Fishing conditions score, the best window of the day and fishing districts from the best conditions Low activity · average of 2 fishing districts 15:00–17:00 Klátovské rameno č. 1, window score 32. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 04:04. 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. Very slow watercourse A lowland, almost stagnant section: calm, often more turbid water; the bottom tends to be muddy and sandy. Typical of carp fishing districts. 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 2 of the watercourse's fishing districts with SHMÚ data have an unmet standard at the nearest site in at least one indicator. 2 of 2 fishing districts with measurements have groundwater nearby with a value above the limit for at least one indicator. Water pollution in the Little Danube basin and on Žitný ostrov (Rye Island)Polluted 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 (30 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 8.1modelled estimate water type Ca–Mg–HCO₃–SO₄ Mineralisation 520 mg/l, hard water (18.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 1 from 15elements in the top 10 % highest: Selenium 0.949 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 95. Interpolation of the Geochemical Atlas of river sediments. 52°C at 1,000 m depth heat flow 85 mW/m² At a depth of 2,000 m about 94 °C (increase of 42 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 49nGy/h dose rate percentile 35 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. 0samples with gold 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. 1 from 10indicators in the top 5 % highest: Lithium 68.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 97 (bez mena, Starý Klátovský kanál a Klátovský kanál – sútok). 275boreholes within 3 km 724 water analyses nearby Of these, 275 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. 91°C at the wellhead 5 geothermal boreholes within 10 km Warmest: Dunajská Streda – DS-1, yield 15.2 l/s, 7.5 km from the water. 10sites within 3 km 10 landfills No environmental burden is registered within 3 km; landfills are only recorded. 10records within 5 km 7 deposits, 3 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 0areas within 3 km 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 The map covers 3 of 10 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 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 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 8.09typical range Most rivers and streams in Slovakia have a pH of 6.5 to 8.5. More acidic water is found in streams on acidic rocks (granites, quartzites), more alkaline water near limestones. 18.0°dH, hard Sum of calcium and magnesium (3.21 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 520mg/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–Mg–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. 49nGy/h in air 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. +51nT range 22 to 83 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. -18mGal residual −7.0 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. 52 / 94 °Cat depths of 1,000 and 2,000 m increase of 42 °C per km The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 85 mW/m². 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: bez mena, Starý Klátovský kanál a Klátovský kanál – sútok2011, 920 m from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: KLÁTOVSKÉ RAMENO1995, 30 m from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: Malý Dunaj1997, 930 m from the water. Comparison: percentile 76 of all samples in Slovakia. Highest value: Malý Dunaj1997, 930 m from the water. Comparison: percentile 72 of all samples in Slovakia. Highest value: bez mena, Starý Klátovský kanál a Klátovský kanál – sútok2011, 920 m from the water. Comparison: percentile 66 of all samples in Slovakia. Highest value: Klátovský kanál2011, 510 m from the water. Comparison: percentile 57 of all samples in Slovakia. Highest value: Klátovské rameno2011, 60 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Klátovské rameno2011, 60 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Klátovské rameno2011, 60 m from the water. Comparison: percentile 32 of all samples in Slovakia. Highest value: Klátovské rameno, 60 m from the water. Comparison: percentile 26 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Klátovské rameno2011, 150 m from the water. Comparison: percentile 49 of all samples in Slovakia. 