Japan. The last stronghold of the indigenous Emishi on Honshu and ...
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Ichinoseki, Iwate
is a city located in Iwate Prefecture, in the Tōhoku region of northern Japan. , the city had a population of 114,476 and a population density of 91 persons per km² in 46,375 households. It is currently the second largest city by population in the prefecture, after Morioka. The total area of the city was . Geography Ichinoseki is located inland in the south of Iwate Prefecture, a little over two hours north of Tokyo by the Tōhoku Shinkansen. A large volume of extremely stable granite rock runs beneath the city, and is the center of the site is being promoted as a suitable location for construction of the International Linear Collider (ILC). Neighboring municipalities Iwate Prefecture *Ōshū *Rikuzentakata * Sumita *Hiraizumi Miyagi Prefecture *Kesennuma *Kurihara * Tome Akita Prefecture * Higashinaruse Climate Ichinoseki has a humid climate (Köppen climate classification ''Cfa'') with warm summers and cold winters. The average annual temperature in Ichinoseki is 10.9  ...
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Lake Furukawanuma
was a lake that existed in Rikuzentakata, Iwate, Japan until March 11, 2011. When the 2011 Tohoku earthquake struck, the resulting tsunami destroyed the sand wall that separated the lake from the sea. The lake's western edge thus became part of the new coastline, and the lake became part of the sea. History Rikuzentakada is the largest alluvial plain along the ria of the Sanriku Coast. The plain started to form at the last stage of the ice age when the sea level rose. Sand was carried from the Kesen River into Hirota Bay. About 7500 years ago, the surface area of the bay grew, thus the present plain was under water. Mud deposited in the Furukawanuma Lake was formed by the formation of sand hills about 1,000 years ago. There was a wide deposition of sand blocking part of the Hirota Bay. Mud was deposited in Hirota Bay which became deeper. Pine trees were planted along the seashore in the Edo period. The Sanriku Coast has many ria coasts which have frequently been shaped by the ...
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List Of Sovereign States
The following is a list providing an overview of sovereign states around the world with information on their status and recognition of their sovereignty. The 206 listed states can be divided into three categories based on membership within the United Nations System: 193 UN member states, 2 UN General Assembly non-member observer states, and 11 other states. The ''sovereignty dispute'' column indicates states having undisputed sovereignty (188 states, of which there are 187 UN member states and 1 UN General Assembly non-member observer state), states having disputed sovereignty (16 states, of which there are 6 UN member states, 1 UN General Assembly non-member observer state, and 9 de facto states), and states having a special political status (2 states, both in free association with New Zealand). Compiling a list such as this can be a complicated and controversial process, as there is no definition that is binding on all the members of the community of nations concerni ...
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Oceanic Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. M ...
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Humid Subtropical Climate
A humid subtropical climate is a zone of climate characterized by hot and humid summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates. It is also known as warm temperate climate in some climate classifications. Under the Köppen climate classification, ''Cfa'' and ''Cwa'' climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classification was officially created under the Trewartha climate classification. In this classification, climates are termed humid subtropical when the ...
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