Fishing conditions score, the best window of the day and fishing districts from the best conditions Average activity · average of one fishing district 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. 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 Move the map with two fingers. In full-screen mode one finger is enough. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. For each fishing district you can see what it is made of, how well it is supported by data and where the data comes from. Measurement of water level, temperature and flow, weather by the watercourse and status from satellites 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. Source: Open Topo Data (eudem25m), 4 Nov 2026. Gradient and fall are approximate and include only the sections of fishing districts. Loading the 3D terrain model… 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. 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 quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby 1 of 1 fishing districts on the watercourse with SHMÚ data: the nearest site has an unmet standard in at least one indicator. 0 of 1 fishing district with measurements has groundwater nearby with a value above the limit for at least one indicator. Water pollution in the Poprad basinPolluted water in Slovakia 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. 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. 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. 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. 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. 35°C at 1,000 m depth heat flow 65 mW/m² Atlas of Geothermal Energy of Slovakia. 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. 0objects within 3 km No old mine working is recorded within 3 km of the water. 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. 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). 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. 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. 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. 10records within 5 km 2 deposits, 8 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 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. 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. 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. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia The map covers 1 of 5 points on the water line. 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. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia 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. 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. 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. 174mg/l mineralisation Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds. Water type by dominant ions: Ca–HCO₃–SO₄ Shares are in equivalents, the usual way of comparing the composition of waters. 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) 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. 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) 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. 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. 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. 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) marker on the bar: share among all sample points on streams in Slovakia 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. +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. -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. 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. marker on the bar: share among all sample points on streams in Slovakia 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. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off. 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. 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. Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 94 of all samples in Slovakia. Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné, 730 m from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 88 of all samples in Slovakia. Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 78 of all samples in Slovakia. Highest value: Nová Lesná, Veľký Slavkov, bezmenný prítok Popradu1997, 740 m from the water. Comparison: percentile 77 of all samples in Slovakia. Highest value: Matejovce, 400 m JJZ od K679 Zadné Rovné1997, 730 m from the water. Comparison: percentile 66 of all samples in Slovakia. Highest value: Nová Lesná, Veľký Slavkov, bezmenný prítok Popradu1997, 740 m from the water. Comparison: percentile 49 of all samples in Slovakia. Highest value: Veľký Slavkov, 1400 m SV od K7061997, 40 m from the water. Comparison: percentile 46 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Nová Lesná, Veľký Slavkov, bezmenný prítok Popradu1997, 740 m from the water. Comparison: percentile 82 of all samples in Slovakia. 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. 