Watercourse

Lesnica (NP Slovak Paradise)

Bodrog basin and HornádSalmonid (trout)
fishing district
1
fishing district length
5.6km
region
Košice Region
Aerial image of watercourse Lesnica (NP Slovak Paradise) 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

The Lesnica (NP Slovak Paradise) watercourse at a glance

On the Lesnica (NP Slovenský raj) je jeden rybársky revír. stream Lesnica (NP Slovak Paradise) is salmonid (trout) fishing district no. 4-0140-4-2. It lies in Spišská Nová Ves district (Košice Region). The district is 5.6 km long. Fishing rules, permits, the map and conditions at the water are on the fishing district's page. It belongs to the Bodrog and Hornád river basin.

Open fishing district Lesnica (NP Slovak Paradise)

Fish typical of this type of water:

Today on the Lesnica (NP Slovak Paradise) watercourse

Is it worth going today? Fishing conditions score, the best window of the day and fishing districts from the best conditions
Conditions score44 / 100Best window06:00

Average of the watercourse's fishing districts

Average activity · average of one fishing district

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

Best window today

06:00–08:00

Lesnica (NP Slovak Paradise), window score 58.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 10:23.

Map and fishing districts of the Lesnica (NP Slovak Paradise) 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.
Fishing districts1Length5,6 km

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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    Fish and catches on the Lesnica (NP Slovak Paradise) watercourse

    Which fish live here and what has been caught? Game species recorded in the fishing districts and approved catches by anglers

    Organizations and districts on the Lesnica (NP Slovak Paradise) watercourse

    Who manages the fishing districts and where they are
    Districts1

    Water pollution on the Lesnica (NP Slovak Paradise) watercourse

    Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby
    Districts failing a standard0 / 1

    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.

    Terrain and satellite images of the Lesnica (NP Slovak Paradise) watercourse

    Elevation profile, 3D terrain of the surroundings and historical satellite images
    Highest point755 m n. m.Lowest point517 m n. m.

    Elevation profile of the watercourse

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

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

    5006007008000 km2 km4 km
    Elevation profile of the watercourse: from 755 to 537 m a.s.l. over 5.5 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
    755 m a.s.l.
    Lowest point
    517 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.
    238 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.
    43 ‰
    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.
    1.13

    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 Lesnica (NP Slovak Paradise) from 2019
    2019imaged 30 Jun 2019
    Aerial image of watercourse Lesnica (NP Slovak Paradise) from 2022
    2022imaged 17 Oct 2022
    Aerial image of watercourse Lesnica (NP Slovak Paradise) from 2025
    2025imaged 2 Jul 2025

    Orthophoto mosaic of Slovakia © GKÚ Bratislava, NLC Zvolen. The year and day of imaging depend on the location, so individual years may differ in season and weather.

    More watercourses near the Lesnica (NP Slovak Paradise) watercourse

    The nearest rivers, streams and water bodies in the same river basin
    Watercourses6

    Geology and geochemistry of the Lesnica (NP Slovak Paradise) stream

    Geology at a glance and a map of the zone

    What lies beneath the water and around it? An overview in tiles, a map of mine workings, deposits, environmental burdens, boreholes and gold finds, and how to read the data

    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 (6 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

    Limestones and dolomites100% of the water line

    Hard, well-buffered water with calcium and bicarbonates; karst springs. Geological Map of Slovakia 1:50,000.

    510

    Water according to the atlas

    pH 8.4modelled estimate

    water type Ca–Mg–HCO₃

    Mineralisation 463 mg/l, hard water (16.5 °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: Cadmium 0.492 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 86. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km30 °C45 °C

    Heat underfoot

    30°C at 1,000 m depth

    heat flow 60 mW/m²

    At a depth of 2,000 m about 45 °C (increase of 15 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    53nGy/h dose rate

    percentile 65 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

    8objects within 3 km

    Nearest: Štôlňa (adit), 210 m from the water.

    Gold in river sediment

    0samples with gold

    9 ore minerals in the sediment

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

    Trace elements in the stream water

    2 from 10indicators in the top 5 %

    highest: Chromium 6.10 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 95 (500m J od osady Blatná).

    Boreholes and groundwater analyses

    84boreholes within 3 km

    292 water analyses nearby

    Of these, 84 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    31°C at the wellhead

    2 geothermal boreholes within 10 km

    Warmest: Arnutovce – HKJ-3, yield 11.8 l/s, 4.4 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

    42records within 5 km

    12 deposits, 30 ore occurrences

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

    Landslides and slope deformations

    0areas within 3 km

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

    Map of the corridor

    Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off.