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: studňa1994, 2.5 km from the water. Comparison: percentile 100 of all samples in Slovakia. Highest value: vrt1993, 1.3 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1994, 660 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1993, 2.8 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1994, 690 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: vrt1993, 180 m from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: studňa1994, 2.5 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1994, 2.5 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1993, 1.5 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1994, 2.7 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: vrt1994, 3.0 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. 275 boreholes in the 3 km zone, of which 77 hydrogeological and 198 other; with an archive report number 275. 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. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. Who manages the fishing districts and where they are Danube basin
By the water now
Today on the Klátovské rameno 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 Trhová Hradská 68 cm 6.6 °C Elevation profile of the watercourse
Terrain in 3D
Historical images



Water pollution on the Klátovské rameno 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 (2)
Geology and geochemistry of the Klátovské rameno 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: resedimented alluvial fine-grained sands 1× Quaternary Holocene fluvial-organic sediments: fine-sandy, clay-like to rot-foot humus clays of dead arms and marshes 1× Quaternary Holocene fluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains 1× Quaternary cover
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
Type of permeability (basic hydrogeological map 1:50,000)
Hydrogeological function
Main hydrogeological region
Genetic type of groundwater
Chemical type of groundwater
Groundwater quality class
Geothermal groundwater bodies
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
85.4 mg/lpercentile 8433.3 mg/lpercentile 8288.5 mg/lpercentile 7824.3 mg/lpercentile 7615.1 mg/lpercentile 71247 mg/lpercentile 620.129 mg/lpercentile 572.92 mg/lpercentile 49Nutrients and organic pollution
12.8 mg/lpercentile 810.251 mg/lpercentile 640.0984 mg/lpercentile 462.18 mg/lpercentile 24Metals
12.8 μg/lpercentile 730.163 mg/lpercentile 6942.8 μg/lpercentile 5846.7 μg/lpercentile 41Elements in river sediments
Potentially toxic and trace elements
0.949 mg/kgpercentile 95182 mg/kgpercentile 870.403 mg/kgpercentile 800.245 mg/kgpercentile 7922.7 mg/kgpercentile 770.300 mg/kgpercentile 7330.2 mg/kgpercentile 718.69 mg/kgpercentile 702.66 mg/kgpercentile 508.35 mg/kgpercentile 4823.6 mg/kgpercentile 450.320 mg/kgpercentile 380.508 mg/kgpercentile 3658.2 mg/kgpercentile 2552.0 mg/kgpercentile 19Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
2.56 %percentile 938.47 %percentile 921,170 mg/kgpercentile 822.44 %percentile 350.760 %percentile 281.34 %percentile 244.76 %percentile 18580 mg/kgpercentile 153,036 mg/kgpercentile 7Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
207 mg/kgpercentile 8926.8 mg/kgpercentile 3411.8 mg/kgpercentile 32376 mg/kgpercentile 2676.9 mg/kgpercentile 2249.2 mg/kgpercentile 220.603 mg/kgpercentile 1045.1 mg/kgpercentile 1016.3 mg/kgpercentile 7164 mg/kgpercentile 5Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
2.71 ppm66th percentile1.27 %percentile 356.55 ppm21th percentile2,603 Bq/m²percentile 82Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Rock temperature with depth
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
Groundwater: chemistry, water types and radioactivity
Chemical water types nearby
Water quality class according to the hydrogeochemical map
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median water source for individual supply 2 7,98 Bq/l 6.27 Bq/l free-flowing borehole with thermal and mineral water 2 12,9 Bq/l 6.54 Bq/l well 10 14,8 Bq/l 3.09 Bq/l water source for public supply 1 7,06 Bq/l 7.06 Bq/l Mine workings, deposits and ore occurrences
Deposits and mining areas
