Fishing conditions score, the best window of the day and fishing districts from the best conditions Low activity · average of 3 fishing districts Most fishing districts have their best window around 15:00. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 16:04. 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 Move the map with two fingers. In full-screen mode one finger is enough. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. For each fishing district you can see what it is made of, how well it is supported by data and where the data comes from. Measurement of water level, temperature and flow, weather by the watercourse and status from satellites How the watercourse falls downstream: fall, gradient and water speed. Fast watercourse Podhorský potok: fast water, stony bottom, riffles and the pools below them. Typical trout waters. Source: Open Topo Data (eudem25m), 4 Nov 2026. Gradient and fall are approximate and include only the sections of fishing districts. Loading the 3D terrain model… Changes in the surroundings and nature from 2019 to 2025: how the banks, vegetation and landscape around the water change. The images switch automatically; you can also browse them by hand. Orthophoto mosaic of Slovakia © GKÚ Bratislava, NLC Zvolen. The year and day of imaging depend on the location, so individual years may differ in season and weather. Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearby 0 of 3 of the watercourse's fishing districts with SHMÚ data have an unmet standard at the nearest site in at least one indicator. 0 of 2 fishing districts with measurements have groundwater nearby with a value above the limit for at least one indicator. Water pollution in the Hornád basinPolluted water in Slovakia 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. 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 (27 km of line in total): stream samples within 1 km, boreholes, mine workings and burdens within 3 km, ore occurrences within 5 km, geothermal sources within 10 km. River alluvium63% of the water line 25% flysch, 13% young sediments Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000. pH 8.4modelled estimate water type Ca–Mg–HCO₃ Mineralisation 510 mg/l, hard water (17.3 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 7 from 15elements in the top 10 % highest: Nickel 56.2 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 95. Interpolation of the Geochemical Atlas of river sediments. 36°C at 1,000 m depth heat flow 65 mW/m² At a depth of 2,000 m about 65 °C (increase of 29 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 46nGy/h dose rate percentile 21 in Slovakia Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ. 10objects within 3 km Nearest: odkalisko Rudňany (odkalisko), 1.7 km from the water. 2samples with gold 14 ore minerals in the sediment Up to 1 grain in one sample (50 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment. 5 from 10indicators in the top 5 % highest: Copper 518 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 99 (700m Z od K538). 300boreholes within 3 km 839 water analyses nearby Of these, 298 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. 31°C at the wellhead 3 geothermal boreholes within 10 km Warmest: Arnutovce – HKJ-3, yield 11.8 l/s, 6.4 km from the water. 37sites within 3 km 1 environmental burden, 36 landfills Nearest burden: Spišská Nová Ves – rušňové depo, 2.9 km from the water. Proximity does not mean that substances leak from the site into the water. 81records within 5 km 18 deposits, 63 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 39areas within 3 km 1 active Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed. Which rock lies beneath the water line (Geological Map of Slovakia 1:50,000), how old it is, how thick the Quaternary cover is and in which tectonic unit the water flows. The bedrock decides the hardness of the water, the bottom, the turbidity after rain and the abundance of springs. The points follow the water line (for a stream and a basin, fishing district after fishing district). The strip is a cross-section by distance, not a map; the width of a section corresponds to the number of points. marker on the bar: share among all sample points on streams in Slovakia River alluvium: Štrkové a piesčité dno a nivy; voda sa dopĺňa z podzemnej vody v náplavoch. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia The map covers 8 of 10 points on the water line. Streams and rivers are fed by groundwater. Hydrogeological maps show in which rocks the water is stored, how permeable they are and what the water in them is like. The data come from ŠGÚDŠ maps, not from measurements at a particular water. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia 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. pH 8.37typical 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. 17.3°dH, hard Sum of calcium and magnesium (3.09 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 510mg/l mineralisation Total amount of dissolved minerals. Clean mountain water has tens of mg/l, lowland and limestone waters hundreds. Water type by dominant ions: Ca–Mg–HCO₃ Shares are in equivalents, the usual way of comparing the composition of waters. dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile) The Geochemical Atlas of Slovakia (river sediments) describes what the river carries in the fine material on its bed. Sediment collects metals from rocks, ore occurrences and past mining and industry. It is not a legal limit or a health risk assessment: it shows how an element on this stream ranks among streams in Slovakia. dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile) 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. 46nGy/h in air range 45 to 55 nGy/h Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains. medium Radon is a natural gas from rocks. The risk concerns buildings and cellars, not the water in the stream; it shows what the bedrock is like. dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile) marker on the bar: share among all sample points on streams in Slovakia 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. -29nT range -55 to -18 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. -33mGal residual +1.0 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. 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. 36 / 65 °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 65 mW/m². marker on the bar: share among all sample points on streams in Slovakia A basin is not just water: slope and elevation determine the speed of runoff, climate the temperature and amount of water, and soils what is washed into the stream. The data come from the geomorphological division, climatic-geographical types and soil maps of ŠGÚDŠ. marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia marker on the bar: share among all sample points on streams in Slovakia 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. Arsenic, antimony, cadmium, lead, copper, zinc and other elements in samples from rivers and streams (Geochemical Atlas of Slovakia, surface waters, 2015). The bar shows where the highest value lies among all samples in Slovakia; the light marker is the median of the samples at this water. Highest value: 700m Z od K538, 1993, 530 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: Levočský potok, 50 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: Levočský potok, 1992, 60 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: Markušovce, 2000, 860 m from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: Markušovce, 2000, 860 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: Markušovce, 2000, 860 m from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: Hornád, 1992, 920 m from the water. Comparison: percentile 94 of all samples in Slovakia. Highest value: Hornád, 1992, 920 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: 800m S od K613 Lúč, 1993, 990 m from the water. Comparison: percentile 78 of all samples in Slovakia. Highest value: Odorica, potok, 1992, 140 m from the water. Comparison: percentile 46 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Odorica, potok, 1992, 140 m from the water. Comparison: percentile 73 of all samples in Slovakia. Regional panning prospecting: the heavy fraction was washed out of river gravel and the mineral grains in it were counted. The map of finds is positive: a sample without gold is not listed in the atlas, so the absence of a find is not proof that there is no gold. 