Today on the VN Sigord 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 Sigord, window score 30.

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

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
Pick a category to narrow the selection. Next to each option you can see how many fishing districts remain.
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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.

    4004054104154204250.0 km0.1 km0.2 km0.3 km
    Terrain elevation profile (Reservoir): from 422 to 406 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
    414 m a.s.l.
    Lowest point of the profile
    406 m a.s.l.
    Highest point of the profile
    422 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 2019 to 2025: 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 Sigord from 2019
    2019imaged 1 Jul 2019
    Aerial image of watercourse VN Sigord from 2022
    2022imaged 8 Oct 2022
    Aerial image of watercourse VN Sigord from 2025
    2025imaged 3 Jul 2025

    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 Sigord 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

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

    • harmful substances above the standard at at least one station (metals, pesticides, PFAS, solvents)1

    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 Sigord 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.

    Rock under the water

    River alluvium100% of the water line

    Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000.

    510

    Water according to the atlas

    pH 7.9modelled estimate

    water type Ca–Mg–HCO₃–SO₄

    Mineralisation 250 mg/l, soft water (7.7 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    2 from 15elements in the top 10 %

    highest: Mercury 1.88 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 95. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km45 °C85 °C

    Heat underfoot

    45°C at 1,000 m depth

    heat flow 85 mW/m²

    At a depth of 2,000 m about 85 °C (increase of 40 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    57nGy/h dose rate

    percentile 79 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

    2samples with gold

    15 ore minerals in the sediment

    Up to 3 grains in one sample (650 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.

    Trace elements in the stream water

    0 from 10indicators in the top 5 %

    highest: Antimony 1.50 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 90 (Malá Delna, pod nádržou).

    Boreholes and groundwater analyses

    52boreholes within 3 km

    124 water analyses nearby

    Of these, 50 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    12 geothermal and mineral water springs within 10 km.

    Environmental burdens and landfills

    5sites within 3 km

    5 landfills

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

    Deposits and ore occurrences

    3records within 5 km

    3 ore occurrences

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

    Landslides and slope deformations

    16areas within 3 km

    2 active

    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.

    The points follow the water line (for a stream and a basin, fishing district after fishing district). The strip is a cross-section by distance, not a map; the width of a section corresponds to the number of points.

    • River alluvium100%SR 72 %

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

    River alluvium: Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium.

    Geological age of the rocks

    • Quaternary100%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains1×

    Tectonic division

    • NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

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

    Neotectonic units

    • positive unit (lowland hills)100%SR 14 %

    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

    • neovolcanic rocks100%SR 10 %

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

    Regional geological division (subunits)

    • neovolcanic rocks of the Slanské vrchy100%SR 1.2 %

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

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

    Hydrogeology: aquifers and groundwater

    Streams and rivers are fed by groundwater. Hydrogeological maps show in which rocks the water is stored, how permeable they are and what the water in them is like. The data come from ŠGÚDŠ maps, not from measurements at a particular water.

    Main hydrogeological region

    • neovolcanic rocks of the Slanské vrchy100%SR 1.7 %

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

    Geothermal groundwater bodies

    • Košice Basin100%SR 4.8 %

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

    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 7.94typical 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

    7.7°dH, soft

    Sum of calcium and magnesium (1.37 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    250mg/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–SO₄

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

    Major ions

    • SulphatesSO470.4 mg/lpercentile 76
    • FluoridesF0.168 mg/lpercentile 72
    • SodiumNa12.9 mg/lpercentile 65
    • PotassiumK3.10 mg/lpercentile 52
    • ChloridesCl6.85 mg/lpercentile 43
    • MagnesiumMg11.2 mg/lpercentile 36
    • CalciumCa36.4 mg/lpercentile 24
    • BicarbonatesHCO3106 mg/lpercentile 20

    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 demandChSK2.33 mg/lpercentile 28
    • PhosphatesPO40.0452 mg/lpercentile 25
    • NitratesNO31.74 mg/lpercentile 5
    • AmmoniumNH40.0257 mg/lpercentile 3

    Metals

    • ZincZn31.5 μg/lpercentile 93
    • AluminiumAl415 μg/lpercentile 93
    • ManganeseMn196 μg/lpercentile 90
    • IronFe0.193 mg/lpercentile 74

