On the Veľký potok (Sabinov) je jeden rybársky revír. stream Veľký potok (Sabinov) is salmonid (trout) fishing district no. 4-3170-4-1. It lies in Sabinov district (Prešov Region). The district is 13.9 km long. The district is managed by SRZ organization Sabinov Fishing rules, permits, the map and conditions at the water are on the fishing district's page. It belongs to the Bodrog and Hornád river basin. Open fishing district Veľký potok (Sabinov) Game fish of the district (2): Average activity · average of one fishing district 14:00–16:00 Veľký potok (Sabinov), window score 60. The score is an estimate of conditions based on weather, water and surroundings, not a bite forecast. Recalculated at 13:23. 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. 1 of 1 fishing district with measurements has 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. How the watercourse falls downstream: fall, gradient and water speed. Torrent A mountain stream with a steep gradient, cascades and a rocky bottom. The water is clear and cold; fishing requires a careful approach. 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. 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 (14 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 alluvium33% of the water line 33% young sediments, 33% flysch Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. Geological Map of Slovakia 1:50,000. pH 8.0modelled estimate water type Ca–Mg–HCO₃ Mineralisation 407 mg/l, hard water (14.4 °dH). Interpolation of measurements from the Geochemical Atlas of Slovakia, not a measurement in the stream. 0 from 15elements in the top 10 % highest: Chromium 95.9 mg/kg Position of the highest-ranked element among the sample points on streams in Slovakia: percentile 79. Interpolation of the Geochemical Atlas of river sediments. 42°C at 1,000 m depth heat flow 75 mW/m² At a depth of 2,000 m about 75 °C (increase of 33 °C per kilometre). Atlas of Geothermal Energy of Slovakia. 47nGy/h dose rate percentile 23 in Slovakia Natural background from rocks and soil (potassium, uranium, thorium), not a value measured at the water. Airborne gamma-ray spectrometry by ŠGÚDŠ. 0objects within 3 km No old mine working is recorded within 3 km of the water. 6samples with gold 13 ore minerals in the sediment Up to 3 grains in one sample (260 m from the water). Panning prospecting counted gold grains in a concentrate from river sediment. 0 from 10indicators in the top 5 % highest: Copper 5.00 μg/l Position of the highest measured value in the distribution of all surface water samples in Slovakia: percentile 91 (Ratvaj). 182boreholes within 3 km 518 water analyses nearby Of these, 182 have an archive report from Geofond. The boreholes are hydrogeological, geological, engineering-geological and other. – 10 geothermal and mineral water springs within 10 km. 9sites within 3 km 9 landfills No environmental burden is registered within 3 km; landfills are only recorded. 16records within 5 km 9 deposits, 7 ore occurrences Geofond registers, the metallogenetic map and the mineral resources map. 25areas within 3 km 2 active Documented landslides in the Geofond register. A landslide into a stream can cloud the water and change the bed. 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. Data: © ŠGÚDŠ (https://www.geology.sk), downloaded 8 Nov 2026. Details in the Methodology. 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: Gravelly and sandy bottom and floodplains; the water is replenished from groundwater in the alluvium. 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 3 of 6 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 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 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. -42nT range -50 to -26 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. -27mGal residual +3.4 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. 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 7.96typical 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. 