Watercourse

Slavkovský potok (Poprad)

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
15.0km
region
Prešov Region
Aerial image of watercourse Slavkovský potok (Poprad) 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 Slavkovský potok (Poprad) watercourse

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

Average of the watercourse's fishing districts

Average activity · average of one fishing district

The number in the header is an estimate for the middle of the watercourse based on weather and measurements. The average of the fishing districts also counts satellite data, shading and geology of each district.

Best window today

15:00–17:00

Slavkovský potok (Poprad), window score 51.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 17:04.

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
    Brezovica8 cm–
    Poprad – Matejovce70 cm–
    Source: SHMÚUpdated 10 Nov 2026 16:57

    Elevation profile of the watercourse

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

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

    6507007508000 km2 km4 km6 km8 km
    Elevation profile of the watercourse: from 760 to 662 m a.s.l. over 8.2 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
    760 m a.s.l.
    Lowest point
    656 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.
    103 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.
    13 ‰
    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 Slavkovský potok (Poprad) from 2019
    2019imaged 24 Aug 2019
    Aerial image of watercourse Slavkovský potok (Poprad) from 2022
    2022imaged 26 Aug 2022
    Aerial image of watercourse Slavkovský potok (Poprad) from 2025
    2025imaged 10 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 Slavkovský potok (Poprad) 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

    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.

    Watercourse profile from source to mouthnumber of unmet indicators in 2025 at SHMÚ sites

    01234Cesta Slobody, above, river km 11.8: 2 indicators (2022)mouth, river km 0.0: no failed standard (2025)river km 12 (upper course)river km 0 (towards the mouth)
    Show sites in the table (2)
    • Cesta Slobody, aboveriver km 11.82 indicators
    • mouthriver km 0.0no unmet standard
    • standard not met
    • no unmet standard
    • site not in the yearbook

    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 Slavkovský potok (Poprad) 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 (15 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

    Flysch100% of the water line

    Alternating sandstones and claystones; moderately mineralised water that turns turbid quickly in rain. Geological Map of Slovakia 1:50,000.

    510

    Water according to the atlas

    pH 7.5modelled estimate

    water type Ca–HCO₃–SO₄

    Mineralisation 174 mg/l, soft water (5.8 °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: Antimony 3.53 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.

    0 °C80

    Heat underfoot

    35°C at 1,000 m depth

    heat flow 65 mW/m²

    Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    50nGy/h dose rate

    percentile 47 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

    2samples with gold

    14 ore minerals in the sediment

    Up to 1 grain in one sample (30 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.

    Trace elements in the stream water

    1 from 9indicators in the top 5 %

    highest: Copper 14.4 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 96 (Matejovce, 400 m JJZ od K679 Zadné Rovné).

    Boreholes and groundwater analyses

    331boreholes within 3 km

    366 water analyses nearby

    Of these, 331 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    62°C at the wellhead

    11 geothermal boreholes within 10 km

    Warmest: Veľká Lomnica – GVL-1, yield 54.9 l/s, 6.0 km from the water.

    Environmental burdens and landfills

    22sites within 3 km

    4 environmental burdens, 18 landfills

    Nearest burden: Veľký Slavkov – skládka Pod farmou, 1.3 km from the water. Proximity does not mean that substances leak from the site into the water.

    Deposits and ore occurrences

    10records within 5 km

    2 deposits, 8 ore occurrences

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

    Landslides and slope deformations

    8areas within 3 km

    1 active

    Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed.

    Geological structure beneath the water

    Which rock lies beneath the water line (Geological Map of Slovakia 1:50,000), how old it is, how thick the Quaternary cover is and in which tectonic unit the water flows. The bedrock decides the hardness of the water, the bottom, the turbidity after rain and the abundance of springs.

    The points follow the water line (for a stream and a basin, fishing district after fishing district). The strip is a cross-section by distance, not a map; the width of a section corresponds to the number of points.

    • Flysch100%SR 4.7 %

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

    Flysch: Alternating sandstones and claystones; moderately mineralised water that turns turbid quickly in rain.

