Watercourse

Klátovské rameno

fishing districts
2
fishing district length
30.3km
region
Trnava Region
Aerial image of watercourse Klátovské rameno 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 Klátovské rameno 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 2 fishing districts

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.
  • Very high0
  • High0
  • Average0
  • Low2

Best window today

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.

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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    Water state on the watercourse

    Measurement of water level, temperature and flow, weather by the watercourse and status from satellites

    Water levels on the watercourse

    StationStatusChangeTemperature
    Trhová Hradská68 cm6.6 °C
    Source: SHMÚUpdated 9 Nov 2026 03:57

    Elevation profile of the watercourse

    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.

    1101121141161180 km10 km20 km30 kmNo. 2No. 1
    Elevation profile of the watercourse: from 117 to 111 m a.s.l. over 30.2 km.
    Fishing districts in order from the highest (left) to the lowest. There may be a section without a fishing district between districts; it is not displayed.
    Highest point
    118 m a.s.l.
    Lowest point
    110 m a.s.l.
    Fall of the fishing districtsFallThe difference in altitude between the upper and lower end of the fishing district in metres. The greater the fall over a shorter length, the faster the water.
    7.1 m
    Average slopeWatercourse gradientFall per kilometre in per mille (‰, metres per kilometre). Up to 2 ‰ is a slow lowland river, 5 to 10 ‰ a foothill river (grayling, trout), above 10 ‰ a fast stream.
    0.2 ‰
    SinuositySinuosityThe length of the watercourse divided by the straight-line distance between its ends. 1.0 is a straight watercourse; above 1.3 it meanders strongly. Meanders create pools under the banks and shallows in the reaches between.
    1.60

    Source: Open Topo Data (eudem25m), 4 Nov 2026. Gradient and fall are approximate and include only the sections of fishing districts.

    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 Klátovské rameno from 2017
    2017imaged 1 Aug 2017
    Aerial image of watercourse Klátovské rameno from 2020
    2020imaged 20 Aug 2020
    Aerial image of watercourse Klátovské rameno from 2023
    2023imaged 29 Sep 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 Klátovské rameno 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

    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.

    • No unmet standard2

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

    2 of 2 fishing districts with measurements have groundwater nearby with a value above the limit for at least one indicator.

    • harmful substances above the standard at at least one station (metals, pesticides, PFAS, solvents)2

    Watercourse profile from source to mouthnumber of unmet indicators in 2025 at SHMÚ sites

    01234Trhová Hradská, river km 6.5: no failed standard (2025)Topoľníky, river km 3.0: no failed standard (2025)river km 7 (upper course)river km 3 (towards the mouth)
    Show sites in the table (2)
    • Trhová Hradskáriver km 6.5no unmet standard
    • Topoľníkyriver km 3.0no unmet standard
    • standard not met
    • no unmet standard
    • site not in the yearbook

    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 Klátovské rameno 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 (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.

    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 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.

    Elements in river sediment

    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.

    1 km2 km52 °C94 °C

    Heat underfoot

    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.

    20200

    Natural gamma radiation

    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.

    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

    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).

    Boreholes and groundwater analyses

    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.

    0 °C120

    Geothermal energy

    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.

    Environmental burdens and landfills

    10sites within 3 km

    10 landfills

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

    Deposits and ore occurrences

    10records within 5 km

    7 deposits, 3 ore occurrences

    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: resedimented alluvial fine-grained sands1×
    QuaternaryHolocenefluvial-organic sediments: fine-sandy, clay-like to rot-foot humus clays of dead arms and marshes1×
    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 cover130m
    • 150 – 20033%SR 0.6 %
    • 100 – 15033%SR 0.7 %
    • 80 – 10033%SR 0.1 %

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

    Neotectonic units

    • negative unit (lowland plains and basins, neotectonic depressions)100%SR 13 %

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

    Direction of neotectonic movements

    • large subsidence100%SR 2.8 %

    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)

    • Danube Basin100%SR 23 %

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

    Engineering-geological districts

    • region of peatlands60%SR 1.0 %
    • region of alluvial-plain deposits40%SR 15 %

    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 3 of 10 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.