    Štôlňa – 2 – adit (210 m from the water)Pingový ťah – 4 – pinge (mining subsidence pit), line of pinge pits (2.9 km from the water)Štôlňa – 2 – adit (2.9 km from the water)Halda – 5 – spoil heap (2.9 km from the water)Halda – 5 – spoil heap (2.9 km from the water)Halda – 5 – spoil heap (2.9 km from the water)Štôlňa – 2 – adit (3.0 km from the water)Halda – 5 – spoil heap (3.0 km from the water)Spišská Nová Ves-Novoveská Huta, žily Rybník a M – Copper ores (2.4 km from the water)Spišská Nová Ves, žila Hanisková – Copper ores (3.0 km from the water)Spišská Nová Ves – Hanisková – Copper ores (3.0 km from the water)Spišská Nová Ves, Strážanský kopec a Malý Muráň – Copper ores (3.5 km from the water)Spišská Nová Ves – Novoveská Huta – Copper ores (3.9 km from the water)Hnilec, žila Michal-Jozef – Complex iron ores (4.0 km from the water)Spišská Nová Ves – Novoveská Huta – Uranium-molybdenum ores (4.0 km from the water)Spišská Nová Ves, Muráň – Uranium-molybdenum ores (4.1 km from the water)Hnilec, žilník Kráľov vrch – Complex iron ores (4.2 km from the water)Hnilec, žily Amália, Jozef a Samuel – Complex iron ores (4.2 km from the water)Spišská Nová Ves – Viničiar – Copper ores (4.3 km from the water)Hnilec, žila Ida – Complex iron ores (4.6 km from the water)Spišské Tomášovce – occasional (2.0 km from the water)Arnutovce – HKJ-3 – non-spa (4.4 km from the water)Letanovce – HKJ-4 – non-spa (5.0 km from the water)HKJ-3 – j2 (4.8 km from the water)a1 (6.8 km from the water)a1 (8.5 km from the water)a1 (9.1 km from the water)a1 (9.9 km from the water)Spišské Tomášovce – building stone (1.1 km from the water)Smižany – Spišská Nová Ves – brick raw materials (4.1 km from the water)Spišská Nová Ves – uranium ores (4.1 km from the water)Spišská Nová Ves – copper ores (4.1 km from the water)Spišské Tomášovce – building stone (1.1 km from the water)Mlynky – Biele Vody – gypsum (3.5 km from the water)Mlynky – Biele Vody – anhydrite (3.5 km from the water)Spišská Nová Ves – copper ores (4.1 km from the water)Spišská Nová Ves – uranium ores (4.1 km from the water)Smižany – Spišská Nová Ves – brick raw materials (4.1 km from the water)Spišská Nová Ves – uranium ores (4.1 km from the water)Spišská Nová Ves – copper ores (4.1 km from the water)Smižany – Klauzy – stavebný piesok – dolomite (130 m from the water)Smižany – Fe ores (2.4 km from the water)Maša – kameňolom – building stone – sandstone (2.6 km from the water)Maša – lom – building stone – microconglomerates (2.9 km from the water)Letanovce – building stone – piesčité bridlice až pi (3.2 km from the water)Smižany – gravelly sands (3.4 km from the water)Spišská Nová Ves – Novoveská Huta – Cu ores (3.8 km from the water)Smižany – gravelly sands (3.9 km from the water)Spišská Nová Ves – Novoveská Huta – Cu ores (4.0 km from the water)Novoveská Huta – Cu ores, Cu metal (4.1 km from the water)Spišská Nová Ves – Novoveská Huta – Cu ores (4.2 km from the water)Novoveská Huta – Cu ores (4.4 km from the water)Spišská Nová Ves – stavebný piesok (konglomerát – sandstone (4.7 km from the water)Arnutovce II – building stone – sandstone (4.9 km from the water)Sp. N. Ves – Hanisková – copper ores (3.1 km from the water)Sp. N. Ves – Novoveská Huta – molybdenum ores (3.4 km from the water)Sp. N. Ves – Muráň – molybdenum ores (3.4 km from the water)Sp. N. Ves – Novoveská Huta – copper ores (4.6 km from the water)Spišské Tomášovce – general geology (770 m from the water)Novoveská Huta – mineralogy (2.1 km from the water)Medvedia jaskyňa (planina Glac) – paleontology (2.7 km from the water)Novoveská Huta – mining (3.7 km from the water)Mlynky – mineralogy (4.2 km from the water)Čingov – širokoprofilový vrt (Ø vŕtania nad 600 m (390 m from the water)Čingov-Sp.Tomášovce – širokoprofilový vrt (Ø vŕtania nad 600 m (500 m from the water)Čingov-Sp.Tomášovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.4 km from the water)Čingov – úzkoprofilový vrt s obyčajnou pitnou a ú (1.4 km from the water)Smižany – štruktúrny vrt s obyčajnou vodou (nad 20 (1.8 km from the water)Spišské Tomášovce – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Smižany-Košiarny briežok – úzkoprofilový vrt s obyčajnou pitnou a ú (1.9 km from the water)Spišské Tomášovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.0 km from the water)Spišské Tomášovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Spišské Tomášovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Spišské Tomášovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Spišské Tomášovce – úzkoprofilový vrt s obyčajnou pitnou a ú (2.5 km from the water)Spišské Tomášovce – štruktúrny vrt s obyčajnou vodou (nad 20 (2.6 km from the water)Spišská Nová Ves – úzkoprofilový vrt s obyčajnou