HCOV_0400, Oligocene Aquifer System Prevention Area
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. This hydrogeological main unit comprises the complete aquifer system between the closing layers of the Boom clay (Formation of Boom) and the Bartoon clay (Formation of Maldegem). This is a sequence of aquifers, whether or not in contact with each other, separated by non-continuous clay layers of limited size. This main unit is formed by the layers belonging to the Formations of Bilzen, Borgloon, Sint-Huibrechts-Hern and Zelzate.
Resources
| Name |
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Description |
Link |
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25 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/b7e46b38-c67b-46df-9741-f465855ed02e |
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17 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/b7e46b38-c67b-46df-9741-f465855ed02e |
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0 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/b7e46b38-c67b-46df-9741-f465855ed02e |
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0 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/b7e46b38-c67b-46df-9741-f465855ed02e |
Tags
- vmm
- vlaanderen
- hcov
- ondergrond
- dov
- databank-ondergrond-vlaanderen