Watercourse

VN Zákruty

fishing district
1
fishing district length
0.6km
region
Banská Bystrica Region
Aerial image of watercourse VN Zákruty 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 Zákruty watercourse

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

Average of the watercourse's fishing districts

Low activity · average of one fishing district

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

Best window today

15:00–17:00

VN Zákruty, window score 19.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 06:04.

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
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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.

    2522542562582602620.0 km0.2 km0.4 km0.6 km
    Terrain elevation profile (Reservoir): from 260 to 254 m a.s.l. over 0.6 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    254 m a.s.l.
    Lowest point of the profile
    254 m a.s.l.
    Highest point of the profile
    260 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 2018 to 2024: 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 Zákruty from 2018
    2018imaged 9 Aug 2018
    Aerial image of watercourse VN Zákruty from 2021
    2021imaged 5 Sep 2021
    Aerial image of watercourse VN Zákruty from 2024
    2024imaged 19 Oct 2024

    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 Zákruty 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

    • VN ZákrutyVN Zákruty · standard not met in 1 of 4 years1 indicator

    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.

    • harmful substances above the standard at at least one station (metals, pesticides, PFAS, solvents)1

    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 Zákruty 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 (1 km of line in total): stream samples within 1 km, boreholes, mine workings and burdens within 3 km, ore occurrences within 5 km, geothermal sources within 10 km.

    510

    Water according to the atlas

    pH 7.8modelled estimate

    water type Ca–Mg–HCO₃–SO₄

    Mineralisation 276 mg/l, moderately hard water (8.8 °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: Cobalt 12.2 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 87. Interpolation of the Geochemical Atlas of river sediments.

    1 km2 km55 °C95 °C

    Heat underfoot

    55°C at 1,000 m depth

    heat flow 95 mW/m²

    At a depth of 2,000 m about 95 °C (increase of 40 °C per kilometre). Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    65nGy/h dose rate

    percentile 94 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

    1sample with gold

    6 ore minerals in the sediment

    Up to 5 grains in one sample (630 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.

    Trace elements in the stream water

    2 from 10indicators in the top 5 %

    highest: Arsenic 7.50 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 95 (600m SZ od K295 Dolná Trnávka).

    Boreholes and groundwater analyses

    103boreholes within 3 km

    105 water analyses nearby

    Of these, 103 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    0 °C120

    Geothermal energy

    54°C at the wellhead

    14 geothermal boreholes within 10 km

    Warmest: Sklené Teplice – ST-4, yield 13.3 l/s, 5.2 km from the water.

    Environmental burdens and landfills

    5sites within 3 km

    5 landfills

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

    Deposits and ore occurrences

    9records within 5 km

    6 deposits, 3 ore occurrences

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

    Landslides and slope deformations

    43areas within 3 km

    4 active

    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.

    Tectonic division

    • NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

    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)

    • inner basins100%SR 4.5 %

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

    Engineering-geological districts

    • region of mountain-stream deposits100%SR 21 %

    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 0 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.

    Genetic type of groundwater

    • carbonate-silicate mineralization100%SR 2.1 %

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

    Chemical type of groundwater

    • Ca-(Mg)-HCO3 typ100%SR 0.0 %

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

    Groundwater quality class

    • E100%SR 6.5 %

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

    Geothermal groundwater bodies

    • Žiar Basin100%SR 6.4 %

    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 7.82typical 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

    8.8°dH, moderately hard

    Sum of calcium and magnesium (1.57 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    276mg/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

    • FluoridesF0.202 mg/lpercentile 80
    • PotassiumK5.36 mg/lpercentile 76
    • ChloridesCl13.4 mg/lpercentile 60
    • SulphatesSO445.8 mg/lpercentile 57
    • SodiumNa9.38 mg/lpercentile 51
    • MagnesiumMg12.8 mg/lpercentile 41
    • CalciumCa41.8 mg/lpercentile 29
    • BicarbonatesHCO3115 mg/lpercentile 22

    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

    • NitratesNO331.1 mg/lpercentile 95
    • PhosphatesPO40.688 mg/lpercentile 88
    • Chemical oxygen demandChSK4.46 mg/lpercentile 74
    • AmmoniumNH40.0435 mg/lpercentile 22

