Watercourse

Zadielsky potok

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
3.8km
region
Košice Region
Aerial image of watercourse Zadielsky potok 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 Zadielsky potok 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

Zadielsky potok, window score 46.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 18:04.

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 of the watercourse

    How the watercourse falls downstream: fall, gradient and water speed.

    Fast watercourse Podhorský potok: fast water, stony bottom, riffles and the pools below them. Typical trout waters.

    1802002202402600 km1 km2 km3 km
    Elevation profile of the watercourse: from 248 to 196 m a.s.l. over 3.7 km.
    Fishing districts in order from the highest (left) to the lowest. There may be a section without a fishing district between districts; it is not displayed.
    Highest point
    248 m a.s.l.
    Lowest point
    189 m a.s.l.
    Fall of the fishing districtsFallThe difference in altitude between the upper and lower end of the fishing district in metres. The greater the fall over a shorter length, the faster the water.
    59 m
    Average slopeWatercourse gradientFall per kilometre in per mille (‰, metres per kilometre). Up to 2 ‰ is a slow lowland river, 5 to 10 ‰ a foothill river (grayling, trout), above 10 ‰ a fast stream.
    16 ‰
    SinuositySinuosityThe length of the watercourse divided by the straight-line distance between its ends. 1.0 is a straight watercourse; above 1.3 it meanders strongly. Meanders create pools under the banks and shallows in the reaches between.
    1.08

    Source: Open Topo Data (eudem25m), 4 Nov 2026. Gradient and fall are approximate and include only the sections of fishing districts.

    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 Zadielsky potok from 2019
    2019imaged 30 Jun 2019
    Aerial image of watercourse Zadielsky potok from 2022
    2022imaged 30 Aug 2022
    Aerial image of watercourse Zadielsky potok from 2025
    2025imaged 23 Jun 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 Zadielsky potok 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 Zadielsky potok 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 (4 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 alluvium50% of the water line

    50% young sediments

    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 8.4modelled estimate

    water type Ca–HCO₃

    Mineralisation 367 mg/l, moderately hard water (12.8 °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: Bismuth 0.592 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 92. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km40 °C65 °C

    Heat underfoot

    40°C at 1,000 m depth

    heat flow 65 mW/m²

    At a depth of 2,000 m about 65 °C (increase of 25 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    58nGy/h dose rate

    percentile 81 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

    1object within 3 km

    Nearest: Halda cementárne Turňa (spoil heap), 1.4 km from the water.

    Gold in river sediment

    0samples with gold

    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

    1 from 10indicators in the top 5 %

    highest: Chromium 6.50 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 95 (Zádielský náhon, potok).

    Boreholes and groundwater analyses

    319boreholes within 3 km

    220 water analyses nearby

    Of these, 319 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    No geothermal borehole or spring is recorded within 10 km.

    Environmental burdens and landfills

    12sites within 3 km

    12 landfills

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

    Deposits and ore occurrences

    13records within 5 km

    11 deposits, 2 ore occurrences

    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.

    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 alluvium50%SR 72 %
    • Young sediments50%SR 8.6 %

    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×
    QuaternaryPleistoceneproluvial sediments: clay and sandy gravel with rock fragments in low alluvial cones1×

    Quaternary cover

    • fluvial sediments of floodplains50%SR 68 %
    • proluvial sediments of terraced alluvial cones50%SR 2.5 %

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

    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)50%SR 14 %
    • positive unit (mountain range)50%SR 60 %

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

    Direction of neotectonic movements

    • very small uplift50%SR 6.4 %
    • medium uplift50%SR 32 %

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

    Regional geological division

    • intramontane basins50%SR 44 %
    • Gemer Belt50%SR 5.9 %

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

    Regional geological division (subunits)

    • East Slovak Basin50%SR 7.6 %
    • Slovak Karst50%SR 1.9 %

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

    Engineering-geological districts

    • region of lowland-stream deposits50%SR 20 %
    • region of proluvial cones and mantles50%SR 2.7 %

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

    Engineering-geological formations

    • formation of Quaternary sediments100%SR 71 %

    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 2 of 2 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.

