Watercourse

OR Moravský Svätý Ján – dolné

fishing district
1
fishing district length
2.1km
region
Trnava Region
Aerial image of watercourse OR Moravský Svätý Ján - dolné with the line highlighted
Blue line: course of the watercourse (approximate). Orthophoto mosaic of Slovakia © GKÚ Bratislava, CC BY 4.0Google Maps

By the water now

Today on the OR Moravský Svätý Ján – dolné watercourse

Fishing conditions score, the best window of the day and fishing districts from the best conditions

Average of the watercourse's fishing districts

Low activity · average of one fishing district

The number in the header is an estimate for the middle of the watercourse based on weather and measurements. The average of the fishing districts also counts satellite data, shading and geology of each district.

Best window today

15:00–17:00

OR Moravský Svätý Ján – dolné, window score 28.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 17:04.

Map and fishing districts of the watercourse

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

1445fishing districts
Pick a category to narrow the selection. Next to each option you can see how many fishing districts remain.
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    Elevation profile: standing water

    Terrain height along the fishing district and the approximate water level.

    Still water This is standing water, 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.

    1481501521541560.0 km0.5 km1.0 km1.5 km2.0 km
    Terrain elevation profile (Standing water): from 154 to 149 m a.s.l. over 2.1 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    151 m a.s.l.
    Lowest point of the profile
    149 m a.s.l.
    Highest point of the profile
    154 m a.s.l.

    Source: Open Topo Data (eudem25m), 4 Nov 2026. The height is approximate (error of a few metres).

    Terrain in 3D

    Loading the 3D terrain model…

    Historical images

    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.

    Aerial image of watercourse OR Moravský Svätý Ján - dolné from 2017
    2017imaged 24 Aug 2017
    Aerial image of watercourse OR Moravský Svätý Ján - dolné from 2020
    2020imaged 22 Aug 2020
    Aerial image of watercourse OR Moravský Svätý Ján - dolné from 2023
    2023imaged 27 May 2023

    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 pollution on the OR Moravský Svätý Ján – dolné watercourse

    Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby

    Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025

    1 of 1 fishing districts on the watercourse with SHMÚ data: the nearest site has an unmet standard in at least one indicator.

    • 1 to 2 indicators1

    Most polluted fishing districtsall with an unmet standard

    Groundwater: measured valuestypical value from stations within 10 km, 2025

    1 of 1 fishing district with measurements has groundwater nearby with a value above the limit for at least one indicator.

    • ammonium or nitrites above the standard at at least one station1
    • iron from 1 mg/l1

    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.

    Geology and geochemistry of the OR Moravský Svätý Ján – dolné stream

    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 (2 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.

    Rock under the water

    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.

    510

    Water according to the atlas

    pH 7.9modelled estimate

    water type Ca–HCO₃

    Mineralisation 428 mg/l, moderately hard water (12.4 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    0 from 15elements in the top 10 %

    highest: Selenium 0.206 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 40. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km45 °C75 °C

    Heat underfoot

    45°C at 1,000 m depth

    heat flow 50 mW/m²

    At a depth of 2,000 m about 75 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    51nGy/h dose rate

    percentile 58 in Slovakia

    Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ.

    Old mine workings

    0objects within 3 km

    No old mine working is recorded within 3 km of the water.

    Gold in river sediment

    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.

    Trace elements in the stream water

    0 from 9indicators in the top 5 %

    highest: Copper 4.30 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 89 (mŕtve rameno rieky Morava, lok. Rozpad).

    Boreholes and groundwater analyses

    58boreholes within 3 km

    30 water analyses nearby

    Of these, 52 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    No geothermal borehole or spring is recorded within 10 km.

    Environmental burdens and landfills

    0sites within 3 km

    No environmental burden is registered within 3 km; landfills are only recorded.

    Deposits and ore occurrences

    3records within 5 km

    2 deposits, 1 ore occurrence

    Geofond registers, the metallogenetic map and the mineral resources map.

    Landslides and slope deformations

    0areas within 3 km

    Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed.

    Geological structure beneath the water

    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.

    • River alluvium100%SR 72 %

    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.