    Metals

    • AluminiumAl522 μg/lpercentile 95
    • ZincZn27.6 μg/lpercentile 92
    • ManganeseMn135 μg/lpercentile 85
    • IronFe0.0809 mg/lpercentile 40

    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

    • CobaltCo12.2 mg/kgpercentile 87
    • ArsenicAs13.0 mg/kgpercentile 83
    • VanadiumV88.4 mg/kgpercentile 81
    • AntimonySb1.59 mg/kgpercentile 80
    • LeadPb18.2 mg/kgpercentile 63
    • SeleniumSe0.288 mg/kgpercentile 60
    • ZincZn99.0 mg/kgpercentile 53
    • MolybdenumMo0.393 mg/kgpercentile 53
    • MercuryHg0.0953 mg/kgpercentile 46
    • CopperCu21.6 mg/kgpercentile 40
    • TinSn2.39 mg/kgpercentile 39
    • CadmiumCd0.136 mg/kgpercentile 37
    • BismuthBi0.178 mg/kgpercentile 33
    • ChromiumCr59.1 mg/kgpercentile 29
    • NickelNi18.1 mg/kgpercentile 22

    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)
    • ManganeseMn1,784 mg/kgpercentile 93
    • TitaniumTi5,838 mg/kgpercentile 84
    • PhosphorusP1,183 mg/kgpercentile 82
    • AluminiumAl6.30 %percentile 70
    • IronFe3.13 %percentile 70
    • PotassiumK1.63 %percentile 69
    • SodiumNa0.835 %percentile 43
    • MagnesiumMg0.596 %percentile 13
    • CalciumCa0.754 %percentile 6
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • YttriumY37.5 mg/kgpercentile 90
    • RubidiumRb104 mg/kgpercentile 82
    • ZirconiumZr507 mg/kgpercentile 81
    • LithiumLi36.4 mg/kgpercentile 80
    • CeriumCe69.6 mg/kgpercentile 79
    • BerylliumBe1.80 mg/kgpercentile 73
    • BariumBa510 mg/kgpercentile 72
    • GalliumGa14.4 mg/kgpercentile 54
    • BoronB55.8 mg/kgpercentile 36
    • StrontiumSr109 mg/kgpercentile 23

    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

    65nGy/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

    low

    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)eU3.91 ppm95th percentile
    • Equivalent thorium (eTh)eTh9.44 ppm90th percentile
    • Potassium (K)K1.44 %percentile 78

    dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile)

    • Areal activity of 137CsCS1371,224 Bq/m²percentile 33

    Radon risk by isopleths

    • low100%SR 36 %

    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

    -21nT

    range -21 to -21 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

    -41mGal

    residual −19.1 mGal

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

    Geothermal potential

    The Atlas of Geothermal Energy of Slovakia records rock temperature and heat flow from the Earth's interior. It is the potential of the area, not the actual warmth of the water in the stream. Specific geothermal boreholes and springs near this water are in the geothermal energy section below.

    1 km2 km55 °C95 °C

    Rock temperature with depth

    55 / 95 °Cat depths of 1,000 and 2,000 m

    increase of 40 °C per km

    The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 95 mW/m².

    Geothermal groundwater bodies beneath the water line

    • Žiar Basin100%SR 6.4 %

    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)220–509m a.s.l.
    • Average elevation of the units313m a.s.l.
    • Average slope4.3°
    • Average January temperature-3.0°C
    • Average July temperature19.3°C
    • Annual precipitation650mm

    Geomorphological units

    • Žiar Basin100%SR 0.0 %

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

    Geomorphological regions

    • Slovak Central Mountains100%SR 9.1 %

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

    Climatic-geographical types

    • basin climate100%SR 29 %

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

    Susceptibility of soils to acidification

    • soils moderately susceptible to acidification100%SR 25 %

    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.

