Watercourse

VN Tríbeč – Sekanina

fishing district
1
fishing district length
0.4km
region
Nitra Region
Aerial image of watercourse VN Tríbeč - Sekanina with the line highlighted
Blue line: course of the watercourse (approximate). Orthophoto mosaic of Slovakia © GKÚ Bratislava, CC BY 4.0Google Maps

By the water now

Today on the VN Tríbeč – Sekanina watercourse

Fishing conditions score, the best window of the day and fishing districts from the best conditions

Average of the watercourse's fishing districts

Low activity · average of one fishing district

The number in the header is an estimate for the middle of the watercourse based on weather and measurements. The average of the fishing districts also counts satellite data, shading and geology of each district.

Best window today

15:00–17:00

VN Tríbeč – Sekanina, window score 34.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 17:04.

Map and fishing districts of the watercourse

The course of the watercourse and its fishing districts. You can switch the line color to today's conditions, quality or any other parameter.

Detailed filtersregion, district, riverbed, depth, shading, satellites, water chemistry and pollution, fish, geology

1445fishing districts
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    Elevation profile: reservoir

    Terrain height along the fishing district and the approximate water level.

    Reservoir This is a reservoir, so the watercourse is not assessed here: the water has no current, fall or gradient. The chart shows the terrain height along the fishing district.

    2502552602652700.0 km0.1 km0.2 km0.3 km
    Terrain elevation profile (Reservoir): from 267 to 253 m a.s.l. over 0.4 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    253 m a.s.l.
    Lowest point of the profile
    253 m a.s.l.
    Highest point of the profile
    267 m a.s.l.

    Source: Open Topo Data (eudem25m), 4 Nov 2026. The height is approximate (error of a few metres).

    Terrain in 3D

    Loading the 3D terrain model…

    Historical images

    Changes in the surroundings and nature from 2017 to 2023: how the banks, vegetation and landscape around the water change. The images switch automatically; you can also browse them by hand.

    Aerial image of watercourse VN Tríbeč - Sekanina from 2017
    2017imaged 16 Aug 2017
    Aerial image of watercourse VN Tríbeč - Sekanina from 2020
    2020imaged 2 Aug 2020
    Aerial image of watercourse VN Tríbeč - Sekanina from 2023
    2023imaged 1 Jun 2023

    Orthophoto mosaic of Slovakia © GKÚ Bratislava, NLC Zvolen. The year and day of imaging depend on the location, so individual years may differ in season and weather.

    Water pollution on the VN Tríbeč – Sekanina watercourse

    Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby

    Groundwater: measured valuestypical value from stations within 10 km, 2025

    0 of 1 fishing district with measurements has groundwater nearby with a value above the limit for at least one indicator.

    Source: SHMÚ (yearbooks on surface and groundwater quality), the register of wastewater treatment plants from VÚVH and the EEA. A SHMÚ site is assigned to a fishing district by the same watercourse name and by distance; the yearbook lists the sites that failed the standard, so a missing site is not proof of clean water.

    Geology and geochemistry of the VN Tríbeč – Sekanina stream

    Metals and gold in river sediments and water, old mine workings and deposits, boreholes with archive reports, geothermal energy, environmental burdens and landslides around the stream

    The overview is based on public registers and atlases of the State Geological Institute of Dionýz Štúr. The search covers a zone around the water of all fishing districts of the stream (0 km of line in total): stream samples within 1 km, boreholes, mine workings and burdens within 3 km, ore occurrences within 5 km, geothermal sources within 10 km.

    510

    Water according to the atlas

    pH 7.8modelled estimate

    water type Ca–Mg–HCO₃

    Mineralisation 279 mg/l, soft water (8.4 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    0 from 15elements in the top 10 %

    highest: Arsenic 15.3 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 86. Interpolation of the Geochemical Atlas of river sediments.

    20200

    Natural gamma radiation

    67nGy/h dose rate

    percentile 95 in Slovakia

    Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ.

    Old mine workings

    0objects within 3 km

    No old mine working is recorded within 3 km of the water.

    Gold in river sediment

    0samples with gold

    8 ore minerals in the sediment

    No gold was found in river sediment samples within 1 km of the water. The samples do not cover every stream, so this does not mean there is no gold here.

    Trace elements in the stream water

    0 from 8indicators in the top 5 %

    highest: Lithium 10.0 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 75 (Kompanová).

