Fishing conditions score, the best window of the day and fishing districts from the best conditions Average activity · average of one fishing district 15:00–17:00 Biela voda (Kežmarok), window score 51. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 13:04. 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. Measurement of water level, temperature and flow, weather by the watercourse and status from satellites How the watercourse falls downstream: fall, gradient and water speed. Fast watercourse Podhorský potok: fast water, stony bottom, riffles and the pools below them. Typical trout waters. Source: Open Topo Data (eudem25m), 4 Nov 2026. Gradient and fall are approximate and include only the sections of fishing districts. Loading the 3D terrain model… Changes in the surroundings and nature from 2019 to 2025: 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 (5 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 8.0modelled estimate water type Ca–Mg–HCO₃ Mineralisation 129 mg/l, soft water (4.2 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Tin 3.02 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 63. Interpolation of the Geochemical Atlas of river sediments. 35°C at 1,000 m depth heat flow 65 mW/m² At a depth of 2,000 m about 65 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 53nGy/h dose rate percentile 65 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 12 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. 1 from 7indicators in the top 5 % highest: Cadmium 1.30 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 97 (Kežmarok). 127boreholes within 3 km 236 water analyses nearby Of these, 127 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. 62°C at the wellhead 5 geothermal boreholes within 10 km Warmest: Veľká Lomnica – GVL-1, yield 54.9 l/s, 4.5 km from the water. 25sites within 3 km 2 environmental burdens, 23 landfills Nearest burden: Kežmarok – bývalé kasárne, 670 m from the water. Proximity does not mean that substances leak from the site into the water. 4records within 5 km 1 deposit, 3 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 8areas 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 marker on the bar: share among all sample points on streams in Slovakia The map covers 0 of 3 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 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 8.00typical 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. 4.2°dH, soft Sum of calcium and magnesium (0.74 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 129mg/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. 53nGy/h in air range 49 to 58 nGy/h 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. -24nT range -27 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. -56mGal residual −11.9 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. 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 65 mW/m². marker on the bar: share among all sample points on streams in Slovakia 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 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: Kežmarok, 190 m from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: Kežmarok2002, 190 m from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: Kežmarok2002, 190 m from the water. Comparison: percentile 82 of all samples in Slovakia. Highest value: Kežmarok2002, 190 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: Kežmarok2002, 190 m from the water. Comparison: percentile 66 of all samples in Slovakia. Highest value: Kežmarok2002, 190 m from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: Kežmarok2002, 100 m from the water. Comparison: percentile 37 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: prameň1992, 900 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1992, 900 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: vrt1992, 1.3 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1992, 1.2 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1992, 