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Kvinnherad

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Kvinnherad is a municipality in Vestland county, Norway . It is located in the traditional district of Sunnhordland , along the Hardangerfjorden . The municipality was the 5th in size in former Hordaland county.

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74-399: The administrative centre of the municipality is the village of Rosendal . The largest village is Husnes , with about 6,000 people living in or near the village. Other villages include Ænes , Åkra , Dimmelsvik , Eidsvik , Hatlestrand , Herøysund , Høylandsbygd , Ølve , Sæbøvik , Sundal , Sunde , Uskedal , and Valen . The 1,091-square-kilometre (421 sq mi) municipality

148-404: A chef-lieu ( French pronunciation: [ʃɛfljø] , plural form chefs-lieux , literally 'chief place' or 'main place'), is a town or city that is important from an administrative perspective. The capital of an Algerian province is called a chef-lieu . The capital of a district , the next largest division, is also called a chef-lieu , whilst the capital of the lowest division,

222-424: A lake , bay or ocean but joins another river (a parent river). Sometimes also called a branch or fork. A distributary , or a distributary channel , is a stream that branches off and flows away from a main stream channel, and the phenomenon is known as river bifurcation . Distributaries are common features of river deltas , and are often found where a valleyed stream enters wide flatlands or approaches

296-403: A bed armor layer, and other depositional features, plus well defined banks due to bank erosion, are good identifiers when assessing for perennial streams. Particle size will help identify a perennial stream. Perennial streams cut through the soil profile, which removes fine and small particles. By assessing areas for relatively coarse material left behind in the stream bed and finer sediments along

370-662: A central city as chef-lieu of delegation . In the United Kingdom it is the centre of a local authority , which is distinct from a historic county with a county town. Stream A stream is a continuous body of surface water flowing within the bed and banks of a channel . Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long, large streams are usually called rivers , while smaller, less voluminous and more intermittent streams are known as streamlets , brooks or creeks . The flow of

444-658: A continuous aquatic habitat until they reach maturity. Crayfish and other crustaceans , snails , bivalves (clams), and aquatic worms also indicate the stream is perennial. These require a persistent aquatic environment for survival. Fish and amphibians are secondary indicators in assessment of a perennial stream because some fish and amphibians can inhabit areas without persistent water regime. When assessing for fish, all available habitat should be assessed: pools, riffles, root clumps and other obstructions. Fish will seek cover if alerted to human presence, but should be easily observed in perennial streams. Amphibians also indicate

518-470: A continuous or intermittent stream. The same non-perennial channel might change characteristics from intermittent to ephemeral over its course. Washes can fill up quickly during rains, and there may be a sudden torrent of water after a thunderstorm begins upstream, such as during monsoonal conditions. In the United States, an intermittent or seasonal stream is one that only flows for part of

592-409: A district ( liwa ), or a governorate ( muhafazah ). Luxembourg is divided into two judicial arrondissements (Luxembourg City, Diekirch), four electoral circonscriptions (constituencies), twelve cantons , as well as 100 communes (municipalities; Luxembourgish: Gemengen ). Arrondissements, districts and cantons have each a chef-lieu and are named after it. The same is true for each commune which

666-422: A drainage network. Although each tributary has its own source, international practice is to take the source farthest from the river mouth as the source of the entire river system, from which the most extended length of the river measured as the starting point is taken as the length of the whole river system, and that furthest starting point is conventionally taken as the source of the whole river system. For example,

740-404: A path into mines or other underground chambers. According to official U.S. definitions, the channels of intermittent streams are well-defined, as opposed to ephemeral streams, which may or may not have a defined channel, and rely mainly on storm runoff, as their aquatic bed is above the water table . An ephemeral stream does not have the biological, hydrological, and physical characteristics of

