Fishing conditions score, the best window of the day and fishing districts from the best conditions Low activity · average of one fishing district 06:00–08:00 Tovarský potok, window score 27. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 05:04. 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 2017 to 2023: 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 0 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 Váh 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 (20 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. River alluvium100% of the water line Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000. pH 8.3modelled estimate water type Ca–HCO₃ Mineralisation 410 mg/l, moderately hard water (14.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Nickel 29.5 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 69. Interpolation of the Geochemical Atlas of river sediments. 35°C at 1,000 m depth heat flow 64 mW/m² At a depth of 2,000 m about 55 °C (increase of 20 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 40nGy/h dose rate percentile 5 in Slovakia Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ. 1object within 3 km Nearest: Halda Tunežice (spoil heap), 2.9 km from the water. 0samples with gold 10 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. 4 from 10indicators in the top 5 % highest: Lead 10.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (Zapotok, potok). 253boreholes within 3 km 472 water analyses nearby Of these, 253 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. 21°C at the wellhead 4 geothermal boreholes within 10 km Warmest: Belušské Slatiny – BS-1, 6.6 km from the water. 13sites within 3 km 13 landfills No environmental burden is registered within 3 km; landfills are only recorded. 22records within 5 km 12 deposits, 10 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 130areas within 3 km 10 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 River alluvium: Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. 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 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 3 of 7 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 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 8.34typical 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. 14.0°dH, moderately hard Sum of calcium and magnesium (2.50 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 410mg/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 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. 40nGy/h in air range 27 to 46 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. -4nT range -11 to 5 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. -44mGal residual −5.9 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. 35 / 55 °Cat depths of 1,000 and 2,000 m increase of 20 °C per km The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 64 mW/m². 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: Zapotok, potok1995, 40 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: Tovarský, potok, 110 m from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: Tovarský, potok1995, 80 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: Červený Kameň, 1450 m JZ od K635 Zavlacne1995, 540 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: Červený Kameň, 1450 m JZ od K635 Zavlacne, 540 m from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: Tovarský, potok, 110 m from the water. Comparison: percentile 81 of all samples in Slovakia. Highest value: Mikušovce, 1200 m SV od K470 Kalvária1995, 70 m from the water. Comparison: percentile 73 of all samples in Slovakia. Highest value: Tovarský, potok, 110 m from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: Dulov, 1500 m JJZ od K2651995, 110 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Dulov, 1500 m JJZ od K2651995, 110 m from the water. Comparison: percentile 37 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Tovarský, potok, 110 m from the water. Comparison: percentile 86 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: studňa1993, 2.1 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1993, 1.0 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1993, 780 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: prameň1993, 110 m from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1993, 200 m from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: studňa1993, 910 m from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: vrt1993, 2.5 km from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: studňa1993, 1.0 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: vrt1993, 2.5 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. 253 boreholes in the 3 km zone, of which 73 hydrogeological and 180 other; with an archive report number 253. 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 Váh basin
