Watercourse

VN Bukovec I.

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
1.0km
region
Košice Region
Aerial image of watercourse VN Bukovec I. 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 Bukovec I. watercourse

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

Average of the watercourse's fishing districts

Average 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

06:00–08:00

VN Bukovec I., window score 52.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 17:21.

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.

    3343353363373383393400.0 km0.2 km0.4 km0.6 km0.8 km
    Terrain elevation profile (Reservoir): from 339 to 335 m a.s.l. over 1.0 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    336 m a.s.l.
    Lowest point of the profile
    336 m a.s.l.
    Highest point of the profile
    338 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 Bukovec I. from 2019
    2019imaged 15 Jun 2019
    Aerial image of watercourse VN Bukovec I. from 2022
    2022imaged 30 Aug 2022
    Aerial image of watercourse VN Bukovec I. from 2025
    2025imaged 5 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 Bukovec I. 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.

    • chlorides from 230 mg/l1

    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 Bukovec I. 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 (1 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 192 mg/l, soft water (5.7 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    7 from 15elements in the top 10 %

    highest: Arsenic 124 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 96. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km45 °C75 °C

    Heat underfoot

    45°C at 1,000 m depth

    At a depth of 2,000 m about 75 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    71nGy/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

    5samples with gold

    15 ore minerals in the sediment

    Up to 4 grains in one sample (850 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.

    Trace elements in the stream water

    3 from 10indicators in the top 5 %

    highest: Antimony 18.0 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 98 (Ida).

    Boreholes and groundwater analyses

    49boreholes within 3 km

    198 water analyses nearby

    Of these, 49 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    26°C at the wellhead

    1 geothermal borehole within 10 km

    Warmest: Košice – Anička/ Ťahanovce – G-4, 9.2 km from the water.

    Environmental burdens and landfills

    2sites within 3 km

    2 landfills

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

    Deposits and ore occurrences

    8records within 5 km

    4 deposits, 4 ore occurrences

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

    Landslides and slope deformations

    8areas within 3 km

    1 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×

    Quaternary cover

    • fluvial sediments of floodplains100%SR 68 %

    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

    Tectonic units

    • GEMERIKUM100%SR 13 %

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

    Tectonic division

    • Paleo-Alpine tectonic units of the Inner Western Carpathians100%SR 16 %

    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

    • Gemer Belt100%SR 5.9 %

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

    Regional geological division (subunits)

    • Spiš–Gemer Ore Mountains100%SR 2.9 %

    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 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.

    Aquifer rocks (hydrogeological map 1:200,000)

    • Gravel100%SR 52 %

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

    Aquifer type

    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Gravel)100%SR 22 %

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

    Main hydrogeological region

    • the Paleozoic of the Volovské vrchy in the Bodva basin100%SR 0.0 %

    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 7.86typical 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

    5.7°dH, soft

    Sum of calcium and magnesium (1.02 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    192mg/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

    • FluoridesF0.150 mg/lpercentile 66
    • PotassiumK3.73 mg/lpercentile 61
    • ChloridesCl14.0 mg/lpercentile 61
    • SodiumNa11.7 mg/lpercentile 60
    • SulphatesSO433.1 mg/lpercentile 39
    • MagnesiumMg9.32 mg/lpercentile 29
    • CalciumCa25.5 mg/lpercentile 15
    • BicarbonatesHCO383.3 mg/lpercentile 14

    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

    • NitratesNO310.3 mg/lpercentile 74
    • PhosphatesPO40.257 mg/lpercentile 65
    • Chemical oxygen demandChSK3.33 mg/lpercentile 54
    • AmmoniumNH40.0408 mg/lpercentile 20

    Metals

    • ManganeseMn263 μg/lpercentile 92
    • AluminiumAl221 μg/lpercentile 82
    • IronFe0.207 mg/lpercentile 76
    • ZincZn11.9 μg/lpercentile 71