pitnou a ú (2.6 km from the water)Smižany – úzkoprofilový vrt s obyčajnou pitnou a ú (2.7 km from the water)Smižany – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Smižany – úzkoprofilový vrt s obyčajnou pitnou a ú (2.9 km from the water)Smižany – úzkoprofilový vrt s obyčajnou pitnou a ú (2.9 km from the water)Smižany – úzkoprofilový vrt s obyčajnou pitnou a ú (2.9 km from the water)prameň – Groundwater springs (20 m from the water)prameň s monitorovaním výdatnosti – Groundwater springs (50 m from the water)prameň – Groundwater springs (80 m from the water)prameň – Groundwater springs (100 m from the water)prameň – Groundwater springs (370 m from the water)vrt, ktorý poskytol hydrogeologické informácie, – Hydrogeological boreholes (390 m from the water)pramenná línia – Groundwater springs (390 m from the water)prameň – Groundwater springs (480 m from the water)prameň – Groundwater springs (480 m from the water)vrt, ktorý poskytol hydrogeologické informácie, – Hydrogeological boreholes (500 m from the water)závrt – Point karst features (630 m from the water)závrt – Point karst features (770 m from the water)prameň – Groundwater springs (770 m from the water)prameň – Groundwater springs (830 m from the water)prameň – Groundwater springs (870 m from the water)prameň – Groundwater springs (1.2 km from the water)vodárensky využívaný prameň – Groundwater springs (1.2 km from the water)prameň – Groundwater springs (1.2 km from the water)vodárensky využívaný prameň – Groundwater springs (1.3 km from the water)prameň – Groundwater springs (1.3 km from the water)prameň – Groundwater springs (1.3 km from the water)vodárensky využívaný a monitorovaný prameň – Groundwater springs (1.3 km from the water)závrt – Point karst features (1.3 km from the water)prameň – Groundwater springs (1.3 km from the water)vodárensky využívaný prameň – Groundwater springs (1.3 km from the water)prameň – Groundwater springs (1.3 km from the water)vodárensky využívaný prameň – Groundwater springs (1.3 km from the water)prameň – Groundwater springs (1.4 km from the water)vodárensky využívaný prameň – Groundwater springs (1.4 km from the water)vodárensky využívaný prameň – Groundwater springs (1.4 km from the water)vodárensky využívaný prameň – Groundwater springs (1.4 km from the water)vodárensky využívaný prameň – Groundwater springs (1.4 km from the water)vodárensky využívaný prameň – Groundwater springs (1.4 km from the water)pramenná línia – Groundwater springs (1.5 km from the water)vodárensky využívaný prameň – Groundwater springs (1.5 km from the water)závrt – Point karst features (1.6 km from the water)prameň – Groundwater springs (1.6 km from the water)prameň – Groundwater springs (1.6 km from the water)prameň – Groundwater springs (1.6 km from the water)prameň s monitorovaním výdatnosti – Groundwater springs (1.6 km from the water)Lesnica – source (50 m from the water)Lesnica – source (60 m from the water)Smižany – source (60 m from the water)Smižany – source (140 m from the water)Sp. Nová Ves – source (180 m from the water)Lesnica – source (360 m from the water)Lesnica – source (450 m from the water)Sp. Nová Ves – source (480 m from the water)Lesnica – source (680 m from the water)Sp. Nová Ves – source (770 m from the water)Spišské Tomášovce – source (980 m from the water)Sp. Nová Ves – source (1.1 km from the water)Smižany – source (1.2 km from the water)Novoveská Huta – Čertova dolina, 750m S od K 115 – source (1.3 km from the water)Sp. Nová Ves – source (1.4 km from the water)Sp. Nová Ves – source (1.4 km from the water)Smižany – source (1.4 km from the water)Smižany – source (1.4 km from the water)Smižany – source (1.4 km from the water)Novoveská Huta – source (1.4 km from the water)Smižany – source (1.4 km from the water)Čertov potok – source (1.4 km from the water)Novoveská Huta – Čertova dolina, 1200m SSV od K – source (1.5 km from the water)Spišská Nová Ves – source (1.5 km from the water)Novoveská Huta – source (1.5 km from the water)Spišské Tomášovce – source (1.5 km from the water)Spišské Tomášovce – source (1.6 km from the water)Biely potok, prameň Zlatá diera – source (1.6 km from the water)Novoveská Huta, dolina Fleišer – source (1.7 km from the water)Sp. Nová Ves – source (1.8 km from the water)Spišské Tomášovce – source (1.8 km from the water)dolina Bieleho potoka – source (1.9 km from the water)Čertov potok – source (2.0 km from the water)Čertov potok – source (2.2 km from the water)Smižany – well (2.3 km from the water)Čingov – source (2.3 km from the water)Mlynky, 1200m JZ od K 1158 Hýľ – source (2.5 km from the water)Hrabušice – source (2.5 km from the water)Čingov – source (2.5 km from the water)Smižany – source (2.5 km from the water)5 km