    Type of permeability (basic hydrogeological map 1:50,000)

    • intergranular100%SR 86 %

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

    Hydrogeological function

    • aquifer100%SR 95 %

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

    Main hydrogeological region

    • Mesozoic of the central and eastern part of the Slovak Karst100%SR 1.4 %

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

    Genetic type of groundwater

    • carbonatogenic mineralisation100%SR 2.6 %

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

    Chemical type of groundwater

    • Ca-HCO3100%SR 6.1 %

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

    Groundwater quality class

    • F100%SR 8.8 %

    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 8.41typical 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

    12.8°dH, moderately hard

    Sum of calcium and magnesium (2.28 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    367mg/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–HCO₃

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

    Major ions

    • CalciumCa75.6 mg/lpercentile 65
    • SulphatesSO453.4 mg/lpercentile 64
    • ChloridesCl12.3 mg/lpercentile 58
    • BicarbonatesHCO3195 mg/lpercentile 44
    • PotassiumK2.08 mg/lpercentile 33
    • SodiumNa5.51 mg/lpercentile 31
    • MagnesiumMg9.65 mg/lpercentile 30
    • FluoridesF0.0725 mg/lpercentile 25

    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

    • NitratesNO312.4 mg/lpercentile 81
    • PhosphatesPO40.0768 mg/lpercentile 37
    • Chemical oxygen demandChSK1.92 mg/lpercentile 18
    • AmmoniumNH40.0284 mg/lpercentile 8

    Metals

    • AluminiumAl426 μg/lpercentile 93
    • ManganeseMn22.7 μg/lpercentile 42
    • ZincZn2.60 μg/lpercentile 17
    • IronFe0.0389 mg/lpercentile 15

    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

    • BismuthBi0.592 mg/kgpercentile 92
    • ArsenicAs21.9 mg/kgpercentile 91
    • MercuryHg0.486 mg/kgpercentile 89
    • AntimonySb3.95 mg/kgpercentile 89
    • TinSn3.98 mg/kgpercentile 81
    • ZincZn131 mg/kgpercentile 74
    • SeleniumSe0.302 mg/kgpercentile 63
    • CopperCu25.1 mg/kgpercentile 56
    • MolybdenumMo0.401 mg/kgpercentile 54
    • CadmiumCd0.192 mg/kgpercentile 51
    • LeadPb15.6 mg/kgpercentile 50
    • ChromiumCr69.3 mg/kgpercentile 45
    • NickelNi21.7 mg/kgpercentile 36
    • VanadiumV52.7 mg/kgpercentile 14
    • CobaltCo5.39 mg/kgpercentile 10

    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)
    • CalciumCa8.23 %percentile 92
    • PhosphorusP1,234 mg/kgpercentile 85
    • IronFe3.36 %percentile 78
    • PotassiumK1.68 %percentile 75
    • ManganeseMn921 mg/kgpercentile 58
    • AluminiumAl5.68 %percentile 52
    • MagnesiumMg0.843 %percentile 46
    • TitaniumTi3,968 mg/kgpercentile 30
    • SodiumNa0.691 %percentile 17
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • BoronB136 mg/kgpercentile 96
    • LithiumLi42.1 mg/kgpercentile 91
    • CeriumCe64.5 mg/kgpercentile 67
    • RubidiumRb91.9 mg/kgpercentile 59
    • YttriumY27.5 mg/kgpercentile 49
    • BerylliumBe1.36 mg/kgpercentile 47
    • BariumBa412 mg/kgpercentile 41
    • StrontiumSr125 mg/kgpercentile 39
    • GalliumGa10.6 mg/kgpercentile 24
    • ZirconiumZr260 mg/kgpercentile 14

    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

    58nGy/h in air

    range 54 to 61 nGy/h

    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)K1.49 %percentile 83
    • Equivalent thorium (eTh)eTh8.86 ppm82th percentile
    • Equivalent uranium (eU)eU2.78 ppm71th 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 137CsCS137243 Bq/m²percentile 2

    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 -16 to -11 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

    -5mGal

    residual +6.6 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 km40 °C65 °C

    Rock temperature with depth

    40 / 65 °Cat depths of 1,000 and 2,000 m

    increase of 25 °C per km

    The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 65 mW/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.

    • Elevation of geomorphological units (from–to)175–406m a.s.l.
    • Average elevation of the units216m a.s.l.
    • Average slope3.6°
    • Average January temperature-3.8°C
    • Average July temperature17.8°C
    • Annual precipitation700mm

    Geomorphological units

    • Slovak Karst100%SR 0.0 %

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

    Geomorphological regions

    • Slovak Ore Mountains100%SR 10 %

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

    Climatic-geographical types

    • basin climate100%SR 29 %

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

    Susceptibility of soils to acidification

    • soils susceptible to acidification50%SR 31 %
    • soils not susceptible to acidification50%SR 27 %

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

    Soil contamination (map 1:500,000)

    • relatively clean soil50%SR 53 %
    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A50%SR 45 %

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

    Lithogeochemical types

    • Neogene50%SR 48 %
    • Mesozoic of the Bradl zone and the central Western Carpathians50%SR 10 %

    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.

    Halda cementárne Turňa – 5 – spoil heap (1.4 km from the water)Lúčka – Iron ores (3.2 km from the water)Lúčka – Iron ores (4.4 km from the water)Zádielské Dvorníky IV. – Zádiel – none (80 m from the water)Nová Bodva Hosťovce III. – Hosťovce – none (190 m from the water)Zádielské Dvorníky III. – Zádiel – none (310 m from the water)Zádielské Dvorníky II. – Zádiel – none (430 m from the water)Nová Bodva Hosťovce II. – Hosťovce – occasional (820 m from the water)Nová Bodva Hosťovce I. – Hosťovce – none (830 m from the water)Zádielské Dvorníky I. – Zádiel – none (1.3 km from the water)Včeláre I. – Včeláre – none (1.4 km from the water)Včeláre II. – Včeláre – occasional (2.3 km from the water)Nová Bodva Chorváty II. – Chorváty – none (2.6 km from the water)Turnianske Podhradie II – Turňa nad Bodvou – none (2.8 km from the water)Turnianske Podhradie I. – Turňa nad Bodvou – none (3.0 km from the water)Hosťovce – limestone, other (480 m from the water)Včeláre – sialitic raw material (1.8 km from the water)Včeláre – limestone, other (2.4 km from the water)Žarnov I – decorative stone (4.2 km from the water)Hosťovce – limestone, other (480 m from the water)Včeláre – sialitic raw material (1.8 km from the water)Včeláre – limestone, other (2.4 km from the water)Včeláre I – sialitic raw material (3.3 km from the water)Žarnov I – decorative stone (4.2 km from the water)Žarnov – sialitic raw material (4.4 km from the water)Žarnov I – decorative stone (4.2 km from the water)Zádielská tiesňava – geomorphology (480 m from the water)Včeláre – paleontology (3.5 km from the water)Jaskyňa Skalistého potoka – geomorphology (3.9 km from the water)Kunia priepasť, Turnianske Podhradie – geomorphology (3.9 km from the water)Zádielske Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (100 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (150 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (180 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (220 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (240 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (250 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (250 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (510 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (530 m from the water)Zádielske Dvorníky – širokoprofilový vrt (Ø vŕtania nad 600 m (660 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (720 m from the water)Turňa nad Bodvou – negative borehole (760 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (810 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (870 m from the water)Dvorníky – úzkoprofilový vrt s obyčajnou pitnou a ú (880 m from the water)Turňanská Nová Ves – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Turňa nad Bodvou – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.3 km from the water)Turňa nad Bodvou – širokoprofilový vrt (Ø vŕtania nad 600 m (1.6 km from the water)Hosťovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.7 km from the water)Turňa nad Bodvou – úzkoprofilový vrt s obyčajnou pitnou a ú (1.7 km from the water)Turňa nad Bodvou – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Turňa nad Bodvou – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Turňanská Nová Ves – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Hosťovce – monitoring borehole (1.9 km from the water)Hosťovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.9 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.0 km from the water)Turrňa nad Bodvou – úzkoprofilový vrt s obyčajnou pitnou a ú (2.0 km from the water)Turňa nad Bodvou – úzkoprofilový vrt s obyčajnou pitnou a ú (2.0 km from the water)Turňanská Nová Ves – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)Hosťovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)prameň – Groundwater springs (80 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (100 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (150 m from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (150 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (180 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (220 m from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (230 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (240 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (250 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (250 m from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (250 m from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (460 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (510 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (530 m from the water)prameň – Groundwater springs (660 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (660 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (720 m from the water)vodárensky využívaný prameň – Groundwater springs (750 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (760 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (810 m from the water)prameň – Groundwater springs (840 m from the water)vodárensky využívaný prameň – Groundwater springs (850 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (870 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (880 m from the water)vodárensky využívaný a monitorovaný prameň – Groundwater springs (880 m from the water)prameň – Groundwater springs (1.1 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.2 km from the water)prameň – Groundwater springs (1.2 km from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (1.2 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.2 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.3 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.6 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.7 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.8 km from the water)vodárensky využívaný prameň s monitorovaním výda – Groundwater springs (1.8 km from the water)vodárensky využívaný prameň s monitorovaním výda – Groundwater springs (1.9 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.0 km from the water)prameň – Groundwater springs (2.0 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.0 km from the water)Zádiel, č.d. 34, 600m V od K267 – well (60 m from the water)Dvorníky, pred č.d. 39, 500mJ od K269 – source (110 m from the water)Dvorniky, 500m J od K267 – source (550 m from the water)Dvorniky, 800m V od K269 Strážne – well (720 m from the water)Turnianske Podhradie – source (890 m from the water)Hosťovce, 1100m SV od K169 č.d. 94 – well (1.5 km from the water)Turňa nad Bodvou, štátny majetok, 2700m JZ od K1 – well (1.7 km from the water)Turnianske Podhradie – source (1.8 km from the water)Turňa nad Bodvou – prameň Turňa I. – III. – source (1.8 km from the water)Turňa nad Bodvou, 2500m JZ od K190 – source (1.9 km from the water)Hrhov, 400m J od K334 Hradište – source (2.1 km from the water)Včeláre, záchyt pre Carmeuse, prameň Teplá voda – source (2.1 km from the water)Zádielske Dvorníky – Hradisko – source (2.1 km from the water)Hrhov, 1200m V od K424 Kerek – source (2.2 km from the water)Turňa nad Bodvou, č.d. 311, 2000m JZ od K190 – well (2.3 km from the water)Turňa nad Bodvou, č.d. 175, 2400m JZ od K190 – well (2.4 km from the water)Včeláre, 1500m S od K469 – well (2.7 km from the water)Hrhov, 1200m V od K424 Kerek – source (2.7 km from the water)Včeláre, pred domom c.3, 900m VJV od K198 – well (2.8 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.

    • ChromiumCrhigh (top 5 %)
      highest 6.50 μg/lmedian 6.40 μg/l5 samples

      Highest value: Zádielský náhon, potok1993, 160 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • StrontiumSrslightly elevated
      highest 390 μg/lmedian 190 μg/l5 samples

      Highest value: Turňa, potok1993, 210 m from the water. Comparison: percentile 81 of all samples in Slovakia.

    • CadmiumCdslightly elevated
      highest 0.250 μg/lmedian 0.250 μg/l5 samples

      Highest value: Turňa, potok, 210 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.10 μg/lmedian 1.00 μg/l5 samples80 % below the limit of quantification

      Highest value: Turňa, potok1993, 210 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l5 samples100 % below the limit of quantification

      Highest value: Turňa, potok1993, 210 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l5 samples100 % below the limit of quantification

      Highest value: Turňa, potok1993, 210 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • AntimonySbbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l5 samples100 % below the limit of quantification

      Highest value: Turňa, potok1993, 210 m from the water. Comparison: percentile 37 of all samples in Slovakia.

    • BariumBabelow half of Slovakia
      highest 30.0 μg/lmedian 30.0 μg/l5 samples

      Highest value: Turňa, potok1993, 210 m from the water. Comparison: percentile 37 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l5 samples100 % below the limit of quantification

      Highest value: Turňa, potok1993, 210 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l5 samples100 % below the limit of quantification

      Highest value: Turňa, potok1993, 210 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 dioxideSiO2below half of Slovakia
      highest 4.50 mg/lmedian 4.50 mg/l5 samples

      Highest value: Chotárny potok1993, 60 m from the water. Comparison: percentile 10 of all samples in Slovakia.

    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-HCO39×
    • Ca-SO4-HCO37×
    • Ca-Cl-HCO32×
    • Ca-HCO3-SO41×

    Water quality class according to the hydrogeochemical map

    • class A9×
    • class E6×
    • class G1×
    • class H1×
    • class C1×
    • class F1×

    Metals in groundwater

    • CadmiumCdhigh (top 5 %)
      highest 1.70 μg/lmedian 0.250 μg/l15 samples93 % below the limit of quantification

      Highest value: prameň1992, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 1.10 μg/lmedian 0.100 μg/l15 samples60 % below the limit of quantification

      Highest value: studňa1992, 2.8 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ArsenicAselevated (top 10 %)
      highest 3.70 μg/lmedian 0.500 μg/l15 samples73 % below the limit of quantification

      Highest value: studňa1992, 1.7 km from the water. Comparison: percentile 94 of all samples in Slovakia.

    • ZincZnelevated (top 10 %)
      highest 904 μg/lmedian 97.0 μg/l15 samples

      Highest value: studňa1992, 1.5 km from the water. Comparison: percentile 94 of all samples in Slovakia.