    Lovča – none (960 m from the water)Dolná Trnávka – none (1.6 km from the water)Dolná Ždaňa – none (2.2 km from the water)Horná Trnávka – none (2.7 km from the water)Lovča – cannot be estimated (2.8 km from the water)Žiar nad Hronom – RGŽ-2 – non-spa (5.1 km from the water)Sklené Teplice – ST-4 – non-spa (5.2 km from the water)Sklené Teplice – STH-2 – non-spa (7.4 km from the water)Sklené Teplice – spa (7.6 km from the water)Sklené Teplice – spa (7.7 km from the water)Sklené Teplice – ST-2 – spa (7.7 km from the water)Sklené Teplice – spa (7.7 km from the water)Sklené Teplice – spa (7.7 km from the water)Sklené Teplice – ST-1 – spa (7.7 km from the water)Sklené Teplice – spa (7.8 km from the water)Sklené Teplice – spa (7.8 km from the water)Vyhne – H-2 – non-spa (7.9 km from the water)Vyhne – H-1 – non-spa (8.0 km from the water)Sklené Teplice – ST-5 – non-spa (8.7 km from the water)a1 (2.9 km from the water)b1 (5.0 km from the water)a1 (5.6 km from the water)a1 (6.2 km from the water)d1 (6.4 km from the water)a1 (6.9 km from the water)a1 (7.6 km from the water)d1 (7.8 km from the water)c1 (7.8 km from the water)a1 (8.3 km from the water)d1 (8.6 km from the water)c1 (8.7 km from the water)c1 (9.5 km from the water)c2 (9.6 km from the water)d1 (9.9 km from the water)Sklené Teplice (7.6 km from the water)Lehôtka pod Brehmi – perlite (4.1 km from the water)Hliník nad Hronom – building stone (4.9 km from the water)Lehôtka pod Brehmi – perlite (4.1 km from the water)Lehôtka pod Brehmi – Bralo – perlite (4.4 km from the water)Hliník nad Hronom – building stone (5.0 km from the water)Lehôtka pod Brehmi – perlite (4.1 km from the water)Štrkopiesky v koryte Hrona, úsek 139,158 – 149,0 – gravelly sands (2.5 km from the water)Hliník nad Hronom – drahé a ozdobné kamene – jasper; chalcedony (4.8 km from the water)Prestavlky Za Dúbravou – building stone – andesite (4.9 km from the water)Hliník nad Hronom, Szabóova skala – volcanic rocks (4.5 km from the water)Hliník nad Hronom, Panská hora – volcanic rocks (4.9 km from the water)DOLNA TRNAVKA – Landslides (170 m from the water)DOLNA TRNAVKA – Landslides (190 m from the water)LOVCA – Landslides (300 m from the water)– Landslides (450 m from the water)DOLNA TRNAVKA – Landslides (480 m from the water)TRUBIN – Landslides (700 m from the water)– Landslides (800 m from the water)DOLNA TRNAVKA – Landslides (840 m from the water)HORNA TRNAVKA – Landslides (1.0 km from the water)– Landslides (1.1 km from the water)– Landslides (1.2 km from the water)– Landslides (1.2 km from the water)DOLNA TRNAVKA – Landslides (1.3 km from the water)TRUBIN – Landslides (1.4 km from the water)TRUBIN – Landslides (1.4 km from the water)KUPCA – Landslides (1.4 km from the water)– Landslides (1.4 km from the water)HORNA TRNAVKA – Landslides (1.5 km from the water)DOLNA TRNAVKA – Landslides (1.6 km from the water)KUPCA – Landslides (1.7 km from the water)HORNA ZDANA – Landslides (1.8 km from the water)– Landslides (1.9 km from the water)– Landslides (1.9 km from the water)KUPCA – Landslides (2.0 km from the water)DOLNA TRNAVKA – Landslides (2.0 km from the water)– Landslides (2.1 km from the water)– Landslides (2.3 km from the water)DOLNA TRNAVKA – Landslides (2.3 km from the water)KUPCA – Landslides (2.4 km from the water)LOVCA – Landslides (2.4 km from the