Watercourse

VN Horné Orešany

fishing district
1
fishing district length
2.0km
region
Trnava Region
Aerial image of watercourse VN Horné Orešany 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 VN Horné Orešany 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

VN Horné Orešany, window score 33.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 16:16.

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
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    Elevation profile: reservoir

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

    Reservoir This is a reservoir, so the watercourse is not assessed here: the water has no current, fall or gradient. The chart shows the terrain height along the fishing district.

    2152202252302352400.0 km0.5 km1.0 km1.5 km
    Terrain elevation profile (Reservoir): from 235 to 218 m a.s.l. over 2.0 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    218 m a.s.l.
    Lowest point of the profile
    218 m a.s.l.
    Highest point of the profile
    235 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 VN Horné Orešany from 2017
    2017imaged 22 May 2017
    Aerial image of watercourse VN Horné Orešany from 2020
    2020imaged 28 Aug 2020
    Aerial image of watercourse VN Horné Orešany from 2023
    2023imaged 28 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 VN Horné Orešany 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

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

    Source: SHMÚ (yearbooks on surface and groundwater quality), the register of wastewater treatment plants from VÚVH and the EEA. A SHMÚ site is assigned to a fishing district by the same watercourse name and by distance; the yearbook lists the sites that failed the standard, so a missing site is not proof of clean water.

    Geology and geochemistry of the VN Horné Orešany 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 7.8modelled estimate

    water type Ca–Mg–HCO₃

    Mineralisation 517 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

    0 from 15elements in the top 10 %

    highest: Bismuth 0.245 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 60. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km35 °C65 °C

    Heat underfoot

    35°C at 1,000 m depth

    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

    52nGy/h dose rate

    percentile 61 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

    1object within 3 km

    Nearest: Kutacie práce na kopci Jahodník (other type of object), 2.8 km from the water.

    Gold in river sediment

    0samples with gold

    10 ore minerals in the sediment

    No gold was found in river sediment samples within 1 km of the water. The samples do not cover every stream, so this does not mean there is no gold here.

    Trace elements in the stream water

    1 from 9indicators in the top 5 %

    highest: Copper 13.7 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 96 (Smutná, potok).

    Boreholes and groundwater analyses

    52boreholes within 3 km

    223 water analyses nearby

    Of these, 38 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    5 geothermal and mineral water springs within 10 km.

    Environmental burdens and landfills

    10sites within 3 km

    1 environmental burden, 9 landfills

    Nearest burden: Horné Orešany – časť Majdan – bývalá chemická továreň, 160 m from the water. Proximity does not mean that substances leak from the site into the water.

    Deposits and ore occurrences

    9records within 5 km

    2 deposits, 7 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: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains1×

    Quaternary cover

    • deluvial sediments100%SR 16 %

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

    Tectonic units

    • FATRIKUM100%SR 14 %

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

    Tectonic division

    • Paleo-Alpine tectonic units of the Inner Western Carpathians100%SR 16 %

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

    Regional geological division

    • core mountains100%SR 11 %

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

    Regional geological division (subunits)

    • Malé Karpaty100%SR 1.4 %

    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 1 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)

    • Sandstones100%SR 15 %

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

    Aquifer type

    • Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Sandstones)100%SR 15 %

    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

    • crystalline and Mesozoic of the southeastern part of the Pezinok Carpathians100%SR 0.0 %

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

    Genetic type of groundwater

    • silicate-carbonate to polygenic100%SR 1.1 %

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

    Groundwater quality class

    • A100%SR 36 %

    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 7.79typical 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 (3.22 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    517mg/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

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

    Major ions

    • BicarbonatesHCO3323 mg/lpercentile 82
    • CalciumCa92.9 mg/lpercentile 82
    • MagnesiumMg22.0 mg/lpercentile 71
    • SulphatesSO453.1 mg/lpercentile 64
    • FluoridesF0.124 mg/lpercentile 55
    • ChloridesCl5.50 mg/lpercentile 37
    • SodiumNa5.06 mg/lpercentile 28
    • PotassiumK1.83 mg/lpercentile 28

    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

    • NitratesNO313.1 mg/lpercentile 82
    • AmmoniumNH40.0962 mg/lpercentile 45
    • Chemical oxygen demandChSK2.77 mg/lpercentile 40
    • PhosphatesPO40.0383 mg/lpercentile 21

    Metals

    • ZincZn16.9 μg/lpercentile 82
    • ManganeseMn38.2 μg/lpercentile 55
    • AluminiumAl31.5 μg/lpercentile 30
    • IronFe0.0270 mg/lpercentile 8