900 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1992, 870 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: prameň1992, 2.3 km from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: prameň1992, 2.0 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1992, 2.5 km from the water. Comparison: percentile 82 of all samples in Slovakia. Highest value: prameň1992, 1.7 km from the water. Comparison: percentile 54 of all samples in Slovakia. Highest value: prameň1992, 2.0 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1992, 2.6 km from the water. Comparison: percentile 47 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. 127 boreholes in the 3 km zone, of which 45 hydrogeological and 82 other; with an archive report number 127. 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 Bodrog basin and Hornád
By the water now
Today on the Biela voda (Kežmarok) watercourse
Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the watercourse
Water state on the watercourse
Water levels on the watercourse
Station Status Change Temperature Dohňany 23 cm – Ždiar – Lysá Poľana 163 cm – Elevation profile of the watercourse
Terrain in 3D
Historical images



Water pollution on the Biela voda (Kežmarok) watercourse
Problem treatment plants near the fishing districts1 treatment plant within 2 km of the fishing district
Groundwater: measured valuestypical value from stations within 10 km, 2025
Watercourse profile from source to mouthnumber of unmet indicators in 2025 at SHMÚ sites
Show sites in the table (2)
Geology and geochemistry of the Biela voda (Kežmarok) 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
Tectonic division
Neotectonic units
Direction of neotectonic movements
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
Type of permeability (basic hydrogeological map 1:50,000)
Hydrogeological function
Main hydrogeological region
Geothermal groundwater bodies
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
0.101 mg/lpercentile 434.07 mg/lpercentile 283.46 mg/lpercentile 1678.0 mg/lpercentile 131.11 mg/lpercentile 1221.4 mg/lpercentile 115.07 mg/lpercentile 1114.4 mg/lpercentile 6Nutrients and organic pollution
0.210 mg/lpercentile 693.24 mg/lpercentile 520.131 mg/lpercentile 490.686 mg/lpercentile 1Metals
11.9 μg/lpercentile 710.159 mg/lpercentile 67117 μg/lpercentile 6546.0 μg/lpercentile 60Elements in river sediments
Potentially toxic and trace elements
3.02 mg/kgpercentile 630.290 mg/kgpercentile 6026.0 mg/kgpercentile 560.220 mg/kgpercentile 5169.3 mg/kgpercentile 450.345 mg/kgpercentile 446.04 mg/kgpercentile 4287.9 mg/kgpercentile 4013.5 mg/kgpercentile 370.125 mg/kgpercentile 340.470 mg/kgpercentile 320.0688 mg/kgpercentile 2858.6 mg/kgpercentile 266.01 mg/kgpercentile 1515.4 mg/kgpercentile 12Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1.47 %percentile 941,392 mg/kgpercentile 861.65 %percentile 716.22 %percentile 68925 mg/kgpercentile 602.53 %percentile 400.656 %percentile 201.07 %percentile 163,469 mg/kgpercentile 14Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
220 mg/kgpercentile 9179.6 mg/kgpercentile 91625 mg/kgpercentile 8836.0 mg/kgpercentile 7889.4 mg/kgpercentile 5313.8 mg/kgpercentile 481.35 mg/kgpercentile 4626.6 mg/kgpercentile 45383 mg/kgpercentile 4351.6 mg/kgpercentile 26Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.56 %percentile 877.57 ppm57th percentile2.36 ppm25th percentile1,178 Bq/m²percentile 30Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Rock temperature with depth
Geothermal groundwater bodies beneath the water line
Relief, climate and soils
Geomorphological units
Geomorphological regions
Climatic-geographical types
Susceptibility of soils to acidification
Soil contamination (map 1:500,000)
Lithogeochemical types
Map of the corridor
Trace elements in surface waters
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 4 14,1 Bq/l 9.84 Bq/l well 4 13,4 Bq/l 7.65 Bq/l water source for individual supply 1 4,17 Bq/l 4.17 Bq/l developed spring 1 9,00 Bq/l 9.00 Bq/l Mine workings, deposits and ore occurrences