water)KUPCA – Landslides (2.5 km from the water)– Landslides (2.5 km from the water)ZIAR NAD HRONOM – Landslides (2.5 km from the water)TRUBIN – Landslides (2.6 km from the water)LOVCA – Landslides (2.6 km from the water)– Landslides (2.6 km from the water)LOVCA – Landslides (2.7 km from the water)KUPCA – Landslides (2.8 km from the water)LOVCA – Landslides (2.8 km from the water)TRUBIN – Landslides (2.8 km from the water)ZIAR NAD HRONOM – Landslides (2.9 km from the water)PRESTAVLKY – Landslides (2.9 km from the water)– Landslides (2.9 km from the water)Lovča – širokoprofilový vrt (Ø vŕtania nad 600 m (1.6 km from the water)Dolná Trnávka – SHMÚ observation borehole (1.9 km from the water)Lovča – širokoprofilový vrt (Ø vŕtania nad 600 m (2.0 km from the water)Horná Trnávka – širokoprofilový vrt (Ø vŕtania nad 600 m (2.2 km from the water)Horná Trnávka – širokoprofilový vrt (Ø vŕtania nad 600 m (2.2 km from the water)prameň – Groundwater springs (600 m from the water)prameň – Groundwater springs (670 m from the water)pramenná línia – Groundwater springs (880 m from the water)prameň – Groundwater springs (890 m from the water)vodárensky využívaný vrt – Hydrogeological boreholes (980 m from the water)prameň s monitorovaním výdatnosti – Groundwater springs (1.2 km from the water)vodárensky využívaný vrt – Hydrogeological boreholes (1.4 km from the water)prameň – Groundwater springs (1.6 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (1.6 km from the water)pramenná línia – Groundwater springs (1.9 km from the water)vodárensky využívaný vrt – Hydrogeological boreholes (1.9 km from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (1.9 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.0 km from the water)prameň – Groundwater springs (2.1 km from the water)prameň – Groundwater springs (2.1 km from the water)pramenná línia – Groundwater springs (2.2 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.2 km from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (2.2 km from the water)pramenná línia – Groundwater springs (2.3 km from the water)prameň – Groundwater springs (2.3 km from the water)prameň – Groundwater springs (2.6 km from the water)pramenná línia – Groundwater springs (2.6 km from the water)prameň – Groundwater springs (2.8 km from the water)pramenná línia – Groundwater springs (2.8 km from the water)pramenná línia – Groundwater springs (2.9 km from the water)monitorovanie hladiny podzemných vôd vo vrte – Hydrogeological boreholes (2.9 km from the water)prameň – Groundwater springs (2.9 km from the water)pramenná línia – Groundwater springs (3.0 km from the water)Dolná Trnávka – source (1.2 km from the water)Dolná Trnávka, č.d. 79, 650m JZ od K268 – well (1.4 km from the water)Lovča, č.d. 180, 1800m VSV od K268 – well (2.0 km from the water)Dolná Trnávka – source (2.1 km from the water)Horná Trnávka, Kopaniská, 650m SV od K353 – well (2.2 km from the water)Lovča, č.d. 152, 1900m SZ od K241 – well (2.3 km from the water)Dolná Žďaňa – source (2.6 km from the water)Prestavlky, č.d. 205, 1200m V od K429 – well (2.6 km from the water)Lutila – Kupča, prameň potoka, 800m JV od K382 – source (2.6 km from the water)Horná Trnávka, č.d. 7, 800 m SSZ od K353 – well (2.8 km from the water)zlato 5 ks – gold (630 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.

