Fishing conditions score, the best window of the day and fishing districts from the best conditions
Average of the watercourse's fishing districts
39from 100
Average activity · average of one fishing district
The number in the header is an estimate for the middle of the watercourse based on weather and measurements. The average of the fishing districts also counts satellite data, shading and geology of each district.
Best window today
15:00–17:00
Železný potok, window score 46.
The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 14:04.
Map and fishing districts of the watercourse
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
1445fishing districts
Pick a category to narrow the selection. Next to each option you can see how many fishing districts remain.
Map color
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Move the map with two fingers. In full-screen mode one finger is enough.
CarpSalmonid (trout)Salmonid (grayling)
lowerhigher
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.
Elevation profile of the watercourse
How the watercourse falls downstream: fall, gradient and water speed.
TorrentA mountain stream with a steep gradient, cascades and a rocky bottom. The water is clear and cold; fishing requires a careful approach.
Elevation profile of the watercourse: from 1,001 to 533 m a.s.l. over 13.3 km.Fishing districts in order from the highest (left) to the lowest. There may be a section without a fishing district between districts; it is not displayed.
Highest point
1,001 m a.s.l.
Lowest point
506 m a.s.l.
Fall of the fishing districtsFallThe difference in altitude between the upper and lower end of the fishing district in metres. The greater the fall over a shorter length, the faster the water.
495 m
Average slopeWatercourse gradientFall per kilometre in per mille (‰, metres per kilometre). Up to 2 ‰ is a slow lowland river, 5 to 10 ‰ a foothill river (grayling, trout), above 10 ‰ a fast stream.
37 ‰
SinuositySinuosityThe length of the watercourse divided by the straight-line distance between its ends. 1.0 is a straight watercourse; above 1.3 it meanders strongly. Meanders create pools under the banks and shallows in the reaches between.
1.21
Source: Open Topo Data (eudem25m), 4 Nov 2026. Gradient and fall are approximate and include only the sections of fishing districts.
Terrain in 3D
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Historical images
Changes in the surroundings and nature from 2019 to 2025: how the banks, vegetation and landscape around the water change. The images switch automatically; you can also browse them by hand.
2019imaged 30 Jun 20192022imaged 17 Oct 20222025imaged 22 Jun 2025
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.
Geology and geochemistry of the Železný potok stream
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 (13 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.
Rock under the water
Sandstones and conglomerates75% of the water line
25% river alluvium
Moderately mineralised water, depending on the share of carbonates. Geological Map of Slovakia 1:50,000.
Water according to the atlas
pH 8.1modelled estimate
water type Ca–Mg–HCO₃–SO₄
Mineralisation 158 mg/l, soft water (5.6 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.
Elements in river sediment
12 from 15elements in the top 10 %
highest: Copper 390 mg/kg
Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 95. Interpolation of the Geochemical Atlas of river sediments.
up to 50 %
50–75
75–90
90–99
above 99
Heat underfoot
27°C at 1,000 m depth
heat flow 55 mW/m²
At a depth of 2,000 m about 45 °C (increase of 18 °C per kilometre). Atlas of Geothermal Energy of Slovakia.
Natural gamma radiation
41nGy/h dose rate
percentile 8 in Slovakia
Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ.
Old mine workings
1,451objects within 3 km
mined: Fe, Cu, Kr
Nearest: Obwaser št. (adit), 20 m from the water.
Gold in river sediment
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.
Trace elements in the stream water
0 from 10indicators in the top 5 %
highest: Antimony 3.00 μg/l
Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 93 (Hnilčík).
up to 50 %
50–75
75–90
90–99
above 99
Boreholes and groundwater analyses
1,223boreholes within 3 km
701 water analyses nearby
Of these, 1220 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.
Geothermal energy
–
1 geothermal and mineral water spring within 10 km.
Environmental burdens and landfills
4sites within 3 km
4 landfills
No environmental burden is registered within 3 km; landfills are only recorded.
Deposits and ore occurrences
119records within 5 km
20 deposits, 99 ore occurrences
Geofond registers, the metallogenetic map and the mineral resources map.
Landslides and slope deformations
1areas within 3 km
Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed.
Geological structure beneath the water
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.
Sandstones and conglomerates75%SR 1.8 %
River alluvium25%SR 72 %
marker on the bar: share among all sample points on streams in Slovakia
Sandstones and conglomerates: Moderately mineralised water, depending on the share of carbonates.
