Metadata 1692

This digital soil map shows the geology 1 meter below surface, just beneath ploughing- and culture layers. The map is digitized from redrafted maps originating from fieldwork, where soil samples are collected using a charting spear in a 100 m grid throughout the country. This map is a result of systematic geological mapping, and is an ongoing effort.This version 4.0 from 2015 classifies 88 % of Denmark's area. The legend shows 82 different soil types. The map is used for research, in relation to environme...

The dataset has been created by combining, generalizing and vectorizing information from maps of bedrock and Quaternary sediments of at 1:200 000 and 1:50 000 scales. The areas depicted on the map correspond in age, genetic type and lithological composition to the sediments and rocks lying directly under the topsoil layer. In other words, the map shows the distribution and composition of Quaternary sediments, including small alvar areas with bedrock outcrops.

The dataset incorporating information about the surface geology of Finland is a seamless presentation of the surface geology depicting the distribution of both Quaternary and Pre-Quaternary deposits. Soil cover is omitted. The bedrock outcrops in the map of Superficial Geology at a scale of 1:1M are replaced by data from the Bedrock Map of Finland at a scale of 1:1M.

The dataset for the Surface Geology of Ireland at a scale of 1:1M was created by generalizing Quaternary mapping at a scale of 1:50 000 published by the GSI and incorporating information from 1:70 000 scale digital mapping of the subsoil by Teagasc.

Likelihood of occurrence (below seafloor) of marine hydrates in the sediment column, and subsequently the likelihood of them being affected by dissociation processes resulting from natural or human-induced activities (liquefaction, explosions, collapse, crater-like depressions or submarine landslides). Reference: https://doi.org/10.3390/app11062865

The database containing information on mineral and energy resources of Poland and the exploitation of deposits. It provides access to information on: - deposits (deposits details, data on raw material, deposits resources and output); - mining areas and mining countries as well as related concessions; - mineral resources management (domestic export and import of ra materials, world production, demand, export and import of selected raw materials); - deposits location on the map of Poland.

The aquifer media layer is created by calculation of the slope value from the national topographic data. S values were classified into DRASTIC S values from 1-10. Due the generally flat topography, the majority of the catchment is assigned the higher ‘T’-values.

The topography layer is created by calculation of the slope value from the national topographic data. S values were classified into DRASTIC S values from 1-10. Due the generally flat topography, the majority of the catchment is assigned the higher ‘T’-values.

T layer represents topographical information, where calculation of the slope was effectuated and represented in rasterfile, reclassified into T index values.

T layer represents topographical information, where calculation of the slope was effectuated and represented in rasterfile, reclassified into T index values. The highest values correspond to low slope areas (alluvial aquifers) and the highest values correspond to steepest areas in mountains.