Watercourse

Jovsanský potok

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
4.9km
region
Prešov Region
Aerial image of watercourse Jovsanský 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 Jovsanský 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

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

06:00–08:00

Jovsanský potok, window score 37.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 08:04.

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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    Water state on the watercourse

    Measurement of water level, temperature and flow, weather by the watercourse and status from satellites

    Water levels on the watercourse

    StationStatusChangeTemperature
    Jovsa3 cm–
    Source: SHMÚUpdated 9 Nov 2026 07:58

    Elevation profile of the watercourse

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

    Bystrina A mountain stream with a steep gradient, cascades and a rocky bottom. The water is clear and cold; fishing requires a careful approach.

    2003004005006007008000 km1 km2 km3 km4 km
    Elevation profile of the watercourse: from 694 to 306 m a.s.l. over 4.9 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
    694 m a.s.l.
    Lowest point
    263 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.
    431 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.
    88 ‰
    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.
    1.10

    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 Jovsanský potok from 2019
    2019imaged 4 Jul 2019
    Aerial image of watercourse Jovsanský potok from 2022
    2022imaged 10 Oct 2022
    Aerial image of watercourse Jovsanský potok from 2025
    2025imaged 7 Aug 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 Jovsanský 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

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

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

    Geology and geochemistry of the Jovsanský 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 (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

    Young sediments67% of the water line

    33% river alluvium

    Young unconsolidated sediments; fine material easily washes into the stream during rain. Geological Map of Slovakia 1:50,000.

    510

    Water according to the atlas

    pH 7.2modelled estimate

    water type Ca–HCO₃–SO₄

    Mineralisation 77.8 mg/l, soft water (2.1 °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: Cadmium 0.882 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.

    0 °C80

    Heat underfoot

    45°C at 1,000 m depth

    Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    41nGy/h dose rate

    percentile 8 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

    5 ore minerals in the sediment

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

    Trace elements in the stream water

    0 from 9indicators in the top 5 %

    highest: Selenium 0.570 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 92 (Jovsiansky, potok).

    Boreholes and groundwater analyses

    27boreholes within 3 km

    316 water analyses nearby

    Of these, 26 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    39°C at the wellhead

    1 geothermal borehole within 10 km

    Warmest: Kaluža – GTH-1, 9.2 km from the water.

    Environmental burdens and landfills

    1sites within 3 km

    1 landfill

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

    Deposits and ore occurrences

    6records within 5 km

    1 deposit, 5 ore occurrences

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

    Landslides and slope deformations

    19areas 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.

    • Young sediments67%SR 8.6 %
    • River alluvium33%SR 72 %

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

    Young sediments: Young unconsolidated sediments; fine material easily washes into the stream during rain.

    Geological age of the rocks

    • Quaternary100%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryPleistocene – Holocenedeluvial sediments: sandy-stone-like and boulder-like blocks2×
    QuaternaryHolocenefluvial sediments: resedimented alluvial sandy gravels of the near-channel zone1×

    Quaternary cover

    • proluvial sediments of terraced alluvial cones50%SR 2.5 %
    • deluvial sediments50%SR 16 %

    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

    Regional geological division

    • neovolcanic rocks100%SR 10 %

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

    Regional geological division (subunits)

    • neovolcanic rocks of Vihorlatské vrchy100%SR 0.0 %

    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)

    • Acid volcanic rocks67%SR 3.2 %
    • Basic volcanic rocks33%SR 6.6 %

    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 vody67%SR 3.2 %
    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody33%SR 6.4 %

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

    Main hydrogeological region

    • neovolcanic rocks of Vihorlatské vrchy100%SR 0.0 %

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

    Genetic type of groundwater

    • silicate67%SR 2.9 %
    • silicate-carbonate-potamogenic33%SR 1.4 %

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

    Chemical type of groundwater

    • Ca-Mg-HCO367%SR 26 %
    • Ca-(+/-Mg)-HCO333%SR 1.1 %

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

    Groundwater quality class

    • B100%SR 18 %

    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 7.16typical 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

    2.1°dH, soft

    Sum of calcium and magnesium (0.38 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    77.8mg/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–SO₄