Geological age of the rocks
Permian75%
Quaternary25%
Most common rock units
System
Age
Unit
Points
Permian
Early Permian
Knol Formation
3×
Quaternary
Holocene
fluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains
1×
Quaternary cover
fluvial sediments of floodplains100%SR 68 %
marker on the bar: share among all sample points on streams in Slovakia
Typical thickness of the Quaternary cover2.3m
2 – 550%SR 48 %
0 – 250%SR 16 %
marker on the bar: share among all sample points on streams in Slovakia
Tectonic units
GEMERIKUM100%SR 13 %
marker on the bar: share among all sample points on streams in Slovakia
Tectonic division
Paleo-Alpine tectonic units of the Inner Western Carpathians100%SR 16 %
marker on the bar: share among all sample points on streams in Slovakia
Neotectonic units
positive unit (mountain range)100%SR 60 %
marker on the bar: share among all sample points on streams in Slovakia
Direction of neotectonic movements
large uplift100%SR 26 %
marker on the bar: share among all sample points on streams in Slovakia
Regional geological division
Gemer Belt100%SR 5.9 %
marker on the bar: share among all sample points on streams in Slovakia
Regional geological division (subunits)
Spiš–Gemer Ore Mountains50%SR 2.9 %
Slovak Paradise50%SR 0.7 %
marker on the bar: share among all sample points on streams in Slovakia
Engineering-geological districts
region of low-grade metamorphic rocks60%SR 1.7 %
region of mountain-stream deposits20%SR 21 %
region of metamorphosed volcanic rocks20%SR 0.2 %
marker on the bar: share among all sample points on streams in Slovakia
Engineering-geological formations
formation of epimetamorphic rocks80%SR 2.2 %
formation of Quaternary sediments20%SR 71 %
marker on the bar: share among all sample points on streams in Slovakia
Susceptibility of the area to slope deformations
Region of stable areas100%SR 95 %
marker on the bar: share among all sample points on streams in Slovakia
The map covers 4 of 6 points on the water line.
Hydrogeology: aquifers and groundwater
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.
Aquifer rocks (hydrogeological map 1:200,000)
Basic volcanic rocks67%SR 6.6 %
Gravel33%SR 52 %
marker on the bar: share among all sample points on streams in Slovakia
Aquifer type
Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody67%SR 6.4 %
Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Gravel)33%SR 22 %
marker on the bar: share among all sample points on streams in Slovakia
Type of permeability (basic hydrogeological map 1:50,000)
fissure80%SR 12 %
intergranular20%SR 86 %
marker on the bar: share among all sample points on streams in Slovakia
Hydrogeological function
aquifer100%SR 95 %
marker on the bar: share among all sample points on streams in Slovakia
Main hydrogeological region
Paleozoic of the Slovak Ore Mountains in the Hornád basin100%SR 2.1 %
marker on the bar: share among all sample points on streams in Slovakia
Genetic type of groundwater
fluviogenic50%SR 6.4 %
silicate-carbonate50%SR 2.9 %
marker on the bar: share among all sample points on streams in Slovakia
Chemical type of groundwater
Ca-Mg-Na-HCO3-SO450%SR 4.5 %
Ca-Mg-HCO3 and Ca-Mg-HCO3-SO450%SR 0.0 %
marker on the bar: share among all sample points on streams in Slovakia
Groundwater quality class
B67%SR 18 %
A33%SR 36 %
marker on the bar: share among all sample points on streams in Slovakia
Surface water chemistry according to the atlas
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.
Water acidity
pH 8.12typical 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.
Water hardness
5.6°dH, soft
Sum of calcium and magnesium (1.00 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.
soft
medium
hard
very hard
Dissolved substances
158mg/l mineralisation
Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds.
up to 50 %
50–75
75–90
90–99
above 99
Ionic composition of the water
Cations (positive ions)
Ca 61Mg 33
Anions (negative ions)
HCO₃ 64SO₄ 30
Water type by dominant ions: Ca–Mg–HCO₃–SO₄
Shares are in equivalents, the usual way of comparing the composition of waters.
Major ions
SulphatesSO429.6 mg/lpercentile 33
ChloridesCl4.26 mg/lpercentile 29
MagnesiumMg8.58 mg/lpercentile 26
FluoridesF0.0596 mg/lpercentile 16
CalciumCa25.8 mg/lpercentile 15
BicarbonatesHCO379.4 mg/lpercentile 13
SodiumNa2.32 mg/lpercentile 7
PotassiumK0.697 mg/lpercentile 6
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)
Nutrients and organic pollution
NitratesNO36.67 mg/lpercentile 53
PhosphatesPO40.0358 mg/lpercentile 20
AmmoniumNH40.0329 mg/lpercentile 13
Chemical oxygen demandChSK1.46 mg/lpercentile 9
Metals
AluminiumAl189 μg/lpercentile 77
IronFe0.131 mg/lpercentile 60
ManganeseMn40.9 μg/lpercentile 57
ZincZn1.92 μg/lpercentile 12
Elements in river sediments
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.