14.4°dH, hard Sum of calcium and magnesium (2.58 mmol/l). Hard water is buffered and its pH changes more slowly; soft water is more sensitive to acid rain. 407mg/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) 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: Ratvaj2003, 810 m from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: Šarišské Michaľany, 480 m from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: Šarišské Michaľany2003, 480 m from the water. Comparison: percentile 90 of all samples in Slovakia. Highest value: Šarišské Michaľany2003, 480 m from the water. Comparison: percentile 84 of all samples in Slovakia. Highest value: Ratvaj2003, 810 m from the water. Comparison: percentile 83 of all samples in Slovakia. Highest value: Šarišské Michaľany2003, 480 m from the water. Comparison: percentile 82 of all samples in Slovakia. Highest value: Šarišské Michaľany2003, 480 m from the water. Comparison: percentile 75 of all samples in Slovakia. Highest value: Torysa1992, 750 m from the water. Comparison: percentile 62 of all samples in Slovakia. Highest value: Torysa1992, 750 m from the water. Comparison: percentile 46 of all samples in Slovakia. Highest value: Torysa1992, 750 m from the water. Comparison: percentile 32 of all samples in Slovakia. Basic water chemistry: which rocks the minerals in it come from. Highest value: Veľký potok – 522007, 40 m from the water. Comparison: percentile 33 of all samples in Slovakia. 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) Hydrogeochemical objects (analyses of springs and boreholes) and the geochemical atlas of groundwater (1996). Groundwater feeds streams, so its composition also affects the water in the stream. Highest value: vrt1992, 2.3 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1992, 2.9 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: prameň1992, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia. Highest value: studňa1992, 1.0 km from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 98 of all samples in Slovakia. Highest value: studňa1992, 800 m from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: studňa1992, 800 m from the water. Comparison: percentile 97 of all samples in Slovakia. Highest value: prameň1992, 130 m from the water. Comparison: percentile 96 of all samples in Slovakia. Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 95 of all samples in Slovakia. Highest value: studňa1992, 2.6 km from the water. Comparison: percentile 91 of all samples in Slovakia. Highest value: prameň1992, 660 m from the water. Comparison: percentile 88 of all samples in Slovakia. Highest value: prameň1992, 2.7 km from the water. Comparison: percentile 50 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. 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. 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. 42 / 75 °Cat depths of 1,000 and 2,000 m increase of 33 °C per km The line shows the rock temperature; the dotted part is only an extension to the surface. Heat flow 75 mW/m². marker on the bar: share among all sample points on streams in Slovakia 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. 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. 182 boreholes in the 3 km zone, of which 85 hydrogeological and 97 other; with an archive report number 182. 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. 47nGy/h in air range 42 to 57 nGy/h Natural background from rocks and soil; higher over granites and some acidic volcanic rocks, lower over limestones and floodplains. 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. 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 Radiohydrochemical sampling of springs, wells and watercourses: radon activity concentration in water. The bar shows the highest measured value for each kind of site. 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.
By the water now
The Veľký potok (Sabinov) watercourse at a glance
Today on the Veľký potok (Sabinov) watercourse
Is it worth going today? Fishing conditions score, the best window of the day and fishing districts from the best conditionsConditions score57 / 100Best window14:00Average of the watercourse's fishing districts
Best window today
Map and fishing districts of the Veľký potok (Sabinov) 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.Fishing districts1Length13,9 kmFish and catches on the Veľký potok (Sabinov) watercourse
Which fish live here and what has been caught? Game species recorded in the fishing districts and approved catches by anglersGame species2Game species recorded in the fishing district
Organizations and districts on the Veľký potok (Sabinov) watercourse
Who manages the fishing districts and where they areOrganisations1Districts1Organizations on the watercoursewho manages the fishing districts and what the conditions are there today
