Fishing conditions score, the best window of the day and fishing districts from the best conditions Average activity · average of one fishing district 06:00–08:00 VN Zbojné, window score 51. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 00:04. 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. 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 (1 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 8.3modelled estimate water type Ca–HCO₃ Mineralisation 344 mg/l, moderately hard water (12.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Nickel 34.2 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 80. Interpolation of the Geochemical Atlas of river sediments. 45°C at 1,000 m depth heat flow 75 mW/m² Atlas of Geothermal Energy of Slovakia. 53nGy/h dose rate percentile 66 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 8 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 8indicators in the top 5 % highest: Barium 64.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 75 (Výrava). 73boreholes within 3 km 116 water analyses nearby Of these, 71 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 6 geothermal and mineral water springs within 10 km. 3sites within 3 km 3 landfills No environmental burden is registered within 3 km; landfills are only recorded. 3records within 5 km 3 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 27areas 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. 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 The map covers 1 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 8.33typical 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. 12.0°dH, moderately hard Sum of calcium and magnesium (2.15 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 344mg/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. 53nGy/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. -41nT range -41 to -41 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. -17mGal residual +7.5 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. A basin is not just water: slope and elevation determine the speed of runoff, climate the temperature and amount of water, and soils what is washed into the stream. The data come from the geomorphological division, climatic-geographical types and soil maps of ŠGÚDŠ. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off. The line is the water of the fishing district, the light band is the 3 km zone in which boreholes, mine workings and burdens were searched for. The map shows the nearest objects (at most a few dozen from each register), not all of them. The points correspond to the position in the register; area objects are marked by their centre. Arsenic, antimony, cadmium, lead, copper, zinc and other elements in samples from rivers and streams (Geochemical Atlas of Slovakia, surface waters, 2015). The bar shows where the highest value lies among all samples in Slovakia; the light marker is the median of the samples at this water. Highest value: Výrava2009, 80 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: Výrava2009, 80 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Výrava2009, 80 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Výrava2009, 80 m from the water. Comparison: percentile 34 of all samples in Slovakia. Highest value: Výrava2009, 80 m from the water. Comparison: percentile 32 of all samples in Slovakia. Highest value: Výrava, 80 m from the water. Comparison: percentile 26 of all samples in Slovakia. Highest value: Výrava2009, 80 m from the water. Comparison: percentile 22 of all samples in Slovakia. Highest value: Výrava2009, 80 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: Výrava2009, 80 m from the water. Comparison: percentile 24 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: prameň1993, 1.6 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1993, 630 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 78 of all samples in Slovakia. Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: prameň1993, 630 m from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 40 of all samples in Slovakia. Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 39 of all samples in Slovakia. Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 38 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. 73 boreholes in the 3 km zone, of which 2 hydrogeological and 71 other; with an archive report number 71. 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 Zbojné 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



Geology and geochemistry of the VN Zbojné 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 1× Quaternary cover
Tectonic units
Tectonic division