Potentially toxic and trace elements
CopperCu390 mg/kgpercentile 95
CobaltCo18.0 mg/kgpercentile 95
TinSn18.1 mg/kgpercentile 95
BismuthBi1.97 mg/kgpercentile 95
MolybdenumMo1.27 mg/kgpercentile 95
SeleniumSe0.766 mg/kgpercentile 95
AntimonySb12.3 mg/kgpercentile 95
MercuryHg1.12 mg/kgpercentile 95
CadmiumCd1.13 mg/kgpercentile 95
ArsenicAs28.8 mg/kgpercentile 94
VanadiumV108 mg/kgpercentile 91
ZincZn211 mg/kgpercentile 90
NickelNi39.7 mg/kgpercentile 89
LeadPb28.9 mg/kgpercentile 86
ChromiumCr87.5 mg/kgpercentile 71
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)
Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
PotassiumK2.17 %percentile 96
IronFe4.79 %percentile 95
ManganeseMn2,281 mg/kgpercentile 95
AluminiumAl7.14 %percentile 88
TitaniumTi6,022 mg/kgpercentile 86
MagnesiumMg1.11 %percentile 67
PhosphorusP967 mg/kgpercentile 65
SodiumNa0.925 %percentile 61
CalciumCa1.45 %percentile 31
Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
YttriumY48.0 mg/kgpercentile 96
BoronB126 mg/kgpercentile 95
RubidiumRb120 mg/kgpercentile 93
LithiumLi43.2 mg/kgpercentile 92
BerylliumBe2.11 mg/kgpercentile 87
GalliumGa16.4 mg/kgpercentile 70
BariumBa471 mg/kgpercentile 61
CeriumCe62.1 mg/kgpercentile 61
ZirconiumZr400 mg/kgpercentile 49
StrontiumSr112 mg/kgpercentile 27
Natural radioactivity and radon
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.
Gamma radiation dose rate
41nGy/h in air
range 29 to 62 nGy/h
Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains.
up to 50 %
50–75
75–90
90–99
above 99
Radon risk of the bedrock
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.
Potassium (K)K1.38 %percentile 69
Equivalent thorium (eTh)eTh5.38 ppm5th percentile
Equivalent uranium (eU)eU1.70 ppm4th percentile
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)
Areal activity of 137CsCS1372,285 Bq/m²percentile 77
Radon risk by isopleths
medium83%SR 64 %
high17%SR 0.1 %
marker on the bar: share among all sample points on streams in Slovakia
Geophysical fields: magnetics and gravity
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.
Magnetic anomaly
-42nT
range -139 to 138 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.
negativepositive
Bouguer gravity anomaly
-19mGal
residual +9.3 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.
Geothermal potential
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.
Rock temperature with depth
27 / 45 °Cat depths of 1,000 and 2,000 m
increase of 18 °C per km
The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 55 mW/m².
Relief, climate and soils
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.
Elevation of geomorphological units (from–to)308–1 161m a.s.l.
Average elevation of the units700m a.s.l.
Average slope15.4°
Average January temperature-5.8°C
Average July temperature14.5°C
Annual precipitation1,025mm
Geomorphological units
Volovec Mountains100%SR 2.8 %
marker on the bar: share among all sample points on streams in Slovakia
Geomorphological regions
Slovak Ore Mountains100%SR 10 %
marker on the bar: share among all sample points on streams in Slovakia
Climatic-geographical types
mountain climate100%SR 33 %
marker on the bar: share among all sample points on streams in Slovakia
Susceptibility of soils to acidification
soils moderately susceptible to acidification80%SR 25 %
naturally acidic soils20%SR 8.5 %
marker on the bar: share among all sample points on streams in Slovakia
Soil contamination (map 1:500,000)
uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A100%SR 45 %
marker on the bar: share among all sample points on streams in Slovakia
Lithogeochemical types
Late Paleozoic of the Central Western Carpathians100%SR 1.9 %
marker on the bar: share among all sample points on streams in Slovakia
Map of the corridor
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.
Trace elements in surface waters
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.
