Fishing conditions score, the best window of the day and fishing districts from the best conditions
Average of the watercourse's fishing districts
53from 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
Jasenica – Starý potok, window score 58.
The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 16:16.
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.
Fast watercoursePodhorský potok: fast water, stony bottom, riffles and the pools below them. Typical trout waters.
Elevation profile of the watercourse: from 660 to 279 m a.s.l. over 21.6 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
660 m a.s.l.
Lowest point
271 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.
388 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.
18 ‰
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.
1.50
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 2018 to 2024: how the banks, vegetation and landscape around the water change. The images switch automatically; you can also browse them by hand.
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 Jasenica – Starý 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 (21 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 alluvium80% of the water line
20% young sediments
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 7.6modelled estimate
water type Ca–Mg–SO₄–HCO₃
Mineralisation 270 mg/l, soft water (8.0 °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: Cadmium 4.21 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
48°C at 1,000 m depth
heat flow 113 mW/m²
At a depth of 2,000 m about 77 °C (increase of 29 °C per kilometre). Atlas of Geothermal Energy of Slovakia.
Natural gamma radiation
67nGy/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
451objects within 3 km
mined: Au, Ag, Pb, Zn, Cu
Nearest: Halda (spoil heap), 10 m from the water.
Gold in river sediment
6samples with gold
17 ore minerals in the sediment
Up to 2 grains in one sample (110 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
3 from 10indicators in the top 5 %
highest: Lithium 82.0 μg/l
Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (Jasenica).
up to 50 %
50–75
75–90
90–99
above 99
Boreholes and groundwater analyses
144boreholes within 3 km
617 water analyses nearby
Of these, 144 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.
Geothermal energy
54°C at the wellhead
24 geothermal boreholes within 10 km
Warmest: Sklené Teplice – ST-4, yield 13.3 l/s, 9.8 km from the water.
Environmental burdens and landfills
13sites within 3 km
2 environmental burdens, 11 landfills
Nearest burden: Banská Belá – odkalisko Sedem žien, 1.9 km from the water. Proximity does not mean that substances leak from the site into the water.
Deposits and ore occurrences
45records within 5 km
12 deposits, 33 ore occurrences
Geofond registers, the metallogenetic map and the mineral resources map.
Landslides and slope deformations
37areas within 3 km
1 active
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 alluvium80%SR 72 %
Young sediments20%SR 8.6 %
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
Quaternary100%
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
4×
Quaternary
Pleistocene – Holocene
deluvial sediments: predominantly loamy-stoney (subordinate sandy-stone) slopes and rubble
1×
Quaternary cover
deluvial sediments100%SR 16 %
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 division
NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %
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
neovolcanic rocks100%SR 10 %
marker on the bar: share among all sample points on streams in Slovakia
Regional geological division (subunits)
Central Slovak neovolcanic rocks100%SR 8.8 %
marker on the bar: share among all sample points on streams in Slovakia
Engineering-geological districts
region of mountain-stream deposits50%SR 21 %
region of colluvial sediments50%SR 1.8 %
marker on the bar: share among all sample points on streams in Slovakia
Engineering-geological formations
formation of Quaternary sediments100%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 5 of 8 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)
Acid volcanic rocks75%SR 3.2 %
Gravel13%SR 52 %
Basic volcanic rocks13%SR 6.6 %
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 vody75%SR 3.2 %
Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody (Gravel)13%SR 22 %
Menšie zvodnence s medzizrnovým alebo puklinovým typom priepustnosti alebo oblasti s takmer žiadnymi množstvami podzemnej vody13%SR 6.4 %
marker on the bar: share among all sample points on streams in Slovakia
Main hydrogeological region
neovolcanic rocks of the northern slopes of Štiavnické vrchy and Javoria83%SR 1.5 %
Quaternary Niva Hrona and Slatina from Slovenská Ľupča to Tlmače17%SR 0.0 %
marker on the bar: share among all sample points on streams in Slovakia
Geothermal groundwater bodies
Bátovce and Rykynčice Depression100%SR 4.4 %
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 7.60typical 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
8.0°dH, soft
Sum of calcium and magnesium (1.42 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
270mg/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 57Mg 26Na+K 17
Anions (negative ions)
SO₄ 48HCO₃ 43
Water type by dominant ions: Ca–Mg–SO₄–HCO₃
Shares are in equivalents, the usual way of comparing the composition of waters.
