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102-701: The River Sow / s aʊ / is a tributary of the River Trent in Staffordshire , England , and is the river that flows through Stafford . The river rises to the south of Loggerheads , near Broughton and flows south-east beside the villages of Fairoak, Bishop's Offley and Walk Mill until it reaches Cop Mere . East of the Mere the river is joined by the Brockton Brook before it flows past Eccleshall and its castle. The Sow continues south-east passing Chebsey, where it

204-459: A band of Triassic Sherwood sandstone at Sandon, and it meets the same sandstone again as it flows beside Cannock Chase, between Great Haywood and Armitage, there is also another outcrop between Weston-on-Trent and King's Mill. Downstream of Armitage the solid geology is primarily Mercia Mudstones , the course of the river following the arc of these mudstones as they pass through the Midlands all

306-400: A bridge ( German : Brücke , f. ) more often used the words 'beautiful', 'elegant', 'pretty', and 'slender', while Spanish speakers, whose word for bridge is masculine ( puente , m. ), used 'big', 'dangerous', 'strong', and 'sturdy' more often. However, studies of this kind have been criticized on various grounds and yield an unclear pattern of results overall. A noun may belong to

408-669: A considerable deterioration in the water quality of both the Trent and its tributaries, especially the Tame. To bring clean water to the West Midlands, Birmingham Corporation created a large reservoir chain and aqueduct system to bring water from the Elan Valley . Underlying the upper reaches of the Trent, are formations of Millstone Grit and Carboniferous Coal Measures which include layers of sandstones, marls and coal seams. The river crosses

510-401: A given class because of characteristic features of its referent , such as sex, animacy, shape, although in some instances a noun can be placed in a particular class based purely on its grammatical behavior. Some authors use the term "grammatical gender" as a synonym of "noun class", but others use different definitions for each. Many authors prefer "noun classes" when none of the inflections in

612-590: A grander design, diverting the river east towards the Wash such that he would benefit from a much larger share of the divided Kingdom. Downstream of Burton upon Trent , the river increasingly trends northwards, cutting off a portion of Nottinghamshire and nearly all of Lincolnshire from his share, north of the Trent. The idea for this scene, may have been based on the disagreement regarding a mill weir near Shelford Manor , between local landowners Gilbert Talbot, Earl of Shrewsbury , and Sir Thomas Stanhope which culminated with

714-445: A language relate to sex, such as when an animate –inanimate distinction is made. Note, however, that the word "gender" derives from Latin genus (also the root of genre ) which originally meant "kind", so it does not necessarily have a sexual meaning. A classifier, or measure word , is a word or morpheme used in some languages together with a noun, principally to enable numbers and certain other determiners to be applied to

816-462: A language which uses classifiers normally has a number of different ones, used with different sets of nouns. These sets depend largely on properties of the things that the nouns denote (for example, a particular classifier may be used for long thin objects, another for flat objects, another for people, another for abstracts, etc.), although sometimes a noun is associated with a particular classifier more by convention than for any obvious reason. However it

918-675: A long diversion channel being dug to bypass the mill. This took place in 1593 so would have been a contemporary topic in the Shakespearean period. During the Pleistocene epoch (1.7 million years ago), the River Trent rose in the Welsh hills and flowed almost east from Nottingham through the present Vale of Belvoir to cut a gap through the limestone ridge at Ancaster and thence to the North Sea. At

1020-500: A low pressure weather system, produced elevated tidal river levels in the lower reaches. The resulting surge overtopped the flood defences in the area near Keadby and Burringham, flooding 50 properties. The fifth largest flood recorded at Nottingham occurred in November 2000 , with widespread flooding of low-lying land along the Trent valley, including many roads and railways. The flood defences around Nottingham and Burton constructed during

1122-417: A noun manifests itself in two principal ways: in the modifications that the noun itself undergoes, and in modifications of other related words ( agreement ). Grammatical gender manifests itself when words related to a noun like determiners , pronouns or adjectives change their form ( inflect ) according to the gender of noun they refer to ( agreement ). The parts of speech affected by gender agreement,

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1224-604: A quarter of the total flow for the Trent, with the other significant tributaries being the Derwent at 18%, Soar 17%, the Dove 13%, and the Sow 8%. Four of these main tributaries, including the Dove and Derwent which drain the upland Peak District, all join within the middle reaches, giving rise to a comparatively energetic river system for the UK. Rainfall in the catchment generally follows topography with

1326-624: A rapid thaw. Due to the size of the flood and the ice entrained in the flow, nearly every bridge along the Trent was badly damaged or washed away. The bridges at Wolseley, Wychnor and the main span at Swarkestone were all destroyed. In Nottingham, residents of Narrow Marsh were trapped by the floodwaters in their first floor rooms, boats were used to take supplies to those stranded. Livestock was badly affected, 72 sheep drowned in Wilford and ten cows were lost in Bridgford. The vulnerable flood bank at Spalford