    Geological age of the rocks

    • Paleogene100%

    Most common rock units

    SystemAgeUnitPoints
    PaleogeneEocene – OligoceneZuberec Formation1×

    Quaternary cover

    • glacifluvial sediments100%SR 0.5 %

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

    Tectonic division

    • NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

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

    Neotectonic units

    • negative unit (intermountain basins)100%SR 14 %

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

    Direction of neotectonic movements

    • small subsidence100%SR 8.8 %

    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)

    • Poprad Basin100%SR 1.4 %

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

    Engineering-geological districts

    • region of mountain-stream deposits50%SR 21 %
    • region of flyschoid rocks50%SR 5.4 %

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

    Engineering-geological formations

    • formation of Quaternary sediments50%SR 71 %
    • flysch formation50%SR 13 %

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

    Susceptibility of the area to slope deformations

    • Region of stable areas100%SR 95 %

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

    The map covers 1 of 5 points on the water line.

    Hydrogeology: aquifers and groundwater

    Streams and rivers are fed by groundwater. Hydrogeological maps show in which rocks the water is stored, how permeable they are and what the water in them is like. The data come from ŠGÚDŠ maps, not from measurements at a particular water.

    Aquifer rocks (hydrogeological map 1:200,000)

    • Gravel100%SR 52 %

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

    Aquifer type

    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Gravel)50%SR 22 %
    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Gravel)50%SR 0.3 %

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

    Main hydrogeological region

    • kryštalinikum časti Vysokých Tatier a kvartér ich predpolia100%SR 1.2 %

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

    Geothermal groundwater bodies

    • Levoča Basin – W and S part100%SR 9.5 %

    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 7.54typical range

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

    Water hardness

    5.8°dH, soft

    Sum of calcium and magnesium (1.03 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    174mg/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

    • ChloridesCl12.5 mg/lpercentile 58
    • FluoridesF0.0995 mg/lpercentile 42
    • SulphatesSO431.4 mg/lpercentile 36
    • SodiumNa6.23 mg/lpercentile 35
    • MagnesiumMg6.96 mg/lpercentile 20
    • CalciumCa29.8 mg/lpercentile 19
    • PotassiumK1.23 mg/lpercentile 15
    • BicarbonatesHCO378.0 mg/lpercentile 13

    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

    • AmmoniumNH40.160 mg/lpercentile 62
    • Chemical oxygen demandChSK3.56 mg/lpercentile 58
    • PhosphatesPO40.171 mg/lpercentile 56
    • NitratesNO36.31 mg/lpercentile 50

    Metals

    • IronFe0.434 mg/lpercentile 90
    • AluminiumAl262 μg/lpercentile 86
    • ManganeseMn73.6 μg/lpercentile 73
    • ZincZn6.86 μg/lpercentile 51

    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

    • AntimonySb3.53 mg/kgpercentile 88
    • NickelNi36.5 mg/kgpercentile 84
    • BismuthBi0.341 mg/kgpercentile 79
    • CadmiumCd0.337 mg/kgpercentile 75
    • MercuryHg0.197 mg/kgpercentile 74
    • LeadPb20.3 mg/kgpercentile 71
    • ZincZn114 mg/kgpercentile 65
    • MolybdenumMo0.422 mg/kgpercentile 58
    • SeleniumSe0.270 mg/kgpercentile 55
    • TinSn2.60 mg/kgpercentile 48
    • CopperCu20.1 mg/kgpercentile 34
    • ArsenicAs5.26 mg/kgpercentile 30
    • VanadiumV58.8 mg/kgpercentile 26
    • ChromiumCr52.0 mg/kgpercentile 19
    • CobaltCo5.99 mg/kgpercentile 15