    Aquifer rocks (hydrogeological map 1:200,000)

    • Gravel100%SR 52 %

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

    Aquifer type

    • Zvodnence s prevažne medzizrnovým typom priepustnosti (prevažne nespevnené sedimenty) (Gravel; Fluviálne)100%SR 27 %

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

    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 southwestern part of the Danube Plain100%SR 5.3 %

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

    Genetic type of groundwater

    • fluviogenic100%SR 14 %

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

    Chemical type of groundwater

    • Ca-SO4-HCO380%SR 3.8 %
    • Ca-Mg-HCO320%SR 26 %

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

    Groundwater quality class

    • D90%SR 15 %
    • H10%SR 8.8 %

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

    Geothermal groundwater bodies

    • Central depression of the Danube Basin100%SR 21 %

    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 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.

    Water hardness

    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.

    Dissolved substances

    520mg/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–Mg–HCO₃–SO₄

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

    Major ions

    • SulphatesSO485.4 mg/lpercentile 84
    • ChloridesCl33.3 mg/lpercentile 82
    • CalciumCa88.5 mg/lpercentile 78
    • MagnesiumMg24.3 mg/lpercentile 76
    • SodiumNa15.1 mg/lpercentile 71
    • BicarbonatesHCO3247 mg/lpercentile 62
    • FluoridesF0.129 mg/lpercentile 57
    • PotassiumK2.92 mg/lpercentile 49

    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

    • NitratesNO312.8 mg/lpercentile 81
    • PhosphatesPO40.251 mg/lpercentile 64
    • AmmoniumNH40.0984 mg/lpercentile 46
    • Chemical oxygen demandChSK2.18 mg/lpercentile 24

    Metals

    • ZincZn12.8 μg/lpercentile 73
    • IronFe0.163 mg/lpercentile 69
    • ManganeseMn42.8 μg/lpercentile 58
    • AluminiumAl46.7 μg/lpercentile 41

    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

    • SeleniumSe0.949 mg/kgpercentile 95
    • ZincZn182 mg/kgpercentile 87
    • CadmiumCd0.403 mg/kgpercentile 80
    • MercuryHg0.245 mg/kgpercentile 79
    • LeadPb22.7 mg/kgpercentile 77
    • BismuthBi0.300 mg/kgpercentile 73
    • CopperCu30.2 mg/kgpercentile 71
    • ArsenicAs8.69 mg/kgpercentile 70
    • TinSn2.66 mg/kgpercentile 50
    • CobaltCo8.35 mg/kgpercentile 48
    • NickelNi23.6 mg/kgpercentile 45
    • MolybdenumMo0.320 mg/kgpercentile 38
    • AntimonySb0.508 mg/kgpercentile 36
    • VanadiumV58.2 mg/kgpercentile 25
    • ChromiumCr52.0 mg/kgpercentile 19

    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)
    • MagnesiumMg2.56 %percentile 93
    • CalciumCa8.47 %percentile 92
    • PhosphorusP1,170 mg/kgpercentile 82
    • IronFe2.44 %percentile 35
    • SodiumNa0.760 %percentile 28
    • PotassiumK1.34 %percentile 24
    • AluminiumAl4.76 %percentile 18
    • ManganeseMn580 mg/kgpercentile 15
    • TitaniumTi3,036 mg/kgpercentile 7
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • StrontiumSr207 mg/kgpercentile 89
    • LithiumLi26.8 mg/kgpercentile 34
    • GalliumGa11.8 mg/kgpercentile 32
    • BariumBa376 mg/kgpercentile 26
    • RubidiumRb76.9 mg/kgpercentile 22
    • BoronB49.2 mg/kgpercentile 22
    • BerylliumBe0.603 mg/kgpercentile 10
    • CeriumCe45.1 mg/kgpercentile 10
    • YttriumY16.3 mg/kgpercentile 7
    • ZirconiumZr164 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

    49nGy/h in air

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

    Radon risk of the bedrock

    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.