    • LeadPbelevated (top 10 %)
      highest 2.00 μg/lmedian 0.500 μg/l15 samples67 % below the limit of quantification

      Highest value: studňa1992, 1.7 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 29.0 μg/lmedian 4.00 μg/l15 samples7 % below the limit of quantification

      Highest value: studňa1992, 2.7 km from the water. Comparison: percentile 86 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 2.80 μg/lmedian 0.500 μg/l15 samples

      Highest value: prameň1992, 1.9 km from the water. Comparison: percentile 82 of all samples in Slovakia.

    • AluminiumAlslightly elevated
      highest 0.0200 mg/lmedian 0.0100 mg/l15 samples13 % below the limit of quantification

      Highest value: studňa1992, 1.5 km from the water. Comparison: percentile 80 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 1.10 μg/lmedian 0.600 μg/l15 samples33 % 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/l14 samples100 % below the limit of quantification

      Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l15 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/l15 samples100 % below the limit of quantification

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

    Radon in waters

    Type of siteSamplesHighest radonMedian
    stream, river40,360 Bq/l0.0500 Bq/l
    water source for public supply20,960 Bq/l0.665 Bq/l
    developed spring16,49 Bq/l6.49 Bq/l
    source12,12 Bq/l2.12 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.

    Types of mining objects

    • spoil heap1×

    Nearest old mine workings

    NameTypeMinedEndedFrom the water
    Halda cementárne Turňaspoil heaplimestone1.4 km

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    Hosťovcelimestone, otherMined deposit – Danucem Slovensko a.s.480 m
    Hosťovcelimestone, otherMined deposit – Danucem Slovensko a.s.480 m
    Včeláresialitic raw materialMined deposit – Danucem Slovensko a.s.1.8 km
    Včeláresialitic raw materialMined deposit – Danucem Slovensko a.s.1.8 km
    Včelárelimestone, otherMined deposit – Carmeuse Slovakia, s.r.o.2.4 km
    Včelárelimestone, otherMined deposit – Carmeuse Slovakia, s.r.o.2.4 km
    Včeláre Isialitic raw materialDeposit with expected use of reserves – Danucem Slovensko a.s.3.3 km
    Žarnov Idecorative stoneMined deposit – KLP s.r.o4.2 km
    Žarnov Idecorative stoneMined deposit – KLP s.r.o4.2 km
    Žarnov Idecorative stoneMined deposit – KLP s.r.o4.2 km
    Žarnovsialitic raw materialDeposit with expected use of reserves – Danucem Slovensko a.s.4.4 km

    Ore occurrences in the metallogenic map

    OccurrenceOre typeMetalsTypeFrom the water
    LúčkaIron oresFemineralogical occurrence3.2 km
    LúčkaIron oresFemineralogical occurrence4.4 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.

    319 boreholes in the 3 km zone, of which 57 hydrogeological and 262 other; with an archive report number 319.

    Borehole depths

    • up to 10 m86×
    • 10–30 m176×
    • 30–100 m42×
    • 100–300 m14×
    • over 300 m1×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    J-201engineering-geological3.3 m7846340 m
    V-8engineering-geological8.0 m396680 m
    V-4engineering-geological11.0 m396680 m
    Zádielske Dvorníkynarrow-diameter borehole with ordinary drinking and process water18.0 m72087 126Ba37.pdf100 m
    V-1engineering-geological12.0 m17293100 m
    V-2engineering-geological12.0 m17293110 m
    V-10engineering-geological8.0 m3966120 m
    V-5engineering-geological8.0 m3966130 m
    Dvorníkynarrow-diameter borehole with ordinary drinking and process water14.4 m38731 126Ba10.pdf150 m
    Dvorníkynarrow-diameter borehole with ordinary drinking and process water15.6 m38731 126Ba9.pdf180 m
    V-9engineering-geological10.0 m3966180 m
    Dvorníkynarrow-diameter borehole with ordinary drinking and process water8.7 m38731 126Ba8.pdf220 m

    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
    Zádielské Dvorníky IV. – Zádiel–1982–80 m
    Nová Bodva Hosťovce III. – Hosťovce250 m²1987–190 m
    Zádielské Dvorníky III. – Zádiel–1982–310 m
    Zádielské Dvorníky II. – Zádiel300 m²1988–430 m
    Nová Bodva Hosťovce II. – Hosťovce400 m²1984–820 m
    Nová Bodva Hosťovce I. – Hosťovce150 m²1985–830 m
    Zádielské Dvorníky I. – Zádiel–1989–1.3 km
    Včeláre I. – Včeláre–––1.4 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.
    • 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. Moldava nad Bodvou1 fishing district · 3.8 km38Zadielsky potok38

    More watercourses nearby

    Bodrog basin and Hornád