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 Šibská voda, window score 40. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 07:04. 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. Bystrina A mountain stream with a steep gradient, cascades and a rocky bottom. The water is clear and cold; fishing requires a careful approach. 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 1 of 1 fishing districts on the watercourse with SHMÚ data: the nearest site has an unmet standard in at least one indicator. 0 of 1 fishing district with measurements has groundwater nearby with a value above the limit for at least one indicator. Water pollution in the Bodrog basinPolluted water in Slovakia 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 (14 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. River alluvium50% of the water line 25% sandstones and conglomerates, 25% flysch Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000. pH 8.3modelled estimate water type Ca–HCO₃ Mineralisation 406 mg/l, moderately hard water (12.9 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Chromium 91.4 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 75. Interpolation of the Geochemical Atlas of river sediments. 45°C at 1,000 m depth heat flow 75 mW/m² At a depth of 2,000 m about 75 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 45nGy/h dose rate percentile 15 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. 12samples with gold 17 ore minerals in the sediment Up to 2 grains in one sample (80 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment. 0 from 8indicators in the top 5 % highest: Barium 62.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 73 (bez mena). 2,618boreholes within 3 km 492 water analyses nearby Of these, 2618 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 13 geothermal and mineral water springs within 10 km. 26sites within 3 km 4 environmental burdens, 22 landfills Nearest burden: Bardejov – areál SNAHA v.d., 490 m from the water. Proximity does not mean that substances leak from the site into the water. 14records within 5 km 14 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 33areas within 3 km 11 active 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. The points follow the water line (for a stream and a basin, fishing district after fishing district). The strip is a cross-section by distance, not a map; the width of a section corresponds to the number of points. marker on the bar: share among all sample points on streams in Slovakia River alluvium: Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. 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 marker on the bar: share among all sample points on streams in Slovakia The map covers 4 of 6 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 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 8.33typical 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. 12.9°dH, moderately hard Sum of calcium and magnesium (2.31 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 406mg/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–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. 45nGy/h in air range 42 to 49 nGy/h Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains. 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. 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. -39nT range -48 to -35 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. -29mGal residual +7.2 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. 45 / 75 °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 75 mW/m². 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: bez mena2008, 60 m from the water. Comparison: percentile 73 of all samples in Slovakia. Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 34 of all samples in Slovakia. Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 32 of all samples in Slovakia. Highest value: Šibská voda, 100 m from the water. Comparison: percentile 26 of all samples in Slovakia. Highest value: Šibská voda2008, 100 m from the water. Comparison: percentile 22 of all samples in Slovakia. Highest value: Šibská voda2008, 100 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: Richvaldský potok2008, 790 m from the water. Comparison: percentile 46 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: studňa1993, 1.9 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1993, 2.0 km from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: studňa1993, 1.5 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1993, 760 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1993, 1.5 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: prameň1993, 2.2 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1993, 40 m from the water. Comparison: percentile 83 of all samples in Slovakia. Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 46 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. 2,618 boreholes in the 3 km zone, of which 126 hydrogeological and 2492 other; with an archive report number 2618. 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 Šibská voda 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 Kľušovská Zábava 55 cm – Elevation profile of the watercourse
Terrain in 3D
Historical images



Water pollution on the Šibská voda watercourse
Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025
Most polluted fishing districtsall with an unmet standard
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the Šibská voda stream
Rock under the water
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
Geological age of the rocks
Most common rock units
System Age Unit Points Quaternary Holocene fluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains 2× flysch Eocene – Oligocene Malcov Formation 1× flysch Eocene Strihovce and older Malcov Formations 1× Quaternary cover
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
Genetic type of groundwater
Chemical type of groundwater
Groundwater quality class