1428-467: A single season, and depths of 1.5 metres (5 ft) have been accumulated over time at some locations. A number of the smaller Trent tributaries are still named as warping drains, such as Morton warping drain, near Gainsborough. Warp was also used as a commercial product, after being collected from the river banks at low tide, it was transported along the Chesterfield Canal to Walkeringham where it

1530-497: A system include later forms of Proto-Indo-European (see below ), Sanskrit , some Germanic languages , most Slavic languages , a few Romance languages ( Romanian , Asturian and Neapolitan ), Marathi , Latin , and Greek . Here nouns that denote animate things (humans and animals) generally belong to one gender, and those that denote inanimate things to another (although there may be some deviation from that principle). Examples include earlier forms of Proto-Indo-European and

1632-527: A way that sounds like the masculine declensions in South-Eastern Norwegian dialects. The same does not apply to Swedish common gender, as the declensions follow a different pattern from both the Norwegian written languages. Norwegian Nynorsk , Norwegian Bokmål and most spoken dialects retain masculine, feminine and neuter even if their Scandinavian neighbors have lost one of the genders. As shown,

1734-494: A well-documented example being the meander cutoff at Sawley . The river's propensity to change course is referred to in Shakespeare 's play Henry IV, Part 1 : Methinks my moiety, north from Burton here, In quantity equals not one of yours: See how this river comes me cranking in, And cuts me from the best of all my land A huge half-moon, a monstrous cantle out. I'll have the current in this place damm'd up; And here

1836-485: Is a third available gender, so nouns with sexless or unspecified-sex referents may be either masculine, feminine, or neuter. There are also certain exceptional nouns whose gender does not follow the denoted sex, such as the German Mädchen , meaning "girl", which is neuter. This is because it is actually a diminutive of "Magd" and all diminutive forms with the suffix -chen are neuter. Examples of languages with such

1938-529: Is also found in Dravidian languages . (See below .) It has been shown that grammatical gender causes a number of cognitive effects. For example, when native speakers of gendered languages are asked to imagine an inanimate object speaking, whether its voice is male or female tends to correspond to the grammatical gender of the object in their language. This has been observed for speakers of Spanish, French, and German, among others. Caveats of this research include

2040-515: Is also possible for a given noun to be usable with any of several classifiers; for example, the Mandarin Chinese classifier 个 ( 個 ) gè is frequently used as an alternative to various more specific classifiers. Grammatical gender can be realized as inflection and can be conditioned by other types of inflection, especially number inflection, where the singular-plural contrast can interact with gender inflection. The grammatical gender of

2142-613: Is assigned to one of the genders, and few or no nouns can occur in more than one gender. Gender is considered an inherent quality of nouns, and it affects the forms of other related words, a process called "agreement" . Nouns may be considered the "triggers" of the process, whereas other words will be the "target" of these changes. These related words can be, depending on the language: determiners , pronouns , numerals , quantifiers , possessives , adjectives , past and passive participles , articles , verbs , adverbs , complementizers , and adpositions . Gender class may be marked on

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2244-431: Is described on an old map as 'Old Trent Water', records show that this was once the main navigable route, with the river having switched to a more northerly course in the 18th century. Farther downstream at Hemington , archaeologists have found the remains of a medieval bridge across another abandoned channel. Researchers using aerial photographs and historical maps have identified many of these palaeochannel features,

2346-523: Is joined by the Meece Brook before reaching the mill at Worston and then Little and Great Bridgeford . The river then flows through the nature reserve of Doxey Marshes until it reaches Stafford, where it flows through Victoria park. Beyond the town at Baswich the Sow is joined by its largest tributary the River Penk , it then continues beneath the bridge between Milford and Tixall until it flows through

2448-418: Is masculine (meaning "lake") its genitive singular form is Sees , but when it is feminine (meaning "sea"), the genitive is See , because feminine nouns do not take the genitive -s . Gender is sometimes reflected in other ways. In Welsh , gender marking is mostly lost on nouns; however, Welsh has initial mutation , where the first consonant of a word changes into another in certain conditions. Gender

2550-416: Is one of the factors that can cause one form of mutation (soft mutation). For instance, the word merch "girl" changes into ferch after the definite article . This only occurs with feminine singular nouns: mab "son" remains unchanged. Adjectives are affected by gender in a similar way. Additionally, in many languages, gender is often closely correlated with the basic unmodified form ( lemma ) of

2652-450: Is only partially valid, and many nouns may belong to a gender category that contrasts with their meaning, e.g. the word for "manliness" could be of feminine gender, as it is in French with "la masculinité" and "la virilité". In such a case, the gender assignment can also be influenced by the morphology or phonology of the noun, or in some cases can be apparently arbitrary. Usually each noun

