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47-621: Niimi is located on a karst plateau in the Chugoku Mountains in northeast Okayama Prefecture. More than 85% of the city area is mountainous, with Mount Hanami being the highest peak at 1188 meters. Due to the rugged terrain, there are many waterfalls, dams, hot springs and multiple limestone caves in the city. The main urban area is located on the upper reaches of the Takahashi River (110.7 kilometres (68.8 mi). Hiroshima Prefecture Okayama Prefecture Tottori Prefecture Niimi has

94-582: A humid subtropical climate ( Köppen climate classification Cfa ). The average annual temperature in Niimi is 12.4 °C (54.3 °F). The average annual rainfall is 1,361.1 mm (53.59 in) with July as the wettest month. The temperatures are highest on average in August, at around 24.5 °C (76.1 °F), and lowest in January, at around 1.1 °C (34.0 °F). The highest temperature ever recorded in Niimi

141-620: A directly elected mayor and a unicameral city legislature of 16 members. The city contributes one member to the Okayama Prefectural Assembly. In terms of national politics, the city is part of Okayama 3rd district of the lower house of the Diet of Japan . Niimi was historically known for its iron sand quarries and the production of wagyu beef. The principle industries in modern Niimi are limestone quarrying , cement production, forestry , and tourism . Yamasa Company, Ltd. ,

188-507: A pioneer of the study of karst in Slovenia and a fellow of the Royal Society , London, introduced the word karst to European scholars in 1689 to describe the phenomenon of underground flows of rivers in his account of Lake Cerknica . Jovan Cvijić greatly advanced the knowledge of karst regions to the point where he became known as the "father of karst geomorphology". Primarily discussing

235-487: A producer of pachinko slot machines , is headquartered in the city. Farms in Niimi produce grapes, chestnuts , peaches , and Japanese pears . A black tea plantation is also being trialled here. The city is served by Niimi Kōritsu Tanki Daigaku, known in English as Niimi College. Niimi has 17 public elementary schools and seven public junior high schools operated by the city government, and one public high school operated by

282-562: A proper noun, the Slovene form Grast was first attested in 1177. Ultimately, the word is of Mediterranean origin. It has also been suggested that the word may derive from the Proto-Indo-European root karra- 'rock'. The name may also be connected to the oronym Kar(u)sádios oros cited by Ptolemy , and perhaps also to Latin Carusardius . Johann Weikhard von Valvasor ,

329-401: A sport than a science and so the underground karst caves and their associated watercourses were, from a scientific perspective, understudied. Karst is most strongly developed in dense carbonate rock , such as limestone, that is thinly bedded and highly fractured . Karst is not typically well developed in chalk , because chalk is highly porous rather than dense, so the flow of groundwater

376-413: A variety of spatial and temporal scales in karst regions, with the purpose of understanding karst aquifers and ecosystems, and the development of the surface and underground structure, so that the environment can be protected and human activities planned effectively. West Japan Railway Company The West Japan Railway Company , also referred to as JR West ( JR西日本 , Jeiāru Nishi-Nihon ) ,

423-519: A well in a fracture trace or intersection of fracture traces increases the likelihood to encounter good water production. Voids in karst aquifers can be large enough to cause destructive collapse or subsidence of the ground surface that can initiate a catastrophic release of contaminants. Groundwater flow rate in karst aquifers is much more rapid than in porous aquifers. For example, in the Barton Springs Edwards aquifer, dye traces measured

470-493: Is a UNESCO World Heritage Site. Many karst-related terms derive from South Slavic languages , entering scientific vocabulary through early research in the Western Balkan Dinaric Alpine karst. The study of the various aspects of karst regions is called karstology. This includes biological, chemical, ecological, geomorphological, hydrogeological, hydrological, political, socio-economical, and other processes over

517-542: Is a development of karst observed in geological history and preserved within the rock sequence, effectively a fossil karst. There are for example palaeokarst surfaces exposed within the Clydach Valley Subgroup of the Carboniferous Limestone sequence of South Wales which developed as sub-aerial weathering of recently formed limestones took place during periods of non-deposition within the early part of

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564-525: Is a karst landscape which is developed beneath a cover of insoluble rocks. Typically this will involve a cover of sandstone overlying limestone strata undergoing solution. In the United Kingdom for example extensive doline fields have developed at Cefn yr Ystrad , Mynydd Llangatwg and Mynydd Llangynidr in South Wales across a cover of Twrch Sandstone which overlies concealed Carboniferous Limestone ,