    Geological age of the rocks

    • Quaternary100%

    Most common rock units

    SystemAgeUnitPoints
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains1×

    Quaternary cover

    • fluvial sediments of floodplains100%SR 68 %

    marker on the bar: share among all sample points on streams in Slovakia

    • Typical thickness of the Quaternary cover7.5m
    • 5 – 10100%SR 20 %

    marker on the bar: share among all sample points on streams in Slovakia

    Tectonic division

    • NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

    marker on the bar: share among all sample points on streams in Slovakia

    Neotectonic units

    • positive unit (lowland hills)100%SR 14 %

    marker on the bar: share among all sample points on streams in Slovakia

    Direction of neotectonic movements

    • very small uplift100%SR 6.4 %

    marker on the bar: share among all sample points on streams in Slovakia

    Regional geological division

    • intramontane basins100%SR 44 %

    marker on the bar: share among all sample points on streams in Slovakia

    Regional geological division (subunits)

    • Vienna Basin100%SR 4.0 %

    marker on the bar: share among all sample points on streams in Slovakia

    Engineering-geological districts

    • region of lowland-stream deposits100%SR 20 %

    marker on the bar: share among all sample points on streams in Slovakia

    Engineering-geological formations

    • formation of Quaternary sediments100%SR 71 %

    marker on the bar: share among all sample points on streams in Slovakia

    Susceptibility of the area to slope deformations

    • Region of stable areas100%SR 95 %

    marker on the bar: share among all sample points on streams in Slovakia

    The map covers 1 of 2 points on the water line.

    Hydrogeology: aquifers and groundwater

    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.

    Type of permeability (basic hydrogeological map 1:50,000)

    • intergranular100%SR 86 %

    marker on the bar: share among all sample points on streams in Slovakia

    Hydrogeological function

    • aquifer100%SR 95 %

    marker on the bar: share among all sample points on streams in Slovakia

    Main hydrogeological region

    • Quaternary of the Morava from Brodské to Vysoká pri Morave100%SR 0.0 %

    marker on the bar: share among all sample points on streams in Slovakia

    Surface water chemistry according to the atlas

    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.

    510

    Water acidity

    pH 7.88typical 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.

    Water hardness

    12.4°dH, moderately hard

    Sum of calcium and magnesium (2.22 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    428mg/l mineralisation

    Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds.

    Ionic composition of the water

    Water type by dominant ions: Ca–HCO₃

    Shares are in equivalents, the usual way of comparing the composition of waters.

    Major ions

    • FluoridesF0.279 mg/lpercentile 92
    • PotassiumK8.60 mg/lpercentile 90
    • ChloridesCl42.4 mg/lpercentile 87
    • SodiumNa27.2 mg/lpercentile 87
    • SulphatesSO467.3 mg/lpercentile 74
    • MagnesiumMg16.4 mg/lpercentile 54
    • CalciumCa61.9 mg/lpercentile 49
    • BicarbonatesHCO3190 mg/lpercentile 42

    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)

    Nutrients and organic pollution

    • Chemical oxygen demandChSK13.0 mg/lpercentile 95
    • AmmoniumNH41.88 mg/lpercentile 95
    • PhosphatesPO40.420 mg/lpercentile 76
    • NitratesNO310.5 mg/lpercentile 74

    Metals

    • ManganeseMn350 μg/lpercentile 94
    • ZincZn19.8 μg/lpercentile 86
    • IronFe0.279 mg/lpercentile 83
    • AluminiumAl62.7 μg/lpercentile 49

    Elements in river sediments

    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.

    Potentially toxic and trace elements

    • SeleniumSe0.206 mg/kgpercentile 40
    • MolybdenumMo0.277 mg/kgpercentile 29
    • TinSn2.15 mg/kgpercentile 28
    • ChromiumCr56.5 mg/kgpercentile 25
    • LeadPb11.8 mg/kgpercentile 25
    • NickelNi17.3 mg/kgpercentile 19
    • CobaltCo6.13 mg/kgpercentile 16
    • CadmiumCd0.0675 mg/kgpercentile 12
    • MercuryHg0.0445 mg/kgpercentile 10
    • BismuthBi0.109 mg/kgpercentile 9
    • CopperCu13.7 mg/kgpercentile 8
    • VanadiumV47.3 mg/kgpercentile 7
    • ZincZn47.2 mg/kgpercentile 4
    • ArsenicAs2.17 mg/kgpercentile 2
    • AntimonySb0.133 mg/kgpercentile 1

    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)

    Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
    • SodiumNa0.769 %percentile 30
    • CalciumCa1.28 %percentile 24
    • PotassiumK1.29 %percentile 18
    • TitaniumTi3,595 mg/kgpercentile 17
    • PhosphorusP546 mg/kgpercentile 12
    • AluminiumAl4.19 %percentile 7
    • ManganeseMn464 mg/kgpercentile 5
    • MagnesiumMg0.465 %percentile 4
    • IronFe1.46 %percentile 4
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • ZirconiumZr606 mg/kgpercentile 93
    • GalliumGa14.8 mg/kgpercentile 56
    • BariumBa409 mg/kgpercentile 40
    • BerylliumBe1.19 mg/kgpercentile 37
    • RubidiumRb82.2 mg/kgpercentile 33
    • YttriumY24.0 mg/kgpercentile 30
    • StrontiumSr113 mg/kgpercentile 28
    • BoronB45.7 mg/kgpercentile 17
    • CeriumCe46.3 mg/kgpercentile 11
    • LithiumLi19.9 mg/kgpercentile 5

    Natural radioactivity and radon

    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.