    • Equivalent uranium (eU)eU2.71 ppm66th percentile
    • Potassium (K)K1.27 %percentile 35
    • Equivalent thorium (eTh)eTh6.55 ppm21th 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 137CsCS1372,603 Bq/m²percentile 82

    Radon risk by isopleths

    • medium100%SR 64 %

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

    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

    +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.

    Bouguer gravity anomaly

    -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.

    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 km52 °C94 °C

    Rock temperature with depth

    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.

    Geothermal groundwater bodies beneath the water line

    • Central depression of the Danube Basin100%SR 21 %

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

    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)103–191m a.s.l.
    • Average elevation of the units119m a.s.l.
    • Average slope0.4°
    • Average January temperature-2.5°C
    • Average July temperature20.0°C
    • Annual precipitation590mm

    Geomorphological units

    • Danubian Plain100%SR 8.4 %

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

    Geomorphological regions

    • Danubian Lowland100%SR 18 %

    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 not susceptible to acidification100%SR 27 %

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

    Soil contamination (map 1:500,000)

    • relatively clean soil100%SR 53 %

    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.

    Jahodná – za cintorínon – Dunajský Klátov – none (140 m from the water)Trhová Hradská – permanent (200 m from the water)Topoľníky – Dolné – Dolné Topoľníky – none (420 m from the water)Kútniky – medzi traťou – Trhová Hradská – permanent (450 m from the water)Jahodná – pri Malom Dunaji – Horné Mýto – permanent (500 m from the water)Malé Dvorníky – pri cintoríne. – Malé Dvorníky – cannot be estimated (510 m from the water)Dolný Štál – Dolné Topoľníky – none (670 m from the water)Dolný Štál – bývalé ihrisko – Dolné Topoľníky – cannot be estimated (1.6 km from the water)Malé Dvorníky – cannot be estimated (2.0 km from the water)Ohrady – permanent (2.4 km from the water)Topoľníky – FGT-1 – non-spa (190 m from the water)Dunajský Klátov – VDK-15 – non-spa (270 m from the water)Dunajská Streda – DS-1 – non-spa (7.5 km from the water)Dunajská Streda – DS-2 – non-spa (7.8 km from the water)Boheľov – GPB-1 – non-spa (8.3 km from the water)VDK-15 – l3 (1.0 km from the water)FGT-1 – l3 (1.3 km from the water)DS-1,2 – m3 (6.5 km from the water)VFP-12-R – l3 (9.7 km from the water)a1 (120 m from the water)a1 (870 m from the water)a1 (8.0 km from the water)a1 (8.7 km from the water)a1 (8.9 km from the water)a1 (9.5 km from the water)Topoľníky (2.4 km from the water)Dunajská Streda (7.1 km from the water)Dunajský Klátov – gravelly sands and sands (210 m from the water)Čečínska Potôň – gravelly sands and sands (1.4 km from the water)Čečínska Potôň II – gravelly sands and sands (1.8 km from the water)Mostová – Šoriakoš – gravelly sands and sands (2.1 km from the water)Čečínska Potôň III – Jazero Ikra – gravelly sands and sands (2.2 km from the water)Nové Osady – gravelly sands and sands (4.1 km from the water)Ostrov – gravelly sands and sands (4.6 km from the water)Topoľníky – brick raw materials (110 m from the water)Trhová Hradská – brick raw materials (240 m from the water)Ohrady – gravelly sands (4.0 km from the water)Klátovské rameno – hydrogeology (30 m from the water)Dunajský Klátov-Csotfa – širokoprofilový vrt (Ø vŕtania nad 600 m (80 m from