814-412: A perennial stream and include tadpoles , frogs , salamanders , and newts . These amphibians can be found in stream channels, along stream banks, and even under rocks. Frogs and tadpoles usually inhabit shallow and slow moving waters near the sides of stream banks. Frogs will typically jump into water when alerted to human presence. Well defined river beds composed of riffles, pools, runs, gravel bars,

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888-483: A perennial stream, fine sediment may cling to riparian plant stems and tree trunks. Organic debris drift lines or piles may be found within the active overbank area after recent high flow. Streams, headwaters, and streams flowing only part of the year provide many benefits upstream and downstream. They defend against floods, remove contaminants, recycle nutrients that are potentially dangerous as well as provide food and habitat for many forms of fish. Such streams also play

962-406: A slow-moving wetted channel or stagnant area. This is evidence that iron-oxidizing bacteria are present, indicating persistent expression of oxygen-depleted ground water. In a forested area, leaf and needle litter in the stream channel is an additional indicator. Accumulation of leaf litter does not occur in perennial streams since such material is continuously flushed. In the adjacent overbank of

1036-486: A stream as intermittent, "showing interruptions in time or space". Generally, streams that flow only during and immediately after precipitation are termed ephemeral . There is no clear demarcation between surface runoff and an ephemeral stream, and some ephemeral streams can be classed as intermittent—flow all but disappearing in the normal course of seasons but ample flow (backups) restoring stream presence — such circumstances are documented when stream beds have opened up

1110-424: A stream is a critical factor in determining its character and is entirely determined by its base level of erosion. The base level of erosion is the point at which the stream either enters the ocean, a lake or pond, or enters a stretch in which it has a much lower gradient, and may be specifically applied to any particular stretch of a stream. In geological terms, the stream will erode down through its bed to achieve

1184-574: A stream is controlled by three inputs – surface runoff (from precipitation or meltwater ), daylighted subterranean water , and surfaced groundwater ( spring water ). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in

1258-524: A thin layer called sheet wash, combined with a network of tiny rills, which together form the sheet runoff; when this water is focused in a channel, a stream is born. Some rivers and streams may begin from lakes or ponds. Freshwater's primary sources are precipitation and mountain snowmelt. However, rivers typically originate in the highlands, and are slowly created by the erosion of mountain snowmelt into lakes or rivers. Rivers usually flow from their source topographically, and erode as they pass until they reach

1332-627: A vital role in preserving our drinking water quality and supply, ensuring a steady flow of water to surface waters and helping to restore deep aquifers. The extent of land basin drained by a stream is termed its drainage basin (also known in North America as the watershed and, in British English, as a catchment). A basin may also be composed of smaller basins. For instance, the Continental Divide in North America divides

1406-414: Is a large natural stream that is much wider and deeper than a creek and not easily fordable, and may be a navigable waterway . The linear channel between the parallel ridges or bars on a shoreline beach or river floodplain, or between a bar and the shore. Also called a swale . A tributary is a contributory stream to a larger stream, or a stream which does not reach a static body of water such as

1480-506: Is a term commonly ascribed to the settlement that serves as a municipal administrative centre. This level handles the local administrative and political tasks of the surrounding settlements. Since central place theory was the guiding principle during the municipal reform 1962–1977, most municipalities were dominated by a larger urban area where the political seat was located. Most municipalities are named for their central locality, but there are several exceptions. There are many deviations from

1554-599: Is composed of more than one town or village. Usually (with a few exceptions), the commune is named after the communal chef-lieu. In Russia , several million-plus cities in federal districts have the official status of an administrative centre: Moscow (as the main city of the Central Federal District ), Vladivostok , Volgograd , Yekaterinburg , Nizhny Novgorod , Novosibirsk , Pyatigorsk , Rostov-on-Don and St. Petersburg . The main cities of regions and municipal districts are also called unofficially

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1628-547: Is governed by a municipal council of directly elected representatives. The mayor is indirectly elected by a vote of the municipal council. The municipality is under the jurisdiction of the Haugaland og Sunnhordland District Court and the Gulating Court of Appeal . The municipal council ( Kommunestyre ) of Kvinnherad is made up of 35 representatives that are elected to four year terms. The tables below show

