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 2 fishing districts
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.
Very high0
High0
Average2
Low0
Best window today
07:00–09:00
VN Bukovec II., window score 48.
The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 18:04.
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: reservoir
Terrain height along the fishing district and the approximate water level.
ReservoirThis 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.
Terrain elevation profile (Reservoir): from 814 to 413 m a.s.l. over 12.2 km.Terrain height along the fishing district line, from the start (left) to the end
Approximate water level
482 m a.s.l.
Lowest point of the profile
413 m a.s.l.
Highest point of the profile
814 m a.s.l.
Source: Open Topo Data (eudem25m), 4 Nov 2026. The height is approximate (error of a few metres).
Terrain in 3D
Loading the 3D terrain model…
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 11 Jun 20192022imaged 10 Oct 20222025imaged 3 Jul 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 VN Bukovec II. 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 (15 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
River alluvium50% of the water line
25% volcanic rocks, 25% metamorphic rocks
Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000.
Water according to the atlas
pH 7.4modelled estimate
water type Ca–Mg–HCO₃–SO₄
Mineralisation 102 mg/l, soft water (3.2 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.
Elements in river sediment
6 from 15elements in the top 10 %
highest: Arsenic 179 mg/kg
Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 96. Interpolation of the Geochemical Atlas of river sediments.
up to 50 %
50–75
75–90
90–99
above 99
Heat underfoot
42°C at 1,000 m depth
heat flow 65 mW/m²
At a depth of 2,000 m about 69 °C (increase of 28 °C per kilometre). Atlas of Geothermal Energy of Slovakia.
Natural gamma radiation
71nGy/h dose rate
percentile 95 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
1,118objects within 3 km
mined: Sb, Fe
Nearest: Halda po neznámej štôlni (spoil heap), 60 m from the water.
Gold in river sediment
53samples with gold
22 ore minerals in the sediment
Up to 8 grains in one sample (40 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.
up to 50 %
50–75
75–90
90–99
above 99
Trace elements in the stream water
4 from 10indicators in the top 5 %
highest: Antimony 143 μg/l
Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (bez mena).
up to 50 %
50–75
75–90
90–99
above 99
Boreholes and groundwater analyses
86boreholes within 3 km
489 water analyses nearby
Of these, 86 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.
Geothermal energy
26°C at the wellhead
1 geothermal borehole within 10 km
Warmest: Košice – Anička/ Ťahanovce – G-4, 9.9 km from the water.
Environmental burdens and landfills
3sites within 3 km
3 landfills
No environmental burden is registered within 3 km; landfills are only recorded.
Deposits and ore occurrences
95records within 5 km
22 deposits, 73 ore occurrences
Geofond registers, the metallogenetic map and the mineral resources map.
Landslides and slope deformations
5areas 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.
River alluvium50%SR 72 %
Volcanic rocks25%SR 3.2 %
Metamorphic rocks25%SR 1.4 %
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.
Geological age of the rocks
Quaternary50%
older Paleozoic50%
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
2×
older Paleozoic
Late Silurian
Bystrý potok Formation
1×
older Paleozoic
Early Devonian
Drnava Formation
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 cover3.5m
2 – 5100%SR 48 %
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
medium uplift57%SR 32 %
large uplift43%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 Mountains100%SR 2.9 %
marker on the bar: share among all sample points on streams in Slovakia
Engineering-geological districts
region of low-grade metamorphic rocks67%SR 1.7 %
region of mountain-stream deposits33%SR 21 %
marker on the bar: share among all sample points on streams in Slovakia
Engineering-geological formations
formation of epimetamorphic rocks67%SR 2.2 %
formation of Quaternary sediments33%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 7 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)
Gravel75%SR 52 %
Metamorphic rocks25%SR 2.4 %
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 vody (Gravel)75%SR 22 %
Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Metamorphic rocks)25%SR 2.3 %
marker on the bar: share among all sample points on streams in Slovakia
Main hydrogeological region
the Paleozoic of the Volovské vrchy in the Bodva basin100%SR 0.0 %
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 7.45typical 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
3.2°dH, soft
Sum of calcium and magnesium (0.58 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
102mg/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 49Mg 35Na+K 15
Anions (negative ions)
HCO₃ 49SO₄ 42
Water type by dominant ions: Ca–Mg–HCO₃–SO₄
Shares are in equivalents, the usual way of comparing the composition of waters.
