Watercourse

Zbojský potok

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
9.6km
region
Prešov Region
Aerial image of watercourse Zbojský 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 Zbojský 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

Zbojský potok č. 1, window score 39.

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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    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.

    2004006008001,0000 km2 km4 km6 km8 km
    Elevation profile of the watercourse: from 841 to 389 m a.s.l. over 9.6 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
    841 m a.s.l.
    Lowest point
    360 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.
    480 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.
    50 ‰
    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.
    1.22

    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 Zbojský potok from 2019
    2019imaged 4 Jul 2019
    Aerial image of watercourse Zbojský potok from 2022
    2022imaged 27 Aug 2022
    Aerial image of watercourse Zbojský potok from 2025
    2025imaged 13 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 Zbojský potok watercourse

    Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby

    Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025

    1 of 1 fishing districts on the watercourse with SHMÚ data: the nearest site has an unmet standard in at least one indicator.

    • 1 to 2 indicators1

    Most polluted fishing districtsall with an unmet standard

    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 Zbojský 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 (10 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

    Sandstones and conglomerates75% of the water line

    25% river alluvium

    Moderately mineralised water, depending on the share of carbonates. Geological Map of Slovakia 1:50,000.

    510

    Water according to the atlas

    pH 8.1modelled estimate

    water type Ca–HCO₃

    Mineralisation 233 mg/l, soft water (7.3 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    0 from 15elements in the top 10 %

    highest: Vanadium 99.4 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 88. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km45 °C85 °C

    Heat underfoot

    45°C at 1,000 m depth

    heat flow 75 mW/m²

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

    20200

    Natural gamma radiation

    53nGy/h dose rate

    percentile 64 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

    1sample with gold

    12 ore minerals in the sediment

    Up to 1 grain in one sample (70 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.

    Trace elements in the stream water

    0 from 8indicators in the top 5 %

    highest: Chromium 2.22 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 76 (Zbojský potok, prítok).

    Boreholes and groundwater analyses

    5boreholes within 3 km

    369 water analyses nearby

    Of these, 4 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

    2sites within 3 km

    2 landfills

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

    Deposits and ore occurrences

    0records within 5 km

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

    Landslides and slope deformations

    58areas 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.

    • Sandstones and conglomerates75%SR 1.8 %
    • River alluvium25%SR 72 %

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

    Sandstones and conglomerates: Moderately mineralised water, depending on the share of carbonates.

    Geological age of the rocks

    • flysch75%
    • Quaternary25%

    Most common rock units

    SystemAgeUnitPoints
    flyschMiddle Cretaceous – PaleoceneLupkov Formation3×
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains1×

    Quaternary cover

    • fluvial sediments of floodplains50%SR 68 %
    • deluvial sediments50%SR 16 %

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

    • Typical thickness of the Quaternary cover3.5m
    • 2 – 5100%SR 48 %

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

    Tectonic units

    • DUKLIANSKY PRÍKROV100%SR 3.8 %

    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

    • large uplift100%SR 26 %

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

    Regional geological division

    • flysch belt100%SR 9.6 %

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

    Regional geological division (subunits)

    • Dukla–Bukovec flysch100%SR 1.8 %

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

    Engineering-geological districts

    • region of sandstone rocks75%SR 4.1 %
    • region of mountain-stream deposits25%SR 21 %

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

    Engineering-geological formations

    • flysch formation75%SR 13 %
    • formation of Quaternary sediments25%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 4 of 4 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)100%SR 15 %

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

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

    • intergranular50%SR 86 %
    • fissure50%SR 12 %

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

    Hydrogeological function

    • aquifer50%SR 95 %
    • regional aquiclude50%SR 2.3 %

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

    Main hydrogeological region

    • Paleogene Basin Uhu100%SR 0.0 %

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

    Genetic type of groundwater

    • natural silicate-carbonatogenic100%SR 0.0 %

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

    Chemical type of groundwater

    • predominantly Ca-HCO3, sporadically Ca-Na-HCO3 or Ca-K-HCO3-NO3100%SR 0.0 %

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

    Groundwater quality class

    • A50%SR 36 %
    • B50%SR 18 %

    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 8.09typical range

    Most rivers and streams in Slovakia have a pH of 6.5 to 8.5. More acidic water is found in streams on acidic rocks (granites, quartzites), more alkaline water near limestones.