    Boreholes and groundwater analyses

    14boreholes within 3 km

    136 water analyses nearby

    Of these, 14 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    27°C at the wellhead

    1 geothermal borehole within 10 km

    Warmest: Obyce – KD-1, yield 3.5 l/s, 9.9 km from the water.

    Environmental burdens and landfills

    8sites within 3 km

    8 landfills

    No environmental burden is registered within 3 km; landfills are only recorded.

    Deposits and ore occurrences

    4records within 5 km

    3 deposits, 1 ore occurrence

    Geofond registers, the metallogenetic map and the mineral resources map.

    Landslides and slope deformations

    0areas within 3 km

    Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed.

    Geological structure beneath the water

    Which rock lies beneath the water line (Geological Map of Slovakia 1:50,000), how old it is, how thick the Quaternary cover is and in which tectonic unit the water flows. The bedrock decides the hardness of the water, the bottom, the turbidity after rain and the abundance of springs.

    Quaternary cover

    • aeolian sediments100%SR 3.8 %

    marker on the bar: share among all sample points on streams in Slovakia

    • Typical thickness of the Quaternary cover7.5m
    • 5 – 10100%SR 20 %

    marker on the bar: share among all sample points on streams in Slovakia

    Neotectonic units

    • positive unit (mountain range)100%SR 60 %

    marker on the bar: share among all sample points on streams in Slovakia

    Direction of neotectonic movements

    • medium uplift100%SR 32 %

    marker on the bar: share among all sample points on streams in Slovakia

    Regional geological division

    • intramontane basins100%SR 44 %

    marker on the bar: share among all sample points on streams in Slovakia

    Regional geological division (subunits)

    • Danube Basin100%SR 23 %

    marker on the bar: share among all sample points on streams in Slovakia

    Susceptibility of the area to slope deformations

    • Region of stable areas100%SR 95 %

    marker on the bar: share among all sample points on streams in Slovakia

    The map covers 0 of 1 points on the water line.

    Surface water chemistry according to the atlas

    Modelled composition of the water in the area the fishing district line runs through. The rasters of the Geochemical Atlas of Slovakia (surface waters) are an interpolation of measurements in sampled streams, so they show the typical background of the area, not a measurement in a particular stream.

    510

    Water acidity

    pH 7.78typical range

    Most rivers and streams in Slovakia have a pH of 6.5 to 8.5. More acidic water is found in streams on acidic rocks (granites, quartzites), more alkaline water near limestones.

    Water hardness

    8.4°dH, soft

    Sum of calcium and magnesium (1.50 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    279mg/l mineralisation

    Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds.

    Ionic composition of the water

    Water type by dominant ions: Ca–Mg–HCO₃

    Shares are in equivalents, the usual way of comparing the composition of waters.

    Major ions

    • PotassiumK3.19 mg/lpercentile 53
    • SodiumNa9.68 mg/lpercentile 53
    • ChloridesCl9.48 mg/lpercentile 51
    • SulphatesSO433.4 mg/lpercentile 40
    • MagnesiumMg11.2 mg/lpercentile 36
    • BicarbonatesHCO3141 mg/lpercentile 30
    • CalciumCa41.7 mg/lpercentile 29
    • FluoridesF0.0506 mg/lpercentile 5

    dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile)

    Nutrients and organic pollution

    • Chemical oxygen demandChSK7.26 mg/lpercentile 93
    • NitratesNO38.55 mg/lpercentile 66
    • AmmoniumNH40.0914 mg/lpercentile 43
    • PhosphatesPO40.0494 mg/lpercentile 27

    Metals

    • IronFe0.528 mg/lpercentile 93
    • AluminiumAl244 μg/lpercentile 84
    • ManganeseMn66.8 μg/lpercentile 70
    • ZincZn10.5 μg/lpercentile 67

    Elements in river sediments

    The Geochemical Atlas of Slovakia (river sediments) describes what the river carries in the fine material on its bed. Sediment collects metals from rocks, ore occurrences and past mining and industry. It is not a legal limit or a health risk assessment: it shows how an element on this stream ranks among streams in Slovakia.