2754-415: Is reserved for abstract concepts derived from adjectives: such as lo bueno , lo malo ("that which is good/bad"). Natural gender refers to the biological sex of most animals and people, while grammatical gender refers to certain phonetic characteristics (the sounds at the end, or beginning) of a noun. Among other lexical items, the definite article changes its form according to this categorization. In

2856-700: The Avon to the south and west, the Weaver to the north-west, the tributaries of the Yorkshire Ouse to the North and the basins of the Welland , Witham and Ancholme to the east. A distinctive feature of the catchment is the marked variation in the topography and character of the landscape, which varies from the upland moorland headwaters of the Dark Peak , where the highest point of

2958-684: The River Sow joins it from Stafford . The Trent now flows south-east past the town of Rugeley until it reaches Kings Bromley where it meets the Blithe. After the confluence with the Swarbourn, it passes Alrewas and reaches Wychnor, where it is crossed by the A38 road dual carriageway, which follows the route of the Roman Ryknild Street . The river turns north-east where it is joined by its largest tributary,

3060-561: The River Tame (which is at this point actually the larger, though its earlier length shorter) and immediately afterwards by the River Mease , creating a larger river that now flows through a broad floodplain. The river continues north-east, passing the village of Walton-on-Trent until it reaches the large town of Burton-upon-Trent . The river in Burton is crossed by a number of bridges including

3162-572: The Romano-British Trisantona , a Romano-British reflex of the combined elements * tri-sent(o)-on-ā- (through-path- augmentative - feminine -) ‘great thoroughfare’. A traditional but almost certainly wrong opinion is that of Izaak Walton, who states in The Compleat Angler (1653) that the Trent is "... so called from thirty kind of fishes that are found in it, or for that it receiveth thirty lesser rivers." The Trent rises within

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3264-624: The Staffordshire Moorlands district, near the village of Biddulph Moor , from a number of sources including the Trent Head Well. It is then joined by other small streams to form the Head of Trent, which flows south, to the only reservoir along its course at Knypersley Reservoir . Downstream of the reservoir it passes through Stoke-on-Trent and merges with the Lyme, Fowlea and other brooks that drain

3366-662: The White Peak in the Dove catchment, and the large woodland areas, including Sherwood Forest in the Dukeries area of the Idle catchment, the upland Charnwood Forest , and the National Forest in the Soar and Mease drainage basins respectively. Land use is predominantly rural, with some three-quarters of the Trent catchment given over to agriculture. This ranges from moorland grazing of sheep in

3468-455: The "triggers" of the process, because they have an inherent gender, whereas related words that change their form to match the gender of the noun can be considered the "target" of these changes. These related words can be, depending on the language: determiners , pronouns , numerals , quantifiers , possessives , adjectives , past and passive participles , verbs , adverbs , complementizers , and adpositions . Gender class may be marked on

3570-527: The 1950s, following the 1947 event, stopped any major urban flooding , but problems did occur in undefended areas such as Willington and Gunthorpe, and again at Girton where 19 houses were flooded. The flood defences in Nottingham that protect 16,000 homes and those in Burton where they prevent 7,000 properties from flooding were reassessed after this flood, and were subsequently improved between 2006 and 2012. Grammatical gender Whereas some authors use

3672-572: The Holocene period, which created lowland mires such as the Thorne and Hatfield Moors . The topography, geology and land use of the Trent catchment all have a direct influence on the hydrology of the river. The variation in these factors is also reflected in the contrasting runoff characteristics and subsequent inflows of the principal tributaries. The largest of these is the River Tame, which contributes nearly

3774-617: The Pleistocene epoch between 450,000 and 12,000 years BP. Contained within these terraces is evidence of the mega fauna that once lived along the river, the bones and teeth of animals such as the woolly mammoth, bison and wolves that existed during colder periods have all been identified. Another notable find in a related terrace system near Derby from a warmer interglacial period, was the Allenton hippopotamus . The lower sequences of these terraces have been widely quarried for sand and gravel, and

3876-585: The Toot and Trent Hills before reaching Hazelford Ferry , Fiskerton and Farndon . To the north of Farndon, beside the Staythorpe Power Station the river splits, with one arm passing Averham and Kelham , and the other arm, which is navigable, being joined by the Devon before passing through the market town of Newark-on-Trent and beneath the town's castle walls. The two arms recombine at Crankley Point beyond

3978-571: The Trent adopted its current course into the Humber. The Trent basin covers a large part of the Midlands, and includes the majority of the counties of Staffordshire , Derbyshire, Leicestershire , Nottinghamshire and the West Midlands ; but also includes parts of Lincolnshire , South Yorkshire, Warwickshire and Rutland . The catchment is located between the drainage basins of the Severn and its tributary