    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)
    • SodiumNa1.63 %percentile 96
    • AluminiumAl6.85 %percentile 83
    • ManganeseMn1,225 mg/kgpercentile 80
    • PhosphorusP1,137 mg/kgpercentile 79
    • PotassiumK1.58 %percentile 61
    • CalciumCa1.78 %percentile 42
    • IronFe2.50 %percentile 39
    • MagnesiumMg0.742 %percentile 32
    • TitaniumTi3,735 mg/kgpercentile 22
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • StrontiumSr301 mg/kgpercentile 95
    • CeriumCe106 mg/kgpercentile 95
    • BoronB106 mg/kgpercentile 95
    • LithiumLi43.7 mg/kgpercentile 92
    • BariumBa658 mg/kgpercentile 90
    • GalliumGa16.8 mg/kgpercentile 73
    • BerylliumBe1.58 mg/kgpercentile 60
    • RubidiumRb88.5 mg/kgpercentile 50
    • YttriumY26.3 mg/kgpercentile 43
    • ZirconiumZr361 mg/kgpercentile 35

    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

    50nGy/h in air

    range 42 to 54 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)K1.52 %percentile 85
    • Equivalent thorium (eTh)eTh7.13 ppm41th percentile
    • Equivalent uranium (eU)eU2.11 ppm11th 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 137CsCS1371,362 Bq/m²percentile 42

    Radon risk by isopleths

    • medium80%SR 64 %
    • low20%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

    +9nT

    range -12 to 34 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

    -56mGal

    residual −13.1 mGal

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

    Geothermal potential

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

    • Rock temperature at 1,000 m depth35°C
    • Surface heat flow density65mW/m²

    Geothermal groundwater bodies beneath the water line

    • Levoča Basin – W and S part100%SR 9.5 %

    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)585–1 095m a.s.l.
    • Average elevation of the units759m a.s.l.
    • Average slope3.3°
    • Average January temperature-4.8°C
    • Average July temperature16.5°C
    • Annual precipitation725mm

    Geomorphological units

    • Sub-Tatra Basin100%SR 3.9 %

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

    Geomorphological regions

    • Fatra–Tatra area100%SR 21 %

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

    Climatic-geographical types

    • basin climate100%SR 29 %

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

    Susceptibility of soils to acidification

    • naturally acidic soils75%SR 8.5 %
    • soils susceptible to acidification25%SR 31 %

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

    Soil contamination (map 1:500,000)

    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A100%SR 45 %

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

    Lithogeochemical types

    • Inner Carpathian Paleogene100%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.

