Watercourse

VN Starina

Bodrog basin and HornádSalmonid (trout)
fishing districts
2
fishing district length
33.5km
region
Prešov Region
Aerial image of watercourse VN Starina with the line highlighted
Blue line: course of the watercourse (approximate). Orthophoto mosaic of Slovakia © GKÚ Bratislava, CC BY 4.0Google Maps

By the water now

Today on the VN Starina watercourse

Fishing conditions score, the best window of the day and fishing districts from the best conditions

Average of the watercourse's fishing districts

Low 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
  • Average0
  • Low2

Best window today

06:00–08:00

Vodárenská nádrž Starina, window score 38.

The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 03:04.

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.
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    Elevation profile: reservoir

    Terrain height along the fishing district and the approximate water level.

    Reservoir This is a reservoir, so the watercourse is not assessed here: the water has no current, fall or gradient. The chart shows the terrain height along the fishing district.

    3004005006007000 km5 km10 kmVN Starina – prítoky
    Terrain elevation profile (Reservoir): from 649 to 331 m a.s.l. over 10.2 km.
    Terrain height along the fishing district line, from the start (left) to the end
    Approximate water level
    386 m a.s.l.
    Lowest point of the profile
    331 m a.s.l.
    Highest point of the profile
    649 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.

    Aerial image of watercourse VN Starina from 2019
    2019imaged 5 Jul 2019
    Aerial image of watercourse VN Starina from 2022
    2022imaged 4 Aug 2022
    Aerial image of watercourse VN Starina from 2025
    2025imaged 13 Aug 2025

    Orthophoto mosaic of Slovakia © GKÚ Bratislava, NLC Zvolen. The year and day of imaging depend on the location, so individual years may differ in season and weather.

    Water pollution on the VN Starina watercourse

    Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby

    Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025

    1 of 1 fishing districts on the watercourse with SHMÚ data: the nearest site has an unmet standard in at least one indicator.

    • 3 or more indicators1
    • No SHMÚ data1
    SHMÚ has no data for 1 fishing districts: there is no monitoring site with the same name near their watercourse.

    Most polluted fishing districtsall with an unmet standard

    Groundwater: measured valuestypical value from stations within 10 km, 2025

    0 of 2 fishing districts with measurements have groundwater nearby with a value above the limit for at least one indicator.

    Source: SHMÚ (yearbooks on surface and groundwater quality), the register of wastewater treatment plants from VÚVH and the EEA. A SHMÚ site is assigned to a fishing district by the same watercourse name and by distance; the yearbook lists the sites that failed the standard, so a missing site is not proof of clean water.

    Geology and geochemistry of the VN Starina 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 (33 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 conglomerates36% of the water line

    36% flysch, 18% river alluvium

    Moderately mineralised water, depending on the share of carbonates. Geological Map of Slovakia 1:50,000.

    510

    Water according to the atlas

    pH 7.9modelled estimate

    water type Ca–HCO₃

    Mineralisation 180 mg/l, soft water (6.0 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream.

    Elements in river sediment

    1 from 15elements in the top 10 %

    highest: Nickel 43.3 mg/kg

    Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 92. Interpolation of the Geochemical Atlas of river sediments.

    0 °C80

    Heat underfoot

    45°C at 1,000 m depth

    heat flow 75 mW/m²

    Atlas of Geothermal Energy of Slovakia.

    20200

    Natural gamma radiation

    51nGy/h dose rate

    percentile 53 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

    0objects within 3 km

    No old mine working is recorded within 3 km of the water.

    Gold in river sediment

    1sample with gold

    13 ore minerals in the sediment

    Up to 1 grain in one sample (760 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment.

    Trace elements in the stream water

    0 from 8indicators in the top 5 %

    highest: Barium 60.0 μg/l

    Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 71 (Cirocha. prítok).

    Boreholes and groundwater analyses

    79boreholes within 3 km

    834 water analyses nearby

    Of these, 65 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other.

    Geothermal energy

    –

    5 geothermal and mineral water springs within 10 km.

