Fishing conditions score, the best window of the day and fishing districts from the best conditions Low activity · average of one fishing district 15:00–17:00 VVN Domaša, window score 17. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 01:04. 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. Still water This is standing water, 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 (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. River alluvium100% of the water line Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000. pH 8.2modelled estimate water type Ca–HCO₃ Mineralisation 136 mg/l, moderately hard water (11.2 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 1 from 15elements in the top 10 % highest: Chromium 130 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 91. 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. 48nGy/h dose rate percentile 28 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 10 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. 2 from 6indicators in the top 5 % highest: Cadmium 1.00 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 96 (Ondava). 104boreholes within 3 km 227 water analyses nearby Of these, 104 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 7 geothermal and mineral water springs within 10 km. 14sites within 3 km 14 landfills No environmental burden is registered within 3 km; landfills are only recorded. 10records within 5 km 10 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 53areas within 3 km 6 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 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 3 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 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. 11.2°dH, moderately hard Sum of calcium and magnesium (2.00 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 136mg/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. 48nGy/h in air range 45 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 -43 to -36 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. -5mGal residual +14.1 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. 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: Ondava, 60 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: Ondava2000, 220 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: Ondava2000, 220 m from the water. Comparison: percentile 76 of all samples in Slovakia. Highest value: Ondava2000, 220 m from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: Ondava1999, 60 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Ondava1999, 60 m from the water. Comparison: percentile 32 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: prameň1994, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1993, 1.7 km from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: prameň1992, 2.9 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1993, 280 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1993, 280 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: prameň1994, 2.3 km from the water. Comparison: percentile 94 of all samples in Slovakia. Highest value: studňa1993, 2.5 km from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: studňa1993, 270 m from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1993, 270 m from the water. Comparison: percentile 87 of all samples in Slovakia. Highest value: studňa1993, 270 m from the water. Comparison: percentile 83 of all samples in Slovakia. Highest value: studňa1993, 1.4 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: studňa1993, 1.4 km from the water. Comparison: percentile 46 of all samples in Slovakia. 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. 104 boreholes in the 3 km zone, of which 74 hydrogeological and 30 other; with an archive report number 104. 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 VVN Domaša watercourse
Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the watercourse
Elevation profile: standing water
Terrain in 3D
Historical images



Water pollution on the VVN Domaša watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VVN Domaša 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× Quaternary Holocene fluvial sediments: resedimented alluvial sandy gravels of the near-channel zone 1× Quaternary cover
Tectonic units
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
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