Major ions
FluoridesF0.122 mg/lpercentile 54
ChloridesCl3.94 mg/lpercentile 27
SulphatesSO425.4 mg/lpercentile 26
SodiumNa4.15 mg/lpercentile 21
MagnesiumMg5.80 mg/lpercentile 14
PotassiumK1.12 mg/lpercentile 13
CalciumCa13.5 mg/lpercentile 5
BicarbonatesHCO338.2 mg/lpercentile 5
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
NitratesNO39.00 mg/lpercentile 69
PhosphatesPO40.107 mg/lpercentile 45
Chemical oxygen demandChSK2.43 mg/lpercentile 31
AmmoniumNH40.0296 mg/lpercentile 10
Metals
AluminiumAl131 μg/lpercentile 68
ZincZn10.8 μg/lpercentile 67
ManganeseMn14.7 μg/lpercentile 31
IronFe0.0472 mg/lpercentile 21
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
ArsenicAs179 mg/kgpercentile 96
AntimonySb339 mg/kgpercentile 96
LeadPb196 mg/kgpercentile 96
CadmiumCd1.88 mg/kgpercentile 95
MercuryHg0.726 mg/kgpercentile 92
BismuthBi0.502 mg/kgpercentile 90
TinSn4.68 mg/kgpercentile 87
ZincZn161 mg/kgpercentile 83
CopperCu28.4 mg/kgpercentile 67
MolybdenumMo0.318 mg/kgpercentile 37
VanadiumV61.0 mg/kgpercentile 32
NickelNi18.7 mg/kgpercentile 24
SeleniumSe0.119 mg/kgpercentile 15
ChromiumCr40.2 mg/kgpercentile 8
CobaltCo4.89 mg/kgpercentile 7
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)
PotassiumK1.89 %percentile 90
SodiumNa1.20 %percentile 86
AluminiumAl6.22 %percentile 68
TitaniumTi4,613 mg/kgpercentile 55
ManganeseMn875 mg/kgpercentile 53
IronFe2.34 %percentile 29
PhosphorusP675 mg/kgpercentile 27
MagnesiumMg0.538 %percentile 7
CalciumCa0.477 %percentile 3
Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
BoronB214 mg/kgpercentile 97
RubidiumRb126 mg/kgpercentile 95
BerylliumBe2.65 mg/kgpercentile 95
YttriumY40.1 mg/kgpercentile 93
LithiumLi36.8 mg/kgpercentile 81
GalliumGa15.3 mg/kgpercentile 61
ZirconiumZr421 mg/kgpercentile 56
CeriumCe59.3 mg/kgpercentile 51
BariumBa421 mg/kgpercentile 45
StrontiumSr65.5 mg/kgpercentile 2
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
71nGy/h in air
range 57 to 78 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.
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 137CsCS1371,646 Bq/m²percentile 57
Radon risk by isopleths
medium100%SR 64 %
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
-32nT
range -47 to -9 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
-14mGal
residual +1.5 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.
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
42 / 69 °Cat depths of 1,000 and 2,000 m
increase of 28 °C per km
The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 65 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)226–1 247m a.s.l.
Average elevation of the units619m a.s.l.
Average slope15.4°
Average January temperature-5.0°C
Average July temperature16.5°C
Annual precipitation850mm
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 acidification71%SR 25 %
naturally acidic soils29%SR 8.5 %
marker on the bar: share among all sample points on streams in Slovakia
Soil contamination (map 1:500,000)
contaminated soil, the content of risk elements is higher than the limit values of C80%SR 0.9 %
relatively clean soil20%SR 53 %
marker on the bar: share among all sample points on streams in Slovakia
Lithogeochemical types
Early Paleozoic of the Gemericum100%SR 1.7 %
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.
AntimonySbextreme (top 1 %)
highest 143 μg/lmedian 41.0 μg/l25 samples20 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: bez mena1993, 150 m from the water. Comparison: percentile 99 of all samples in Slovakia.
ArsenicAsextreme (top 1 %)
highest 104 μg/lmedian 29.0 μg/l25 samples16 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: bez mena1993, 150 m from the water. Comparison: percentile 99 of all samples in Slovakia.
LeadPbhigh (top 5 %)
highest 6.00 μg/lmedian 2.50 μg/l25 samples92 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: 500m Z od obce Hylov1993, 630 m from the water. Comparison: percentile 96 of all samples in Slovakia.
