On the Porubský potok (Dubnica) je jeden rybársky revír. stream Porubský potok (Dubnica) is salmonid (trout) fishing district no. 3-2930-4-1. It lies in Ilava district (Trenčín Region). The fishing district is 11.7 km long. The fishing district is managed by City SRZ organization Dubnica nad Váhom Fishing rules, permits, the map and conditions at the water are on the fishing district's page. It belongs to the Váh river basin. Open fishing district Porubský potok (Dubnica) Game fish of the fishing district (1): High activity · average of one fishing district 15:00–17:00 Porubský potok (Dubnica), window score 76. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 16:23. 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. Model celej rieky sa práve počíta z leteckého skenovania terénu: hotových je 9 % výšok. Trvá to niekoľko minút, potom obnov stránku. Loading the 3D model… From the start 0 kmWater surface elevation –Fishing district The strip of terrain follows the watercourse and is widened and vertically exaggerated for readability. The color of the water is the fishing district type: gold for carp, blue for trout, violet for grayling. Elevations come from airborne laser scanning (DMR 5.0, ÚGKK SR). 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. How the watercourse falls downstream: fall, gradient and water speed. Torrent A mountain stream with a steep gradient, cascades and a rocky bottom. The water is clear and cold; fishing requires a careful approach. 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. 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 (12 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 alluvium50% of the water line 50% limestones and dolomites Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000. pH 8.3modeled estimate water type Ca–HCO₃ Mineralization 446 mg/l, hard water (15.5 °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 39.7 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 89. Interpolation of the Geochemical Atlas of river sediments. 25°C at 1,000 m depth heat flow 61 mW/m² At a depth of 2,000 m about 55 °C (increase of 30 °C per kilometer). 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 13 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. 4 from 10indicators in the top 5% highest: Chromium 13.0 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (Košeca, 650 m S od K442). 162boreholes within 3 km 457 water analyzes nearby Of these, 162 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. 21°C at the wellhead 4 geothermal boreholes within 10 km Warmest: Belušské Slatiny – BS-1, 8.1 km from the water. 2sites within 3 km 2 landfills No environmental burden is registered within 3 km; landfills are only recorded. 15records within 5 km 7 deposits, 8 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 15areas within 3 km 1 active Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed. 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 center. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. 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 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 2 of 5 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 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 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 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. -19nT range -30 to -13 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. -29mGal residual +5.5 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. Modeled 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 8.34typical 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. 15.5°dH, hard Sum of calcium and magnesium (2.77 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 446mg/l mineralization 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) 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: Košeca, 650 m S od K4421995, 860 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: Horná Poruba, 700 m JZ od K5241995, 70 m from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: Košeca, 650 m S od K4421995, 860 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: Košeca, 650 m S od K4421995, 860 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: Horná Poruba, 700 m JZ od K524, 70 m from the water. Comparison: percentile 94 of all samples in Slovakia. Highest value: Ilava-Plancie, 750 m VSV od K5171995, 100 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: Horná Poruba, 700 m JZ od K5241995, 70 m from the water. Comparison: percentile 85 of all samples in Slovakia. Highest value: Nosický, kanál, 340 m from the water. Comparison: percentile 76 of all samples in Slovakia. Highest value: Horná Poruba, 1, 5 km ZJZ od K956 Vapec1995, 80 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Horná Poruba, 1, 5 km ZJZ od K956 Vapec1995, 80 m from the water. Comparison: percentile 34 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Nosický, kanál, 340 m from the water. Comparison: percentile 9 of all samples in Slovakia. 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) Hydrogeochemical objects (analyzes of springs and boreholes) and the geochemical atlas of groundwater (1996). Groundwater feeds streams, so its composition also affects the water in the stream. Highest value: studňa1993, 2.9 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: vrt1993, 2.9 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1993, 60 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: prameň1992, 2.2 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: prameň1993, 410 m from the water. Comparison: percentile 94 of all samples in Slovakia. Highest value: studňa1993, 2.6 km from the water. Comparison: percentile 92 of all samples in Slovakia. Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 88 of all samples in Slovakia. Highest value: studňa1993, 1.8 km from the water. Comparison: percentile 86 of all samples in Slovakia. Highest value: vrt1993, 2.2 km from the water. Comparison: percentile 83 of all samples in Slovakia. Highest value: prameň1993, 2.2 km from the water. Comparison: percentile 50 of all samples in Slovakia. Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 47 of all samples in Slovakia. Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 39 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. 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. 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. 25 / 55 °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 61 mW/m². marker on the bar: share among all sample points on streams in Slovakia 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. Register of hydrogeological boreholes, other boreholes and geothermal boreholes. Each borehole has a report in the Geofond archive (geological profiles, pumping tests, chemical analyzes of the water); the report number is in the table. 162 boreholes in the 3 km zone, of which 49 hydrogeological and 113 other; with an archive report number 162. 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 range 47 to 56 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 Radiohydrochemical sampling of springs, wells and watercourses: radon activity concentration in water. The bar shows the highest measured value for each kind of site. 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.