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

    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.

    Rocks, groundwater and landscape

    What does the water flow over? Geological structure and age of the rocks, groundwater aquifers, relief, climate, soils and geophysical fields

    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.

    • Limestones and dolomites100%SR 2.7 %

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

    Limestones and dolomites: Hard, well-buffered water with calcium and bicarbonates; karst springs.

    Geological age of the rocks

    • Triassic100%

    Most common rock units

    SystemAgeUnitPoints
    TriassicMiddle TriassicNadaš limestones: bedded pink limestones1×
    TriassicLate Triassicdachstein limestones: riff and lagunar organogenic and organodetritic limestones; light limestone (light gray and1×

    Quaternary cover

    • Typical thickness of the Quaternary cover2.3m
    • 0 – 250%SR 16 %
    • 2 – 550%SR 48 %

    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

    • Gemer Belt100%SR 5.9 %

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

    Regional geological division (subunits)

    • Slovak Paradise100%SR 0.7 %

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

    Engineering-geological districts

    • region of limestone rocks100%SR 1.1 %

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

    Engineering-geological formations

    • limestone-dolomite formation100%SR 1.5 %

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

    Susceptibility of the area to slope deformations

    • Region of potentially unstable areas100%SR 4.4 %

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

    The map covers 2 of 2 points on the water line.

    Hydrogeology: aquifers and groundwater

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

    Aquifer rocks (hydrogeological map 1:200,000)

    • Gravel50%SR 52 %
    • Dolomity50%SR 1.8 %

    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 %
    • Zvodnence s prevažne puklinovým typom priepustnosti, vrátane krasových (spevnené horninové masívy s diskontinuitami) (Dolomity; Nerozlíšené)50%SR 1.8 %

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

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

    • fissure-karst100%SR 0.6 %

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

    Hydrogeological function

    • aquifer100%SR 95 %

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

    Main hydrogeological region

    • Mesozoic of the Slovak Paradise and Raven Hills with the adjacent Paleozoic100%SR 0.0 %

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

    Genetic type of groundwater

    • carbonate100%SR 0.0 %

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

    Chemical type of groundwater

    • Ca-(Mg)-HCO3100%SR 1.7 %

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

    Groundwater quality class

    • A100%SR 36 %

    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)459–1 267m a.s.l.
    • Average elevation of the units870m a.s.l.
    • Average slope18.8°
    • Average January temperature-5.3°C
    • Average July temperature15.6°C
    • Annual precipitation838mm

    Geomorphological units

    • Spiš–Gemer Karst100%SR 0.0 %

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

    Geomorphological regions

    • Slovak Ore Mountains100%SR 10 %

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

    Climatic-geographical types

    • basin climate50%SR 29 %
    • mountain climate50%SR 33 %

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

    Susceptibility of soils to acidification

    • soils not susceptible to acidification100%SR 27 %

    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 Paleogene50%SR 11 %
    • Mesozoic of the Bradl zone and the central Western Carpathians50%SR 10 %

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

    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

    -55nT

    range -59 to -51 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

    -33mGal

    residual −0.7 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.