Major ions
SulphatesSO479.9 mg/lpercentile 81
PotassiumK6.08 mg/lpercentile 81
FluoridesF0.138 mg/lpercentile 61
ChloridesCl11.0 mg/lpercentile 55
SodiumNa9.74 mg/lpercentile 53
MagnesiumMg10.8 mg/lpercentile 35
CalciumCa39.1 mg/lpercentile 27
BicarbonatesHCO391.3 mg/lpercentile 16
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
AmmoniumNH40.756 mg/lpercentile 91
PhosphatesPO40.712 mg/lpercentile 89
Chemical oxygen demandChSK3.53 mg/lpercentile 58
NitratesNO37.24 mg/lpercentile 58
Metals
ZincZn160 μg/lpercentile 95
AluminiumAl572 μg/lpercentile 95
ManganeseMn311 μg/lpercentile 93
IronFe0.297 mg/lpercentile 84
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
CadmiumCd4.21 mg/kgpercentile 96
CobaltCo20.5 mg/kgpercentile 96
ZincZn575 mg/kgpercentile 96
LeadPb99.6 mg/kgpercentile 95
VanadiumV129 mg/kgpercentile 95
CopperCu59.8 mg/kgpercentile 91
MolybdenumMo0.710 mg/kgpercentile 87
BismuthBi0.363 mg/kgpercentile 82
MercuryHg0.252 mg/kgpercentile 80
AntimonySb1.40 mg/kgpercentile 79
TinSn3.20 mg/kgpercentile 68
SeleniumSe0.276 mg/kgpercentile 57
ArsenicAs5.33 mg/kgpercentile 31
ChromiumCr46.0 mg/kgpercentile 12
NickelNi14.9 mg/kgpercentile 12
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)
IronFe4.42 %percentile 94
ManganeseMn1,730 mg/kgpercentile 92
AluminiumAl7.39 %percentile 92
TitaniumTi6,817 mg/kgpercentile 91
SodiumNa1.07 %percentile 79
PhosphorusP1,055 mg/kgpercentile 73
MagnesiumMg1.06 %percentile 64
PotassiumK1.52 %percentile 51
CalciumCa1.94 %percentile 47
Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
StrontiumSr222 mg/kgpercentile 91
BariumBa570 mg/kgpercentile 83
YttriumY33.1 mg/kgpercentile 76
BerylliumBe1.73 mg/kgpercentile 69
RubidiumRb92.2 mg/kgpercentile 60
GalliumGa15.0 mg/kgpercentile 59
CeriumCe60.5 mg/kgpercentile 55
ZirconiumZr403 mg/kgpercentile 50
LithiumLi27.9 mg/kgpercentile 41
BoronB29.4 mg/kgpercentile 5
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
67nGy/h in air
range 56 to 71 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 137CsCS1374,986 Bq/m²percentile 95
Radon risk by isopleths
medium88%SR 64 %
low13%SR 36 %
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
-131nT
range -483 to 156 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
-31mGal
residual −12.1 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
48 / 77 °Cat depths of 1,000 and 2,000 m
increase of 29 °C per km
The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 113 mW/m².
Geothermal groundwater bodies beneath the water line
Bátovce and Rykynčice Depression100%SR 4.4 %
marker on the bar: share among all sample points on streams in Slovakia
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)176–940m a.s.l.
Average elevation of the units534m a.s.l.
