HCOV_0500, basis of the Bartoon Aquitard system
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_0500 (Bartoon Aquitard system) includes the closing layer formed by successive clay layers belonging to the Formation of Maldegem. This includes some sand layers that are hydrogeologically very different from the clay layers, but they are too limited in dimension to play a major hydrogeological role. The dataset ‘HCOV_0500, basis of the Bartoon Aquitard system’ shows in a grid per grid cell the elevation value (in m TAW) of the lower limit of this hydrogeological layer.
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/0b272c57-b305-4b02-b585-4ec3a499ecba |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/0b272c57-b305-4b02-b585-4ec3a499ecba |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/0b272c57-b305-4b02-b585-4ec3a499ecba |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/0b272c57-b305-4b02-b585-4ec3a499ecba |
Tags
- geologie
- vmm
- vlaanderen
- 0500
- bartoon-aquitardsysteem
- hcov
- ondergrond
- dov
- databank-ondergrond-vlaanderen