VN Kežmarok

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.

• Flysch100%SR 4.7 %

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

Flysch: Alternating sandstones and claystones; moderately mineralised water that turns turbid quickly in rain.

Geological age of the rocks

• Paleogene100%

Most common rock units

Tectonic division

• NEOALPÍNSKE TEKTONICKÉ ŠTRUKTÚRY ZÁPADNÝCH KARPÁT100%SR 84 %

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

Neotectonic units

• negative unit (intermountain basins)100%SR 14 %

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

Direction of neotectonic movements

• very small subsidence100%SR 7.3 %

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

Regional geological division

• Inner Carpathian Paleogene100%SR 11 %

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

Regional geological division (subunits)

• Poprad Basin100%SR 1.4 %

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

Engineering-geological districts

• region of flyschoid rocks100%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 areas100%SR 95 %

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

The map covers 1 of 1 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)

• Gravel100%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 (Gravel)100%SR 22 %

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

Type of permeability (basic hydrogeological map 1:50,000)

• fissure100%SR 12 %

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

Hydrogeological function

• aquifer100%SR 95 %

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

Main hydrogeological region

• kryštalinikum časti Vysokých Tatier a kvartér ich predpolia100%SR 1.2 %

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

Geothermal groundwater bodies

• Levoča Basin – W and S part100%SR 9.5 %

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.

Ionic composition of the water

Water type by dominant ions: Ca–Mg–HCO₃

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

Major ions

• ChloridesCl7.58 mg/lpercentile 46
• FluoridesF0.105 mg/lpercentile 45
• SodiumNa5.83 mg/lpercentile 33
• PotassiumK1.70 mg/lpercentile 25
• SulphatesSO422.6 mg/lpercentile 21
• MagnesiumMg7.20 mg/lpercentile 21
• BicarbonatesHCO394.7 mg/lpercentile 17
• CalciumCa26.6 mg/lpercentile 16

dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile)

Nutrients and organic pollution

• AmmoniumNH40.387 mg/lpercentile 82
• PhosphatesPO40.269 mg/lpercentile 66
• Chemical oxygen demandChSK3.91 mg/lpercentile 65
• NitratesNO30.862 mg/lpercentile 1

Metals

• IronFe0.237 mg/lpercentile 79
• AluminiumAl182 μg/lpercentile 77
• ZincZn13.5 μg/lpercentile 75
• ManganeseMn60.2 μg/lpercentile 67

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

• MolybdenumMo0.840 mg/kgpercentile 91
• TinSn4.41 mg/kgpercentile 86
• ZincZn155 mg/kgpercentile 82
• NickelNi33.4 mg/kgpercentile 78
• AntimonySb1.16 mg/kgpercentile 75
• SeleniumSe0.343 mg/kgpercentile 70
• LeadPb18.4 mg/kgpercentile 64
• CopperCu26.3 mg/kgpercentile 61
• ChromiumCr77.2 mg/kgpercentile 58
• BismuthBi0.231 mg/kgpercentile 56
• ArsenicAs6.71 mg/kgpercentile 51
• MercuryHg0.104 mg/kgpercentile 51
• VanadiumV67.8 mg/kgpercentile 49
• CadmiumCd0.176 mg/kgpercentile 48
• CobaltCo6.09 mg/kgpercentile 16

dot: average along the water line, line: from the lowest to the highest value, scale: position among sample points on streams in Slovakia (0 to 100th percentile)

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.

• Potassium (K)K1.53 %percentile 86
• Equivalent uranium (eU)eU2.62 ppm57th percentile
• Equivalent thorium (eTh)eTh7.55 ppm57th 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 137CsCS1371,349 Bq/m²percentile 41

Radon risk by isopleths

• medium100%SR 64 %

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

Geophysical fields: magnetics and gravity

Maps of the magnetic field and gravity (ŠGÚDŠ) reveal what lies beneath the sediments and the surface: volcanic bodies, faults and crustal thickness. For an angler they are interesting indirectly: they show where the bedrock changes, and with it the water.

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.

Geothermal groundwater bodies beneath the water line

• Levoča Basin – W and S part100%SR 9.5 %

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

Relief, climate and soils

A basin is not just water: slope and elevation determine the speed of runoff, climate the temperature and amount of water, and soils what is washed into the stream. The data come from the geomorphological division, climatic-geographical types and soil maps of ŠGÚDŠ.

• Elevation of geomorphological units (from–to)555–771m a.s.l.
• Average elevation of the units650m a.s.l.
• Average slope3.4°
• Average January temperature-4.8°C
• Average July temperature16.5°C
• Annual precipitation725mm

Geomorphological units

• Sub-Tatra Basin100%SR 3.9 %

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

Geomorphological regions

• Fatra–Tatra area100%SR 21 %

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

Climatic-geographical types

• basin climate100%SR 29 %

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

Susceptibility of soils to acidification

• soils susceptible to acidification100%SR 31 %

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

Lithogeochemical types

• Inner Carpathian Paleogene100%SR 11 %

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

Map of the corridor

Where the nearest mine workings, deposits, burdens, geothermal boreholes and gold finds are. Groups can be switched off.

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.

• LithiumLiextreme (top 1 %)
  highest 180 μg/lmedian 180 μg/l1 sample
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: Kežmarok2002, 80 m from the water. Comparison: percentile 99 of all samples in Slovakia.

• ArsenicAselevated (top 10 %)
  highest 6.00 μg/lmedian 6.00 μg/l1 sample
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: Kežmarok2002, 80 m from the water. Comparison: percentile 95 of all samples in Slovakia.

• CadmiumCdelevated (top 10 %)
  highest 0.300 μg/lmedian 0.300 μg/l1 sample
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: Kežmarok, 80 m from the water. Comparison: percentile 90 of all samples in Slovakia.