Average slope12.5°
Average January temperature-4.9°C
Average July temperature16.9°C
Annual precipitation800mm
Geomorphological units
Štiavnica Mountains88%SR 2.2 %
Kremnica Mountains13%SR 0.0 %
marker on the bar: share among all sample points on streams in Slovakia
Geomorphological regions
Slovak Central Mountains100%SR 9.1 %
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 acidification75%SR 25 %
soils susceptible to acidification25%SR 31 %
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
Neogene volcanics100%SR 11 %
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.
LithiumLihigh (top 5 %)
highest 82.0 μg/lmedian 62.0 μg/l7 samples43 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Jasenica2011, 70 m from the water. Comparison: percentile 99 of all samples in Slovakia.
ArsenicAshigh (top 5 %)
highest 9.00 μg/lmedian 0.500 μg/l7 samples71 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Hron1993, 590 m from the water. Comparison: percentile 96 of all samples in Slovakia.
CadmiumCdhigh (top 5 %)
highest 0.900 μg/lmedian 0.250 μg/l8 samples38 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Jasenica, 70 m from the water. Comparison: percentile 95 of all samples in Slovakia.
AntimonySbelevated (top 10 %)
highest 2.30 μg/lmedian 0.500 μg/l3 samples67 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Hron1993, 590 m from the water. Comparison: percentile 92 of all samples in Slovakia.
CopperCuelevated (top 10 %)
highest 5.00 μg/lmedian 2.73 μg/l8 samples25 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Jasenica2011, 50 m from the water. Comparison: percentile 91 of all samples in Slovakia.
ChromiumCrslightly elevated
highest 2.50 μg/lmedian 1.00 μg/l7 samples86 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Hron1993, 590 m from the water. Comparison: percentile 78 of all samples in Slovakia.
StrontiumSrtypical value
highest 230 μg/lmedian 200 μg/l3 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Hron1993, 590 m from the water. Comparison: percentile 60 of all samples in Slovakia.
BariumBatypical value
highest 48.0 μg/lmedian 30.0 μg/l7 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Jasenica2011, 50 m from the water. Comparison: percentile 58 of all samples in Slovakia.
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l7 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Jasenica2011, 50 m from the water. Comparison: percentile 46 of all samples in Slovakia.
LeadPbbelow half of Slovakia
highest 2.50 μg/lmedian 2.50 μg/l8 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Jasenica2011, 50 m from the water. Comparison: percentile 43 of all samples in Slovakia.
Major ions, mineralisation and pH
Basic water chemistry: which rocks the minerals in it come from.
Silicon dioxideSiO2high (top 5 %)
highest 41.0 mg/lmedian 25.2 mg/l7 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: Jasenica2011, 50 m from the water. Comparison: percentile 95 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.
Magnetite (Fe₃O₄)42 samples, at most 4115 grains
Ilmenit (FeTiO₃)41 samples, at most 4115 grains
Pyrite (FeS₂)39 samples, at most 4115 grains
Barite (BaSO₄)37 samples, at most 315 grains
Limonite (FeO(OH)·nH₂O)37 samples, at most 1815 grains
Sphalerite (ZnS)25 samples, at most 500 grains
Hematite (Fe₂O₃)25 samples, at most 1815 grains
Rutil (TiO₂)16 samples, at most 315 grains
Anatas (TiO₂)11 samples, at most 55 grains
Chalcopyrite (CuFeS₂)10 samples, at most 400 grains
Galena (PbS)6 samples, at most 50 grains
Gold (Au)6 samples, at most 2 grains
Cinabarit (HgS)3 samples, at most 5 grains
Arsenopyrite (FeAsS)2 samples, at most 5 grains
Scheelit (CaWO₄)2 samples, at most 4 grains
Monazit ((Ce,La,Nd)PO₄)1 sample, at most 5 grains
Kasiterit (SnO₂)1 sample, at most 1 grains
Nearest samples with gold
Sample
Gold in sample
From the water
6
1 grain
30 m
Bč-63
1 grain
100 m
4
2 grains
110 m
279
1 grain
440 m
291
1 grain
530 m
186
1 grain
890 m
Rock-forming and accessory minerals
Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)42 samples, at most 4115 grains
Zirconium (ZrSiO₄)42 samples, at most 815 grains
Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)41 samples, at most 1815 grains
Korund (Al₂O₃)38 samples, at most 15 grains
Apatit (Ca₅(PO₄)₃(F,Cl,OH))35 samples, at most 55 grains
Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)33 samples, at most 1815 grains
Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))12 samples, at most 315 grains
Sillimanit (Al₂SiO₅)5 samples, at most 55 grains
Staurolit (Fe₂Al₉Si₄O₂₃(OH))4 samples, at most 315 grains
Kyanit (Al₂SiO₅)3 samples, at most 55 grains
Andaluzit (Al₂SiO₅)1 sample, at most 5 grains
Titanit (CaTiSiO₅)1 sample, at most 63 grains
Tourmalines (complex borosilicate)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.