    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

    • BismuthBi0.245 mg/kgpercentile 60
    • CobaltCo8.19 mg/kgpercentile 46
    • SeleniumSe0.220 mg/kgpercentile 43
    • CadmiumCd0.156 mg/kgpercentile 43
    • LeadPb14.3 mg/kgpercentile 42
    • ZincZn89.2 mg/kgpercentile 42
    • NickelNi21.9 mg/kgpercentile 36
    • CopperCu19.3 mg/kgpercentile 30
    • AntimonySb0.425 mg/kgpercentile 27
    • ArsenicAs4.94 mg/kgpercentile 24
    • MercuryHg0.0609 mg/kgpercentile 22
    • MolybdenumMo0.221 mg/kgpercentile 19
    • ChromiumCr51.5 mg/kgpercentile 18
    • VanadiumV52.9 mg/kgpercentile 14
    • TinSn1.76 mg/kgpercentile 12

    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)
    • SodiumNa0.968 %percentile 68
    • CalciumCa2.77 %percentile 63
    • ManganeseMn903 mg/kgpercentile 56
    • TitaniumTi4,371 mg/kgpercentile 47
    • PotassiumK1.49 %percentile 45
    • MagnesiumMg0.824 %percentile 43
    • AluminiumAl5.17 %percentile 33
    • IronFe2.14 %percentile 17
    • PhosphorusP538 mg/kgpercentile 12
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • GalliumGa17.1 mg/kgpercentile 75
    • BoronB67.3 mg/kgpercentile 69
    • CeriumCe59.8 mg/kgpercentile 52
    • LithiumLi29.4 mg/kgpercentile 50
    • ZirconiumZr400 mg/kgpercentile 50
    • RubidiumRb87.1 mg/kgpercentile 46
    • BariumBa416 mg/kgpercentile 43
    • YttriumY24.7 mg/kgpercentile 33
    • StrontiumSr114 mg/kgpercentile 29
    • BerylliumBe0.772 mg/kgpercentile 17

    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

    52nGy/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.

    • Potassium (K)K1.40 %percentile 72
    • Equivalent uranium (eU)eU2.61 ppm56th percentile
    • Equivalent thorium (eTh)eTh7.38 ppm52th 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 137CsCS137688 Bq/m²percentile 7

    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

    -3nT

    range -3 to -3 nT

    Deviation of the Earth's magnetic field from its surroundings. Positive and negative anomalies reveal rocks with magnetite (basalts, basic volcanic rocks) and boundaries in the bedrock.

    Bouguer gravity anomaly

    -1mGal

    residual +25.8 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 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 –.

    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.

    • Average January temperature-3.5°C
    • Average July temperature18.5°C
    • Annual precipitation700mm

    Climatic-geographical types

    • mountain climate100%SR 33 %

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

    Susceptibility of soils to acidification

    • soils susceptible to acidification100%SR 31 %

    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

    • Mesozoic of the Bradl zone and the central Western Carpathians100%SR 10 %

    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.