Deposits and mining areas
Deposit Mineral Status and organisation From the water Rakúsy gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – AGROSTAV, stavebno-obchodné družstvo Poprad 3.6 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water BV-31 engineering-geological 3.5 m 7647210 m K-12š engineering-geological 5.0 m 8614210 m Kežmarok – 18913 101Db22.pdf70 m Kežmarok – 18913 101Db21.pdf80 m Kežmarok narrow-diameter borehole with ordinary drinking and process water 4.3 m 3869 101Db30.pdf80 m BV-20 engineering-geological 3.5 m 76472130 m K-11š engineering-geological 4.5 m 86142130 m K-10š engineering-geological 4.5 m 86142150 m K-10v engineering-geological 3.5 m 86142160 m K-8š engineering-geological 4.5 m 86142250 m K-8v engineering-geological 3.5 m 86142250 m Kežmarok wide-diameter borehole 6.0 m 19645 101Db13.pdf260 m Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Kežmarok – GTK-1 47 °C 1.5 l/s 2500 m Na-HCO3 in use 2.5 km Veľká Lomnica – GVL-1 62 °C 54.9 l/s 2100 m Ca-Mg-HCO3-SO4 in use 4.5 km Stará Lesná – FGP-1 58 °C 22.0 l/s 3616 m Ca-Mg-HCO3 unused 6.0 km Vrbov – Vr-2 59 °C 33.0 l/s 2502 m Ca-Mg-HCO3-SO4 in use 7.1 km Vrbov – Vr-1 56 °C 28.3 l/s 1742 m Ca-Mg-HCO3-SO4 in use 7.5 km Sources of geothermal and mineral waters
Source Type Water temperature (°C) Yield (l/s) Count Nearest from water FGP-1 geothermal water 55 – 80 16 – 30 1 5.9 km category a1 mineral water < 15 < 5 9 6.0 km Vr-1.2 geothermal water 55 – 80 16 – 30 1 6.5 km category Stará Lesná thermal baths – – 1 6.7 km category Vrbov thermal baths – – 1 8.3 km Environmental burdens, landfills and anthropogenic sediments
Environmental burdens
Site Activity Substance Classification From the water Kežmarok – bývalé kasárne SK1001000P 670 m Kežmarok – OKTAN SK1001000P 1.1 km Waste landfills
Landfill Area Year established Monitoring From the water Kežmarok 100 m² 1985 – 40 m Kežmarok – 1955 – 50 m Mlynčeky 40 m² 1980 – 80 m Kežmarok 80 m² 1980 – 110 m Tatranská Lomnica – 1970 – 140 m Tatranská Lomnica – 1970 – 330 m Kežmarok – 1960 – 910 m Kežmarok 150 m² 1960 – 920 m 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
47from 100
1445fishing districts
Map color
Loading map…
lowerhigher
Cations (positive ions)
Anions (negative ions)
CadmiumCdhigh (top 5 %)
highest 1.30 μg/lmedian 0.300 μg/l3 samples
LeadPbelevated (top 10 %)
highest 4.00 μg/lmedian 4.00 μg/l3 samples
AntimonySbslightly elevated
highest 1.00 μg/lmedian 1.00 μg/l3 samples
LithiumLislightly elevated
highest 10.0 μg/lmedian 10.0 μg/l3 samples
CopperCutypical value
highest 2.00 μg/lmedian 2.00 μg/l3 samples
ArsenicAstypical value
highest 1.00 μg/lmedian 1.00 μg/l3 samples
BariumBabelow half of Slovakia
highest 30.0 μg/lmedian 30.0 μg/l3 samples
ChromiumCrextreme (top 1 %)
highest 26.1 μg/lmedian 0.250 μg/l19 samples68 % below the limit of quantification
AluminiumAlextreme (top 1 %)
highest 0.210 mg/lmedian 0.0100 mg/l19 samples42 % below the limit of quantification
LithiumLihigh (top 5 %)
highest 121 μg/lmedian 15.0 μg/l19 samples5 % below the limit of quantification
MercuryHghigh (top 5 %)
highest 0.300 μg/lmedian 0.100 μg/l19 samples79 % below the limit of quantification
AntimonySbhigh (top 5 %)
highest 1.20 μg/lmedian 0.200 μg/l19 samples32 % below the limit of quantification
CopperCuhigh (top 5 %)
highest 6.80 μg/lmedian 0.700 μg/l19 samples
SeleniumSeelevated (top 10 %)
highest 2.10 μg/lmedian 0.500 μg/l19 samples89 % below the limit of quantification
LeadPbelevated (top 10 %)
highest 2.00 μg/lmedian 0.500 μg/l19 samples79 % below the limit of quantification
ArsenicAsslightly elevated
highest 1.20 μg/lmedian 0.500 μg/l19 samples95 % below the limit of quantification
ZincZntypical value
highest 37.0 μg/lmedian 6.00 μg/l19 samples16 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l1 sample100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l19 samples100 % below the limit of quantification

