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 Rakovec, window score 30. 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. 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 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 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 8.2modelled estimate water type Ca–HCO₃ Mineralisation 580 mg/l, hard water (18.2 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Selenium 0.415 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 79. Interpolation of the Geochemical Atlas of river sediments. 65°C at 1,000 m depth heat flow 115 mW/m² At a depth of 2,000 m about 115 °C (increase of 50 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 54nGy/h dose rate percentile 69 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 6 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 9indicators in the top 5 % highest: Lithium 14.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 79 (Rakovec, potok). 126boreholes within 3 km 97 water analyses nearby Of these, 50 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 1 geothermal and mineral water spring within 10 km. 1sites within 3 km 1 landfill No environmental burden is registered within 3 km; landfills are only recorded. 16records within 5 km 8 deposits, 8 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 21areas within 3 km 1 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. 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. 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 8.19typical 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. 18.2°dH, hard Sum of calcium and magnesium (3.25 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 580mg/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. 54nGy/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. -5nT range -5 to -5 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. -6mGal residual +3.5 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. 65 / 115 °Cat depths of 1,000 and 2,000 m increase of 50 °C per km The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 115 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: Rakovec, potok1999, 810 m from the water. Comparison: percentile 79 of all samples in Slovakia. Highest value: Rakovec, potok1999, 810 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: Rakovec, potok1999, 810 m from the water. Comparison: percentile 74 of all samples in Slovakia. Highest value: Rakovec, potok1999, 810 m from the water. Comparison: percentile 57 of all samples in Slovakia. Highest value: Rakovec, potok1999, 810 m from the water. Comparison: percentile 57 of all samples in Slovakia. Highest value: Rakovec, potok1999, 810 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Rakovec, potok1999, 810 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Rakovec, potok1999, 810 m from the water. Comparison: percentile 37 of all samples in Slovakia. Highest value: Rakovec, potok, 810 m from the water. Comparison: percentile 26 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Rakovec, potok1999, 810 m from the water. Comparison: percentile 71 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, 1.0 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1993, 1.9 km from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: vrt1993, 1.9 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: vrt1993, 960 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: vrt1993, 2.5 km from the water. Comparison: percentile 89 of all samples in Slovakia. Highest value: vrt1993, 550 m from the water. Comparison: percentile 88 of all samples in Slovakia. Highest value: studňa1993, 1.0 km from the water. Comparison: percentile 86 of all samples in Slovakia. Highest value: vrt1993, 1.9 km from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: vrt1993, 2.9 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: vrt1993, 2.9 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: vrt1993, 2.9 km from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: vrt1993, 2.9 km from the water. Comparison: percentile 40 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. 126 boreholes in the 3 km zone, of which 11 hydrogeological and 115 other; with an archive report number 50. 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 VN Rakovec 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 Rakovec watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VN Rakovec 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
Quaternary cover
Tectonic division
Neotectonic units
Direction of neotectonic movements
Regional geological division
Regional geological division (subunits)
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
0.320 mg/lpercentile 94100 mg/lpercentile 87353 mg/lpercentile 876.28 mg/lpercentile 8216.6 mg/lpercentile 7423.8 mg/lpercentile 7418.4 mg/lpercentile 6142.4 mg/lpercentile 53Nutrients and organic pollution