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. Highest value: studňa, 1993, 1.1 km from the water. Comparison: percentile 100 of all samples in Slovakia. Highest value: studňa, 1993, 110 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň, 1992, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa, 1992, 450 m from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň, 1992, 1.9 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa, 1993, 1.1 km from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: studňa, 1993, 2.7 km from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: vrt, 1992, 540 m from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: studňa, 1993, 2.7 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa, 1993, 2.3 km from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa, 1992, 580 m from the water. Comparison: percentile 93 of all samples in Slovakia. Highest value: prameň, 1992, 2.2 km from the water. Comparison: percentile 50 of all samples in Slovakia. 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. 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. 300 boreholes in the 3 km zone, of which 139 hydrogeological and 161 other; with an archive report number 298. 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. Recorded environmental burdens (industrial sites, landfills, mining), the register of waste landfills and monitoring of anthropogenic sediments (industrial sludge). It is a list of places, not a measurement of water pollution. Register of documented slope deformations (Geofond). Landslides by a stream can bring fine material into the water, change the bed and dam the channel. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. Who manages the fishing districts and where they are Bodrog basin and Hornád
By the water now
Today on the Levočský potok watercourse
Average of the watercourse's fishing districts
When the best window ishow many fishing districts have their best two-hour window in a given hour
Map and fishing districts of the watercourse
Water state on the watercourse
Water levels on the watercourse
Station Status Change Temperature Markušovce 34 cm – Elevation profile of the watercourse
Terrain in 3D
Historical images
Water pollution on the Levočský potok watercourse
Surface water near the fishing districtsnearest SHMÚ monitoring site, 2025
Groundwater: measured valuestypical value from stations within 10 km, 2025
Geology and geochemistry of the Levočský potok stream
Rock under the water
Water according to the atlas
Elements in river sediment
Heat underfoot
Natural gamma radiation
Old mine workings
Gold in river sediment
Trace elements in the stream water
Boreholes and groundwater analyses
Geothermal energy
Environmental burdens and landfills
Deposits and ore occurrences
Landslides and slope deformations
Geological structure beneath the water
Geological age of the rocks
Most common rock units
System Age Unit Points kvartér holocén fluviálne sedimenty: litofaciálne nečlenené nivné hliny, alebo piesčité až štrkovité hliny dolinných nív a nív 5× paleogén oligocén – miocén bielopotocké súvrstvie 2× kvartér pleistocén – holocén deluviálne sedimenty vcelku: litofaciálne nerozlíšené svahoviny a sutiny 1× Quaternary cover
Tectonic division
Neotectonic units
Direction of neotectonic movements
Regional geological division
Regional geological division (subunits)
Engineering-geological districts
Engineering-geological formations
Susceptibility of the area to slope deformations
Hydrogeology: aquifers and groundwater
Aquifer rocks (hydrogeological map 1:200,000)
Aquifer type
Type of permeability (basic hydrogeological map 1:50,000)
Hydrogeological function
Main hydrogeological region
Genetic type of groundwater
Chemical type of groundwater
Groundwater quality class
Geothermal groundwater bodies
Surface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
73.2 mg/lpercentile 7885.0 mg/lpercentile 7523.5 mg/lpercentile 745.11 mg/lpercentile 74279 mg/lpercentile 7118.1 mg/lpercentile 6612.4 mg/lpercentile 630.116 mg/lpercentile 51Nutrients and organic pollution
0.482 mg/lpercentile 8011.6 mg/lpercentile 783.50 mg/lpercentile 570.0431 mg/lpercentile 22Metals
522 μg/lpercentile 950.327 mg/lpercentile 8662.5 μg/lpercentile 686.53 μg/lpercentile 49Elements in river sediments
Potentially toxic and trace elements
56.2 mg/kgpercentile 95140 mg/kgpercentile 9520.2 mg/kgpercentile 951.88 mg/kgpercentile 951.11 mg/kgpercentile 957.23 mg/kgpercentile 950.982 mg/kgpercentile 94171 mg/kgpercentile 8513.9 mg/kgpercentile 84101 mg/kgpercentile 820.423 mg/kgpercentile 800.236 mg/kgpercentile 6113.6 mg/kgpercentile 386.96 mg/kgpercentile 2656.1 mg/kgpercentile 20Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1.13 %percentile 83835 mg/kgpercentile 491.47 %percentile 44747 mg/kgpercentile 361.57 %percentile 354,074 mg/kgpercentile 345.05 %percentile 280.714 %percentile 282.27 %percentile 25Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
