Site visits | 98 |
Sites | 0 |
Records | 0 |
Site code | Site description | Sampling date | Owner | Total occurrences | Actions |
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G2JONK-00058 Validated |
Falls within primary catchment g on the eerste river flowing through stellenbosch town river make up majorly pools then runs and riffleswater murky and stagnant in some areasdebri present, water slightly murky , replicates teeming with hirudinea and oligochaetes tall trees on either side of river promote shading of certain areas at certain times of the day
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2015-10-23 | Cole Grainger | 1 | |
H2HEXR-00035 Validated |
Falls within primary catchment h on the hex river and is situated alongside the n1 between worcester and de doorns channel bank sandy and unstable flows unaltered but nutrient enrichment severe
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2015-10-22 | Cole Grainger | 1 | |
H1BREE-00057 Validated |
Falls within primary catchment on the Breede River between Wolseley and Ceres
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2015-10-22 | Cole Grainger | 1 | |
G4PALM-00116 Validated |
Falls withing primary catchment g on palmiet river just right of the n2 after sir lowry's pass situated downstream of kogelberg dam, this site is considered impacted with flow alterations and enrichment occuring river make up consisting of riffles and runssubstrate different to other sites with abundance of bedrock
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2015-10-17 | Cole Grainger | 1 | |
H8DUIW-00039 Validated |
Falls within primary catchment h on the duiwenhoks river on route to vermaklikheid opposite heidelberg river make up consists of riffles, runs and pools with the water being a "dark tea" colour
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2015-10-17 | Cole Grainger | 1 | |
E1JAND-00004 Validated |
This site was situated on the Jan Dissels River some 6 kilometers upstream the Town of Clan William Some moderate shading was unavoidable here but this site was selected to add to the list of pristine sites in the Western Cape
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2015-10-16 | Cole Grainger | 1 | |
G2JONK-00059 Validated |
Situated on the Jonkershoek River in the Jonkershoek Nature Reserve just outside the town of Stellenbosch This is considered a pristine site with no flow alteration or enrichment The channel floor was a mixture of small cobbles, large cobbles and boulders with odd occasion of gravel
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2015-10-15 | Cole Grainger | 1 | |
U2MSUN-00041 Validated |
Downstream of Pietermaritzburg and the Darvil WWTW, in the vicinity of the gauging weir at the motocross track Open canopy with a steep bank in some areas, upstream receives sewage and industrial waste from several minor tributaries River is a
mix of pools, runs and riffles with a mixture of boulders, cobbles, gravel and mud Site is very nutrient enriched from treated effluent discharge atWWTW
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2015-10-14 | Cole Grainger | 1 | |
T5MZIM-00077 Validated |
Site is directly upstream of a shallow gravel bed section used for washing vehicles, tents and related function hire equipment Cobble and boulder dominated runs or rapids with gravel dominated pools representing this river reach
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2015-10-13 | Cole Grainger | 1 | |
T5MZIM-00078 Validated |
At the bridge crossing at Calloway Farm River is mostly bedrock and boulder dominated with cobbles, gravel and some sand It is moderate to fast flowing with runs, riffles and occasional rapids
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2015-10-13 | Cole Grainger | 1 | |
U6MLAZ-00059 Validated |
Located below the district road and Baynesfield Dam, and upstream of Baynesfield School
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2015-10-13 | Cole Grainger | 1 | |
U2KARK-00080 Validated |
The sample site at Morton's Drift was dominated by a run over large cobbles and boulders in water less than 40cm deep
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2015-10-08 | Cole Grainger | 1 | |
U4MVOT-00035 Validated |
Site downstream of the Umvoti River rail sliding and local district road at the Umgeni Water gauging weir The sample site below the weir was scoured and predominantly bedrock with a few large boulders and cobbles
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2015-10-08 | Cole Grainger | 1 | |
U2ALBE-00012 Validated |
Downstream of Albert Falls Dam at the falls The river bed is mostly armoured with boulders and large cobbles dominating the sample site
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2015-10-07 | Cole Grainger | 1 | |
U2MGEN-00132 Validated |
The site was directly below the Umgeni Water gauging weir in a braided section of river containing bedrock, boulders and a variety of medium to large cobbles which flows into the Nagel Dam
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2015-10-07 | Cole Grainger | 1 | |
G4KLEI-00051 Validated |
Situated some 14 kilometers NE of the town Stanford on the Klein River, a second order stream formed through the joining of the Hartbees and Steenbok rivers that drains out at Hermanus This river is said not to flow in summer due to the large amount of water abstraction taking place for dairy farming
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2015-10-01 | Cole Grainger | 1 | |
J1BOKR-00002 Validated |
Falls within primary catchment on the bok river situated in the bok river nature reserve left off n1 before entering touws river considered a pristine site as sampling was done close to sourcewith no anthropogenic influence channel very shallow (mostly ≤ 10 cm) and narrow with an abundance of small cobblessampled a foothill section downstream of weir where canopy opened up
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2015-10-01 | Cole Grainger | 1 | |
U2MSUN-00039 Validated |
Cobble bed river with an open canopy upstream of Henley Dam in the peri-urban surrounds north of Pietermaritzburg CBD
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2015-06-01 | Cole Grainger | 11 | |
U2MSUN-00040 Validated |
Cobble bed river with a riparian fringe invaded with aliens, although the canopy remains largely open Downstream of the Henley Dam
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2015-06-01 | Cole Grainger | 13 | |
U2MGEN-00130 Validated |
Located outside the town of Howick, immediately upstream of the Midmar dam (above the Petrus Stroom Road bridge crossing the Umgeni River) This site has a natural flow regime, albeit somewhat enriched by surrounding agricultural activities
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2015-06-01 | Cole Grainger | 15 |