    Water hardness

    7.3°dH, soft

    Sum of calcium and magnesium (1.31 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    233mg/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

    • FluoridesF0.103 mg/lpercentile 44
    • BicarbonatesHCO3150 mg/lpercentile 32
    • CalciumCa44.9 mg/lpercentile 31
    • SodiumNa4.24 mg/lpercentile 22
    • SulphatesSO418.9 mg/lpercentile 13
    • PotassiumK1.10 mg/lpercentile 12
    • MagnesiumMg4.60 mg/lpercentile 9
    • ChloridesCl1.17 mg/lpercentile 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)

    Nutrients and organic pollution

    • AmmoniumNH40.0400 mg/lpercentile 20
    • NitratesNO32.80 mg/lpercentile 15
    • PhosphatesPO40.0151 mg/lpercentile 0
    • Chemical oxygen demandChSK0.319 mg/lpercentile 0

    Metals

    • AluminiumAl43.2 μg/lpercentile 39
    • IronFe0.0678 mg/lpercentile 33
    • ManganeseMn8.08 μg/lpercentile 16
    • ZincZn2.05 μg/lpercentile 13

    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

    • VanadiumV99.4 mg/kgpercentile 88
    • NickelNi30.8 mg/kgpercentile 73
    • TinSn3.37 mg/kgpercentile 72
    • SeleniumSe0.343 mg/kgpercentile 70
    • ArsenicAs8.06 mg/kgpercentile 65
    • ChromiumCr77.2 mg/kgpercentile 58
    • CopperCu24.7 mg/kgpercentile 55
    • CobaltCo8.27 mg/kgpercentile 47
    • AntimonySb0.585 mg/kgpercentile 45
    • ZincZn83.1 mg/kgpercentile 34
    • MolybdenumMo0.234 mg/kgpercentile 21
    • LeadPb9.85 mg/kgpercentile 12
    • BismuthBi0.0935 mg/kgpercentile 5
    • MercuryHg0.0313 mg/kgpercentile 4
    • CadmiumCd0.0527 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)
    • PotassiumK2.12 %percentile 95
    • AluminiumAl7.41 %percentile 92
    • IronFe3.59 %percentile 84
    • TitaniumTi5,039 mg/kgpercentile 70
    • SodiumNa0.888 %percentile 55
    • MagnesiumMg0.727 %percentile 29
    • CalciumCa1.12 %percentile 18
    • ManganeseMn552 mg/kgpercentile 12
    • PhosphorusP475 mg/kgpercentile 6
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • LithiumLi58.4 mg/kgpercentile 96
    • BerylliumBe2.83 mg/kgpercentile 95
    • RubidiumRb125 mg/kgpercentile 95
    • BoronB99.0 mg/kgpercentile 95
    • GalliumGa18.4 mg/kgpercentile 84
    • YttriumY32.9 mg/kgpercentile 75
    • CeriumCe61.3 mg/kgpercentile 58
    • StrontiumSr132 mg/kgpercentile 46
    • ZirconiumZr383 mg/kgpercentile 43
    • BariumBa372 mg/kgpercentile 25

    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

    53nGy/h in air

    range 50 to 53 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)K1.40 %percentile 71
    • Equivalent thorium (eTh)eTh7.94 ppm67th percentile
    • Equivalent uranium (eU)eU2.51 ppm41th 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 137CsCS1371,883 Bq/m²percentile 66

    Radon risk by isopleths

    • low67%SR 36 %
    • medium33%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

    -47nT

    range -82 to -20 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

    -29mGal

    residual −6.1 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 °C85 °C

    Rock temperature with depth

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

    increase of 40 °C per km

    The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 75 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)261–1 205m a.s.l.
    • Average elevation of the units595m a.s.l.
    • Average slope14.5°
    • Average January temperature-5.4°C
    • Average July temperature15.6°C
    • Annual precipitation900mm

    Geomorphological units

    • Bukovské Mountains100%SR 0.0 %

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

    Geomorphological regions

    • Poloniny100%SR 0.8 %

    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 soil100%SR 53 %

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

    Lithogeochemical types

    • Cretaceous and Paleogene of the Outer Carpathians100%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.