    Environmental burdens and landfills

    2sites within 3 km

    2 landfills

    No environmental burden is registered within 3 km; landfills are only recorded.

    Deposits and ore occurrences

    12records within 5 km

    12 ore occurrences

    Geofond registers, the metallogenetic map and the mineral resources map.

    Landslides and slope deformations

    138areas 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 conglomerates36%SR 1.8 %
    • Flysch36%SR 4.7 %
    • River alluvium18%SR 72 %
    • Limestones and dolomites9.1%SR 2.7 %

    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

    • flysch82%
    • Quaternary18%

    Most common rock units

    SystemAgeUnitPoints
    flyschMiddle Cretaceous – PaleoceneLupkov Formation4×
    flyschPaleocene – EoceneSubmenilite Formation4×
    QuaternaryHolocenefluvial sediments: lithofacial undivided alluvial clays, or sandy to gravelly clays of valleys and floodplains2×
    flyschEocene – OligoceneMenilite and Smilno Formations1×

    Quaternary cover

    • fluvial sediments of floodplains50%SR 68 %
    • deluvial sediments38%SR 16 %
    • landslides13%SR 0.8 %

    marker on the bar: share among all sample points on streams in Slovakia

    • Typical thickness of the Quaternary cover2.9m
    • 2 – 577%SR 48 %
    • 0 – 223%SR 16 %

    marker on the bar: share among all sample points on streams in Slovakia

    Tectonic units

    • DUKLIANSKY PRÍKROV100%SR 3.8 %

    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

    • medium uplift100%SR 32 %

    marker on the bar: share among all sample points on streams in Slovakia

    Regional geological division

    • flysch belt100%SR 9.6 %

    marker on the bar: share among all sample points on streams in Slovakia

    Regional geological division (subunits)

    • Dukla–Bukovec flysch100%SR 1.8 %

    marker on the bar: share among all sample points on streams in Slovakia

    Engineering-geological districts

    • region of sandstone rocks75%SR 4.1 %
    • region of flyschoid rocks25%SR 5.4 %

    marker on the bar: share among all sample points on streams in Slovakia

    Engineering-geological formations

    • flysch formation100%SR 13 %

    marker on the bar: share among all sample points on streams in Slovakia

    Susceptibility of the area to slope deformations

    • Region of stable areas75%SR 95 %
    • Region of potentially unstable areas25%SR 4.4 %

    marker on the bar: share among all sample points on streams in Slovakia

    The map covers 11 of 13 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)

    • Sandstones67%SR 15 %
    • 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 vody (Sandstones)67%SR 15 %
    • 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)

    • fissure88%SR 12 %
    • intergranular13%SR 86 %

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    Hydrogeological function

    • regional aquiclude88%SR 2.3 %
    • aquifer13%SR 95 %

    marker on the bar: share among all sample points on streams in Slovakia

    Main hydrogeological region

    • Paleogene and Quaternary of the Laborca Povodia to Brekov and the Mesozoic of the Humen Mountains100%SR 3.0 %

    marker on the bar: share among all sample points on streams in Slovakia

    Genetic type of groundwater

    • natural silicate-carbonatogenic and carbonatogenic100%SR 0.0 %

    marker on the bar: share among all sample points on streams in Slovakia

    Chemical type of groundwater

    • predominantly Ca-HCO3, Ca-Mg-HCO3 or Ca-Mg-HCO3-SO4, sporadically Ca-Mg-Na-HCO3, Mg-Ca-HCO3-SO480%SR 0.5 %
    • predominantly Ca-HCO3 or Ca-Mg-HCO3, less Ca-Mg-HCO3-SO420%SR 0.0 %

    marker on the bar: share among all sample points on streams in Slovakia

    Groundwater quality class

    • A67%SR 36 %
    • B33%SR 18 %

    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.

    510

    Water acidity

    pH 7.91typical 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

    6.0°dH, soft

    Sum of calcium and magnesium (1.08 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain.

    Dissolved substances

    180mg/l mineralisation

    Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds.

