Taiwanese Hot Springs
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Taiwanese Hot Springs
Taiwan is part of the collision zone between the Yangtze Plate and Philippine Sea Plate. Eastern and southern Taiwan are the northern end of the Philippine Mobile Belt. Located next to an oceanic trench and volcanic system in a tectonic collision zone, Taiwan has evolved a unique environment that produces high-temperature springs with crystal-clear water, usually both clean and safe to drink. These hot springs are commonly used for spas and resorts. Soaking in hot springs became popular in Taiwan around 1895 during the 50-year long colonial rule by Japan. History The first mention of Taiwan's hot springs came from a 1697 manuscript, , but they were not developed until 1893, when a German businessman discovered Beitou and later established a small local spa. Under Japanese rule, the government constantly promoted and further enhanced the natural hot springs. The Japanese rule brought with them their rich onsen culture of spring soaking, which had a great influence on Taiwan. ...
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Beitou Hell Valley 3
Beitou District is the northernmost of the twelve districts of Taipei City, Taiwan. The historical spelling of the district is Peitou. The name originates from the Ketagalan word ''Kipatauw'', meaning witch. Beitou is the most mountainous and highest of Taipei's districts, encompassing a meadow with rivers running through the valley which have abundant steam rising from them; the result of geothermal warming. The valley is often surrounded by mist shrouding the trees and grass. Beitou is famous for its hot springs. In March 2012, it was named one of the ''Top 10 Small Tourist Towns'' by the Tourism Bureau of Taiwan. History The area's hot springs had long been enjoyed by the aboriginal people of Taiwan. Shortly before the Japanese period a German sulfur merchant established the first hot spring club in Beitou. During early Japanese rule, ''Hokutō'' () was a village at the entrance of the well-known North Formosa sulfur district. Three Japanese extracting plants in this dist ...
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Zhiben Hot Spring
The Zhiben Hot Spring () is a hot spring in Beinan, Taitung County, Taiwan. It is one of the most famous Taiwanese hot springs. History The Puyuma people, which inhabited in the area, learned that the Zhiben Hot Spring was healthy to the human body. During the Japanese rule era, the government set up public baths using water from the hot spring. On 8 August 2009 Zhiben was one of many places in Taiwan to be badly hit by Typhoon Morakot (2009) and made international news headlines when an eyewitness filmed the collapse of a riverside hotel undermined by flood waters. However, Zhiben's infrastructure was very rapidly restored and as of autumn 2009 the main spas are once more operational and easy to reach from Taitung City Taitung City () is a county-administered city and the county seat of Taitung County, Taiwan. It lies on the southeast coast of Taiwan facing the Pacific Ocean. Taitung City is the most populous subdivision of Taitung County and it is one of the .... Refer ...
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Dakeng
Dakeng (traditional Chinese: 大坑, Hanyu Pinyin: dàkēng) is the area that contains most of the mountain region of Beitun District, Taichung, Taiwan. Hiking and Biking Trails Dakeng also boasts a variety of mountain biking and hiking trails. These trails are managed by the Taichung City Government. A total of 10 hiking trails exist. Each trail varies in difficulty in ascent and descent; with trails 6-10 being more flat and suitable for beginners while trails 1-5 are more vertical and pose more of a challenge. Trails 1-5 are composed of log steps throughout much of the trail with ropes on both sides to help support hikers. Guanyin Mountain Dakeng is also home to the Guanyin Temple on Guanyin Mountain located near Central Taiwan University of Science and Technology (CTUST)Central Taiwan University of Science and Technology
Taiwan.
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Jiaoxi, Yilan
Jiaoxi Township () or Chiaohsi Township is a rural township in the northern section of Yilan County, Taiwan. Geography * Area: 101.43 km² * Population: 35,945 people (2014) Administrative divisions The township includes eighteen rural villages: *Baiyun (), Yushi (Yushih; ), Deyang (), Dazhong (), Dayi (), Liujie (), Erlong (), Shichao (), Yutian (), Sanmin (), Linmei (), Baie (), Yuguang (), Guangwu (), Wusha (), Longtan (), Paolun () and Erjie Village (). Education * Fo Guang University *Tamkang University Lanyang Campus Tourist attractions Jiaoxi is famous for its hot springs. These attract large numbers of visitors so as the result, Jiaoxi has become a favorite weekend resort, mostly people from Taipei, featuring an array of hotels from the budget to the luxurious. There is also a few free public hot springs, mostly sheltered, where visitors can enjoy a leisurely foot bath at any time. In March 2012, it was named one of the ''Top 10 Small Tourist Towns'' ...
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Guguan Hot Springs
Guguan is an island in the Northern Mariana Islands in the Pacific Ocean. The island is currently uninhabited. Guguan is located south from Alamagan and north from Saipan, and is northeast from Sarigan. History Guguan was discovered in 1668 by the Spanish missionary Diego Luis de Sanvitores who charted it as ''San Felipe''. It is likely that it was previously visited in 1522 by the Spanish sailor Gonzalo de Vigo, deserter from the Magellan expedition in 1521, who was the first European castaway in the history of the Pacific. Uninhabited at the time, in contrast to other islands in the Marianas it was never colonized. As with the other islands in the northern Marianna, Guguan was sold by Spain to the German Empire in 1899, and administered as part of German New Guinea. From 1909 to 1912, the island was leased to a Japanese company, who sent hunters to gather bird feathers for the European hat industry. During World War I, Guguan came under the control of the Empire of Japan ...
