Metadata 1677
Cone penetration tests (CPT) are used in geotechnical engineering. The test involves pushing a cone-shaped probe into the seabed. As the cone penetrates the sediment, it records data on cone resistance, sleeve friction, and pore water pressure. This layer shows places (polygons) where data can be downloaded directly from this website. The data package that is downloaded will typically contain data from many CPT sites and may also include other types of data besides CPT data. The file format will typically ...
Applications shows results of SQL query to Minerals Occurrence database.
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.