Today on the VVN Domaša 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

VVN Domaša, window score 17.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 01:04.

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: standing water

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

    Still water This is standing water, 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.

    1301401501600 km1 km2 km3 km4 km
    Terrain elevation profile (Standing water): from 158 to 133 m a.s.l. over 4.6 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    134 m a.s.l.
    Lowest point of the profile
    133 m a.s.l.
    Highest point of the profile
    158 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 VVN Domaša from 2019
    2019imaged 19 Aug 2019
    Aerial image of watercourse VVN Domaša from 2022
    2022imaged 27 Aug 2022
    Aerial image of watercourse VVN Domaša from 2025
    2025imaged 24 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 VVN Domaša 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
    • ammonium or nitrites above the standard at at least one station1

    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 VVN Domaša 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 (5 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 8.2modelled estimate

    water type Ca–HCO₃

    Mineralisation 136 mg/l, moderately hard water (11.2 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    1 from 15elements in the top 10 %

    highest: Chromium 130 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 91. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km45 °C75 °C

    Heat underfoot

    45°C at 1,000 m depth

    heat flow 75 mW/m²

    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

    48nGy/h dose rate

    percentile 28 in Slovakia

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

    Old mine workings

    0objects within 3 km

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

    Gold in river sediment

    0samples with gold

    10 ore minerals in the sediment

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

    Trace elements in the stream water

    2 from 6indicators in the top 5 %

    highest: Cadmium 1.00 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 96 (Ondava).

    Boreholes and groundwater analyses

    104boreholes within 3 km

    227 water analyses nearby

    Of these, 104 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    7 geothermal and mineral water springs within 10 km.

    Environmental burdens and landfills

    14sites within 3 km

    14 landfills

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

    Deposits and ore occurrences

    10records within 5 km

    10 ore occurrences

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

    Landslides and slope deformations

    53areas within 3 km

    6 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 floodplains2×
    QuaternaryHolocenefluvial sediments: resedimented alluvial sandy gravels of the near-channel zone1×

    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

    • ORAVIKUM100%SR 1.8 %

    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 (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

    • Inner Carpathian Paleogene100%SR 11 %

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

    Regional geological division (subunits)

    • Spiš–Šariš Paleogene100%SR 5.8 %

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

    Engineering-geological districts

    • region of mountain-stream deposits100%SR 21 %

    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 3 of 3 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)

    • Sandstones100%SR 15 %

    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 (Sandstones)50%SR 15 %
    • ;;50%SR 0.5 %

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

    Main hydrogeological region

    • Paleogene basin of Ondava to Kučín100%SR 2.7 %

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

    Geothermal groundwater bodies

    • Humenné Ridge100%SR 4.4 %

    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 8.15typical 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

    11.2°dH, moderately hard

    Sum of calcium and magnesium (2.00 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    136mg/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

    • FluoridesF0.374 mg/lpercentile 95
    • SodiumNa21.3 mg/lpercentile 81
    • PotassiumK6.14 mg/lpercentile 81
    • BicarbonatesHCO3274 mg/lpercentile 70
    • SulphatesSO448.4 mg/lpercentile 60
    • CalciumCa61.0 mg/lpercentile 48
    • ChloridesCl6.57 mg/lpercentile 42
    • MagnesiumMg11.6 mg/lpercentile 37

    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

    • NitratesNO37.28 mg/lpercentile 58
    • AmmoniumNH40.123 mg/lpercentile 54
    • Chemical oxygen demandChSK3.27 mg/lpercentile 52
    • PhosphatesPO40.0596 mg/lpercentile 31

    Metals

    • AluminiumAl77.0 μg/lpercentile 54
    • IronFe0.0609 mg/lpercentile 29
    • ZincZn3.37 μg/lpercentile 24
    • ManganeseMn9.70 μg/lpercentile 20