611-468: Is developed in areas where salt is undergoing solution underground. It can lead to surface depressions and collapses which present a geo-hazard. Karst areas tend to have unique types of forests. The karst terrain is difficult for humans to traverse, so that their ecosystems are often relatively undisturbed. The soil tends to have a high pH, which encourages growth of unusual species of orchids, palms, mangroves, and other plants. Paleokarst or palaeokarst

658-612: Is frequently unseen until the roof of a cavern suddenly collapses. Such events have swallowed homes, cattle, cars, and farm machinery. In the United States, sudden collapse of such a cavern-sinkhole swallowed part of the collection of the National Corvette Museum in Bowling Green, Kentucky in 2014. The world's largest limestone karst is Australia's Nullarbor Plain . Slovenia has the world's highest risk of sinkholes, while

705-664: Is highly automated, and during peak hours trains run as often as every two minutes. JR-West's Urban Network competes with a number of private commuter rail operators around Osaka, the "Big 4" being Hankyu Railway / Hanshin Railway (Hankyu bought Hanshin in April 2005), Keihan Railway , Kintetsu , and Nankai Railway . JR-West's market share in the region is roughly equal to that of the Big 4 put together, largely due to its comprehensive network and high-speed commuter trains (Special Rapid Service trains on

752-407: Is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock , and much of this is found in porous karst systems. The English word karst was borrowed from German Karst in the late 19th century, which entered German usage much earlier, to describe a number of geological, geomorphological, and hydrological features found within

799-399: Is not concentrated along fractures. Karst is also most strongly developed where the water table is relatively low, such as in uplands with entrenched valleys , and where rainfall is moderate to heavy. This contributes to rapid downward movement of groundwater, which promotes dissolution of the bedrock, whereas standing groundwater becomes saturated with carbonate minerals and ceases to dissolve

846-804: Is one of the Japan Railways Group (JR Group) companies and operates in western Honshu . It has its headquarters in Kita-ku, Osaka . It is listed in the Tokyo Stock Exchange , is a constituent of the TOPIX Large70 index, and is also one of only three Japan Railways Group constituents of the Nikkei 225 index: the others are JR East and JR Central . It was also listed in the Nagoya and Fukuoka stock exchanges until late 2020. JR-West's highest-grossing line

893-772: Is the Sanyo Shinkansen high-speed rail line between Osaka and Fukuoka . The Sanyo Shinkansen alone accounts for about 40% of JR-West's passenger revenues. The company also operates Hakata Minami Line , a short commuter line with Shinkansen trains in Fukuoka . The "Urban Network" is JR-West's name for its commuter rail lines in the Osaka-Kobe-Kyoto metropolitan area. These lines together comprise 610 km of track, have 245 stations and account for about 43% of JR-West's passenger revenues. Urban Network stations are equipped to handle ICOCA fare cards. Train control on these lines

940-611: Is the following: In very rare conditions, oxidation can play a role. Oxidation played a major role in the formation of ancient Lechuguilla Cave in the US state of New Mexico and is presently active in the Frasassi Caves of Italy. The oxidation of sulfides leading to the formation of sulfuric acid can also be one of the corrosion factors in karst formation. As oxygen (O 2 )-rich surface waters seep into deep anoxic karst systems, they bring oxygen, which reacts with sulfide present in

987-593: The Heian period (794–1185) when a shōen manorial estate called Niimi-shō' occupied much of the area of present-day Niimi. In the middle of the Kamakura period , the Niimi clan, served as jito of northern Bitchū and built a castle at Niimi as their residence. After that, the area became the territory of Tō-ji temple in Kyoto and later was under the control of the Amago clan during

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1034-587: The Sanyō Shinkansen , from the separate Shinkansen Holding Corporation. JR-West purchased the line in October 1991 at a cost of 974.1 billion JPY (about US$ 7.2 billion) in long-term debt. JNRSC sold 68.3% of JR-West in an initial public offering on the Tokyo Stock Exchange in October 1996. After JNRSC was dissolved in October 1998, its shares of JR-West were transferred to the government-owned Japan Railway Construction Public Corporation (JRCC), which merged into

1081-688: The Sengoku period . During the early Edo Period , it was part of the holdings of Bitchū-Matsuyama Domain and developed as an important center of inland trade, due to its connection by the Takahashi River with the jōkamachi of Matsuyama. In 1697, the Tokugawa Shogunate established Niimi Domain , which was ruled by the Seki clan to the Meiji restoration . The village of Niimi was established on July 22, 1889 with

1128-626: The range of the Dinaric Alps , stretching from the northeastern corner of Italy above the city of Trieste , across the Balkan peninsula along the coast of the eastern Adriatic to Kosovo and North Macedonia , where the massif of the Šar Mountains begins. The karst zone is at the northwesternmost section, described in early topographical research as a plateau between Italy and Slovenia . Languages preserving this form include Italian : Carso , German : Karst , and Albanian : karsti . In