    Potentially toxic and trace elements

    • ArsenicAs15.3 mg/kgpercentile 86
    • CobaltCo11.7 mg/kgpercentile 85
    • BismuthBi0.255 mg/kgpercentile 63
    • AntimonySb0.796 mg/kgpercentile 62
    • MolybdenumMo0.423 mg/kgpercentile 58
    • ZincZn101 mg/kgpercentile 55
    • VanadiumV69.7 mg/kgpercentile 53
    • CopperCu24.3 mg/kgpercentile 53
    • TinSn2.64 mg/kgpercentile 49
    • NickelNi22.8 mg/kgpercentile 41
    • SeleniumSe0.196 mg/kgpercentile 37
    • LeadPb13.5 mg/kgpercentile 37
    • ChromiumCr55.3 mg/kgpercentile 23
    • MercuryHg0.0553 mg/kgpercentile 17
    • CadmiumCd0.0590 mg/kgpercentile 8

    dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile)

    Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
    • ManganeseMn3,240 mg/kgpercentile 95
    • PotassiumK1.92 %percentile 91
    • TitaniumTi6,214 mg/kgpercentile 88
    • AluminiumAl6.77 %percentile 82
    • PhosphorusP1,073 mg/kgpercentile 74
    • SodiumNa0.990 %percentile 71
    • IronFe3.13 %percentile 70
    • MagnesiumMg0.736 %percentile 31
    • CalciumCa1.05 %percentile 15
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • GalliumGa22.9 mg/kgpercentile 95
    • BariumBa842 mg/kgpercentile 95
    • CeriumCe86.1 mg/kgpercentile 94
    • ZirconiumZr556 mg/kgpercentile 89
    • StrontiumSr196 mg/kgpercentile 86
    • RubidiumRb104 mg/kgpercentile 81
    • LithiumLi34.7 mg/kgpercentile 74
    • BerylliumBe1.62 mg/kgpercentile 63
    • YttriumY29.6 mg/kgpercentile 61
    • BoronB55.0 mg/kgpercentile 34

    Natural radioactivity and radon

    Airborne gamma-ray spectrometry by ŠGÚDŠ measures radiation from potassium, uranium and thorium in rocks and soil. Granites and some acidic volcanic rocks have the highest values, limestones and floodplains the lowest. Caesium-137 is a remnant of fallout from the Chernobyl accident and nuclear weapons tests.

    20200

    Gamma radiation dose rate

    67nGy/h in air

    Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains.

    Radon risk of the bedrock

    medium

    Radon is a natural gas from rocks. The risk concerns buildings and cellars, not the water in the stream; it shows what the bedrock is like.

    • Potassium (K)K1.98 %percentile 95
    • Equivalent uranium (eU)eU3.36 ppm93th percentile
    • Equivalent thorium (eTh)eTh8.47 ppm77th percentile

    dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile)

    • Areal activity of 137CsCS1372,654 Bq/m²percentile 83

    Radon risk by isopleths

    • medium100%SR 64 %

    marker on the bar: share among all sample points on streams in Slovakia

    Geophysical fields: magnetics and gravity

    Maps of the magnetic field and gravity (ŠGÚDŠ) reveal what lies beneath the sediments and the surface: volcanic bodies, faults and crustal thickness. For an angler they are interesting indirectly: they show where the bedrock changes, and with it the water.

    SVJZ

    Magnetic anomaly

    -13nT

    range -13 to -13 nT

    Deviation of the Earth's magnetic field from its surroundings. Positive and negative anomalies reveal rocks with magnetite (basalts, basic volcanic rocks) and boundaries in the bedrock.

    Bouguer gravity anomaly

    -2mGal

    residual +14.3 mGal

    Negative values lie over thick sediments and under mountains (light crust), positive over dense rocks and thinner crust. It shows the structure of the Earth's crust, not the water.

    Geothermal potential

    The Atlas of Geothermal Energy of Slovakia records rock temperature and heat flow from the Earth's interior. It is the potential of the area, not the actual warmth of the water in the stream. Specific geothermal boreholes and springs near this water are in the geothermal energy section below.

    • Rock temperature at 2,000 m depth75°C
    • Surface heat flow density75mW/m²

    Relief, climate and soils

    A basin is not just water: slope and elevation determine the speed of runoff, climate the temperature and amount of water, and soils what is washed into the stream. The data come from the geomorphological division, climatic-geographical types and soil maps of ŠGÚDŠ.

