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 VN Sigord, window score 30. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 04:04. 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. 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 7.9modelled estimate water type Ca–Mg–HCO₃–SO₄ Mineralisation 250 mg/l, soft water (7.7 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 2 from 15elements in the top 10 % highest: Mercury 1.88 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 95. Interpolation of the Geochemical Atlas of river sediments. 45°C at 1,000 m depth heat flow 85 mW/m² At a depth of 2,000 m about 85 °C (increase of 40 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 57nGy/h dose rate percentile 79 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. 2samples with gold 15 ore minerals in the sediment Up to 3 grains in one sample (650 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment. 0 from 10indicators in the top 5 % highest: Antimony 1.50 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 90 (Malá Delna, pod nádržou). 52boreholes within 3 km 124 water analyses nearby Of these, 50 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 12 geothermal and mineral water springs within 10 km. 5sites within 3 km 5 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. 16areas within 3 km 2 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 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 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 7.94typical 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. 7.7°dH, soft Sum of calcium and magnesium (1.37 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 250mg/l mineralisation Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds. Water type by dominant ions: Ca–Mg–HCO₃–SO₄ 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. 57nGy/h in air 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. -82nT range -82 to -82 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. -24mGal residual −3.2 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 / 85 °Cat depths of 1,000 and 2,000 m increase of 40 °C per km The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 85 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 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: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 86 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou, 80 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 48 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 44 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 34 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 32 of all samples in Slovakia. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 23 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Malá Delna, pod nádržou1992, 80 m from the water. Comparison: percentile 91 of all samples in Slovakia. Regional panning prospecting: the heavy fraction was washed out of river gravel and the mineral grains in it were counted. The map of finds is positive: a sample without gold is not listed in the atlas, so the absence of a find is not proof that there is no gold. Hydrogeochemical objects (analyses of springs and boreholes), the geochemical atlas of groundwater (1996) and radiohydrochemical sampling. Groundwater feeds streams, so its composition also affects the water in the stream. Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1992, 1.4 km from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: vrt1992, 850 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: vrt1992, 850 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1993, 1.8 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: prameň1992, 1.9 km from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1992, 1.7 km from the water. Comparison: percentile 79 of all samples in Slovakia. Highest value: studňa1992, 1.7 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: prameň1992, 3.0 km from the water. Comparison: percentile 39 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. 52 boreholes in the 3 km zone, of which 23 hydrogeological and 29 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 Sigord 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 Sigord watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VN Sigord 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× Tectonic division
Neotectonic units
Direction of neotectonic movements
Regional geological division
Regional geological division (subunits)
Hydrogeology: aquifers and groundwater
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
70.4 mg/lpercentile 760.168 mg/lpercentile 7212.9 mg/lpercentile 653.10 mg/lpercentile 526.85 mg/lpercentile 4311.2 mg/lpercentile 3636.4 mg/lpercentile 24106 mg/lpercentile 20Nutrients and organic pollution
2.33 mg/lpercentile 280.0452 mg/lpercentile 251.74 mg/lpercentile 50.0257 mg/lpercentile 3Metals
31.5 μg/lpercentile 93415 μg/lpercentile 93196 μg/lpercentile 900.193 mg/lpercentile 74Elements in river sediments