Water pollution on the Veľký potok (Sabinov) watercourse
Water quality according to SHMÚ, wastewater treatment plants near the fishing districts and groundwater nearbyDistricts failing a standard1 / 1Groundwater: measured valuestypical value from stations within 10 km, 2025
Highest nitrates
Watercourse profile from source to mouthnumber of unmet indicators in 2025 at SHMÚ sites
Show sites in the table (2)
Terrain and satellite images of the Veľký potok (Sabinov) watercourse
Elevation profile, 3D terrain of the surroundings and historical satellite imagesHighest point757 m n. m.Lowest point243 m n. m.Elevation profile of the watercourse
Terrain in 3D
Historical images
More watercourses near the Veľký potok (Sabinov) watercourse
The nearest rivers, streams and water bodies in the same river basinWatercourses6Geology and geochemistry of the Veľký potok (Sabinov) stream
Geology at a glance and a map of the zone
What lies beneath the water and around it? An overview in tiles, a map of mine workings, deposits, environmental burdens, boreholes and gold finds, and how to read the dataRock 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
Map of the corridor
How to read these data
Rocks, groundwater and landscape
What does the water flow over? Geological structure and age of the rocks, groundwater aquifers, relief, climate, soils and geophysical fieldsGeological structure beneath the water
Geological age of the rocks
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 1× Quaternary Pleistocene – Holocene deluvial-polygenetic sediments: clay-clay and sandy slope clays 1× flysch Eocene Strihovce and older Malcov Formations 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
Relief, climate and soils
Geomorphological units
Geomorphological regions
Climatic-geographical types
Susceptibility of soils to acidification
Soil contamination (map 1:500,000)
Lithogeochemical types
Geophysical fields: magnetics and gravity
Magnetic anomaly
Bouguer gravity anomaly
Chemistry of water and river sediments
What is in the water and on the bed? Trace elements and metals, nutrients, major ions, elements in sediments and groundwaterSurface water chemistry according to the atlas
Water acidity
Water hardness
Dissolved substances
Ionic composition of the water
Major ions
4.68 mg/lpercentile 7174.3 mg/lpercentile 6351.0 mg/lpercentile 620.136 mg/lpercentile 6017.5 mg/lpercentile 5811.2 mg/lpercentile 55228 mg/lpercentile 558.09 mg/lpercentile 46Nutrients and organic pollution
0.367 mg/lpercentile 817.21 mg/lpercentile 580.170 mg/lpercentile 562.88 mg/lpercentile 42Metals
9.94 μg/lpercentile 6541.5 μg/lpercentile 5763.3 μg/lpercentile 490.0446 mg/lpercentile 19Trace elements in surface waters
Major ions, mineralisation and pH
Elements in river sediments
Potentially toxic and trace elements
95.9 mg/kgpercentile 791.16 mg/kgpercentile 750.447 mg/kgpercentile 620.270 mg/kgpercentile 5522.8 mg/kgpercentile 410.140 mg/kgpercentile 382.12 mg/kgpercentile 270.135 mg/kgpercentile 174.24 mg/kgpercentile 155.71 mg/kgpercentile 1352.0 mg/kgpercentile 1263.3 mg/kgpercentile 110.0469 mg/kgpercentile 1113.1 mg/kgpercentile 68.17 mg/kgpercentile 5Major elements (iron, aluminium, calcium, magnesium, potassium, sodium, titanium, manganese, phosphorus)
1.30 %percentile 914,440 mg/kgpercentile 490.730 %percentile 301.41 %percentile 291.36 %percentile 274.99 %percentile 26606 mg/kgpercentile 19562 mg/kgpercentile 141.98 %percentile 10Further elements (barium, strontium, lithium, rubidium, zirconium, yttrium, cerium, boron, beryllium, gallium)
1.87 mg/kgpercentile 76438 mg/kgpercentile 6215.3 mg/kgpercentile 6158.8 mg/kgpercentile 4452.0 mg/kgpercentile 2476.2 mg/kgpercentile 2124.4 mg/kgpercentile 2121.6 mg/kgpercentile 2094.0 mg/kgpercentile 8317 mg/kgpercentile 8Groundwater: chemistry and water types
Chemical water types nearby
Water quality class according to the hydrogeochemical map
Metals in groundwater
Gold, mines and deposits
Was gold panned and ore mined here? Gold and ore minerals in river sediments, old mine workings, deposits and ore occurrencesSamples with gold6Gold and ore minerals in river sediments
Nearest samples with gold
Rock-forming and accessory minerals
Mine workings, deposits and ore occurrences
Deposits and mining areas
Geothermal energy, mineral waters and boreholes