1702-441: Is known as surface hydrology and is a core element of environmental geography . A brook is a stream smaller than a creek, especially one that is fed by a spring or seep . It is usually small and easily forded . A brook is characterised by its shallowness. A creek ( / k r iː k / ) or crick ( / k r ɪ k / ): In hydrography, gut is a small creek; this is seen in proper names in eastern North America from

1776-425: Is sometimes termed a "young" or "immature" stream, and the later state a "mature" or "old" stream. Meanders are looping changes of direction of a stream caused by the erosion and deposition of bank materials. These are typically serpentine in form. Typically, over time the meanders gradually migrate downstream. If some resistant material slows or stops the downstream movement of a meander, a stream may erode through

1850-546: Is the 104th largest by area out of the 356 municipalities in Norway. Kvinnherad is the 93rd most populous municipality in Norway with a population of 13,058. The municipality's population density is 12.5 inhabitants per square kilometre (32/sq mi) and its population has decreased by 1.9% over the previous 10-year period. In the southern part of Kvinnherad you will find the typical fjord landscape of western Norway . The areas of Mauranger and Rosendal are said to have about

1924-456: Is usually called a creek and marked on topographic maps with a solid blue line. There are five generic classifications: "Macroinvertebrate" refers to easily seen invertebrates , larger than 0.5 mm, found in stream and river bottoms. Macroinvertebrates are larval stages of most aquatic insects and their presence is a good indicator that the stream is perennial. Larvae of caddisflies , mayflies , stoneflies , and damselflies require

1998-594: The Folgefonna glacier , is partially located in Kvinnherad. The northern part of the municipality is often referred to as Mauranger . It is the area surrounding the Maurangsfjorden . The notable Bondhusbreen glacier is located just south of that fjord, near the village of Sundal . The Jondal Tunnel and Folgefonna Tunnel both connect Mauranger with neighboring Odda and Jondal by cutting through

2072-501: The Stockholm metropolitan area . The term central locality has no legal standing and it is unclear how it should be applied to these municipalities. Some municipalities appointing one or several localities to be the central locality. A residence city (Swedish: "residensstad") is the town or city which is the political and administrative seat of the county . This level handles the more regional political and administrative tasks of

2146-691: The Tombigbee River basin. Continuing in this vein, a component of the Mississippi River basin is the Ohio River basin, which in turn includes the Kentucky River basin, and so forth. Stream crossings are where streams are crossed by roads , pipelines , railways , or any other thing which might restrict the flow of the stream in ordinary or flood conditions. Any structure over or in a stream which results in limitations on

2220-512: The Västra Götaland Region . The term chef-lieu is applied to the capital of each Swiss canton . In 16 of the 26 cantons, the territory is subdivided into districts. Every district also has a location nominated as chef-lieu and each has a prefect. The term chef-lieu is used to designate the capital of each gouvernorat (department). Each of the 24 gouvernorats is subdivided into delegations (districts) which each have

2294-713: The coastal plains around a lake or an ocean . They can also occur inland, on alluvial fans , or where a tributary stream bifurcates as it nears its confluence with a larger stream. Common terms for individual river distributaries in English-speaking countries are arm and channel . There are a number of regional names for a stream. A stream's source depends on the surrounding landscape and its function within larger river networks. While perennial and intermittent streams are typically supplied by smaller upstream waters and groundwater, headwater and ephemeral streams often derive most of their water from precipitation in

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2368-588: The confluence of two blue rivers into one on a white or silver background. The rivers symbolize the many streams and rivers in the municipality, especially the Hattebergselvi and the Melselvi, that come together just before they run into the sea at Rosendal . The arms were designed by Truls Nygaard, after a proposal by Magnus Hardeland. The municipal flag has the same design as the coat of arms. The Church of Norway has nine parishes ( sokn ) within