    Veľký Slavkov – skládka Pod farmou – SK1001000P (1.3 km from the water)Vysoké Tatry – skládka Pod lesom – SK1001000P (1.7 km from the water)Poprad – ČS PHM – areál SAD – SK1001000P (2.5 km from the water)Poprad – ŽSR – stanica – SK1001000P (2.5 km from the water)Veľký Slavkov – skládka Pod farmou – Veľký Slavk – cannot be estimated (100 m from the water)Veľký Slavkov – pri salaši – Veľký Slavkov – none (110 m from the water)Matejovce – Starý mlyn – Matejovce – none (130 m from the water)Veľký Slavkov – none (140 m from the water)Veľký Slavkov – none (500 m from the water)Matejovce – none (720 m from the water)Veľký Slavkov – none (1.3 km from the water)Gerlachov – pri pieskovni. – Gerlachov pod Tatra – none (1.4 km from the water)Gerlachov – Gerlachov pod Tatrami – none (1.6 km from the water)Nová Lesná – none (1.7 km from the water)Starý Smokovec – skládka Pod lesom – Starý Smoko – none (1.7 km from the water)Mlynica – none (1.8 km from the water)Nová Lesná – none (1.8 km from the water)Poprad – Spišská Sobota – none (1.8 km from the water)Starý Smokovec – none (1.8 km from the water)Mlynica – none (2.2 km from the water)Poprad – Veľká – none (2.3 km from the water)Starý Smokovec – none (3.0 km from the water)Veľký Slavkov – VSČ-1 – non-spa (900 m from the water)Poprad – PP-1 – non-spa (2.3 km from the water)Stará Lesná – FGP-1 – non-spa (4.4 km from the water)Gánovce – GA-1A – non-spa (5.6 km from the water)Gánovce – GA-1 – non-spa (5.6 km from the water)Gánovce – ŠHG-1 – non-spa (5.9 km from the water)Gánovce – ŠHG-2 – non-spa (6.0 km from the water)Veľká Lomnica – GVL-1 – non-spa (6.0 km from the water)Vrbov – Vr-2 – non-spa (6.5 km from the water)Vrbov – Vr-1 – non-spa (6.7 km from the water)Kežmarok – GTK-1 – non-spa (8.7 km from the water)PP-1 – k4 (1.8 km from the water)FGP-1 – l3 (5.0 km from the water)Vr-1,2 – l3 (6.5 km from the water)a1 (510 m from the water)a1 (920 m from the water)a1 (1.3 km from the water)a1 (2.3 km from the water)a1 (2.7 km from the water)a1 (3.0 km from the water)a1 (6.2 km from the water)c1 (6.8 km from the water)a1 (6.9 km from the water)b1 (6.9 km from the water)a1 (6.9 km from the water)c1 (6.9 km from the water)b1 (6.9 km from the water)c2 (7.0 km from the water)b1 (7.1 km from the water)a1 (7.4 km from the water)a1 (7.6 km from the water)a1 (7.6 km from the water)b1 (7.8 km from the water)a1 (7.9 km from the water)a1 (7.9 km from the water)c1 (7.9 km from the water)b1 (7.9 km from the water)a1 (8.0 km from the water)b1 (8.1 km from the water)b2 (8.2 km from the water)a1 (8.5 km from the water)a2 (8.6 km from the water)a1 (8.9 km from the water)a1 (9.8 km from the water)Stará Lesná (4.0 km from the water)Vrbov (6.5 km from the water)Gerlachov – Juh – gravelly sands and sands (1.0 km from the water)Veľká Lomnica I – gravelly sands and sands (4.4 km from the water)Gerlachov – stavebný piesok – sandy gravel (1.4 km from the water)Nová Lesná – stavebný piesok – weathered granite (1.6 km from the water)Mlynica – stavebný piesok – weathered granite (2.2 km from the water)Stráže pod Tatrami – building stone – pieskovec (slabo vápnit (2.7 km from the water)Spišská Teplica – gravelly sands (3.2 km from the water)Veľká Lomnica – gravelly sands (3.7 km from the water)Gerlachov – stavebný piesok – sandy gravel (3.9 km from the water)Tatranská Polianka – gravelly sands (3.9 km from the water)MATEJOVCE – Landslides (1.2 km from the water)– Landslides (1.2 km from the water)MATEJOVCE – Landslides (1.8 km from the water)– Landslides (2.2 km from the water)VELKA LOMNICA – Landslides (2.6 km from the water)NOVA LESNA – Landslides (2.7 km from the water)NOVY SMOKOVEC – Landslides (2.9 km from the water)ZAKOVCE – Landslides (2.9 km from the water)Veľký Slavkov – širokoprofilový vrt (Ø vŕtania nad 600 m (240 m from the water)Veľký Slavkov – SHMÚ observation borehole (420 m from the water)Veľký Slavkov – širokoprofilový vrt (Ø vŕtania nad 600 m (520 m from the water)Matejovce nad Hornádom – širokoprofilový vrt (Ø vŕtania nad 600 m (630 m from the water)Kráľova Lehota – úzkoprofilový vrt s obyčajnou pitnou a ú (650 m from the water)Matejovce – úzkoprofilový vrt s obyčajnou pitnou a ú (650 m from the water)Matejovce – úzkoprofilový vrt s obyčajnou pitnou a ú (670 m from the water)Smokovec-Žiakovská poľana – úzkoprofilový vrt s obyčajnou pitnou a ú (680 m from the water)Matejovce – úzkoprofilový vrt s obyčajnou pitnou a ú (720 m from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (900 m from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (930 m from the water)Matejovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.5 km from the water)Smokovec, Pod Lesom – štruktúrny vrt s obyčajnou vodou (nad 20 (1.5 km from the water)Matejovce – monitoring borehole (1.5 km from the water)Spišská Sobota – Matejovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.5 km from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (2.0 km from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)Poprad – Veľká – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)JRD Gerlachov – úzkoprofilový vrt s obyčajnou pitnou a ú (2.2 km from the water)Poprad – negative borehole (2.2 km from the water)Poprad – monitoring borehole (2.3 km from the water)Poprad – monitoring borehole (2.3 km from the water)Poprad – monitoring borehole (2.3 km from the water)Poprad – monitoring borehole (2.3 km from the water)Poprad – monitoring borehole (2.3 km from the water)Poprad – monitoring borehole (2.3 km from the water)Poprad – vagónka – negative borehole (2.3 km from the water)Poprad – vagónka – širokoprofilový vrt (Ø vŕtania nad 600 m (2.4 km from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Gerlachov – SHMÚ observation borehole (2.4 km from the water)Poprad – structural borehole with thermal water, minerálnou v (2.4 km from the water)Poprad – širokoprofilový vrt (Ø vŕtania nad 600 m (2.4 km from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Poprad – širokoprofilový vrt (Ø vŕtania nad 600 m (2.4 km from the water)Poprad – SHMÚ observation borehole (2.5 km from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Poprad – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Veľká Lomnica – úzkoprofilový vrt s obyčajnou pitnou a ú (2.6 km from the water)zlato 1 ks – gold (30 m from the water)zlato 1 ks – gold (580 m 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.

