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Habitat types key navigation

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  • Help information
You can use the 'key navigation' function to identify a specific habitat by answering a set of questions. Starting from first question to next questions you select one of the possible answers. Here are samples of possible answers:
  • No ( 002 ) - Leading to question named '002'
  • Yes [ G ] - Leading to another questions subset of level G
  • No Factsheet icon[ E6 ] - Links directly to factsheet for E6
Additionally the diagram may be used for reference.


Category : (C2 )Surface running waters
Diagram : Diagram icon


Question c05 :   Temporary?
   Seasonal and otherwise temporary running surface waters (path = <strong>Yes</strong>) are separated from surface running waters of more permanent character.
Answers:
Yes Factsheet icon [ C2.5 ] No (Question c06 )


Question c06 :   Up-welling?
   Springs and geysers where the flow is caused by up-welling from the substrate and the stream immediately below, where the temperature regime is similar to the source water and significantly different from the surroundings, are distinguished (path = <strong>Yes</strong>).
Answers:
Yes Factsheet icon [ C2.1 ] No (Question c07 )


Question c07 :   Water in thin sheets over rock?
   Habitats characterised by thin layers of moving water over rock surfaces adjacent to open water are distinguished (path = <strong>Yes</strong>) from the main open waterbody with which they are associated.
Answers:
Yes Factsheet icon [ C2.6 ] No (Question c08 )


Question c08 :   Tidal water?
   Tidal rivers and streams (which may or may not be brackish) upstream of the estuary are distinguished (path = <strong>Yes</strong>) from running water not affected by tides. Note that estuarine waters, with variable salinity usually greater than 0.5 ppt, are categorised under A and estuaries as complex X01.
Answers:
Yes Factsheet icon [ C2.4 ] No (Question c09 )


Question c09 :   Flow
   Watercourses where the flow-rate is <strong>fast and turbulent</strong> are distinguished from rivers where flow is <strong>slower and tending towards becoming laminar</strong>. Note that where flow is fast and turbulent, the oxygen concentration is high, and the bed usually composed of rocks, stones or gravel with only occasional sandy and silty patches; where flow is slower, oxygen concentration deficits may occur at times, and normally the substrate is mainly sand and mud. Rivers that are fast but with laminar flow follow path = <strong>slower and tending towards becoming laminar</strong>. Note that where there is no perceptible flow, habitats are classified under C1.
Answers:
fast and turbulent Factsheet icon [ C2.2 ] slower and tending towards laminar Factsheet icon [ C2.3 ]

EUNIS

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