Metadata 1844
Submerged accumulation of partially decayed vegetation or organic matter. 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
Submerged springs are a common groundwater discharge feature of the karst aquifers along the Mediterranean coast. They form in karst areas where, during previous geological periods, the sea level has risen, or the shoreline lowered.
Areas of relict wetland. Where known the type of wetland is included e.g. salt marsh, tidal flat, peat bog, supra tidal zone, swamp, other. 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.
Any subsurface installations, which might lead to conflicts with drilling wells and borehole heat exchangers.
Iso-content maps of Sulphur (S), one of the chemical elements.obtained in the Geochemical Atlas of Spain Project, distributed in stream sediments (14,864 samples), superficial soils (0-20 cm.) (13,505 samples) and deeper soils (20-40 cm.) (7,682 samples). The results of the chemical analysis are shown in two types: total dissolution of the sample with 4 acids and partial dissolution with aqua regia. With the analytical results of all the sampled points, an isocontent map is made with adjustment to a square...
The superficial deposits data uses polygons to show the extent of deposit-types (also named soil types), classified after their formative process. Line- and point-symbols show smaller occurrences of superficial deposits, as well as landforms and other geological observations. The data shows which superficial deposit type dominates the upper meter of the terrain surface, but other sediment types may occur deeper in the substrate. The data also shows areas with exposed bedrock without sediment cover. Exampl...
The superficial deposits data uses polygons to show the extent of deposit-types (also named soil types), classified after their formative process. Line- and point-symbols show smaller occurrences of superficial deposits, as well as landforms and other geological observations. The data shows which superficial deposit type dominates the upper meter of the terrain surface, but other sediment types may occur deeper in the substrate. The data also shows areas with exposed bedrock without sediment cover. Example...
The superficial deposits data uses polygons to show the extent of deposit-types (also named soil types), classified after their formative process. Line- and point-symbols show smaller occurrences of superficial deposits, as well as landforms and other geological observations. The data shows which superficial deposit type dominates the upper meter of the terrain surface, but other sediment types may occur deeper in the substrate. The data also shows areas with exposed bedrock without sediment cover. Example...
Sediment data show mainly the prevalence of soil types covering the bedrock surface for whole Norway. Most of the soils were formed during and after the last ice age. The data shows only the soil that dominates in the upper meters of the terrain surface. Thick and thin layers by other soils may occur further down in the soil profile. The dataset was first published i 1990, and updated in 2013.
The map of Quaternary deposits of Finland at 1:1 000 000 scale depicts the main features of the Quaternary geology of Finland. The dataset consists of areas defined according to deposit type and genesis.