    • CopperCuhigh (top 5 %)
      highest 14.4 μg/lmedian 1.60 μg/l5 samples

      Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • StrontiumSrelevated (top 10 %)
      highest 604 μg/lmedian 135 μg/l7 samples

      Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 94 of all samples in Slovakia.

    • CadmiumCdelevated (top 10 %)
      highest 0.500 μg/lmedian 0.150 μg/l5 samples80 % below the limit of quantification

      Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné, 730 m from the water. Comparison: percentile 92 of all samples in Slovakia.

    • LeadPbslightly elevated
      highest 3.50 μg/lmedian 2.50 μg/l5 samples80 % below the limit of quantification

      Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 88 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 13.0 μg/lmedian 5.00 μg/l7 samples86 % below the limit of quantification

      Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 78 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.650 μg/lmedian 0.500 μg/l7 samples86 % below the limit of quantification

      Highest value: Nová Lesná, Veľký Slavkov, bezmenný prítok Popradu1997, 740 m from the water. Comparison: percentile 77 of all samples in Slovakia.

    • ChromiumCrtypical value
      highest 1.20 μg/lmedian 1.00 μg/l5 samples80 % below the limit of quantification

      Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 66 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.960 μg/lmedian 0.500 μg/l7 samples71 % below the limit of quantification

      Highest value: Nová Lesná, Veľký Slavkov, bezmenný prítok Popradu1997, 740 m from the water. Comparison: percentile 49 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: Veľký Slavkov, 1400 m SV od K7061997, 40 m from the water. Comparison: percentile 46 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 24.5 mg/lmedian 18.5 mg/l7 samples

      Highest value: Nová Lesná, Veľký Slavkov, bezmenný prítok Popradu1997, 740 m from the water. Comparison: percentile 82 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.

    • Cinabarit (HgS)23 samples, at most 50 grains
    • Barite (BaSO₄)20 samples, at most 55 grains
    • Pyrite (FeS₂)16 samples, at most 315 grains
    • Ilmenit (FeTiO₃)13 samples, at most 4115 grains
    • Rutil (TiO₂)11 samples, at most 55 grains
    • Magnetite (Fe₃O₄)9 samples, at most 1815 grains
    • Hematite (Fe₂O₃)8 samples, at most 4115 grains
    • Limonite (FeO(OH)·nH₂O)8 samples, at most 315 grains
    • Anatas (TiO₂)7 samples, at most 5 grains
    • Scheelit (CaWO₄)6 samples, at most 400 grains
    • Monazit ((Ce,La,Nd)PO₄)5 samples, at most 5 grains
    • Gold (Au)2 samples, at most 1 grains
    • Markazit (FeS₂)2 samples, at most 15 grains
    • Chalcopyrite (CuFeS₂)1 sample, at most 5 grains

