Metadata 1657
This is PSI data for Santo Stefano d'Aveto, Italy. It has been provided by TRE as part of the ESA funded Terrafirma project.
This is PSI data for Santo Stefano d'Aveto, Italy. It has been provided by TRE as part of the ESA funded Terrafirma project.
Iso-content maps of Scandium (Sc), 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 squa...
Within EMODnet Geology, the German Federal Institute for Geosciences and Natural Resources (BGR) is leading the workpackage “Seafloor Geology” to compile and harmonize the European marine geology map data as detailed as possible for the themes – pre-Quaternary and – Quaternary geology; – geomorphology. These three data layers on Seafloor Geology show the underlying geology from Earths ancient past (more than 2500 Million years ago) to modern Quaternary deposits and geomorphological features. From it we can...
Pre-Quaternary -age This web map service shows the chronostratigraphic age of geological units of the seafloor originated earlier than 2,588 Ma from now (pre-Quaternary). International Geological Map of Europe and Adjacent Areas (Asch, 2005). The scale varies between 25,000 and 5 000 000. The data were compiled by BGR from the EMODnet geology partner organisations in the EMODnet Geology project phases I, II and III between 2009 and 2019. Pre-Quaternary -lithology This web map service shows the rock type (l...
This web map service shows faults and structures of geological units of the seafloor originated earlier than 2,588 Ma from now (pre-Quaternary). The data were compiled by BGR from the EMODnet geology partner organisations in the EMODnet Geology project phases I, II and III between 2009 and 2019 and the International Geological Map of Europe and Adjacent Areas (Asch, 2005). The scale varies between 1:200 000 and 1:5 000 000
Quaternary –age This web map service shows the chronostratigraphic age of geological units of the seafloor originated in the Quaternary period (i.e. 2,588 Ma from now until today). The data were compiled by BGR from the EMODnet geology partner organisations in the EMODnet Geology project phases II and III between 2009 and 2019. The scale varies between 20 000 and 2 500 000. Quaternary -lithology This web map service shows the rock type (lithology) of geological units of the seafloor originated in the Quate...
The data were compiled by BGR from the EMODnet geology partner organisations in the EMODnet Geology project between 2017 and 2021.The scale varies between 10 000 and 5 000 000.
Primary and Secondary Sea Level Index Points. Where information is available on the genesis of the index point it is given. 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
The past position of sea level over space and time can be defined by what is termed the Sea Level Index Points (SLIPs), which are characterised by the following fundamental fields: a) geographic location (latitude and longitude); b) age (traditionally determined by radiometric methods, e.g. radiocarbon or U-series dating); c) the altitude (preferably relative to a national levelling datum); and d) the vertical relationship a contemporaneous tide level.