the water)Dunajský Klátov – úzkoprofilový vrt s obyčajnou pitnou a ú (90 m from the water)Dunajský Klátov – úzkoprofilový vrt s obyčajnou pitnou a ú (90 m from the water)Topoľníky – širokoprofilový vrt (Ø vŕtania nad 600 m (90 m from the water)Dunajský Klátov (100 m from the water)Horné Mýto – širokoprofilový vrt (Ø vŕtania nad 600 m (100 m from the water)Dunajský Klátov – monitoring borehole (110 m from the water)Jahodná – širokoprofilový vrt (Ø vŕtania nad 600 m (120 m from the water)Topoľníky – structural borehole with thermal water, minerálnou v (190 m from the water)Topoľníky – širokoprofilový vrt (Ø vŕtania nad 600 m (210 m from the water)Dunajský Klátov-Kele Majeť – SHMÚ observation borehole (220 m from the water)Dunajský Klatov – úzkoprofilový vrt s obyčajnou pitnou a ú (220 m from the water)Dunajský Klátov – monitoring borehole (250 m from the water)Dunajský Klátov-farma Lang – širokoprofilový vrt (Ø vŕtania nad 600 m (250 m from the water)Dunajský Klátov – monitoring borehole (260 m from the water)Dunajský Klátov – monitoring borehole (270 m from the water)Dunajský Klátov – monitoring borehole (270 m from the water)Dunajský Klátov – structural borehole with thermal water, minerálnou v (270 m from the water)Dunajský Klátov – monitoring borehole (280 m from the water)Dunajský Klátov – monitoring borehole (280 m from the water)Dunajský Klátov – monitoring borehole (300 m from the water)Dunajský Klátov – monitoring borehole (310 m from the water)Dunajský Klátov – úzkoprofilový vrt s obyčajnou pitnou a ú (310 m from the water)Dunajský Klatov – úzkoprofilový vrt s obyčajnou pitnou a ú (330 m from the water)Dunajský Klátov – monitoring borehole (330 m from the water)Trhové Mýto – širokoprofilový vrt (Ø vŕtania nad 600 m (340 m from the water)Topoľníky – monitoring borehole (390 m from the water)Dunajský Klátov – monitoring borehole (420 m from the water)Dunajský Klátov – širokoprofilový vrt (Ø vŕtania nad 600 m (440 m from the water)Topoľníky – úzkoprofilový vrt s obyčajnou pitnou a ú (450 m from the water)Dun.Klatov – širokoprofilový vrt (Ø vŕtania nad 600 m (510 m from the water)Topoľníky – monitoring borehole (520 m from the water)Trhové Mýto – širokoprofilový vrt (Ø vŕtania nad 600 m (580 m from the water)Dunajský Klátov – úzkoprofilový vrt s obyčajnou pitnou a ú (600 m from the water)Jahodná – SHMÚ observation borehole (640 m from the water)Topoľníky – úzkoprofilový vrt s obyčajnou pitnou a ú (640 m from the water)Bogdany – SHMÚ observation borehole (700 m from the water)Topoľníky – úzkoprofilový vrt s obyčajnou pitnou a ú (700 m from the water)Topoľníky – širokoprofilový vrt (Ø vŕtania nad 600 m (710 m from the water)Trhové Mýto – širokoprofilový vrt (Ø vŕtania nad 600 m (780 m from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (20 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (60 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (70 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (70 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (80 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (90 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (90 m from the water)vodárensky využívaný vrt – Hydrogeological boreholes (90 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (100 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (100 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (110 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (120 m from the water)termálne vody – Hydrogeological boreholes (190 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (210 m from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (220 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (220 