    Nearest samples with gold

    SampleGold in sampleFrom the water
    51871 grain30 m
    51811 grain580 m

    Rock-forming and accessory minerals

    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)12 samples, at most 55 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)11 samples, at most 815 grains
    • Tourmalines (complex borosilicate)11 samples, at most 5 grains
    • Zirconium (ZrSiO₄)11 samples, at most 815 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))10 samples, at most 1815 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))7 samples, at most 5 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)5 samples, at most 55 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))3 samples, at most 5 grains
    • Titanit (CaTiSiO₅)3 samples, at most 31 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)2 samples, at most 5 grains
    • Kyanit (Al₂SiO₅)1 sample, at most 5 grains
    • Sillimanit (Al₂SiO₅)1 sample, at most 5 grains
    • Andaluzit (Al₂SiO₅)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.

    Metals in groundwater

    • MercuryHgextreme (top 1 %)
      highest 1.00 μg/lmedian 0.100 μg/l29 samples72 % below the limit of quantification

      Highest value: drén1994, 1.4 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AluminiumAlextreme (top 1 %)
      highest 0.340 mg/lmedian 0.0100 mg/l29 samples41 % below the limit of quantification

      Highest value: drén1994, 30 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 6.00 μg/lmedian 0.500 μg/l29 samples52 % below the limit of quantification

      Highest value: prameň1992, 2.4 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 1.40 μg/lmedian 0.100 μg/l29 samples62 % below the limit of quantification

      Highest value: studňa1992, 1.8 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ZincZnhigh (top 5 %)
      highest 1,324 μg/lmedian 13.0 μg/l29 samples34 % below the limit of quantification

      Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 0.500 μg/lmedian 0.250 μg/l29 samples93 % below the limit of quantification

      Highest value: drén1994, 30 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LithiumLielevated (top 10 %)
      highest 43.0 μg/lmedian 18.0 μg/l29 samples10 % below the limit of quantification

      Highest value: studňa1994, 90 m from the water. Comparison: percentile 93 of all samples in Slovakia.

    • SeleniumSeelevated (top 10 %)
      highest 2.10 μg/lmedian 0.500 μg/l29 samples83 % below the limit of quantification

      Highest value: studňa1992, 1.8 km from the water. Comparison: percentile 93 of all samples in Slovakia.

    • ChromiumCrelevated (top 10 %)
      highest 2.80 μg/lmedian 0.500 μg/l29 samples34 % below the limit of quantification

      Highest value: drenáž1992, 2.8 km from the water. Comparison: percentile 92 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 2.00 μg/lmedian 0.500 μg/l29 samples93 % below the limit of quantification

      Highest value: prameň1992, 2.1 km from the water. Comparison: percentile 88 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 3.00 μg/lmedian 0.600 μg/l29 samples

      Highest value: prameň1992, 100 m from the water. Comparison: percentile 84 of all samples in Slovakia.

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

      Highest value: prameň1992, 2.8 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    free-flowing borehole with thermal and mineral water11,49 Bq/l1.49 Bq/l
    source819,3 Bq/l7.13 Bq/l
    well59,79 Bq/l3.20 Bq/l
    stream, river31,58 Bq/l0.390 Bq/l
    free-flowing borehole142,7 Bq/l42.7 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
    Gerlachov – Juhgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – Poľnohospodárske družstvo TATRAN1.0 km
    Veľká Lomnica Igravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – RIVERSAND a. s.4.4 km

    Boreholes and Geofond archive reports

    Register of hydrogeological boreholes, other boreholes and geothermal boreholes. Each borehole has a report in the Geofond archive (geological profiles, pumping tests, chemical analyses of the water); the report number is in the table.

    331 boreholes in the 3 km zone, of which 52 hydrogeological and 279 other; with an archive report number 331.