ChromiumCrhigh (top 5 %)
highest 6.10 μg/lmedian 1.40 μg/l25 samples44 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Ida1993, 60 m from the water. Comparison: percentile 95 of all samples in Slovakia.
CadmiumCdelevated (top 10 %)
highest 0.700 μg/lmedian 0.250 μg/l25 samples28 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Ida, 60 m from the water. Comparison: percentile 94 of all samples in Slovakia.
CopperCuslightly elevated
highest 2.80 μg/lmedian 1.10 μg/l25 samples44 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Ida1993, 60 m from the water. Comparison: percentile 78 of all samples in Slovakia.
LithiumLislightly elevated
highest 10.0 μg/lmedian 5.00 μg/l25 samples96 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: 1500m SZ od Zlatej Idky1993, 330 m from the water. Comparison: percentile 75 of all samples in Slovakia.
BariumBatypical value
highest 40.0 μg/lmedian 10.0 μg/l25 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: 500m Z od obce Hylov1993, 630 m from the water. Comparison: percentile 50 of all samples in Slovakia.
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l18 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Ida1993, 530 m from the water. Comparison: percentile 46 of all samples in Slovakia.
StrontiumSrbelow half of Slovakia
highest 100 μg/lmedian 40.0 μg/l25 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: 1500m SZ od Zlatej Idky1993, 330 m from the water. Comparison: percentile 28 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 14.8 mg/lmedian 12.2 mg/l25 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: bez mena1993, 150 m from the water. Comparison: percentile 64 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.
Rutil (TiO₂)108 samples, at most 1815 grains
Magnetite (Fe₃O₄)106 samples, at most 4115 grains
Ilmenit (FeTiO₃)104 samples, at most 4115 grains
Limonite (FeO(OH)·nH₂O)98 samples, at most 2815 grains
Pyrite (FeS₂)96 samples, at most 4115 grains
Anatas (TiO₂)92 samples, at most 55 grains
Hematite (Fe₂O₃)86 samples, at most 1815 grains
Arsenopyrite (FeAsS)57 samples, at most 500 grains
Sphalerite (ZnS)57 samples, at most 50 grains
Scheelit (CaWO₄)54 samples, at most 175 grains
Gold (Au)53 samples, at most 8 grains
Barite (BaSO₄)35 samples, at most 4115 grains
Chalcopyrite (CuFeS₂)34 samples, at most 50 grains
Monazit ((Ce,La,Nd)PO₄)25 samples, at most 315 grains
Kasiterit (SnO₂)23 samples, at most 400 grains
Cinabarit (HgS)21 samples, at most 400 grains
Auripigment (As₂S₃)20 samples, at most 50 grains
Antimonite (Sb₂S₃)19 samples, at most 23 grains
Realgár (AsS)16 samples, at most 8 grains
Malachit (Cu₂CO₃(OH)₂)7 samples, at most 5 grains
Galena (PbS)4 samples, at most 5 grains
Markazit (FeS₂)3 samples, at most 5 grains
Nearest samples with gold
Sample
Gold in sample
From the water
28
6 grains
20 m
25
6 grains
30 m
13
3 grains
30 m
67
3 grains
40 m
34
8 grains
40 m
66
1 grain
40 m
147
1 grain
40 m
24
8 grains
40 m
Rock-forming and accessory minerals
Zirconium (ZrSiO₄)107 samples, at most 4115 grains
Tourmalines (complex borosilicate)99 samples, at most 555 grains
Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))90 samples, at most 1815 grains
Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)82 samples, at most 815 grains
Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)77 samples, at most 315 grains
Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)72 samples, at most 555 grains
Staurolit (Fe₂Al₉Si₄O₂₃(OH))10 samples, at most 5 grains
Korund (Al₂O₃)8 samples, at most 5 grains
Apatit (Ca₅(PO₄)₃(F,Cl,OH))6 samples, at most 55 grains
Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)5 samples, at most 55 grains
Titanit (CaTiSiO₅)3 samples, at most 225 grains
Sillimanit (Al₂SiO₅)2 samples, 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-HCO32×
Ca-Na-Mg-NO3-HCO31×
Ca-SO4-HCO31×
Water quality class according to the hydrogeochemical map
class B4×
Metals in groundwater
ArsenicAsextreme (top 1 %)
highest 65.0 μg/lmedian 1.10 μg/l37 samples43 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: studňa1992, 40 m from the water. Comparison: percentile 99 of all samples in Slovakia.
