Metadata 1660
Forests and wetlands form sedimentary environments where organic-rich material accumulates with time, thus forming natural archives. Remains of macroscopic plants, pollens, insects and other organisms can be preserved in these sediments. These are frequently used to reconstruct palaeoclimate records using various proxy techniques.
Overlying layers, for Sarmatian aquifer in Dobrogea de Sud, Romania
Groundwater uses, which might limit the use of shallow geothermal energy
This factor takes into account the amount and frequency of precipitation in the study area. Annual average precipitation is fairly uniform across the pilot area and was assigned a value of 0.2. The average number of rainy days for this pilot is 225, which results in a low intensity value for for precipitation and an overall low reduction of protection ‘P’ score overall
P 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 annual precipitation and average rainfallin the wet years. Vulnerability classes are: 0.4-0.5 Very High, 0.6 High, 0.7 Moderate, 0.8 Low, 0.9-1 Very low.
A palaeo-alluvial plain is defined as a largely flat landform created by the repeated deposition of alluvial sediments over a long period of time by running water. 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.
A palaeo-alluvial plain is defined as a largely flat landform created by the repeated deposition of alluvial sediments over a long period of time by running water. 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.
Coastal Landforms created during periods of lower sea level. These features may or may not be submerged today (e.g. as a result of isostatic rebound). Where possible these have been subdivided into the type of Coastal Landform e.g. Beachrock, Littoral deposit, Coastal dunes, Cliff, Sand bars, beach ridges, Other. Where information is available on the genesis of the beach deposit this has been provided, e.g. foreshore sediment, aeolian sediment (e.g. dunes). Where information on sediment grain size and comp...
Delineation of Coastal Landforms created during periods of lower sea level. These features may or may not be submerged today (e.g. as a result of isostatic rebound). Where possible these have been subdivided into the type of Coastal Landform e.g. Beachrock, Littoral deposit, Coastal dunes, Cliff, Sand bars, beach ridges, Other. Where information is available on the genesis of the beach deposit this has been provided, e.g. foreshore sediment, aeolian sediment (e.g. dunes). Where information on sediment grai...
Delta Relict delta landform formed by deposition of sediment transported via river as it enters slower-moving / stagnant body of water such as a marine environment, lake or estuary. 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