0.374 mg/lpercentile 9521.3 mg/lpercentile 816.14 mg/lpercentile 81274 mg/lpercentile 7048.4 mg/lpercentile 6061.0 mg/lpercentile 486.57 mg/lpercentile 4211.6 mg/lpercentile 37Nutrients and organic pollution
7.28 mg/lpercentile 580.123 mg/lpercentile 543.27 mg/lpercentile 520.0596 mg/lpercentile 31Metals
77.0 μg/lpercentile 540.0609 mg/lpercentile 293.37 μg/lpercentile 249.70 μg/lpercentile 20Elements in river sediments
Potentially toxic and trace elements
130 mg/kgpercentile 910.644 mg/kgpercentile 8324.8 mg/kgpercentile 510.162 mg/kgpercentile 270.138 mg/kgpercentile 214.26 mg/kgpercentile 1553.4 mg/kgpercentile 155.88 mg/kgpercentile 1414.0 mg/kgpercentile 81.54 mg/kgpercentile 656.4 mg/kgpercentile 50.0541 mg/kgpercentile 40.221 mg/kgpercentile 40.0305 mg/kgpercentile 46.32 mg/kgpercentile 3Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
3.04 %percentile 66761 mg/kgpercentile 400.787 %percentile 333,915 mg/kgpercentile 281.31 %percentile 212.03 %percentile 120.583 %percentile 114.15 %percentile 7447 mg/kgpercentile 5Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
571 mg/kgpercentile 9064.7 mg/kgpercentile 62120 mg/kgpercentile 3554.9 mg/kgpercentile 3522.8 mg/kgpercentile 2524.5 mg/kgpercentile 2171.9 mg/kgpercentile 140.611 mg/kgpercentile 11301 mg/kgpercentile 53.90 mg/kgpercentile 2Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.27 %percentile 377.03 ppm37th percentile2.34 ppm24th percentile2,765 Bq/m²percentile 84Radon 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 developed spring 4 45,8 Bq/l 23.8 Bq/l source 1 0,760 Bq/l 0.760 Bq/l well 5 31,4 Bq/l 12.7 Bq/l other 1 0,670 Bq/l 0.670 Bq/l water source for individual supply 1 16,8 Bq/l 16.8 Bq/l Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water VS-2 engineering-geological 20.0 m 285750 m VS-3 engineering-geological 20.0 m 285760 m VR-1 engineering-geological 15.0 m 2857110 m VS-1 engineering-geological 20.0 m 2857120 m VR-3 engineering-geological 10.0 m 2857140 m VR-2 engineering-geological 15.0 m 2857210 m V.D. Domaša narrow-diameter borehole with ordinary drinking and process water 19.0 m 21309 116Ab29.pdf220 m Domaša monitoring borehole 25.0 m 39008 104Cd55.pdf220 m Domaša monitoring borehole 30.0 m 39008 104Cd47.pdf230 m Slovenská Kajňa wide-diameter borehole – 61514 116Ab58.pdf230 m Domaša monitoring borehole 30.0 m 39008 104Cd48.pdf260 m Domaša monitoring borehole 35.0 m 39008 104Cd49.pdf300 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 6 6.1 km category b1 mineral water 15-22 < 5 1 9.5 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Slovenská Kajňa 50 m² – – 70 m Malá Domaša – – – 560 m Kvakovce 100 m² – – 680 m Slovenská Kajňa 130 m² – – 950 m Slovenská Kajňa 50 m² – – 1.2 km Beniakovce – Benkovce 500 m² – – 1.3 km Žalobín 30 m² – – 1.3 km Žalobín 40 m² – – 1.3 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
10from 100
1445fishing districts
Map color
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Cations (positive ions)
Anions (negative ions)
CadmiumCdhigh (top 5 %)
highest 1.00 μg/lmedian 1.00 μg/l4 samples
LeadPbhigh (top 5 %)
highest 5.00 μg/lmedian 5.00 μg/l5 samples
CopperCuslightly elevated
highest 2.50 μg/lmedian 2.50 μg/l5 samples
ArsenicAstypical value
highest 1.00 μg/lmedian 1.00 μg/l5 samples
BariumBabelow half of Slovakia
highest 37.0 μg/lmedian 36.5 μg/l2 samples
ChromiumCrbelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l3 samples100 % below the limit of quantification
AluminiumAlextreme (top 1 %)
highest 0.350 mg/lmedian 0.0150 mg/l18 samples33 % below the limit of quantification
SeleniumSehigh (top 5 %)
highest 4.80 μg/lmedian 0.500 μg/l18 samples56 % below the limit of quantification
LeadPbhigh (top 5 %)
highest 4.00 μg/lmedian 1.00 μg/l18 samples11 % below the limit of quantification
ChromiumCrhigh (top 5 %)
highest 4.90 μg/lmedian 1.25 μg/l18 samples6 % below the limit of quantification
CadmiumCdhigh (top 5 %)
highest 0.500 μg/lmedian 0.250 μg/l18 samples94 % below the limit of quantification
LithiumLielevated (top 10 %)
highest 50.0 μg/lmedian 14.0 μg/l18 samples
ZincZnelevated (top 10 %)
highest 539 μg/lmedian 44.5 μg/l18 samples
CopperCuelevated (top 10 %)
highest 3.80 μg/lmedian 1.20 μg/l18 samples
AntimonySbslightly elevated
highest 0.300 μg/lmedian 0.100 μg/l18 samples89 % below the limit of quantification
ArsenicAsslightly elevated
highest 1.30 μg/lmedian 0.500 μg/l18 samples89 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l5 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l18 samples100 % below the limit of quantification


