Seathwaite Tarn (original) (raw)
Der Seathwaite Tarn ist ein Stausee im Lake District, Cumbria, England. Der Seathwaite Tarn ist ein natürlicher See, der zwischen 1904 und 1907 durch den Bau eines Damms aufgestaut wurde, um Trinkwasser für Barrow-in-Furness bereitzustellen. Der See liegt südlich des und nördlich der Seathwaite Fells am Rande des Duddon Valley und nördlich des Ortes Seathwaite. Durch die 366 m lange Staumauer erreicht der See eine Tiefe von 28 m. Der Tarn Beck, der in den River Duddon mündet, bildet seinen Abfluss.
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| dbo:abstract | Der Seathwaite Tarn ist ein Stausee im Lake District, Cumbria, England. Der Seathwaite Tarn ist ein natürlicher See, der zwischen 1904 und 1907 durch den Bau eines Damms aufgestaut wurde, um Trinkwasser für Barrow-in-Furness bereitzustellen. Der See liegt südlich des und nördlich der Seathwaite Fells am Rande des Duddon Valley und nördlich des Ortes Seathwaite. Durch die 366 m lange Staumauer erreicht der See eine Tiefe von 28 m. Der Tarn Beck, der in den River Duddon mündet, bildet seinen Abfluss. (de) Seathwaite Tarn is a reservoir in the Furness Fells within the English Lake District. It is located to the south of Grey Friar and to the west of Brim Fell (on the ridge between The Old Man of Coniston and Swirl How) and north east of the village of Seathwaite on the east of the Duddon Valley. In order to create a source of drinking water the existing tarn was considerably enlarged with a dam in 1904. During the dam construction some of the navvies rioted damaging buildings in the village, several rioters were shot, one dying the next day. The dam is almost 400 yards (366 m) long and is concrete cored with slate buttresses, the resulting depth of the tarn being around 80 feet (24 m). Water is not abstracted directly from the tarn, but flows some distance downriver to an off-take weir. On the slopes of Brim Fell, above the head of the reservoir, are the remains of Seathwaite Tarn Mine. This was worked for copper in the mid 19th century, and also appears as a location in the novel The Plague Dogs by Richard Adams. Rocks in the area were the first confirmed occurrence of in the British Isles. Bronze Age ring cairns were found close to Seathwaite Tarn in 2003, these were excavated in 2003 and 2007. Seathwaite Tarn has suffered from acidification. An experiment in 1992–1993 to reduce the acidification by using a phosphorus-based fertiliser increased the pH from 5.1 to 5.6 and changed the levels of the different species of the rotifer assemblage significantly. (en) |
| dbo:areaTotal | 267092.523878 (xsd:double) |
| dbo:country | dbr:United_Kingdom |
| dbo:elevation | 365.760000 (xsd:double) |
| dbo:location | dbr:Lake_District |
| dbo:maximumDepth | 24.384000 (xsd:double) |
| dbo:thumbnail | wiki-commons:Special:FilePath/Seathwaite-Tarn-by-Paul-Lockett.jpg?width=300 |
| dbo:type | dbr:Reservoir_(water) |
| dbo:volume | 2945000.000000 (xsd:double) |
| dbo:wikiPageID | 23851937 (xsd:integer) |
| dbo:wikiPageLength | 7352 (xsd:nonNegativeInteger) |
| dbo:wikiPageRevisionID | 1083677192 (xsd:integer) |