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. Highest value: drén1994, 1.4 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: drén1994, 30 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1992, 2.4 km from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: studňa1992, 1.8 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: drén1994, 30 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1994, 90 m from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: studňa1992, 1.8 km from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: drenáž1992, 2.8 km from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: prameň1992, 2.1 km from the water. Comparison: percentile 88 of all samples in Slovakia. Highest value: prameň1992, 100 m from the water. Comparison: percentile 84 of all samples in Slovakia. Highest value: prameň1992, 2.8 km from the water. Comparison: percentile 50 of all samples in Slovakia. 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. 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. 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. 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. Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. Who manages the fishing districts and where they are Bodrog basin and Hornád
By the water now
Today on the Slavkovský potok (Poprad) watercourse
Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the watercourse
Water state on the watercourse
Water levels on the watercourse
Station Status Change Temperature Brezovica 8 cm – Poprad – Matejovce 70 cm – Elevation profile of the watercourse
Terrain in 3D
Historical images



Water pollution on the Slavkovský potok (Poprad) watercourse
Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025
Most polluted fishing districtsall with an unmet standard
Groundwater: measured valuestypical value from stations within 10 km, 2025
Watercourse profile from source to mouthnumber of unmet indicators in 2025 at SHMÚ sites
Show sites in the table (2)
Geology and geochemistry of the Slavkovský potok (Poprad) stream
Rock under the water
Water according to the atlas
Elements in river sediment
Heat underfoot
Natural gamma radiation
Old mine workings
Gold in river sediment
Trace elements in the stream water
Boreholes and groundwater analyses
Geothermal energy
Environmental burdens and landfills
Deposits and ore occurrences
Landslides and slope deformations
Geological structure beneath the water
Geological age of the rocks
Most common rock units
System Age Unit Points Paleogene Eocene – Oligocene Zuberec Formation 1× Quaternary cover
Tectonic division
Neotectonic units
Direction of neotectonic movements
Regional geological division
Regional geological division (subunits)
Engineering-geological districts
Engineering-geological formations
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Aquifer rocks (hydrogeological map 1:200,000)
Aquifer type
Main hydrogeological region
Geothermal groundwater bodies
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
12.5 mg/lpercentile 580.0995 mg/lpercentile 4231.4 mg/lpercentile 366.23 mg/lpercentile 356.96 mg/lpercentile 2029.8 mg/lpercentile 191.23 mg/lpercentile 1578.0 mg/lpercentile 13Nutrients and organic pollution
0.160 mg/lpercentile 623.56 mg/lpercentile 580.171 mg/lpercentile 566.31 mg/lpercentile 50Metals
0.434 mg/lpercentile 90262 μg/lpercentile 8673.6 μg/lpercentile 736.86 μg/lpercentile 51Elements in river sediments
Potentially toxic and trace elements
3.53 mg/kgpercentile 8836.5 mg/kgpercentile 840.341 mg/kgpercentile 790.337 mg/kgpercentile 750.197 mg/kgpercentile 7420.3 mg/kgpercentile 71114 mg/kgpercentile 650.422 mg/kgpercentile 580.270 mg/kgpercentile 552.60 mg/kgpercentile 4820.1 mg/kgpercentile 345.26 mg/kgpercentile 3058.8 mg/kgpercentile 2652.0 mg/kgpercentile 195.99 mg/kgpercentile 15Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1.63 %percentile 966.85 %percentile 831,225 mg/kgpercentile 801,137 mg/kgpercentile 791.58 %percentile 611.78 %percentile 422.50 %percentile 390.742 %percentile 323,735 mg/kgpercentile 22Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
301 mg/kgpercentile 95106 mg/kgpercentile 95106 mg/kgpercentile 9543.7 mg/kgpercentile 92658 mg/kgpercentile 9016.8 mg/kgpercentile 731.58 mg/kgpercentile 6088.5 mg/kgpercentile 5026.3 mg/kgpercentile 43361 mg/kgpercentile 35Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.52 %percentile 857.13 ppm41th percentile2.11 ppm11th percentile1,362 Bq/m²percentile 42Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Geothermal groundwater bodies beneath the water line
Relief, climate and soils
Geomorphological units
Geomorphological regions
Climatic-geographical types
Susceptibility of soils to acidification
Soil contamination (map 1:500,000)
Lithogeochemical types
Map of the corridor
Trace elements in surface waters
Major ions, mineralisation and pH
Gold and ore minerals in river sediments
Nearest samples with gold
Sample Gold in sample From the water 5187 1 grain 30 m 5181 1 grain 580 m Rock-forming and accessory minerals
Groundwater: chemistry, water types and radioactivity
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median free-flowing borehole with thermal and mineral water 1 1,49 Bq/l 1.49 Bq/l source 8 19,3 Bq/l 7.13 Bq/l well 5 9,79 Bq/l 3.20 Bq/l stream, river 3 1,58 Bq/l 0.390 Bq/l free-flowing borehole 1 42,7 Bq/l 42.7 Bq/l Mine workings, deposits and ore occurrences
Deposits and mining areas