    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

    • ArsenicAs124 mg/kgpercentile 96
    • LeadPb132 mg/kgpercentile 95
    • AntimonySb41.4 mg/kgpercentile 95
    • CopperCu69.2 mg/kgpercentile 93
    • CadmiumCd0.964 mg/kgpercentile 93
    • MercuryHg0.674 mg/kgpercentile 91
    • BismuthBi0.534 mg/kgpercentile 91
    • ZincZn168 mg/kgpercentile 85
    • TinSn4.06 mg/kgpercentile 82
    • VanadiumV85.7 mg/kgpercentile 79
    • MolybdenumMo0.445 mg/kgpercentile 61
    • NickelNi25.2 mg/kgpercentile 53
    • ChromiumCr72.7 mg/kgpercentile 51
    • CobaltCo7.07 mg/kgpercentile 28
    • SeleniumSe0.0770 mg/kgpercentile 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)

    Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
    • PotassiumK2.00 %percentile 93
    • ManganeseMn1,481 mg/kgpercentile 89
    • TitaniumTi5,800 mg/kgpercentile 83
    • AluminiumAl6.76 %percentile 81
    • IronFe3.14 %percentile 70
    • PhosphorusP762 mg/kgpercentile 38
    • MagnesiumMg0.608 %percentile 14
    • SodiumNa0.634 %percentile 11
    • CalciumCa0.463 %percentile 3
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • BoronB141 mg/kgpercentile 96
    • BerylliumBe2.74 mg/kgpercentile 95
    • RubidiumRb123 mg/kgpercentile 95
    • YttriumY41.1 mg/kgpercentile 94
    • LithiumLi37.2 mg/kgpercentile 82
    • GalliumGa17.3 mg/kgpercentile 77
    • BariumBa504 mg/kgpercentile 71
    • ZirconiumZr423 mg/kgpercentile 57
    • CeriumCe58.9 mg/kgpercentile 49
    • StrontiumSr67.9 mg/kgpercentile 3

    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

    71nGy/h in air

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

    • Potassium (K)K2.08 %percentile 96
    • Equivalent thorium (eTh)eTh10.1 ppm95th percentile
    • Equivalent uranium (eU)eU3.22 ppm90th 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 137CsCS137399 Bq/m²percentile 4

    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

    -54nT

    range -54 to -54 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

    +0mGal

    residual +13.1 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 °C75 °C

    Rock temperature with depth

    45 / 75 °Cat depths of 1,000 and 2,000 m

    increase of 30 °C per km

    The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow –.

    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.

    • Elevation of geomorphological units (from–to)194–562m a.s.l.
    • Average elevation of the units304m a.s.l.
    • Average slope5.0°

    Geomorphological units

    • Košice Basin100%SR 2.8 %

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

    Geomorphological regions

    • Lučenec–Košice Depression100%SR 7.6 %

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

    Susceptibility of soils to acidification

    • soils susceptible to acidification100%SR 31 %

    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.

    Nižný Klátov, žila Mlynky – Complex iron ores (2.4 km from the water)Baška II. – Baška – cannot be estimated (2.0 km from the water)Malá Ida II. – Malá Ida – cannot be estimated (3.0 km from the water)Košice – Anička/ Ťahanovce – G-4 – non-spa (9.2 km from the water)a1 (7.8 km from the water)Vyšný Klátov I – building stone (4.6 km from the water)Hodkovce I – ceramic clays (5.0 km from the water)Vyšný Klátov I – building stone (4.5 km from the water)Košice – hĺbka – magnesite (4.9 km from the water)Nižný Klátov – Mlynky – building stone – amphibolite (2.3 km from the water)Myslava – building stone – silicified tuffites (3.0 km from the water)Myslava – gravelly sands (3.4 km from the water)Vyšný Klátov – general geology (2.9 km from the water)Košice – mineralogy (3.0 km from the water)BUKOVEC – Landslides (780 m from the water)BUKOVEC – Landslides (820 m from the water)BASKA – Landslides (1.8 km from the water)MYSLAVA – Landslides (2.0 km from the water)NIZNY KLATOV – Landslides (2.4 km from the water)LORINCIK – Landslides (2.6 km from the water)MYSLAVA – Landslides (2.8 km from the water)LORINCIK – Landslides (2.9 km from the water)Bukove – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Bukovec – širokoprofilový vrt (Ø vŕtania nad 600 m (1.9 km from the water)Bukovec – úzkoprofilový vrt s obyčajnou pitnou a ú (2.3 km from the water)Malá Ida – SHMÚ observation borehole (2.3 km from the water)Malá Ida – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Nižný Klátov – úzkoprofilový vrt s obyčajnou pitnou a ú (2.6 km from the water)Myslava – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Lorinčík – Košice – širokoprofilový vrt (Ø vŕtania nad 600 m (2.8 km from the water)zlato 1 ks – gold (460 m from the water)zlato 3 ks – gold (620 m from the water)zlato 3 ks – gold (720 m from the water)zlato 1 ks – gold (850 m from the water)zlato 4 ks – gold (850 m 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.