    20200

    Gamma radiation dose rate

    51nGy/h in air

    range 51 to 51 nGy/h

    Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains.

    • Equivalent thorium (eTh)eTh8.83 ppm82th percentile
    • Potassium (K)K1.27 %percentile 35
    • Equivalent uranium (eU)eU2.19 ppm15th percentile

    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)

    • Areal activity of 137CsCS1371,740 Bq/m²percentile 61

    Geophysical fields: magnetics and gravity

    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.

    SVJZ

    Magnetic anomaly

    +54nT

    range 54 to 54 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.

    Bouguer gravity anomaly

    -60mGal

    residual −20.1 mGal

    Negative values lie over thick sediments and under mountains (light crust), positive over dense rocks and thinner crust. It shows the structure of the Earth's crust, not the water.

    Geothermal potential

    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.

    1 km2 km45 °C75 °C

    Rock temperature with depth

    45 / 75 °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 50 mW/m².

    Relief, climate and soils

    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.

    • Elevation of geomorphological units (from–to)132–158m a.s.l.
    • Average elevation of the units145m a.s.l.
    • Average slope0.5°
    • Average January temperature-2.5°C
    • Average July temperature20.0°C
    • Annual precipitation590mm

    Geomorphological units

    • Borská Lowland100%SR 2.2 %

    marker on the bar: share among all sample points on streams in Slovakia

    Geomorphological regions

    • Záhorie Lowland100%SR 2.5 %

    marker on the bar: share among all sample points on streams in Slovakia

    Climatic-geographical types

    • lowland climate100%SR 38 %

    marker on the bar: share among all sample points on streams in Slovakia

    Susceptibility of soils to acidification

    • soils very susceptible to acidification100%SR 2.4 %

    marker on the bar: share among all sample points on streams in Slovakia

    Soil contamination (map 1:500,000)

    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A100%SR 45 %

    marker on the bar: share among all sample points on streams in Slovakia

    Lithogeochemical types

    • Neogene100%SR 48 %

    marker on the bar: share among all sample points on streams in Slovakia

    Map of the corridor

    Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off.

    Moravský Svätý Ján – Gergelík I – gravelly sands and sands (3.0 km from the water)Moravský Svätý Ján – Gergelík – gravelly sands and sands (3.2 km from the water)Moravský Svätý Ján – gravelly sands (4.3 km from the water)Moravský Svätý Ján – SHMÚ observation borehole (1.9 km from the water)Moravský Svätý Ján – monitoring borehole (2.0 km from the water)Moravský Svätý Ján – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Veľké Leváre – širokoprofilový vrt (Ø vŕtania nad 600 m (2.7 km from the water)Dlhé Lúky – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.9 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.7 km from the water)1 km

    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.

    Trace elements in surface waters

    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.

    • CopperCuslightly elevated
      highest 4.30 μg/lmedian 1.40 μg/l3 samples33 % below the limit of quantification

      Highest value: mŕtve rameno rieky Morava, lok. Rozpad2003, 430 m from the water. Comparison: percentile 89 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 4.00 μg/lmedian 1.00 μg/l3 samples67 % below the limit of quantification

      Highest value: mŕtve rameno rieky Morava, lok. Rozpad2003, 430 m from the water. Comparison: percentile 87 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 3.00 μg/lmedian 1.00 μg/l3 samples33 % below the limit of quantification

      Highest value: mŕtve rameno rieky Morava, lok. Rozpad2003, 430 m from the water. Comparison: percentile 83 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 1.00 μg/lmedian 0.500 μg/l3 samples67 % below the limit of quantification

      Highest value: mŕtve rameno rieky Morava, lok. Rozpad2003, 430 m from the water. Comparison: percentile 82 of all samples in Slovakia.

    • BariumBaslightly elevated
      highest 77.0 μg/lmedian 71.0 μg/l3 samples

      Highest value: mŕtve rameno rieky Morava2003, 310 m from the water. Comparison: percentile 81 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 11.0 μg/lmedian 5.00 μg/l3 samples67 % below the limit of quantification

      Highest value: Morava2003, 920 m from the water. Comparison: percentile 76 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l3 samples100 % below the limit of quantification

      Highest value: Morava2003, 920 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l3 samples100 % below the limit of quantification

      Highest value: Morava2003, 920 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l3 samples100 % below the limit of quantification

      Highest value: Morava, 920 m from the water. Comparison: percentile 26 of all samples in Slovakia.

    Major ions, mineralisation and pH

    Basic water chemistry: which rocks the minerals in it come from.

    • Silicon dioxideSiO2below half of Slovakia
      highest 9.89 mg/lmedian 2.92 mg/l3 samples

      Highest value: Morava2003, 920 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    Groundwater: chemistry, water types and radioactivity

    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.