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (250 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (250 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (250 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (260 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (260 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (270 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (270 m from the water)termálne vody – Hydrogeological boreholes (270 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (280 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (280 m from the water)zrážkomerná stanica – Artificial hydrogeologically significant objects (290 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (300 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (310 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (310 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (330 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (330 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (340 m from the water)vodárensky využívaný vrt – Hydrogeological boreholes (340 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (370 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (390 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (420 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (440 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (450 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (510 m from the water)Dunajský Klatov – borehole (90 m from the water)Dunajský Klatov – borehole (90 m from the water)Topolniky – borehole (90 m from the water)Topolniky – borehole (90 m from the water)Dunajský Klatov – borehole (100 m from the water)Horné Mýto – borehole (100 m from the water)Dunajský Klatov – borehole (110 m from the water)Jahodná – borehole (120 m from the water)Cudov, 1700m S od K114 – well (120 m from the water)Dunajský Klatov – borehole (130 m from the water)Dunajsky Klatov,900m SV od K114 – borehole (160 m from the water)Dunajský Klatov, 900m SV od K114 – borehole (160 m from the water)Orechová Pôtoň-Lúky, 2000m SV od K117 – well (160 m from the water)Orechova Poton-Luky,2000m SV od K117 – well (160 m from the water)Horné Mýto, 900m JJZ od K114 – well (170 m from the water)Orechová Pôtoň-Lúky, 2400m VSV od K117 – borehole (180 m from the water)Orechova Poton-Luky,2400m VSV od K117 – borehole (180 m from the water)Dunajský Klatov – borehole (220 m from the water)Dunajský Klatov – borehole (220 m from the water)Dunajský Klatov – borehole (230 m from the water)Topolniky – borehole (230 m from the water)Dunajský Klatov – borehole (240 m from the water)Žitný ostrov – oblasť 21/1, vrt P3 – borehole (270 m from the water)Dunajský Klatov – borehole (270 m from the water)Dunajský Klatov – borehole (270 m from the water)Dunajský Klatov – borehole (270 m from the water)Dunajský Klatov – borehole (300 m from the water)Dunajský Klatov – borehole (300 m from the water)Dunajský Klatov – borehole (310 m from the water)Dunajský Klatov – borehole (310 m from the water)Trhové Mýto – borehole (360 m from the water)Dunajský Klatov – borehole (400 m from the water)Dunajsky Klatov – borehole (480 m from the water)Orechová Pôtoň-Lúky, 1700m SV od K117 – well (520 m from the water)Orechova Poton-Luky,1700m SV od K117 – well (520 m from the water)Dunajský Klatov, 500m SV od K114 – borehole (530 m from the water)Trhová Hradská – RD, 1000m JV od K112 – borehole (530 m from the water)Jahodna,750m SV od K114 – borehole (550 m from the water)Dunajsky Klatov – borehole (570 m from the water)Trhové Mýto-Trhová Hradská, 700m Z od K112 – borehole (590 m from the water)5 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.