• LeadPbelevated (top 10 %)
  highest 4.00 μg/lmedian 4.00 μg/l1 sample
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: Kežmarok2002, 80 m from the water. Comparison: percentile 90 of all samples in Slovakia.

• AntimonySbslightly elevated
  highest 1.00 μg/lmedian 1.00 μg/l1 sample
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: Kežmarok2002, 80 m from the water. Comparison: percentile 82 of all samples in Slovakia.

• CopperCutypical value
  highest 2.00 μg/lmedian 2.00 μg/l1 sample
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: Kežmarok2002, 80 m from the water. Comparison: percentile 66 of all samples in Slovakia.

• BariumBabelow half of Slovakia
  highest 30.0 μg/lmedian 30.0 μg/l1 sample
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: Kežmarok2002, 80 m from the water. Comparison: percentile 37 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)3 samples, at most 5 grains
• Ilmenit (FeTiO₃)3 samples, at most 4115 grains
• Pyrite (FeS₂)3 samples, at most 5 grains
• Anatas (TiO₂)2 samples, at most 55 grains
• Magnetite (Fe₃O₄)2 samples, at most 155 grains
• Rutil (TiO₂)2 samples, at most 315 grains
• Limonite (FeO(OH)·nH₂O)1 sample, at most 55 grains

Rock-forming and accessory minerals

• Spinel (Cr-spinel) ((Mg,Fe)(Al,Cr)₂O₄)4 samples, at most 315 grains
• Epidot (Ca₂(Al,Fe)₃Si₃O₁₂(OH))2 samples, at most 815 grains
• Granáty ((Fe,Mg,Ca,Mn)₃Al₂Si₃O₁₂)2 samples, at most 1815 grains
• Tourmalines (complex borosilicate)2 samples, at most 5 grains
• Zirconium (ZrSiO₄)2 samples, at most 315 grains

Groundwater: chemistry, water types and radioactivity

Hydrogeochemical objects (analyses of springs and boreholes), the geochemical atlas of groundwater (1996) and radiohydrochemical sampling. Groundwater feeds streams, so its composition also affects the water in the stream.

Metals in groundwater

• CadmiumCdextreme (top 1 %)
  highest 18.0 μg/lmedian 0.250 μg/l14 samples86 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: prameň1992, 2.9 km from the water. Comparison: percentile 99 of all samples in Slovakia.

• LithiumLihigh (top 5 %)
  highest 121 μg/lmedian 17.0 μg/l14 samples
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: vrt1992, 2.2 km from the water. Comparison: percentile 99 of all samples in Slovakia.

• ChromiumCrhigh (top 5 %)
  highest 7.50 μg/lmedian 0.250 μg/l14 samples57 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: prameň1992, 960 m from the water. Comparison: percentile 97 of all samples in Slovakia.

• AluminiumAlhigh (top 5 %)
  highest 0.130 mg/lmedian 0.0100 mg/l14 samples43 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: prameň1992, 960 m from the water. Comparison: percentile 97 of all samples in Slovakia.

• AntimonySbhigh (top 5 %)
  highest 0.900 μg/lmedian 0.350 μg/l14 samples29 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: prameň1992, 2.2 km from the water. Comparison: percentile 95 of all samples in Slovakia.

• MercuryHghigh (top 5 %)
  highest 0.200 μg/lmedian 0.100 μg/l14 samples86 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: prameň1992, 2.3 km from the water. Comparison: percentile 95 of all samples in Slovakia.

• LeadPbelevated (top 10 %)
  highest 2.00 μg/lmedian 0.500 μg/l14 samples93 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: prameň1992, 2.3 km from the water. Comparison: percentile 90 of all samples in Slovakia.

• SeleniumSeslightly elevated
  highest 1.40 μg/lmedian 0.500 μg/l14 samples93 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: drenáž1992, 2.6 km from the water. Comparison: percentile 87 of all samples in Slovakia.

• ArsenicAsslightly elevated
  highest 1.20 μg/lmedian 0.500 μg/l14 samples93 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: studňa1992, 2.1 km from the water. Comparison: percentile 82 of all samples in Slovakia.

• CopperCuslightly elevated
  highest 1.90 μg/lmedian 0.850 μg/l14 samples
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: studňa1992, 2.7 km from the water. Comparison: percentile 75 of all samples in Slovakia.

• ZincZntypical value
  highest 115 μg/lmedian 8.50 μg/l14 samples
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: studňa1992, 2.3 km from the water. Comparison: percentile 73 of all samples in Slovakia.

• IronFetypical value
  highest 0.00500 mg/lmedian 0.00500 mg/l1 sample100 % below the limit of quantification
  1. up to 50 %
  2. 50–75
  3. 75–90
  4. 90–99
  5. above 99

  Highest value: prameň1992, 2.3 km from the water. Comparison: percentile 50 of all samples in Slovakia.

Radon in waters

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.

94 boreholes in the 3 km zone, of which 27 hydrogeological and 67 other; with an archive report number 94.

Borehole depths

• up to 10 m71×
• 10–30 m8×
• 30–100 m0×
• 100–300 m0×
• over 300 m1×

Nearest boreholes

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

Environmental burdens, landfills and anthropogenic sediments

Recorded environmental burdens (industrial sites, landfills, mining), the register of waste landfills and monitoring of anthropogenic sediments (industrial sludge). It is a list of places, not a measurement of water pollution.

Environmental burdens

Waste landfills

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

• Landslides8×

Degree of activity

• Potenciálny7×
• Stabilizovaný1×

Current state

• Processed only in the scope of registration on a scale of 1:25,0004×
• SD taken from archival materials, ktorá bola konfrontova2×
• SD zaregistrovaná v rámci terénneho výskumu na úlohe Atlas S1×