    Kutacie práce na kopci Jahodník – 6 – other type of object (2.8 km from the water)Horné Orešany – časť Majdan – bývalá chemická to – SK200030FK (160 m from the water)Majdan – Horné Orešany – occasional (270 m from the water)Lošonec – permanent (960 m from the water)Smutná II. – k.ú. Smolenice – Horné Orešany – none (1.3 km from the water)Smolenická Nová Ves – permanent (1.6 km from the water)Lošonec – none (1.7 km from the water)Lošonec – cannot be estimated (1.7 km from the water)Horné Orešany – none (1.9 km from the water)Jahodník – Lošonec – none (2.8 km from the water)Dolné Orešany – none (3.0 km from the water)a1 (1.0 km from the water)a1 (5.2 km from the water)a1 (8.0 km from the water)a1 (8.3 km from the water)a1 (8.8 km from the water)Lošonec – building stone (3.2 km from the water)Lošonec – building stone (3.2 km from the water)Horné Orešany – Políčko – building stone – dolomite (830 m from the water)Smolenická Nová Ves – Jahodník – building stone – limestone (2.1 km from the water)Horné Orešany – Olšovský mlyn – building stone – limestone (2.6 km from the water)Horné Orešany – Rybárňa – building stone – limestone (2.7 km from the water)Smolenice – building stone – limestone (3.7 km from the water)Boleráz – brick raw materials (4.5 km from the water)Smolenice – building stone – limestone (4.6 km from the water)Dolina Hlboče – geomorphology (4.1 km from the water)Tmavá skala – paleontology (4.2 km from the water)Horné Orešany-Majdán – úzkoprofilový vrt s obyčajnou pitnou a ú (150 m from the water)Horné Orešany – širokoprofilový vrt (Ø vŕtania nad 600 m (220 m from the water)Horné Orešany – širokoprofilový vrt (Ø vŕtania nad 600 m (260 m from the water)Horné Orešany – úzkoprofilový vrt s obyčajnou pitnou a ú (460 m from the water)Horné Orešany – úzkoprofilový vrt s obyčajnou pitnou a ú (750 m from the water)Horné Orešany – monitoring borehole (1.3 km from the water)Horné Orešany – monitoring borehole (1.3 km from the water)Horné Orešany – monitoring borehole (1.4 km from the water)Horné Orešany – monitoring borehole (1.4 km from the water)Horné Orešany – monitoring borehole (1.4 km from the water)Horné Orešany – úzkoprofilový vrt s obyčajnou pitnou a ú (1.4 km from the water)Horné Orešany – monitoring borehole (1.4 km from the water)Smolenice-vidiek – úzkoprofilový vrt s obyčajnou pitnou a ú (1.7 km from the water)Smolenice – úzkoprofilový vrt s obyčajnou pitnou a ú (1.8 km from the water)Horné Orešany – širokoprofilový vrt (Ø vŕtania nad 600 m (1.9 km from the water)Horné Orešany – širokoprofilový vrt (Ø vŕtania nad 600 m (1.9 km from the water)Horné Orešany – širokoprofilový vrt (Ø vŕtania nad 600 m (2.0 km from the water)Horné Orešany – širokoprofilový vrt (Ø vŕtania nad 600 m (2.0 km from the water)Horné Orešany – širokoprofilový vrt (Ø vŕtania nad 600 m (2.0 km from the water)Smolenická Nová Ves – monitoring borehole (2.1 km from the water)Smolenická Nová Ves – monitoring borehole (2.1 km from the water)Horné Orešany – úzkoprofilový vrt s obyčajnou pitnou a ú (2.1 km from the water)Smolenice – úzkoprofilový vrt s obyčajnou pitnou a ú (2.7 km from the water)Horné Orešany – negative borehole (2.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (120 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (270 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (360 m from the water)prameň – Groundwater springs (430 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (620 m from the water)prameň – Groundwater springs (890 m from the water)prameň – Groundwater springs (940 m from the water)prameň – Groundwater springs (1.0 km from the water)prameň – Groundwater springs (1.2 km from the water)prameň – Groundwater springs (1.5 km from the water)prameň s monitorovaním výdatnosti – Groundwater springs (1.6 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.7 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.7 km from the water)prameň – Groundwater springs (1.7 km from the water)vodárensky využívaný a monitorovaný prameň – Groundwater springs (1.8 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.8 km from the water)prameň s monitorovaním výdatnosti – Groundwater springs (2.1 km from the water)vodárensky využívaný prameň – Groundwater springs (2.2 km from the water)prameň – Groundwater springs (2.2 km from the water)prameň – Groundwater springs (2.3 km from the water)prameň – Groundwater springs (2.4 km from the water)prameň – Groundwater springs (2.5 km from the water)prameň – Groundwater springs (2.6 km from the water)vodárensky využívaný prameň – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (2.6 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.7 km from the water)vodárensky využívaný a monitorovaný prameň – Groundwater springs (2.7 km from the water)prameň – Groundwater springs (2.7 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.8 km from the water)prameň – Groundwater springs (2.9 km from the water)prameň – Groundwater springs (2.9 km from the water)prameň – Groundwater springs (2.9 km from the water)prameň – Groundwater springs (2.9 km from the water)prameň – Groundwater springs (2.9 km from the water)prameň – Groundwater springs (2.9 km from the water)Lošonec, 1700m SSV od K409 – source (890 m from the water)Horné Orešany – Rybikarka, 1050m ZSZ od K544 – source (1.0 km from the water)Horné Orešany, č.d. 175, 2200m SV od K544 – well (1.1 km from the water)Lošonec, 2400m JV od K372 Červená – source (1.3 km from the water)Horné Orešany, 1500m VSV od K544 – well (1.5 km from the water)Horné Orešany, č.d. 264, 2400m SSV od K544 – well (1.5 km from the water)Lošonec – Olšovský mlyn, 1100m SZ od K409 – source (1.7 km from the water)Horné Orešany, 1250m Z od K409 – source (2.1 km from the water)Dolné Orešany, 800m V od K535 Bolehlav – source (2.5 km from the water)Lošonec – Jahodník, 950m VJV od K372 – source (2.6 km from the water)Lošonec, 1900m ZSZ od K409 – source (2.6 km from the water)Dolné Orešany, 1100m VJV od K535 – source (2.7 km from the water)Smolenice, 1200m VJV od K483 Driny – source (2.7 km from the water)Majdán – borehole (2.8 km from the water)Smolenice – Jahodník, 1400m VSV od K372 – source (2.9 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.

