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 OR Žlutnica, window score 27. 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. How the watercourse falls downstream: fall, gradient and water speed. Very slow watercourse A lowland, almost stagnant section: calm, often more turbid water; the bottom tends to be muddy and sandy. Typical of carp fishing districts. 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 2017 to 2023: 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 8.3modelled estimate water type Ca–HCO₃–SO₄ Mineralisation 558 mg/l, hard water (17.8 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 1 from 15elements in the top 10 % highest: Copper 63.4 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 92. Interpolation of the Geochemical Atlas of river sediments. 35°C at 1,000 m depth heat flow 50 mW/m² At a depth of 2,000 m about 65 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 47nGy/h dose rate percentile 22 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 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. – There is no measurement in the surface water atlas samples within 1 km of the water. 29boreholes within 3 km 25 water analyses nearby Of these, 29 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 2 geothermal and mineral water springs within 10 km. 4sites within 3 km 4 landfills No environmental burden is registered within 3 km; landfills are only recorded. 0records within 5 km Geofond registers, the metallogenetic map and the mineral resources map. 0areas within 3 km Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed. 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 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. 17.8°dH, hard Sum of calcium and magnesium (3.17 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 558mg/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–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. 47nGy/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. +95nT range 95 to 95 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. 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. 35 / 65 °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 50 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 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. 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, 1.8 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 87 of all samples in Slovakia. Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 81 of all samples in Slovakia. Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 66 of all samples in Slovakia. Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 39 of all samples in Slovakia. Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 38 of all samples in Slovakia. Highest value: studňa1993, 2.1 km from the water. Comparison: percentile 30 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. 29 boreholes in the 3 km zone, of which 14 hydrogeological and 15 other; with an archive report number 29. 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. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. Who manages the fishing districts and where they are Danube basin
By the water now
Today on the OR Žlutnica watercourse
Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the watercourse
Elevation profile of the watercourse
Terrain in 3D
Historical images



Water pollution on the OR Žlutnica watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the OR Žlutnica 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
Hydrogeology: aquifers and groundwater
Main hydrogeological region
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
9.47 mg/lpercentile 9128.0 mg/lpercentile 8889.8 mg/lpercentile 8691.2 mg/lpercentile 8129.8 mg/lpercentile 8021.9 mg/lpercentile 71277 mg/lpercentile 700.123 mg/lpercentile 54Nutrients and organic pollution
0.382 mg/lpercentile 820.421 mg/lpercentile 764.42 mg/lpercentile 7410.1 mg/lpercentile 73Metals
25.0 μg/lpercentile 9140.6 μg/lpercentile 5733.2 μg/lpercentile 320.0552 mg/lpercentile 25Elements in river sediments
Potentially toxic and trace elements
63.4 mg/kgpercentile 920.441 mg/kgpercentile 83101 mg/kgpercentile 820.169 mg/kgpercentile 70119 mg/kgpercentile 680.318 mg/kgpercentile 669.37 mg/kgpercentile 6426.6 mg/kgpercentile 596.97 mg/kgpercentile 540.213 mg/kgpercentile 480.324 mg/kgpercentile 3961.5 mg/kgpercentile 3310.9 mg/kgpercentile 191.69 mg/kgpercentile 100.255 mg/kgpercentile 6Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1,207 mg/kgpercentile 843.71 %percentile 721.63 %percentile 67829 mg/kgpercentile 482.52 %percentile 404,182 mg/kgpercentile 395.28 %percentile 380.716 %percentile 280.707 %percentile 19Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
495 mg/kgpercentile 7817.3 mg/kgpercentile 7764.8 mg/kgpercentile 6894.1 mg/kgpercentile 65144 mg/kgpercentile 5629.9 mg/kgpercentile 52415 mg/kgpercentile 4225.6 mg/kgpercentile 381.07 mg/kgpercentile 3153.3 mg/kgpercentile 30Natural radioactivity and radon
Gamma radiation dose rate
1.28 %percentile 406.85 ppm28th percentile2.22 ppm16th percentileGeophysical fields: magnetics and gravity
Magnetic anomaly
Geothermal potential
Rock temperature with depth
Relief, climate and soils
Susceptibility of soils to acidification
Map of the corridor
Groundwater: chemistry, water types and radioactivity
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median well 1 13,2 Bq/l 13.2 Bq/l Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water P-1 hydrogeological 6.0 m 164901.3 km Holíč narrow-diameter borehole with ordinary drinking and process water 8.8 m 17458 119Ad20.pdf1.5 km Holíč narrow-diameter borehole with ordinary drinking and process water 9.5 m 17458 119Ad21.pdf1.8 km Holíč narrow-diameter borehole with ordinary drinking and process water 7.7 m 17458 119Cb6.pdf2.4 km JV-8 engineering-geological 10.0 m 845702.4 km Skalica narrow-diameter borehole with ordinary drinking and process water 9.0 m 16490 119Ad12.pdf2.4 km HV-8 hydrogeological 9.0 m 164902.5 km S-2 hydrogeological 8.0 m 64802.5 km Holíč narrow-diameter borehole with ordinary drinking and process water 9.0 m 17458 119Cb5.pdf2.6 km V-1 engineering-geological 9.0 m 979532.7 km V-2 engineering-geological 6.0 m 979532.7 km Skalica narrow-diameter borehole with ordinary drinking and process water 12.0 m 16490 119Ad8.pdf2.7 km 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 2 7.1 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Kátov 2 400 m² 1975 – 1.8 km Skalica 15 000 m² 1960 – 2.0 km Skalica 55 000 m² 1976 – 2.5 km Skalica 4 800 m² 1972 – 2.6 km 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
28from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
CopperCuextreme (top 1 %)
highest 91.0 μg/lmedian 47.7 μg/l2 samples
LithiumLihigh (top 5 %)
highest 90.0 μg/lmedian 49.0 μg/l2 samples
MercuryHghigh (top 5 %)
highest 0.300 μg/lmedian 0.250 μg/l2 samples
LeadPbelevated (top 10 %)
highest 2.00 μg/lmedian 1.50 μg/l2 samples
AntimonySbslightly elevated
highest 0.300 μg/lmedian 0.200 μg/l2 samples50 % below the limit of quantification
ZincZnslightly elevated
highest 272 μg/lmedian 185 μg/l2 samples
ChromiumCrtypical value
highest 0.500 μg/lmedian 0.375 μg/l2 samples50 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l2 samples100 % below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l2 samples100 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l2 samples100 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l2 samples100 % below the limit of quantification
AluminiumAlbelow half of Slovakia
highest 0.00500 mg/lmedian 0.00500 mg/l2 samples100 % below the limit of quantification