69.1 mg/kgpercentile 73466 mg/kgpercentile 71493 mg/kgpercentile 6832.9 mg/kgpercentile 6762.5 mg/kgpercentile 6287.2 mg/kgpercentile 4626.6 mg/kgpercentile 441.02 mg/kgpercentile 29108 mg/kgpercentile 2310.2 mg/kgpercentile 21Natural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.32 %percentile 582.33 ppm23th percentile6.32 ppm15th percentile1,105 Bq/m²percentile 24Radon risk by isopleths
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Geothermal potential
Rock temperature with depth
Geothermal groundwater bodies beneath the water line
Relief, climate and soils
Geomorphological units
Geomorphological regions
Climatic-geographical types
Susceptibility of soils to acidification
Soil contamination (map 1:500,000)
Lithogeochemical types
Map of the corridor
Trace elements in surface waters
Major ions, mineralisation and pH
Gold and ore minerals in river sediments
Nearest samples with gold
Sample Gold in sample From the water 2970 1 grain 50 m TP-2932 1 grain 100 m Rock-forming and accessory minerals
Groundwater: chemistry, water types and radioactivity
Chemical water types nearby
Water quality class according to the hydrogeochemical map
Metals in groundwater
Radon in waters
Type of site Samples Highest radon Median prameň 19 28,4 Bq/l 2.10 Bq/l vrt s prelivom 1 0,900 Bq/l 0.900 Bq/l studňa 1 2,30 Bq/l 2.30 Bq/l upravený prameň 7 31,0 Bq/l 4.80 Bq/l vodný zdroj pre hromadné zásobovanie 1 11,1 Bq/l 11.1 Bq/l vodný zdroj pre individuálne zásobovanie 3 15,6 Bq/l 8.04 Bq/l potok, rieka 1 1,34 Bq/l 1.34 Bq/l Mine workings, deposits and ore occurrences
Types of mining objects
Nearest old mine workings
Name Type Mined Ended From the water odkalisko Rudňany odkalisko 1.7 km Halda štôlne RŠT-1 halda vápence 1975 1.8 km Štôlňa RŠT-1 štôlňa vápence 1975 1.9 km Halda štôlne RŠT-2 halda vápence 1975 1.9 km Štôlňa RŠT-2 štôlňa vápence 1975 2.0 km Štôlňa RŠT-1 štôlňa vápence 1975 2.0 km Halda štôlne RŠT-3 halda vápence 1975 2.1 km Štôlňa RŠT-3 štôlňa vápence 1975 2.1 km Štôlňa RŠT-2 štôlňa vápence 1975 2.2 km Štôlňa RŠT-3 štôlňa vápence 1975 2.4 km Deposits and mining areas
Deposit Mineral Status and organisation From the water Baláž I štrkopiesky a piesky Ložisko so zastavenou ťažbou alebo na ktorom sa nepredpokladá využívanie zásob – Ing. Babej Jozef B-Gas 120 m Levoča – Baláž štrkopiesky a piesky Ložisko so zastavenou ťažbou alebo na ktorom sa nepredpokladá využívanie zásob – MATRIXSLOVAKIASERVIS, s.r.o. 250 m Markušovce I barit Ložisko so zastavenou ťažbou alebo na ktorom sa nepredpokladá využívanie zásob – RIS, a.s. 1.6 km Markušovce I barit Ložisko so zastavenou ťažbou alebo na ktorom sa nepredpokladá využívanie zásob – RIS, a.s. 1.8 km Markušovce I barit Ložisko so zastavenou ťažbou alebo na ktorom sa nepredpokladá využívanie zásob – RIS, a.s. 1.8 km Markušovce vápenec vysokopercentný Ťažené ložisko – VSK MINERAL s.r.o. 2.3 km Markušovce vápenec vysokopercentný Ťažené ložisko – VSK MINERAL s.r.o. 2.3 km Odorín vápnitý slieň Ložisko s predpokladom využívania zásob – ŠGÚDŠ Bratislava 2.5 km Rudňany stavebný kameň Ložisko so zastavenou ťažbou alebo na ktorom sa nepredpokladá využívanie zásob – DOPRAVEX kameňolomy, s. r. o. 2.9 km Spišský Hrhov stavebný kameň Ložisko so zastavenou ťažbou alebo na ktorom sa nepredpokladá využívanie zásob – DOPRAVEX kameňolomy, s. r. o. 3.4 km Matejovce nad Hornádom sadrovec Ložisko s predpokladom využívania zásob – ŠGÚDŠ Bratislava 3.8 km Matejovce nad Hornádom anhydrit Ložisko s predpokladom využívania zásob – ŠGÚDŠ Bratislava 3.8 km Ore occurrences in the metallogenic map
Occurrence Ore type Metals Type From the water Markušovce Hliníkové rudy (bauxity) Al ložiskový výskyt 1.9 km Matejovce nad Hornádom Uránovo-molybdénové rudy Cu, U, Mo ložiskový výskyt 2.5 km Rudňany – Severná žila Komplexné železné rudy Fe, Cu malé ložisko 3.6 km Závadka pri Nálepkove, Stožky Železné rudy Fe mineralogický výskyt 3.8 km Závadka pri Nálepkove, Slivníky Medené rudy Cu, U mineralogický výskyt 4.0 km Chrásť nad Hornádom Hliníkové rudy (bauxity) Al mineralogický výskyt 4.0 km Rudňany Komplexné železné rudy Fe, Cu, barit malé ložisko 4.2 km Chrasť nad Hornádom, žily Ján, Lendava a Miloj Komplexné železné rudy Fe, Cu ložiskový výskyt 4.2 km Rudňany – Matej a Jakub žila Komplexné železné rudy Fe, Cu malé ložisko 4.3 km Hnilčík, žily Izabela, Farský grund a Baniská Komplexné železné rudy Fe, Cu ložiskový výskyt 4.3 km Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Site