    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.

    • CopperCuhigh (top 5 %)
      highest 13.7 μg/lmedian 3.20 μg/l4 samples

      Highest value: Smutná, potok1999, 910 m from the water. Comparison: percentile 96 of all samples in Slovakia.

    • BariumBaelevated (top 10 %)
      highest 127 μg/lmedian 84.5 μg/l4 samples

      Highest value: pravostr. prítok r. Parná1999, 980 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • ArsenicAstypical value
      highest 1.00 μg/lmedian 0.500 μg/l4 samples75 % below the limit of quantification

      Highest value: Smutná, potok1999, 910 m from the water. Comparison: percentile 50 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l4 samples100 % below the limit of quantification

      Highest value: ľovostr. prítok r. Parná, 100 m nad kúpaliskom1999, 560 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l4 samples100 % below the limit of quantification

      Highest value: ľovostr. prítok r. Parná, 100 m nad kúpaliskom1999, 560 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • AntimonySbbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l4 samples100 % below the limit of quantification

      Highest value: ľovostr. prítok r. Parná, 100 m nad kúpaliskom1999, 560 m from the water. Comparison: percentile 37 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l4 samples100 % below the limit of quantification

      Highest value: ľovostr. prítok r. Parná, 100 m nad kúpaliskom1999, 560 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • ChromiumCrbelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l4 samples100 % below the limit of quantification

      Highest value: ľovostr. prítok r. Parná, 100 m nad kúpaliskom1999, 560 m from the water. Comparison: percentile 32 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l4 samples100 % below the limit of quantification

      Highest value: ľovostr. prítok r. Parná, 100 m nad kúpaliskom, 560 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 dioxideSiO2typical value
      highest 12.5 mg/lmedian 12.0 mg/l4 samples

      Highest value: pravostr. prítok r. Parná1999, 980 m from the water. Comparison: percentile 57 of all samples in Slovakia.

    Gold and ore minerals in river sediments

    Regional panning prospecting: the heavy fraction was washed out of river gravel and the mineral grains in it were counted. The map of finds is positive: a sample without gold is not listed in the atlas, so the absence of a find is not proof that there is no gold.

    • Ilmenit (FeTiO₃)10 samples, at most 1815 grains
    • Limonite (FeO(OH)·nH₂O)10 samples, at most 815 grains
    • Monazit ((Ce,La,Nd)PO₄)10 samples, at most 55 grains
    • Rutil (TiO₂)10 samples, at most 555 grains
    • Anatas (TiO₂)9 samples, at most 55 grains
    • Hematite (Fe₂O₃)9 samples, at most 4115 grains
    • Magnetite (Fe₃O₄)9 samples, at most 315 grains
    • Barite (BaSO₄)8 samples, at most 315 grains
    • Pyrite (FeS₂)8 samples, at most 5 grains
    • Arsenopyrite (FeAsS)1 sample, at most 4 grains

    Rock-forming and accessory minerals

    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))10 samples, at most 315 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)10 samples, at most 1815 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))10 samples, at most 815 grains
    • Tourmalines (complex borosilicate)10 samples, at most 315 grains
    • Zirconium (ZrSiO₄)10 samples, at most 315 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)9 samples, at most 55 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)7 samples, at most 315 grains
    • Korund (Al₂O₃)5 samples, at most 5 grains
    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)4 samples, at most 5 grains
    • Sillimanit (Al₂SiO₅)4 samples, at most 5 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))3 samples, at most 5 grains
    • Kyanit (Al₂SiO₅)2 samples, at most 5 grains

    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-HCO37×
    • CaHCO35×
    • CaMgHCO31×
    • CaSO41×
    • Ca-HCO41×

    Water quality class according to the hydrogeochemical map

    • class A6×
    • class E4×
    • class C1×
    • class G1×
    • class F1×
    • class H1×
    • class B1×

    Metals in groundwater

    • AluminiumAlextreme (top 1 %)
      highest 0.250 mg/lmedian 0.0100 mg/l17 samples12 % below the limit of quantification

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • CopperCuhigh (top 5 %)
      highest 9.20 μg/lmedian 1.00 μg/l17 samples

      Highest value: studňa1993, 1.5 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • LithiumLihigh (top 5 %)
      highest 74.0 μg/lmedian 9.00 μg/l17 samples

      Highest value: studňa1993, 1.0 km from the water. Comparison: percentile 96 of all samples in Slovakia.