Deposit Mineral Status and organisation From the water Dunajský Klátov gravelly sands and sands Mined deposit – ŠKOLSKÉ HOSPODÁRSTVO – BÚŠLAK, spol. s r.o. 210 m Čečínska Potôň gravelly sands and sands Mined deposit – MEUM, a.s. 1.4 km Čečínska Potôň II gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – GOBIO, s.r.o. 1.8 km Mostová – Šoriakoš gravelly sands and sands Mined deposit – DELTA stone s.r.o. 2.1 km Čečínska Potôň III – Jazero Ikra gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – IKRA s.r.o. 2.2 km Nové Osady gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – bez organizácie 4.1 km Ostrov gravelly sands and sands Mined deposit – R 5 C s.r.o. 4.6 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water J-17 engineering-geological 2.0 m 5564430 m Z-19 deposit 5.0 m 6974650 m Dunajský Klátov-Csotfa wide-diameter borehole 80.0 m 58592 144Cd30.pdf80 m J-8 engineering-geological 2.0 m 5564480 m J-3 engineering-geological 2.0 m 5564480 m S-15 engineering-geological 12.0 m 1224080 m Z-17 deposit 5.0 m 6974680 m Dunajský Klátov narrow-diameter borehole with ordinary drinking and process water – 67337 144Cd48.pdf90 m Dunajský Klátov narrow-diameter borehole with ordinary drinking and process water – 67338 144Cd47.pdf90 m Topoľníky wide-diameter borehole 30.0 m 51331 12Ba8.pdf90 m J-1 engineering-geological 2.5 m 5564490 m J-2 engineering-geological 2.0 m 5564490 m Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Topoľníky – FGT-1 74 °C 23.0 l/s 2501 m Na-HCO3-Cl in use 190 m Dunajský Klátov – VDK-15 74 °C 15.4 l/s 2240 m Na-HCO3-Cl unused 270 m Dunajská Streda – DS-1 91 °C 15.2 l/s 2500 m Na-Cl-HCO3 in use 7.5 km Dunajská Streda – DS-2 55 °C 23.0 l/s 1600 m Na-HCO3 in use 7.8 km Boheľov – GPB-1 – – 2800 m – unused 8.3 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 6 120 m VDK-15 geothermal water 55 – 80 16 – 30 1 1.0 km FGT-1 geothermal water 55 – 80 16 – 30 1 1.3 km category Topoľníky thermal baths – – 1 2.4 km DS-1.2 geothermal water 80 – 100 16 – 30 1 6.5 km category Dunajská Streda thermal baths – – 1 7.1 km VFP-12-R geothermal water 55 – 80 16 – 30 1 9.7 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Jahodná – za cintorínon – Dunajský Klátov – 1970 – 140 m Trhová Hradská – 1970 – 200 m Topoľníky – Dolné – Dolné Topoľníky 5 950 m² 1989 – 420 m Kútniky – medzi traťou – Trhová Hradská 18 000 m² 1970 – 450 m Jahodná – pri Malom Danube – Horné Mýto – 1965 – 500 m Malé Dvorníky – pri cintoríne. – Malé Dvorníky – 1960 – 510 m Dolný Štál – Dolné Topoľníky 3 000 m² 1970 – 670 m Dolný Štál – bývalé ihrisko – Dolné Topoľníky 5 000 m² 1970 – 1.6 km 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
22from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
LithiumLihigh (top 5 %)
highest 68.0 μg/lmedian 29.5 μg/l10 samples10 % below the limit of quantification
ArsenicAselevated (top 10 %)
highest 5.00 μg/lmedian 1.00 μg/l11 samples45 % below the limit of quantification
AntimonySbslightly elevated
highest 0.570 μg/lmedian 0.570 μg/l1 sample
StrontiumSrtypical value
highest 300 μg/lmedian 300 μg/l1 sample
CopperCutypical value
highest 2.00 μg/lmedian 1.00 μg/l10 samples80 % below the limit of quantification
BariumBatypical value
highest 47.0 μg/lmedian 37.0 μg/l9 samples
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l10 samples100 % below the limit of quantification
ChromiumCrbelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l10 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.150 μg/lmedian 0.150 μg/l10 samples100 % below the limit of quantification
Silicon dioxideSiO2below half of Slovakia
highest 10.4 mg/lmedian 8.30 mg/l10 samples
LithiumLiextreme (top 1 %)
highest 700 μg/lmedian 4.50 μg/l52 samples
CadmiumCdextreme (top 1 %)
highest 654 μg/lmedian 0.250 μg/l52 samples98 % below the limit of quantification
ChromiumCrextreme (top 1 %)
highest 25.0 μg/lmedian 0.600 μg/l52 samples42 % below the limit of quantification
CopperCuextreme (top 1 %)
highest 19.1 μg/lmedian 1.10 μg/l52 samples
ArsenicAsextreme (top 1 %)
highest 42.0 μg/lmedian 0.500 μg/l52 samples83 % below the limit of quantification
ZincZnextreme (top 1 %)
highest 5,490 μg/lmedian 107 μg/l52 samples
LeadPbhigh (top 5 %)
highest 6.00 μg/lmedian 1.00 μg/l52 samples48 % below the limit of quantification
SeleniumSehigh (top 5 %)
highest 3.50 μg/lmedian 0.500 μg/l52 samples90 % below the limit of quantification
AntimonySbhigh (top 5 %)
highest 1.00 μg/lmedian 0.100 μg/l52 samples63 % below the limit of quantification
MercuryHghigh (top 5 %)
highest 0.200 μg/lmedian 0.100 μg/l52 samples98 % below the limit of quantification
AluminiumAlelevated (top 10 %)
highest 0.0400 mg/lmedian 0.0100 mg/l52 samples37 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l16 samples100 % below the limit of quantification