Metals in groundwater
CopperCuextreme (top 1 %)
highest 128 μg/lmedian 0.700 μg/l46 samples
up to 50 %
50–75
75–90
90–99
above 99
Highest value: štôlňa1991, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia.
AluminiumAlextreme (top 1 %)
highest 14.2 mg/lmedian 0.0100 mg/l46 samples35 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: štôlňa1991, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia.
LeadPbextreme (top 1 %)
highest 17.0 μg/lmedian 0.500 μg/l46 samples83 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: štôlňa1991, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia.
CadmiumCdextreme (top 1 %)
highest 3.10 μg/lmedian 0.250 μg/l46 samples87 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: štôlňa1991, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia.
ZincZnhigh (top 5 %)
highest 3,680 μg/lmedian 3.00 μg/l46 samples26 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: štôlňa1991, 2.3 km from the water. Comparison: percentile 98 of all samples in Slovakia.
ArsenicAshigh (top 5 %)
highest 6.90 μg/lmedian 1.00 μg/l46 samples43 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1991, 1.9 km from the water. Comparison: percentile 96 of all samples in Slovakia.
AntimonySbhigh (top 5 %)
highest 1.20 μg/lmedian 0.100 μg/l46 samples80 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: studňa1991, 2.5 km from the water. Comparison: percentile 96 of all samples in Slovakia.
ChromiumCrhigh (top 5 %)
highest 4.90 μg/lmedian 0.250 μg/l46 samples85 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň, 190 m from the water. Comparison: percentile 96 of all samples in Slovakia.
LithiumLielevated (top 10 %)
highest 52.0 μg/lmedian 2.00 μg/l46 samples33 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: štôlňa1991, 2.3 km from the water. Comparison: percentile 95 of all samples in Slovakia.
SeleniumSeslightly elevated
highest 1.30 μg/lmedian 0.500 μg/l46 samples96 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1991, 2.0 km from the water. Comparison: percentile 86 of all samples in Slovakia.
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l27 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1991, 2.9 km from the water. Comparison: percentile 50 of all samples in Slovakia.
MercuryHgbelow half of Slovakia
highest 0.100 μg/lmedian 0.100 μg/l46 samples100 % below the limit of quantification
up to 50 %
50–75
75–90
90–99
above 99
Highest value: prameň1991, 2.9 km from the water. Comparison: percentile 46 of all samples in Slovakia.