MercuryHgextreme (top 1 %)
highest 1.30 μg/lmedian 0.100 μg/l37 samples65 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 160 m from the water. Comparison: percentile 99 of all samples in Slovakia.
AntimonySbextreme (top 1 %)
highest 4.00 μg/lmedian 0.200 μg/l37 samples49 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 160 m from the water. Comparison: percentile 99 of all samples in Slovakia.
LeadPbhigh (top 5 %)
highest 7.00 μg/lmedian 0.500 μg/l37 samples51 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1993, 2.4 km from the water. Comparison: percentile 98 of all samples in Slovakia.
AluminiumAlhigh (top 5 %)
highest 0.170 mg/lmedian 0.00500 mg/l37 samples62 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1993, 2.2 km from the water. Comparison: percentile 98 of all samples in Slovakia.
ZincZnhigh (top 5 %)
highest 3,020 μg/lmedian 73.0 μg/l37 samples16 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.5 km from the water. Comparison: percentile 98 of all samples in Slovakia.
ChromiumCrhigh (top 5 %)
highest 7.60 μg/lmedian 0.250 μg/l37 samples89 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1993, 2.2 km from the water. Comparison: percentile 98 of all samples in Slovakia.
CadmiumCdhigh (top 5 %)
highest 0.700 μg/lmedian 0.250 μg/l37 samples92 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: štôlňa1993, 1.8 km from the water. Comparison: percentile 96 of all samples in Slovakia.
CopperCuhigh (top 5 %)
highest 7.00 μg/lmedian 0.250 μg/l37 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: studňa1992, 910 m from the water. Comparison: percentile 96 of all samples in Slovakia.
LithiumLislightly elevated
highest 22.0 μg/lmedian 3.00 μg/l37 samples19 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.4 km from the water. Comparison: percentile 80 of all samples in Slovakia.
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l18 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1992, 2.4 km from the water. Comparison: percentile 50 of all samples in Slovakia.
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l37 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1993, 2.3 km from the water. Comparison: percentile 39 of all samples in Slovakia.
Radon in waters
Type of site
Samples
Highest radon
Median
source
16
109 Bq/l
16.2 Bq/l
stream, river
3
0,470 Bq/l
0.330 Bq/l
outflow from a mine working
1
14,2 Bq/l
14.2 Bq/l
developed spring
1
7,25 Bq/l
7.25 Bq/l
water source for individual supply
1
0,730 Bq/l
0.730 Bq/l
water source for public supply
1
12,7 Bq/l
12.7 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)
Sb970×
Fe68×
Types of mining objects
pinge (mining subsidence pit), line of pinge pits544×
spoil heap352×
adit193×
other type of object26×
shaft2×
tailings pond1×
Nearest old mine workings
Name
Type
Mined
Ended
From the water
Halda po neznámej štôlni
spoil heap
Sb ores
60 m
Halda pri štôlni Agoston
spoil heap
Sb ores, antimonite
70 m
Štôlňa Agoston
adit
Sb ores, antimonite
80 m
Bezmenná štôlňa č.14
adit
Sb ores, antimonite
90 m
Halda pri štôlni Zenovicz
spoil heap
Sb ores, antimonite
90 m
Halda pri objekte č.50
spoil heap
Sb ores, antimonite
100 m
Halda pri štôlni Brevner
spoil heap
Sb ores, antimonite
100 m
Bezmenná štôlňa č.4
adit
Sb ores, antimonite
100 m
Halda pri bezmennej štôlni č.14
spoil heap
Sb ores, antimonite
110 m
Halda pri štôlni Ludovika
spoil heap
Sb ores, antimonite
110 m
Deposits and mining areas
Deposit
Mineral
Status and organisation
From the water
Zlatá Idka
technically usable mineral crystals
Deposit with expected use of reserves – ŠGÚDŠ Bratislava
440 m
Zlatá Idka
technically usable mineral crystals
Deposit with expected use of reserves – ŠGÚDŠ Bratislava
460 m
Nováčany
feldspars
Deposit with expected use of reserves – MASEVA, spol. s r.o.