    Nová Sedlica – none (80 m from the water)Zboj – none (2.2 km from the water)NOVA SEDLICA – Landslides (90 m from the water)NOVA SEDLICA – Landslides (120 m from the water)– Landslides (150 m from the water)– Landslides (200 m from the water)– Block fissures (260 m from the water)– Landslides (310 m from the water)– Landslides (340 m from the water)– Landslides (380 m from the water)– Landslides (430 m from the water)– Landslides (430 m from the water)– Landslides (440 m from the water)– Landslides (520 m from the water)– Landslides (650 m from the water)– Landslides (680 m from the water)– Landslides (740 m from the water)– Landslides (760 m from the water)– Landslides (850 m from the water)– Landslides (940 m from the water)ZBOJ – Landslides (960 m from the water)– Landslides (960 m from the water)– Landslides (990 m from the water)ZBOJ – Landslides (1.0 km from the water)– Landslides (1.1 km from the water)– Landslides (1.3 km from the water)– Landslides (1.3 km from the water)– Landslides (1.3 km from the water)– Landslides (1.3 km from the water)– Landslides (1.3 km from the water)– Landslides (1.4 km from the water)– Landslides (1.4 km from the water)– Landslides (1.5 km from the water)– Landslides (1.5 km from the water)– Landslides (1.5 km from the water)– Landslides (1.5 km from the water)– Landslides (1.6 km from the water)– Landslides (1.6 km from the water)– Landslides (1.7 km from the water)– Landslides (1.7 km from the water)– Landslides (1.7 km from the water)– Landslides (1.8 km from the water)ZBOJ – Landslides (1.8 km from the water)– Landslides (1.8 km from the water)– Landslides (2.1 km from the water)– Landslides (2.1 km from the water)– Landslides (2.1 km from the water)– Landslides (2.4 km from the water)– Landslides (2.5 km from the water)– Landslides (2.5 km from the water)– Landslides (2.5 km from the water)– Landslides (2.6 km from the water)– Block fissures (2.6 km from the water)– Landslides (2.7 km from the water)– Landslides (2.7 km from the water)– Block fields (2.7 km from the water)– Landslides (2.7 km from the water)– Landslides (2.9 km from the water)– Landslides (2.9 km from the water)– Landslides (3.0 km from the water)Zboj – úzkoprofilový vrt s obyčajnou pitnou a ú (1.6 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (20 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (60 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (60 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (80 m from the water)prameň – Groundwater springs (160 m from the water)prameň – Groundwater springs (170 m from the water)prameň – Groundwater springs (280 m from the water)prameň – Groundwater springs (300 m from the water)prameň – Groundwater springs (330 m from the water)prameň – Groundwater springs (350 m from the water)prameň – Groundwater springs (380 m from the water)prameň – Groundwater springs (540 m from the water)prameň – Groundwater springs (640 m from the water)skupina prameňov – Groundwater springs (870 m from the water)prameň – Groundwater springs (1.0 km from the water)prameň – Groundwater springs (1.1 km from the water)prameň – Groundwater springs (1.2 km from the water)prameň – Groundwater springs (1.5 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.6 km from the water)prameň – Groundwater springs (1.6 km from the water)pramenná línia – Groundwater springs (1.6 km from the water)zrážkomerná stanica – Artificial hydrogeologically significant objects (1.8 km from the water)prameň – Groundwater springs (1.8 km from the water)skupina prameňov – Groundwater springs (2.0 km from the water)prameň – Groundwater springs (2.1 km from the water)prameň – Groundwater springs (2.1 km from the water)pramenná línia – Groundwater springs (2.1 km from the water)prameň – Groundwater springs (2.1 km from the water)prameň – Groundwater springs (2.2 km from the water)pramenná línia – Groundwater springs (2.3 km from the water)prameň – Groundwater springs (2.3 km from the water)prameň – Groundwater springs (2.3 km from the water)prameň minerálnej vody – Groundwater springs (2.5 km from the water)prameň minerálnej vody – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (2.7 km from the water)skupina prameňov – Groundwater springs (2.7 km from the water)prameň – Groundwater springs (2.7 km from the water)prameň – Groundwater springs (2.8 km from the water)prameň – Groundwater springs (2.8 km from the water)1500 m JJZ od k. Čelo (1159) – source (70 m from the water)N.Sedlica dol.Zbojsk.p.1500m J od K857 – source (130 m from the water)N.Sedlica dol.Zbojsk.p.1200m JJZ odK1169 – source (140 m from the water)N.Sedlica v obci,1300m JV od K596 – source (150 m from the water)N.Sedlica dol.Zbojsk.p.500m JZ od K609 – source (180 m from the water)N.Sedlica dol.Zbojsk.p.700m JZ od K1159 – source (190 m from the water)N.Sedlica dol.Zbojsk.p.800m SV od K596 – source (240 m from the water)N.Sedlica dol.Zbojsk.p.600m SV od K649 – source (310 m from the water)N.Sedlica,400m J od K544 – source (460 m from the water)N.Sedlica dol.Zbojsk.p.1500m Z od K1159 – source (570 m from the water)N.Sedlica dol.Zbojsk.p.600m S od K609 – source (890 m from the water)Pod Príkrym; 1130 m JJZ od k. Príkry (952) – source (1.0 km from the water)N.Sedlica,1200m ZJZ od K656 – source (1.1 km from the water)N.Sedlica – Zboj,200m VSV od K380 – source (1.1 km from the water)Fľašová; 1100 m JV od k. Ďurkovec – source (1.2 km from the water)3,5 km SSZ od obce Zboj, 730 m JZ od k. Beskyd ( – source (1.4 km from the water)N.Sedlica dol.Zbojsk.p.500m VSV od K857 – source (1.9 km from the water)Zboj dol.Bystriansk.p.600m JZ od K506 – source (2.0 km from the water)N.Sedlica dol.Zbojsk.p.1000m J od K1188 – source (2.0 km from the water)N.Sedlica,900m JJZ od K872 – source (2.1 km from the water)Zboj dol.pot.Dlha,1200m S od K445 – source (2.2 km from the water)Runina,1000m JZ od K971 – source (2.4 km from the water)N.Sedlica,600m JZ od K654 – source (2.4 km from the water)Romanov Zlab,1200m SZ od K971 – source (2.4 km from the water)1300 m SV od obce, 1150 m ZSZ od k. Minčol (974) – source (2.4 km from the water)Grenicova skala,600m JZ od K1128 – source (2.4 km from the water)Runina,1200m ZSZ od K971 – source (2.6 km from the water)Zboj nad PD,400m V od K343 – source (2.6 km from the water)J okraj obce na ľavom brehu Zbojského potoka – source (2.6 km from the water)Zboj dol.Zahrabova,1500m SV od K725 – source (2.7 km from the water)N.Sedlica dol.Kamenist.p.900m SV od K952 – source (2.8 km from the water)Zboj dol.Zahrabova,1600m V od K1012 – source (2.8 km from the water)1100 m SV od obce, 1650 m ZSZ od k. Minčol (974) – source (2.9 km from the water)zlato 1 ks – gold (70 m from the water)2 km