    Ionic composition of the water

    Water type by dominant ions: Ca–HCO₃

    Shares are in equivalents, the usual way of comparing the composition of waters.

    Major ions

    • FluoridesF0.0923 mg/lpercentile 37
    • CalciumCa34.4 mg/lpercentile 23
    • BicarbonatesHCO3109 mg/lpercentile 21
    • PotassiumK1.32 mg/lpercentile 17
    • SodiumNa3.57 mg/lpercentile 16
    • MagnesiumMg5.38 mg/lpercentile 12
    • SulphatesSO414.7 mg/lpercentile 6
    • ChloridesCl1.65 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

    • NitratesNO34.63 mg/lpercentile 34
    • AmmoniumNH40.0441 mg/lpercentile 22
    • Chemical oxygen demandChSK1.76 mg/lpercentile 14
    • PhosphatesPO40.0163 mg/lpercentile 4

    Metals

    • IronFe0.0737 mg/lpercentile 36
    • AluminiumAl25.3 μg/lpercentile 24
    • ZincZn2.87 μg/lpercentile 19
    • ManganeseMn9.17 μg/lpercentile 19

    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

    • NickelNi43.3 mg/kgpercentile 92
    • VanadiumV99.4 mg/kgpercentile 88
    • MolybdenumMo0.703 mg/kgpercentile 87
    • SeleniumSe0.480 mg/kgpercentile 85
    • CopperCu35.2 mg/kgpercentile 80
    • ChromiumCr88.7 mg/kgpercentile 72
    • CobaltCo10.00 mg/kgpercentile 71
    • TinSn3.08 mg/kgpercentile 65
    • AntimonySb0.742 mg/kgpercentile 59
    • ArsenicAs7.27 mg/kgpercentile 58
    • ZincZn87.5 mg/kgpercentile 40
    • CadmiumCd0.0875 mg/kgpercentile 21
    • LeadPb11.1 mg/kgpercentile 20
    • BismuthBi0.133 mg/kgpercentile 16
    • MercuryHg0.0511 mg/kgpercentile 14

    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)
    • PotassiumK2.00 %percentile 93
    • AluminiumAl6.89 %percentile 84
    • IronFe3.46 %percentile 81
    • TitaniumTi4,869 mg/kgpercentile 65
    • SodiumNa0.932 %percentile 62
    • ManganeseMn908 mg/kgpercentile 56
    • MagnesiumMg0.883 %percentile 49
    • CalciumCa1.02 %percentile 14
    • PhosphorusP509 mg/kgpercentile 9
    Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
    • LithiumLi52.9 mg/kgpercentile 96
    • BerylliumBe2.53 mg/kgpercentile 95
    • GalliumGa21.8 mg/kgpercentile 95
    • BoronB92.2 mg/kgpercentile 93
    • RubidiumRb118 mg/kgpercentile 92
    • CeriumCe80.1 mg/kgpercentile 91
    • YttriumY32.5 mg/kgpercentile 73
    • ZirconiumZr401 mg/kgpercentile 50
    • BariumBa432 mg/kgpercentile 48
    • StrontiumSr121 mg/kgpercentile 36

    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.

    20200

    Gamma radiation dose rate

    51nGy/h in air

    range 44 to 55 nGy/h

    Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains.

    Radon risk of the bedrock

    low

    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)K1.33 %percentile 60
    • Equivalent thorium (eTh)eTh7.60 ppm58th percentile
    • Equivalent uranium (eU)eU2.46 ppm35th 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 137CsCS1371,102 Bq/m²percentile 24

    Radon risk by isopleths

    • low57%SR 36 %
    • medium43%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.

    SVJZ

    Magnetic anomaly

    -21nT

    range -31 to -13 nT

    Deviation of the Earth's magnetic field from its surroundings. Positive and negative anomalies reveal rocks with magnetite (basalts, basic volcanic rocks) and boundaries in the bedrock.