2442-473: The municipalities , is called agglomération de chef-lieu (chef-lieu agglomeration ) and is abbreviated as A.C.L. The chef-lieu in Belgium is the administrative centre of each of the ten provinces of Belgium . Three of these cities also give their name to their province ( Antwerp , Liège and Namur ). The chef-lieu of a département is known as the préfecture . This is the town or city where

2516-469: The prefect of the department (and all services under their control) are situated, in a building known as the prefecture . In every French region , one of the departments has pre-eminence over the others, and the prefect carries the title of Prefect of region X..., Prefect of Department Z... and the city where the regional prefect is found is known as chef-lieu of the region or, more commonly, Regional prefecture . The services are, however, controlled by

2590-638: The shipping mural in Høylandsbygd , and Radiohola . Rosendal, the administrative centre of the municipality, is the site of the greatest tourist attraction in Kvinnherad: the Barony Rosendal . The Barony is the only one of its kind in Norway. It is a museum, which offers valuable information about the Union with Denmark, an important period of Norwegian history. It was one of the locations of

2664-480: The velocity of the stream. A perennial stream is one which flows continuously all year. Some perennial streams may only have continuous flow in segments of its stream bed year round during years of normal rainfall. Blue-line streams are perennial streams and are marked on topographic maps with a solid blue line. The word "perennial" from the 1640s, meaning "evergreen," is established in Latin perennis, keeping

2738-416: The water cycle , instruments in groundwater recharge , and corridors for fish and wildlife migration. The biological habitat in the immediate vicinity of a stream is called a riparian zone . Given the status of the ongoing Holocene extinction , streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity . The study of streams and waterways in general

2812-512: The 1958 film "The Vikings" starring Kirk Douglas, Tony Curtis, Janet Leigh and Ernest Borgnine. Many of the citizens of Kvinnherad/Hardanger, Norway were used as extras. Administrative centre An administrative centre is a seat of regional administration or local government, or a county town , or the place where the central administration of a commune , is located. In countries with French as administrative language (such as Belgium, Luxembourg, Switzerland and many African countries),

2886-584: The 1960s, there were many municipal mergers across Norway due to the work of the Schei Committee . On 1 January 1965, the following areas were merged into one large municipality of Kvinnherad: On 1 January 2013, the southwestern part of the Folgefonna peninsula (south of Kysnesstranda) was transferred from Kvinnherad to the neighboring Jondal municipality. This removed forty residents and 37.1 square kilometres (14.3 sq mi) of land area from

2960-480: The 1990s, the chef-lieu has transitioned from the location of the Governor, Commandant, or Prefect and their staff, to the location of Commune, Cercles of Mali / Departments of Niger , and Regional Councils and a variety of decentralized bodies. The chefs-lieux of a Region, Cercle or Département, is usually also a Communal chef-lieu. Both nations collect these councils in a "High Council of Collectivites" seated at

3034-840: The Mid-Atlantic states (for instance, The Gut in Pennsylvania, Ash Gut in Delaware, and other streams) down into the Caribbean (for instance, Guinea Gut , Fish Bay Gut , Cob Gut , Battery Gut and other rivers and streams in the United States Virgin Islands , in Jamaica (Sandy Gut, Bens Gut River, White Gut River), and in many streams and creeks of the Dutch Caribbean ). A river

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3108-499: The administration being devolved usually to the Secretary-general of the departmental prefecture , who functions as sub-prefect for the arrondissement. The chef-lieu of a canton is usually the biggest city or town within the canton, but has only a nominal role. No specific services are controlled by it. In past decades, there was always a Gendarmerie , a treasurer and a justice of the peace. The chef-lieu indicates

3182-430: The administrative centre or simply the centre. The only exception to this rule is the republics , for which the term " capital " is used to refer to the seat of government. The capital of Russia is also an entity to which the term "administrative centre" does not apply. In Sweden there are two levels of administrative centre; the local municipal and the regional county . Central locality ( Swedish : "centralort")