AntimonySbelevated (top 10 %)
highest 3.00 μg/lmedian 0.650 μg/l20 samples50 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Hnilčík1999, 10 m from the water. Comparison: percentile 93 of all samples in Slovakia.
ChromiumCrelevated (top 10 %)
highest 4.90 μg/lmedian 3.20 μg/l20 samples20 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Ráztoka, potok1992, 940 m from the water. Comparison: percentile 91 of all samples in Slovakia.
ArsenicAselevated (top 10 %)
highest 4.00 μg/lmedian 0.500 μg/l20 samples70 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Hnilec1992, 280 m from the water. Comparison: percentile 90 of all samples in Slovakia.
CopperCuslightly elevated
highest 4.00 μg/lmedian 2.00 μg/l20 samples35 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Nálepkovo-Prvý Hámor2000, 950 m from the water. Comparison: percentile 86 of all samples in Slovakia.
CadmiumCdslightly elevated
highest 0.250 μg/lmedian 0.250 μg/l20 samples20 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Hnilec, 320 m from the water. Comparison: percentile 75 of all samples in Slovakia.
BariumBatypical value
highest 40.0 μg/lmedian 10.0 μg/l20 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Železný potok1992, 60 m from the water. Comparison: percentile 50 of all samples in Slovakia.
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l20 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Nálepkovo-Prvý Hámor2000, 950 m from the water. Comparison: percentile 46 of all samples in Slovakia.
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l20 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Nálepkovo-Prvý Hámor2000, 950 m from the water. Comparison: percentile 43 of all samples in Slovakia.
LithiumLibelow half of Slovakia
highest 5.00 μg/lmedian 5.00 μg/l20 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Nálepkovo-Prvý Hámor2000, 950 m from the water. Comparison: percentile 34 of all samples in Slovakia.
StrontiumSrbelow half of Slovakia
highest 80.0 μg/lmedian 45.0 μg/l20 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Nálepkovo-Prvý Hámor2000, 950 m from the water. Comparison: percentile 22 of all samples in Slovakia.
Major ions, mineralisation and pH
Basic water chemistry: which rocks the minerals in it come from.
Silicon dioxideSiO2typical value
highest 10.9 mg/lmedian 7.26 mg/l20 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: 1000m J od obce Závadka1992, 640 m from the water. Comparison: percentile 51 of all samples in Slovakia.
Gold and ore minerals in river sediments
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.
Limonite (FeO(OH)·nH₂O)2 samples, at most 315 grains
Magnetite (Fe₃O₄)2 samples, at most 4115 grains
Rutil (TiO₂)2 samples, at most 55 grains
Anatas (TiO₂)1 sample, at most 5 grains
Barite (BaSO₄)1 sample, at most 315 grains
Cinabarit (HgS)1 sample, at most 5 grains
Hematite (Fe₂O₃)1 sample, at most 5 grains
Chalcopyrite (CuFeS₂)1 sample, at most 5 grains
Pyrite (FeS₂)1 sample, at most 815 grains
Rock-forming and accessory minerals
Apatit (Ca₅(PO₄)₃(F,Cl,OH))2 samples, at most 5 grains
Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))2 samples, at most 1815 grains
Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)2 samples, at most 55 grains
Tourmalines (complex borosilicate)2 samples, at most 5 grains
Korund (Al₂O₃)1 sample, at most 5 grains
Zirconium (ZrSiO₄)1 sample, at most 5 grains
Groundwater: chemistry, water types and radioactivity
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.
Chemical water types nearby
Ca-Mg-SO4-HCO324×
Ca-Mg-HCO317×
Mg-Ca-HCO310×
Ca-Mg-HCO3-SO49×
Ca-SO4-HCO35×
Ca-HCO35×
Mg-Ca-SO4-HCO34×
Ca-Mg-SO43×
Water quality class according to the hydrogeochemical map
class B40×
class A28×
class H9×
class F8×
class E2×
class D2×
class C2×
class G1×
Metals in groundwater
CopperCuextreme (top 1 %)
highest 53.4 μg/lmedian 0.250 μg/l47 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 99 of all samples in Slovakia.
AntimonySbextreme (top 1 %)
highest 9.40 μg/lmedian 0.100 μg/l47 samples51 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 99 of all samples in Slovakia.
AluminiumAlextreme (top 1 %)
highest 0.370 mg/lmedian 0.00500 mg/l47 samples62 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1993, 330 m from the water. Comparison: percentile 99 of all samples in Slovakia.