    Bouguer gravity anomaly

    -23mGal

    residual +0.7 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 at 1,000 m depth45°C
    • Surface heat flow density75mW/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)261–1 205m a.s.l.
    • Average elevation of the units583m a.s.l.
    • Average slope14.0°
    • Average January temperature-5.2°C
    • Average July temperature16.2°C
    • Annual precipitation870mm

    Geomorphological units

    • Bukovské Mountains100%SR 0.0 %

    marker on the bar: share among all sample points on streams in Slovakia

    Geomorphological regions

    • Poloniny100%SR 0.8 %

    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 acidification100%SR 25 %

    marker on the bar: share among all sample points on streams in Slovakia

    Soil contamination (map 1:500,000)

    • relatively clean soil54%SR 53 %
    • uncontaminated soil, the geogenically determined content of some risk elements reaches limit values A46%SR 45 %

    marker on the bar: share among all sample points on streams in Slovakia

    Lithogeochemical types

    • Cretaceous and Paleogene of the Outer Carpathians100%SR 9.5 %

    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.

    Jalová – Stakčínska Roztoka – none (1.9 km from the water)Jalová – Stakčínska Roztoka – none (2.2 km from the water)a1 (2.0 km from the water)a1 (2.9 km from the water)a1 (4.2 km from the water)a1 (5.1 km from the water)a1 (9.6 km from the water)Veľká Poľana – building stone – sandstone (90 m from the water)Smolník nad Cirochou – brick raw materials (110 m from the water)Ruské – brick raw materials (130 m from the water)Ostrožnica – brick raw materials (150 m from the water)Veľká Poľana – brick raw materials (190 m from the water)Ruské – building stone – sandstone, chert (210 m from the water)Starina – brick raw materials (290 m from the water)Zvala – brick raw materials (290 m from the water)Dara – brick raw materials (2.9 km from the water)Čukalovce – brick raw materials (4.3 km from the water)Runina – building stone – sandstone (4.3 km from the water)Pčoliné – building stone – sandstone, quartzite (4.9 km from the water)Starina – general geology (2.5 km from the water)SMOLNIK – Landslides (50 m from the water)– Landslides (70 m from the water)– Landslides (80 m from the water)– Landslides (120 m from the water)– Landslides (120 m from the water)ZVALA – Landslides (120 m from the water)RUSKE – Landslides (130 m from the water)OSTROZNICA – Landslides (130 m from the water)– Landslides (140 m from the water)– Landslides (140 m from the water)– Landslides (160 m from the water)– Landslides (160 m from the water)SMOLNIK – Landslides (170 m from the water)VELKA POLANA – Landslides (170 m from the water)ZVALA – Landslides (180 m from the water)– Landslides (180 m from the water)OSADNE – Landslides (210 m from the water)– Landslides (210 m from the water)– Landslides (220 m from the water)– Landslides (220 m from the water)– Landslides (240 m from the water)– Landslides (240 m from the water)ZVALA – Landslides (250 m from the water)– Landslides (260 m from the water)– Landslides (260 m from the water)– Landslides (260 m from the water)ZVALA – Landslides (270 m from the water)PRISLOP – Landslides (270 m from the water)– Landslides (280 m from the water)SMOLNIK – Landslides (290 m from the water)STARINA – Landslides (300 m from the water)SMOLNIK – Landslides (300 m from the water)STARINA – Landslides (320 m from the water)– Landslides (320 m from the water)– Landslides (370 m from the water)SMOLNIK – Landslides (380 m from the water)– Landslides (400 m from the water)– Landslides (420 m