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 VN Kučišdorf, window score 29. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 19:04. 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. Terrain height along the fishing district and the approximate water level. Reservoir This is a reservoir, so the watercourse is not assessed here: the water has no current, fall or gradient. The chart shows the terrain height along the fishing district. Source: Open Topo Data (eudem25m), 4 Nov 2026. The height is approximate (error of a few metres). 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 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. 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 (1 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 7.7modelled estimate water type Ca–HCO₃–SO₄ Mineralisation 259 mg/l, soft water (8.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 5 from 15elements in the top 10 % highest: Arsenic 65.4 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. 53nGy/h dose rate percentile 66 in Slovakia Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ. 83objects within 3 km mined: Sb, Au, As, Pb, Zn Nearest: Halda pri V – 1117 štôlni (spoil heap), 1.4 km from the water. 1sample with gold 11 ore minerals in the sediment Up to 1 grain in one sample (20 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment. 1 from 9indicators in the top 5 % highest: Copper 14.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 96 (potok, 400 m J od kóty Široký vrch 326). 355boreholes within 3 km 131 water analyses nearby Of these, 355 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 1 geothermal and mineral water spring within 10 km. 7sites within 3 km 7 environmental burdens Nearest burden: PK (015) / Pezinok – oblasť rudných baní a starých banských diel, 2.0 km from the water. Proximity does not mean that substances leak from the site into the water. 38records within 5 km 17 deposits, 21 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 The map covers 1 of 1 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 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 7.72typical 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. 8.0°dH, soft Sum of calcium and magnesium (1.43 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 259mg/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. 53nGy/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. +3nT range 3 to 3 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. -1mGal residual +23.3 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. 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 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: potok, 400 m J od kóty Široký vrch 3261999, 440 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: ľavostr. prítok Trnianskeho p. pod Širokým vrchom1999, 940 m from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: ľavostr. prítok Trnianskeho p. pod Širokým vrchom1999, 940 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: bez mena2000, 870 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: bez mena2000, 870 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: bez mena2000, 870 m from the water. Comparison: percentile 37 of all samples in Slovakia. Highest value: bez mena2000, 870 m from the water. Comparison: percentile 34 of all samples in Slovakia. Highest value: bez mena2000, 870 m from the water. Comparison: percentile 32 of all samples in Slovakia. Highest value: bez mena, 870 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: potok, 400 m J od kóty Široký vrch 3261999, 440 m from the water. Comparison: percentile 92 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: štôlňa1994, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: drenáž1993, 2.8 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: drenáž1993, 2.8 km from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: štôlňa1994, 2.2 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1994, 1.5 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1994, 730 m from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: studňa1994, 2.4 km from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: studňa1994, 730 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: štôlňa1994, 2.2 km from the water. Comparison: percentile 73 of all samples in Slovakia. Highest value: drenáž1993, 2.8 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: drenáž1993, 2.8 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: drenáž1993, 2.8 km from the water. Comparison: percentile 46 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. 355 boreholes in the 3 km zone, of which 17 hydrogeological and 338 other; with an archive report number 355. 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 VN Kučišdorf watercourse
Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the watercourse
Elevation profile: reservoir
Terrain in 3D
Historical images



Water pollution on the VN Kučišdorf watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VN Kučišdorf stream
Rock under the water
Water according to the atlas
Elements in river sediment
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 1× Quaternary cover
Neotectonic units
Direction of neotectonic movements
Regional geological division
Regional geological division (subunits)
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Type of permeability (basic hydrogeological map 1:50,000)
Hydrogeological function
Main hydrogeological region
Genetic type of groundwater
Groundwater quality class
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
67.1 mg/lpercentile 7410.7 mg/lpercentile 572.76 mg/lpercentile 460.106 mg/lpercentile 455.33 mg/lpercentile 369.60 mg/lpercentile 3041.4 mg/lpercentile 29119 mg/lpercentile 24Nutrients and organic pollution
3.65 mg/lpercentile 600.0870 mg/lpercentile 400.0797 mg/lpercentile 392.07 mg/lpercentile 8Metals
12.2 μg/lpercentile 7231.2 μg/lpercentile 500.0538 mg/lpercentile 2522.8 μg/lpercentile 22Elements in river sediments
Potentially toxic and trace elements
65.4 mg/kgpercentile 951.68 mg/kgpercentile 9518.8 mg/kgpercentile 9514.7 mg/kgpercentile 9440.7 mg/kgpercentile 9048.2 mg/kgpercentile 8894.3 mg/kgpercentile 860.476 mg/kgpercentile 85157 mg/kgpercentile 820.165 mg/kgpercentile 692.87 mg/kgpercentile 580.280 mg/kgpercentile 580.233 mg/kgpercentile 5759.4 mg/kgpercentile 2912.2 mg/kgpercentile 28Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
15,526 mg/kgpercentile 1003,248 mg/kgpercentile 965.53 %percentile 961.09 %percentile 806.68 %percentile 801.16 %percentile 691.63 %percentile 681.99 %percentile 494,100 mg/kgpercentile 35Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
1,644 mg/kgpercentile 95226 mg/kgpercentile 9220.3 mg/kgpercentile 912.15 mg/kgpercentile 8837.0 mg/kgpercentile 8128.8 mg/kgpercentile 5659.5 mg/kgpercentile 5179.6 mg/kgpercentile 27236 mg/kgpercentile 1134.4 mg/kgpercentile 7Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.45 %percentile 802.72 ppm67th percentile7.35 ppm51th percentile1,080 Bq/m²percentile 23Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Relief, climate and soils
Geomorphological units
Geomorphological regions
Soil contamination (map 1:500,000)
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 26 1 grain 20 m Rock-forming and accessory minerals
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 free-flowing borehole 1 4,63 Bq/l 4.63 Bq/l well 1 37,4 Bq/l 37.4 Bq/l source 3 26,9 Bq/l 9.82 Bq/l developed spring 2 49,4 Bq/l 47.7 Bq/l mineral spring 1 3,65 Bq/l 3.65 Bq/l Mine workings, deposits and ore occurrences
What was mined here (according to the register of old mine workings)
Types of mining objects
Nearest old mine workings
Name Type Mined Ended From the water Halda pri V – 1117 štôlni spoil heap Sulfide (pyritic) ores 1.4 km V – 1117 adit adit sulfide (pyritic) ores 1.5 km Halda pri V – 1118 štôlni spoil heap Sulfide (pyritic) ores 1.5 km V – 1118 adit adit sulfide (pyritic) ores 1.5 km 1.bezmenný komín štôlne V-1117 shaft Sulfide (pyritic) ores 1.5 km Halda 4. bezmennej št. spoil heap Sulfide (pyritic) ores 1.5 km 4.bezmenná štôlňa adit sulfide (pyritic) ores 1.5 km Halda 3. bezmennej št. spoil heap Sulfide (pyritic) ores 1.6 km 3.bezmenná štôlňa adit sulfide (pyritic) ores 1.6 km Halda 2. bezmennej št. spoil heap Sulfide (pyritic) ores 1.6 km Deposits and mining areas
Deposit Mineral Status and organisation From the water Pezinok – odkaliská gold ores Deposit with expected use of reserves – ELGEO – BANSKÁ, s.r.o. 2.3 km Pezinok antimony ores Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.3 km Pezinok – Sb antimony ores Deposit with halted mining or where use of reserves is not expected – ELGEO – BANSKÁ, s.r.o. 2.3 km Pezinok gold ores Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.3 km Pezinok – Zlatá žila gold ores Deposit with halted mining or where use of reserves is not expected – ELGEO – BANSKÁ, s.r.o. 2.3 km Pezinok – odkaliská gold ores Deposit with expected use of reserves – ELGEO – BANSKÁ, s.r.o. 2.4 km Pezinok – Vinohrady antimony ores Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.4 km Pezinok gold ores Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.4 km Pezinok – Zlatá žila gold ores Deposit with halted mining or where use of reserves is not expected – ELGEO – BANSKÁ, s.r.o. 2.4 km Pezinok – Sb antimony ores Deposit with halted mining or where use of reserves is not expected – ELGEO – BANSKÁ, s.r.o. 2.4 km Pezinok – Sb antimony ores Deposit with halted mining or where use of reserves is not expected – METAL – ECO SERVIS, spol. s r.o. 2.4 km Pezinok antimony ores Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.4 km Ore occurrences in the metallogenic map