    • Average January temperature-2.8°C
    • Average July temperature19.0°C
    • Annual precipitation675mm

    Climatic-geographical types

    • lowland climate100%SR 38 %

    marker on the bar: share among all sample points on streams in Slovakia

    Soil contamination (map 1:500,000)

    • relatively clean soil100%SR 53 %

    marker on the bar: share among all sample points on streams in Slovakia

    Map of the corridor

    Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off.

    Velčice – none (460 m from the water)Velčice – none (1.0 km from the water)Velčice – occasional (1.4 km from the water)Velčice – none (2.0 km from the water)Velčice – none (2.0 km from the water)Mankovce – Zlatno – none (2.1 km from the water)Mankovce – Hušťavky – Mankovce – none (2.1 km from the water)Velčice – none (2.4 km from the water)Obyce – KD-1 – non-spa (9.9 km from the water)KD-1 – j1 (8.4 km from the water)Zlatno – quartzite (2.4 km from the water)Ladice – ceramic clays (3.3 km from the water)Ladice – ceramic clays (3.3 km from the water)Dolné Sľažany – ceramic clays (4.5 km from the water)Velčice – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Mankovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.5 km from the water)Mankovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.9 km from the water)Velčice – úzkoprofilový vrt s obyčajnou pitnou a ú (2.0 km from the water)Mankovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.0 km from the water)Velčice – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Mankovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)Velčice – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Slažany – štruktúrny vrt s obyčajnou vodou (nad 20 (2.7 km from the water)Velčice – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Zlatno – negative borehole (3.0 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.2 km from the water)výtok z podzemnej drenáže (trubky, horizontálne – Artificial hydrogeologically significant objects (1.5 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.9 km from the water)vodárensky využívaný vrt – Hydrogeological boreholes (2.0 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.0 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.1 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.5 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.7 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.8 km from the water)Velčice, 800m J od rybníka, 700m JV odK314 – well (810 m from the water)Velčice, 1300m JJV od K314 – well (1.5 km from the water)Maňkovce – pri MŠ, 1000m SV od K220 – well (1.9 km from the water)Maňkovce, 600m od mlyna, 1600m SSV od K220 – source (1.9 km from the water)Velčice, 600m ZJZ od K232 – well (2.1 km from the water)Maňkovce – starý mlyn, 1500m JJV od K419 – well (2.2 km from the water)2 km

    The line is the water of the fishing district, the light band is the 3 km zone in which boreholes, mine workings and burdens were searched for. The map shows the nearest objects (at most a few dozen from each register), not all of them. The points correspond to the position in the register; area objects are marked by their centre.

    Trace elements in surface waters

    Arsenic, antimony, cadmium, lead, copper, zinc and other elements in samples from rivers and streams (Geochemical Atlas of Slovakia, surface waters, 2015). The bar shows where the highest value lies among all samples in Slovakia; the light marker is the median of the samples at this water.

    • LithiumLislightly elevated
      highest 10.0 μg/lmedian 10.0 μg/l1 sample

      Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 2.00 μg/lmedian 2.00 μg/l1 sample

      Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • BariumBatypical value
      highest 44.0 μg/lmedian 44.0 μg/l1 sample

      Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 54 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification

      Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l1 sample100 % below the limit of quantification

      Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • ChromiumCrbelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification

      Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 32 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l1 sample100 % below the limit of quantification

      Highest value: Kompanová, 160 m from the water. Comparison: percentile 26 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification

      Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 22 of all samples in Slovakia.

    Major ions, mineralisation and pH

    Basic water chemistry: which rocks the minerals in it come from.

    • Silicon dioxideSiO2slightly elevated
      highest 22.1 mg/lmedian 22.1 mg/l1 sample

      Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 79 of all samples in Slovakia.

    Gold and ore minerals in river sediments

    Regional panning prospecting: the heavy fraction was washed out of river gravel and the mineral grains in it were counted. The map of finds is positive: a sample without gold is not listed in the atlas, so the absence of a find is not proof that there is no gold.

