Fishing conditions score, the best window of the day and fishing districts from the best conditions Low activity · average of one fishing district 06:00–08:00 VN Tajch (Podbrezová), window score 16. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 17:40. 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), 9 Nov 2026. The height is approximate (error of a few metres). Loading the 3D terrain model… 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. 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 1 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 8.1modelled estimate water type Ca–Mg–HCO₃–SO₄ Mineralisation 276 mg/l, moderately hard water (10.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 7 from 15elements in the top 10 % highest: Cadmium 3.05 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 95. Interpolation of the Geochemical Atlas of river sediments. 25°C at 1,000 m depth Atlas of Geothermal Energy of Slovakia. 59nGy/h dose rate percentile 84 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 13 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 10indicators in the top 5 % highest: Barium 90.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 88 (Horná Lehota, 1700m SZ od K702). 48boreholes within 3 km 121 water analyses nearby Of these, 48 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 1 geothermal and mineral water spring within 10 km. 6sites within 3 km 6 landfills No environmental burden is registered within 3 km; landfills are only recorded. 18records within 5 km 1 deposit, 17 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 9areas 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 The map covers 0 of 1 points on the water line. 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. 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 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 8.15typical 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. 10.0°dH, moderately hard Sum of calcium and magnesium (1.79 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 276mg/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–SO₄ 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. 59nGy/h in air Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains. 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) 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. -48nT range -48 to -48 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. -41mGal residual −5.9 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 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: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 88 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 83 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 82 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K702, 100 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 60 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 48 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 34 of all samples in Slovakia. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 32 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Horná Lehota, 1700m SZ od K7021993, 100 m from the water. Comparison: percentile 11 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: studňa1991, 2.7 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1991, 1.3 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1991, 2.2 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1991, 2.2 km from the water. Comparison: percentile 77 of all samples in Slovakia. Highest value: prameň1991, 2.3 km from the water. Comparison: percentile 56 of all samples in Slovakia. Highest value: prameň1991, 240 m from the water. Comparison: percentile 52 of all samples in Slovakia. Highest value: prameň1991, 240 m from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1991, 1.3 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: prameň1991, 1.3 km from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: prameň1991, 1.3 km from the water. Comparison: percentile 30 of all samples in Slovakia. Highest value: prameň1991, 1.3 km from the water. Comparison: percentile 30 of all samples in Slovakia. Highest value: prameň1991, 1.3 km from the water. Comparison: percentile 29 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. 48 boreholes in the 3 km zone, of which 7 hydrogeological and 41 other; with an archive report number 48. 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. Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel. 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 Tajch (Podbrezová) 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 Tajch (Podbrezová) watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VN Tajch (Podbrezová) stream
Water according to the atlas
Elements in river sediment
Heat underfoot
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
Regional geological division
Regional geological division (subunits)
Engineering-geological districts
Engineering-geological formations
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Aquifer rocks (hydrogeological map 1:200,000)
Aquifer type
Main hydrogeological region
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
5.19 mg/lpercentile 7512.2 mg/lpercentile 6250.2 mg/lpercentile 6114.6 mg/lpercentile 487.14 mg/lpercentile 4547.6 mg/lpercentile 330.0812 mg/lpercentile 30138 mg/lpercentile 29Nutrients and organic pollution