4080-686: The Trent between Scunthorpe and Alkborough are also made up of mudstones, but are of the younger Rhaetic Penarth Group . In the wider catchment the geology is more varied, ranging from the Precambrian rocks of the Charnwood Forest, through to the Jurassic limestone that forms the Lincolnshire Edge and the eastern watershed of the Trent. The most important in terms of the river are the extensive sandstone and limestone aquifers that underlie many of

4182-696: The Trent is joined by the Chesterfield Canal and the River Idle and soon after enters Lincolnshire fully, passing to the west of Scunthorpe . The last bridge over the river is at Keadby where it is joined by both the Stainforth and Keadby Canal and the River Torne . Downstream of Keadby the river progressively widens, passing Amcotts and Flixborough to reach Burton upon Stather and finally Trent Falls . At this point, between Alkborough and Faxfleet

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4284-483: The autumn being followed by further rainfall, producing flood conditions in November of that year. Another meteorological risk, although one that occurs less often, is that related to the rapid melting of snow lying in the catchment. This can be a result of a sudden rise in temperature after a prolonged cold period, or when combined with extensive rainfall. Many of the largest historical floods were caused by snowmelt, but

4386-598: The average flow rises to 83.8 m /s (2,960 cu ft/s), due to the combined inputs of the other major tributaries namely the Dove, Derwent and Soar. The last point of measurement is North Muskham here the average flow is 88.4 m /s (3,120 cu ft/s), a relatively small increase due to the input of the Devon, and other smaller Nottinghamshire tributaries. The Trent has marked variations in discharge, with long term average monthly flows at Colwick fluctuating from 45 m /s (1,600 cu ft/s) in July during

4488-613: The basin from the Atlantic, especially during the autumn and winter when evaporation is at its lowest. This combination can produce a water-logged catchment that can respond rapidly in terms of runoff, to any additional rainfall. Such conditions occurred in February 1977, with widespread flooding in the lower reaches of the Trent when heavy rain produced a peak flow of nearly 1,000 m /s (35,000 cu ft/s) at Nottingham. In 2000 similar conditions occurred again, with above average rainfall in

4590-462: The boundary between the Midlands and the north of England. The name "Trent" is possibly from a Romano-British word meaning "strongly flooding". More specifically, the name may be a contraction of two Romano-British words, tros ("over") and hynt ("way"). This may indeed indicate a river that is prone to flooding. However, a more likely explanation may be that it was considered to be a river that could be crossed principally by means of fords , i.e.

4692-456: The catchment is the Kinder Scout plateau at 634 metres (2,080 ft); through to the intensively farmed and drained flat fenland areas that exist alongside the lower tidal reaches, where ground levels can equal sea level. These lower reaches are protected from tidal flooding by a series of floodbanks and defences. Elsewhere there is a distinct contrast between the open limestone areas of

4794-400: The circumstances in which it occurs, and the way words are marked for gender vary between languages. Gender inflection may interact with other grammatical categories like number or case . In some languages the declension pattern followed by the noun itself will be different for different genders. The gender of a noun may affect the modifications that the noun itself undergoes, particularly

4896-486: The city and surrounding areas were flooded with 9,000 properties and nearly a hundred industrial premises affected some to first floor height. The suburbs of Long Eaton , West Bridgford and Beeston all suffered particularly badly. Two days later, in the lower tidal reaches of the river, the peak of the flood combined with a high spring tide to flood villages and 2,000 properties in Gainsborough. River levels dropped when

4998-547: The city, it passes the suburbs of Beeston , Clifton and Wilford ; where it is joined by the Leen. On reaching West Bridgford it flows beneath Trent Bridge near the cricket ground of the same name, and beside The City Ground , home of Nottingham Forest F.C. , until it reaches Holme Sluices . Downstream of Nottingham it passes Radcliffe-on-Trent , Stoke Bardolph and Burton Joyce before reaching Gunthorpe with its bridge, lock and weir. The river now flows north-east below

5100-782: The earliest family known to have split off from it, the extinct Anatolian languages (see below ). Modern examples include Algonquian languages such as Ojibwe . Here a masculine–feminine–neuter system previously existed, but the distinction between masculine and feminine genders has been lost in nouns (they have merged into what is called common gender ), though not in pronouns that can operate under natural gender. Thus nouns denoting people are usually of common gender, whereas other nouns may be of either gender. Examples include Danish and Swedish (see Gender in Danish and Swedish ), and to some extent Dutch (see Gender in Dutch grammar ). The dialect of

5202-444: The earliest floods can be assessed by using Spalford bank as a substitute measure for the size of a particular flood, as it has been estimated that the bank only failed when flows were greater than 1,000 m /s (35,000 cu ft/s), the bank was also breached in 1403 and 1795. Early bridges were vulnerable to floods, and in 1309 many bridges were washed away or damaged by severe winter floods, including Hethbeth Bridge. In 1683