    • Anatas (TiO₂)2 samples, at most 5 grains
    • Hematite (Fe₂O₃)2 samples, at most 815 grains
    • Ilmenit (FeTiO₃)2 samples, at most 815 grains
    • Magnetite (Fe₃O₄)2 samples, at most 315 grains
    • Monazit ((Ce,La,Nd)PO₄)2 samples, at most 5 grains
    • Rutil (TiO₂)2 samples, at most 5 grains
    • Limonite (FeO(OH)·nH₂O)1 sample, at most 55 grains
    • Barite (BaSO₄)1 sample, at most 5 grains

    Rock-forming and accessory minerals

    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))2 samples, at most 815 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)2 samples, at most 5 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)2 samples, at most 5 grains
    • Titanit (CaTiSiO₅)2 samples, at most 74 grains
    • Tourmalines (complex borosilicate)2 samples, at most 55 grains
    • Zirconium (ZrSiO₄)2 samples, at most 155 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)1 sample, at most 5 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))1 sample, at most 315 grains

    Groundwater: chemistry, water types and radioactivity

    Hydrogeochemical objects (analyses of springs and boreholes), the geochemical atlas of groundwater (1996) and radiohydrochemical sampling. Groundwater feeds streams, so its composition also affects the water in the stream.

    Chemical water types nearby

    • Ca-HCO32×
    • Ca-SO4-HCO31×
    • Ca-NO3-SO41×
    • Ca-Mg-HCO31×
    • Ca-Mg-SO4-HCO31×

    Water quality class according to the hydrogeochemical map

    • class F1×
    • class A1×
    • class E1×
    • class H1×
    • class B1×
    • class C1×

    Metals in groundwater

    • LeadPbextreme (top 1 %)
      highest 270 μg/lmedian 0.500 μg/l11 samples73 % below the limit of quantification

      Highest value: studňa1992, 1.9 km from the water. Comparison: percentile 100 of all samples in Slovakia.

    • ZincZnelevated (top 10 %)
      highest 771 μg/lmedian 10.0 μg/l11 samples9 % below the limit of quantification

      Highest value: studňa1992, 810 m from the water. Comparison: percentile 93 of all samples in Slovakia.

    • ArsenicAselevated (top 10 %)
      highest 2.90 μg/lmedian 1.60 μg/l11 samples27 % below the limit of quantification

      Highest value: prameň1992, 1.2 km from the water. Comparison: percentile 92 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.200 μg/lmedian 0.100 μg/l11 samples82 % below the limit of quantification

      Highest value: studňa1992, 1.5 km from the water. Comparison: percentile 83 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 2.50 μg/lmedian 0.500 μg/l11 samples

      Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 80 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 17.0 μg/lmedian 5.00 μg/l11 samples9 % below the limit of quantification

      Highest value: studňa1992, 2.2 km from the water. Comparison: percentile 76 of all samples in Slovakia.

    • ChromiumCrtypical value
      highest 0.600 μg/lmedian 0.250 μg/l11 samples91 % below the limit of quantification

      Highest value: prameň1992, 2.1 km from the water. Comparison: percentile 69 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l6 samples100 % below the limit of quantification

      Highest value: studňa1992, 810 m from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l11 samples100 % below the limit of quantification

      Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l11 samples100 % below the limit of quantification

      Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l11 samples100 % below the limit of quantification

      Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 39 of all samples in Slovakia.

    • AluminiumAlbelow half of Slovakia
      highest 0.00500 mg/lmedian 0.00500 mg/l11 samples100 % below the limit of quantification

      Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 30 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    well14,59 Bq/l4.59 Bq/l

    Mine workings, deposits and ore occurrences

    Old mine workings outside mining areas (Geofond register), deposits and mining areas, and the metallogenetic map. Gold, silver and other metals near streams can get into sediments and water.

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    ZlatnoquartziteDeposit with expected use of reserves – ŠGÚDŠ Bratislava2.4 km
    Ladiceceramic claysDeposit with expected use of reserves – ŠGÚDŠ Bratislava3.3 km
    Ladiceceramic claysDeposit with expected use of reserves – ŠGÚDŠ Bratislava3.3 km

    Boreholes and Geofond archive reports

    Register of hydrogeological boreholes, other boreholes and geothermal boreholes. Each borehole has a report in the Geofond archive (geological profiles, pumping tests, chemical analyses of the water); the report number is in the table.

    14 boreholes in the 3 km zone, of which 11 hydrogeological and 3 other; with an archive report number 14.