    • ArsenicAshigh (top 5 %)
      highest 7.50 μg/lmedian 4.60 μg/l3 samples

      Highest value: 600m SZ od K295 Dolná Trnávka1993, 980 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 0.800 μg/lmedian 0.600 μg/l3 samples

      Highest value: SV od obce Trnávka, 900 m from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 21.0 μg/lmedian 5.00 μg/l3 samples67 % below the limit of quantification

      Highest value: 600m SZ od K295 Dolná Trnávka1993, 980 m from the water. Comparison: percentile 85 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 2.90 μg/lmedian 2.00 μg/l3 samples

      Highest value: SV od obce Trnávka1993, 900 m from the water. Comparison: percentile 79 of all samples in Slovakia.

    • ChromiumCrtypical value
      highest 1.40 μg/lmedian 1.10 μg/l3 samples33 % below the limit of quantification

      Highest value: SV od obce Trnávka1993, 900 m from the water. Comparison: percentile 68 of all samples in Slovakia.

    • StrontiumSrtypical value
      highest 240 μg/lmedian 190 μg/l3 samples

      Highest value: 600m SZ od K295 Dolná Trnávka1993, 980 m from the water. Comparison: percentile 62 of all samples in Slovakia.

    • BariumBatypical value
      highest 50.0 μg/lmedian 40.0 μg/l3 samples

      Highest value: SV od obce Trnávka1993, 900 m from the water. Comparison: percentile 60 of all samples in Slovakia.

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

      Highest value: SV od obce Trnávka1993, 900 m from the water. Comparison: percentile 46 of all samples in Slovakia.

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

      Highest value: SV od obce Trnávka1993, 900 m from the water. Comparison: percentile 43 of all samples in Slovakia.

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

      Highest value: SV od obce Trnávka1993, 900 m from the water. Comparison: percentile 37 of all samples in Slovakia.

    Major ions, mineralisation and pH

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

    • Silicon dioxideSiO2slightly elevated
      highest 27.8 mg/lmedian 20.2 mg/l3 samples

      Highest value: 600m SZ od K295 Dolná Trnávka1993, 980 m from the water. Comparison: percentile 86 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.

    • Pyrite (FeS₂)7 samples, at most 55 grains
    • Antimonite (Sb₂S₃)1 sample, at most 1 grains
    • Chalcopyrite (CuFeS₂)1 sample, at most 1 grains
    • Cinabarit (HgS)1 sample, at most 1 grains
    • Gold (Au)1 sample, at most 5 grains
    • Hematite (Fe₂O₃)1 sample, at most 5 grains

    Nearest samples with gold

    SampleGold in sampleFrom the water
    108/G5 grains630 m

    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-HCO35×
    • Ca-HCO32×
    • Ca-Cl-HCO31×
    • Ca-Mg-SO4-HCO31×
    • Ca-SO41×

    Water quality class according to the hydrogeochemical map

    • class E3×
    • class G2×
    • class B2×
    • class A1×
    • class F1×
    • class H1×

    Metals in groundwater

    • ArsenicAshigh (top 5 %)
      highest 8.40 μg/lmedian 1.70 μg/l7 samples14 % below the limit of quantification

      Highest value: studňa1991, 2.6 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • CadmiumCdhigh (top 5 %)
      highest 1.00 μg/lmedian 0.250 μg/l7 samples86 % below the limit of quantification

      Highest value: studňa1991, 2.8 km from the water. Comparison: percentile 97 of all samples in Slovakia.

    • AntimonySbelevated (top 10 %)
      highest 0.500 μg/lmedian 0.100 μg/l7 samples86 % below the limit of quantification

      Highest value: studňa1991, 2.6 km from the water. Comparison: percentile 92 of all samples in Slovakia.

    • ZincZnelevated (top 10 %)
      highest 487 μg/lmedian 140 μg/l7 samples

      Highest value: studňa1991, 2.8 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • LeadPbelevated (top 10 %)
      highest 2.00 μg/lmedian 1.00 μg/l7 samples43 % below the limit of quantification

      Highest value: prameň1991, 2.5 km from the water. Comparison: percentile 90 of all samples in Slovakia.

    • LithiumLislightly elevated
      highest 31.0 μg/lmedian 13.0 μg/l7 samples

      Highest value: studňa1991, 2.3 km from the water. Comparison: percentile 88 of all samples in Slovakia.

    • SeleniumSeslightly elevated
      highest 1.10 μg/lmedian 0.500 μg/l7 samples86 % below the limit of quantification

      Highest value: studňa1991, 1.4 km from the water. Comparison: percentile 84 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 2.90 μg/lmedian 0.700 μg/l7 samples

      Highest value: studňa1991, 2.3 km from the water. Comparison: percentile 83 of all samples in Slovakia.

    • AluminiumAlslightly elevated
      highest 0.0200 mg/lmedian 0.0100 mg/l7 samples43 % below the limit of quantification

      Highest value: studňa1991, 2.2 km from the water. Comparison: percentile 80 of all samples in Slovakia.