    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

    • MercuryHg1.88 mg/kgpercentile 95
    • CadmiumCd0.900 mg/kgpercentile 92
    • ArsenicAs17.3 mg/kgpercentile 88
    • ZincZn165 mg/kgpercentile 84
    • AntimonySb2.07 mg/kgpercentile 83
    • VanadiumV90.3 mg/kgpercentile 83
    • TinSn3.66 mg/kgpercentile 77
    • BismuthBi0.315 mg/kgpercentile 76
    • CobaltCo10.4 mg/kgpercentile 75
    • LeadPb16.9 mg/kgpercentile 57
    • CopperCu19.5 mg/kgpercentile 31
    • MolybdenumMo0.282 mg/kgpercentile 30
    • SeleniumSe0.156 mg/kgpercentile 26
    • ChromiumCr56.9 mg/kgpercentile 26
    • NickelNi18.6 mg/kgpercentile 24

    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)
    • AluminiumAl7.20 %percentile 89
    • TitaniumTi6,310 mg/kgpercentile 89
    • IronFe3.83 %percentile 88
    • ManganeseMn1,196 mg/kgpercentile 78
    • SodiumNa0.982 %percentile 70
    • MagnesiumMg0.982 %percentile 59
    • PotassiumK1.44 %percentile 39
    • CalciumCa1.65 %percentile 38
    • PhosphorusP662 mg/kgpercentile 25
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • BoronB74.6 mg/kgpercentile 82
    • YttriumY33.4 mg/kgpercentile 77
    • LithiumLi30.6 mg/kgpercentile 56
    • BerylliumBe1.44 mg/kgpercentile 52
    • GalliumGa14.2 mg/kgpercentile 51
    • StrontiumSr128 mg/kgpercentile 42
    • ZirconiumZr374 mg/kgpercentile 40
    • RubidiumRb82.1 mg/kgpercentile 33
    • BariumBa389 mg/kgpercentile 32
    • CeriumCe49.9 mg/kgpercentile 18

    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

    57nGy/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

    low

    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.

    • Equivalent uranium (eU)eU3.07 ppm85th percentile
    • Equivalent thorium (eTh)eTh8.84 ppm82th percentile
    • Potassium (K)K1.29 %percentile 45

    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 137CsCS1372,493 Bq/m²percentile 81

    Radon risk by isopleths

    • low100%SR 36 %

    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

    -82nT

    range -82 to -82 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

    -24mGal

    residual −3.2 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.

    1 km2 km45 °C85 °C

    Rock temperature with depth

    45 / 85 °Cat depths of 1,000 and 2,000 m

    increase of 40 °C per km

    The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 85 mW/m².

    Geothermal groundwater bodies beneath the water line

    • Košice Basin100%SR 4.8 %

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

    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-3.8°C
    • Average July temperature17.8°C
    • Annual precipitation700mm

    Climatic-geographical types

    • basin climate100%SR 29 %

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

    Soil contamination (map 1:500,000)

    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A100%SR 45 %

    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.