ArsenicAsextreme (top 1 %)
highest 25.0 μg/lmedian 0.500 μg/l47 samples68 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 99 of all samples in Slovakia.
MercuryHgextreme (top 1 %)
highest 0.700 μg/lmedian 0.100 μg/l47 samples85 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: štôlňa1992, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia.
ChromiumCrhigh (top 5 %)
highest 5.90 μg/lmedian 0.250 μg/l47 samples66 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: studňa1993, 1.3 km from the water. Comparison: percentile 96 of all samples in Slovakia.
ZincZnhigh (top 5 %)
highest 1,530 μg/lmedian 0.500 μg/l47 samples60 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: studňa1993, 1.5 km from the water. Comparison: percentile 96 of all samples in Slovakia.
LeadPbelevated (top 10 %)
highest 2.00 μg/lmedian 0.500 μg/l47 samples70 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: studňa1993, 2.4 km from the water. Comparison: percentile 90 of all samples in Slovakia.
SeleniumSeslightly elevated
highest 1.00 μg/lmedian 0.500 μg/l47 samples96 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.6 km from the water. Comparison: percentile 83 of all samples in Slovakia.
LithiumLislightly elevated
highest 16.0 μg/lmedian 1.00 μg/l47 samples60 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: studňa1993, 70 m from the water. Comparison: percentile 75 of all samples in Slovakia.
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l20 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.6 km from the water. Comparison: percentile 50 of all samples in Slovakia.
CadmiumCdbelow half of Slovakia
highest 0.250 μg/lmedian 0.250 μg/l47 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.6 km from the water. Comparison: percentile 47 of all samples in Slovakia.
Radon in waters
Type of site
Samples
Highest radon
Median
developed spring
1
13,8 Bq/l
13.8 Bq/l
outflow from a mine working
6
49,3 Bq/l
3.70 Bq/l
source
10
35,7 Bq/l
6.22 Bq/l
water source for public supply
1
2,49 Bq/l
2.49 Bq/l
stream, river
1
0,0500 Bq/l
0.0500 Bq/l
free-flowing borehole
1
8,48 Bq/l
8.48 Bq/l
Mine workings, deposits and ore occurrences
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.
What was mined here (according to the register of old mine workings)
Fe1116×
Cu623×
Kr1×
Types of mining objects
adit753×
spoil heap547×
pinge (mining subsidence pit), line of pinge pits108×
shaft28×
other type of object15×
Nearest old mine workings
Name
Type
Mined
Ended
From the water
Obwaser št.
adit
20 m
Gezwäng št. (druhé ústie)
adit
20 m
Obwaser št.
adit
20 m
Spoil heap
spoil heap
Fe,Cu
30 m
Št.
adit
Fe,Cu
30 m
Utwaser št.
adit
50 m
Halda Bezmennej št. 14
spoil heap
50 m
Halda Martini št.
spoil heap
Fe,Cu
50 m
Halda bezmennej št.
spoil heap
Fe
50 m
Sophia št.
adit
50 m
Deposits and mining areas
Deposit
Mineral
Status and organisation
From the water
Markušovce
anhydrite
Mined deposit – VSK MINERAL s.r.o.
930 m
Markušovce
gypsum
Mined deposit – VSK MINERAL s.r.o.
930 m
Hnilčík – Roztoky
other raw materials
Mined deposit – Obec Hnilčík
1.3 km
Markušovce
gypsum
Mined deposit – VSK MINERAL s.r.o.
1.3 km
Markušovce
anhydrite
Mined deposit – VSK MINERAL s.r.o.
1.3 km
Závadka
quartz
Deposit with expected use of reserves – ŠGÚDŠ Bratislava
1.8 km
Spišská Nová Ves – Gretla, Tisovec
building stone
Mined deposit – VSK MINERAL s.r.o.
1.8 km
Závadka
quartz
Deposit with expected use of reserves – ŠGÚDŠ Bratislava
1.8 km
Spišská Nová Ves – Gretla, Tisovec
building stone
Mined deposit – VSK MINERAL s.r.o.
1.9 km
Spišská Nová Ves I
anhydrite
Deposit with expected use of reserves – URANPRES, spol. s r.o.
2.0 km
Spišská Nová Ves I
anhydrite
Deposit with expected use of reserves – URANPRES, spol. s r.o.
2.0 km
Spišská Nová Ves
copper ores
Deposit with halted mining or where use of reserves is not expected – Ludovika Energy s.r.o.