    Chemistry of water and river sediments

    What is in the water and on the bed? Trace elements and metals, nutrients, major ions, elements in sediments and groundwater

    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 8.38typical 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

    16.5°dH, hard

    Sum of calcium and magnesium (2.95 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    463mg/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–Mg–HCO₃

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

    Major ions

    • MagnesiumMg26.9 mg/lpercentile 81
    • SulphatesSO463.6 mg/lpercentile 71
    • BicarbonatesHCO3273 mg/lpercentile 69
    • CalciumCa74.0 mg/lpercentile 63
    • ChloridesCl11.4 mg/lpercentile 56
    • FluoridesF0.110 mg/lpercentile 48
    • SodiumNa8.33 mg/lpercentile 47
    • PotassiumK2.55 mg/lpercentile 42

    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

    • Chemical oxygen demandChSK2.75 mg/lpercentile 39
    • PhosphatesPO40.0579 mg/lpercentile 31
    • NitratesNO33.28 mg/lpercentile 19
    • AmmoniumNH40.0360 mg/lpercentile 16

    Metals

    • AluminiumAl177 μg/lpercentile 76
    • ManganeseMn20.1 μg/lpercentile 39
    • ZincZn2.40 μg/lpercentile 15
    • IronFe0.0271 mg/lpercentile 8

    Trace elements in surface waters

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

    • ChromiumCrhigh (top 5 %)
      highest 6.10 μg/lmedian 4.80 μg/l5 samples

      Highest value: 500m J od osady Blatná1992, 280 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 5.00 μg/lmedian 2.50 μg/l5 samples80 % below the limit of quantification

      Highest value: Hornád1992, 360 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • StrontiumSrelevated (top 10 %)
      highest 630 μg/lmedian 40.0 μg/l5 samples

      Highest value: Hornád1992, 360 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LithiumLielevated (top 10 %)
      highest 30.0 μg/lmedian 5.00 μg/l5 samples80 % below the limit of quantification

      Highest value: Hornád1992, 360 m from the water. Comparison: percentile 91 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 3.20 μg/lmedian 0.500 μg/l5 samples60 % below the limit of quantification

      Highest value: Hornád1992, 360 m from the water. Comparison: percentile 85 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 3.60 μg/lmedian 1.00 μg/l5 samples80 % below the limit of quantification

      Highest value: Hornád1992, 360 m from the water. Comparison: percentile 84 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.600 μg/lmedian 0.500 μg/l5 samples80 % below the limit of quantification

      Highest value: 100m Z od rybníka1992, 100 m from the water. Comparison: percentile 76 of all samples in Slovakia.

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

      Highest value: 1000m ZSZ od K1107 Holý kameň, 990 m from the water. Comparison: percentile 75 of all samples in Slovakia.

    • BariumBatypical value
      highest 50.0 μg/lmedian 10.0 μg/l5 samples

      Highest value: Hornád1992, 360 m from the water. Comparison: percentile 60 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: 1000m ZSZ od K1107 Holý kameň1993, 990 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 dioxideSiO2below half of Slovakia
      highest 5.40 mg/lmedian 4.70 mg/l5 samples

      Highest value: 1000m S od kaplnky Svrch Jána1992, 420 m from the water. Comparison: percentile 15 of all samples in Slovakia.

    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

    • CadmiumCd0.492 mg/kgpercentile 86
    • SeleniumSe0.484 mg/kgpercentile 85
    • AntimonySb0.866 mg/kgpercentile 66
    • ArsenicAs7.24 mg/kgpercentile 57
    • BismuthBi0.230 mg/kgpercentile 55
    • LeadPb15.7 mg/kgpercentile 51
    • MercuryHg0.0998 mg/kgpercentile 49
    • TinSn2.59 mg/kgpercentile 47
    • MolybdenumMo0.315 mg/kgpercentile 37
    • CopperCu18.2 mg/kgpercentile 25
    • NickelNi17.0 mg/kgpercentile 18
    • ChromiumCr45.0 mg/kgpercentile 11
    • VanadiumV48.2 mg/kgpercentile 8
    • ZincZn58.2 mg/kgpercentile 6
    • CobaltCo4.12 mg/kgpercentile 4