4.04 mg/lpercentile 9511.6 mg/lpercentile 784.36 mg/lpercentile 730.126 mg/lpercentile 48Metals
472 μg/lpercentile 950.517 mg/lpercentile 93235 μg/lpercentile 835.10 μg/lpercentile 38Elements in river sediments
Potentially toxic and trace elements
0.415 mg/kgpercentile 7993.8 mg/kgpercentile 7728.5 mg/kgpercentile 660.437 mg/kgpercentile 607.36 mg/kgpercentile 599.00 mg/kgpercentile 590.539 mg/kgpercentile 400.0722 mg/kgpercentile 300.113 mg/kgpercentile 3060.2 mg/kgpercentile 3012.4 mg/kgpercentile 2918.8 mg/kgpercentile 2765.6 mg/kgpercentile 141.53 mg/kgpercentile 60.0778 mg/kgpercentile 3Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
3,663 mg/kgpercentile 961.74 %percentile 814,625 mg/kgpercentile 56888 mg/kgpercentile 562.60 %percentile 455.24 %percentile 361.51 %percentile 330.718 %percentile 200.545 %percentile 7Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
17.8 mg/kgpercentile 80478 mg/kgpercentile 63436 mg/kgpercentile 6192.8 mg/kgpercentile 6161.3 mg/kgpercentile 5825.5 mg/kgpercentile 3826.8 mg/kgpercentile 3451.5 mg/kgpercentile 26105 mg/kgpercentile 190.520 mg/kgpercentile 8Natural radioactivity and radon
Gamma radiation dose rate
8.48 ppm77th percentile2.78 ppm71th percentile1.30 %percentile 50297 Bq/m²percentile 3Geophysical 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
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 2 18,7 Bq/l 11.6 Bq/l well 1 15,7 Bq/l 15.7 Bq/l Mine workings, deposits and ore occurrences
Deposits and mining areas
Deposit Mineral Status and organisation From the water Rakovec nad Ondavou combustible natural gas Deposit, where geological exploration is under way – NAFTA a.s. 1.3 km Moravany combustible natural gas Deposit with halted mining or where use of reserves is not expected – NAFTA a.s. 3.2 km Moravany combustible natural gas Deposit with halted mining or where use of reserves is not expected – NAFTA a.s. 3.3 km Moravany combustible natural gas Deposit with halted mining or where use of reserves is not expected – NAFTA a.s. 3.3 km Trhovište – Pozdišovce combustible natural gas Deposit with halted mining or where use of reserves is not expected – NAFTA a.s. 4.0 km Trhovište – Pozdišovce gasoline Deposit with halted mining or where use of reserves is not expected – NAFTA a.s. 4.0 km Trhovište – Pozdišovce combustible natural gas Deposit with halted mining or where use of reserves is not expected – NAFTA a.s. 4.0 km Trhovište – Pozdišovce gasoline Deposit with halted mining or where use of reserves is not expected – NAFTA a.s. 4.0 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Cf Me-172 deposit 313.0 m – 270 m Rak-5 deposit 1,495.0 m – 330 m VS-5 deposit 301.3 m 82068340 m Rak-4 deposit 1,500.0 m – 430 m Rakovec nad Ondavou narrow-diameter borehole with ordinary drinking and process water 50.8 m 4828 116Da37.pdf470 m Cf Me-171 deposit 310.0 m – 560 m Pb40 engineering-geological 4.2 m 90850590 m Cf Me-173 deposit 303.0 m – 610 m Pb41 engineering-geological 4.1 m 90850650 m Rakovec-3 deposit 3,700.0 m 60756700 m Pb39 engineering-geological 4.2 m 90850740 m Cf Sč-351 deposit 303.0 m – 760 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 1 2.1 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Rakovec nad Ondavou 12 500 m² 1965 – 1.7 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
26from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
LithiumLislightly elevated
highest 14.0 μg/lmedian 14.0 μg/l1 sample
StrontiumSrtypical value
highest 319 μg/lmedian 319 μg/l1 sample
ChromiumCrtypical value
highest 1.90 μg/lmedian 1.90 μg/l1 sample
CopperCutypical value
highest 1.60 μg/lmedian 1.60 μg/l1 sample
ArsenicAstypical value
highest 1.26 μg/lmedian 1.26 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
AntimonySbbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 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
Silicon dioxideSiO2typical value
highest 17.0 mg/lmedian 17.0 mg/l1 sample
SeleniumSeextreme (top 1 %)
highest 6.50 μg/lmedian 0.500 μg/l8 samples75 % below the limit of quantification
CopperCuhigh (top 5 %)
highest 9.30 μg/lmedian 0.525 μg/l8 samples
LeadPbhigh (top 5 %)
highest 4.00 μg/lmedian 1.00 μg/l8 samples38 % below the limit of quantification
ZincZnhigh (top 5 %)
highest 1,216 μg/lmedian 189 μg/l8 samples
ArsenicAsslightly elevated
highest 2.10 μg/lmedian 0.500 μg/l8 samples75 % below the limit of quantification
ChromiumCrslightly elevated
highest 1.80 μg/lmedian 0.600 μg/l8 samples38 % below the limit of quantification
LithiumLislightly elevated
highest 28.0 μg/lmedian 17.0 μg/l8 samples
AluminiumAlslightly elevated
highest 0.0100 mg/lmedian 0.00500 mg/l8 samples88 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l4 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l8 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l8 samples100 % below the limit of quantification
AntimonySbbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l8 samples100 % below the limit of quantification

