Nissum Fjord
Encyclopedia
Nissum Fjord is a inlet
Inlet
An inlet is a narrow body of water between islands or leading inland from a larger body of water, often leading to an enclosed body of water, such as a sound, bay, lagoon or marsh. In sea coasts an inlet usually refers to the actual connection between a bay and the ocean and is often called an...

 located in West Jutland, west of Vemb
Vemb
Vemb is a little town in west Jutland, Denmark with a population of 1,337 . The town is close to Nissum Fjord and Storå. Vemb also has a station on the railway line between Ringkøbing and Holstebro. Two kilometers south of the town is Nørre Vosborg, a manor house surrounded by ramparts. It is one...

 and is demarcated from the North Sea
North Sea
In the southwest, beyond the Straits of Dover, the North Sea becomes the English Channel connecting to the Atlantic Ocean. In the east, it connects to the Baltic Sea via the Skagerrak and Kattegat, narrow straits that separate Denmark from Norway and Sweden respectively...

 by a 13 km wide isthmus, Bøvling Klit, and passes through a lock
Lock (water transport)
A lock is a device for raising and lowering boats between stretches of water of different levels on river and canal waterways. The distinguishing feature of a lock is a fixed chamber in which the water level can be varied; whereas in a caisson lock, a boat lift, or on a canal inclined plane, it is...

 in Thorsminde. The inlet has a water area of 70 km² or 7.000 ha. but the average water depth is only about 1 meter, and the deepest areas in Felsted Kog and the center of the inlet are between 2 to 3 meters. The northern part of the inlet, called Bøvling Fjord, is so shallow that it is sometimes completely drained by strong winds. Nissum Fjord has several creeks which empty into it, such as Ramme Creek, Flynder Creek, Damhus Creek and the largest creek, Storåen
Storå, Denmark
Storå or Storåen is Denmark's second longest creek, spanning 104 km., and only surpassed by Gudenå. Storå originates southeast of Ikast, winding its way between Herning, Sunds, and Ørre. Then it winds through Nybro, Hodsager and Holstebro before ending up in Nissum Fjord.Storå is one of Denmark's...

, which has its mouth at the eastern corner of Felsted Kog in the southeastern end of the inlet. Since the 1870s, Thorsminde has regulated the inlet's water level and salinity content at the lock, which facilitates water exchange in the inlet. The whole inlet as well as some surrounding land is designated as a wildlife sanctuary and Ramsar wetland, and the inlet and its surrounding reeds and meadows have a rich variety of bird
Bird
Birds are feathered, winged, bipedal, endothermic , egg-laying, vertebrate animals. Around 10,000 living species and 188 families makes them the most speciose class of tetrapod vertebrates. They inhabit ecosystems across the globe, from the Arctic to the Antarctic. Extant birds range in size from...

 life.

Fjandø

In the southwest part of Nissum Fjord, off of the peninsula
Peninsula
A peninsula is a piece of land that is bordered by water on three sides but connected to mainland. In many Germanic and Celtic languages and also in Baltic, Slavic and Hungarian, peninsulas are called "half-islands"....

 Nørre Fjand, lies a small uninhabited island of 40 hectares called Fjandø. The island's heath
Heath (habitat)
A heath or heathland is a dwarf-shrub habitat found on mainly low quality acidic soils, characterised by open, low growing woody vegetation, often dominated by plants of the Ericaceae. There are some clear differences between heath and moorland...

 vegetation is kept in check by a flock of sheep during the summer, giving good conditions for bird life. From 1 April to 31 August there is a total traffic ban on the island and in a 100 meter zone around the island.

Felsted Kog

Felsted Kog is the result of a drainage project in the latter half of the 1800s. The "Kog" got its name during the time people attempted to drain the entire inlet; "kog" means "acquired land." The project succeeded only at Felsted where a 13 km long dike was constructed and approximately 1400 ha. were drained. But it was soon found that the soil was not suitable for agricultural usage, and the dike often breached under heavy storms; thus the project was abandoned in 1885.

External sources/references

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