By the water now
Today on the Tovarský potok 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 Tuchyňa 35 cm – Elevation profile of the watercourse
Terrain in 3D
Historical images



Water pollution on the Tovarský potok watercourse
Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025
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 (3)
Geology and geochemistry of the Tovarský potok 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 Quaternary Holocene fluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains 3× Quaternary cover
Tectonic units
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
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
81.7 mg/lpercentile 71251 mg/lpercentile 630.112 mg/lpercentile 4938.1 mg/lpercentile 476.50 mg/lpercentile 3711.2 mg/lpercentile 362.01 mg/lpercentile 324.09 mg/lpercentile 28Nutrients and organic pollution
0.279 mg/lpercentile 760.0867 mg/lpercentile 404.86 mg/lpercentile 362.09 mg/lpercentile 22Metals
7.77 μg/lpercentile 5680.0 μg/lpercentile 5523.5 μg/lpercentile 430.0760 mg/lpercentile 37Elements in river sediments
Potentially toxic and trace elements
29.5 mg/kgpercentile 690.330 mg/kgpercentile 6828.1 mg/kgpercentile 669.50 mg/kgpercentile 66105 mg/kgpercentile 5867.7 mg/kgpercentile 4970.4 mg/kgpercentile 4714.9 mg/kgpercentile 462.44 mg/kgpercentile 410.188 mg/kgpercentile 380.0690 mg/kgpercentile 285.05 mg/kgpercentile 260.0989 mg/kgpercentile 250.343 mg/kgpercentile 160.136 mg/kgpercentile 7Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
5.12 %percentile 81817 mg/kgpercentile 462.52 %percentile 400.794 %percentile 405.32 %percentile 39668 mg/kgpercentile 283,796 mg/kgpercentile 240.686 %percentile 161.18 %percentile 9Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
74.3 mg/kgpercentile 82167 mg/kgpercentile 7416.7 mg/kgpercentile 7334.4 mg/kgpercentile 7389.8 mg/kgpercentile 541.00 mg/kgpercentile 28360 mg/kgpercentile 21283 mg/kgpercentile 1819.8 mg/kgpercentile 1547.4 mg/kgpercentile 13Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.17 %percentile 185.92 ppm9th percentile1.64 ppm4th percentile1,720 Bq/m²percentile 60Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Rock temperature with depth
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
Rock-forming and accessory minerals
Groundwater: chemistry, water types and radioactivity
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median well 8 22,1 Bq/l 12.2 Bq/l source 6 19,6 Bq/l 12.0 Bq/l developed spring 5 25,3 Bq/l 16.3 Bq/l water source for public supply 2 23,9 Bq/l 13.4 Bq/l Mine workings, deposits and ore occurrences
Types of mining objects
Nearest old mine workings
Name Type Mined Ended From the water Halda Tunežice spoil heap building stone 2.9 km Deposits and mining areas
Deposit Mineral Status and organisation From the water Dulov – Dolné Prúdy gravelly sands and sands Mined deposit – AGROFARMA, spol. s r.o. Červený Kameň 1.7 km Horovce gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – ZEMPRA, s.r.o. 2.2 km Tunežice building stone Mined deposit – PK Metrostav, a.s. 3.0 km Tunežice building stone Mined deposit – PK Metrostav, a.s. 3.0 km Ilava brick raw materials Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 3.1 km Ilava brick raw materials Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 3.1 km Pruské – Kúty gravelly sands and sands Mined deposit – INFINITY TRUST, s.r.o. 3.4 km Lednické Rovne – Sigoť gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – SESTAV, s.r.o. 4.1 km Krivoklát limestone, other Deposit with expected use of reserves – ŠGÚDŠ Bratislava 4.3 km Krivoklát calcareous marl Deposit with expected use of reserves – ŠGÚDŠ Bratislava 4.3 km Za Váh II gravelly sands and sands Mined deposit – SESTAV s.r.o. 4.7 km Za Váh gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – SESTAV s.r.o. 4.8 km Ore occurrences in the metallogenic map