    The line is the water of the fishing district, the light band is the 3 km zone in which boreholes, mine workings and burdens were searched for. The map shows the nearest objects (at most a few dozen from each register), not all of them. The points correspond to the position in the register; area objects are marked by their centre.

    Trace elements in surface waters

    Arsenic, antimony, cadmium, lead, copper, zinc and other elements in samples from rivers and streams (Geochemical Atlas of Slovakia, surface waters, 2015). The bar shows where the highest value lies among all samples in Slovakia; the light marker is the median of the samples at this water.

    • ChromiumCrslightly elevated
      highest 2.22 μg/lmedian 1.00 μg/l5 samples80 % below the limit of quantification

      Highest value: Zbojský potok, prítok2009, 700 m from the water. Comparison: percentile 76 of all samples in Slovakia.

    • BariumBatypical value
      highest 52.0 μg/lmedian 47.0 μg/l5 samples

      Highest value: Zbojský potok2009, 60 m from the water. Comparison: percentile 63 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: Zbojský potok, prítok2009, 700 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: Zbojský potok, prítok2009, 700 m from the water. Comparison: percentile 43 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: Zbojský potok, prítok2009, 700 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l5 samples100 % below the limit of quantification

      Highest value: Zbojský potok, prítok, 700 m from the water. Comparison: percentile 26 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l5 samples100 % below the limit of quantification

      Highest value: Zbojský potok, prítok2009, 700 m from the water. Comparison: percentile 22 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: Zbojský potok, prítok2009, 700 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 7.10 mg/lmedian 5.80 mg/l5 samples

      Highest value: Zbojský potok, prítok2009, 140 m from the water. Comparison: percentile 27 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)58 samples, at most 555 grains
    • Rutil (TiO₂)30 samples, at most 4115 grains
    • Limonite (FeO(OH)·nH₂O)23 samples, at most 1815 grains
    • Anatas (TiO₂)20 samples, at most 55 grains
    • Pyrite (FeS₂)14 samples, at most 5 grains
    • Magnetite (Fe₃O₄)13 samples, at most 315 grains
    • Monazit ((Ce,La,Nd)PO₄)8 samples, at most 55 grains
    • Ilmenit (FeTiO₃)6 samples, at most 1815 grains
    • Scheelit (CaWO₄)1 sample, at most 5 grains
    • Kasiterit (SnO₂)1 sample, at most 1 grains
    • Gold (Au)1 sample, at most 1 grains
    • Cinabarit (HgS)1 sample, at most 2 grains