from the water)– Landslides (420 m from the water)STARINA – Landslides (420 m from the water)VELKA POLANA – Landslides (430 m from the water)– Landslides (440 m from the water)OSTROZNICA – Landslides (460 m from the water)STARINA – Landslides (460 m from the water)RUSKE – Landslides (470 m from the water)– Landslides (490 m from the water)– Landslides (500 m from the water)– Landslides (500 m from the water)– Landslides (500 m from the water)– Landslides (510 m from the water)– Landslides (520 m from the water)VELKA POLANA – Landslides (520 m from the water)– Landslides (530 m from the water)– Landslides (580 m from the water)– Landslides (590 m from the water)VELKA POLANA – Landslides (600 m from the water)– Landslides (610 m from the water)– Landslides (640 m from the water)– Landslides (650 m from the water)– Landslides (680 m from the water)STARINA – Landslides (710 m from the water)– Landslides (740 m from the water)– Landslides (770 m from the water)– Landslides (790 m from the water)– Landslides (830 m from the water)– Landslides (840 m from the water)– Landslides (870 m from the water)STARINA – Landslides (890 m from the water)– Block fissures (900 m from the water)– Landslides (900 m from the water)– Landslides (920 m from the water)– Landslides (940 m from the water)– Landslides (960 m from the water)– Landslides (980 m from the water)– Landslides (1.0 km from the water)– Landslides (1.1 km from the water)– Landslides (1.1 km from the water)– Landslides (1.1 km from the water)– Landslides (1.1 km from the water)RUSKE – Landslides (1.1 km from the water)Ruské – úzkoprofilový vrt s obyčajnou pitnou a ú (50 m from the water)Ostrožnica – širokoprofilový vrt (Ø vŕtania nad 600 m (60 m from the water)Smolník – širokoprofilový vrt (Ø vŕtania nad 600 m (70 m from the water)Starina – borehole for a waterworks (80 m from the water)Stariná – širokoprofilový vrt (Ø vŕtania nad 600 m (100 m from the water)Veľká Poľana – širokoprofilový vrt (Ø vŕtania nad 600 m (110 m from the water)Starina – borehole for a waterworks (120 m from the water)JRD Stariná – úzkoprofilový vrt s obyčajnou pitnou a ú (150 m from the water)Starina – borehole for a waterworks (150 m from the water)Zvala-Škola – úzkoprofilový vrt s obyčajnou pitnou a ú (150 m from the water)Veľká Poľana – širokoprofilový vrt (Ø vŕtania nad 600 m (150 m from the water)Starina – širokoprofilový vrt (Ø vŕtania nad 600 m (220 m from the water)Veľká Poľana – úzkoprofilový vrt s obyčajnou pitnou a ú (220 m from the water)Starina – širokoprofilový vrt (Ø vŕtania nad 600 m (270 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (50 m from the water)prameň – Groundwater springs (60 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (60 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (70 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (80 m from the water)prameň – Groundwater springs (90 m from the water)prameň – Groundwater springs (90 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (100 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (110 m from the water)vodomerná stanica s monitorovaním vodných stavov – Artificial hydrogeologically significant objects (110 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (150 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (150 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (150 m from the water)zrážkomerná stanica – Artificial hydrogeologically significant objects (170 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (220 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (220 m from the water)prameň – Groundwater springs (250 m from the water)existujúci