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

    Major ions

    • PotassiumK1.17 mg/lpercentile 14
    • SodiumNa2.84 mg/lpercentile 11
    • FluoridesF0.0522 mg/lpercentile 8
    • BicarbonatesHCO334.5 mg/lpercentile 4
    • CalciumCa11.3 mg/lpercentile 4
    • SulphatesSO411.5 mg/lpercentile 4
    • MagnesiumMg2.47 mg/lpercentile 3
    • ChloridesCl0.918 mg/lpercentile 2

    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

    • NitratesNO38.15 mg/lpercentile 64
    • Chemical oxygen demandChSK2.27 mg/lpercentile 27
    • AmmoniumNH40.0432 mg/lpercentile 22
    • PhosphatesPO40.0246 mg/lpercentile 13

    Metals

    • ZincZn9.25 μg/lpercentile 62
    • AluminiumAl84.2 μg/lpercentile 56
    • IronFe0.0775 mg/lpercentile 38
    • ManganeseMn7.94 μg/lpercentile 16

    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

    • CadmiumCd0.882 mg/kgpercentile 92
    • CobaltCo13.2 mg/kgpercentile 91
    • VanadiumV101 mg/kgpercentile 89
    • LeadPb19.9 mg/kgpercentile 70
    • AntimonySb0.876 mg/kgpercentile 66
    • ChromiumCr74.1 mg/kgpercentile 53
    • TinSn2.50 mg/kgpercentile 43
    • SeleniumSe0.208 mg/kgpercentile 40
    • BismuthBi0.187 mg/kgpercentile 37
    • ZincZn80.5 mg/kgpercentile 32
    • MercuryHg0.0685 mg/kgpercentile 28
    • MolybdenumMo0.251 mg/kgpercentile 24
    • NickelNi13.5 mg/kgpercentile 9
    • CopperCu14.1 mg/kgpercentile 8
    • ArsenicAs3.58 mg/kgpercentile 8

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

    Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
    • TitaniumTi7,129 mg/kgpercentile 93
    • IronFe4.13 %percentile 92
    • MagnesiumMg1.51 %percentile 81
    • AluminiumAl6.65 %percentile 79
    • ManganeseMn1,119 mg/kgpercentile 74
    • SodiumNa0.775 %percentile 31
    • CalciumCa1.44 %percentile 30
    • PotassiumK1.25 %percentile 14
    • PhosphorusP417 mg/kgpercentile 4
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • GalliumGa21.2 mg/kgpercentile 94
    • ZirconiumZr414 mg/kgpercentile 54
    • BerylliumBe1.47 mg/kgpercentile 53
    • YttriumY28.2 mg/kgpercentile 53
    • StrontiumSr113 mg/kgpercentile 28
    • BariumBa362 mg/kgpercentile 21
    • LithiumLi24.4 mg/kgpercentile 20
    • RubidiumRb74.5 mg/kgpercentile 18
    • CeriumCe44.4 mg/kgpercentile 9
    • BoronB36.6 mg/kgpercentile 8

    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

    41nGy/h in air

    range 40 to 43 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)K1.15 %percentile 16
    • Equivalent thorium (eTh)eTh6.27 ppm14th percentile
    • Equivalent uranium (eU)eU1.86 ppm5th 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 137CsCS137966 Bq/m²percentile 16

    Radon risk by isopleths

    • medium67%SR 64 %
    • low33%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

    +17nT

    range -136 to 210 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

    -3mGal

    residual +10.5 mGal

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

    Geothermal potential

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

    • Rock temperature at 1,000 m depth45°C

    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)239–1 072m a.s.l.
    • Average elevation of the units661m a.s.l.
    • Average slope14.3°
    • Average January temperature-5.0°C
    • Average July temperature16.5°C
    • Annual precipitation850mm

    Geomorphological units

    • Vihorlat Mountains100%SR 0.0 %

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

    Geomorphological regions

    • Vihorlat–Gutin area100%SR 0.5 %

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

    Climatic-geographical types

    • mountain climate100%SR 33 %

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

    Susceptibility of soils to acidification

    • soils moderately susceptible to acidification100%SR 25 %

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

    Soil contamination (map 1:500,000)

    • relatively clean soil67%SR 53 %
    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A33%SR 45 %

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

    Lithogeochemical types

    • Neogene volcanics100%SR 11 %

    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.

