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 Korytno II., window score 20. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 15:44. 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 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 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. Young sediments50% of the water line 50% river alluvium Young unconsolidated sediments; fine material easily washes into the stream during rain. Geological Map of Slovakia 1:50,000. pH 8.1modelled estimate water type Ca–Mg–SO₄–HCO₃ Mineralisation 687 mg/l, very hard water (24.1 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 11 from 15elements in the top 10 % highest: Mercury 112 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 98. Interpolation of the Geochemical Atlas of river sediments. 25°C at 1,000 m depth heat flow 65 mW/m² At a depth of 2,000 m about 55 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 46nGy/h dose rate percentile 20 in Slovakia Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ. 55objects within 3 km mined: Fe, Cu, Ba Nearest: Halda štôlne RŠT-1 (spoil heap), 130 m from the water. 0samples with gold 12 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. 3 from 10indicators in the top 5 % highest: Antimony 45.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (1000m SZ od K664). 98boreholes within 3 km 280 water analyses nearby Of these, 96 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 1 geothermal borehole within 10 km 3 geothermal and mineral water springs within 10 km. 2sites within 3 km 2 landfills No environmental burden is registered within 3 km; landfills are only recorded. 78records within 5 km 35 deposits, 43 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 Young sediments: Young unconsolidated sediments; fine material easily washes into the stream during 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 The map covers 2 of 2 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 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. 24.1°dH, very hard Sum of calcium and magnesium (4.30 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 687mg/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–SO₄–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. 46nGy/h in air Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains. 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) 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. -64nT range -64 to -64 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. -20mGal residual +8.4 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. 25 / 55 °Cat depths of 1,000 and 2,000 m increase of 30 °C per km The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 65 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 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: 1000m SZ od K6641992, 660 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: 800m SSV od K6641992, 300 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: 1000m SZ od K6641992, 660 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: 2000m V od K640 Babiná1992, 440 m from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: 1000m SZ od K6641992, 660 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: 800m SSV od K6641992, 300 m from the water. Comparison: percentile 87 of all samples in Slovakia. Highest value: 2000m V od K640 Babiná1992, 440 m from the water. Comparison: percentile 78 of all samples in Slovakia. Highest value: 2000m V od K640 Babiná, 440 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: 2000m V od K640 Babiná1992, 440 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: 2000m V od K640 Babiná1992, 440 m from the water. Comparison: percentile 43 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: 800m SSV od K6641992, 300 m from the water. Comparison: percentile 64 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: prameň1992, 460 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1992, 1.5 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1992, 270 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1992, 1.5 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1992, 2.5 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 86 of all samples in Slovakia. Highest value: studňa1992, 2.7 km from the water. Comparison: percentile 61 of all samples in Slovakia. Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 39 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. 98 boreholes in the 3 km zone, of which 9 hydrogeological and 89 other; with an archive report number 96. 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 Bodrog basin and Hornád
By the water now
Today on the VN Korytno II. 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 Korytno II. watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VN Korytno II. 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 Pleistocene – Holocene deluvial sediments as a whole: lithofacial undifferentiated slopes and debris 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)
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
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
239 mg/lpercentile 9649.5 mg/lpercentile 9510.6 mg/lpercentile 9321.8 mg/lpercentile 8290.7 mg/lpercentile 800.182 mg/lpercentile 7624.9 mg/lpercentile 75243 mg/lpercentile 61Nutrients and organic pollution
0.426 mg/lpercentile 770.119 mg/lpercentile 535.82 mg/lpercentile 462.76 mg/lpercentile 39Metals
216 μg/lpercentile 910.326 mg/lpercentile 86192 μg/lpercentile 783.05 μg/lpercentile 21Elements in river sediments
Potentially toxic and trace elements
112 mg/kgpercentile 9858.3 mg/kgpercentile 981,126 mg/kgpercentile 983,324 mg/kgpercentile 98465 mg/kgpercentile 986.47 mg/kgpercentile 982.35 mg/kgpercentile 9517.9 mg/kgpercentile 957.25 mg/kgpercentile 951.04 mg/kgpercentile 9442.2 mg/kgpercentile 91178 mg/kgpercentile 8625.9 mg/kgpercentile 8397.8 mg/kgpercentile 8081.0 mg/kgpercentile 74Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
8.74 %percentile 973,216 mg/kgpercentile 951.10 %percentile 662.39 %percentile 57886 mg/kgpercentile 551.52 %percentile 515.58 %percentile 484,048 mg/kgpercentile 330.547 %percentile 6Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