    • ArsenicAshigh (top 5 %)
      highest 4.80 μg/lmedian 0.500 μg/l17 samples53 % below the limit of quantification

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • SeleniumSeelevated (top 10 %)
      highest 2.20 μg/lmedian 0.500 μg/l17 samples94 % below the limit of quantification

      Highest value: studňa1993, 1.0 km from the water. Comparison: percentile 93 of all samples in Slovakia.

    • AntimonySbelevated (top 10 %)
      highest 0.500 μg/lmedian 0.100 μg/l17 samples94 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 92 of all samples in Slovakia.

    • ZincZnelevated (top 10 %)
      highest 624 μg/lmedian 16.0 μg/l17 samples12 % below the limit of quantification

      Highest value: studňa1993, 1.0 km from the water. Comparison: percentile 91 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 1.20 μg/lmedian 0.250 μg/l17 samples82 % below the limit of quantification

      Highest value: studňa1993, 2.3 km from the water. Comparison: percentile 80 of all samples in Slovakia.

    • LeadPbslightly elevated
      highest 1.00 μg/lmedian 0.500 μg/l17 samples82 % below the limit of quantification

      Highest value: prameň1993, 2.1 km from the water. Comparison: percentile 75 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l5 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l17 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l17 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    water source for individual supply236,5 Bq/l33.2 Bq/l
    source12,08 Bq/l2.08 Bq/l
    well313,4 Bq/l5.20 Bq/l
    developed spring226,1 Bq/l17.3 Bq/l
    stream, river16,64 Bq/l6.64 Bq/l
    water source for public supply115,9 Bq/l15.9 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.

    Types of mining objects

    • other type of object1×

    Nearest old mine workings

    NameTypeMinedEndedFrom the water
    Kutacie práce na kopci Jahodníkother type of objectbarite19372.8 km

    Deposits and mining areas

    DepositMineralStatus and organisationFrom the water
    Lošonecbuilding stoneMined deposit – ALAS SLOVAKIA, s.r.o.3.2 km
    Lošonecbuilding stoneMined deposit – ALAS SLOVAKIA, 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.

    52 boreholes in the 3 km zone, of which 24 hydrogeological and 28 other; with an archive report number 38.

    Borehole depths

    • up to 10 m24×
    • 10–30 m8×
    • 30–100 m8×
    • 100–300 m4×
    • over 300 m8×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Horné Orešany-Majdánnarrow-diameter borehole with ordinary drinking and process water40.0 m44787 131Db18.pdf150 m
    Horné Orešanywide-diameter borehole5.0 m31122 131Db10.pdf220 m
    Horné Orešanywide-diameter borehole4.0 m31122 131Db11.pdf260 m
    Horné Orešanynarrow-diameter borehole with ordinary drinking and process water80.0 m77720 131Db44.pdf460 m
    Horné Orešanynarrow-diameter borehole with ordinary drinking and process water50.0 m45766 131Db19.pdf750 m
    1-256 Lošonechydrogeological14.0 m1017481.2 km
    Horné Orešanymonitoring borehole5.0 m77272 131Db43.pdf1.3 km
    IS-3engineering-geological19.0 m860461.3 km
    Horné Orešanymonitoring borehole6.0 m77272 131Db38.pdf1.3 km
    Horné Orešanymonitoring borehole6.0 m77272 131Db39.pdf1.4 km
    Horné Orešanymonitoring borehole5.5 m77272 131Db42.pdf1.4 km
    Horné Orešanymonitoring borehole5.0 m77272 131Db40.pdf1.4 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< 551.0 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.

    Environmental burdens

    SiteActivitySubstanceClassificationFrom the water
    Horné Orešany – časť Majdan – bývalá chemická továreňSK200030FK160 m

    Waste landfills

    LandfillAreaYear establishedMonitoringFrom the water
    Majdan – Horné Orešany1 500 m²1975–270 m
    Lošonec5 000 m²1980–960 m
    Smutná II. – k.ú. Smolenice – Horné Orešany50 000 m²1980monitored1.3 km
    Smolenická Nová Ves100 m²1975–1.6 km
    Lošonec100 m²1990–1.7 km
    Lošonec2 500 m²1970–1.7 km
    Horné Orešany4 000 m²1980–1.9 km
    Jahodník – Lošonec80 m²1975–2.8 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. Trnava1 fishing district · 2.0 km28VN Horné Orešany28

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