    Porubský potok – Iron ores (1.9 km from the water)Poruba pod Vihorlatom – none (2.6 km from the water)Kaluža – GTH-1 – non-spa (9.2 km from the water)b1 (3.5 km from the water)Lom Jovsa – building stone (3.4 km from the water)Poruba pod Vihorlatom – Fe ores – limonite (2.1 km from the water)Kamienka – building stone – andesite breccias (4.2 km from the water)Vyšné Remety – building stone – pyroxene andesite (4.3 km from the water)Vihorlat – Veľká Postavka, Ďurova mláka, Hypkani – peat (4.9 km from the water)Poruba pod Vihorlatom – mineralogy (3.2 km from the water)VIHORLAT – Landslides (90 m from the water)VIHORLAT – Landslides (160 m from the water)JOVSA – Landslides (210 m from the water)JOVSA – Landslides (240 m from the water)– Block fields (270 m from the water)– Landslides (290 m from the water)VIHORLAT – Landslides (310 m from the water)– Rockfalls (440 m from the water)JOVSA – Landslides (570 m from the water)– Landslides (950 m from the water)– Landslides (1.6 km from the water)JOVSA – Landslides (1.8 km from the water)JOVSA – Landslides (1.9 km from the water)JOVKA – Landslides (2.0 km from the water)– Landslides (2.2 km from the water)– Landslides (2.3 km from the water)JOVSA – Landslides (2.3 km from the water)– Block fields (2.4 km from the water)– Landslides (2.8 km from the water)Kusín-Jovsa – úzkoprofilový vrt s obyčajnou pitnou a ú (1.2 km from the water)Jovsa – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Poruba pod Vihorlatom – úzkoprofilový vrt s obyčajnou pitnou a ú (2.3 km from the water)Jovsa – structural borehole with thermal water, minerálnou v (2.3 km from the water)Jovsa – širokoprofilový vrt (Ø vŕtania nad 600 m (2.4 km from the water)prameň – Groundwater springs (30 m from the water)prameň – Groundwater springs (40 m from the water)prameň – Groundwater springs (60 m from the water)prameň – Groundwater springs (70 m from the water)prameň – Groundwater springs (80 m from the water)prameň – Groundwater springs (90 m from the water)prameň – Groundwater springs (90 m from the water)prameň – Groundwater springs (110 m from the water)prameň – Groundwater springs (140 m from the water)prameň – Groundwater springs (150 m from the water)prameň – Groundwater springs (170 m from the water)prameň – Groundwater springs (170 m from the water)prameň – Groundwater springs (210 m from the water)prameň – Groundwater springs (210 m from the water)prameň – Groundwater springs (240 m from the water)prameň – Groundwater springs (260 m from the water)prameň – Groundwater springs (260 m from the water)prameň – Groundwater springs (270 m from the water)prameň – Groundwater springs (270 m from the water)prameň – Groundwater springs (300 m from the water)prameň – Groundwater springs (300 m from the water)prameň – Groundwater springs (310 m from the water)prameň – Groundwater springs (320 m from the water)prameň – Groundwater springs (360 m from the water)prameň – Groundwater springs (380 m from the water)prameň – Groundwater springs (480 m from the water)prameň – Groundwater springs (490 m from the water)prameň – Groundwater springs (510 m from the water)prameň – Groundwater springs (520 m from the water)prameň – Groundwater springs (540 m from the water)prameň – Groundwater springs (550 m from the water)prameň – Groundwater springs (570 m from the water)prameň – Groundwater springs (570 m from the water)prameň – Groundwater springs (580 m from the water)prameň – Groundwater springs (600 m from the water)prameň – Groundwater springs (610 m from the water)prameň – Groundwater springs (670 m from the water)prameň – Groundwater springs (670 m from the water)prameň – Groundwater springs (690 m from the water)prameň – Groundwater springs (690 m from the water)Jovsa – source (30 m from the water)400m SZ od K325 – source (70 m from the water)800m SZ od K325 – source (70 m from the water)1150m ZSZ od K894 – source (90 m from the water)1200m SV od K708 – source (100 m from the water)dolina Jovsianskeho potoka – Rakytovec – source (110 m from the water)Jovsa – source (210 m from the water)dolinka ľavostranného prítoku Jovsianského potok – source (310 m from the water)800m SV od K708 – source (480 m from the water)Stredný vrch – source (1.0 km from the water)Jovsa – source (1.0 km from the water)J okraj – borehole (1.2 km from the water)600 m S od k.Vihorlat – source (1.2 km from the water)dolina potoka Myslina – source (1.2 km from the water)550m SSZ od K996 M.Trestia – source (1.6 km from the water)J okraj – borehole (1.8 km from the water)prameňná oblasť Klinového potoka – source (1.8 km from the water)900m SZ od K738 Malý Peňažník – source (1.9 km from the water)Jovsa – source (2.1 km from the water)800m JZ od K595 – source (2.2 km from the water)1600m Z od K345 – source (2.2 km from the water)750m SV od K996 M.Trestia – source (2.2 km from the water)1000m SZ od K590 – source (2.2 km from the water)J okraj – borehole (2.3 km from the water)650m ZSZ od K590 – source (2.3 km from the water)300 m SV od okraja obce – borehole (2.4 km from the water)Petráňa – source (2.5 km from the water)500m SV od K666 – source (2.5 km from the water)1500m Z od K238 – well (2.5 km from the water)Jovsa – source (2.6 km from the water)2000m S od K1076 Vihorlat – source (2.7 km from the water)250m JZ od K590 – source (2.8 km from the water)č.d. 54,1000m SV od K172 – well (2.8 km from the water)1100m J od K691 – source (2.9 km from the water)č.d. 83, 1400m SV od K172 – well (2.9 km from the water)350m V od K584 Brestov – source (2.9 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.

