Watercourse

OR Žlutnica

fishing district
1
fishing district length
0.4km
region
Trnava Region
Aerial image of watercourse OR Žlutnica 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 Žlutnica 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

06:00–08:00

OR Žlutnica, window score 27.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 07:04.

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 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.

    1581591601611621631640.0 km0.1 km0.2 km0.3 km
    Elevation profile of the watercourse: from 163 to 159 m a.s.l. over 0.4 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
    161 m a.s.l.
    Lowest point
    161 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.
    0.1 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.
    0.3 ‰
    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.
    1.01

    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 OR Žlutnica from 2017
    2017imaged 24 Aug 2017
    Aerial image of watercourse OR Žlutnica from 2020
    2020imaged 22 Aug 2020
    Aerial image of watercourse OR Žlutnica from 2023
    2023imaged 14 Aug 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 Žlutnica watercourse

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

    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

    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 Žlutnica 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 (0 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.

    510

    Water according to the atlas

    pH 8.3modelled estimate

    water type Ca–HCO₃–SO₄

    Mineralisation 558 mg/l, hard water (17.8 °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: Copper 63.4 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 92. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km35 °C65 °C

    Heat underfoot

    35°C at 1,000 m depth

    heat flow 50 mW/m²

    At a depth of 2,000 m about 65 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    47nGy/h dose rate

    percentile 22 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

    –

    There is no measurement in the surface water atlas samples within 1 km of the water.

    Boreholes and groundwater analyses

    29boreholes within 3 km

    25 water analyses nearby

    Of these, 29 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    2 geothermal and mineral water springs within 10 km.

    Environmental burdens and landfills

    4sites within 3 km

    4 landfills

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

    Deposits and ore occurrences

    0records within 5 km

    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.

    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.

    Main hydrogeological region

    • Quaternary of the Morava up to Brodské100%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 8.33typical 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

    17.8°dH, hard

    Sum of calcium and magnesium (3.17 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    558mg/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–SO₄

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

    Major ions

    • PotassiumK9.47 mg/lpercentile 91
    • SodiumNa28.0 mg/lpercentile 88
    • SulphatesSO489.8 mg/lpercentile 86
    • CalciumCa91.2 mg/lpercentile 81
    • ChloridesCl29.8 mg/lpercentile 80
    • MagnesiumMg21.9 mg/lpercentile 71
    • BicarbonatesHCO3277 mg/lpercentile 70
    • FluoridesF0.123 mg/lpercentile 54

    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

    • AmmoniumNH40.382 mg/lpercentile 82
    • PhosphatesPO40.421 mg/lpercentile 76
    • Chemical oxygen demandChSK4.42 mg/lpercentile 74
    • NitratesNO310.1 mg/lpercentile 73

    Metals

    • ZincZn25.0 μg/lpercentile 91
    • ManganeseMn40.6 μg/lpercentile 57
    • AluminiumAl33.2 μg/lpercentile 32
    • IronFe0.0552 mg/lpercentile 25

    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

    • CopperCu63.4 mg/kgpercentile 92
    • CadmiumCd0.441 mg/kgpercentile 83
    • ChromiumCr101 mg/kgpercentile 82
    • MercuryHg0.169 mg/kgpercentile 70
    • ZincZn119 mg/kgpercentile 68
    • SeleniumSe0.318 mg/kgpercentile 66
    • CobaltCo9.37 mg/kgpercentile 64
    • NickelNi26.6 mg/kgpercentile 59
    • ArsenicAs6.97 mg/kgpercentile 54
    • BismuthBi0.213 mg/kgpercentile 48
    • MolybdenumMo0.324 mg/kgpercentile 39
    • VanadiumV61.5 mg/kgpercentile 33
    • LeadPb10.9 mg/kgpercentile 19
    • TinSn1.69 mg/kgpercentile 10
    • AntimonySb0.255 mg/kgpercentile 6

    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)
    • PhosphorusP1,207 mg/kgpercentile 84
    • CalciumCa3.71 %percentile 72
    • PotassiumK1.63 %percentile 67
    • ManganeseMn829 mg/kgpercentile 48
    • IronFe2.52 %percentile 40
    • TitaniumTi4,182 mg/kgpercentile 39
    • AluminiumAl5.28 %percentile 38
    • MagnesiumMg0.716 %percentile 28
    • SodiumNa0.707 %percentile 19
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • ZirconiumZr495 mg/kgpercentile 78
    • GalliumGa17.3 mg/kgpercentile 77
    • CeriumCe64.8 mg/kgpercentile 68
    • RubidiumRb94.1 mg/kgpercentile 65
    • StrontiumSr144 mg/kgpercentile 56
    • LithiumLi29.9 mg/kgpercentile 52
    • BariumBa415 mg/kgpercentile 42
    • YttriumY25.6 mg/kgpercentile 38
    • BerylliumBe1.07 mg/kgpercentile 31
    • BoronB53.3 mg/kgpercentile 30

    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

    47nGy/h in air

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

    • Potassium (K)K1.28 %percentile 40
    • Equivalent thorium (eTh)eTh6.85 ppm28th percentile
    • Equivalent uranium (eU)eU2.22 ppm16th 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)

    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

    +95nT

    range 95 to 95 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.