Radon in waters
Type of site
Samples
Highest radon
Median
developed spring
3
28,2 Bq/l
13.3 Bq/l
source
27
58,6 Bq/l
8.47 Bq/l
water source for individual supply
2
58,7 Bq/l
34.5 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)
Au415×
Ag375×
Pb117×
Zn117×
Cu40×
Types of mining objects
spoil heap142×
adit122×
pinge (mining subsidence pit), line of pinge pits108×
shaft66×
other type of object9×
tailings pond4×
Nearest old mine workings
Name
Type
Mined
Ended
From the water
Spoil heap
spoil heap
Au,Ag
10 m
Spoil heap
spoil heap
Au,Ag
60 m
Spoil heap
spoil heap
Au,Ag
19th century
70 m
Spoil heap
spoil heap
Au,Ag
80 m
Belianska dedičná štôlňa
adit
Au,Ag
80 m
Spoil heap
spoil heap
Au,Ag
19th century
90 m
Spoil heap
spoil heap
Au,Ag
90 m
Spoil heap
spoil heap
Au,Ag
100 m
Line of pinge pits
pinge (mining subsidence pit), line of pinge pits
Au,Ag
100 m
Line of pinge pits
pinge (mining subsidence pit), line of pinge pits
Au,Ag
120 m
Deposits and mining areas
Deposit
Mineral
Status and organisation
From the water
Banská Belá
quartzite
Deposit with halted mining or where use of reserves is not expected – ŠGÚDŠ Bratislava
660 m
Ostrá Lúka
building stone
Deposit with expected use of reserves – Organizácia neurčená
2.2 km
Ostrá Lúka
building stone
Deposit with expected use of reserves – Organizácia neurčená
2.2 km
Banská Štiavnica I – Šobov
quartzite
Mined deposit – GEOPARK SLOVENSKO s.r.o.
2.9 km
Banská Štiavnica I – Šobov
quartzite
Mined deposit – GEOPARK SLOVENSKO s.r.o.
3.0 km
Banská Hodruša I
olovené a zinkové (polymetalické) rudy
Mined deposit – Slovenská banská, spol. s r.o.
3.6 km
Banská Štiavnica – Pb, Zn, Cu, Au, Ag
olovené a zinkové (polymetalické) rudy
Mined deposit – Slovenská banská, spol. s r.o.
3.7 km
Banská Štiavnica – Pb, Zn, Cu, Au, Ag
olovené a zinkové (polymetalické) rudy
Mined deposit – Slovenská banská, spol. s r.o.
3.7 km
Dobrá Niva
decorative stone
Mined deposit – Kamenárstvo s.r.o.
3.9 km
Dobrá Niva
decorative stone
Mined deposit – Kamenárstvo s.r.o.
3.9 km
Močiar
diatomite
Deposit with halted mining or where use of reserves is not expected – A. R. C. Logistics, s.r.o.
4.7 km
Močiar
diatomite
Deposit with halted mining or where use of reserves is not expected – A. R. C. Logistics, s.r.o.
4.8 km
Ore occurrences in the metallogenic map
Occurrence
Ore type
Metals
Type
From the water
Banská Belá – Varta
Gold ores
Au
mineralogical occurrence
660 m
Banská Belá – juh
Other ores
Bi
mineralogical occurrence
740 m
Banská Belá
Gold-silver ores
Au, Ag
small deposit
770 m
Banská Štiavnica – Siebenweiber žily
Polymetallic-precious metal ores
Pb, Zn, Au, Ag
deposit occurrence
2.2 km
Banská Štiavnica – Grüner žily
Polymetallic-precious metal ores
Pb, Zn, Au, Ag
small deposit
2.6 km
Banská Štiavnica – Šobov
Gold ores
Au
mineralogical occurrence
3.0 km
Banská Štiavnica – Emil a Alžbeta šachta
Polymetallic ores
Pb, Zn
small deposit
3.3 km
Banská Štiavnica
Polymetallic-precious metal ores
Pb, Zn, Cu, Au, Ag
large deposit
3.8 km
Podhorie – Kozí potok
Copper ores
Cu, Au, Mo
mineralogical occurrence
4.3 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.
144 boreholes in the 3 km zone, of which 37 hydrogeological and 107 other; with an archive report number 144.