    Nearest samples with gold

    SampleGold in sampleFrom the water
    37061 grain70 m

    Rock-forming and accessory minerals

    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)50 samples, at most 555 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)23 samples, at most 4115 grains
    • Tourmalines (complex borosilicate)22 samples, at most 155 grains
    • Zirconium (ZrSiO₄)21 samples, at most 1115 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)14 samples, at most 1815 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))1 sample, at most 5 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)1 sample, at most 5 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))1 sample, at most 5 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))1 sample, at most 5 grains

    Groundwater: chemistry, water types and radioactivity

    Hydrogeochemical objects (analyses of springs and boreholes), the geochemical atlas of groundwater (1996) and radiohydrochemical sampling. Groundwater feeds streams, so its composition also affects the water in the stream.

    Chemical water types nearby

    • Ca-HCO322×
    • Ca-HCO3-SO45×
    • Ca-Mg-HCO3-SO44×
    • Ca-Mg-HCO31×
    • Ca-Na-HCO31×

    Water quality class according to the hydrogeochemical map

    • class B23×
    • class A8×
    • class D2×

    Metals in groundwater

    • AluminiumAlelevated (top 10 %)
      highest 0.0500 mg/lmedian 0.0100 mg/l26 samples31 % below the limit of quantification

      Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 91 of all samples in Slovakia.

    • SeleniumSeslightly elevated
      highest 1.50 μg/lmedian 0.500 μg/l26 samples92 % below the limit of quantification

      Highest value: prameň1993, 240 m from the water. Comparison: percentile 88 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 1.10 μg/lmedian 0.250 μg/l26 samples77 % below the limit of quantification

      Highest value: prameň1993, 310 m from the water. Comparison: percentile 79 of all samples in Slovakia.

    • LeadPbslightly elevated
      highest 1.00 μg/lmedian 0.500 μg/l26 samples92 % below the limit of quantification

      Highest value: prameň1993, 2.8 km from the water. Comparison: percentile 75 of all samples in Slovakia.

    • CopperCutypical value
      highest 1.70 μg/lmedian 0.250 μg/l26 samples

      Highest value: prameň1993, 310 m from the water. Comparison: percentile 70 of all samples in Slovakia.

    • LithiumLitypical value
      highest 11.0 μg/lmedian 3.00 μg/l26 samples27 % below the limit of quantification

      Highest value: prameň1993, 1.9 km from the water. Comparison: percentile 61 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l15 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.0 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l26 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l26 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    • ZincZnbelow half of Slovakia
      highest 16.0 μg/lmedian 4.00 μg/l26 samples8 % below the limit of quantification

      Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 43 of all samples in Slovakia.

    • AntimonySbbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l26 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 40 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l26 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 38 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    stream, river11,76 Bq/l1.76 Bq/l
    mineral spring12,79 Bq/l2.79 Bq/l
    source717,5 Bq/l3.95 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.

    5 boreholes in the 3 km zone, of which 1 hydrogeological and 4 other; with an archive report number 4.

    Borehole depths

    • up to 10 m3×
    • 10–30 m2×
    • 30–100 m0×
    • 100–300 m0×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    S-2hydrogeological3.5 m1309620 m
    S-1hydrogeological19.2 m1309640 m
    Zbojnarrow-diameter borehole with ordinary drinking and process water20.0 m–1.6 km
    V-2engineering-geological5.0 m856642.0 km
    V-1engineering-geological5.0 m856642.0 km

    Environmental burdens, landfills and anthropogenic sediments

    Recorded environmental burdens (industrial sites, landfills, mining), the register of waste landfills and monitoring of anthropogenic sediments (industrial sludge). It is a list of places, not a measurement of water pollution.

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom the water
    Nová Sedlica140 m²1982–80 m
    Zboj200 m²1986–2.2 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

    • Landslides55×
    • Block fissures2×
    • Block fields1×

    Degree of activity

    • Potenciálny55×
    • Stabilizovaný3×

    Current state

    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S53×
    • SD taken from archival materials, ktorá bola konfrontova3×
    • Processed only in the scope of registration on a scale of 1:25,0002×

    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. Snina1 fishing district · 9.6 km30Zbojský potok č. 130

    More watercourses nearby

    Bodrog basin and Hornád