    Metals in groundwater

    • AluminiumAlhigh (top 5 %)
      highest 0.140 mg/lmedian 0.0800 mg/l2 samples

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • ArsenicAshigh (top 5 %)
      highest 5.40 μg/lmedian 2.95 μg/l2 samples50 % below the limit of quantification

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • SeleniumSehigh (top 5 %)
      highest 2.70 μg/lmedian 1.60 μg/l2 samples50 % below the limit of quantification

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 0.700 μg/lmedian 0.400 μg/l2 samples50 % below the limit of quantification

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 1.90 μg/lmedian 1.08 μg/l2 samples50 % below the limit of quantification

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 89 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 3.60 μg/lmedian 2.50 μg/l2 samples

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 88 of all samples in Slovakia.

    • ZincZnslightly elevated
      highest 247 μg/lmedian 142 μg/l2 samples

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 80 of all samples in Slovakia.

    • LeadPbslightly elevated
      highest 1.00 μg/lmedian 0.750 μg/l2 samples50 % below the limit of quantification

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 75 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l2 samples100 % below the limit of quantification

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l2 samples100 % below the limit of quantification

      Highest value: studňa1994, 2.8 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 6.00 μg/lmedian 5.00 μg/l2 samples

      Highest value: vrt1994, 2.8 km from the water. Comparison: percentile 45 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    source28,16 Bq/l5.98 Bq/l
    stream, river20,760 Bq/l0.410 Bq/l
    well19,28 Bq/l9.28 Bq/l

    Mine workings, deposits and ore occurrences

    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.

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    Moravský Svätý Ján – Gergelík Igravelly sands and sandsMined deposit – SAND plus s.r.o.3.0 km
    Moravský Svätý Ján – Gergelíkgravelly sands and sandsMined deposit – SAND plus, s.r.o.3.2 km

    Boreholes and Geofond archive reports

    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.

    58 boreholes in the 3 km zone, of which 5 hydrogeological and 53 other; with an archive report number 52.

    Borehole depths

    • up to 10 m14×
    • 10–30 m24×
    • 30–100 m4×
    • 100–300 m0×
    • over 300 m5×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    km 44.650kengineering-geological15.0 m84381500 m
    km 44.650pengineering-geological5.0 m84381510 m
    km 43.600pengineering-geological12.0 m84381560 m
    km 42.600kengineering-geological10.5 m84381640 m
    km 44.850pengineering-geological12.0 m84381650 m
    km 42.600pengineering-geological5.0 m84381660 m
    km 42.900pengineering-geological11.0 m84381670 m
    km 42.100pengineering-geological11.0 m84381990 m
    Cf J-41deposit–66301.6 km
    Gb-14-73deposit452.0 m379911.6 km
    J-14engineering-geological20.0 m837191.9 km
    Moravský Svätý JánSHMÚ observation borehole16.0 m19159 130Bd5.pdf1.9 km

    How to read these data

    • Zone and distance. The distance is measured from the line of the water to the point in the register (to the centre for areas), with an accuracy of tens of metres. Counts apply only to the zone, not to the whole catchment.
    • Percentile. For chemistry, the highest value is compared with all atlas samples in Slovakia. It is not a legal limit or a health risk assessment; the atlases are historical (published: surface waters 2015, groundwater 1996, river sediments 1999).
    • Limit of quantification. Many samples have a value at the lowest level the laboratory can determine; such results mean "below the limit". For these, the position in the distribution is an estimate.
    • Panning concentrates. Only samples with a find are recorded. The number of grains in a concentrate is not the gold content in grams per tonne.
    • Relation to water. A mine working, landfill or burden nearby proves nothing about the quality of the water in the stream. It serves as a prompt for attention and a starting point for further investigation.
    • Sample points. The area and raster maps of ŠGÚDŠ cannot be downloaded as points, so along the line of each fishing district the value is looked up at points roughly every 3 km. It is a sample of the line, not a continuous record; a very short section may have a single point.
    • Atlas rasters. The chemistry of water and sediments is an interpolation of measurements in a sampling network (Geochemical Atlas of Slovakia). The value at a point is a modelled estimate for the surroundings, not a measurement in the water. The percentile compares the average of this stream with all sample points on streams in Slovakia.
    • Positions and scales. The maps have different scales (1:50,000 to 1:1,000,000), so the level of detail differs between sections. A map outside its coverage means there is no area at that point, not that there is nothing there.

    Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology.

    Organizations and location

    Who manages the fishing districts and where they are

    Organizations on the watercoursewho manages the fishing districts and what the conditions are there today

    1. Sekule1 fishing district · 2.1 km18OR Moravský Svätý Ján – dolné18

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    Danube basin