1175-462: The Kobe and Kyoto lines operate at up to 130 km/h). Those in italics are announcement names. A number of other lines account for more than half of JR-West's track mileage. These lines mainly handle business and leisure travel between smaller cities and rural areas in western Japan. They account for about 20% of the company's passenger revenues. JR-West subsidiaries include the following. JR-West

1222-580: The Okayama Prefectural Board of Education. There is also one private high school, and the prefecture also operates one special education school for the handicapped. Niimi is an important railway center. The city is served by three JR West lines, and all meet at Niimi Station . [REDACTED] JR West (JR West) - Geibi Line [REDACTED] JR West (JR West) - Kishin Line [REDACTED] JR West (JR West) - Hakubi Line Niimi maintains

1269-511: The bedrock. The carbonic acid that causes karst features is formed as rain passes through Earth's atmosphere picking up carbon dioxide (CO 2 ), which readily dissolves in the water. Once the rain reaches the ground, it may pass through soil that provides additional CO 2 produced by soil respiration . Some of the dissolved carbon dioxide reacts with the water to form a weak carbonic acid solution, which dissolves calcium carbonate . The primary reaction sequence in limestone dissolution

1316-450: The complexity of karst aquifers, and need to be supplemented with dye traces , measurement of spring discharges, and analysis of water chemistry. U.S. Geological Survey dye tracing has determined that conventional groundwater models that assume a uniform distribution of porosity are not applicable for karst aquifers. Linear alignment of surface features such as straight stream segments and sinkholes develop along fracture traces . Locating

1363-418: The creation of the modern municipalities system. It was raised to town status on February 26, 1896. Most of the town was destroyed by a fire on April 15, 1938. Niimi was raised to city status on June 1, 1954. On March 31, 2005, Niimi absorbed the towns of Ōsa , Shingō , Tessei and Tetta (all from Atetsu District ) to become a larger and expanded Niimi. Niimi has a mayor-council form of government with

1410-557: The fissures. The enlarged fissures allow a larger quantity of water to enter which leads to a progressive enlargement of openings. Abundant small openings store a large quantity of water. The larger openings form a conduit system that drains the aquifer to springs. Characterization of karst aquifers requires field exploration to locate sinkholes, swallets , sinking streams , and springs in addition to studying geologic maps . Conventional hydrogeologic methods such as aquifer tests and potentiometric mapping are insufficient to characterize

1457-477: The following sister cities . Niimi is known for its limestone caves. They include: Karst Karst ( / k ɑːr s t / ) is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite . It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering -resistant rocks such as quartzite given

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1504-466: The global demand for drinkable water. Farming in karst areas must take into account the lack of surface water. The soils may be fertile enough, and rainfall may be adequate, but rainwater quickly moves through the crevices into the ground, sometimes leaving the surface soil parched between rains. The karst topography also poses peculiar difficulties for human inhabitants. Sinkholes can develop gradually as surface openings enlarge, but progressive erosion

1551-456: The karst groundwater flow rates from 0.5 to 7 miles per day (0.8 to 11.3 km/d). The rapid groundwater flow rates make karst aquifers much more sensitive to groundwater contamination than porous aquifers. Groundwater in karst areas is also just as easily polluted as surface streams, because Karst formations are cavernous and highly permeable, resulting in reduced opportunity for contaminant filtration. Well water may also be unsafe as

1598-525: The karst regions of the Balkans, Cvijić's 1893 publication Das Karstphänomen describes landforms such as karren, dolines and poljes . In a 1918 publication, Cvijić proposed a cyclical model for karst landscape development. Karst hydrology emerged as a discipline in the late 1950s and the early 1960s in France. Previously, the activities of cave explorers, called speleologists , had been dismissed as more of

1645-552: The last-named locality having been declared a site of special scientific interest in respect of it. Kegelkarst is a type of tropical karst terrain with numerous cone-like hills, formed by cockpits, mogotes , and poljes and without strong fluvial erosion processes. This terrain is found in Cuba, Jamaica, Indonesia, Malaysia, the Philippines, Puerto Rico, southern China, Myanmar, Thailand, Laos and Vietnam. Salt karst (or 'halite karst')

1692-412: The local South Slavic languages , all variations of the word are derived from a Romanized Illyrian base (yielding Latin : carsus , Dalmatian : carsus ), later metathesized from the reconstructed form * korsъ into forms such as Slovene : kras and Serbo-Croatian : krš , kras , first attested in the 18th century, and the adjective form kraški in the 16th century. As