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5304-481: The effect for German speakers has also led to a proposal that the effect is restricted to languages with a two-gender system, possibly because such languages are inclined towards a greater correspondence between grammatical and natural gender. Another kind of test asks people to describe a noun, and attempts to measure whether it takes on gender-specific connotations depending on the speaker's native language. For example, one study found that German speakers describing

5406-406: The end of August, and were given a drought return period of greater than one hundred years. The river's flow is measured at several points along its course, at a number of gauging stations . At Stoke-on-Trent in the upper reaches, the average flow is only 0.6 m /s (21 cu ft/s), which increases considerably to 4.4 m /s (160 cu ft/s), at Great Haywood , as it includes

5508-630: The end of the Wolstonian Stage (c. 130,000 years ago) a mass of stagnant ice left in the Vale of Belvoir caused the river to divert north along the old Lincoln river, through the Lincoln gap, along what is now the course of the Witham . During a following glaciation ( Devensian , 70,000 BC) the ice held back vast areas of water – called Glacial Lake Humber – in the current lower Trent basin. When this retreated,

5610-531: The end of the last Devensian glacial period the formation of Lake Humber in the lowest reaches of the river, meant that substantial lake bed clays and silts were laid down to create the flat landscape of the Humberhead Levels . These levels extend across the Trent valley, and include the lower reaches of the Eau, Torne and Idle. In some areas, successive layers of peat were built up above the lacustrine deposits during

5712-464: The entire length of the river, and are an important feature of the middle and lower reaches, with the alluvial river silt producing fertile soils that are used for intensive agriculture in the Trent valley. Beneath the alluvium are widespread deposits of sand and gravel, which also occur as gravel terraces considerably above the height of the current river level. There is thought to be a complex succession of at least six separate gravel terrace systems along

5814-532: The existence of words that denote male and female, such as the difference between "aunt" and "uncle" is not enough to constitute a gender system. In other languages, the division into genders usually correlates to some degree, at least for a certain set of nouns, such as those denoting humans, with some property or properties of the things that particular nouns denote. Such properties include animacy or inanimacy, " humanness " or non-humanness, and biological sex . However, in most languages, this semantic division

5916-483: The extraction of these minerals continues to be an important industry in the Trent Valley, with some three million tonnes of aggregates being produced each year. Once worked out, the remaining gravel pits which are usually flooded by the relatively high water table have been reused for a wide variety of purposes. These include recreational water activities, and once rehabilitated, as nature reserves and wetlands. During

6018-454: The fact that eighty loads of faggots and upwards of four hundred tons of earth were required to fill up the hole, an operation which took several weeks to complete. The flood bank was subsequently strengthened and repaired, following further floods during 1824 and 1852. The principal flood of the 19th century and the second largest recorded, was in October 1875. In Nottingham a cart overturned in

6120-419: The floodbank at Morton breached, resulting in the flooding of some 78 sq mi (200 km ; 50,000 acres) of farmland in the Trent valley. Flooding on the Trent can also be caused by the effects of storm surges independently of fluvial flows, a series of which occurred during October and November 1954, resulting in the worse tidal flooding experienced along the lower reaches. These floods revealed

6222-462: The floodwaters near the Wilford Road and six people drowned, dwellings nearby were flooded to a depth of 6 feet (1.8 m). Although not quite as large as 1795 this flood devastated many places along the river, at Burton upon Trent much of the town was inundated, with flooded streets and houses, and dead animals floating past in the flood. Food was scarce, "in one day 10,000 loaves had to be sent into

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6324-475: The flow of the upper tributaries draining the Potteries conurbation. At Yoxall , the flow increases to 12.8 m /s (450 cu ft/s) due to the input of larger tributaries including the Sow and Blithe. At Drakelow upstream of Burton the flow increases nearly three-fold to 36.1 m /s (1,270 cu ft/s), due to the additional inflow from the largest tributary the Tame. At Colwick near Nottingham,

6426-476: The grounds of Shugborough Hall to meet the Trent near Essex Bridge . Between 1816 and the 1920s, the section between Stafford and Baswich was navigable, and was known as the River Sow Navigation . There are plans to restore it, which are being spearheaded by a community interest company called Stafford Riverway Link. The river was tested in 2009 and had pH levels of 7.6. Oxygen saturation levels at

6528-471: The highest annual rainfall of 1,450 mm (57 in) and above occurring over the high moorland uplands of the Derwent headwaters to the north and west, with the lowest of 580 mm (23 in), in the lowland areas to the north and east. Rainfall totals in the Tame are not as high as would be expected from the moderate relief, due to the rain shadow effect of the Welsh mountains to the west, reducing amounts to an average of 691 mm (27.2 in) for