    Šťavica – Polymetallic ores (3.3 km from the water)Záborské – cannot be estimated (820 m from the water)Kokošovce – cannot be estimated (1.5 km from the water)Baňa – Klenov – cannot be estimated (1.7 km from the water)Bučinová stredná dolina – Kendice – cannot be estimated (1.9 km from the water)Piesková jama – Ruská Nová Ves – none (3.0 km from the water)a1 (2.0 km from the water)a1 (5.2 km from the water)a1 (7.1 km from the water)a1 (7.5 km from the water)a1 (8.2 km from the water)a1 (8.4 km from the water)a1 (8.7 km from the water)a1 (8.7 km from the water)a1 (8.9 km from the water)a1 (9.6 km from the water)a1 (9.8 km from the water)a1 (9.9 km from the water)Zlatá Baňa Šťavica – building stone – diorite porphyry (3.1 km from the water)Žehňa 89 – building stone – andesite (4.0 km from the water)Kokošovce – Landslides (130 m from the water)Kokošovce – Landslides (140 m from the water)KOKOSOVCE – Block fields (280 m from the water)Kokošovce – Landslides (320 m from the water)Kokošovce – Landslides (330 m from the water)– Landslides (690 m from the water)ABRANOVCE – Landslides (920 m from the water)KOKOSOVCE – Landslides (1.2 km from the water)KOKOSOVCE – Landslides (1.4 km from the water)– Landslides (1.5 km from the water)– Block fields (1.8 km from the water)– Landslides (2.3 km from the water)RUSKA NOVA VES – Landslides (2.5 km from the water)PETROVCE – Landslides (2.5 km from the water)KOKOSOVCE – Landslides (2.5 km from the water)DULOVA VES – Landslides (2.8 km from the water)Sigord – negative borehole (80 m from the water)Sigord – negative borehole (80 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (150 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (170 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (230 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (240 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (330 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (380 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (390 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (540 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (620 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (870 m from the water)Kokošovce – negative borehole (970 m from the water)Kokošovce – úzkoprofilový vrt s obyčajnou pitnou a ú (980 m from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (1.0 km from the water)Abramovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.3 km from the water)Kokošovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.7 km from the water)Abranovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.0 km from the water)Abranovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (2.3 km from the water)Dulova Ves – širokoprofilový vrt (Ø vŕtania nad 600 m (2.7 km from the water)Zlatá Baňa – Sigord – úzkoprofilový vrt s obyčajnou pitnou a ú (2.9 km from the water)Dulova Ves – širokoprofilový vrt (Ø vŕtania nad 600 m (2.9 km from the water)zlato 3 ks – gold (650 m from the water)zlato 3 ks – gold (840 m from the water)5 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.

    • AntimonySbelevated (top 10 %)
      highest 1.50 μg/lmedian 1.50 μg/l1 sample

      Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 90 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 3.40 μg/lmedian 3.40 μg/l1 sample

      Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 86 of all samples in Slovakia.

    • CadmiumCdslightly elevated
      highest 0.250 μg/lmedian 0.250 μg/l1 sample

      Highest value: Malá Delna, pod nádržou, 80 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.20 μg/lmedian 1.20 μg/l1 sample

      Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 48 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: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • StrontiumSrbelow half of Slovakia
      highest 150 μg/lmedian 150 μg/l1 sample

      Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 44 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: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l1 sample100 % below the limit of quantification

      Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 34 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: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 32 of all samples in Slovakia.

    • BariumBabelow half of Slovakia
      highest 20.0 μg/lmedian 20.0 μg/l1 sample

      Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 23 of all samples in Slovakia.

    Major ions, mineralisation and pH

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

    • Silicon dioxideSiO2elevated (top 10 %)
      highest 32.8 mg/lmedian 32.8 mg/l1 sample

      Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 91 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.

    • Ilmenit (FeTiO₃)12 samples, at most 4115 grains
    • Limonite (FeO(OH)·nH₂O)12 samples, at most 815 grains
    • Magnetite (Fe₃O₄)12 samples, at most 4115 grains
    • Cinabarit (HgS)9 samples, at most 50 grains
    • Rutil (TiO₂)6 samples, at most 5 grains
    • Anatas (TiO₂)5 samples, at most 5 grains
    • Barite (BaSO₄)2 samples, at most 5 grains
    • Gold (Au)2 samples, at most 3 grains
    • Antimonite (Sb₂S₃)1 sample, at most 5 grains
    • Chalcopyrite (CuFeS₂)1 sample, at most 5 grains
    • Kasiterit (SnO₂)1 sample, at most 5 grains
    • Monazit ((Ce,La,Nd)PO₄)1 sample, at most 5 grains
    • Pyrite (FeS₂)1 sample, at most 5 grains
    • Scheelit (CaWO₄)1 sample, at most 5 grains
    • Hematite (Fe₂O₃)1 sample, at most 55 grains

    Nearest samples with gold

    SampleGold in sampleFrom the water
    10563 grains650 m
    10773 grains840 m

    Rock-forming and accessory minerals

    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)12 samples, at most 815 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)12 samples, at most 4115 grains
    • Zirconium (ZrSiO₄)12 samples, at most 315 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))3 samples, at most 5 grains
    • Korund (Al₂O₃)1 sample, at most 5 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))1 sample, at most 5 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.

    Metals in groundwater

    • CopperCuextreme (top 1 %)
      highest 34.2 μg/lmedian 1.48 μg/l10 samples

      Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AluminiumAlextreme (top 1 %)
      highest 1.44 mg/lmedian 0.00500 mg/l10 samples60 % below the limit of quantification

      Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 1.90 μg/lmedian 0.100 μg/l10 samples80 % below the limit of quantification

      Highest value: studňa1992, 1.4 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • MercuryHghigh (top 5 %)
      highest 0.300 μg/lmedian 0.100 μg/l10 samples90 % below the limit of quantification

      Highest value: vrt1992, 850 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ArsenicAshigh (top 5 %)
      highest 5.80 μg/lmedian 0.950 μg/l10 samples50 % below the limit of quantification

      Highest value: vrt1992, 850 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 3.00 μg/lmedian 0.500 μg/l10 samples70 % below the limit of quantification

      Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LithiumLielevated (top 10 %)
      highest 39.0 μg/lmedian 6.50 μg/l10 samples10 % below the limit of quantification

      Highest value: prameň1992, 1.9 km from the water. Comparison: percentile 92 of all samples in Slovakia.

    • ChromiumCrelevated (top 10 %)
      highest 2.10 μg/lmedian 0.250 μg/l10 samples60 % below the limit of quantification

      Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • ZincZnslightly elevated
      highest 213 μg/lmedian 54.5 μg/l10 samples10 % below the limit of quantification

      Highest value: studňa1992, 1.7 km from the water. Comparison: percentile 79 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l3 samples100 % below the limit of quantification

      Highest value: studňa1992, 1.7 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l10 samples100 % below the limit of quantification

      Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification

      Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 39 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    water source for public supply11,29 Bq/l1.29 Bq/l
    mineral spring17,09 Bq/l7.09 Bq/l
    water source for individual supply17,72 Bq/l7.72 Bq/l
    source15,66 Bq/l5.66 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.

    Ore occurrences in the metallogenic map

    OccurrenceOre typeMetalsTypeFrom the water
    ŠťavicaPolymetallic oresPb, Znmineralogical occurrence3.3 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.

    52 boreholes in the 3 km zone, of which 23 hydrogeological and 29 other; with an archive report number 50.

    Borehole depths

    • up to 10 m21×
    • 10–30 m19×
    • 30–100 m2×
    • 100–300 m8×
    • over 300 m2×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Sigordnegative borehole155.0 m83973 115Ba115.pdf80 m
    Sigordnegative borehole125.0 m83973 115Ba116.pdf80 m
    Sigordnarrow-diameter borehole with ordinary drinking and process water20.0 m83973 115Ba117.pdf150 m
    Sigordnarrow-diameter borehole with ordinary drinking and process water15.0 m83973 115Ba118.pdf170 m
    Sigordnarrow-diameter borehole with ordinary drinking and process water20.0 m83973 115Ba119.pdf230 m
    Sigordnarrow-diameter borehole with ordinary drinking and process water9.0 m83973 115Ba121.pdf240 m
    J-12engineering-geological25.0 m83973250 m
    Sigordnarrow-diameter borehole with ordinary drinking and process water23.0 m83973 115Ba122.pdf330 m
    J-13engineering-geological20.0 m83973340 m
    Sigordnarrow-diameter borehole with ordinary drinking and process water100.0 m70619 115Ba81.pdf380 m
    Sigordnarrow-diameter borehole with ordinary drinking and process water25.0 m83973 115Ba120.pdf390 m
    Sigordnarrow-diameter borehole with ordinary drinking and process water24.0 m83973 115Ba123.pdf540 m

    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.

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 5122.0 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
    Záborské–1980–820 m
    Kokošovce1 200 m²1989–1.5 km
    Baňa – Klenov–1990–1.7 km
    Bučinová stredná dolina – Kendice–1985–1.9 km
    Piesková jama – Ruská Nová Ves500 m²1989–3.0 km

    Landslides and slope deformations

    Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel.

    Types of deformations

    • Landslides14×
    • Block fields2×

    Degree of activity

    • Potenciálny11×
    • Stabilizovaný3×
    • Aktívny2×

    Current state

    • SD taken from archival materials, ktorá bola konfrontova5×
    • SD prebraná z archívnych materiálov (existuje inž. geologick4×
    • Insufficiently documented3×
    • Processed only in the scope of registration on a scale of 1:25,0001×

    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.
    • Šlichy. 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. Prešov1 fishing district · 0.4 km21VN Sigord21

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