    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)
    • MagnesiumMg3.28 %percentile 95
    • CalciumCa7.10 %percentile 89
    • SodiumNa0.815 %percentile 39
    • PhosphorusP634 mg/kgpercentile 22
    • ManganeseMn543 mg/kgpercentile 11
    • PotassiumK1.20 %percentile 10
    • AluminiumAl4.22 %percentile 8
    • IronFe1.88 %percentile 7
    • TitaniumTi2,803 mg/kgpercentile 5
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • BoronB68.4 mg/kgpercentile 72
    • LithiumLi31.2 mg/kgpercentile 59
    • CeriumCe51.0 mg/kgpercentile 21
    • RubidiumRb75.5 mg/kgpercentile 20
    • ZirconiumZr288 mg/kgpercentile 18
    • StrontiumSr103 mg/kgpercentile 17
    • YttriumY19.7 mg/kgpercentile 14
    • GalliumGa7.69 mg/kgpercentile 9
    • BariumBa250 mg/kgpercentile 4
    • BerylliumBe0.337 mg/kgpercentile 4

    Groundwater: chemistry and water types

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

    Chemical water types nearby

    • Ca-Mg-HCO325×
    • Ca-HCO38×
    • Ca-Mg-HCO3-SO46×
    • Ca-Mg-SO4-HCO32×
    • Ca-Mg-HCO3-NO31×
    • Ca-Mg-SO4-NO3-HCO31×
    • Ca-HCO3-SO41×

    Water quality class according to the hydrogeochemical map

    • class A28×
    • class B17×
    • class E2×
    • class F1×
    • class D1×

    Metals in groundwater

    • MercuryHghigh (top 5 %)
      highest 0.400 μg/lmedian 0.100 μg/l18 samples78 % below the limit of quantification

      Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 98 of all samples in Slovakia.

    • CopperCuhigh (top 5 %)
      highest 9.70 μg/lmedian 1.40 μg/l18 samples

      Highest value: studňa1993, 3.0 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • ArsenicAshigh (top 5 %)
      highest 5.90 μg/lmedian 0.500 μg/l18 samples67 % below the limit of quantification

      Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ChromiumCrhigh (top 5 %)
      highest 4.00 μg/lmedian 0.250 μg/l18 samples61 % below the limit of quantification

      Highest value: prameň1993, 1.2 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 0.700 μg/lmedian 0.200 μg/l18 samples39 % below the limit of quantification

      Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LithiumLielevated (top 10 %)
      highest 43.0 μg/lmedian 1.00 μg/l18 samples61 % below the limit of quantification

      Highest value: studňa1993, 3.0 km from the water. Comparison: percentile 93 of all samples in Slovakia.

    • AluminiumAlelevated (top 10 %)
      highest 0.0400 mg/lmedian 0.00500 mg/l18 samples56 % below the limit of quantification

      Highest value: studňa1993, 1.9 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • ZincZnslightly elevated
      highest 274 μg/lmedian 4.50 μg/l18 samples28 % below the limit of quantification

      Highest value: studňa1993, 2.3 km from the water. Comparison: percentile 81 of all samples in Slovakia.

    • LeadPbslightly elevated
      highest 1.00 μg/lmedian 0.500 μg/l18 samples67 % below the limit of quantification

      Highest value: prameň1992, 2.8 km from the water. Comparison: percentile 75 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l6 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l18 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l18 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 39 of all samples in Slovakia.

    Gold, mines and deposits

    Was gold panned and ore mined here? Gold and ore minerals in river sediments, old mine workings, deposits and ore occurrences
    Mine workings8

    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.

    • Pyrite (FeS₂)24 samples, at most 1815 grains
    • Barite (BaSO₄)21 samples, at most 315 grains
    • Hematite (Fe₂O₃)21 samples, at most 4115 grains
    • Magnetite (Fe₃O₄)21 samples, at most 555 grains
    • Rutil (TiO₂)20 samples, at most 555 grains
    • Limonite (FeO(OH)·nH₂O)18 samples, at most 815 grains
    • Anatas (TiO₂)7 samples, at most 5 grains
    • Monazit ((Ce,La,Nd)PO₄)4 samples, at most 5 grains
    • Ilmenit (FeTiO₃)3 samples, at most 315 grains

    Rock-forming and accessory minerals

    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))21 samples, at most 815 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)21 samples, at most 315 grains
    • Zirconium (ZrSiO₄)20 samples, at most 815 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)14 samples, at most 155 grains
    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)5 samples, at most 15 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)2 samples, at most 15 grains

    Mine workings, deposits and ore occurrences

    Old mine workings outside mining areas (Geofond register), deposits and mining areas, and the metallogenetic map. Gold, silver and other metals near streams can get into sediments and water.