    • AntimonySbhigh (top 5 %)
      highest 18.0 μg/lmedian 11.4 μg/l3 samples

      Highest value: Ida1993, 140 m from the water. Comparison: percentile 98 of all samples in Slovakia.

    • ChromiumCrhigh (top 5 %)
      highest 7.50 μg/lmedian 6.00 μg/l3 samples

      Highest value: Ida1993, 140 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ArsenicAshigh (top 5 %)
      highest 9.30 μg/lmedian 8.70 μg/l3 samples

      Highest value: Ida1993, 140 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 3.80 μg/lmedian 2.50 μg/l3 samples

      Highest value: Ida1993, 140 m from the water. Comparison: percentile 85 of all samples in Slovakia.

    • CadmiumCdslightly elevated
      highest 0.250 μg/lmedian 0.250 μg/l3 samples

      Highest value: Ida, 190 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l3 samples100 % below the limit of quantification

      Highest value: Ida1993, 190 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l3 samples100 % below the limit of quantification

      Highest value: Ida1993, 190 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l3 samples100 % below the limit of quantification

      Highest value: Ida1993, 190 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • StrontiumSrbelow half of Slovakia
      highest 60.0 μg/lmedian 60.0 μg/l3 samples

      Highest value: Ida1993, 190 m from the water. Comparison: percentile 16 of all samples in Slovakia.

    • BariumBabelow half of Slovakia
      highest 10.0 μg/lmedian 10.0 μg/l3 samples

      Highest value: Ida1993, 190 m from the water. Comparison: percentile 10 of all samples in Slovakia.

    Major ions, mineralisation and pH

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

    • Silicon dioxideSiO2typical value
      highest 13.1 mg/lmedian 9.19 mg/l3 samples

      Highest value: 800m JV od K496 Zámčisko1993, 610 m from the water. Comparison: percentile 59 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.

    • Hematite (Fe₂O₃)10 samples, at most 4115 grains
    • Ilmenit (FeTiO₃)10 samples, at most 4115 grains
    • Magnetite (Fe₃O₄)10 samples, at most 4115 grains
    • Rutil (TiO₂)10 samples, at most 815 grains
    • Limonite (FeO(OH)·nH₂O)9 samples, at most 4115 grains
    • Anatas (TiO₂)8 samples, at most 55 grains
    • Pyrite (FeS₂)8 samples, at most 55 grains
    • Barite (BaSO₄)5 samples, at most 315 grains
    • Gold (Au)5 samples, at most 4 grains
    • Monazit ((Ce,La,Nd)PO₄)4 samples, at most 55 grains
    • Arsenopyrite (FeAsS)4 samples, at most 5 grains
    • Cinabarit (HgS)4 samples, at most 22 grains
    • Sphalerite (ZnS)4 samples, at most 50 grains
    • Scheelit (CaWO₄)2 samples, at most 8 grains
    • Kasiterit (SnO₂)2 samples, at most 50 grains

    Nearest samples with gold

    SampleGold in sampleFrom the water
    1031 grain460 m
    1023 grains620 m
    3413 grains720 m
    1011 grain850 m
    3424 grains850 m

    Rock-forming and accessory minerals

    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))10 samples, at most 555 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)10 samples, at most 5 grains
    • Tourmalines (complex borosilicate)10 samples, at most 55 grains
    • Zirconium (ZrSiO₄)10 samples, at most 1815 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)7 samples, at most 155 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)6 samples, at most 55 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))3 samples, at most 5 grains
    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)2 samples, at most 5 grains
    • Korund (Al₂O₃)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

    • AntimonySbextreme (top 1 %)
      highest 34.0 μg/lmedian 0.100 μg/l15 samples67 % below the limit of quantification