    • LithiumLihigh (top 5 %)
      highest 68.0 μg/lmedian 29.5 μg/l10 samples10 % below the limit of quantification

      Highest value: bez mena, Starý Klátovský kanál a Klátovský kanál – sútok2011, 920 m from the water. Comparison: percentile 97 of all samples in Slovakia.

    • ArsenicAselevated (top 10 %)
      highest 5.00 μg/lmedian 1.00 μg/l11 samples45 % below the limit of quantification

      Highest value: KLÁTOVSKÉ RAMENO1995, 30 m from the water. Comparison: percentile 92 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.570 μg/lmedian 0.570 μg/l1 sample

      Highest value: Malý Dunaj1997, 930 m from the water. Comparison: percentile 76 of all samples in Slovakia.

    • StrontiumSrtypical value
      highest 300 μg/lmedian 300 μg/l1 sample

      Highest value: Malý Dunaj1997, 930 m from the water. Comparison: percentile 72 of all samples in Slovakia.

    • CopperCutypical value
      highest 2.00 μg/lmedian 1.00 μg/l10 samples80 % below the limit of quantification

      Highest value: bez mena, Starý Klátovský kanál a Klátovský kanál – sútok2011, 920 m from the water. Comparison: percentile 66 of all samples in Slovakia.

    • BariumBatypical value
      highest 47.0 μg/lmedian 37.0 μg/l9 samples

      Highest value: Klátovský kanál2011, 510 m from the water. Comparison: percentile 57 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification

      Highest value: Klátovské rameno2011, 60 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l10 samples100 % below the limit of quantification

      Highest value: Klátovské rameno2011, 60 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • ChromiumCrbelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l10 samples100 % below the limit of quantification

      Highest value: Klátovské rameno2011, 60 m from the water. Comparison: percentile 32 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l10 samples100 % below the limit of quantification

      Highest value: Klátovské rameno, 60 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 10.4 mg/lmedian 8.30 mg/l10 samples

      Highest value: Klátovské rameno2011, 150 m from the water. Comparison: percentile 49 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.

    Chemical water types nearby

    • Ca-Mg-HCO355×
    • Ca-Mg-HCO3-SO428×
    • Ca-Mg-SO4-HCO312×
    • Mg-HCO32×
    • Ca-SO4-HCO31×
    • Ca-Mg-SO4-NO3-HCO31×
    • Mg-Na-SO4-Cl1×
    • Ca-HCO3-SO41×

    Water quality class according to the hydrogeochemical map

    • class D33×
    • class H26×
    • class B20×
    • class C11×
    • class A7×
    • class F4×
    • class G1×

    Metals in groundwater

    • LithiumLiextreme (top 1 %)
      highest 700 μg/lmedian 4.50 μg/l52 samples

      Highest value: studňa1994, 2.5 km from the water. Comparison: percentile 100 of all samples in Slovakia.

    • CadmiumCdextreme (top 1 %)
      highest 654 μg/lmedian 0.250 μg/l52 samples98 % below the limit of quantification

      Highest value: vrt1993, 1.3 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • ChromiumCrextreme (top 1 %)
      highest 25.0 μg/lmedian 0.600 μg/l52 samples42 % below the limit of quantification

      Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • CopperCuextreme (top 1 %)
      highest 19.1 μg/lmedian 1.10 μg/l52 samples

      Highest value: studňa1994, 660 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • ArsenicAsextreme (top 1 %)
      highest 42.0 μg/lmedian 0.500 μg/l52 samples83 % below the limit of quantification

      Highest value: studňa1993, 2.8 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • ZincZnextreme (top 1 %)
      highest 5,490 μg/lmedian 107 μg/l52 samples

      Highest value: studňa1994, 690 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • LeadPbhigh (top 5 %)
      highest 6.00 μg/lmedian 1.00 μg/l52 samples48 % below the limit of quantification

      Highest value: vrt1993, 180 m from the water. Comparison: percentile 97 of all samples in Slovakia.

    • SeleniumSehigh (top 5 %)
      highest 3.50 μg/lmedian 0.500 μg/l52 samples90 % below the limit of quantification

      Highest value: studňa1994, 2.5 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 1.00 μg/lmedian 0.100 μg/l52 samples63 % below the limit of quantification

      Highest value: studňa1994, 2.5 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • MercuryHghigh (top 5 %)
      highest 0.200 μg/lmedian 0.100 μg/l52 samples98 % below the limit of quantification

      Highest value: studňa1993, 1.5 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • AluminiumAlelevated (top 10 %)
      highest 0.0400 mg/lmedian 0.0100 mg/l52 samples37 % below the limit of quantification

      Highest value: studňa1994, 2.7 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l16 samples100 % below the limit of quantification