Potentially toxic and trace elements
1.88 mg/kgpercentile 950.900 mg/kgpercentile 9217.3 mg/kgpercentile 88165 mg/kgpercentile 842.07 mg/kgpercentile 8390.3 mg/kgpercentile 833.66 mg/kgpercentile 770.315 mg/kgpercentile 7610.4 mg/kgpercentile 7516.9 mg/kgpercentile 5719.5 mg/kgpercentile 310.282 mg/kgpercentile 300.156 mg/kgpercentile 2656.9 mg/kgpercentile 2618.6 mg/kgpercentile 24Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
7.20 %percentile 896,310 mg/kgpercentile 893.83 %percentile 881,196 mg/kgpercentile 780.982 %percentile 700.982 %percentile 591.44 %percentile 391.65 %percentile 38662 mg/kgpercentile 25Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
74.6 mg/kgpercentile 8233.4 mg/kgpercentile 7730.6 mg/kgpercentile 561.44 mg/kgpercentile 5214.2 mg/kgpercentile 51128 mg/kgpercentile 42374 mg/kgpercentile 4082.1 mg/kgpercentile 33389 mg/kgpercentile 3249.9 mg/kgpercentile 18Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
3.07 ppm85th percentile8.84 ppm82th percentile1.29 %percentile 452,493 Bq/m²percentile 81Radon 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
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
Nearest samples with gold
Sample Gold in sample From the water 1056 3 grains 650 m 1077 3 grains 840 m Rock-forming and accessory minerals
Groundwater: chemistry, water types and radioactivity
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median water source for public supply 1 1,29 Bq/l 1.29 Bq/l mineral spring 1 7,09 Bq/l 7.09 Bq/l water source for individual supply 1 7,72 Bq/l 7.72 Bq/l source 1 5,66 Bq/l 5.66 Bq/l Mine workings, deposits and ore occurrences
Ore occurrences in the metallogenic map
Occurrence Ore type Metals Type From the water Šťavica Polymetallic ores Pb, Zn mineralogical occurrence 3.3 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Sigord negative borehole 155.0 m 83973 115Ba115.pdf80 m Sigord negative borehole 125.0 m 83973 115Ba116.pdf80 m Sigord narrow-diameter borehole with ordinary drinking and process water 20.0 m 83973 115Ba117.pdf150 m Sigord narrow-diameter borehole with ordinary drinking and process water 15.0 m 83973 115Ba118.pdf170 m Sigord narrow-diameter borehole with ordinary drinking and process water 20.0 m 83973 115Ba119.pdf230 m Sigord narrow-diameter borehole with ordinary drinking and process water 9.0 m 83973 115Ba121.pdf240 m J-12 engineering-geological 25.0 m 83973250 m Sigord narrow-diameter borehole with ordinary drinking and process water 23.0 m 83973 115Ba122.pdf330 m J-13 engineering-geological 20.0 m 83973340 m Sigord narrow-diameter borehole with ordinary drinking and process water 100.0 m 70619 115Ba81.pdf380 m Sigord narrow-diameter borehole with ordinary drinking and process water 25.0 m 83973 115Ba120.pdf390 m Sigord narrow-diameter borehole with ordinary drinking and process water 24.0 m 83973 115Ba123.pdf540 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 2.0 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Záborské – 1980 – 820 m Kokošovce 1 200 m² 1989 – 1.5 km Baňa – Klenov – 1990 – 1.7 km Bučinová stredná dolina – Kendice – 1985 – 1.9 km Piesková jama – Ruská Nová Ves 500 m² 1989 – 3.0 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
21from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
AntimonySbelevated (top 10 %)
highest 1.50 μg/lmedian 1.50 μg/l1 sample
ArsenicAsslightly elevated
highest 3.40 μg/lmedian 3.40 μg/l1 sample
CadmiumCdslightly elevated
highest 0.250 μg/lmedian 0.250 μg/l1 sample
CopperCubelow half of Slovakia
highest 1.20 μg/lmedian 1.20 μg/l1 sample
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l1 sample100 % below the limit of quantification
StrontiumSrbelow half of Slovakia
highest 150 μg/lmedian 150 μg/l1 sample
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
BariumBabelow half of Slovakia
highest 20.0 μg/lmedian 20.0 μg/l1 sample
Silicon dioxideSiO2elevated (top 10 %)
highest 32.8 mg/lmedian 32.8 mg/l1 sample
CopperCuextreme (top 1 %)
highest 34.2 μg/lmedian 1.48 μg/l10 samples
AluminiumAlextreme (top 1 %)
highest 1.44 mg/lmedian 0.00500 mg/l10 samples60 % below the limit of quantification
AntimonySbhigh (top 5 %)
highest 1.90 μg/lmedian 0.100 μg/l10 samples80 % below the limit of quantification
MercuryHghigh (top 5 %)
highest 0.300 μg/lmedian 0.100 μg/l10 samples90 % below the limit of quantification
ArsenicAshigh (top 5 %)
highest 5.80 μg/lmedian 0.950 μg/l10 samples50 % below the limit of quantification
LeadPbhigh (top 5 %)
highest 3.00 μg/lmedian 0.500 μg/l10 samples70 % below the limit of quantification
LithiumLielevated (top 10 %)
highest 39.0 μg/lmedian 6.50 μg/l10 samples10 % below the limit of quantification
ChromiumCrelevated (top 10 %)
highest 2.10 μg/lmedian 0.250 μg/l10 samples60 % below the limit of quantification
ZincZnslightly elevated
highest 213 μg/lmedian 54.5 μg/l10 samples10 % 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/l10 samples100 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification





