- IJssel
Geobox River
name = IJssel
native_name =
other_name = Gelderse IJssel
other_name1 =
image_size = 220
image_caption = Sunset on the IJssel at Deventer
country = The Netherlands
country1 =
state =Gelderland
state1 =Overijssel
region =Liemers
region1 =Veluwe
region2 =Achterhoek
region3 =Salland
district =
district1 =
city =Arnhem (suburb s)
city1 =Doesburg
city2 =Zutphen
city3 =Deventer
city4 =Zwolle (suburbs)
city5 = Kampen
state_type = Province
length = 125
watershed =
discharge_location =
discharge_average =
discharge_max =
discharge_min =
discharge1_location =
discharge1_average =
source_name =Nederrijn
source_location =Westervoort
source_district =
source_region =
source_state = Gelderland
source_country =The Netherlands
source_lat_d =
source_lat_m =
source_lat_s =
source_lat_NS =
source_long_d =
source_long_m =
source_long_s =
source_long_EW =
source_elevation =
source_length =
mouth_name = Ketelmeer (inlet of lakeIJsselmeer )
mouth_location = Kampen
mouth_district =
mouth_region =Salland
mouth_state = Overijssel
mouth_country = The Netherlands
mouth_lat_d =
mouth_lat_m =
mouth_lat_s =
mouth_lat_NS =
mouth_long_d =
mouth_long_m =
mouth_long_s =
mouth_long_EW =
mouth_elevation =
tributary_left =
tributary_left1 =
tributary_right =Oude IJssel
tributary_right1 =Berkel
tributary_right2 =Schipbeek
free_name =
free_value =
map_size = 220
map_caption = Location of river IJssel in dark blue.River IJssel (IPA2|ˈɛi̯səl), sometimes called Gelderse IJssel ("Gelderland IJssel") to avoid confusion with itsHollandse IJssel namesake in the west of the Netherlands, is a branch of theRhine in the Dutchprovinces of Gelderland andOverijssel . River IJssel flows fromWestervoort , east of thecity ofArnhem , until it discharges into theIJsselmeer ("Lake IJssel", until the1932 completion of theAfsluitdijk known as theZuiderzee , aNorth Sea inlet). River IJssel is one of the three majordistributary branches into which theRhine divides itself shortly after crossing the German-Dutch border, the other two being the riversNederrijn andWaal .History
The name "IJssel" is thought to derive from the Germanic "i sala", meaning "dark water". A branch near its mouth (between Zwolle and Kampen) is today called "Zwarte Water", Dutch for "black water". In medieval times, the
Zuiderzee had not yet formed from the complex of lakes known as Flevo; the IJssel flowed through these lakes with the last, tidal stretch being calledVlie . Now cut off from the IJssel by means of theAfsluitdijk , Vlie remains as thestrait separating theisland s ofVlieland (itself named after the Vlie strait) andTerschelling . It is hypothesised that the now-polder ed tidal inlets ofMedem (nearMedemblik ) and IJ (nearAmsterdam ) once were branches of river IJssel.The IJssel as the lower part of the Oude IJssel
The IJssel was the lower part of the small river
Oude IJssel (lit. "Old IJssel", German "Issel"), that rises in Germany and is now a 70 km long tributary of the IJssel. The connection between Rhine and IJssel was probably artificial, allegedly dug by men under the Romangeneral Nero Claudius Drusus as a defence againstGermanic tribes and to let Roman ships carry troops along it [cite book |last=ter Laan |first=K. et al. ed.|title=Van Goor's aardrijkskundig woordenboek van Nederland |year=1942 |publisher=Van Goor Zonen |location=Den Haag |language=Dutch ] . The current Oude IJssel is the second-largest contributor to the flow of the river until today, after river Rhine.The source of the Oude IJssel is near Borken in
North Rhine-Westphalia , Germany. First it flows south-west until it nearly reaches the Rhine nearWesel ; then it turns north-west. After passing throughIsselburg it crosses the border with the Netherlands. The river, called Oude IJssel from here, then flows throughDoetinchem and joins the IJssel at Doesburg.Characteristics
The average discharge of the IJssel can change significantly. The average discharge has been stated as 300 cubic meters per second. This can be as low as 140 and as high as 1800, depending on the Nederrijn locks west of Arnhem, which regulate the amount of water taken in by the Nederrijn and IJssel branches.
As a lowlands river, the IJssel has a lot of bends and naturally occurring dead branches (locally called "hank"); some bends have been cut off by man (most notably near
Rheden andDoesburg ), reducing the river's length from 146 km [cite book |last=Augé |first=Claude ed.|title=Larousse universel en deux volumes |year=1922 |publisher=Larousse |location=Paris |language=French ] to 125 km, but not nearly as radically as with river Meuse. The naturally occurring phenomenon of sedimental island-forming in the outside of bends has been regulated to the point of non-occurrence since the latenineteenth century .The IJssel as a Rhine distributary
From the moment the connection between the Rhine and IJssel was dug, the Rhine became the largest contributor to the flow of the IJssel, although only a relatively small amount of the total Rhine flow makes its way into the IJssel system. Various tributaries can sometimes add a considerable volume of water to the total flow of the IJssel, such as the
Berkel andSchipbeek streams. The IJssel river is the only branch of the Rhine delta that takes up tributary rivers rather than giving rise to distributaries.s, pushing back the saline Zuiderzee water into the IJssel delta and preventing the water flowing from the mouths of the IJssel branches from discharging into the Zuiderzee.
The modern-day names of the delta branches are, west to east, Keteldiep, Kattendiep, Noorddiep, Ganzendiep and Goot. Of these, the Keteldiep and Kattendiep channels are the main navigational arteries; the Noorddiep has been closed off at both sides. Another branch, De Garste, had already completely silted up by the middle of the nineteenth centurycite book |last=Grote |others= |title=Grote historische atlas van Nederland (3) : Oost-Nederland 1830-1855 |year=1990 |publisher=Wolters-Noordhoff Atlasprodukties |location=Groningen |language=Dutch |isbn=90-01-96232-7 ] . Until the beginning of the
twentieth century , the Ganzendiep branch up to the Goot fork was known as IJssel proper due to it being the historical main channel, with the present-day main channel being called Regtediep or Rechterdiep until well into the twentieth century [cite book |last=Kwast |first=B. ed.|title=Schoolatlas der geheele aarde |year=1932 |publisher=Wolters |location=Groningen|language=Dutch ] .The IJssel, although now technically "merely" a Rhine branch, has retained most of the character of a distinct river in its own right, in no small part due to the fact that it has its own tributaries and, in river Oude IJssel, even a former
headstream .Tributaries and connecting canals
The following
canal s andtributary streams connect to the IJssel, in downstream order:
*Apeldoorns Kanaal (west) near thetown ofDieren
* riverOude IJssel (east) at thecity ofDoesburg
* theBerkel stream (east) at the city ofZutphen
* theTwentekanaal (east) between Zutphen and the village ofEefde (municipality ofGorssel )
* theSchipbeek stream (east) near the city ofDeventer
* theGrift stream (west) at the town ofHattem ; its lower reaches have been channelised to form the mouth of theGriftkanaal
* theWillemsvaart canal (east) at the city ofZwolle
* theZwolle-IJsselkanaal (east) near ZwolleRiver crossings
Road bridges
Road bridges across river IJssel (with nearest places on the left and right bank):
* Arnhem - Westervoort
* Arnhem - Duiven (A12motorway )
* Ellecom - Doesburg (N317)
* Brummen - Zutphen (N314)
* Zutphen - Zutphen
* Wilp - Deventer (A1 motorway)
* Deventer - Deventer (N344)
* Hattem - Zwolle
* Hattemerbroek - Zwolle (A28 motorway)
* Kampen - Kampen (N764)
* Kampen - Kampen
* Kampen - Noordoostpolder (N50)Ralroad bridges
Railroad bridges (with nearest train station on the left and right bank):
*Arnhem Velperpoort –Duiven
*Brummen /Klarenbeek –Zutphen
*Twello –Deventer
* Wezep –Zwolle Cable ferries
Only those ferries capable of carrying motorised vehicles are included.
* Dieren – Olburgen
* Brummen – Bronkhorst
* Welsum – Olst
* Vorchten – WijheReferences
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