Fishing conditions score, the best window of the day and fishing districts from the best conditions High activity · average of one fishing district 15:00–17:00 VN Bolešov – Gilianka, window score 63. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 07:05. 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), 9 Nov 2026. The height is approximate (error of a few metres). 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 0 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 8.4modelled estimate water type Ca–Mg–HCO₃ Mineralisation 479 mg/l, hard water (16.2 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Selenium 0.398 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 77. Interpolation of the Geochemical Atlas of river sediments. 57nGy/h dose rate percentile 78 in Slovakia Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ. 1object within 3 km Nearest: Halda (spoil heap), 2.2 km from the water. 0samples with gold 9 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 10indicators in the top 5 % highest: Strontium 490 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 90 (Bolešov-Bolešovská dolina, 1000 m SZ od K438). 91boreholes within 3 km 101 water analyses nearby Of these, 91 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 4 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. 17records within 5 km 13 deposits, 4 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 11areas 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. 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 0 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 8.37typical 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. 16.2°dH, hard Sum of calcium and magnesium (2.89 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 479mg/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. 57nGy/h in air 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. -6nT range -6 to -6 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. -34mGal residual +2.0 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 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: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 80 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 77 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 48 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 43 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 37 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 34 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 32 of all samples in Slovakia. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K438, 950 m from the water. Comparison: percentile 26 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Bolešov-Bolešovská dolina, 1000 m SZ od K4381995, 950 m from the water. Comparison: percentile 30 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, 2.6 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: studňa1993, 570 m from the water. Comparison: percentile 86 of all samples in Slovakia. Highest value: vrt1993, 2.1 km from the water. Comparison: percentile 80 of all samples in Slovakia. Highest value: prameň1993, 2.1 km from the water. Comparison: percentile 76 of all samples in Slovakia. Highest value: studňa1993, 2.2 km from the water. Comparison: percentile 72 of all samples in Slovakia. Highest value: vrt1993, 2.4 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: studňa1993, 2.6 km from the water. Comparison: percentile 40 of all samples in Slovakia. Highest value: studňa1993, 2.6 km from the water. Comparison: percentile 39 of all samples in Slovakia. Highest value: studňa1993, 2.6 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. 91 boreholes in the 3 km zone, of which 13 hydrogeological and 78 other; with an archive report number 91. 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 Váh basin
By the water now
Today on the VN Bolešov – Gilianka 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 Bolešov – Gilianka watercourse
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the VN Bolešov – Gilianka stream
Water according to the atlas
Elements in river sediment
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
Neotectonic units
Direction of neotectonic movements
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Aquifer rocks (hydrogeological map 1:200,000)
Aquifer type
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
294 mg/lpercentile 7583.7 mg/lpercentile 7319.5 mg/lpercentile 6451.8 mg/lpercentile 636.46 mg/lpercentile 427.01 mg/lpercentile 402.15 mg/lpercentile 340.0602 mg/lpercentile 16Nutrients and organic pollution
5.98 mg/lpercentile 470.0810 mg/lpercentile 390.0790 mg/lpercentile 381.80 mg/lpercentile 15Metals
779 μg/lpercentile 9517.0 μg/lpercentile 8211.6 μg/lpercentile 250.0110 mg/lpercentile 2Elements in river sediments
Potentially toxic and trace elements
0.398 mg/kgpercentile 770.268 mg/kgpercentile 6628.1 mg/kgpercentile 659.06 mg/kgpercentile 6076.3 mg/kgpercentile 5616.6 mg/kgpercentile 5522.9 mg/kgpercentile 470.161 mg/kgpercentile 440.0716 mg/kgpercentile 305.13 mg/kgpercentile 2874.0 mg/kgpercentile 2356.4 mg/kgpercentile 201.93 mg/kgpercentile 180.166 mg/kgpercentile 110.229 mg/kgpercentile 4Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
