HCOV_1300, top of the plinth
Description
Flanders is made up of an alternation of aquifers (sand, gravel, chalk, solid rock, ...) and regionally occurring non-aquifers (e.g. clay). The sequence of these aquifers and aquitards has its own coding in Flanders: the Hydrogeological Coding of the Subsurface of Flanders (HCOV-coding). The HCOV coding is made up of hydrogeological main, sub and base units. The main unit groups a sequence of geological layers that have broadly the same hydrogeological properties and thus form a single whole. HCOV_1300 (Socle) includes the geological formations of the Primary that form the pedestal. More specifically, the layers of the Carboniferous, Devonian and Cambro Silurian. The dataset ‘HCOV_1300, top of the plinth’ shows in a grid per grid cell the elevation value (in m TAW) of the upper limit of this hydrogeological layer.
Resources
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25 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/cbd1eded-66ff-4589-b0ab-32555d489c74 |
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0 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/cbd1eded-66ff-4589-b0ab-32555d489c74 |
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0 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/cbd1eded-66ff-4589-b0ab-32555d489c74 |
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0 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/cbd1eded-66ff-4589-b0ab-32555d489c74 |
Tags
- geologie
- 1300
- vmm
- sokkel
- vlaanderen
- hcov
- ondergrond
- dov
- databank-ondergrond-vlaanderen