6630-439: The language and the word, this assignment might bear some relationship with the meaning of the noun (e.g. "woman" is usually feminine), or may be arbitrary. In a few languages, the assignment of any particular noun (i.e., nominal lexeme, that set of noun forms inflectable from a common lemma) to one grammatical gender is solely determined by that noun's meaning, or attributes, like biological sex, humanness, or animacy. However,

6732-473: The last such episode occurred when the bitter winter of 1946-7 was followed by a rapid thaw due to rain in March 1947 and caused severe flooding all along the Trent valley. At the other extreme, extended periods of low rainfall can also cause problems. The lowest flows for the river were recorded during the drought of 1976 , following the dry winter of 1975/6. Flows measured at Nottingham were exceptionally low by

6834-419: The major aquifers in the catchment. In the lower tidal reaches the Trent has a high sediment load, this fine silt which is also known as ‘warp', was used to improve the soil by a process known as warping , whereby river water was allowed to flood into adjacent fields through a series of warping drains, enabling the silt to settle out across the land. Up to 0.3 metres (1 ft) of deposition could occur in

6936-582: The majority of the 6 million people who live in the catchment. The majority of these urban areas are in the upper reaches of either the Trent itself, as is the case with Stoke, or its tributaries. For example, Birmingham lies at the upper end of the Tame, and Leicester is located towards the head of the Soar. Whilst this is not unique for an English river, it does mean that there is an ongoing legacy of issues relating to urban runoff , pollution incidents, and effluent dilution from sewage treatment , industry and coal mining. Historically, these issues resulted in

7038-423: The medieval Hethbeth bridge that pre-dated the existing 19th-century crossing. Historic flood levels have also been recorded at Girton and on the churchyard wall at Collingham . One of the earliest recorded floods along the Trent was in 1141, and like many other large historical events was caused by the melting of snow following heavy rainfall, it also caused a breach in the outer floodbank at Spalford . Some of

7140-747: The merger of masculine and feminine in these languages and dialects can be considered a reversal of the original split in Proto-Indo-European (see below ). Some gender contrasts are referred to as classes ; for some examples, see Noun class . In some of the Slavic languages , for example, within the masculine and sometimes feminine and neuter genders, there is a further division between animate and inanimate nouns—and in Polish , also sometimes between nouns denoting humans and non-humans. (For details, see below .) A human–non-human (or "rational–non-rational") distinction

7242-399: The need for a tidal protection scheme, which would cope with the flows experienced in 1947 and the tidal levels from 1954, and subsequently the floodbanks and defences along the lower river were improved to this standard with the works being completed in 1965. In December 2013, the largest storm surge since the 1950s occurred on the Trent, when a high spring tide combined with strong winds and

7344-438: The noun itself, but can also be marked on other constituents in a noun phrase or sentence. If the noun is explicitly marked, both trigger and target may feature similar alternations. As an example, we consider Spanish , a language with two gender categories: "natural" vs "grammatical". "Natural" gender can be masculine or feminine, while "grammatical" gender can be masculine, feminine, or neuter. This third, or "neuter" gender

7446-1022: The noun itself, but will also always be marked on other constituents in a noun phrase or sentence. If the noun is explicitly marked, both trigger and target may feature similar alternations. Three possible functions of grammatical gender include: Moreover, grammatical gender may serve to distinguish homophones. It is a quite common phenomenon in language development for two phonemes to merge, thereby making etymologically distinct words sound alike. In languages with gender distinction, however, these word pairs may still be distinguishable by their gender. For example, French pot ("pot") and peau ("skin") are homophones /po/ , but disagree in gender: le pot vs. la peau . Common systems of gender contrast include: Nouns that denote specifically male persons (or animals) are normally of masculine gender; those that denote specifically female persons (or animals) are normally of feminine gender; and nouns that denote something that does not have any sex, or do not specify

7548-455: The noun, and sometimes a noun can be modified to produce (for example) masculine and feminine words of similar meaning. See § Form-based morphological criteria , below. Agreement , or concord, is a grammatical process in which certain words change their form so that values of certain grammatical categories match those of related words. Gender is one of the categories which frequently require agreement. In this case, nouns may be considered

7650-654: The noun. They are not regularly used in English or other European languages, although they parallel the use of words such as piece(s) and head in phrases like "three pieces of paper" or "thirty head of cattle". They are a prominent feature of East Asian languages , where it is common for all nouns to require a classifier when being quantified—for example, the equivalent of "three people" is often "three classifier people". A more general type of classifier ( classifier handshapes ) can be found in sign languages . Classifiers can be considered similar to genders or noun classes, in that

7752-551: The old Norwegian capital Bergen also uses common gender and neuter exclusively. The common gender in Bergen and in Danish is inflected with the same articles and suffixes as the masculine gender in Norwegian Bokmål . This makes some obviously feminine noun phrases like "a cute girl", "the well milking cow" or "the pregnant mares" sound strange to most Norwegian ears when spoken by Danes and people from Bergen since they are inflected in

