HCOV_0600, Prevention area of the Ledo-Paniselian-Brusselian Aquifer 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. The Aquifer system formed by the various sand layers of the Formations of Maldegem (Member of Wemmel), Lede, Brussels, Aalter and Ghent, is an important water-carrying system in Flanders.
Resources
| Name |
Format |
Description |
Link |
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17 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/c22aeb51-94a2-4fb7-9a53-42deace66a13 |
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0 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/c22aeb51-94a2-4fb7-9a53-42deace66a13 |
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0 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/c22aeb51-94a2-4fb7-9a53-42deace66a13 |
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25 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/c22aeb51-94a2-4fb7-9a53-42deace66a13 |
Tags
- ledo-paniseliaan-brusseliaan-aquifersysteem
- vmm
- vlaanderen
- hcov
- 0600
- ondergrond
- dov
- databank-ondergrond-vlaanderen