    • SeleniumSeelevated (top 10 %)
      highest 0.570 μg/lmedian 0.535 μg/l2 samples50 % below the limit of quantification

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 92 of all samples in Slovakia.

    • CadmiumCdelevated (top 10 %)
      highest 0.300 μg/lmedian 0.225 μg/l2 samples50 % below the limit of quantification

      Highest value: Jovsiansky, potok, 110 m from the water. Comparison: percentile 90 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.940 μg/lmedian 0.720 μg/l2 samples50 % below the limit of quantification

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 81 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 2.30 μg/lmedian 1.85 μg/l2 samples

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 77 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l2 samples100 % below the limit of quantification

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • StrontiumSrbelow half of Slovakia
      highest 125 μg/lmedian 112 μg/l2 samples

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 36 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l2 samples100 % below the limit of quantification

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l2 samples100 % below the limit of quantification

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 22 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l2 samples100 % below the limit of quantification

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 22 of all samples in Slovakia.

    Major ions, mineralisation and pH

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

    • Silicon dioxideSiO2slightly elevated
      highest 30.8 mg/lmedian 30.4 mg/l2 samples

      Highest value: Jovsiansky, potok1998, 110 m from the water. Comparison: percentile 89 of all samples in Slovakia.

    Gold and ore minerals in river sediments

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

    • Ilmenit (FeTiO₃)3 samples, at most 4115 grains
    • Limonite (FeO(OH)·nH₂O)3 samples, at most 55 grains
    • Magnetite (Fe₃O₄)3 samples, at most 5 grains
    • Rutil (TiO₂)2 samples, at most 5 grains
    • Cinabarit (HgS)1 sample, at most 1 grains

    Rock-forming and accessory minerals

    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)3 samples, at most 4115 grains
    • Zirconium (ZrSiO₄)3 samples, at most 5 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)2 samples, at most 15 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)1 sample, at most 5 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))1 sample, 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.

