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 Podkylavka – Prašník, window score 43. 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. How the watercourse falls downstream: fall, gradient and water speed. Fast watercourse Podhorský potok: fast water, stony bottom, riffles and the pools below them. Typical trout waters. 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 (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. Young sediments100% of the water line Young unconsolidated sediments; fine material easily washes into the stream during rain. Geological Map of Slovakia 1:50,000. pH 8.2modelled estimate water type Ca–Mg–HCO₃ Mineralisation 633 mg/l, very hard water (22.2 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 1 from 15elements in the top 10 % highest: Antimony 6.19 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. 35°C at 1,000 m depth At a depth of 2,000 m about 65 °C (increase of 30 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 61nGy/h dose rate percentile 88 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. 2 from 10indicators in the top 5 % highest: Selenium 2.67 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (Holeška, potok). 22boreholes within 3 km 273 water analyses nearby Of these, 22 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – No geothermal borehole or spring is recorded within 10 km. 14sites within 3 km 14 landfills No environmental burden is registered within 3 km; landfills are only recorded. 30records within 5 km 8 deposits, 22 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 5areas 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 Young sediments: Young unconsolidated sediments; fine material easily washes into the stream during rain. 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 1 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 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 8.18typical 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. 22.2°dH, very hard Sum of calcium and magnesium (3.96 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 633mg/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 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. 61nGy/h in air range 60 to 63 nGy/h Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains. medium 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. +14nT range 11 to 15 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 +22.6 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. 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 –. 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 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: Holeška, potok2002, 660 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: potok – ľavostranný prítok Pokylavského p.1999, 340 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: Prašník – Boorovci, potok 1800 m SZ od k-2472004, 60 m from the water. Comparison: percentile 94 of all samples in Slovakia. Highest value: potok – ľavostranný prítok Pokylavského p.1999, 340 m from the water. Comparison: percentile 86 of all samples in Slovakia. Highest value: Holeška, potok2002, 660 m from the water. Comparison: percentile 83 of all samples in Slovakia. Highest value: Podkylavský, potok1999, 30 m from the water. Comparison: percentile 82 of all samples in Slovakia. Highest value: Holeška, potok, 660 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: potok – ľavostranný prítok Pokylavského p.1999, 340 m from the water. Comparison: percentile 71 of all samples in Slovakia. Highest value: Prašník – Boorovci, potok 1800 m SZ od k-2472004, 60 m from the water. Comparison: percentile 63 of all samples in Slovakia. Highest value: Holeška, potok1999, 360 m from the water. Comparison: percentile 43 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: potok – ľavostranný prítok Pokylavského p.1999, 340 m from the water. Comparison: percentile 76 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, 2.8 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1992, 1.1 km from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: studňa1993, 2.7 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1992, 1.1 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: prameň1992, 720 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1993, 1.6 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1993, 2.4 km from the water. Comparison: percentile 89 of all samples in Slovakia. Highest value: prameň1992, 720 m from the water. Comparison: percentile 87 of all samples in Slovakia. Highest value: studňa1993, 2.0 km from the water. Comparison: percentile 85 of all samples in Slovakia. Highest value: studňa1993, 3.0 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: vrt1993, 2.7 km from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: vrt1993, 2.7 km from the water. Comparison: percentile 38 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. 22 boreholes in the 3 km zone, of which 17 hydrogeological and 5 other; with an archive report number 22. 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 Váh basin
By the water now
Today on the Podkylavka – Prašník 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 Podkylavka – Prašník watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the Podkylavka – Prašník 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 Pleistocene – Holocene deluvial sediments: predominantly loamy-stoney (subordinate sandy-stone) slopes and rubble 1× Quaternary cover
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
Main hydrogeological region
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
381 mg/lpercentile 90105 mg/lpercentile 9032.5 mg/lpercentile 8767.5 mg/lpercentile 7419.9 mg/lpercentile 697.76 mg/lpercentile 440.0799 mg/lpercentile 301.88 mg/lpercentile 29Nutrients and organic pollution
17.0 mg/lpercentile 890.0810 mg/lpercentile 390.0794 mg/lpercentile 392.45 mg/lpercentile 31Metals