      Highest value: studňa1992, 2.9 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • ZincZnextreme (top 1 %)
      highest 7,100 μg/lmedian 318 μg/l15 samples

      Highest value: studňa1992, 1.6 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • ArsenicAsextreme (top 1 %)
      highest 40.5 μg/lmedian 0.500 μg/l15 samples73 % below the limit of quantification

      Highest value: studňa1992, 2.9 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 5.00 μg/lmedian 0.500 μg/l15 samples73 % below the limit of quantification

      Highest value: studňa1993, 2.0 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • MercuryHghigh (top 5 %)
      highest 0.300 μg/lmedian 0.100 μg/l15 samples60 % below the limit of quantification

      Highest value: studňa1992, 2.9 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 0.600 μg/lmedian 0.250 μg/l15 samples87 % below the limit of quantification

      Highest value: studňa1993, 2.0 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • AluminiumAlhigh (top 5 %)
      highest 0.0800 mg/lmedian 0.00500 mg/l15 samples93 % below the limit of quantification

      Highest value: studňa1993, 2.0 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • CopperCuelevated (top 10 %)
      highest 5.30 μg/lmedian 0.250 μg/l15 samples

      Highest value: studňa1992, 2.5 km from the water. Comparison: percentile 94 of all samples in Slovakia.

    • SeleniumSeslightly elevated
      highest 1.40 μg/lmedian 0.500 μg/l15 samples80 % below the limit of quantification

      Highest value: studňa1992, 2.2 km from the water. Comparison: percentile 87 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 28.0 μg/lmedian 5.00 μg/l15 samples13 % below the limit of quantification

      Highest value: studňa1992, 3.0 km from the water. Comparison: percentile 86 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 0.900 μg/lmedian 0.250 μg/l15 samples80 % below the limit of quantification

      Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 76 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l7 samples100 % below the limit of quantification

      Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    well16,14 Bq/l6.14 Bq/l
    stream, river30,470 Bq/l0.340 Bq/l
    source614,0 Bq/l6.39 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
    Vyšný Klátov Ibuilding stoneMined deposit – RICORSO, s.r.o.4.5 km
    Vyšný Klátov Ibuilding stoneMined deposit – RICORSO, s.r.o.4.6 km
    Košice – depthmagnesiteDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.9 km
    Hodkovce Iceramic claysDeposit with expected use of reserves – Organizácia neurčená5.0 km

    Ore occurrences in the metallogenic map

    OccurrenceOre typeMetalsTypeFrom the water
    Nižný Klátov, žila MlynkyComplex iron oresFe, Cumineralogical occurrence2.4 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.

    49 boreholes in the 3 km zone, of which 8 hydrogeological and 41 other; with an archive report number 49.

    Borehole depths

    • up to 10 m16×
    • 10–30 m24×
    • 30–100 m5×
    • 100–300 m4×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    V-4engineering-geological18.8 m232370 m
    V-3engineering-geological23.9 m232380 m
    V-2engineering-geological13.6 m2323150 m
    V-5engineering-geological12.0 m2323160 m
    V-1engineering-geological11.0 m2323230 m
    R-24engineering-geological8.0 m807821.2 km
    604/72deposit187.5 m763081.5 km
    JV-1engineering-geological7.0 m937991.5 km
    MI-12-69deposit14.2 m262491.6 km
    DP-1engineering-geological6.0 m937991.6 km
    DP-2engineering-geological6.0 m937991.6 km
    MI-11-69deposit10.0 m262491.6 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
    Košice – Anička/ Ťahanovce – G-426 °C–310 mNa-Ca-Mg-HCO3-Clunused9.2 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 517.8 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
    Baška II. – Baška–1980–2.0 km
    Malá Ida II. – Malá Ida350 m²1980–3.0 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

    • Landslides8×

    Degree of activity

    • Potenciálny6×
    • Stabilizovaný1×
    • Aktívny1×

    Current state

    • Processed only in the scope of registration on a scale of 1:25,0006×
    • SD prebraná z archívnych materiálov (existuje inž. geologick1×
    • Insufficiently documented1×

    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. Košice1 fishing district · 1.0 km43VN Bukovec I.43

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