1.6 km
Rudník II
feldspars
Deposit with expected use of reserves – Organizácia neurčená
1.6 km
Rudník II
feldspars
Deposit with expected use of reserves – Organizácia neurčená
1.6 km
Nováčany
feldspars
Deposit with expected use of reserves – MASEVA, spol. s r.o.
1.7 km
Rudník II
feldspars
Deposit with expected use of reserves – Organizácia neurčená
1.7 km
Rudník I
feldspars
Deposit with expected use of reserves – MASEVA, spol. s r.o.
2.0 km
Rudník I
feldspars
Deposit with expected use of reserves – MASEVA, spol. s r.o.
2.0 km
Rudník IV
feldspars
Mined deposit – LB MINERALS SK, s.r.o.
2.4 km
Rudník IV
feldspars
Mined deposit – LB MINERALS SK, s.r.o.
2.4 km
Rudník IV
feldspars
Mined deposit – LB MINERALS SK, s.r.o.
2.4 km
Ore occurrences in the metallogenic map
Occurrence
Ore type
Metals
Type
From the water
Poproč, žila Liborius
Antimonite-gold ores
Sb, Au
mineralogical occurrence
340 m
Poproč, žily Zdar Boh and Mikuláš
Complex iron ores
Fe
deposit occurrence
590 m
Zlatá Idka, žily Štefan, Matej, František, Orban krížna, Bodog a Žila upadajúca na sever
Antimonite-gold ores
Sb, Au
deposit occurrence
690 m
Medzev, žila Macová
Complex iron ores
Fe, Cu
mineralogical occurrence
760 m
Poproč, žila Kobylianka
Antimonite-gold ores
Sb, Au
mineralogical occurrence
830 m
Poproč, žila Podkovec
Antimonite-gold ores
Sb, Au
mineralogical occurrence
840 m
Zlatá Idka, žila Bertalan
Antimonite-gold ores
Sb, Au
small deposit
850 m
Zlatá Idka, žila Katalin
Antimonite-gold ores
Sb, Au
deposit occurrence
850 m
Zlatá Idka, žily Jozef, František-Jozef, Žila so sklonom na juh, Alžbeta, Nová žila a Jeremiáš
Antimonite-gold ores
Sb, Au
small deposit
1.1 km
Zlatá Idka, žily Všechsvätých, Peck, Fridrich, Albert, Antal and Tekla
Antimonite-gold ores
Sb, Au
small deposit
1.1 km
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.
86 boreholes in the 3 km zone, of which 9 hydrogeological and 77 other; with an archive report number 86.
Borehole depths
up to 10 m13×
10–30 m22×
30–100 m25×
100–300 m16×
over 300 m2×
Nearest boreholes
Site
Type
Depth
Archive report
From the water
Zlatá Idka
narrow-diameter borehole with ordinary drinking and process water
6.5 m
54070 115Cc9.pdf
30 m
R-45
engineering-geological
3.8 m
80782
50 m
Zlatá Idka
narrow-diameter borehole with ordinary drinking and process water
11.0 m
54070 115Cc8.pdf
70 m
Zlatá Idka
narrow-diameter borehole with ordinary drinking and process water
9.5 m
54070 115Cc10.pdf
70 m
327
deposit
264.8 m
79096
90 m
Zlatá Idka
narrow-diameter borehole with ordinary drinking and process water
3.5 m
25944 115Cc4.pdf
100 m
Bukovec
narrow-diameter borehole with ordinary drinking and process water
30.0 m
73884 115Cd58.pdf
100 m
ID-2
deposit
–
59543
100 m
331
deposit
197.5 m
79096
120 m
330
deposit
262.1 m
79096
120 m
IL-2
deposit
–
59543
190 m
328
deposit
290.1 m
79096
220 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.
Borehole
Temperature
Yield
Depth
Chemical water type
Use
From the water
Košice – Anička/ Ťahanovce – G-4
26 °C
–
310 m
Na-Ca-Mg-HCO3-Cl
unused
9.9 km
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
9.0 km
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
Nižný Klátov I. – Nižný Klátov
–
1980
–
2.2 km
Nižný Klátov II. – Nižný Klátov
–
1980
–
2.4 km
Nováčany I. – Nováčany
–
1989
–
2.9 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
Landslides5×
Degree of activity
Potenciálny5×
Current state
Processed only in the scope of registration on a scale of 1:25,0002×
SD prebraná z archívnych materiálov (existuje inž. geologick1×
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.
Šlichy. 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.