    Borehole depths

    • up to 10 m0×
    • 10–30 m4×
    • 30–100 m8×
    • 100–300 m2×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Velčicenarrow-diameter borehole with ordinary drinking and process water62.0 m68885 121Da13.pdf1.2 km
    Mankovcenarrow-diameter borehole with ordinary drinking and process water47.3 m20579 121Da6.pdf1.5 km
    Mankovcewide-diameter borehole45.0 m55106 121Da9.pdf1.9 km
    Velčicenarrow-diameter borehole with ordinary drinking and process water45.0 m43716 121Dc17.pdf2.0 km
    Mankovcenarrow-diameter borehole with ordinary drinking and process water45.0 m55106 121Da10.pdf2.0 km
    VM-4deposit20.0 m829222.1 km
    Velčicenarrow-diameter borehole with ordinary drinking and process water26.2 m5781 121Dc4.pdf2.1 km
    Mankovcenarrow-diameter borehole with ordinary drinking and process water200.0 m87982 121Da17.pdf2.2 km
    Velčicenarrow-diameter borehole with ordinary drinking and process water46.6 m5781 121Dc5.pdf2.5 km
    Slažanystructural borehole with ordinary water170.0 m77716 121Dc30.pdf2.7 km
    VZL-10-91deposit25.0 m793302.7 km
    Velčicenarrow-diameter borehole with ordinary drinking and process water86.0 m78708 121Dc31.pdf2.8 km

    Geothermal energy and mineral waters

    Geothermal boreholes (wellhead water temperature, yield, chemical type) and sources of geothermal and mineral waters within 10 km. Data on the use and existence of a borehole come from the Geofond register.

    BoreholeTemperatureYieldDepthChemical water typeUseFrom the water
    Obyce – KD-127 °C3.5 l/s464.3 mCa-Mg-SO4-HCO3unused9.9 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    KD-1geothermal water22 – 38< 518.4 km

    Environmental burdens, landfills and anthropogenic sediments

    Recorded environmental burdens (industrial sites, landfills, mining), the register of waste landfills and monitoring of anthropogenic sediments (industrial sludge). It is a list of places, not a measurement of water pollution.

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom the water
    Velčice6 000 m²1975–460 m
    Velčice150 m²1970–1.0 km
    Velčice1 000 m²1970–1.4 km
    Velčice240 m²1978–2.0 km
    Velčice250 m²1980–2.0 km
    Mankovce – Zlatno5 000 m²1960–2.1 km
    Mankovce – Hušťavky – Mankovce2 000 m²1960monitored2.1 km
    Velčice15 000 m²1970–2.4 km

    How to read these data

    • Zone and distance. The distance is measured from the line of the water to the point in the register (to the centre for areas), with an accuracy of tens of metres. Counts apply only to the zone, not to the whole catchment.
    • Percentile. For chemistry, the highest value is compared with all atlas samples in Slovakia. It is not a legal limit or a health risk assessment; the atlases are historical (published: surface waters 2015, groundwater 1996, river sediments 1999).
    • Limit of quantification. Many samples have a value at the lowest level the laboratory can determine; such results mean "below the limit". For these, the position in the distribution is an estimate.
    • Panning concentrates. Only samples with a find are recorded. The number of grains in a concentrate is not the gold content in grams per tonne.
    • Relation to water. A mine working, landfill or burden nearby proves nothing about the quality of the water in the stream. It serves as a prompt for attention and a starting point for further investigation.
    • Sample points. The area and raster maps of ŠGÚDŠ cannot be downloaded as points, so along the line of each fishing district the value is looked up at points roughly every 3 km. It is a sample of the line, not a continuous record; a very short section may have a single point.
    • Atlas rasters. The chemistry of water and sediments is an interpolation of measurements in a sampling network (Geochemical Atlas of Slovakia). The value at a point is a modelled estimate for the surroundings, not a measurement in the water. The percentile compares the average of this stream with all sample points on streams in Slovakia.
    • Positions and scales. The maps have different scales (1:50,000 to 1:1,000,000), so the level of detail differs between sections. A map outside its coverage means there is no area at that point, not that there is nothing there.

    Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology.

    Organizations and location

    Who manages the fishing districts and where they are

    Organizations on the watercoursewho manages the fishing districts and what the conditions are there today

    1. OZ Topoľčianky1 fishing district · 0.4 km25VN Tríbeč – Sekanina25

    More watercourses nearby

    Hron basin