Fishing conditions score, the best window of the day and fishing districts from the best conditions Low activity · average of one fishing district 15:00–17:00 VN Tríbeč – Sekanina, window score 34. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 17:04. 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 Move the map with two fingers. In full-screen mode one finger is enough. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. For each fishing district you can see what it is made of, how well it is supported by data and where the data comes from. 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. Source: Open Topo Data (eudem25m), 4 Nov 2026. The height is approximate (error of a few metres). Loading the 3D terrain model… 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. 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 quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby 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. 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. pH 7.8modelled estimate water type Ca–Mg–HCO₃ Mineralisation 279 mg/l, soft water (8.4 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Arsenic 15.3 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 86. Interpolation of the Geochemical Atlas of river sediments. 67nGy/h dose rate percentile 95 in Slovakia Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ. 0objects within 3 km No old mine working is recorded within 3 km of the water. 0samples with gold 8 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. 0 from 8indicators in the top 5 % highest: Lithium 10.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 75 (Kompanová). 14boreholes within 3 km 136 water analyses nearby Of these, 14 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. 27°C at the wellhead 1 geothermal borehole within 10 km Warmest: Obyce – KD-1, yield 3.5 l/s, 9.9 km from the water. 8sites within 3 km 8 landfills No environmental burden is registered within 3 km; landfills are only recorded. 4records within 5 km 3 deposits, 1 ore occurrence Geofond registers, the metallogenetic map and the mineral resources map. 0areas within 3 km Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed. 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. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia The map covers 0 of 1 points on the water line. 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. pH 7.78typical 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. 8.4°dH, soft Sum of calcium and magnesium (1.50 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 279mg/l mineralisation Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds. Water type by dominant ions: Ca–Mg–HCO₃ Shares are in equivalents, the usual way of comparing the composition of waters. 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) 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. 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) 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. 67nGy/h in air Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains. 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. 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) marker on the bar: share among all sample points on streams in Slovakia 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. -13nT range -13 to -13 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. -2mGal residual +14.3 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. 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. 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. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off. 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. 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. Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 54 of all samples in Slovakia. Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 32 of all samples in Slovakia. Highest value: Kompanová, 160 m from the water. Comparison: percentile 26 of all samples in Slovakia. Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 22 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Kompanová2010, 160 m from the water. Comparison: percentile 79 of all samples in Slovakia. 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. 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. Highest value: studňa1992, 1.9 km from the water. Comparison: percentile 100 of all samples in Slovakia. Highest value: studňa1992, 810 m from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: prameň1992, 1.2 km from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: studňa1992, 1.5 km from the water. Comparison: percentile 83 of all samples in Slovakia. Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 80 of all samples in Slovakia. Highest value: studňa1992, 2.2 km from the water. Comparison: percentile 76 of all samples in Slovakia. Highest value: prameň1992, 2.1 km from the water. Comparison: percentile 69 of all samples in Slovakia. Highest value: studňa1992, 810 m from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 39 of all samples in Slovakia. Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 30 of all samples in Slovakia. 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. 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. 14 boreholes in the 3 km zone, of which 11 hydrogeological and 3 other; with an archive report number 14. 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. 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. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. Who manages the fishing districts and where they are Hron basin
By the water now
Today on the VN Tríbeč – Sekanina watercourse
Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the watercourse
Elevation profile: reservoir
Terrain in 3D
Historical images



Water pollution on the VN Tríbeč – Sekanina watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VN Tríbeč – Sekanina stream
Water according to the atlas
Elements in river sediment
Natural gamma radiation
Old mine workings
Gold in river sediment
Trace elements in the stream water
Boreholes and groundwater analyses
Geothermal energy
Environmental burdens and landfills
Deposits and ore occurrences
Landslides and slope deformations
Geological structure beneath the water
Quaternary cover
Neotectonic units
Direction of neotectonic movements
Regional geological division
Regional geological division (subunits)
Susceptibility of the area to slope deformations
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
3.19 mg/lpercentile 539.68 mg/lpercentile 539.48 mg/lpercentile 5133.4 mg/lpercentile 4011.2 mg/lpercentile 36141 mg/lpercentile 3041.7 mg/lpercentile 290.0506 mg/lpercentile 5Nutrients and organic pollution
7.26 mg/lpercentile 938.55 mg/lpercentile 660.0914 mg/lpercentile 430.0494 mg/lpercentile 27Metals
0.528 mg/lpercentile 93244 μg/lpercentile 8466.8 μg/lpercentile 7010.5 μg/lpercentile 67Elements in river sediments
Potentially toxic and trace elements
15.3 mg/kgpercentile 8611.7 mg/kgpercentile 850.255 mg/kgpercentile 630.796 mg/kgpercentile 620.423 mg/kgpercentile 58101 mg/kgpercentile 5569.7 mg/kgpercentile 5324.3 mg/kgpercentile 532.64 mg/kgpercentile 4922.8 mg/kgpercentile 410.196 mg/kgpercentile 3713.5 mg/kgpercentile 3755.3 mg/kgpercentile 230.0553 mg/kgpercentile 170.0590 mg/kgpercentile 8Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
3,240 mg/kgpercentile 951.92 %percentile 916,214 mg/kgpercentile 886.77 %percentile 821,073 mg/kgpercentile 740.990 %percentile 713.13 %percentile 700.736 %percentile 311.05 %percentile 15Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
22.9 mg/kgpercentile 95842 mg/kgpercentile 9586.1 mg/kgpercentile 94556 mg/kgpercentile 89196 mg/kgpercentile 86104 mg/kgpercentile 8134.7 mg/kgpercentile 741.62 mg/kgpercentile 6329.6 mg/kgpercentile 6155.0 mg/kgpercentile 34Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.98 %percentile 953.36 ppm93th percentile8.47 ppm77th percentile2,654 Bq/m²percentile 83Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Relief, climate and soils
Climatic-geographical types
Soil contamination (map 1:500,000)
Map of the corridor
Trace elements in surface waters
Major ions, mineralisation and pH
Gold and ore minerals in river sediments
Rock-forming and accessory minerals
Groundwater: chemistry, water types and radioactivity
Chemical water types nearby
Water quality class according to the hydrogeochemical map
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median well 1 4,59 Bq/l 4.59 Bq/l Mine workings, deposits and ore occurrences
Deposits and mining areas
Deposit Mineral Status and organisation From the water Zlatno quartzite Deposit with expected use of reserves – ŠGÚDŠ Bratislava 2.4 km Ladice ceramic clays Deposit with expected use of reserves – ŠGÚDŠ Bratislava 3.3 km Ladice ceramic clays Deposit with expected use of reserves – ŠGÚDŠ Bratislava 3.3 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Velčice narrow-diameter borehole with ordinary drinking and process water 62.0 m 68885 121Da13.pdf1.2 km Mankovce narrow-diameter borehole with ordinary drinking and process water 47.3 m 20579 121Da6.pdf1.5 km Mankovce wide-diameter borehole 45.0 m 55106 121Da9.pdf1.9 km Velčice narrow-diameter borehole with ordinary drinking and process water 45.0 m 43716 121Dc17.pdf2.0 km Mankovce narrow-diameter borehole with ordinary drinking and process water 45.0 m 55106 121Da10.pdf2.0 km VM-4 deposit 20.0 m 829222.1 km Velčice narrow-diameter borehole with ordinary drinking and process water 26.2 m 5781 121Dc4.pdf2.1 km Mankovce narrow-diameter borehole with ordinary drinking and process water 200.0 m 87982 121Da17.pdf2.2 km Velčice narrow-diameter borehole with ordinary drinking and process water 46.6 m 5781 121Dc5.pdf2.5 km Slažany structural borehole with ordinary water 170.0 m 77716 121Dc30.pdf2.7 km VZL-10-91 deposit 25.0 m 793302.7 km Velčice narrow-diameter borehole with ordinary drinking and process water 86.0 m 78708 121Dc31.pdf2.8 km Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Obyce – KD-1 27 °C 3.5 l/s 464.3 m Ca-Mg-SO4-HCO3 unused 9.9 km Sources of geothermal and mineral waters
Source Type Water temperature (°C) Yield (l/s) Count Nearest from water KD-1 geothermal water 22 – 38 < 5 1 8.4 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Velčice 6 000 m² 1975 – 460 m Velčice 150 m² 1970 – 1.0 km Velčice 1 000 m² 1970 – 1.4 km Velčice 240 m² 1978 – 2.0 km Velčice 250 m² 1980 – 2.0 km Mankovce – Zlatno 5 000 m² 1960 – 2.1 km Mankovce – Hušťavky – Mankovce 2 000 m² 1960 monitored 2.1 km Velčice 15 000 m² 1970 – 2.4 km How to read these data
Organizations and location
Organizations on the watercoursewho manages the fishing districts and what the conditions are there today
More watercourses nearby
25from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
LithiumLislightly elevated
highest 10.0 μg/lmedian 10.0 μg/l1 sample
ArsenicAsslightly elevated
highest 2.00 μg/lmedian 2.00 μg/l1 sample
BariumBatypical value
highest 44.0 μg/lmedian 44.0 μg/l1 sample
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l1 sample100 % below the limit of quantification
ChromiumCrbelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.150 μg/lmedian 0.150 μg/l1 sample100 % below the limit of quantification
CopperCubelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification
Silicon dioxideSiO2slightly elevated
highest 22.1 mg/lmedian 22.1 mg/l1 sample
LeadPbextreme (top 1 %)
highest 270 μg/lmedian 0.500 μg/l11 samples73 % below the limit of quantification
ZincZnelevated (top 10 %)
highest 771 μg/lmedian 10.0 μg/l11 samples9 % below the limit of quantification
ArsenicAselevated (top 10 %)
highest 2.90 μg/lmedian 1.60 μg/l11 samples27 % below the limit of quantification
AntimonySbslightly elevated
highest 0.200 μg/lmedian 0.100 μg/l11 samples82 % below the limit of quantification
CopperCuslightly elevated
highest 2.50 μg/lmedian 0.500 μg/l11 samples
LithiumLislightly elevated
highest 17.0 μg/lmedian 5.00 μg/l11 samples9 % below the limit of quantification
ChromiumCrtypical value
highest 0.600 μg/lmedian 0.250 μg/l11 samples91 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l6 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l11 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l11 samples100 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l11 samples100 % below the limit of quantification
AluminiumAlbelow half of Slovakia
highest 0.00500 mg/lmedian 0.00500 mg/l11 samples100 % below the limit of quantification