7,620 mg/kgpercentile 98124 mg/kgpercentile 9543.5 mg/kgpercentile 9546.8 mg/kgpercentile 95188 mg/kgpercentile 83101 mg/kgpercentile 7911.9 mg/kgpercentile 331.09 mg/kgpercentile 32335 mg/kgpercentile 2852.7 mg/kgpercentile 27Natural radioactivity and radon
Gamma radiation dose rate
1.29 %percentile 452.38 ppm27th percentile6.33 ppm16th percentile1,787 Bq/m²percentile 63Geophysical 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
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
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 source 3 7,48 Bq/l 3.61 Bq/l free-flowing borehole 1 0,900 Bq/l 0.900 Bq/l water source for public supply 1 0,470 Bq/l 0.470 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 štôlne RŠT-1 spoil heap limestones 1975 130 m Štôlňa RŠT-1 adit limestones 1975 140 m Halda štôlne RŠT-2 spoil heap limestones 1975 150 m Štôlňa RŠT-2 adit limestones 1975 170 m odkalisko Rudňany tailings pond 180 m Halda štôlne RŠT-3 spoil heap limestones 1975 280 m Štôlňa RŠT-1 adit limestones 1975 280 m Štôlňa RŠT-3 adit limestones 1975 290 m Štôlňa RŠT-2 adit limestones 1975 420 m Štôlňa RŠT-3 adit limestones 1975 530 m Deposits and mining areas
Deposit Mineral Status and organisation From the water Markušovce I barite Deposit with halted mining or where use of reserves is not expected – RIS, a.s. 110 m Markušovce I barite Deposit with halted mining or where use of reserves is not expected – RIS, a.s. 110 m Markušovce I barite Deposit with halted mining or where use of reserves is not expected – RIS, a.s. 140 m Markušovce high-grade limestone Mined deposit – VSK MINERAL s.r.o. 460 m Markušovce high-grade limestone Mined deposit – VSK MINERAL s.r.o. 460 m Rudňany building stone Deposit with halted mining or where use of reserves is not expected – DOPRAVEX kameňolomy, s. r. o. 1.2 km Matejovce nad Hornádom gypsum Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.6 km Matejovce nad Hornádom anhydrite Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.6 km Matejovce nad Hornádom anhydrite Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.6 km Matejovce nad Hornádom gypsum Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.6 km Rudňany, časť Poráč – Zlatník iron ores Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 3.7 km Rudňany, časť Rudňany barite Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 3.7 km Ore occurrences in the metallogenic map
Occurrence Ore type Metals Type From the water Markušovce Aluminium ores (bauxites) Al deposit occurrence 620 m Matejovce nad Hornádom Uranium-molybdenum ores Cu, U, Mo deposit occurrence 1.7 km Rudňany – Severná žila Complex iron ores Fe, Cu small deposit 1.8 km Závadka pri Nálepkove, Stožky Iron ores Fe mineralogical occurrence 2.0 km Rudňany Complex iron ores Fe, Cu, barite small deposit 2.4 km Závadka pri Nálepkove, Slivníky Copper ores Cu, U mineralogical occurrence 2.4 km Hnilčík, žily Izabela, Farský grund a Baniská Complex iron ores Fe, Cu deposit occurrence 2.5 km Rudňany – Matej a Jakub žila Complex iron ores Fe, Cu small deposit 2.8 km Poráč – Zlatník Barite barite medium deposit 2.8 km Chrasť nad Hornádom, žily Ján, Lendava and Miloj Complex iron ores Fe, Cu deposit occurrence 3.0 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water VN244-6 environment 11.0 m – 510 m VN244-5 environment 8.5 m – 580 m 1241 deposit 1,110.0 m 79592600 m 1241 deposit 1,110.0 m 79592600 m 1021 deposit 661.2 m 79592710 m 1021 deposit 661.2 m 79592710 m R-117 engineering-geological 8.0 m 80782750 m V-1 deposit 9.0 m 2107890 m V-2 deposit 6.0 m 2107900 m V-3 deposit 4.0 m 2107920 m V-6 deposit 3.0 m 2107960 m V-RHV-23 deposit 1,200.0 m 80787990 m Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Danišovce – DH-1 – 0.1 l/s 1000 m – unused 7.5 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 3 4.8 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water landfill Želba, a.s. OZ Rudňany, 053021 Markušovce – Markušovce 18 100 m² 1998 monitored 260 m Markušovce 210 m² 1985 – 2.4 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
17from 100
1445fishing districts
Map color
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Cations (positive ions)
Anions (negative ions)
AntimonySbextreme (top 1 %)
highest 45.0 μg/lmedian 13.0 μg/l5 samples
LithiumLiextreme (top 1 %)
highest 116 μg/lmedian 20.0 μg/l5 samples40 % below the limit of quantification
ArsenicAsextreme (top 1 %)
highest 27.0 μg/lmedian 6.00 μg/l5 samples20 % below the limit of quantification
ChromiumCrelevated (top 10 %)
highest 5.50 μg/lmedian 1.90 μg/l5 samples40 % below the limit of quantification
CopperCuelevated (top 10 %)
highest 5.00 μg/lmedian 3.00 μg/l5 samples20 % below the limit of quantification
StrontiumSrslightly elevated
highest 450 μg/lmedian 300 μg/l5 samples
BariumBaslightly elevated
highest 70.0 μg/lmedian 60.0 μg/l5 samples
CadmiumCdslightly elevated
highest 0.250 μg/lmedian 0.250 μg/l5 samples40 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l5 samples100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l5 samples100 % below the limit of quantification
Silicon dioxideSiO2typical value
highest 14.7 mg/lmedian 7.86 mg/l5 samples
MercuryHgextreme (top 1 %)
highest 1.00 μg/lmedian 0.100 μg/l19 samples63 % below the limit of quantification
AluminiumAlextreme (top 1 %)
highest 0.210 mg/lmedian 0.00500 mg/l19 samples58 % below the limit of quantification
AntimonySbhigh (top 5 %)
highest 3.30 μg/lmedian 0.200 μg/l19 samples37 % below the limit of quantification
ChromiumCrhigh (top 5 %)
highest 4.70 μg/lmedian 0.250 μg/l19 samples58 % below the limit of quantification
LeadPbhigh (top 5 %)
highest 3.00 μg/lmedian 0.500 μg/l19 samples58 % below the limit of quantification
ArsenicAselevated (top 10 %)
highest 3.20 μg/lmedian 0.500 μg/l19 samples95 % below the limit of quantification
CopperCuelevated (top 10 %)
highest 3.80 μg/lmedian 0.700 μg/l19 samples
ZincZnslightly elevated
highest 375 μg/lmedian 2.00 μg/l19 samples42 % below the limit of quantification
LithiumLitypical value
highest 11.0 μg/lmedian 3.00 μg/l19 samples26 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l8 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l19 samples100 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l19 samples100 % below the limit of quantification