0.219 mg/lpercentile 7779.9 μg/lpercentile 5536.5 μg/lpercentile 546.31 μg/lpercentile 47Elements in river sediments
Potentially toxic and trace elements
6.19 mg/kgpercentile 91106 mg/kgpercentile 8436.3 mg/kgpercentile 840.263 mg/kgpercentile 650.446 mg/kgpercentile 628.67 mg/kgpercentile 536.65 mg/kgpercentile 500.233 mg/kgpercentile 4764.0 mg/kgpercentile 402.36 mg/kgpercentile 3883.5 mg/kgpercentile 350.0763 mg/kgpercentile 3412.0 mg/kgpercentile 2718.6 mg/kgpercentile 260.0663 mg/kgpercentile 12Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1.80 %percentile 853.18 %percentile 68883 mg/kgpercentile 550.891 %percentile 504,334 mg/kgpercentile 454.98 %percentile 262.24 %percentile 220.714 %percentile 20578 mg/kgpercentile 15Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
82.4 mg/kgpercentile 9093.5 mg/kgpercentile 6315.3 mg/kgpercentile 6159.2 mg/kgpercentile 50376 mg/kgpercentile 4027.5 mg/kgpercentile 38123 mg/kgpercentile 3822.7 mg/kgpercentile 240.919 mg/kgpercentile 23363 mg/kgpercentile 22Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.65 %percentile 909.29 ppm88th percentile2.80 ppm73th percentile1,349 Bq/m²percentile 41Radon risk by isopleths
Geophysical 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
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 well 7 25,2 Bq/l 11.7 Bq/l source 3 30,5 Bq/l 28.1 Bq/l developed spring 2 44,2 Bq/l 28.0 Bq/l Mine workings, deposits and ore occurrences
Deposits and mining areas
Deposit Mineral Status and organisation From the water Prašník building stone Deposit with halted mining or where use of reserves is not expected – LOMtrans, s.r.o. 3.7 km Prašník building stone Deposit with halted mining or where use of reserves is not expected – LOMtrans, s.r.o. 3.7 km Vrbové building stone Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 3.8 km Vrbové building stone Deposit with halted mining or where use of reserves is not expected – Organizácia neurčená 3.8 km Košariská dolomite Deposit with expected use of reserves – Organizácia neurčená 4.3 km Košariská dolomite Deposit with expected use of reserves – ŠGÚDŠ Bratislava 4.3 km Košariská dolomite Deposit with expected use of reserves – ŠGÚDŠ Bratislava 4.4 km Košariská dolomite Deposit with expected use of reserves – Organizácia neurčená 4.4 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Prašník monitoring borehole 8.0 m 74931 132Ab30.pdf170 m Prašník monitoring borehole 7.5 m 74931 132Ab31.pdf250 m Podkulava narrow-diameter borehole with ordinary drinking and process water 22.0 m 82456 120Cd13.pdf260 m Prašník – Pustá Ves narrow-diameter borehole with ordinary drinking and process water 9.0 m 55362 132Ab20.pdf280 m Prašník monitoring borehole 7.5 m 74931 132Ab34.pdf480 m Prašník monitoring borehole 7.5 m 74931 132Ab33.pdf480 m Prašník monitoring borehole 7.5 m 74931 132Ab32.pdf500 m Prašník monitoring borehole 8.0 m 74931 132Ab35.pdf620 m Krajné-Podkylava narrow-diameter borehole with ordinary drinking and process water 9.2 m 74054 120Cd10.pdf860 m V-1 engineering-geological 9.0 m 844851.2 km Trenčín-Krajné narrow-diameter borehole with ordinary drinking and process water 8.0 m 64740 120Cd8.pdf1.2 km KV-2 engineering-geological 5.0 m 868191.9 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Prašník 1 000 m² 1980 – 80 m Prašník 5 000 m² 1970 – 630 m Podkylava – Krížne cesty – Krajné 5 685 m² 1972 monitored 740 m Prašník 1 500 m² 1970 – 860 m Prašník 1 500 m² 1980 – 1.1 km Prašník 12 000 m² 1992 – 1.1 km Prašník 250 m² 1990 – 1.1 km Dobrovodský Mlyn – Prašník 2 000 m² 1970 – 1.2 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
33from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
SeleniumSeextreme (top 1 %)
highest 2.67 μg/lmedian 0.500 μg/l6 samples83 % below the limit of quantification
CopperCuhigh (top 5 %)
highest 8.60 μg/lmedian 6.50 μg/l6 samples17 % below the limit of quantification
StrontiumSrelevated (top 10 %)
highest 597 μg/lmedian 594 μg/l2 samples
LithiumLislightly elevated
highest 23.0 μg/lmedian 5.00 μg/l6 samples67 % below the limit of quantification
ChromiumCrslightly elevated
highest 3.40 μg/lmedian 1.00 μg/l6 samples83 % below the limit of quantification
AntimonySbslightly elevated
highest 1.00 μg/lmedian 0.500 μg/l6 samples83 % below the limit of quantification
CadmiumCdslightly elevated
highest 0.250 μg/lmedian 0.150 μg/l6 samples83 % below the limit of quantification
BariumBatypical value
highest 60.0 μg/lmedian 54.5 μg/l4 samples
ArsenicAstypical value
highest 1.53 μg/lmedian 0.855 μg/l6 samples33 % below the limit of quantification
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l6 samples100 % below the limit of quantification
Silicon dioxideSiO2slightly elevated
highest 19.1 mg/lmedian 11.5 mg/l6 samples
CopperCuextreme (top 1 %)
highest 70.0 μg/lmedian 0.750 μg/l22 samples
ZincZnhigh (top 5 %)
highest 2,210 μg/lmedian 115 μg/l22 samples
LithiumLihigh (top 5 %)
highest 69.0 μg/lmedian 15.5 μg/l22 samples
SeleniumSehigh (top 5 %)
highest 2.90 μg/lmedian 0.500 μg/l22 samples77 % below the limit of quantification
CadmiumCdhigh (top 5 %)
highest 0.600 μg/lmedian 0.250 μg/l22 samples86 % below the limit of quantification
LeadPbelevated (top 10 %)
highest 2.00 μg/lmedian 0.500 μg/l22 samples64 % below the limit of quantification
ChromiumCrslightly elevated
highest 1.90 μg/lmedian 0.250 μg/l22 samples55 % below the limit of quantification
AntimonySbslightly elevated
highest 0.300 μg/lmedian 0.100 μg/l22 samples91 % below the limit of quantification
AluminiumAlslightly elevated
highest 0.0300 mg/lmedian 0.00500 mg/l22 samples59 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l8 samples100 % below the limit of quantification
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l22 samples100 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l22 samples100 % below the limit of quantification