    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

    • ChromiumCr130 mg/kgpercentile 91
    • MolybdenumMo0.644 mg/kgpercentile 83
    • NickelNi24.8 mg/kgpercentile 51
    • BismuthBi0.162 mg/kgpercentile 27
    • SeleniumSe0.138 mg/kgpercentile 21
    • ArsenicAs4.26 mg/kgpercentile 15
    • VanadiumV53.4 mg/kgpercentile 15
    • CobaltCo5.88 mg/kgpercentile 14
    • CopperCu14.0 mg/kgpercentile 8
    • TinSn1.54 mg/kgpercentile 6
    • ZincZn56.4 mg/kgpercentile 5
    • CadmiumCd0.0541 mg/kgpercentile 4
    • AntimonySb0.221 mg/kgpercentile 4
    • MercuryHg0.0305 mg/kgpercentile 4
    • LeadPb6.32 mg/kgpercentile 3

    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)
    • CalciumCa3.04 %percentile 66
    • ManganeseMn761 mg/kgpercentile 40
    • SodiumNa0.787 %percentile 33
    • TitaniumTi3,915 mg/kgpercentile 28
    • PotassiumK1.31 %percentile 21
    • IronFe2.03 %percentile 12
    • MagnesiumMg0.583 %percentile 11
    • AluminiumAl4.15 %percentile 7
    • PhosphorusP447 mg/kgpercentile 5
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • ZirconiumZr571 mg/kgpercentile 90
    • BoronB64.7 mg/kgpercentile 62
    • StrontiumSr120 mg/kgpercentile 35
    • CeriumCe54.9 mg/kgpercentile 35
    • YttriumY22.8 mg/kgpercentile 25
    • LithiumLi24.5 mg/kgpercentile 21
    • RubidiumRb71.9 mg/kgpercentile 14
    • BerylliumBe0.611 mg/kgpercentile 11
    • BariumBa301 mg/kgpercentile 5
    • GalliumGa3.90 mg/kgpercentile 2

    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

    48nGy/h in air

    range 45 to 49 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

    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.

    • Potassium (K)K1.27 %percentile 37
    • Equivalent thorium (eTh)eTh7.03 ppm37th percentile
    • Equivalent uranium (eU)eU2.34 ppm24th percentile

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

    • Areal activity of 137CsCS1372,765 Bq/m²percentile 84

    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

    -39nT

    range -43 to -36 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 +14.1 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 75 mW/m².

    Geothermal groundwater bodies beneath the water line

    • Humenné Ridge100%SR 4.4 %

    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.

    • Elevation of geomorphological units (from–to)119–749m a.s.l.
    • Average elevation of the units293m a.s.l.
    • Average slope9.2°
    • Average January temperature-3.6°C
    • Average July temperature18.3°C
    • Annual precipitation700mm

    Geomorphological units

    • Ondava Highlands67%SR 4.4 %
    • Beskydy Foothills33%SR 1.2 %

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

    Geomorphological regions

    • Nízke Beskydy100%SR 7.5 %

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

    Climatic-geographical types

    • mountain climate67%SR 33 %
    • basin climate33%SR 29 %

    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)

    • relatively clean soil100%SR 53 %

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

    Lithogeochemical types

    • Clayey-sandy sediments of the Cretaceous and Paleogene of the Klippen Belt, Tatricum and Hronicum50%SR 2.9 %
    • Cretaceous and Paleogene of the Outer Carpathians50%SR 9.5 %

    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.

