Metadata 1687
Concentration on flow, for Sarmatian aquifer in Dobrogea de Sud, Romania
Digital records of seismological stations of the Czech Regioanl Seismic Network (CRSN). The network consits of twenty broadband stations on the territory of the Czech Republic. Seismic stations are operated by the following geoscience institutions: Institute of Geophysics CAS (10 stations), Institute of Rock Structure and Mechanics CAS (3 stations0, Institute of Physics of the Earth MU Brno (4 stations), Research Institute of Geography, Topography and Cartography Zdiby {1 station), Charles University Pragu...
Digital records of seismic stations of the Czech RegionalSeismic Network operated by the Institute of Geophysics CAS in Prague.
Seismic digital records of the Czech Regional Seismological Network - stations operated by the Institute of Geonics
ArcGIS Server service provides an access to basic information about the geophysical networks of the CzechGeo consortium.
The database contains information on two dozen geophysical networks operated by czech geoscience institutions of the CzechGeo consortium (institutes of the ASCR, faculties of universities, etc.) in the Czech Republic and abroad. There are observatories, permanent stations and measuring points of campaigns (seismic, GPS, magnetic, gravimetric and geodynamic), connected to local and global data networks.
Seismické digitální záznamy stanic České regionální seismické sítě - stanice provozované Ústavem fyziky Země Přírodovědecké fakulty Masarykovy univerzity.
D layer represents depth to groundwater table from the surface, where values are reclassified values into D index values from 1 to 10.
The D layer is the depth to the water table from the surface. The Boyne study area is based on 401 historical water level data points along with spring data and data from groundwater surface water interactions. Spatial interpolation using kriging was used and then the values were classified into the D index values. The highest D values correspond to where the water table is shallowest, generally found in the lower areas in the catchment, with the lowest D values meaning greater depth to the watertable, fou...
D layer represents depth to groundwater table from the surface, where values are reclassified values into D index values from 1 to 10. High values of "D" factor correspond mostly with alluvial aquifers in NE part of the area where shallow groundwater prevails. Low values correspond mainly with steepest mountainous areas and deeper aquifers.