hydrogeologický vrt – Hydrogeological boreholes (270 m from the water)prameň – Groundwater springs (350 m from the water)skupina prameňov – Groundwater springs (400 m from the water)skupina prameňov – Groundwater springs (410 m from the water)prameň – Groundwater springs (470 m from the water)prameň – Groundwater springs (500 m from the water)prameň – Groundwater springs (500 m from the water)skupina prameňov – Groundwater springs (530 m from the water)prameň – Groundwater springs (530 m from the water)prameň – Groundwater springs (630 m from the water)prameň – Groundwater springs (640 m from the water)skupina prameňov – Groundwater springs (640 m from the water)pramenná línia – Groundwater springs (670 m from the water)prameň – Groundwater springs (710 m from the water)prameň – Groundwater springs (720 m from the water)skupina prameňov – Groundwater springs (740 m from the water)prameň – Groundwater springs (810 m from the water)prameň – Groundwater springs (810 m from the water)skupina prameňov – Groundwater springs (820 m from the water)prameň – Groundwater springs (850 m from the water)prameň – Groundwater springs (850 m from the water)prameň – Groundwater springs (850 m from the water)pramenná línia – Groundwater springs (890 m from the water)Ruské,700m J od K512 – source (10 m from the water)Zvala,850m JJZ od K929 – source (20 m from the water)Ruské,500m S od K740 – source (40 m from the water)Smolník,500m JJV od K1012 – source (70 m from the water)povodie Stružnice (nad VN Starina), 1830 m ZJZ o – source (70 m from the water)povodie potoka Smolník 2050 m ZJZ od k. Solište – source (90 m from the water)pramenná oblasť Cirochy 670 m JV od Ruského sedl – source (180 m from the water)Smolník,1300m SZ od K531 – source (220 m from the water)Starina,2100, JZ od K683 – source (230 m from the water)Ruské,900m JJV od K512 – source (260 m from the water)Ruské,1500m SSZ od K512 – source (320 m from the water)Veľká Poľana,900m V od K683 – source (390 m from the water)Zvala,1000m VSV od K774 – source (390 m from the water)Ruské,200m SZ od K740 – source (400 m from the water)Smolník,1800m Z od K817 – source (410 m from the water)Zvala,300m JZ od K528 – source (410 m from the water)Ostrožnica,1700m SV od K645 – source (420 m from the water)Veľká Poľana,1400m J od K597 – source (430 m from the water)Veľká Poľana,1700m SV od K652 – source (490 m from the water)Veľká Poľana,1100m SV od K550 – source (510 m from the water)Ruské,800m JJV od K512 – source (560 m from the water)Ostrožnica,650m ZSZ od K412 – source (690 m from the water)Starina,500m S od K566 – source (700 m from the water)Ruske,1000m JJZ od K807 – source (710 m from the water)Smolník,600m SSZ od K531 – source (720 m from the water)Veľká Poľana,2300m J od K591 – source (720 m from the water)Ostrožnica,1800m JZ od K412 – source (730 m from the water)Starina,1100m ZSZ od K324 – source (840 m from the water)V.Polana,1300m VSV od K531 – source (970 m from the water)Starina.1200m SV od K655 – source (1.0 km from the water)Parizahovce,400m SSZ od K929 – source (1.0 km from the water)Ostrožnica,550m JZ od K725 – source (1.1 km from the water)Starina,700m JV od K645 – source (1.2 km from the water)Zvala,400m J od K920 – source (1.3 km from the water)Starina,800m SV od K655 – source (1.4 km from the water)Smolník,400m Z od K817 – source (1.4 km from the water)Veľká Poľana,900m JV od K817 – source (1.4 km from the water)Veľká Poľana,500m S od K639 – source (1.5 km from the water)Ruské,1200m J od K1002 – source (1.5 km from the water)Veľká Poľana,1300m JV od K597 – source (1.6 km from the water)zlato 1 ks – gold (760 m from the water)5 km