    Borehole depths

    • up to 10 m217×
    • 10–30 m89×
    • 30–100 m2×
    • 100–300 m0×
    • over 300 m1×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    J 48engineering-geological10.0 m7953540 m
    J 162engineering-geological10.0 m7953590 m
    J 49engineering-geological10.0 m7953590 m
    J 53engineering-geological10.0 m79535100 m
    J 54engineering-geological10.0 m79535170 m
    J 51engineering-geological10.0 m79535190 m
    Veľký Slavkovwide-diameter borehole17.0 m64513 101Da14.pdf240 m
    V-5engineering-geological6.0 m87239260 m
    V-3engineering-geological6.0 m87239270 m
    V-4engineering-geological6.0 m87239300 m
    V-2engineering-geological6.0 m87239310 m
    V-1engineering-geological6.0 m87239340 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.

    BoreholeTemperatureYieldDepthChemical water typeUseFrom the water
    Veľký Slavkov – VSČ-157 °C–2400 mCa-Mg-HCO3unused900 m
    Poprad – PP-148 °C61.2 l/s1205 mCa-Mg-SO4-HCO3in use2.3 km
    Stará Lesná – FGP-158 °C22.0 l/s3616 mCa-Mg-HCO3unused4.4 km
    Gánovce – GA-1A27 °C1.9 l/s276 mCa-Mg-HCO3-SO4in use without data reporting5.6 km
    Gánovce – GA-123 °C2.8 l/s50 mCa-Mg-HCO3-SO4unused5.6 km
    Gánovce – ŠHG-126 °C3.0 l/s150 mCa-Mg-HCO3-SO4unused5.9 km
    Gánovce – ŠHG-225 °C2.5 l/s110 mCa-Mg-HCO3-SO4unused6.0 km
    Veľká Lomnica – GVL-162 °C54.9 l/s2100 mCa-Mg-HCO3-SO4in use6.0 km
    Vrbov – Vr-259 °C33.0 l/s2502 mCa-Mg-HCO3-SO4in use6.5 km
    Vrbov – Vr-156 °C28.3 l/s1742 mCa-Mg-HCO3-SO4in use6.7 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 518510 m
    PP-1geothermal water38 – 5531 – 5011.8 km
    category Stará Lesnáthermal baths––14.0 km
    FGP-1geothermal water55 – 8016 – 3015.0 km
    Vr-1.2geothermal water55 – 8016 – 3016.5 km
    category Vrbovthermal baths––16.5 km
    category c1mineral water23-38< 536.8 km
    category b1mineral water15-22< 566.9 km
    category c2mineral water23-385-1517.0 km
    category b2mineral water15-225-1518.2 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.

    Environmental burdens

    SiteActivitySubstanceClassificationFrom the water
    Veľký Slavkov – landfill Pod farmouSK1001000P1.3 km
    High Tatras – skládka Pod lesomSK1001000P1.7 km
    Poprad – ČS PHM – areál SADSK1001000P2.5 km
    Poprad – ŽSR – stationSK1001000P2.5 km

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom the water
    Veľký Slavkov – landfill Pod farmou – Veľký Slavkov–1950monitored100 m
    Veľký Slavkov – pri salaši – Veľký Slavkov300 m²1960–110 m
    Matejovce – Starý mlyn – Matejovce100 m²1960–130 m
    Veľký Slavkov750 m²1975–140 m
    Veľký Slavkov500 m²1988–500 m
    Matejovce–1988monitored720 m
    Veľký Slavkov20 531 m²1982monitored1.3 km
    Gerlachov – pri pieskovni. – Gerlachov pod Tatrami–1980–1.4 km

    Landslides and slope deformations

    Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel.

    Types of deformations

    • Landslides8×

    Degree of activity

    • Potenciálny7×
    • Aktívny1×

    Current state

    • Processed only in the scope of registration on a scale of 1:25,0004×
    • SD taken from archival materials, ktorá bola konfrontova4×

    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.
    • Panning concentrates. 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. Poprad1 fishing district · 15 km43Slavkovský potok (Poprad)43

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