Metadata 1667

Zharmonizowany zbiór danych przedstawia odwierty na obszarze Polski. Zbiór danych jest zgodny z modelem INSPIRE Geology – Boreholes.

Zharmonizowany zbiór danych przedstawia odwierty na potrzeby szczelinowania hydraulicznego na obszarze Polski. Zbiór danych jest zgodny z modelem INSPIRE Geology – Boreholes.

GeoMol Pilot Area Upper Austria - Upper Bavaria: Map of oil and gas deposits (active and inactive/depleted), lateral extension at the oil/gas-water interface. Map derived from the information provided by the regulatory agency projected into the 3D geological model as prepared in the GeoMol Project. Details in the Project Report http://www.geomol.eu/report/

Forests and wetlands form sedimentary environments where organic-rich material accumulates with time, thus forming natural archives. Remains of macroscopic plants, pollens, insects and other organisms can be preserved in these sediments. These are frequently used to reconstruct palaeoclimate records using various proxy techniques.

Overlying layers, for Sarmatian aquifer in Dobrogea de Sud, Romania

Groundwater uses, which might limit the use of shallow geothermal energy

This factor takes into account the amount and frequency of precipitation in the study area. Annual average precipitation is fairly uniform across the pilot area and was assigned a value of 0.2. The average number of rainy days for this pilot is 225, which results in a low intensity value for for precipitation and an overall low reduction of protection ‘P’ score overall

P map in Slovenia represents one layer of vulnerability map COP in Slovenia that has been applied on the area covered by karstic rocks. The map is constituated from annual precipitation and average rainfallin the wet years. Vulnerability classes are: 0.4-0.5 Very High, 0.6 High, 0.7 Moderate, 0.8 Low, 0.9-1 Very low.

A palaeo-alluvial plain is defined as a largely flat landform created by the repeated deposition of alluvial sediments over a long period of time by running water. Chronological information is presented as calendar age BP. Confidence is defined as follows: 1. High: Sampled feature with good age and palaeoenvironmental control. 2. Sampled feature with poor or none age and palaeoenvironmental control. 3. Constructed by remote sensing data only. 4. Low: Reasonable without any direct evidence.

A palaeo-alluvial plain is defined as a largely flat landform created by the repeated deposition of alluvial sediments over a long period of time by running water. Chronological information is presented as calendar age BP. Confidence is defined as follows: 1. High: Sampled feature with good age and palaeoenvironmental control. 2. Sampled feature with poor or none age and palaeoenvironmental control. 3. Constructed by remote sensing data only. 4. Low: Reasonable without any direct evidence.