By the water now
The Porubský potok (Dubnica) watercourse at a glance
Today on the Porubský potok (Dubnica) watercourse
Is it worth going today? Fishing conditions score, the best window of the day and fishing districts from the best conditionsConditions score73 / 100Best window15:00Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the Porubský potok watercourse (Dubnica)
The course of the watercourse and its fishing districts. You can switch the line color to today's conditions, quality or any other parameter.Fishing districts1Length11,7 kmThe stream Porubský potok (Dubnica) in 3D
The terrain along the watercourse from its highest point to its lowest, with fishing districts and a flight downstreamDrop440 mTerrain sections48Fish and catches on the Porubský potok watercourse (Dubnica)
Which fish live here and what has been caught? Game species recorded in the fishing districts and approved catches by anglersGame species1Game species recorded in the fishing district
Organizations and districts on the Porubský potok watercourse (Dubnica)
Who manages the fishing districts and where they areOrganizations1Districts1Organizations on the watercoursewho manages the fishing districts and what the conditions are there today
Water pollution on the Porubský potok (Dubnica) watercourse
Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearbyFishing districts failing a standard0 / 1Groundwater: measured valuestypical value from stations within 10 km, 2025
Watercourse profile from source to mouthnumber of unmet indicators in 2025 at SHMÚ sites
Show sites in the table (3)
Terrain and satellite images of the Porubský potok watercourse (Dubnica)
Elevation profile, 3D terrain of the surroundings and historical satellite imagesHighest point616 m n. m.Lowest point235 m n. m.Elevation profile of the watercourse
Terrain in 3D
Historical images
More watercourses near the Porubský potok watercourse (Dubnica)
The nearest rivers, streams and water bodies in the same river basinWatercourses6Prejtiansky potok
1 fishing district
Salmonid (trout)Podhradský potok
1 fishing districtPodhorský potok
1 fishing districtRybník Prejta – Vystrkov č. 1,2,3
1 fishing district
CarpNosický kanál
1 fishing district
Salmonid (trout)Dubnický potok
1 fishing districtGeology and geochemistry of the Porubský potok (Dubnica) stream
Geology at a glance and a map of the zone
What lies beneath the water and around it? An overview in tiles, a map of mine workings, deposits, environmental burdens, boreholes and gold finds, and how to read the dataRock 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 analyzes
Geothermal energy
Environmental burdens and landfills
Deposits and ore occurrences
Landslides and slope deformations
Map of the corridor
How to read these data
Rocks, groundwater and landscape
What does the water flow over? Geological structure and age of the rocks, groundwater aquifers, relief, climate, soils and geophysical fieldsGeological 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× Cretaceous older – Late Cretaceous Poruba Formation 1× Quaternary cover
Tectonic units
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
Aquifer rocks (hydrogeological map 1:200,000)
Aquifer type
Main hydrogeological region
Genetic type of groundwater
Chemical type of groundwater
Groundwater quality class
Geothermal groundwater bodies
Relief, climate and soils
Geomorphological units
Geomorphological regions
Climatic-geographical types
Susceptibility of soils to acidification
Soil contamination (map 1:500,000)
Lithogeochemical types
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Chemistry of water and river sediments
What is in the water and on the bed? Trace elements and metals, nutrients, major ions, elements in sediments and groundwaterSurface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
288 mg/lpercentile 7383.7 mg/lpercentile 730.172 mg/lpercentile 7316.7 mg/lpercentile 5534.8 mg/lpercentile 422.08 mg/lpercentile 334.16 mg/lpercentile 284.55 mg/lpercentile 24Nutrients and organic pollution
0.0658 mg/lpercentile 340.0637 mg/lpercentile 324.14 mg/lpercentile 292.10 mg/lpercentile 22Metals
205 μg/lpercentile 8011.3 μg/lpercentile 6911.0 μg/lpercentile 230.0342 mg/lpercentile 13Trace elements in surface waters
Major ions, mineralization and pH
Elements in river sediments
Potentially toxic and trace elements
39.7 mg/kgpercentile 89156 mg/kgpercentile 820.405 mg/kgpercentile 7830.2 mg/kgpercentile 719.79 mg/kgpercentile 698.16 mg/kgpercentile 660.254 mg/kgpercentile 6317.9 mg/kgpercentile 6276.2 mg/kgpercentile 560.0984 mg/kgpercentile 482.54 mg/kgpercentile 450.145 mg/kgpercentile 3961.4 mg/kgpercentile 330.437 mg/kgpercentile 280.204 mg/kgpercentile 16Major elements (iron, aluminum, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