1739-637: The most dramatic of these formations can be seen in Thailand 's Phangnga Bay and at Halong Bay in Vietnam . Calcium carbonate dissolved into water may precipitate out where the water discharges some of its dissolved carbon dioxide. Rivers which emerge from springs may produce tufa terraces, consisting of layers of calcite deposited over extended periods of time. In caves, a variety of features collectively called speleothems are formed by deposition of calcium carbonate and other dissolved minerals. Interstratal karst

1786-704: The period. Sedimentation resumed and further limestone strata were deposited on an irregular karst surface, the cycle recurring several times in connection with fluctuating sea levels over prolonged periods. Pseudokarsts are similar in form or appearance to karst features but are created by different mechanisms. Examples include lava caves and granite tors —for example, Labertouche Cave in Victoria, Australia —and paleocollapse features. Mud Caves are an example of pseudokarst. Karst formations have unique hydrology, resulting in many unusual features. A karst fenster (karst window) occurs when an underground stream emerges onto

1833-418: The right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of paleokarst (buried karst in the stratigraphic column )

1880-757: The river flows into a cave in a formation known as the Madison Limestone and then rises again 800 m ( 1 ⁄ 2  mi) down the canyon in a placid pool. A turlough is a unique type of seasonal lake found in Irish karst areas which are formed through the annual welling-up of water from the underground water system. Main Article Aquifer#Karst Karst aquifers typically develop in limestone . Surface water containing natural carbonic acid moves down into small fissures in limestone. This carbonic acid gradually dissolves limestone thereby enlarging

1927-625: The surface between layers of rock, cascades some distance, and then disappears back down, often into a sinkhole. Rivers in karst areas may disappear underground a number of times and spring up again in different places, even under a different name, like Ljubljanica , the "river of seven names". Another example of this is the Popo Agie River in Fremont County, Wyoming , where, at a site named "The Sinks" in Sinks Canyon State Park ,

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1974-415: The surface, complex underground drainage systems (such as karst aquifers ) and extensive caves and cavern systems may form. Erosion along limestone shores, notably in the tropics , produces karst topography that includes a sharp makatea surface above the normal reach of the sea, and undercuts that are mostly the result of biological activity or bioerosion at or a little above mean sea level . Some of

2021-1002: The system ( pyrite or hydrogen sulfide ) to form sulfuric acid (H 2 SO 4 ). Sulfuric acid then reacts with calcium carbonate, causing increased erosion within the limestone formation. This chain of reactions is: This reaction chain forms gypsum . The karstification of a landscape may result in a variety of large- or small-scale features both on the surface and beneath. On exposed surfaces, small features may include solution flutes (or rillenkarren), runnels , limestone pavement (clints and grikes), kamenitzas collectively called karren or lapiez. Medium-sized surface features may include sinkholes or cenotes (closed basins), vertical shafts, foibe (inverted funnel shaped sinkholes), disappearing streams, and reappearing springs . Large-scale features may include limestone pavements , poljes , and karst valleys. Mature karst landscapes, where more bedrock has been removed than remains, may result in karst towers , or haystack/eggbox landscapes. Beneath

2068-461: The water may have run unimpeded from a sinkhole in a cattle pasture, bypassing the normal filtering that occurs in a porous aquifer . Sinkholes have often been used as farmstead or community trash dumps . Overloaded or malfunctioning septic tanks in karst landscapes may dump raw sewage directly into underground channels. Geologists are concerned with these negative effects of human activity on karst hydrology which, as of 2007 , supplied about 25% of

2115-507: The western Highland Rim in the eastern United States is at the second-highest risk of karst sinkholes. In Canada, Wood Buffalo National Park , Northwest Territories contains areas of karst sinkholes. Mexico hosts important karst regions in the Yucatán Peninsula and Chiapas . The West of Ireland is home to The Burren , a karst limestone area. The South China Karst in the provinces of Guizhou , Guangxi , and Yunnan provinces

2162-440: Was 36.8 °C (98.2 °F) on 7 August 1994; the coldest temperature ever recorded was −14.9 °C (5.2 °F) on 28 February 1981. Per Japanese census data, the population of Niimi in 2020 was 28,079 people. Niimi has been conducting censuses since 1920. Niimi was part of ancient Bitchū Province and was divided between Aga District and Tetsuta District by the Takahashi River. It appears in documentary records as early as

2209-518: Was incorporated as a business corporation ( kabushiki kaisha ) on April 1, 1987, as part of the breakup of the state-owned Japanese National Railways (JNR). Initially, it was a wholly owned subsidiary of the JNR Settlement Corporation (JNRSC), a special company created to hold the assets of the former JNR while they were shuffled among the new JR companies. For the first four years of its existence, JR-West leased its highest-revenue line,

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