      Highest value: vrt1994, 3.0 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    water source for individual supply27,98 Bq/l6.27 Bq/l
    free-flowing borehole with thermal and mineral water212,9 Bq/l6.54 Bq/l
    well1014,8 Bq/l3.09 Bq/l
    water source for public supply17,06 Bq/l7.06 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
    Dunajský Klátovgravelly sands and sandsMined deposit – ŠKOLSKÉ HOSPODÁRSTVO – BÚŠLAK, spol. s r.o.210 m
    Čečínska Potôňgravelly sands and sandsMined deposit – MEUM, a.s.1.4 km
    Čečínska Potôň IIgravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – GOBIO, s.r.o.1.8 km
    Mostová – Šoriakošgravelly sands and sandsMined deposit – DELTA stone s.r.o.2.1 km
    Čečínska Potôň III – Jazero Ikragravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – IKRA s.r.o.2.2 km
    Nové Osadygravelly sands and sandsDeposit with halted mining or where use of reserves is not expected – bez organizácie4.1 km
    Ostrovgravelly sands and sandsMined deposit – R 5 C s.r.o.4.6 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.

    275 boreholes in the 3 km zone, of which 77 hydrogeological and 198 other; with an archive report number 275.

    Borehole depths

    • up to 10 m176×
    • 10–30 m50×
    • 30–100 m36×
    • 100–300 m2×
    • over 300 m4×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    J-17engineering-geological2.0 m5564430 m
    Z-19deposit5.0 m6974650 m
    Dunajský Klátov-Csotfawide-diameter borehole80.0 m58592 144Cd30.pdf80 m
    J-8engineering-geological2.0 m5564480 m
    J-3engineering-geological2.0 m5564480 m
    S-15engineering-geological12.0 m1224080 m
    Z-17deposit5.0 m6974680 m
    Dunajský Klátovnarrow-diameter borehole with ordinary drinking and process water–67337 144Cd48.pdf90 m
    Dunajský Klátovnarrow-diameter borehole with ordinary drinking and process water–67338 144Cd47.pdf90 m
    Topoľníkywide-diameter borehole30.0 m51331 12Ba8.pdf90 m
    J-1engineering-geological2.5 m5564490 m
    J-2engineering-geological2.0 m5564490 m

    Geothermal energy and mineral waters

    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.

    BoreholeTemperatureYieldDepthChemical water typeUseFrom the water
    Topoľníky – FGT-174 °C23.0 l/s2501 mNa-HCO3-Clin use190 m
    Dunajský Klátov – VDK-1574 °C15.4 l/s2240 mNa-HCO3-Clunused270 m
    Dunajská Streda – DS-191 °C15.2 l/s2500 mNa-Cl-HCO3in use7.5 km
    Dunajská Streda – DS-255 °C23.0 l/s1600 mNa-HCO3in use7.8 km
    Boheľov – GPB-1––2800 m–unused8.3 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 56120 m
    VDK-15geothermal water55 – 8016 – 3011.0 km
    FGT-1geothermal water55 – 8016 – 3011.3 km
    category Topoľníkythermal baths––12.4 km
    DS-1.2geothermal water80 – 10016 – 3016.5 km
    category Dunajská Stredathermal baths––17.1 km
    VFP-12-Rgeothermal water55 – 8016 – 3019.7 km

    Environmental burdens, landfills and anthropogenic sediments

    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.

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom the water
    Jahodná – za cintorínon – Dunajský Klátov–1970–140 m
    Trhová Hradská–1970–200 m
    Topoľníky – Dolné – Dolné Topoľníky5 950 m²1989–420 m
    Kútniky – medzi traťou – Trhová Hradská18 000 m²1970–450 m
    Jahodná – pri Malom Danube – Horné Mýto–1965–500 m
    Malé Dvorníky – pri cintoríne. – Malé Dvorníky–1960–510 m
    Dolný Štál – Dolné Topoľníky3 000 m²1970–670 m
    Dolný Štál – bývalé ihrisko – Dolné Topoľníky5 000 m²1970–1.6 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.
    • Šlichy. 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. Dunajská Streda1 fishing district · 26 km22Klátovské rameno č. 222
    2. Topoľníky1 fishing district · 4.3 km22Klátovské rameno č. 122

    More watercourses nearby

    Danube basin