3.54 mg/lpercentile 580.139 mg/lpercentile 580.0578 mg/lpercentile 310.683 mg/lpercentile 1Metals
15.0 μg/lpercentile 7924.2 μg/lpercentile 4441.6 μg/lpercentile 380.0103 mg/lpercentile 2Elements in river sediments
Potentially toxic and trace elements
3.05 mg/kgpercentile 95396 mg/kgpercentile 959.65 mg/kgpercentile 9523.2 mg/kgpercentile 9535.8 mg/kgpercentile 950.801 mg/kgpercentile 9536.3 mg/kgpercentile 9148.3 mg/kgpercentile 880.440 mg/kgpercentile 820.217 mg/kgpercentile 760.516 mg/kgpercentile 7178.8 mg/kgpercentile 719.46 mg/kgpercentile 6524.8 mg/kgpercentile 5157.2 mg/kgpercentile 26Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1,558 mg/kgpercentile 941.96 %percentile 921.37 %percentile 773.30 %percentile 766.41 %percentile 744,710 mg/kgpercentile 592.19 %percentile 53819 mg/kgpercentile 470.822 %percentile 40Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
126 mg/kgpercentile 9546.4 mg/kgpercentile 95851 mg/kgpercentile 9585.2 mg/kgpercentile 9137.1 mg/kgpercentile 892.04 mg/kgpercentile 8469.2 mg/kgpercentile 78154 mg/kgpercentile 6515.1 mg/kgpercentile 60384 mg/kgpercentile 43Natural radioactivity and radon
Gamma radiation dose rate
3.70 ppm95th percentile1.38 %percentile 697.93 ppm67th percentile1,128 Bq/m²percentile 26Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Relief, climate and soils
Geomorphological units
Geomorphological regions
Climatic-geographical types
Lithogeochemical types
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
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median source 5 39,3 Bq/l 10.8 Bq/l water source for individual supply 1 56,2 Bq/l 56.2 Bq/l Mine workings, deposits and ore occurrences
Deposits and mining areas
Deposit Mineral Status and organisation From the water Podbrezová – Lopej decorative stone Deposit with expected use of reserves – ŠGÚDŠ Bratislava 4.3 km Ore occurrences in the metallogenic map
Occurrence Ore type Metals Type From the water Dolná Lehota – Vajskovský potok Gold ores Au mineralogical occurrence 3.7 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water JK-3 engineering-geological 6.0 m 85748970 m JK-4 engineering-geological 6.0 m 85748980 m JK-2 engineering-geological 5.0 m 85748980 m JK-1 engineering-geological 5.0 m 85748990 m Piesok monitoring borehole 7.0 m 80337 112Ca15.pdf1.5 km Podbrezová structural borehole with ordinary water 100.0 m 57810 112Ca5.pdf2.0 km Podbrezová monitoring borehole 12.5 m 75838 112Ca12.pdf2.0 km DPS-03 engineering-geological 5.0 m 1006612.1 km DPS-04A engineering-geological 0.5 m 1006612.1 km DPS-04B engineering-geological 4.5 m 1006612.1 km KS-1 engineering-geological 0.6 m 1006612.1 km KS-2 engineering-geological 0.7 m 1006612.1 km Geothermal energy and mineral waters
Sources of geothermal and mineral waters
Source Type Water temperature (°C) Yield (l/s) Count Nearest from water category a1 mineral water < 15 < 5 1 9.2 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water TKO Šiklov – Podbrezová 20 000 m² 1980 monitored 1.2 km Valaská – 1979 – 1.7 km Valaská 450 m² 1978 – 1.8 km Izolovaná kazeta 2 – ( JZ smerom je vybudovaná 2.K., ktorá bude rekultivovaná ) – Podbrezová 1 898 m² 2012 monitored 1.8 km Halda Šiklov – Podbrezová – Podbrezová 52 500 m² 1967 monitored 2.0 km Za Húščavou – Valaská – 1982 – 2.8 km Landslides and slope deformations
Types of deformations
Degree of activity
Current state
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
6from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
BariumBaslightly elevated
highest 90.0 μg/lmedian 90.0 μg/l1 sample
StrontiumSrslightly elevated
highest 410 μg/lmedian 410 μg/l1 sample
AntimonySbslightly elevated
highest 1.00 μg/lmedian 1.00 μg/l1 sample
CadmiumCdslightly elevated
highest 0.250 μg/lmedian 0.250 μg/l1 sample
ArsenicAstypical value
highest 1.40 μg/lmedian 1.40 μg/l1 sample
CopperCubelow half of Slovakia
highest 1.20 μg/lmedian 1.20 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
LithiumLibelow half of Slovakia
highest 5.00 μg/lmedian 5.00 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
Silicon dioxideSiO2below half of Slovakia
highest 4.80 mg/lmedian 4.80 mg/l1 sample
AntimonySbextreme (top 1 %)
highest 32.5 μg/lmedian 1.10 μg/l9 samples22 % below the limit of quantification
ArsenicAshigh (top 5 %)
highest 6.40 μg/lmedian 0.500 μg/l9 samples67 % below the limit of quantification
SeleniumSehigh (top 5 %)
highest 3.00 μg/lmedian 0.500 μg/l9 samples78 % below the limit of quantification
CopperCuslightly elevated
highest 2.20 μg/lmedian 1.70 μg/l9 samples
LithiumLitypical value
highest 9.00 μg/lmedian 2.00 μg/l9 samples44 % below the limit of quantification
ZincZntypical value
highest 28.0 μg/lmedian 2.00 μg/l9 samples33 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l2 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l9 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l9 samples100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l9 samples100 % below the limit of quantification
AluminiumAlbelow half of Slovakia
highest 0.00500 mg/lmedian 0.00500 mg/l9 samples100 % below the limit of quantification
ChromiumCrbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l9 samples100 % below the limit of quantification