    Slovenská Kajňa – none (70 m from the water)Malá Domaša – cannot be estimated (560 m from the water)Kvakovce – permanent (680 m from the water)Slovenská Kajňa – none (950 m from the water)Slovenská Kajňa – none (1.2 km from the water)Beniakovce – Benkovce – cannot be estimated (1.3 km from the water)Žalobín – cannot be estimated (1.3 km from the water)Žalobín – cannot be estimated (1.3 km from the water)Beniakovce – Benkovce – none (1.8 km from the water)Kvakovce – permanent (2.0 km from the water)Giglovce – cannot be estimated (2.2 km from the water)Benkovce – occasional (2.3 km from the water)Vyšný Kazimír – none (2.8 km from the water)Jasenovce – cannot be estimated (2.9 km from the water)a1 (6.1 km from the water)a1 (6.3 km from the water)a1 (7.3 km from the water)a1 (7.6 km from the water)a1 (8.1 km from the water)a1 (9.4 km from the water)b1 (9.5 km from the water)Malá Domaša – gravelly sands – gravel (680 m from the water)Malá Domaša – brick raw materials (1.0 km from the water)Kvakovce – building stone – calcareous sandstone (1.6 km from the water)Žalobín – brick raw materials (1.9 km from the water)Ondavské Matiašovce – gravelly sands – gravel (1.9 km from the water)Kvakovce – brick raw materials (2.0 km from the water)Holčíkovce – brick raw materials (2.9 km from the water)Jasenovce – building stone – sandstone (3.1 km from the water)Benkovce – gravelly sands – gravel (3.2 km from the water)Poloma – building stone – sandstone (4.2 km from the water)SLOVENSKA KAJNA – Landslides (80 m from the water)– Landslides (210 m from the water)VELKA DOMASA – Landslides (360 m from the water)KVAKOVCE – Landslides (360 m from the water)SLOVENSKA KAJNA – Landslides (370 m from the water)SLOVENSKA KAJNA – Landslides (420 m from the water)GIGLOVCE – Landslides (430 m from the water)– Landslides (590 m from the water)MALA DOMASA – Landslides (610 m from the water)CICAVA – Landslides (740 m from the water)SLOVENSKA KAJNA – Landslides (740 m from the water)SLOVENSKA KAJNA – Landslides (850 m from the water)MALA DOMASA – Landslides (880 m from the water)SLOVENSKA KAJNA – Landslides (1.1 km from the water)VYCHODNA – Landslides (1.3 km from the water)– Landslides (1.4 km from the water)GRUN – Landslides (1.4 km from the water)KVAKOVCE – Landslides (1.4 km from the water)– Landslides (1.5 km from the water)HOLCIKOVCE – Landslides (1.6 km from the water)KVAKOVCE – Landslides (1.6 km from the water)GIGLOVCE – Landslides (1.7 km from the water)JASENOVCE – Landslides (1.7 km from the water)KVAKOVCE – Landslides (1.8 km from the water)HOLCIKOVCE – Landslides (1.9 km from the water)ZALOBIN – Landslides (2.0 km from the water)ZALOBIN – Landslides (2.0 km from the water)KVAKOVCE (2.1 km from the water)ZALOBIN – Landslides (2.1 km from the water)GIGLOVCE – Landslides (2.1 km from the water)KVAKOVCE – Landslides (2.1 km from the water)– Landslides (2.3 km from the water)ZALOBIN – Landslides (2.3 km from the water)GIGLOVCE – Landslides (2.3 km from the water)ZALOBIN – Landslides (2.4 km from the water)BENKOVCE – Landslides (2.4 km from the water)KVAKOVCE – Landslides (2.4 km from the water)GIGLOVCE – Landslides (2.5 km from the water)– Landslides (2.5 km from the water)ZALOBIN – Landslides (2.5 km from the water)GIGLOVCE – Landslides (2.6 km from the water)ZALOBIN – Landslides (2.6 km from the water)– Landslides (2.7 km from the water)ZALOBIN – Landslides (2.8 km from the water)HOLCIKOVCE – Landslides (2.8 km from the water)BENKOVCE – Landslides (2.8 km from the water)– Landslides (2.8 km from the water)– Landslides (2.8 km from the water)ZALOBIN – Landslides (2.9 km from the water)RUSKY KAZIMIR – Landslides (2.9 km from the water)– Landslides (2.9 km from the water)RUSKY KAZIMIR – Landslides (2.9 km from the water)ZALOBIN – Landslides (3.0 km from the water)V.D. Domaša – úzkoprofilový vrt s obyčajnou pitnou a ú (220 m from the water)Domaša – monitoring borehole (220 m from the water)Domaša – monitoring borehole (230 m from the water)Slovenská Kajňa – širokoprofilový vrt (Ø vŕtania nad 600 m (230 m from the water)Domaša – monitoring borehole (260 m from the water)Domaša – monitoring borehole (300 m from the water)Domaša – monitoring borehole (320 m from the water)Domaša – monitoring borehole (330 m from the water)Domaša – monitoring borehole (350 m from the water)Domaša – monitoring borehole (380 m from the water)Malá Domaša – širokoprofilový vrt (Ø vŕtania nad 600 m (390 m from the water)Slovenská Kajňa-Benkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (400 m from the water)Domaša – monitoring borehole (410 m from the water)Slovenská Kajňa – úzkoprofilový vrt s obyčajnou pitnou a ú (490 m from the water)Slovenská Kajňa – širokoprofilový vrt (Ø vŕtania nad 600 m (500 m from the water)Slovenská Kajňa-Benkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (550 m from the water)Slovenská Kajňa – úzkoprofilový vrt s obyčajnou pitnou a ú (810 m from the water)Slovenská Kajňa-Benkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (850 m from the water)Veľká Domaša – úzkoprofilový vrt s obyčajnou pitnou a ú (910 m from the water)Domaša – negative borehole (940 m from the water)Domaša – úzkoprofilový vrt s obyčajnou pitnou a ú (960 m from the water)Benkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (970 m from the water)Slovenská Kajňa-Benkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (990 m from the water)Domaša – úzkoprofilový vrt s obyčajnou pitnou a ú (1.0 km from the water)Benkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.1 km from the water)Holčíkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Benkovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.3 km from the water)Beniakovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.3 km from the water)Benkovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.4 km from the water)Benkovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.4 km from the water)Benkovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.5 km from the water)Holčíkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.5 km from the water)Benkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.5 km from the water)Benkovce-Ondavské Matiašovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.6 km from the water)Holčíkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.7 km from the water)Domaša – úzkoprofilový vrt s obyčajnou pitnou a ú (1.7 km from the water)Benkovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Benkovce-Ondavské Matiašovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.8 km from the water)Benkovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.9 km from the water)Benkovce-Ondavské Matiašovce – širokoprofilový vrt (Ø vŕtania nad 600 m (1.9 km 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.