Occurrence Ore type Metals Type From the water Lednické Rovne Manganese ores Mn mineralogical occurrence 4.0 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Červený Kameň narrow-diameter borehole with ordinary drinking and process water 8.0 m 21014 97Cb2.pdf20 m S-9 engineering-geological 5.0 m 1192020 m S-12 engineering-geological 2.5 m 1192030 m T-6 hydrogeological 10.0 m 6680640 m S-10 engineering-geological 5.0 m 1192040 m Tuchyňa II. narrow-diameter borehole with ordinary drinking and process water 11.0 m 66806 97Cd30.pdf60 m Červený Kameň narrow-diameter borehole with ordinary drinking and process water 14.4 m 88899 97Cd47.pdf60 m Mikušovce narrow-diameter borehole with ordinary drinking and process water 12.0 m 74629 97Cd41.pdf60 m HVT-4 hydrogeological 11.0 m 6680660 m T-5 hydrogeological 10.0 m 6680660 m V-1 engineering-geological 6.0 m 9943460 m S-1 engineering-geological 8.0 m 1192060 m Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Belušské Slatiny – BS-1 21 °C – 58.5 m Ca-HCO3-(SO4) unused 6.6 km Belušské Slatiny – BHS-2 20 °C – 501 m Ca-Na-HCO3-SO4 unused 6.7 km Belušské Slatiny – BHS-1 21 °C – 226 m Ca-Na-HCO3-SO4 unused 6.7 km Belušské Slatiny – BHS-3 21 °C 0.0 l/s 1671 m Ca-Na-HCO3-SO4 unused 6.9 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 4 3.7 km category b1 mineral water 15-22 < 5 3 6.7 km category b2 mineral water 15-22 5-15 1 6.8 km category Belušské Slatiny thermal baths – – 1 8.0 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Mikušovce – Nad obcou – Mikušovce pri Pruskom – 1975 – 60 m Červený Kameň – nad cintorínom. – Červený Kameň – 1975 – 330 m Tuchyňa – Šustínsky járok – Tuchyňa – 1975 – 340 m Mikušovce – osada Babinec – Mikušovce pri Pruskom – 1985 – 380 m Dúlov – Nad obcou – Dulov – 1970 – 860 m Dulov – Pri Váh – Dulov – 1970 – 1.2 km Pruské – Nad Kamenicami – Pruské – 1975 – 1.6 km Nad cintorínom – Kvašov – 1975 – 1.7 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
20from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
LeadPbhigh (top 5 %)
highest 10.0 μg/lmedian 2.50 μg/l10 samples80 % below the limit of quantification
StrontiumSrhigh (top 5 %)
highest 1,010 μg/lmedian 460 μg/l10 samples
ChromiumCrhigh (top 5 %)
highest 6.50 μg/lmedian 1.85 μg/l10 samples20 % below the limit of quantification
BariumBahigh (top 5 %)
highest 130 μg/lmedian 88.0 μg/l7 samples
CadmiumCdelevated (top 10 %)
highest 0.600 μg/lmedian 0.150 μg/l10 samples80 % below the limit of quantification
LithiumLislightly elevated
highest 17.0 μg/lmedian 5.00 μg/l10 samples90 % below the limit of quantification
CopperCutypical value
highest 2.30 μg/lmedian 1.40 μg/l10 samples40 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.760 μg/lmedian 0.500 μg/l10 samples80 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification
AntimonySbbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification
Silicon dioxideSiO2slightly elevated
highest 27.7 mg/lmedian 6.72 mg/l10 samples
CopperCuextreme (top 1 %)
highest 24.5 μg/lmedian 0.850 μg/l38 samples
ZincZnextreme (top 1 %)
highest 4,925 μg/lmedian 19.5 μg/l38 samples
CadmiumCdextreme (top 1 %)
highest 1.90 μg/lmedian 0.250 μg/l38 samples95 % below the limit of quantification
LithiumLihigh (top 5 %)
highest 112 μg/lmedian 12.0 μg/l38 samples
AluminiumAlhigh (top 5 %)
highest 0.130 mg/lmedian 0.0100 mg/l38 samples39 % below the limit of quantification
SeleniumSehigh (top 5 %)
highest 3.00 μg/lmedian 0.500 μg/l38 samples89 % below the limit of quantification
MercuryHghigh (top 5 %)
highest 0.200 μg/lmedian 0.100 μg/l38 samples97 % below the limit of quantification
ChromiumCrelevated (top 10 %)
highest 3.10 μg/lmedian 0.250 μg/l38 samples79 % below the limit of quantification
AntimonySbelevated (top 10 %)
highest 0.500 μg/lmedian 0.100 μg/l38 samples97 % below the limit of quantification
ArsenicAselevated (top 10 %)
highest 2.60 μg/lmedian 0.500 μg/l38 samples92 % below the limit of quantification
LeadPbelevated (top 10 %)
highest 2.00 μg/lmedian 0.500 μg/l38 samples76 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l17 samples100 % below the limit of quantification