Deposit Mineral Status and organisation From the water Gerlachov – Juh gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – Poľnohospodárske družstvo TATRAN 1.0 km Veľká Lomnica I gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – RIVERSAND a. s. 4.4 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water J 48 engineering-geological 10.0 m 7953540 m J 162 engineering-geological 10.0 m 7953590 m J 49 engineering-geological 10.0 m 7953590 m J 53 engineering-geological 10.0 m 79535100 m J 54 engineering-geological 10.0 m 79535170 m J 51 engineering-geological 10.0 m 79535190 m Veľký Slavkov wide-diameter borehole 17.0 m 64513 101Da14.pdf240 m V-5 engineering-geological 6.0 m 87239260 m V-3 engineering-geological 6.0 m 87239270 m V-4 engineering-geological 6.0 m 87239300 m V-2 engineering-geological 6.0 m 87239310 m V-1 engineering-geological 6.0 m 87239340 m Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Veľký Slavkov – VSČ-1 57 °C – 2400 m Ca-Mg-HCO3 unused 900 m Poprad – PP-1 48 °C 61.2 l/s 1205 m Ca-Mg-SO4-HCO3 in use 2.3 km Stará Lesná – FGP-1 58 °C 22.0 l/s 3616 m Ca-Mg-HCO3 unused 4.4 km Gánovce – GA-1A 27 °C 1.9 l/s 276 m Ca-Mg-HCO3-SO4 in use without data reporting 5.6 km Gánovce – GA-1 23 °C 2.8 l/s 50 m Ca-Mg-HCO3-SO4 unused 5.6 km Gánovce – ŠHG-1 26 °C 3.0 l/s 150 m Ca-Mg-HCO3-SO4 unused 5.9 km Gánovce – ŠHG-2 25 °C 2.5 l/s 110 m Ca-Mg-HCO3-SO4 unused 6.0 km Veľká Lomnica – GVL-1 62 °C 54.9 l/s 2100 m Ca-Mg-HCO3-SO4 in use 6.0 km Vrbov – Vr-2 59 °C 33.0 l/s 2502 m Ca-Mg-HCO3-SO4 in use 6.5 km Vrbov – Vr-1 56 °C 28.3 l/s 1742 m Ca-Mg-HCO3-SO4 in use 6.7 km Sources of geothermal and mineral waters
Source Type Water temperature (°C) Yield (l/s) Count Nearest from water category a1 mineral water < 15 < 5 18 510 m PP-1 geothermal water 38 – 55 31 – 50 1 1.8 km category Stará Lesná thermal baths – – 1 4.0 km FGP-1 geothermal water 55 – 80 16 – 30 1 5.0 km Vr-1.2 geothermal water 55 – 80 16 – 30 1 6.5 km category Vrbov thermal baths – – 1 6.5 km category c1 mineral water 23-38 < 5 3 6.8 km category b1 mineral water 15-22 < 5 6 6.9 km category c2 mineral water 23-38 5-15 1 7.0 km category b2 mineral water 15-22 5-15 1 8.2 km Environmental burdens, landfills and anthropogenic sediments
Environmental burdens
Site Activity Substance Classification From the water Veľký Slavkov – landfill Pod farmou SK1001000P 1.3 km High Tatras – skládka Pod lesom SK1001000P 1.7 km Poprad – ČS PHM – areál SAD SK1001000P 2.5 km Poprad – ŽSR – station SK1001000P 2.5 km Waste landfills
Landfill Area Year established Monitoring From the water Veľký Slavkov – landfill Pod farmou – Veľký Slavkov – 1950 monitored 100 m Veľký Slavkov – pri salaši – Veľký Slavkov 300 m² 1960 – 110 m Matejovce – Starý mlyn – Matejovce 100 m² 1960 – 130 m Veľký Slavkov 750 m² 1975 – 140 m Veľký Slavkov 500 m² 1988 – 500 m Matejovce – 1988 monitored 720 m Veľký Slavkov 20 531 m² 1982 monitored 1.3 km Gerlachov – pri pieskovni. – Gerlachov pod Tatrami – 1980 – 1.4 km Landslides and slope deformations
Types of deformations
Degree of activity
Current state
How to read these data
Organizations and location
Organizations on the watercoursewho manages the fishing districts and what the conditions are there today
More watercourses nearby
43from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
CopperCuhigh (top 5 %)
highest 14.4 μg/lmedian 1.60 μg/l5 samples
StrontiumSrelevated (top 10 %)
highest 604 μg/lmedian 135 μg/l7 samples
CadmiumCdelevated (top 10 %)
highest 0.500 μg/lmedian 0.150 μg/l5 samples80 % below the limit of quantification
LeadPbslightly elevated
highest 3.50 μg/lmedian 2.50 μg/l5 samples80 % below the limit of quantification
LithiumLislightly elevated
highest 13.0 μg/lmedian 5.00 μg/l7 samples86 % below the limit of quantification
AntimonySbslightly elevated
highest 0.650 μg/lmedian 0.500 μg/l7 samples86 % below the limit of quantification
ChromiumCrtypical value
highest 1.20 μg/lmedian 1.00 μg/l5 samples80 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.960 μg/lmedian 0.500 μg/l7 samples71 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l5 samples100 % below the limit of quantification
Silicon dioxideSiO2slightly elevated
highest 24.5 mg/lmedian 18.5 mg/l7 samples
MercuryHgextreme (top 1 %)
highest 1.00 μg/lmedian 0.100 μg/l29 samples72 % below the limit of quantification
AluminiumAlextreme (top 1 %)
highest 0.340 mg/lmedian 0.0100 mg/l29 samples41 % below the limit of quantification
LeadPbhigh (top 5 %)
highest 6.00 μg/lmedian 0.500 μg/l29 samples52 % below the limit of quantification
AntimonySbhigh (top 5 %)
highest 1.40 μg/lmedian 0.100 μg/l29 samples62 % below the limit of quantification
ZincZnhigh (top 5 %)
highest 1,324 μg/lmedian 13.0 μg/l29 samples34 % below the limit of quantification
CadmiumCdhigh (top 5 %)
highest 0.500 μg/lmedian 0.250 μg/l29 samples93 % below the limit of quantification
LithiumLielevated (top 10 %)
highest 43.0 μg/lmedian 18.0 μg/l29 samples10 % below the limit of quantification
SeleniumSeelevated (top 10 %)
highest 2.10 μg/lmedian 0.500 μg/l29 samples83 % below the limit of quantification
ChromiumCrelevated (top 10 %)
highest 2.80 μg/lmedian 0.500 μg/l29 samples34 % below the limit of quantification
ArsenicAsslightly elevated
highest 2.00 μg/lmedian 0.500 μg/l29 samples93 % below the limit of quantification
CopperCuslightly elevated
highest 3.00 μg/lmedian 0.600 μg/l29 samples
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l5 samples100 % below the limit of quantification