7854-612: The only toll bridge along its course at Dunham on Trent . Downstream of Dunham the river passes Church Laneham and reaches Torksey , where it meets the Foss Dyke navigation which connects the Trent to Lincoln and the River Witham . Further north at Littleborough is the site of the Roman town of Segelocum, where a Roman road once crossed the river. It then reaches the town of Gainsborough with its own Trent Bridge . The river frontage in

7956-505: The ornate 19th-century Ferry Bridge that links Stapenhill to the town. To the north-east of Burton the river is joined by the River Dove at Newton Solney and enters Derbyshire , before passing between the villages of Willington and Repton where it turns directly east to reach Swarkestone Bridge . Shortly afterwards, the river becomes the Derbyshire - Leicestershire border, passing

8058-684: The past often caused the river to change course. The river passes through Stoke-on-Trent , Stone, Staffordshire , Rugeley , Burton-upon-Trent and Nottingham before joining the River Ouse, Yorkshire at Trent Falls to form the Humber Estuary, which empties into the North Sea between Kingston upon Hull in Yorkshire and Immingham in Lincolnshire. The wide Humber estuary has often been described as

8160-458: The possibility of subjects' "using grammatical gender as a strategy for performing the task", and the fact that even for inanimate objects the gender of nouns is not always random. For example, in Spanish, female gender is often attributed to objects that are "used by women, natural, round, or light" and male gender to objects "used by men, artificial, angular, or heavy." Apparent failures to reproduce

8262-589: The river flowed over major road routes. This may explain the presence of the Romano-British element rid (cf. Welsh rhyd , "ford") in various place names along the Trent, such as Hill Ridware , as well as the Old English‐derived ford . Another translation is given as "the trespasser", referring to the waters flooding over the land. According to Koch at the University of Wales , the name Trent derives from

8364-476: The river reaches the boundary with Yorkshire and joins the River Ouse to form the Humber which flows into the North Sea . Unusually for an English river, the channel altered significantly during historic times, and has been described as being similar to the Mississippi in this respect, especially in its middle reaches, where there are numerous old meanders and cut-off loops. An abandoned channel at Repton

8466-427: The river, deposited when a much larger Trent flowed through the existing valley, and along its ancestral routes through the water gaps at Lincoln and Ancaster. This ‘staircase’ of flat topped terraces was created as a result of successive periods of deposition and subsequent down cutting by the river, a product of the meltwater and glacially eroded material produced from ice sheets at the end of glacial periods through

8568-557: The same bridge was partially destroyed by a flood that also meant the loss of the bridge at Newark. Historical archives often record details of the bridge repairs that followed floods, as the cost of these repairs or pontage had to be raised by borrowing money and charging a local toll. The largest known flood was the Candlemas flood of February 1795, which followed an eight-week period of harsh winter weather, rivers froze which that meant mills were unable to grind corn, and then followed

8670-563: The sex of their referent, have come to belong to one or other of the genders, in a way that may appear arbitrary. Examples of languages with such a system include most of the modern Romance languages , the Baltic languages , the Celtic languages , some Indo-Aryan languages (e.g., Hindi ), and the Afroasiatic languages . This is similar to systems with a masculine–feminine contrast, except that there

8772-468: The six towns of the Staffordshire Potteries to become the River Trent. On the southern fringes of Stoke, it passes through the landscaped parkland of Trentham Gardens . The river then continues south through the market town of Stone, and after passing the village of Salt , it reaches Great Haywood , where it is spanned by the 16th-century Essex Bridge near Shugborough Hall . At this point

8874-431: The smug and silver Trent shall run In a new channel, fair and evenly; It shall not wind with such a deep indent, To rob me of so rich a bottom here. Henry Hotspur's speech complaining about the river has been linked to the meanders near West Burton , however, given the wider context of the scene, in which conspirators propose to divide England into three after a revolt, it is thought that Hotspur's intentions were of

8976-603: The source of the river are 68%. Fish species found in the river include Chub , Roach , Pike and Bream . River Trent The Trent is the third longest river in the United Kingdom. Its source is in Staffordshire , on the southern edge of Biddulph Moor . It flows through and drains the North Midlands into the Humber Estuary . The river is known for dramatic flooding after storms and spring snowmelt, which in

9078-498: The summer, and increasing to 151 m /s (5,300 cu ft/s) in January. During lower flows the Trent and its tributaries are heavily influenced by effluent returns from sewage works, especially the Tame where summer flows can be made up of 90% effluent. For the Trent this proportion is lower, but with nearly half of low flows being made up of these effluent inflows, it is still significant. There are also baseflow contributions from