    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 km35 °C65 °C

    Rock temperature with depth

    35 / 65 °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.

    Susceptibility of soils to acidification

    • soils susceptible to acidification100%SR 31 %

    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.

    Kátov – permanent (1.8 km from the water)Skalica – occasional (2.0 km from the water)Skalica – occasional (2.5 km from the water)Skalica – permanent (2.6 km from the water)a1 (7.1 km from the water)a1 (7.5 km from the water)Holíč – úzkoprofilový vrt s obyčajnou pitnou a ú (1.5 km from the water)Holíč – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Holíč – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Skalica – úzkoprofilový vrt s obyčajnou pitnou a ú (2.4 km from the water)Holíč – úzkoprofilový vrt s obyčajnou pitnou a ú (2.6 km from the water)Skalica – úzkoprofilový vrt s obyčajnou pitnou a ú (2.7 km from the water)Holíč – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Skalica – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Holíč – úzkoprofilový vrt s obyčajnou pitnou a ú (2.8 km from the water)Holíč – úzkoprofilový vrt s obyčajnou pitnou a ú (2.9 km from the water)Holíč – širokoprofilový vrt (Ø vŕtania nad 600 m (2.9 km from the water)Skalica – úzkoprofilový vrt s obyčajnou pitnou a ú (3.0 km from the water)Holíč – SHMÚ observation borehole (3.0 km from the water)Holíč – monitoring borehole (3.0 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.5 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.9 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.3 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.4 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.7 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.7 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.8 km from the water)vrt s prelivom – Hydrogeological boreholes (2.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.9 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (3.0 km from the water)2 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.

    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

    • CopperCuextreme (top 1 %)
      highest 91.0 μg/lmedian 47.7 μg/l2 samples

      Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • LithiumLihigh (top 5 %)
      highest 90.0 μg/lmedian 49.0 μg/l2 samples

      Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • MercuryHghigh (top 5 %)
      highest 0.300 μg/lmedian 0.250 μg/l2 samples

      Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • LeadPbelevated (top 10 %)
      highest 2.00 μg/lmedian 1.50 μg/l2 samples

      Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • AntimonySbslightly elevated
      highest 0.300 μg/lmedian 0.200 μg/l2 samples50 % below the limit of quantification

      Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 87 of all samples in Slovakia.

    • ZincZnslightly elevated
      highest 272 μg/lmedian 185 μg/l2 samples

      Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 81 of all samples in Slovakia.

    • ChromiumCrtypical value
      highest 0.500 μg/lmedian 0.375 μg/l2 samples50 % below the limit of quantification

      Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 66 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l2 samples100 % below the limit of quantification

      Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 50 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: studňa1993, 2.1 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l2 samples100 % below the limit of quantification

      Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 39 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l2 samples100 % below the limit of quantification

      Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 38 of all samples in Slovakia.

    • AluminiumAlbelow half of Slovakia
      highest 0.00500 mg/lmedian 0.00500 mg/l2 samples100 % below the limit of quantification

      Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 30 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    well113,2 Bq/l13.2 Bq/l

    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.

    29 boreholes in the 3 km zone, of which 14 hydrogeological and 15 other; with an archive report number 29.

    Borehole depths

    • up to 10 m20×
    • 10–30 m7×
    • 30–100 m0×
    • 100–300 m1×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    P-1hydrogeological6.0 m164901.3 km
    Holíčnarrow-diameter borehole with ordinary drinking and process water8.8 m17458 119Ad20.pdf1.5 km
    Holíčnarrow-diameter borehole with ordinary drinking and process water9.5 m17458 119Ad21.pdf1.8 km
    Holíčnarrow-diameter borehole with ordinary drinking and process water7.7 m17458 119Cb6.pdf2.4 km
    JV-8engineering-geological10.0 m845702.4 km
    Skalicanarrow-diameter borehole with ordinary drinking and process water9.0 m16490 119Ad12.pdf2.4 km
    HV-8hydrogeological9.0 m164902.5 km
    S-2hydrogeological8.0 m64802.5 km
    Holíčnarrow-diameter borehole with ordinary drinking and process water9.0 m17458 119Cb5.pdf2.6 km
    V-1engineering-geological9.0 m979532.7 km
    V-2engineering-geological6.0 m979532.7 km
    Skalicanarrow-diameter borehole with ordinary drinking and process water12.0 m16490 119Ad8.pdf2.7 km

    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.

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 527.1 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
    Kátov2 400 m²1975–1.8 km
    Skalica15 000 m²1960–2.0 km
    Skalica55 000 m²1976–2.5 km
    Skalica4 800 m²1972–2.6 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. Skalica1 fishing district · 0.4 km28OR Žlutnica28

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