    Types of mining objects

    • spoil heap4×
    • adit3×
    • pinge (mining subsidence pit), line of pinge pits1×

    Nearest old mine workings

    1. AditTypeaditMinedspecularite
      210 m
    2. Line of pinge pitsTypepinge (mining subsidence pit), line of pinge pitsMinedFe-Cu ores
      2.9 km
    3. AditTypeaditMinedFe-Cu ores
      2.9 km
    4. Spoil heapTypespoil heapMinedFe-Cu ores
      2.9 km
    5. Spoil heapTypespoil heapMinedFe-Cu ores
      2.9 km
    6. Spoil heapTypespoil heapMinedFe-Cu ores
      2.9 km
    7. AditTypeaditMinedFe-Cu ores
      3.0 km
    8. Spoil heapTypespoil heapMinedFe-Cu ores
      3.0 km

    Deposits and mining areas

    1. Spišské TomášovceMineralbuilding stoneStatus and organisationDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená
      1.1 km
    2. Spišské TomášovceMineralbuilding stoneStatus and organisationDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená
      1.1 km
    3. Mlynky – Biele VodyMineralgypsumStatus and organisationDeposit with expected use of reserves – ŠGÚDŠ Bratislava
      3.5 km
    4. Mlynky – Biele VodyMineralanhydriteStatus and organisationDeposit with expected use of reserves – ŠGÚDŠ Bratislava
      3.5 km
    5. Spišská Nová VesMineralcopper oresStatus and organisationDeposit with halted mining or where use of reserves is not expected – Ludovika Energy s.r.o.
      4.1 km
    6. Spišská Nová VesMineraluranium oresStatus and organisationDeposit with halted mining or where use of reserves is not expected – Ludovika Energy s.r.o.
      4.1 km
    7. Spišská Nová VesMineraluranium oresStatus and organisationDeposit with halted mining or where use of reserves is not expected – Ludovika Energy, s. r. o.
      4.1 km
    8. Spišská Nová VesMineralcopper oresStatus and organisationDeposit with halted mining or where use of reserves is not expected – Ludovika Energy s.r.o.
      4.1 km
    9. Smižany – Spišská Nová VesMineralbrick raw materialsStatus and organisationDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená
      4.1 km
    10. Smižany – Spišská Nová VesMineralbrick raw materialsStatus and organisationDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená
      4.1 km
    11. Spišská Nová VesMineraluranium oresStatus and organisationDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená
      4.1 km
    12. Spišská Nová VesMineralcopper oresStatus and organisationDeposit with halted mining or where use of reserves is not expected – Organizácia neurčená
      4.1 km

    Ore occurrences in the metallogenic map

    1. Spišská Nová Ves-Novoveská Huta, žily Rybník a Medvedia hlavaOre typeCopper oresMetalsCu, UTypedeposit occurrence
      2.4 km
    2. Spišská Nová Ves, žila HaniskováOre typeCopper oresMetalsCu, FeTypedeposit occurrence
      3.0 km
    3. Spišská Nová Ves – HaniskováOre typeCopper oresMetalsCu, MoTypedeposit occurrence
      3.0 km
    4. Spišská Nová Ves, Strážanský kopec a Malý MuráňOre typeCopper oresMetalsCu, UTypemineralogical occurrence
      3.5 km
    5. Spišská Nová Ves – Novoveská HutaOre typeCopper oresMetalsCu, MoTypesmall deposit
      3.9 km
    6. Hnilec, žila Michal-JozefOre typeComplex iron oresMetalsCuTypemineralogical occurrence
      4.0 km
    7. Spišská Nová Ves – Novoveská HutaOre typeUranium-molybdenum oresMetalsMo, UTypemedium deposit
      4.0 km
    8. Spišská Nová Ves, MuráňOre typeUranium-molybdenum oresMetalsMo, U, CuTypesmall deposit
      4.1 km
    9. Hnilec, žilník Kráľov vrchOre typeComplex iron oresMetalsCuTypemineralogical occurrence
      4.2 km
    10. Hnilec, žily Amália, Jozef and SamuelOre typeComplex iron oresMetalsFe, CuTypemineralogical occurrence
      4.2 km