9180-666: The term "grammatical gender" as a synonym of "noun class", others use different definitions for each. Many authors prefer "noun classes" when none of the inflections in a language relate to sex or gender . According to one estimate, gender is used in approximately half of the world's languages . According to one definition: "Genders are classes of nouns reflected in the behavior of associated words." Languages with grammatical gender usually have two to four different genders, but some are attested with up to 20. Common gender divisions include masculine and feminine; masculine, feminine, and neuter; or animate and inanimate. Depending on

9282-433: The town and distributed gratuitously to save people from famine". In Newark the water was deep enough to allow four grammar school boys to row across the countryside to Kelham. The flood marks at Girton show that this flood was only 4 inches (100 mm) lower than that of 1795, when the village was flooded to a depth of 3 feet (0.91 m). On 17–18 March 1947 the Trent overtopped its banks in Nottingham. Large parts of

9384-456: The town is lined with warehouses, that were once used when the town was an inland port, many of which have been renovated for modern use. Downstream of the town the villages are often named in pairs, representing the fact that they were once linked by a river ferry between the two settlements. These villages include West Stockwith and East Stockwith , Owston Ferry and East Ferry , and West Butterwick and East Butterwick . At West Stockwith

9486-466: The town, where the river turns due north to pass North Muskham and Holme to reach Cromwell Weir , below which the Trent becomes tidal. The now tidal river meanders across a wide floodplain, at the edge of which are located riverside villages such as Carlton and Sutton on Trent , Besthorpe and Girton . After passing the site of High Marnham power station , it becomes the approximate boundary between Nottinghamshire and Lincolnshire and reaches

9588-681: The traditional crossing point of King's Mill , Castle Donington, Weston-on-Trent and Aston-on-Trent . At Shardlow , where the Trent and Mersey Canal begins, the river also meets the Derwent at Derwent Mouth. After this confluence, the river turns north-east and is joined by the River Soar before reaching the outskirts of Nottingham , where it is joined by the River Erewash near the Attenborough nature reserve and enters Nottinghamshire . As it enters

9690-418: The tributary basin. The average for the whole Trent catchment is 720 mm (28 in) which is significantly lower than the average for United Kingdom at 1,101 mm (43.3 in) and lower than that for England at 828 mm (32.6 in). Like other large lowland British rivers, the Trent is vulnerable to long periods of rainfall caused by sluggish low pressure weather systems repeatedly crossing

9792-591: The tributary catchments. These include the Sherwood sandstones that occur beneath much of eastern Nottinghamshire, the Permian Lower Magnesian limestone and the carboniferous limestone in Derbyshire. Not only do these provide baseflows to the major tributaries, the groundwater is an important source for public water supply. Sand, gravels and alluvium deposits that overlie the mudstone bedrock occur almost along

9894-568: The upland areas, through to improved pasture and mixed farms in the middle reaches, where dairy farming is important. Intensive arable farming of cereals and root vegetables, chiefly potatoes and sugar beet occurs in the lowland areas, such as the Vale of Belvoir and the lower reaches of the Trent, Torne and Idle. Water level management is important in these lowland areas, and the local watercourses are usually maintained by internal drainage boards and their successors, with improved drainage being assisted by

9996-524: The use of pumping stations to lift water into embanked carrier rivers , which subsequently discharge into the Trent. The less populous rural areas are offset by a number of large urbanised areas including the conurbations of Stoke-on-Trent , Birmingham and the surrounding Black Country in the West Midlands; and in the East Midlands the major university cities and historical county seats of Leicester , Derby and Nottingham . Together these contain

10098-456: The way in which the noun inflects for number and case . For example, a language like Latin , German or Russian has a number of different declension patterns, and which pattern a particular noun follows may be highly correlated with its gender. For some instances of this, see Latin declension . A concrete example is provided by the German word See , which has two possible genders: when it

10200-423: The way to the Humber. The mudstones are not exposed by the bed of the river, as there is a layer of gravels and then alluvium above the bedrock. In places, however the mudstones do form river cliffs, most notably at Gunthorpe and Stoke Lock near Radcliffe on Trent, the village being named after the distinctive red coloured strata. The low range of hills, which have been formed into a steep set of cliffs overlooking

10302-490: Was breached again, floodwaters spreading out across the low-lying land, even reaching the River Witham and flooding Lincoln. Some 20,000 acres (81 km ; 31 sq mi) were flooded for a period of over three weeks. A description of the breach was given as follows: The bank is formed upon a plain of sandy nature, and when it was broken in 1795, the water forced an immense breach, the size of which may be judged from

10404-439: Was dried out and refined to be eventually sold as a silver polish for cutlery manufacturers. The Trent is widely known for its tendency to cause significant flooding along its course, and there is a well documented flood history extending back for some 900 years. In Nottingham the heights of significant historic floods from 1852 have been carved into a bridge abutment next to Trent Bridge, with flood marks being transferred from

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