3256-501: The administrative subdivisions down to the Commune level each have a formal place of administrative headquarters, titled the chef-lieu. The larger portion of the terminology of administrative division is inherited from colonial rule as part of French West Africa , and has survived and been somewhat modified over time. In both nations there have been remarkably parallel histories. With the decentralization process begun in both nations in

3330-533: The atmosphere either by evaporation from soil and water bodies, or by plant evapotranspiration. By infiltration some of the water sinks into the earth and becomes groundwater, much of which eventually enters streams. Most precipitated water is partially bottled up by evaporation or freezing in snow fields and glaciers. The majority of the water flows as a runoff from the ground; the proportion of this varies depending on several factors, such as climate, temperature, vegetation, types of rock, and relief. This runoff begins as

3404-525: The base level of erosion throughout its course. If this base level is low, then the stream will rapidly cut through underlying strata and have a steep gradient, and if the base level is relatively high, then the stream will form a flood plain and meander. Typically, streams are said to have a particular elevation profile , beginning with steep gradients, no flood plain, and little shifting of channels, eventually evolving into streams with low gradients, wide flood plains, and extensive meanders. The initial stage

3478-597: The base stage of erosion. The scientists have offered a way based on data to define the origin of the lake. A classified sample was the one measured by the Chinese researchers from the University of Chinese Academy of Sciences. As an essential symbol of the river formation environment, the river source needs an objective and straightforward and effective method of judging . A calculation model of river source catchment area based on critical support flow (CSD) proposed, and

3552-450: The central locality principle. Some municipalities are dominated by two or more towns of similar size, and sometimes they share the municipal administration, with the municipality having its official address in one of the towns. For example, both Skillingaryd and Vaggeryd are central localities of Vaggeryd Municipality . Conversely, there are municipalities within metropolitan areas . For example, there are twenty-six municipalities within

3626-504: The county, such as healthcare and public transport . The name comes from that this is the town or city where the governor ( Swedish : "landshövding") have their residence . There are some exceptions to this, however. In the newer amalgamated "greater counties", often referred to as "regions", the administrative centre is placed in one of the older residence cities . Examples of this is Malmö in Region Scania and Gothenburg in

3700-484: The current and historical composition of the council by political party . The mayors ( Nynorsk : ordførar ) of Kvinnherad: The municipality is located along the large Hardangerfjorden , mostly on the southeast side of the fjord on the Folgefonna peninsula, but also a small part on the other side. It includes several notable islands in the fjord including Varaldsøy , Fjelbergøya , Borgundøya , and Halsnøya . The large Folgefonna National Park , which surrounds

3774-707: The flow is reduced to a trickle or less. Typically torrents have Apennine rather than Alpine sources, and in the summer they are fed by little precipitation and no melting snow. In this case the maximum discharge will be during the spring and autumn. An intermittent stream can also be called a winterbourne in Britain, a wadi in the Arabic -speaking world or torrente or rambla (this last one from arabic origin) in Spain and Latin America. In Australia, an intermittent stream

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3848-447: The form of rain and snow. Most of this precipitated water re-enters the atmosphere by evaporation from soil and water bodies, or by the evapotranspiration of plants. Some of the water proceeds to sink into the earth by infiltration and becomes groundwater, much of which eventually enters streams. Some precipitated water is temporarily locked up in snow fields and glaciers , to be released later by evaporation or melting. The rest of

3922-532: The lake has significant feeder rivers. The Kagera River, which flows into Lake Victoria near Bukoba's Tanzanian town , is the longest feeder, though sources do not agree on which is the Kagera's longest tributary and therefore the Nile's most remote source itself. To qualify as a stream, a body of water must be either recurring or perennial. Recurring (intermittent) streams have water in the channel for at least part of