    • ChromiumCrtypical value
      highest 0.500 μg/lmedian 0.250 μg/l7 samples86 % below the limit of quantification

      Highest value: studňa1991, 2.2 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: studňa1991, 2.3 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l7 samples100 % below the limit of quantification

      Highest value: studňa1991, 1.4 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    stream, river10,640 Bq/l0.640 Bq/l
    well17,13 Bq/l7.13 Bq/l
    source356,6 Bq/l12.5 Bq/l
    developed spring112,2 Bq/l12.2 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
    Lehôtka pod BrehmiperliteMined deposit – LBK PERLIT, s.r.o.4.1 km
    Lehôtka pod BrehmiperliteMined deposit – LBK PERLIT, s.r.o.4.1 km
    Lehôtka pod BrehmiperliteMined deposit – LBK PERLIT, s.r.o.4.1 km
    Lehôtka pod Brehmi – BraloperliteDeposit with expected use of reserves – ŠGÚDŠ Bratislava4.4 km
    Hliník nad Hronbuilding stoneMined deposit – LEVITRADE,s.r.o.4.9 km
    Hliník nad Hronbuilding stoneMined deposit – LEVITRADE,s.r.o.5.0 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.

    103 boreholes in the 3 km zone, of which 5 hydrogeological and 98 other; with an archive report number 103.

    Borehole depths

    • up to 10 m74×
    • 10–30 m19×
    • 30–100 m2×
    • 100–300 m0×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    Lovčawide-diameter borehole12.5 m18976 122Bc35.pdf1.6 km
    Dolná TrnávkaSHMÚ observation borehole10.3 m12878 122Bc20.pdf1.9 km
    Lovčawide-diameter borehole45.0 m42946 122Bc48.pdf2.0 km
    J-111engineering-geological8.0 m589292.0 km
    JV-21engineering-geological6.0 m857772.1 km
    J-110engineering-geological8.0 m589292.1 km
    JV-12engineering-geological7.0 m857772.1 km
    JV-22engineering-geological6.0 m857772.2 km
    Horná Trnávkawide-diameter borehole25.0 m10393 122Bc7.pdf2.2 km
    Horná Trnávkawide-diameter borehole40.5 m32736 122Bc41.pdf2.2 km
    JV-23engineering-geological7.0 m857772.4 km
    ZV-276engineering-geological1.0 m126082.4 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.

    BoreholeTemperatureYieldDepthChemical water typeUseFrom the water
    Žiar nad Hronom – RGŽ-2––2500 m–unused5.1 km
    Sklené Teplice – ST-454 °C13.3 l/s1820 mCa-SO4-HCO3in use5.2 km
    Sklené Teplice – STH-245 °C3.0 l/s81 mCa-SO4-HCO3in use without data reporting7.4 km
    Sklené Teplice46 °C4.5 l/s29.7 mCa-SO4unused7.6 km
    Sklené Teplice43 °C0.0 l/s–Ca-SO4unused7.7 km
    Sklené Teplice – ST-251 °C4.5 l/s107 mCa-SO4in use7.7 km
    Sklené Teplice48 °C0.2 l/s–Ca-SO4unused7.7 km
    Sklené Teplice49 °C0.1 l/s2.5 mCa-SO4unused7.7 km
    Sklené Teplice – ST-152 °C22.3 l/s69.7 mCa-SO4in use7.7 km
    Sklené Teplice39 °C0.4 l/s–Ca-SO4in use7.8 km

    Sources of geothermal and mineral waters

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 562.9 km
    category b1mineral water15-22< 515.0 km
    category d1mineral water39-55< 546.4 km
    category Sklené Teplicethermal baths––17.6 km
    category c1mineral water23-38< 537.8 km
    category c2mineral water23-385-1519.6 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
    Lovča50 m²1985–960 m
    Dolná Trnávka–1972–1.6 km
    Dolná Ždaňa600 m²1960–2.2 km
    Horná Trnávka–1990–2.7 km
    Lovča30 m²1970–2.8 km

    Landslides and slope deformations

    Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel.

    Types of deformations

    • Landslides43×

    Degree of activity

    • Stabilizovaný21×
    • Potenciálny18×
    • Aktívny4×

    Current state

    • Processed only in the scope of registration on a scale of 1:25,00028×
    • SD taken from archival materials, ktorá bola konfrontova2×

    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. Žiar nad Hronom1 fishing district · 0.6 km14VN Zákruty14

    More watercourses nearby

    Hron basin