| dbo:wikiPageWikiLink | dbr:Rotifer dbr:Reservoir_(water) dbr:Richard_Adams dbr:United_Kingdom dbr:United_Utilities dbr:Erosion dbr:Geomembrane dbr:Concrete dbr:Copper dbr:Dam dbr:The_Plague_Dogs dbr:MWH_Global dbr:Furness_Fells dbr:Tarn_(lake) dbr:Brim_Fell dbr:British_Isles dbr:Bronze_Age dbr:Duddon_Valley dbr:Siloxane dbr:Head_of_the_reservoir dbr:Fertiliser dbr:PVC dbr:Geosynthetic dbr:Reservoir dbr:Grey_Friar dbr:Acrylic_resin dbc:South_Lakeland_District dbr:Lake_District dbr:Swirl_How dbr:Efflorescence dbr:Weir dbr:Buttress dbr:Phosphorus dbc:Reservoirs_in_Cumbria dbr:Seathwaite,_South_Lakeland dbr:Slate dbr:Navvies dbr:Parapet dbr:Ring_cairn dbr:Riprap dbr:The_Old_Man_of_Coniston dbr:Abstracted dbr:File:Seathwaite_Reservoir.png dbr:Wittichenite |
| dbp:basinCountries | dbr:United_Kingdom |
| dbp:inflow | Tarn Head Beck, Near Gill, Far Gill, Bleaberry Gill (en) |
| dbp:location | dbr:Lake_District |
| dbp:name | Seathwaite Tarn (en) Seathwaite Tarn dam (en) |
| dbp:outflow | Tarn Beck (en) |
| dbp:pushpinMap | Cumbria (en) |
| dbp:type | dbr:Reservoir_(water) |
| dbp:wikiPageUsesTemplate | dbt:Other_places dbt:! dbt:Authority_control dbt:Convert dbt:Coord dbt:Infobox_body_of_water dbt:Reflist dbt:Short_description dbt:Use_dmy_dates dbt:Infobox_dam |
| dcterms:subject | dbc:South_Lakeland_District dbc:Reservoirs_in_Cumbria |
| gold:hypernym | dbr:Reservoir |
| georss:point | 54.37907222222222 -3.154952777777778 |
| rdf:type | owl:Thing dbo:Infrastructure wikidata:Q12323 dbo:Dam yago:WikicatLakesOfCumbria yago:WikicatLakesOfEngland geo:SpatialThing dbo:ArchitecturalStructure yago:BodyOfWater109225146 yago:Lake109328904 yago:PhysicalEntity100001930 yago:YagoGeoEntity yago:YagoPermanentlyLocatedEntity dbo:Lake yago:Thing100002452 |
| rdfs:comment | Der Seathwaite Tarn ist ein Stausee im Lake District, Cumbria, England. Der Seathwaite Tarn ist ein natürlicher See, der zwischen 1904 und 1907 durch den Bau eines Damms aufgestaut wurde, um Trinkwasser für Barrow-in-Furness bereitzustellen. Der See liegt südlich des und nördlich der Seathwaite Fells am Rande des Duddon Valley und nördlich des Ortes Seathwaite. Durch die 366 m lange Staumauer erreicht der See eine Tiefe von 28 m. Der Tarn Beck, der in den River Duddon mündet, bildet seinen Abfluss. (de) Seathwaite Tarn is a reservoir in the Furness Fells within the English Lake District. It is located to the south of Grey Friar and to the west of Brim Fell (on the ridge between The Old Man of Coniston and Swirl How) and north east of the village of Seathwaite on the east of the Duddon Valley. In order to create a source of drinking water the existing tarn was considerably enlarged with a dam in 1904. During the dam construction some of the navvies rioted damaging buildings in the village, several rioters were shot, one dying the next day. (en) |
| rdfs:label | Seathwaite Tarn (de) Seathwaite Tarn (en) |
| owl:sameAs | freebase:Seathwaite Tarn wikidata:Seathwaite Tarn dbpedia-de:Seathwaite Tarn dbpedia-nn:Seathwaite Tarn https://global.dbpedia.org/id/7ZfV |
| geo:geometry | POINT(-3.1549527645111 54.37907409668) |
| geo:lat | 54.379074 (xsd:float) |
| geo:long | -3.154953 (xsd:float) |
| prov:wasDerivedFrom | wikipedia-en:Seathwaite_Tarn?oldid=1083677192&ns=0 |
| foaf:depiction | wiki-commons:Special:FilePath/Seathwaite-Tarn-by-Paul-Lockett.jpg wiki-commons:Special:FilePath/Seathwaite_Reservoir.png |
| foaf:isPrimaryTopicOf | wikipedia-en:Seathwaite_Tarn |
| foaf:name | Seathwaite Tarn (en) |
| is dbo:wikiPageDisambiguates of | dbr:Seathwaite |
| is dbo:wikiPageWikiLink of | dbr:List_of_lakes_of_the_Lake_District dbr:River_Duddon dbr:Furness_Fells dbr:Brim_Fell dbr:Cumbria dbr:Dow_Crag dbr:Grey_Friar dbr:Swirl_How dbr:Seathwaite,_South_Lakeland dbr:Seathwaite |
| is foaf:primaryTopic of | wikipedia-en:Seathwaite_Tarn |