8.64 %percentile 931.43 %percentile 79811 mg/kgpercentile 461.45 %percentile 40676 mg/kgpercentile 292.30 %percentile 274.69 %percentile 160.663 %percentile 143,357 mg/kgpercentile 12Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
76.9 mg/kgpercentile 85163 mg/kgpercentile 7127.5 mg/kgpercentile 3876.9 mg/kgpercentile 229.34 mg/kgpercentile 1619.0 mg/kgpercentile 130.649 mg/kgpercentile 1246.5 mg/kgpercentile 12241 mg/kgpercentile 12318 mg/kgpercentile 8Groundwater: chemistry and water types
Chemical water types nearby
Water quality class according to the hydrogeochemical map
Metals in groundwater
Gold, mines and deposits
Was gold panned and ore mined here? Gold and ore minerals in river sediments, old mine workings, deposits and ore occurrencesGold and ore minerals in river sediments
Rock-forming and accessory minerals
Mine workings, deposits and ore occurrences
Deposits and mining areas
Geothermal energy, mineral waters and boreholes
Is there heat underground? Geothermal potential, geothermal boreholes by temperature, mineral springs and the borehole archiveHottest borehole21 °CBoreholes162Geothermal potential
Rock temperature with depth
Geothermal groundwater bodies beneath the water line
Geothermal energy and mineral waters
Geothermal boreholes by water temperature
Sources of geothermal and mineral waters
Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Natural radioactivity and radon
How much does the ground radiate here? Gamma radiation of rocks, radon in soil and radon in watersNatural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.55 %percentile 867.54 ppm57th percentile2.40 ppm28th percentile1,265 Bq/m²percentile 35Radon risk by isopleths
Radon in waters
Environmental burdens, landfills and landslides
What in the surroundings can harm the water? Environmental burdens, waste landfills, anthropogenic sediments and slope deformationsBurdens and landfills2Landslides15Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landslides and slope deformations
Types of deformations
Degree of activity
Current state
73from 100
1445fishing districts
Map color
Loading map…
lowerhigher
Najvyššie
Najnižšie
Cations (positive ions)
Anions (negative ions)
ChromiumCrhigh (top 5%)
highest 13.0 μg/lmedian 7.00 μg/l7 samples
BariumBahigh (top 5%)
highest 250 μg/lmedian 93.0 μg/l6 samples
LeadPbhigh (top 5%)
highest 7.00 μg/lmedian 3.00 μg/l7 samples29% below the limit of quantification
StrontiumSrhigh (top 5%)
highest 750 μg/lmedian 470 μg/l7 samples
CadmiumCdelevated (top 10%)
highest 0.700 μg/lmedian 0.600 μg/l7 samples43% below the limit of quantification
ArsenicAselevated (top 10%)
highest 4.50 μg/lmedian 2.32 μg/l7 samples
AntimonySbslightly elevated
highest 1.20 μg/lmedian 0.820 μg/l7 samples
CopperCuslightly elevated
highest 2.50 μg/lmedian 1.50 μg/l7 samples14% below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l7 samples100% below the limit of quantification
LithiumLibelow half of Slovakia
highest 5.00 μg/lmedian 5.00 μg/l7 samples100% below the limit of quantification
Silicon dioxideSiO2below half of Slovakia
highest 4.03 mg/lmedian 1.41 mg/l7 samples
CopperCuextreme (top 1%)
highest 19.2 μg/lmedian 0.900 μg/l35 samples
ZincZnhigh (top 5%)
highest 1,880 μg/lmedian 9.00 μg/l35 samples20% below the limit of quantification
LeadPbhigh (top 5%)
highest 4.00 μg/lmedian 0.500 μg/l35 samples60% below the limit of quantification
MercuryHghigh (top 5%)
highest 0.200 μg/lmedian 0.100 μg/l35 samples94% below the limit of quantification
AluminumAlelevated (top 10%)
highest 0.0700 mg/lmedian 0.00500 mg/l35 samples54% below the limit of quantification
AntimonySbelevated (top 10%)
highest 0.500 μg/lmedian 0.100 μg/l35 samples94% below the limit of quantification
LithiumLislightly elevated
highest 31.0 μg/lmedian 6.00 μg/l35 samples
ArsenicAsslightly elevated
highest 1.70 μg/lmedian 0.500 μg/l35 samples97% below the limit of quantification
ChromiumCrslightly elevated
highest 1.40 μg/lmedian 0.250 μg/l35 samples69% below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l12 samples100% below the limit of quantification
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l35 samples100% below the limit of quantification
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l35 samples100% below the limit of quantification
Ilava
910 m
Ilava
940 m
Pruské – Kúty
1.2 km
Prejta
2.6 km
Bolešov – Objekt 2 (odhadom – preskúmanosť)
4.1 km
Tunežice
4.4 km
Tunežice
4.4 km
Belušské Slatiny – BS-1
21 °C
Belušské Slatiny – BHS-1
21 °C
Belušské Slatiny – BHS-3
21 °C
Belušské Slatiny – BHS-2
20 °C
category b2
7.3 km
category b1
7.3 km
category a1
7.7 km
category d2
9.8 km
category d1
10 km
V-1
50 m
V-1
50 m
VM-37/4
60 m
V-2
70 m
V-2
70 m
VM-37/5
80 m
VM-37/6
80 m
V-4
90 m
V-3
100 m
VT-37/3
100 m
VT-37/4
120 m
Ilava
140 m
Košecké Podhradie – Nad časťou Kopec – Veľké Košecké Podhradie
2.5 km
Košecké Podhradie – Za obcou – Veľké Košecké Podhradie
3.0 km