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
69.3 mg/lpercentile 5810.1 mg/lpercentile 54225 mg/lpercentile 543.12 mg/lpercentile 529.58 mg/lpercentile 5214.1 mg/lpercentile 4636.2 mg/lpercentile 440.0781 mg/lpercentile 29Nutrients and organic pollution
30.0 mg/lpercentile 950.0939 mg/lpercentile 420.0516 mg/lpercentile 262.08 mg/lpercentile 22Metals
21.8 μg/lpercentile 410.0578 mg/lpercentile 271.13 μg/lpercentile 310.3 μg/lpercentile 1Elements in river sediments
Potentially toxic and trace elements
91.4 mg/kgpercentile 750.269 mg/kgpercentile 6722.0 mg/kgpercentile 370.181 mg/kgpercentile 352.08 mg/kgpercentile 250.145 mg/kgpercentile 2210.6 mg/kgpercentile 1716.4 mg/kgpercentile 160.185 mg/kgpercentile 1364.0 mg/kgpercentile 1251.1 mg/kgpercentile 110.292 mg/kgpercentile 105.06 mg/kgpercentile 80.0384 mg/kgpercentile 62.99 mg/kgpercentile 4Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1.16 %percentile 844,663 mg/kgpercentile 571.51 %percentile 495.08 %percentile 301.18 %percentile 20536 mg/kgpercentile 100.575 %percentile 101.97 %percentile 9496 mg/kgpercentile 8Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
465 mg/kgpercentile 701.51 mg/kgpercentile 5658.7 mg/kgpercentile 4426.1 mg/kgpercentile 4180.8 mg/kgpercentile 30367 mg/kgpercentile 2350.6 mg/kgpercentile 2023.9 mg/kgpercentile 188.00 mg/kgpercentile 1090.4 mg/kgpercentile 6Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.26 %percentile 336.36 ppm16th percentile2.17 ppm13th percentile1,069 Bq/m²percentile 22Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Rock temperature with depth
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
Major ions, mineralisation and pH
Gold and ore minerals in river sediments
Nearest samples with gold
Sample Gold in sample From the water 2004 2 grains 20 m 2013 2 grains 40 m 1999 1 grain 50 m 1817 1 grain 60 m 2001 1 grain 70 m 1823 1 grain 70 m 2000 2 grains 80 m 1825 1 grain 80 m 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 stream, river 1 0,500 Bq/l 0.500 Bq/l developed spring 2 18,8 Bq/l 10.8 Bq/l source 6 12,5 Bq/l 9.17 Bq/l water source for public supply 1 3,82 Bq/l 3.82 Bq/l Mine workings, deposits and ore occurrences
Ore occurrences in the metallogenic map
Occurrence Ore type Metals Type From the water Kľušov Mercury ores Hg mineralogical occurrence? 2.3 km Bardejov Arsenic ores As mineralogical occurrence 3.7 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Bardejov narrow-diameter borehole with ordinary drinking and process water 7.3 m 25039 103Ba62.pdf10 m S-2 engineering-geological 7.0 m 2489410 m V-5 engineering-geological 6.0 m 1744320 m S-5 engineering-geological 5.0 m 2489420 m V-1 engineering-geological 8.8 m 6151320 m Bardejov narrow-diameter borehole with ordinary drinking and process water 5.8 m 21066 103Ba21.pdf30 m Bardejov wide-diameter borehole 8.0 m 64502 103Ba95.pdf30 m S-4 engineering-geological 3.0 m 2489430 m S-1 engineering-geological 2.4 m 196330 m JV-5 engineering-geological 3.2 m 7200930 m JV-4 engineering-geological 7.0 m 7202230 m JV-3 engineering-geological 9.0 m 7202230 m 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 12 820 m category b1 mineral water 15-22 < 5 1 2.4 km Environmental burdens, landfills and anthropogenic sediments
Environmental burdens
Site Activity Substance Classification From the water Bardejov – areál SNAHA v.d. SK1001300P 490 m Bardejov – areál podniku JAS SK1001300P 940 m Bardejov – areál Bardejovských strojární (ZŤS) SK1001300P 1.8 km Bardejov – elektrická stanica (ES) SK1001300P 2.2 km Waste landfills
Landfill Area Year established Monitoring From the water Bardejov 200 m² 1980 – 60 m Bardejovská Zábava – Bardejov 80 m² 1980 – 60 m Bardejovská Zábava – Bardejov 60 m² 1985 – 60 m Bardejovská Zábava – Bardejov – 1985 – 70 m Šiba – 1980 – 80 m Bardejov 500 m² 1980 – 120 m Bardejov 300 m² 1975 – 150 m Bardejov 100 m² 1980 – 160 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
34from 100
1445fishing districts
Map color
Loading map…
lowerhigher
Cations (positive ions)
Anions (negative ions)
BariumBatypical value
highest 62.0 μg/lmedian 56.0 μg/l3 samples
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l3 samples100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l3 samples100 % below the limit of quantification
LithiumLibelow half of Slovakia
highest 5.00 μg/lmedian 5.00 μg/l3 samples100 % below the limit of quantification
ChromiumCrbelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l3 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.150 μg/lmedian 0.150 μg/l3 samples100 % below the limit of quantification
CopperCubelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l3 samples100 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l3 samples100 % below the limit of quantification
Silicon dioxideSiO2below half of Slovakia
highest 9.97 mg/lmedian 9.72 mg/l3 samples
ZincZnextreme (top 1 %)
highest 6,275 μg/lmedian 14.0 μg/l38 samples5 % below the limit of quantification
ChromiumCrhigh (top 5 %)
highest 9.20 μg/lmedian 0.250 μg/l38 samples79 % below the limit of quantification
CopperCuhigh (top 5 %)
highest 9.60 μg/lmedian 0.250 μg/l38 samples
ArsenicAshigh (top 5 %)
highest 6.30 μg/lmedian 0.500 μg/l38 samples97 % below the limit of quantification
SeleniumSeelevated (top 10 %)
highest 1.80 μg/lmedian 0.500 μg/l38 samples66 % below the limit of quantification
AluminiumAlelevated (top 10 %)
highest 0.0400 mg/lmedian 0.0100 mg/l38 samples47 % below the limit of quantification
LithiumLielevated (top 10 %)
highest 33.0 μg/lmedian 9.50 μg/l38 samples5 % below the limit of quantification
LeadPbelevated (top 10 %)
highest 2.00 μg/lmedian 0.500 μg/l38 samples76 % below the limit of quantification
AntimonySbslightly elevated
highest 0.200 μg/lmedian 0.100 μg/l38 samples97 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l25 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l38 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l38 samples100 % below the limit of quantification