    • CadmiumCdhigh (top 5 %)
      highest 1.00 μg/lmedian 1.00 μg/l4 samples

      Highest value: Ondava, 60 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 5.00 μg/lmedian 5.00 μg/l5 samples

      Highest value: Ondava2000, 220 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 2.50 μg/lmedian 2.50 μg/l5 samples

      Highest value: Ondava2000, 220 m from the water. Comparison: percentile 76 of all samples in Slovakia.

    • ArsenicAstypical value
      highest 1.00 μg/lmedian 1.00 μg/l5 samples

      Highest value: Ondava2000, 220 m from the water. Comparison: percentile 50 of all samples in Slovakia.

    • BariumBabelow half of Slovakia
      highest 37.0 μg/lmedian 36.5 μg/l2 samples

      Highest value: Ondava1999, 60 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • ChromiumCrbelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l3 samples100 % below the limit of quantification

      Highest value: Ondava1999, 60 m from the water. Comparison: percentile 32 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.

    • Barite (BaSO₄)6 samples, at most 315 grains
    • Monazit ((Ce,La,Nd)PO₄)3 samples, at most 5 grains
    • Anatas (TiO₂)2 samples, at most 5 grains
    • Hematite (Fe₂O₃)2 samples, at most 315 grains
    • Ilmenit (FeTiO₃)2 samples, at most 1815 grains
    • Limonite (FeO(OH)·nH₂O)2 samples, at most 5 grains
    • Magnetite (Fe₃O₄)2 samples, at most 4115 grains
    • Pyrite (FeS₂)2 samples, at most 5 grains
    • Rutil (TiO₂)2 samples, at most 55 grains
    • Cinabarit (HgS)2 samples, at most 2 grains

    Rock-forming and accessory minerals

    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)2 samples, at most 1815 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)2 samples, at most 815 grains
    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)2 samples, at most 315 grains
    • Tourmalines (complex borosilicate)2 samples, at most 5 grains
    • Zirconium (ZrSiO₄)2 samples, at most 5 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))1 sample, at most 5 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))1 sample, at most 55 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

    • AluminiumAlextreme (top 1 %)
      highest 0.350 mg/lmedian 0.0150 mg/l18 samples33 % below the limit of quantification