    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.

    • BariumBatypical value
      highest 60.0 μg/lmedian 41.0 μg/l10 samples

      Highest value: Cirocha. prítok2009, 80 m from the water. Comparison: percentile 71 of all samples in Slovakia.

    • SeleniumSebelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification

      Highest value: Cirocha2009, 480 m from the water. Comparison: percentile 46 of all samples in Slovakia.

    • LeadPbbelow half of Slovakia
      highest 2.50 μg/lmedian 2.50 μg/l10 samples100 % below the limit of quantification

      Highest value: Cirocha2009, 480 m from the water. Comparison: percentile 43 of all samples in Slovakia.

    • LithiumLibelow half of Slovakia
      highest 5.00 μg/lmedian 5.00 μg/l10 samples100 % below the limit of quantification

      Highest value: Cirocha2009, 480 m from the water. Comparison: percentile 34 of all samples in Slovakia.

    • ChromiumCrbelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l10 samples100 % below the limit of quantification

      Highest value: Cirocha2009, 480 m from the water. Comparison: percentile 32 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.150 μg/lmedian 0.150 μg/l10 samples100 % below the limit of quantification

      Highest value: Cirocha, 480 m from the water. Comparison: percentile 26 of all samples in Slovakia.

    • CopperCubelow half of Slovakia
      highest 1.00 μg/lmedian 1.00 μg/l10 samples100 % below the limit of quantification

      Highest value: Cirocha2009, 480 m from the water. Comparison: percentile 22 of all samples in Slovakia.

    • ArsenicAsbelow half of Slovakia
      highest 0.500 μg/lmedian 0.500 μg/l10 samples100 % below the limit of quantification

      Highest value: Cirocha2009, 480 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 dioxideSiO2below half of Slovakia
      highest 8.08 mg/lmedian 6.66 mg/l10 samples

      Highest value: Hricov potok2009, 880 m from the water. Comparison: percentile 34 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.

    • Barite (BaSO₄)156 samples, at most 1815 grains
    • Pyrite (FeS₂)72 samples, at most 815 grains
    • Rutil (TiO₂)60 samples, at most 4115 grains
    • Limonite (FeO(OH)·nH₂O)50 samples, at most 4115 grains
    • Anatas (TiO₂)46 samples, at most 315 grains
    • Magnetite (Fe₃O₄)39 samples, at most 315 grains
    • Monazit ((Ce,La,Nd)PO₄)21 samples, at most 315 grains
    • Ilmenit (FeTiO₃)19 samples, at most 155 grains
    • Hematite (Fe₂O₃)3 samples, at most 55 grains
    • Scheelit (CaWO₄)3 samples, at most 5 grains
    • Cinabarit (HgS)2 samples, at most 4 grains
    • Kasiterit (SnO₂)2 samples, at most 5 grains
    • Gold (Au)1 sample, at most 1 grains

    Nearest samples with gold

    SampleGold in sampleFrom the water
    31121 grain760 m

    Rock-forming and accessory minerals

    • Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)131 samples, at most 815 grains
    • Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)52 samples, at most 4115 grains
    • Tourmalines (complex borosilicate)52 samples, at most 815 grains
    • Zirconium (ZrSiO₄)48 samples, at most 4115 grains
    • Pyroxény ((Mg,Fe,Ca)₂Si₂O₆)41 samples, at most 4115 grains
    • Korund (Al₂O₃)5 samples, at most 5 grains
    • Apatit (Ca₅(PO₄)₃(F,Cl,OH))5 samples, at most 55 grains
    • Staurolit (Fe₂Al₉Si₄O₂₃(OH))3 samples, at most 5 grains
    • Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))2 samples, at most 5 grains
    • Amfiboly (Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂)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-HCO328×
    • Ca-Mg-HCO315×
    • Ca-Mg-HCO3-SO410×
    • Ca-HCO3-SO43×
    • Ca-Mg-Na-HCO31×
    • Mg-Ca-HCO3-SO41×
    • Ca-Na-HCO3-SO41×

    Water quality class according to the hydrogeochemical map

    • class B31×
    • class A22×
    • class D4×
    • class C2×

    Metals in groundwater

    • AluminiumAlextreme (top 1 %)
      highest 0.350 mg/lmedian 0.0100 mg/l61 samples41 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 99 of all samples in Slovakia.

    • LeadPbextreme (top 1 %)
      highest 8.00 μg/lmedian 0.500 μg/l61 samples64 % below the limit of quantification

      Highest value: prameň1993, 230 m from the water. Comparison: percentile 99 of all samples in Slovakia.

    • AntimonySbhigh (top 5 %)
      highest 0.700 μg/lmedian 0.100 μg/l61 samples89 % below the limit of quantification

      Highest value: prameň1993, 2.5 km from the water. Comparison: percentile 95 of all samples in Slovakia.

    • LithiumLielevated (top 10 %)
      highest 45.0 μg/lmedian 7.00 μg/l61 samples16 % below the limit of quantification

      Highest value: prameň1993, 220 m from the water. Comparison: percentile 93 of all samples in Slovakia.