Borehole depths
up to 10 m40×
10–30 m36×
30–100 m10×
100–300 m33×
over 300 m16×
Nearest boreholes
Site
Type
Depth
Archive report
From the water
J-5
engineering-geological
6.0 m
87593
10 m
J-1
engineering-geological
6.0 m
87593
30 m
Banský Studenec
narrow-diameter borehole with ordinary drinking and process water
150.0 m
34665 122Db5.pdf
40 m
Banská Belá
wide-diameter borehole
100.0 m
35289 122Db8.pdf
50 m
J-6
engineering-geological
6.0 m
87593
50 m
Banský Studenec
wide-diameter borehole
120.0 m
34856 122Db6.pdf
60 m
Banská Belá
negative borehole
140.0 m
88800 122Db37.pdf
60 m
J-2
engineering-geological
6.0 m
87593
60 m
Banský Studenec
monitoring borehole
7.0 m
86634 122Db31.pdf
70 m
Banský Studenec
wide-diameter borehole
155.0 m
34665 122Db4.pdf
70 m
JD-4
engineering-geological
7.0 m
86634
70 m
Banský Studenec
monitoring borehole
7.0 m
86634 122Db32.pdf
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.
Borehole
Temperature
Yield
Depth
Chemical water type
Use
From the water
Banská Štiavnica – HR-1
46 °C
–
910 m
Na-Ca-SO4-HCO3
unused
1.7 km
Sklené Teplice – ST-5
46 °C
–
1001 m
Ca-Mg-SO4-HCO3
unused
6.3 km
Sklené Teplice
38 °C
0.4 l/s
–
Ca-SO4
unused
7.3 km
Sklené Teplice
39 °C
0.4 l/s
–
Ca-SO4
in use
7.3 km
Sklené Teplice – ST-1
52 °C
22.3 l/s
69.7 m
Ca-SO4
in use
7.3 km
Sklené Teplice
49 °C
0.1 l/s
2.5 m
Ca-SO4
unused
7.3 km
Sklené Teplice
48 °C
0.2 l/s
–
Ca-SO4
unused
7.3 km
Sklené Teplice – ST-2
51 °C
4.5 l/s
107 m
Ca-SO4
in use
7.4 km
Sklené Teplice
43 °C
0.0 l/s
–
Ca-SO4
unused
7.4 km
Sklené Teplice
46 °C
4.5 l/s
29.7 m
Ca-SO4
unused
7.4 km
Sources of geothermal and mineral waters
Source
Type
Water temperature (°C)
Yield (l/s)
Count
Nearest from water
category d3
mineral water
39-55
16-30
1
2.9 km
category d1
mineral water
39-55
< 5
4
5.1 km
category a1
mineral water
< 15
< 5
8
6.2 km
category c1
mineral water
23-38
< 5
3
6.9 km
category d4
mineral water
39-55
31-50
1
7.2 km
category d2
mineral water
39-55
5-15
1
7.3 km
category Sklené Teplice
thermal baths
–
–
1
7.4 km
category Kováčová
thermal baths
–
–
1
7.4 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.
Environmental burdens
Site
Activity
Substance
Classification
From the water
Banská Belá – odkalisko Sedem žien
SK200220FP
1.9 km
Banská Štiavnica – odkalisko Lintich
SK200220FP
2.8 km
Waste landfills
Landfill
Area
Year established
Monitoring
From the water
Banský Studenec
200 m²
1990
–
430 m
Principlac – Banská Štiavnica
18 328 m²
1991
monitored
680 m
Banská Belá – odkalisko Sedem žien – Banská Belá
–
1975
–
1.9 km
Podhorie – Žakýl – Žakýl
–
1970
–
2.0 km
Banská Štiavnica
–
1940
–
2.2 km
Banská Štiavnica – FOUR TRADE – Banská Štiavnica
1 100 m²
2019
–
2.3 km
Banská Štiavnica
–
1940
–
2.3 km
Banská Štiavnica
–
1979
–
2.4 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
Landslides27×
Block fields3×
Block fissures1×
Block fields + landslides1×
Degree of activity
Potenciálny16×
Stabilizovaný14×
Aktívny1×
With stabilised and potential forms1×
Current state
SD taken from archival materials, ktorá bola konfrontova24×
SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S4×
Processed only in the scope of registration on a scale of 1:25,0002×
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.