Is there heat underground? Geothermal potential, geothermal boreholes by temperature, mineral springs and the borehole archiveBoreholes182Geothermal potential
Rock temperature with depth
Geothermal groundwater bodies beneath the water line
Geothermal energy and mineral waters
Sources of geothermal and mineral waters
Boreholes and Geofond archive reports
Borehole depths
Nearest boreholes
Natural radioactivity and radon
How much does the ground radiate here? Gamma radiation of rocks, radon in soil and radon in watersNatural radioactivity and radon
Gamma radiation dose rate
Radon risk of the bedrock
1.34 %percentile 636.58 ppm22th percentile2.20 ppm15th percentile1,289 Bq/m²percentile 37Radon risk by isopleths
Radon in waters
Environmental burdens, landfills and landslides
What in the surroundings can harm the water? Environmental burdens, waste landfills, anthropogenic sediments and slope deformationsBurdens and landfills9Landslides25Environmental burdens, landfills and anthropogenic sediments
Waste landfills
Landslides and slope deformations
Types of deformations
Degree of activity
Current state
57from 100
1445fishing districts
Map color
Loading map…
lowerhigher
Cations (positive ions)
Anions (negative ions)
CopperCuelevated (top 10 %)
highest 5.00 μg/lmedian 3.00 μg/l7 samples29 % below the limit of quantification
CadmiumCdelevated (top 10 %)
highest 0.300 μg/lmedian 0.300 μg/l7 samples14 % below the limit of quantification
LeadPbelevated (top 10 %)
highest 4.00 μg/lmedian 4.00 μg/l7 samples29 % below the limit of quantification
LithiumLislightly elevated
highest 20.0 μg/lmedian 10.0 μg/l7 samples29 % below the limit of quantification
BariumBaslightly elevated
highest 80.0 μg/lmedian 50.0 μg/l7 samples
AntimonySbslightly elevated
highest 1.00 μg/lmedian 1.00 μg/l7 samples29 % below the limit of quantification
ArsenicAsslightly elevated
highest 2.00 μg/lmedian 1.00 μg/l7 samples29 % below the limit of quantification
StrontiumSrtypical value
highest 240 μg/lmedian 240 μg/l1 sample
SeleniumSebelow half of Slovakia
highest 0.500 μg/lmedian 0.500 μg/l2 samples100 % below the limit of quantification
ChromiumCrbelow half of Slovakia
highest 1.00 μg/lmedian 1.00 μg/l2 samples100 % below the limit of quantification
Silicon dioxideSiO2below half of Slovakia
highest 8.04 mg/lmedian 6.80 mg/l2 samples
SeleniumSeextreme (top 1 %)
highest 8.00 μg/lmedian 0.500 μg/l39 samples92 % below the limit of quantification
AluminiumAlextreme (top 1 %)
highest 0.560 mg/lmedian 0.00500 mg/l39 samples67 % below the limit of quantification
MercuryHgextreme (top 1 %)
highest 0.900 μg/lmedian 0.100 μg/l39 samples79 % below the limit of quantification
AntimonySbhigh (top 5 %)
highest 2.90 μg/lmedian 0.100 μg/l39 samples82 % below the limit of quantification
ChromiumCrhigh (top 5 %)
highest 8.40 μg/lmedian 0.250 μg/l39 samples59 % below the limit of quantification
LithiumLihigh (top 5 %)
highest 90.0 μg/lmedian 11.0 μg/l39 samples10 % below the limit of quantification
LeadPbhigh (top 5 %)
highest 5.00 μg/lmedian 0.500 μg/l39 samples54 % below the limit of quantification
CadmiumCdhigh (top 5 %)
highest 0.900 μg/lmedian 0.250 μg/l39 samples97 % below the limit of quantification
ZincZnhigh (top 5 %)
highest 1,390 μg/lmedian 14.0 μg/l39 samples15 % below the limit of quantification
CopperCuelevated (top 10 %)
highest 4.20 μg/lmedian 0.700 μg/l39 samples
ArsenicAsslightly elevated
highest 1.90 μg/lmedian 0.500 μg/l39 samples87 % below the limit of quantification
IronFetypical value
highest 0.00500 mg/lmedian 0.00500 mg/l7 samples100 % below the limit of quantification
TP-4456
1 grain
60 m
TP-4453
2 grains
70 m
1381
3 grains
260 m
1388
1 grain
630 m
1383
3 grains
660 m
1385
3 grains
890 m
Šarišské Michaľany
2.8 km
Orkucany
2.9 km
Orkucany – Buchanec
3.3 km
Ražňany
3.5 km
Hubošovce
4.2 km
Hubošovce
4.2 km
Gregorovce
4.5 km
Gregorovce
4.6 km
Mošurov
4.8 km
category a1
1.1 km
category b1
7.4 km
Šarišské Sokolovce
40 m
Uzovce
100 m
Šarišské Sokolovce
130 m
M-2
150 m
Veľký Šariš
180 m
Kráľova Lehota
270 m
Veľký Šariš
310 m
Veľký Šariš
340 m
Veľký Šariš
440 m
M-1
510 m
Veľký Šariš
600 m
Šarišská Poruba
620 m
Veľký Śariš – Veľký Šariš
1.5 km
Veľký Šariš – landfill TKO – Veľký Šariš
1.5 km
Šarišská Trstená – Jama PD – Šarišské Michaľany
1.7 km
Veľký Śariš – Veľký Šariš
2.2 km
Pod Makom – Gregorovce
2.4 km
Fintice – landfill v bani – Fintice
2.6 km
TKO Ražňany – Gregorovce
2.6 km
Nemcovce
2.8 km