    • ChromiumCrslightly elevated
      highest 1.90 μg/lmedian 0.250 μg/l61 samples70 % below the limit of quantification

      Highest value: prameň1993, 2.1 km from the water. Comparison: percentile 89 of all samples in Slovakia.

    • SeleniumSeslightly elevated
      highest 1.50 μg/lmedian 0.500 μg/l61 samples97 % below the limit of quantification

      Highest value: prameň1993, 2.7 km from the water. Comparison: percentile 88 of all samples in Slovakia.

    • ArsenicAsslightly elevated
      highest 1.90 μg/lmedian 0.500 μg/l61 samples97 % below the limit of quantification

      Highest value: prameň1993, 2.9 km from the water. Comparison: percentile 88 of all samples in Slovakia.

    • CopperCuslightly elevated
      highest 3.20 μg/lmedian 0.600 μg/l61 samples

      Highest value: prameň1993, 320 m from the water. Comparison: percentile 85 of all samples in Slovakia.

    • ZincZntypical value
      highest 37.0 μg/lmedian 14.0 μg/l61 samples5 % below the limit of quantification

      Highest value: prameň1993, 510 m from the water. Comparison: percentile 54 of all samples in Slovakia.

    • IronFetypical value
      highest 0.00500 mg/lmedian 0.00500 mg/l26 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.9 km from the water. Comparison: percentile 50 of all samples in Slovakia.

    • CadmiumCdbelow half of Slovakia
      highest 0.250 μg/lmedian 0.250 μg/l61 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 47 of all samples in Slovakia.

    • MercuryHgbelow half of Slovakia
      highest 0.100 μg/lmedian 0.100 μg/l61 samples100 % below the limit of quantification

      Highest value: prameň1993, 2.6 km from the water. Comparison: percentile 46 of all samples in Slovakia.

    Radon in waters

    Type of siteSamplesHighest radonMedian
    source1622,1 Bq/l8.70 Bq/l
    stream, river11,04 Bq/l1.04 Bq/l
    developed spring22,68 Bq/l2.11 Bq/l

    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.

    79 boreholes in the 3 km zone, of which 14 hydrogeological and 65 other; with an archive report number 65.

    Borehole depths

    • up to 10 m72×
    • 10–30 m7×
    • 30–100 m0×
    • 100–300 m0×
    • over 300 m0×

    Nearest boreholes

    SiteTypeDepthArchive reportFrom the water
    VP-9engineering-geological4.0 m3323310 m
    VO-10engineering-geological6.0 m3323330 m
    VO-13engineering-geological5.5 m3323330 m
    VO-12engineering-geological5.5 m3323340 m
    Ruskénarrow-diameter borehole with ordinary drinking and process water9.6 m–50 m
    VP-8engineering-geological4.0 m3323350 m
    MV-18engineering-geological5.0 m3323350 m
    VO-18engineering-geological6.0 m3323350 m
    VO-2engineering-geological4.0 m3323350 m
    Ostrožnicawide-diameter borehole6.1 m–60 m
    V-1engineering-geological4.0 m1355960 m
    VO-1engineering-geological5.0 m3323360 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

    SourceTypeWater temperature (°C)Yield (l/s)CountNearest from water
    category a1mineral water< 15< 552.0 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

    LandfillAreaYear establishedMonitoringFrom the water
    Jalová – Stakčínska Roztoka60 m²1990–1.9 km
    Jalová – Stakčínska Roztoka75 m²1992–2.2 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

    • Landslides133×
    • Block fissures3×
    • Slope flows2×

    Degree of activity

    • Potenciálny135×
    • Stabilizovaný3×

    Current state

    • SD taken from archival materials, ktorá bola konfrontova65×
    • SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S62×
    • Processed only in the scope of registration on a scale of 1:25,0005×
    • SD prebraná z archívnych materiálov (existuje inž. geologick2×

    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.

    Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology.

    Organizations and location

    Who manages the fishing districts and where they are

    Organizations on the watercoursewho manages the fishing districts and what the conditions are there today

    1. OZ Košice2 fishing districts · 34 km31Vodárenská nádrž Starina32

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