    Chemical water types nearby

    • Ca-Mg-HCO313×
    • Ca-Mg-HCO3-SO45×
    • Ca-HCO3-SO45×
    • Ca-HCO34×
    • Ca-SO4-HCO33×
    • Ca-Mg-HCO3-NO32×
    • Ca-Na-HCO3-SO41×
    • Ca-HCO3-NO31×

    Water quality class according to the hydrogeochemical map

    • class B31×
    • class D3×
    • class H2×

    Metals in groundwater

    • ZincZnextreme (top 1 %)
      highest 7,500 μg/lmedian 38.0 μg/l22 samples

      Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • LeadPbextreme (top 1 %)
      highest 9.00 μg/lmedian 1.00 μg/l22 samples18 % below the limit of quantification

      Highest value: prameň1993, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AluminiumAlhigh (top 5 %)
      highest 0.160 mg/lmedian 0.0100 mg/l22 samples14 % below the limit of quantification

      Highest value: prameň1993, 90 m from the water. Comparison: percentile 97 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 1.10 μg/lmedian 0.250 μg/l22 samples59 % below the limit of quantification

      Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • CopperCuelevated (top 10 %)
      highest 5.40 μg/lmedian 1.10 μg/l22 samples

      Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 94 of all samples in Slovakia.

    • ChromiumCrelevated (top 10 %)
      highest 2.10 μg/lmedian 0.250 μg/l22 samples59 % below the limit of quantification

      Highest value: prameň1993, 2.2 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 2.10 μg/lmedian 0.500 μg/l22 samples91 % below the limit of quantification

      Highest value: prameň1993, 2.4 km from the water. Comparison: percentile 89 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l10 samples100 % below the limit of quantification

      Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l22 samples100 % below the limit of quantification

      Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    • AntimonySbbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l22 samples100 % below the limit of quantification

      Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 40 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l22 samples100 % below the limit of quantification

      Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 39 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 4.00 μg/lmedian 1.00 μg/l22 samples77 % below the limit of quantification

      Highest value: prameň1993, 2.4 km from the water. Comparison: percentile 35 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    free-flowing borehole with thermal and mineral water114,1 Bq/l14.1 Bq/l
    source761,9 Bq/l27.5 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
    Lom Jovsabuilding stoneMined deposit – VLaM SR, štátny podnik – Odštepný závod Kamenica nad Cirochou3.4 km

    Ore occurrences in the metallogenic map

    OccurrenceOre typeMetalsTypeFrom the water
    Porubský potokIron oresFemineralogical occurrence1.9 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.

    27 boreholes in the 3 km zone, of which 5 hydrogeological and 22 other; with an archive report number 26.

    Borehole depths

    • up to 10 m0×
    • 10–30 m7×
    • 30–100 m15×
    • 100–300 m5×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Kusín-Jovsanarrow-diameter borehole with ordinary drinking and process water136.0 m70715 117Ac1.pdf1.2 km
    Jovsanarrow-diameter borehole with ordinary drinking and process water151.0 m70715 117Ca52.pdf1.8 km
    PV-22deposit27.1 m146792.0 km
    PV-16deposit20.3 m89922.1 km
    Poruba pod Vihorlatomnarrow-diameter borehole with ordinary drinking and process water100.0 m70339 117Cb45.pdf2.3 km
    PV-15deposit45.0 m89922.3 km
    PV-28deposit30.7 m146792.3 km
    Jovsastructural borehole with thermal water, mineral water250.0 m41342 117Ca38.pdf2.3 km
    J-1-67deposit250.3 m–2.3 km
    PV-13deposit33.0 m89922.3 km
    Jovsawide-diameter borehole75.0 m62427 117Ca50.pdf2.4 km
    VH-P-1deposit30.4 m88392.4 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
    Kaluža – GTH-139 °C––Na-Cl-SO4-HCO3/ Na-Clin use9.2 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category b1mineral water15-22< 513.5 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
    Poruba pod Vihorlatom1 500 m²1992–2.6 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

    • Landslides16×
    • Block fields2×
    • Rockfalls1×

    Degree of activity

    • Potenciálny16×
    • Stabilizovaný3×

    Current state

    • SD taken from archival materials, ktorá bola konfrontova12×
    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S7×

    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. VO Valaškovce1 fishing district · 4.9 km27Jovsanský potok27

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