Type Depth Archive report From the water Harichovce pozorovací vrt SHMÚ 6.6 m 21365 114Aa6.pdf10 m JV 16-02 inžiniersko-geologický 5.0 m 8765420 m Levočská dolina úzkoprofilový vrt s obyčajnou pitnou a úžitkovou vodou 150.2 m 66203 102Cc29.pdf40 m Levočské Lúky úzkoprofilový vrt s obyčajnou pitnou a úžitkovou vodou 6.7 m 13672 114Aa17.pdf40 m Levoča širokoprofilový vrt – 64931 102Cc23.pdf40 m Levočské Lúky úzkoprofilový vrt s obyčajnou pitnou a úžitkovou vodou 9.2 m 13672 114Aa19.pdf50 m BK-VMr-30 ložiskový 8.8 m 1289250 m Levočská dolina úzkoprofilový vrt s obyčajnou pitnou a úžitkovou vodou 80.9 m 66203 102Cc31.pdf60 m BK-VMr-27 ložiskový 7.4 m 1289270 m V-2 inžiniersko-geologický 4.5 m 8723070 m Levoča 43.0 m 71466 102Cc39.pdf80 m BK-VMr-29 ložiskový 8.2 m 1289280 m Geothermal energy and mineral waters
Borehole Temperature Yield Depth Chemical water type Use From the water Danišovce – DH-1 – 0.1 l/s 1000 m – nevyužívaný 2.5 km Arnutovce – HKJ-3 31 °C 11.8 l/s 1133 m Ca-Mg-HCO3 nevyužívaný 6.4 km Letanovce – HKJ-4 25 °C 8.0 l/s 607 m Ca-Mg-HCO3 nevyužívaný 8.7 km Sources of geothermal and mineral waters
Source Type Water temperature (°C) Yield (l/s) Count Nearest from water kategória a1 minerálna voda < 15 < 5 10 480 m HKJ-3 geotermálna voda 22 – 38 5 – 15 1 6.1 km Environmental burdens, landfills and anthropogenic sediments
Environmental burdens
Site Activity Substance Classification From the water Spišská Nová Ves – rušňové depo SK2004900F 2.9 km Waste landfills
Landfill Area Year established Monitoring From the water Markušovce 210 m² 1985 – 30 m Levoča 300 m² 1985 – 50 m Levočské Lúky – Levoča 500 m² 1993 – 120 m Levoča 400 m² 1992 – 130 m Levoča 1 000 m² 1989 – 160 m Levočská dolina – Levoča 2 500 m² 1987 – 160 m Levoča 60 m² 1992 – 210 m Lieskovany 100 m² 1990 – 250 m Landslides and slope deformations
Types of deformations
Degree of activity
Current state
How to read these data
Organizations and location
Organizations on the watercoursewho manages the fishing districts and what the conditions are there today
More watercourses nearby
22from 100
1445fishing districts
Map color
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lowerhigher
Cations (positive ions)
Anions (negative ions)
CopperCuextreme (top 1 %)
highest 518 μg/lmedian 1.80 μg/l27 samples19 % below the limit of quantification
CadmiumCdextreme (top 1 %)
highest 2.10 μg/lmedian 0.250 μg/l27 samples7 % below the limit of quantification
ChromiumCrhigh (top 5 %)
highest 13.1 μg/lmedian 3.80 μg/l27 samples
AntimonySbhigh (top 5 %)
highest 16.0 μg/lmedian 0.500 μg/l27 samples59 % below the limit of quantification
LeadPbhigh (top 5 %)
highest 5.00 μg/lmedian 2.50 μg/l27 samples96 % below the limit of quantification
ArsenicAselevated (top 10 %)
highest 6.00 μg/lmedian 0.500 μg/l27 samples56 % below the limit of quantification
StrontiumSrelevated (top 10 %)
highest 610 μg/lmedian 280 μg/l27 samples
LithiumLielevated (top 10 %)
highest 31.0 μg/lmedian 16.0 μg/l27 samples
BariumBaslightly elevated
highest 70.0 μg/lmedian 40.0 μg/l27 samples
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l27 samples100 % below the limit of quantification
Silicon dioxideSiO2typical value
highest 17.3 mg/lmedian 8.57 mg/l27 samples
LithiumLiextreme (top 1 %)
highest 590 μg/lmedian 17.5 μg/l64 samples5 % below the limit of quantification
SeleniumSeextreme (top 1 %)
highest 9.60 μg/lmedian 0.500 μg/l64 samples84 % below the limit of quantification
MercuryHgextreme (top 1 %)
highest 1.00 μg/lmedian 0.100 μg/l64 samples89 % below the limit of quantification
AntimonySbextreme (top 1 %)
highest 8.90 μg/lmedian 0.100 μg/l64 samples67 % below the limit of quantification
AluminiumAlextreme (top 1 %)
highest 0.210 mg/lmedian 0.00750 mg/l64 samples50 % below the limit of quantification
LeadPbhigh (top 5 %)
highest 7.00 μg/lmedian 0.500 μg/l64 samples63 % below the limit of quantification
ChromiumCrhigh (top 5 %)
highest 8.50 μg/lmedian 0.250 μg/l64 samples56 % below the limit of quantification
CadmiumCdhigh (top 5 %)
highest 1.20 μg/lmedian 0.250 μg/l64 samples97 % below the limit of quantification
CopperCuhigh (top 5 %)
highest 8.10 μg/lmedian 0.700 μg/l64 samples
ZincZnhigh (top 5 %)
highest 1,540 μg/lmedian 5.00 μg/l64 samples34 % below the limit of quantification
ArsenicAselevated (top 10 %)
highest 3.20 μg/lmedian 0.500 μg/l64 samples92 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l27 samples100 % below the limit of quantification