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Beitou Thermal Valley Warning Sign 20050814
Beitou District is the northernmost of the twelve districts of Taipei City, Taiwan. The historical spelling of the district is Peitou. The name originates from the Ketagalan word ''Kipatauw'', meaning witch. Beitou is the most mountainous and highest of Taipei's districts, encompassing a meadow with rivers running through the valley which have abundant steam rising from them; the result of geothermal warming. The valley is often surrounded by mist shrouding the trees and grass. Beitou is famous for its hot springs. In March 2012, it was named one of the ''Top 10 Small Tourist Towns'' by the Tourism Bureau of Taiwan. History The area's hot springs had long been enjoyed by the aboriginal people of Taiwan. Shortly before the Japanese period a German sulfur merchant established the first hot spring club in Beitou. During early Japanese rule, ''Hokutō'' () was a village at the entrance of the well-known North Formosa sulfur district. Three Japanese extracting plants in this dist ...
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Sodium Hydrogen Carbonate
Sodium bicarbonate (IUPAC name: sodium hydrogencarbonate), commonly known as baking soda or bicarbonate of soda, is a chemical compound with the formula NaHCO3. It is a salt composed of a sodium cation ( Na+) and a bicarbonate anion ( HCO3−). Sodium bicarbonate is a white solid that is crystalline, but often appears as a fine powder. It has a slightly salty, alkaline taste resembling that of washing soda (sodium carbonate). The natural mineral form is nahcolite. It is a component of the mineral natron and is found dissolved in many mineral springs. Nomenclature Because it has long been known and widely used, the salt has many different names such as baking soda, bread soda, cooking soda, and bicarbonate of soda and can often be found near baking powder in stores. The term ''baking soda'' is more common in the United States, while ''bicarbonate of soda'' is more common in Australia, United Kingdom and Ireland. and in many northern/central European countries it is called ''Na ...
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Fumarole
A fumarole (or fumerole) is a vent in the surface of the Earth or other rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids. Fumaroles are characteristic of the late stages of volcanic activity, but fumarole activity can also precede a volcanic eruption and has been used for eruption prediction. Most fumaroles die down within a few days or weeks of the end of an eruption, but a few are persistent, lasting for decades or longer. An area containing fumaroles is known as a fumarole field. The predominant vapor emitted by fumaroles is steam, formed by the circulation of groundwater through heated rock. This is typically accompanied by volcanic gases given off by magma cooling deep below the surface. These volcanic gases include sulfur compounds, such as various sulfur oxides and hydrogen sulfide, and sometimes hydrogen chloride, hydrogen fluoride, and other gases. A fumarole that emits significant sulfur compounds is some ...
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Ring Of Fire
The Ring of Fire (also known as the Pacific Ring of Fire, the Rim of Fire, the Girdle of Fire or the Circum-Pacific belt) is a region around much of the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur. The Ring of Fire is a horseshoe-shaped belt about long and up to about wide. The Ring of Fire includes the Pacific coasts of South America, North America and Kamchatka, and some islands in the western Pacific Ocean. Although there is consensus among geologists about almost all areas which are included in the Ring of Fire, they disagree about the inclusion or exclusion of a few areas, for example, the Antarctic Peninsula and western Indonesia. The Ring of Fire is a direct result of plate tectonics: specifically the movement, collision and destruction of lithospheric plates (e.g. the Pacific Plate) under and around the Pacific Ocean. The collisions have created a nearly continuous series of subduction zones, where volcanoes are created and ear ...
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Eurasian Plate
The Eurasian Plate is a tectonic plate that includes most of the continent of Eurasia (a landmass consisting of the traditional continents of Europe and Asia), with the notable exceptions of the Indian subcontinent, the Arabian subcontinent and the area east of the Chersky Range in eastern Siberia. It also includes oceanic crust extending westward to the Mid-Atlantic Ridge and northward to the Gakkel Ridge. The eastern edge is a boundary with the North American Plate to the north and a boundary with the Philippine Sea Plate to the south and possibly with the Okhotsk Plate and the Amurian Plate. The southern edge is a boundary with the African Plate to the west, the Arabian Plate in the middle and the Indo-Australian Plate to the east. The western edge is a divergent boundary with the North American Plate forming the northernmost part of the Mid-Atlantic Ridge, which is straddled by Iceland. All volcanic eruptions in Iceland, such as the 1973 eruption of Eldfell, the 1783 eruptio ...
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Philippine Plate
The Philippine Sea Plate or the Philippine Plate is a tectonic plate comprising oceanic lithosphere that lies beneath the Philippine Sea, to the east of the Philippines. Most segments of the Philippines, including northern Luzon, are part of the Philippine Mobile Belt, which is geologically and tectonically separate from the Philippine Sea Plate. The plate is bordered mostly by convergent boundaries:Smoczyk, G.M., Hayes, G.P., Hamburger, M.W., Benz, H.M., Villaseñor, Antonio, and Furlong, K.P., 2013Seismicity of the Earth 1900–2012 Philippine Sea Plate and vicinity U.S. Geological Survey Open-File Report 2010–1083-M, scale 1:10,000,000, ''https://dx.doi.org/10.3133/ofr20101083m''. To the north, the Philippine Sea Plate meets the Okhotsk Plate at the Nankai Trough. The Philippine Sea Plate, the Amurian Plate, and the Okhotsk Plate meet near Mount Fuji in Japan. The thickened crust of the Izu–Bonin–Mariana arc colliding with Japan constitutes the Izu Collision Zone. The ...
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