Occurrence Ore type Metals Type From the water Pezinok Sb – II Antimony ores Sb deposit occurrence 1.0 km Pezinok-Sb Antimony ores Sb small deposit 1.7 km Pezinok Antimony ores Sb, Au small deposit 1.9 km Pezinok – Vinohrady Gold ores Au, Sb small deposit 2.1 km Pezinok – Zlatá žila Gold ores Au, Sb small deposit 2.8 km Pezinok – Sb Antimony ores Sb small deposit 3.0 km Rybníček Pyrite pyrite, pyrrhotite deposit occurrence 4.3 km Pezinok – I Gold-silver ores Au, Ag, Sb deposit occurrence 4.6 km Pezinok Gold ores Au small deposit 4.6 km Augustín Pyrite pyrite, pyrrhotite medium deposit 4.9 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water VMK-18-92 deposit 23.0 m 8101590 m VMK-26-92 deposit 19.0 m 81015330 m VMK-23-92 deposit 26.0 m 81015340 m C-3 engineering-geological 3.0 m 85768450 m VMK-19-92 deposit 21.0 m 81015460 m VMK-27-92 deposit 11.0 m 81015510 m VMK-24-92 deposit 14.0 m 81015700 m C-2 engineering-geological 4.0 m 85768730 m Pezinok wide-diameter borehole 42.0 m 56642 131Dc38.pdf760 m VMK-25-92 deposit 13.0 m 81015770 m VMK-22-92 deposit 12.0 m 81015900 m Pezinok narrow-diameter borehole with ordinary drinking and process water 45.0 m 89017 143Ba64.pdf910 m Geothermal energy and mineral waters
Sources of geothermal and mineral waters
Source Type Water temperature (°C) Yield (l/s) Count Nearest from water category a1 mineral water < 15 < 5 1 9.2 km Environmental burdens, landfills and anthropogenic sediments
Environmental burdens
Site Activity Substance Classification From the water PK (015) / Pezinok – oblasť rudných baní a starých banských diel ore mining – mining of mineral resources As 62b. (41 -21) 2.0 km Pezinok – oblasť rudných baní a starých banských diel SK200030FK 2.0 km PK (008) / Pezinok – Budúcnosť – adit ore mining – mining of mineral resources Sb 52b. (31-21) 2.1 km PK (017) / Pezinok – Rudné bane – odkaliská tailings pond – waste management facilities As 70b. (44-26) 2.1 km PK (022) / Pezinok – Sirková – adit and spoil heap ore mining – mining of mineral resources As 57b. (36-21) 2.2 km PK (016) / Pezinok – Pyritová – adit ore mining – mining of mineral resources Sb 57b. (36-21) 2.5 km PK (014) / Pezinok – Kolársky vrch – povrchová dobývka – landfill landfill priemyselného odpadu – zariadenia na nakladanie s odpadmi Pb 53 b. (36-17) 2.8 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
18from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
CopperCuhigh (top 5 %)
highest 14.0 μg/lmedian 3.30 μg/l3 samples
BariumBaelevated (top 10 %)
highest 115 μg/lmedian 93.0 μg/l3 samples
ArsenicAsslightly elevated
highest 2.00 μg/lmedian 1.00 μg/l3 samples33 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l3 samples100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l3 samples100 % below the limit of quantification
AntimonySbbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l3 samples100 % below the limit of quantification
LithiumLibelow half of Slovakia
highest 5.00 μg/lmedian 5.00 μg/l3 samples100 % below the limit of quantification
ChromiumCrbelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l3 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.150 μg/lmedian 0.150 μg/l3 samples100 % below the limit of quantification
Silicon dioxideSiO2elevated (top 10 %)
highest 34.5 mg/lmedian 28.1 mg/l3 samples
AntimonySbextreme (top 1 %)
highest 34.2 μg/lmedian 0.300 μg/l9 samples44 % below the limit of quantification
ArsenicAsextreme (top 1 %)
highest 14.9 μg/lmedian 1.70 μg/l9 samples33 % below the limit of quantification
CopperCuhigh (top 5 %)
highest 13.0 μg/lmedian 1.10 μg/l9 samples
LithiumLihigh (top 5 %)
highest 77.0 μg/lmedian 16.0 μg/l9 samples
SeleniumSehigh (top 5 %)
highest 3.10 μg/lmedian 0.500 μg/l9 samples89 % below the limit of quantification
ChromiumCrelevated (top 10 %)
highest 2.70 μg/lmedian 0.800 μg/l9 samples44 % below the limit of quantification
AluminiumAlelevated (top 10 %)
highest 0.0500 mg/lmedian 0.0100 mg/l9 samples33 % below the limit of quantification
LeadPbslightly elevated
highest 1.00 μg/lmedian 0.500 μg/l9 samples89 % below the limit of quantification
ZincZntypical value
highest 117 μg/lmedian 29.0 μg/l9 samples
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l1 sample100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l9 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l9 samples100 % below the limit of quantification