Neotectonic units
Direction of neotectonic movements
Regional geological division
Regional geological division (subunits)
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Aquifer rocks (hydrogeological map 1:200,000)
Aquifer type
Main hydrogeological region
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
67.7 mg/lpercentile 569.14 mg/lpercentile 50210 mg/lpercentile 490.108 mg/lpercentile 472.54 mg/lpercentile 4211.1 mg/lpercentile 3630.6 mg/lpercentile 354.31 mg/lpercentile 30Nutrients and organic pollution
0.0620 mg/lpercentile 310.0167 mg/lpercentile 51.72 mg/lpercentile 50.506 mg/lpercentile 1Metals
0.0971 mg/lpercentile 483.54 μg/lpercentile 2525.8 μg/lpercentile 257.75 μg/lpercentile 15Elements in river sediments
Potentially toxic and trace elements
34.2 mg/kgpercentile 800.402 mg/kgpercentile 780.538 mg/kgpercentile 7426.9 mg/kgpercentile 6377.6 mg/kgpercentile 5971.1 mg/kgpercentile 560.609 mg/kgpercentile 470.170 mg/kgpercentile 468.00 mg/kgpercentile 435.77 mg/kgpercentile 3885.8 mg/kgpercentile 3812.9 mg/kgpercentile 320.0627 mg/kgpercentile 231.96 mg/kgpercentile 190.0666 mg/kgpercentile 2Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1.66 %percentile 725.68 %percentile 524,468 mg/kgpercentile 502.67 %percentile 490.793 %percentile 341.32 %percentile 25636 mg/kgpercentile 230.663 %percentile 21484 mg/kgpercentile 7Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
36.7 mg/kgpercentile 8117.7 mg/kgpercentile 801.89 mg/kgpercentile 7869.8 mg/kgpercentile 7598.8 mg/kgpercentile 74430 mg/kgpercentile 5928.6 mg/kgpercentile 5557.6 mg/kgpercentile 45120 mg/kgpercentile 36380 mg/kgpercentile 28Natural radioactivity and radon
Gamma radiation dose rate
1.40 %percentile 728.10 ppm70th percentile2.50 ppm40th percentile1,365 Bq/m²percentile 42Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Relief, climate and soils
Geomorphological units
Geomorphological regions
Climatic-geographical types
Soil contamination (map 1:500,000)
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 developed spring 1 2,14 Bq/l 2.14 Bq/l source 2 13,6 Bq/l 11.8 Bq/l Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water JV-4 engineering-geological 13.0 m 7256540 m V-28 engineering-geological 5.8 m 2078950 m JV-5 engineering-geological 8.0 m 7256560 m JV-1 engineering-geological 10.6 m 7256580 m JV-3 engineering-geological 8.0 m 7256580 m V-6 engineering-geological 10.0 m 7024780 m JV-2 engineering-geological 8.2 m 7256590 m V-9 engineering-geological 10.0 m 70247100 m V-8 engineering-geological 5.5 m 70247150 m JV-4 engineering-geological 9.0 m 71420150 m JV-2 engineering-geological 7.8 m 71420160 m JV-3 engineering-geological 7.6 m 71420170 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 6.2 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Svetlice 200 m² 1984 – 1.5 km Svetlice 2 000 m² 1991 – 2.4 km Zbojné 240 m² 1984 – 2.4 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
44from 100
1445fishing districts
Map color
Loading map…
lowerhigher
Cations (positive ions)
Anions (negative ions)
BariumBaslightly elevated
highest 64.0 μg/lmedian 64.0 μg/l1 sample
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l1 sample100 % below the limit of quantification
LithiumLibelow half of Slovakia
highest 5.00 μg/lmedian 5.00 μg/l1 sample100 % below the limit of quantification
ChromiumCrbelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.150 μg/lmedian 0.150 μg/l1 sample100 % below the limit of quantification
CopperCubelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l1 sample100 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification
Silicon dioxideSiO2below half of Slovakia
highest 6.73 mg/lmedian 6.73 mg/l1 sample
ChromiumCrextreme (top 1 %)
highest 120 μg/lmedian 0.250 μg/l9 samples56 % below the limit of quantification
AluminiumAlextreme (top 1 %)
highest 0.720 mg/lmedian 0.0100 mg/l9 samples33 % below the limit of quantification
CopperCuhigh (top 5 %)
highest 8.20 μg/lmedian 0.900 μg/l9 samples
LithiumLielevated (top 10 %)
highest 37.0 μg/lmedian 21.0 μg/l9 samples
ZincZnslightly elevated
highest 187 μg/lmedian 17.0 μg/l9 samples
LeadPbslightly elevated
highest 1.00 μg/lmedian 0.500 μg/l9 samples89 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l3 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l9 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l9 samples100 % below the limit of quantification
AntimonySbbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l9 samples100 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l9 samples100 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l9 samples100 % below the limit of quantification





