Metadata 1644
Growing demand for materials suitable for decorative and building purposes has contributed significantly to the development of the mining and stone-processing industry. This database contains basic types of rocks that have been quarried for these purposes in the Czech Republic in past and presence.
Growing demand for materials suitable for decorative and building purposes has contributed significantly to the development of the mining and stone-processing industry. This database contains basic types of rocks that have been quarried for these purposes in the Czech Republic in past and presence.
Readings of seismic events (earthquakes, mining induced events, explosions) in the Czech Republec and worldwide of seismological stations of the Czech Regional Seismic Network. Data from 1976 to present are stored in monthly files. Older annual bulletins from 1908 to 1954 are available in the pdf format.
Měsíční soubory čtení časů příchodu seismických jevů z celého světa ze stanic JAVC (od r. 1997), KRUC (od r. 1997), MORC (od r. 1995) a VRAC (od r. 1993), provozovaných Ústavem fyziky Země PřF Masarykovy univerzity Brno.
Created using karst information for Rockingham Catchment Region in the West of Ireland. The catchment for each swallow hole was delineated and distance from each swallow hole was calculated within the catchment. These were assigned the appropriate value according to COP methodology. The slope and vegetation types within and outside that catchments were also assigned appropriate values.
C layer represents hydraulic conductivity of hydrological units and direct assignment of C index to each aquifer.
The Hydraulic conductivity layer is taken as a direct assignment of the hydraulic conductivities from the aquifer parameter database to the C index values according to DRASTIC, ranging from 1 to 10
C layer represents hydraulic conductivity of hydrological units (from cp map Kennesey) and direct assignment of C index to each aquifer. Higher values of C correspond to alluvial aquifers, and smaller values to metamorphic and igneous rocks.
The Hydraulic conductivity layer is taken as a direct assignment of the hydraulic conductivities from the aquifer parameter database to the C index values according to DRASTIC, ranging from 1 to 10.
C 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 calcualation of distance to swallow holes and sinkihg streams, slope, high and low vegetation cover. Vulnerability classes are: 0-0.2 Very High,0.2-0.4 High, 0.4-0.6 Moderate, 0.6-0.8 Low, 0.8-1.0 Very low.