      Highest value: prameň1994, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • SeleniumSehigh (top 5 %)
      highest 4.80 μg/lmedian 0.500 μg/l18 samples56 % below the limit of quantification

      Highest value: studňa1993, 1.7 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 4.00 μg/lmedian 1.00 μg/l18 samples11 % below the limit of quantification

      Highest value: prameň1992, 2.9 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ChromiumCrhigh (top 5 %)
      highest 4.90 μg/lmedian 1.25 μg/l18 samples6 % below the limit of quantification

      Highest value: studňa1993, 280 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 0.500 μg/lmedian 0.250 μg/l18 samples94 % below the limit of quantification

      Highest value: studňa1993, 280 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LithiumLielevated (top 10 %)
      highest 50.0 μg/lmedian 14.0 μg/l18 samples

      Highest value: prameň1994, 2.3 km from the water. Comparison: percentile 94 of all samples in Slovakia.

    • ZincZnelevated (top 10 %)
      highest 539 μg/lmedian 44.5 μg/l18 samples

      Highest value: studňa1993, 2.5 km from the water. Comparison: percentile 91 of all samples in Slovakia.

    • CopperCuelevated (top 10 %)
      highest 3.80 μg/lmedian 1.20 μg/l18 samples

      Highest value: studňa1993, 270 m from the water. Comparison: percentile 90 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.300 μg/lmedian 0.100 μg/l18 samples89 % below the limit of quantification

      Highest value: studňa1993, 270 m from the water. Comparison: percentile 87 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 1.30 μg/lmedian 0.500 μg/l18 samples89 % below the limit of quantification

      Highest value: studňa1993, 270 m from the water. Comparison: percentile 83 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l5 samples100 % below the limit of quantification

      Highest value: studňa1993, 1.4 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l18 samples100 % below the limit of quantification

      Highest value: studňa1993, 1.4 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    developed spring445,8 Bq/l23.8 Bq/l
    source10,760 Bq/l0.760 Bq/l
    well531,4 Bq/l12.7 Bq/l
    other10,670 Bq/l0.670 Bq/l
    water source for individual supply116,8 Bq/l16.8 Bq/l

    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.

    104 boreholes in the 3 km zone, of which 74 hydrogeological and 30 other; with an archive report number 104.

    Borehole depths

    • up to 10 m43×
    • 10–30 m41×
    • 30–100 m18×
    • 100–300 m1×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    VS-2engineering-geological20.0 m285750 m
    VS-3engineering-geological20.0 m285760 m
    VR-1engineering-geological15.0 m2857110 m
    VS-1engineering-geological20.0 m2857120 m
    VR-3engineering-geological10.0 m2857140 m
    VR-2engineering-geological15.0 m2857210 m
    V.D. Domašanarrow-diameter borehole with ordinary drinking and process water19.0 m21309 116Ab29.pdf220 m
    Domašamonitoring borehole25.0 m39008 104Cd55.pdf220 m
    Domašamonitoring borehole30.0 m39008 104Cd47.pdf230 m
    Slovenská Kajňawide-diameter borehole–61514 116Ab58.pdf230 m
    Domašamonitoring borehole30.0 m39008 104Cd48.pdf260 m
    Domašamonitoring borehole35.0 m39008 104Cd49.pdf300 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< 566.1 km
    category b1mineral water15-22< 519.5 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
    Slovenská Kajňa50 m²––70 m
    Malá Domaša–––560 m
    Kvakovce100 m²––680 m
    Slovenská Kajňa130 m²––950 m
    Slovenská Kajňa50 m²––1.2 km
    Beniakovce – Benkovce500 m²––1.3 km
    Žalobín30 m²––1.3 km
    Žalobín40 m²––1.3 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

    • Landslides52×

    Degree of activity

    • Potenciálny30×
    • Stabilizovaný16×
    • Aktívny6×

    Current state

    • Processed only in the scope of registration on a scale of 1:25,00032×
    • SD taken from archival materials, ktorá bola konfrontova14×
    • P1×
    • 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. Vranov nad Topľou1 fishing district · 4.6 km10VVN Domaša10

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