2.2 km
Ore occurrences in the metallogenic map
Occurrence
Ore type
Metals
Type
From the water
Spišská Nová Ves, Piata žila a žila Zenóbia
Complex iron ores
Fe, Cu
mineralogical occurrence
100 m
Nálepkovo – žila Žigmund
Iron ores
Fe
mineralogical occurrence
320 m
Nálepkovo – žilník Lujza
Iron ores
Fe
mineralogical occurrence
380 m
Spišská Nová Ves, žila Alžbeta and Kaluža
Complex iron ores
Fe, Cu
mineralogical occurrence
400 m
Hnilčík I.
Copper ores
Fe, Cu
deposit occurrence
410 m
Hnilčík
Uranium-molybdenum ores
Mo, U, Cu
deposit occurrence
420 m
Spiššká Nová Ves, Trubačovec
Copper ores
Cu, U
mineralogical occurrence
570 m
Spišská Nová Ves, Nová žila a Prvá až Štvrtá žila
Complex iron ores
Fe, Cu
mineralogical occurrence
630 m
Spišská Nová Ves – Sandstone
Copper ores
Cu, Mo
deposit occurrence
700 m
Hnilčík, žila Široká
Complex iron ores
Fe, Cu
small deposit
750 m
Boreholes and Geofond archive reports
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.
1,223 boreholes in the 3 km zone, of which 18 hydrogeological and 1205 other; with an archive report number 1220.
Borehole depths
up to 10 m53×
10–30 m118×
30–100 m426×
100–300 m374×
over 300 m248×
Nearest boreholes
Site
Type
Depth
Archive report
From the water
Hn-3
deposit
245.9 m
8487
20 m
Hn-11
deposit
250.0 m
8487
40 m
Hn-5
deposit
301.0 m
8487
40 m
Hn-8
deposit
417.4 m
8487
40 m
GP 1/21
deposit
55.1 m
92799
70 m
GP 2/21
deposit
53.9 m
92799
70 m
MAP-146
deposit
36.3 m
84400
70 m
Hn-9
deposit
200.0 m
2684
70 m
MAP-143
deposit
50.5 m
84400
80 m
Hn-10
deposit
151.0 m
8487
80 m
GP 6/21
deposit
45.0 m
92799
80 m
Hn-4
deposit
156.6 m
8487
80 m
Geothermal energy and mineral waters
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.
Sources of geothermal and mineral waters
Source
Type
Water temperature (°C)
Yield (l/s)
Count
Nearest from water
category a1
mineral water
< 15
< 5
1
990 m
Environmental burdens, landfills and anthropogenic sediments
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.
Waste landfills
Landfill
Area
Year established
Monitoring
From the water
Nálepkovo
800 m²
1990
–
520 m
Nálepkovo
600 m²
1989
–
560 m
Nálepkovo
4 800 m²
1985
–
1.3 km
Nálepkovo
200 m²
1985
–
1.6 km
Landslides and slope deformations
Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel.
Types of deformations
Landslides1×
Degree of activity
Stabilizovaný1×
Current state
SD taken from archival materials, ktorá bola konfrontova1×
How to read these data
Zone and distance. The distance is measured from the line of the water to the point in the register (to the centre for areas), with an accuracy of tens of metres. Counts apply only to the zone, not to the whole catchment.
Percentile. For chemistry, the highest value is compared with all atlas samples in Slovakia. It is not a legal limit or a health risk assessment; the atlases are historical (published: surface waters 2015, groundwater 1996, river sediments 1999).
Limit of quantification. Many samples have a value at the lowest level the laboratory can determine; such results mean "below the limit". For these, the position in the distribution is an estimate.
Panning concentrates. Only samples with a find are recorded. The number of grains in a concentrate is not the gold content in grams per tonne.
Relation to water. A mine working, landfill or burden nearby proves nothing about the quality of the water in the stream. It serves as a prompt for attention and a starting point for further investigation.
Sample points. The area and raster maps of ŠGÚDŠ cannot be downloaded as points, so along the line of each fishing district the value is looked up at points roughly every 3 km. It is a sample of the line, not a continuous record; a very short section may have a single point.
Atlas rasters. The chemistry of water and sediments is an interpolation of measurements in a sampling network (Geochemical Atlas of Slovakia). The value at a point is a modelled estimate for the surroundings, not a measurement in the water. The percentile compares the average of this stream with all sample points on streams in Slovakia.
Positions and scales. The maps have different scales (1:50,000 to 1:1,000,000), so the level of detail differs between sections. A map outside its coverage means there is no area at that point, not that there is nothing there.