7.46 %percentile 901.31 %percentile 213,632 mg/kgpercentile 19601 mg/kgpercentile 180.637 %percentile 18591 mg/kgpercentile 170.683 %percentile 162.02 %percentile 114.45 %percentile 11Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
74.1 mg/kgpercentile 82163 mg/kgpercentile 7129.0 mg/kgpercentile 47343 mg/kgpercentile 3074.8 mg/kgpercentile 1820.9 mg/kgpercentile 180.728 mg/kgpercentile 1548.5 mg/kgpercentile 15330 mg/kgpercentile 117.68 mg/kgpercentile 9Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.58 %percentile 888.20 ppm72th percentile2.67 ppm62th percentile1,160 Bq/m²percentile 28Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Relief, climate and soils
Geomorphological units
Geomorphological regions
Susceptibility of soils to acidification
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 3 12,1 Bq/l 11.5 Bq/l source 2 25,9 Bq/l 16.6 Bq/l water source for individual supply 1 8,32 Bq/l 8.32 Bq/l Mine workings, deposits and ore occurrences
Types of mining objects
Nearest old mine workings
Name Type Mined Ended From the water Spoil heap spoil heap limestone 2.2 km Deposits and mining areas
Deposit Mineral Status and organisation From the water Horné Srnie limestone, other Mined deposit – CEMMAC a.s. 1.9 km Horné Srnie sialitic raw material Mined deposit – CEMMAC a.s. 1.9 km Horné Srnie calcareous marl Mined deposit – CEMMAC a.s. 1.9 km Horné Srnie sialitic raw material Mined deposit – CEMMAC a.s. 1.9 km Horné Srnie limestone, other Mined deposit – CEMMAC a.s. 1.9 km Horné Srnie calcareous marl Mined deposit – CEMMAC a.s. 1.9 km Bolešov – Objekt 2 (odhadom – preskúmanosť) gravelly sands and sands Deposit with halted mining or where use of reserves is not expected – DARJA spol. s r.o. 3.3 km Dubnica n/Váhom – Pažite gravelly sands and sands Mined deposit – ÚTES spol. s r. o. 3.4 km Dubnica nad Váhom gravelly sands and sands Mined deposit – SLOVENSKÉ ŠTRKOPIESKY, s.r.o. 3.8 km Dubnica nad Váhom gravelly sands and sands Mined deposit – SLOVENSKÉ ŠTRKOPIESKY, s.r.o. 3.8 km Krivoklát limestone, other Deposit with expected use of reserves – ŠGÚDŠ Bratislava 4.1 km Krivoklát calcareous marl Deposit with expected use of reserves – ŠGÚDŠ Bratislava 4.1 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Bolešov narrow-diameter borehole with ordinary drinking and process water 20.0 m 33341 109Ab53.pdf670 m Bolešov narrow-diameter borehole with ordinary drinking and process water 15.0 m 33341 109Ab54.pdf780 m J-11 engineering-geological 6.0 m 741711.3 km J-10 engineering-geological 6.0 m 741711.3 km J-9 engineering-geological 3.0 m 741711.5 km J-142 engineering-geological 6.0 m 741711.5 km J-12 engineering-geological 3.0 m 741711.5 km J-16 engineering-geological 6.0 m 741711.5 km J-15 engineering-geological 6.0 m 741711.5 km J-17 engineering-geological 3.0 m 741711.6 km J-18 engineering-geological 3.0 m 741711.6 km J-14 engineering-geological 3.0 m 741711.6 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 4 4.4 km Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landfill Area Year established Monitoring From the water Bolešov – Pri trati – Bolešov – 1975 – 1.7 km Slávnica – Nad Podhorím – Slavnica 500 m² 1975 – 2.0 km Bolešov – Za ihriskom – Bolešov – 1975 – 2.7 km Sedmerovec – Járok – Sedmerovec – 1975 – 2.9 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
61from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
StrontiumSrelevated (top 10 %)
highest 490 μg/lmedian 490 μg/l1 sample
BariumBaslightly elevated
highest 74.0 μg/lmedian 74.0 μg/l1 sample
CopperCuslightly elevated
highest 2.70 μg/lmedian 2.70 μg/l1 sample
ArsenicAsbelow half of Slovakia
highest 0.840 μg/lmedian 0.840 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
AntimonySbbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 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
Silicon dioxideSiO2below half of Slovakia
highest 7.52 mg/lmedian 7.52 mg/l1 sample
MercuryHghigh (top 5 %)
highest 0.300 μg/lmedian 0.100 μg/l8 samples88 % below the limit of quantification
CopperCuhigh (top 5 %)
highest 6.90 μg/lmedian 2.05 μg/l8 samples
CadmiumCdhigh (top 5 %)
highest 0.500 μg/lmedian 0.250 μg/l8 samples88 % below the limit of quantification
LeadPbelevated (top 10 %)
highest 2.00 μg/lmedian 1.00 μg/l8 samples38 % below the limit of quantification
ZincZnslightly elevated
highest 387 μg/lmedian 41.0 μg/l8 samples
AluminiumAlslightly elevated
highest 0.0200 mg/lmedian 0.00500 mg/l8 samples63 % below the limit of quantification
LithiumLislightly elevated
highest 17.0 μg/lmedian 8.50 μg/l8 samples
ChromiumCrtypical value
highest 0.700 μg/lmedian 0.250 μg/l8 samples63 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l5 samples100 % below the limit of quantification
AntimonySbbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l8 samples100 % below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l8 samples100 % below the limit of quantification
ArsenicAsbelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l8 samples100 % below the limit of quantification