3996-476: The large mountains surrounding Mauranger. The municipality has many large lakes including Blådalsvatnet , Juklavatnet , and Onarheimsvatnet . Many of these lakes are utilized for hydroelectric power generation. Kvinnherad is a popular tourist location because of its natural landscape as well as several places of interest. The most notable of which include Kvinnherad Church , the Bondhusbreen glacier,

4070-683: The mainly easterly-draining Atlantic Ocean and Arctic Ocean basins from the largely westerly-flowing Pacific Ocean basin. The Atlantic Ocean basin, however, may be further subdivided into the Atlantic Ocean and Gulf of Mexico drainages. (This delineation is termed the Eastern Continental Divide .) Similarly, the Gulf of Mexico basin may be divided into the Mississippi River basin and several smaller basins, such as

4144-412: The meaning as "everlasting all year round," per "over" plus annus "year." This has been proved since the 1670s by the "living years" in the sense of botany. The metaphorical sense of "enduring, eternal" originates from 1750. They are related to "perennial." See biennial for shifts in vowels. Perennial streams have one or more of these characteristics: Absence of such characteristics supports classifying

4218-453: The most beautiful fjord landscape of Hardanger as a whole: narrow fjords, wild water-falls, and the nearby Folgefonna , the third biggest glacier in Norway. The parish of Qvindherred was established as a municipality on 1 January 1838 (see formannskapsdistrikt law). On 1 January 1907, a small area northwest of the villages of Ølve and Husa (population: 67) was transferred from neighboring Tysnes municipality to Kvinnherad. During

4292-623: The municipality of Kvinnherad. It is part of the Sunnhordland prosti ( deanery ) in the Diocese of Bjørgvin . The economy of Kvinnherad is based on the rich water resources within its boundaries. This includes power production , aluminium production ( Sør-Norge Aluminium ), fish farming , shipbuilding ( Eidsvik Skipsbyggeri , Hellesøy Verft , Bergen Group Halsnøy ), and lifeboat production ( Umoe Schat-Harding , Norsafe , Eide Marine Tech , Noreq ). These industries are spread throughout

4366-406: The municipality. Kvinnherad has two local newspapers, Kvinnheringen and Grenda , as well as a local TV channel, TV Sydvest . Kvinnherad Municipality is responsible for primary education (through 10th grade), outpatient health services , senior citizen services, welfare and other social services , zoning , economic development , and municipal roads and utilities. The municipality

4440-483: The municipality. The municipality (originally the parish ) is named after the old name for the area ( Old Norse : Kvinnaherað ). The first element may be derived from the word tvinnr which means "double", likely referring to the two rivers running through Rosendal , the administrative centre of the municipality. The last element is herað which means "district" or "countryside". The municipal name has been spelled several ways throughout history. Before 1889,

4514-431: The name was written Quindherred , then in 1889 the spelling was "modernized" to Kvinnherred . At that time, all municipalities in Norway were titled herred (which was used similarly to the word "municipality"), so it was formally named Kvinnherred herred , which looked a little repetitive. On 3 November 1917, a royal resolution changed the spelling of the name of the municipality to Kvinnherad . The coat of arms

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4588-644: The nation's capital. Smaller sub-divisions in Mali's Communes (Villages, Tribal councils, Quarters) are administered from or identified as a Place / Site ( Site in French), so the chef-lieu is literally the Chief-Place even at the lowest level. In the Hashemite Kingdom of Jordan , the administrative centres are known as "chief towns" or nahias . Nahias may be in charge of a sub-district ( qda ),

4662-453: The neck between two legs of a meander to become temporarily straighter, leaving behind an arc-shaped body of water termed an oxbow lake or bayou . A flood may also cause a meander to be cut through in this way. The stream load is defined as the solid matter carried by a stream. Streams can carry sediment, or alluvium. The amount of load it can carry (capacity) as well as the largest object it can carry (competence) are both dependent on

4736-596: The origin of the Nile River is the confluence of the White Nile and the Blue Nile, but the source of the whole river system is in its upper reaches. If there is no specific designation, "length of the Nile" refers to the "river length of the Nile system", rather than to the length of the Nile river from the point where it is formed by a confluence of tributaries. The Nile's source is often cited as Lake Victoria, but

4810-405: The prefecture of the department. The chef-lieu of an arrondissement , commonly known as the sous-préfecture is the city or town where the sub-prefect of the arrondissement (and the services directly under their control) are situated, in a building called the sub-prefecture . The arrondissement where the département prefecture is located does not normally have a sub-prefect or sub-prefecture,

4884-469: The principal city of the provinces of New Caledonia. So Nouméa is the chef-lieu of South Province. But the chef-lieu can also mean the principal area within a town. So Wé is part of the town of Lifou , but is the chef-lieu of Lifou. In the Loyalty Islands and the other islands, the name of the chef-lieu differs from that of the name of the town. For the towns of the mainland, the chef-lieu has

4958-469: The relationship between CSA and CSD with a minimum catchment area established. Using the model for comparison in two basins in Tibet (Helongqu and Niyang River White Water), the results show that the critical support flow (Qc) of the housing dragon song is 0.0028 m /s. At the same time, the white water curvature is 0.0085 m /s. Besides, the critical support flow can vary with hydrologic climate conditions, and

5032-596: The same name as the town. Nouméa is a town composed only of Nouméa. Many of the West African states which gained independence from France in the mid-20th century also inherited the French administrative structure of Departments and Communes, headed by a Chief-Lieu . States still using Chief-Lieu to identify the administrative headquarters of a government subdivision include Senegal , Burkina Faso , Benin , Mali , and Niger . Taking Niger and Mali as examples,

5106-425: The side of the stream or within the floodplain will be a good indicator of persistent water regime. A perennial stream can be identified 48 hours after a storm. Direct storm runoff usually has ceased at this point. If a stream is still flowing and contributing inflow is not observed above the channel, the observed water is likely baseflow. Another perennial stream indication is an abundance of red rust material in

5180-655: The vital support flow Qc in wet areas (white water) is larger than in semi-arid regions (heap slot). The proposed critical support flow (CSD) concept and model method can be used to determine the hydrographic indicators of river sources in complex geographical areas, and it can also reflect the impact of hydrologic climate change on river recharge in different regions. The source of a river or stream (its point of origin) can consist of lakes, swamps, springs, or glaciers. A typical river has several tributaries; each of these may be made up of several other smaller tributaries, so that together this stream and all its tributaries are called

5254-512: The water flows off the land as runoff, the proportion of which varies according to many factors, such as wind, humidity, vegetation, rock types, and relief. This runoff starts as a thin film called sheet wash, combined with a network of tiny rills, together constituting sheet runoff; when this water is concentrated in a channel, a stream has its birth. Some creeks may start from ponds or lakes. The streams typically derive most of their water from rain and snow precipitation. Most of this water re-enters

5328-521: The year and is marked on topographic maps with a line of blue dashes and dots. A wash , desert wash, or arroyo is normally a dry streambed in the deserts of the American Southwest , which flows after sufficient rainfall. In Italy, an intermittent stream is termed a torrent ( Italian : torrente ). In full flood the stream may or may not be "torrential" in the dramatic sense of the word, but there will be one or more seasons in which

5402-402: The year. A stream of the first order is a stream which does not have any other recurring or perennial stream feeding into it. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream. Streams of lower order joining a higher order stream do not change the order of the higher stream. The gradient of

5476-408: Was granted on 18 June 1982. The official blazon is " Argent , a pall wavy azure " ( Norwegian : På kvit grunn ein blå gaffelkross laga med bølgjesnitt ). This means the arms have a field (background) has a tincture of argent which means it is commonly colored white, but if it is made out of metal, then silver is used. The ordinary is a pall with wavy edges. The design of the arms show

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