    Geothermal energy, mineral waters and boreholes

    Is there heat underground? Geothermal potential, geothermal boreholes by temperature, mineral springs and the borehole archive
    Hottest borehole31 °CBoreholes84

    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 km30 °C45 °C

    Rock temperature with depth

    30 / 45 °Cat depths of 1,000 and 2,000 m

    increase of 15 °C per km

    The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 60 mW/m².

    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.

    Geothermal boreholes by water temperature

    1. Arnutovce – HKJ-3Yield11.8 l/sDepth1133 mChemical water typeCa-Mg-HCO3UseunusedFrom the water4.4 km
      31 °C
    2. Letanovce – HKJ-4Yield8.0 l/sDepth607 mChemical water typeCa-Mg-HCO3UseunusedFrom the water5.0 km
      25 °C

    Sources of geothermal and mineral waters

    1. HKJ-3Typegeothermal waterWater temperature (°C)22 – 38Yield (l/s)5 – 15Count1
      4.8 km
    2. category a1Typemineral waterWater temperature (°C)< 15Yield (l/s)< 5Count4
      6.8 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.

    84 boreholes in the 3 km zone, of which 19 hydrogeological and 65 other; with an archive report number 84.

    Borehole depths

    • up to 10 m44×
    • 10–30 m5×
    • 30–100 m6×
    • 100–300 m13×
    • over 300 m15×

    Nearest boreholes

    1. ČingovTypewide-diameter boreholeArchive report63125 113Bb34.pdf
      390 m
    2. Čingov-Sp.TomášovceTypewide-diameter boreholeDepth10.0 mArchive report59343 113Bb30.pdf
      500 m
    3. V-SPH-13/87TypehydrogeologicalDepth300.0 mArchive report76784
      1.1 km
    4. R-157Typeengineering-geologicalDepth7.0 mArchive report80782
      1.2 km
    5. Čingov-Sp.TomášovceTypenarrow-diameter borehole with ordinary drinking and process waterDepth149.0 mArchive report21935 113Bb10.pdf
      1.4 km
    6. R-137Typeengineering-geologicalDepth15.0 mArchive report80782
      1.4 km
    7. ČingovTypenarrow-diameter borehole with ordinary drinking and process waterDepth32.0 mArchive report22611 113Bb1.pdf
      1.4 km
    8. V-SPH-14/86TypehydrogeologicalDepth375.0 mArchive report76784
      1.6 km
    9. S-6Typeengineering-geologicalDepth4.4 mArchive report85552
      1.8 km
    10. S-4Typeengineering-geologicalDepth4.5 mArchive report85552
      1.8 km
    11. S-5Typeengineering-geologicalDepth4.5 mArchive report85552
      1.8 km
    12. SmižanyTypestructural borehole with ordinary waterDepth1,902.8 mArchive report22558 114Aa2.pdf
      1.8 km

    Natural radioactivity and radon

    How much does the ground radiate here? Gamma radiation of rocks, radon in soil and radon in waters

    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 47 to 58 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.

    • Equivalent thorium (eTh)eTh8.38 ppm75th percentile
    • Equivalent uranium (eU)eU2.60 ppm55th percentile
    • Potassium (K)K1.30 %percentile 50

    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 137CsCS1373,355 Bq/m²percentile 90

    Radon risk by isopleths

    • low50%SR 36 %
    • medium50%SR 64 %

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

    Radon in waters

    Radiohydrochemical sampling of springs, wells and watercourses: radon activity concentration in water. The bar shows the highest measured value for each kind of site.

    • developed spring21.6 Bq/l · median 10.8 Bq/l · 4 samples
    • source10.1 Bq/l · median 2.90 Bq/l · 5 samples
    • water source for public supply2.54 Bq/l · median 2.54 Bq/l · 1 sample
    • stream, river2.12 Bq/l · median 1.22 Bq/l · 2 samples

    Environmental burdens, landfills and landslides

    What in the surroundings can harm the water? Environmental burdens, waste landfills, anthropogenic sediments and slope deformations
    Burdens and landfills1

    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

    1. Spišské TomášovceArea250 m²Year established1989Monitoring–
      2.0 km